SCIENTIFIC ABSTRACT GALPERIN, YE.A. - GALPERIN, YE.I.

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• Collection: Scientific Abstracts
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• Release Decision: RIF
• Original Classification: S
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• Document Creation Date: November 2, 2016
• Document Release Date: July 19, 2001
• Sequence Number: 5
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

41 7 JL)t_WV
ACC NR: AP6000544
A special form of the nonanalytic Lyapunov function satisfying the theorems oniasymp-
totic stability is constructed and the stability of the simplified system is analyzed
on the basis of the general theory of stability and the special methods for con-
structing the regulators. Conditions under which the construction of regulators
ensuring the asymptotic stability, of such nonlinear control syst=s Is possible and
v,hen it is impossible are established. An example illustrating the theory'is pre-
sented. Orig. art. has: 65 formulas. (LKI
SUB CODE: 12/ SUBM DATE: 06Nov65/ ORIG REF: 009 ATD PRESS:

SOV/ 1137- 58-9-20021 D
Translation from: Referativnyy zhurnal, Metallurgiya, 19i8, Nr 9, p Z75 (USSR)
AUTHOR: GaPperin, Ye.A.
TFFLE- /Changes in the Crystal Structure of Steel Under Cold and I-lot
Working (Izmeneniye kristallicheskoy struktury stali prt
kholodnoy i termicheskoy obrabotkakh)
ABSTRACT: Bibliographic entry on the author's dissertation for the de-
gree of Candidate of Physical - Mathematical Sciences, pre-
sented to the Leningrad. gos. ped. in-ta im. A.1. Gertsena
(Leningrad State Pedagogical Institute im. A.1. Gertsen,
Leningrad, 1958
ASSOCIATION: Leningrad. gos. ped. in-ta irn. A.I. Gertsena (Leningrad
State Pedagogical Institute im. A.I. Gertsen ), Leningrad
1. Steel--Crystal structure 2. Steel--Deformati4on 3. Crystal
structure--Temperature factors
Card 1/1

(110o'k-'J'a)
Stabilization of the steady-st.jite nio,Jan of a nonlinear controllable
system in the critical case of a pair of purely ima,-,inary roots.
Prikl. mat. i raekh. 29 no.6:1070-1080 N-D 165.
(!,! I -T LA 19 : --- 11
1. Submitted Nlovember 6, 1965.

BALZHI, M.F.; BERFZKIN, P.N.; GOLIDSHTEIN, Ya.Ye.; OALIPEPJN, Ye.B.;
YEDLICHKO, V.V.; KERAS, A.F.; LEKUS, I.D.; POTRTJTn1N-'ff.-T';
FOZDNYSHOV, V.M.; 51JE-BOTINO N.A.; SAVINT-3EV) R.I.; TAMARG113KIYj
V.M.; SHEREMETIYEV, A.D.; BAKSHI, O.A., kand. tekhn. nauk,
retsenzent; BONDIN, Ye.A., inzh., retsenzent; EOYKO, F.I., inzh.,
retsenzent; VASIN, Yu.P., inzh., retsenzent; LAZAREEV, A.A., inzh.,
retsenzent; SOROKIN, A.I., inzh., retsenzent; KONtKOV, Arkadiy
Sergeyevich, dots., red.; DUGINA, N.A., tekhn. red.
[Economy of metals in the machinery industry]Ekonomiia metallov
v mashinostroenii. (By]M.F.Balzhi i dr. Moskva, Mashgiz, 1962.
235 P. (MIRA 16:2)
(Machinery--Design and construction)
(Metals, Substitutes for)

USSR/Geophysics - Seismic correlation method
Card 1/1
Author Gamburtsev, G. A., and Gallperin, Ye. I.
Title Proceduzes followed in operations conducted in accordance with the correlation
method for the study of earthquakes
Feriodical Izv. AN SSSR, Ser. geofiz. 1, 3-10, Jan/Feb 1954
Abstract Describe two modifications of the correlation method for studying earLh-
quakes (KMIZ) in application to the problem of investigating the terri-
torial distribufion governing the foci of local; very weak, high-frequency
seismic shocks-1 Consider the problems concerning apparatus, procedures of
field observations and interpretation of their results. Refer to their
previous reports appearing in Doklady Akademii Nauk SSR, 1952-1953-
Institution : Geophysics Institute, Academy of Sciences, USSR
Submitted : August 20, 1953

FD
USSR/Geophysics Seismic observations
Card 1/1
Author Gamburtsev, G. A.) and Gal'Perin, Ye. I.
Title Azimuthal seismic observations with inclined seismographs
Periodical : Izv- AIN SSSR, Ser. geofiz. 2, 184-189, Mar/Apr 1954
Abstract : Describe a procedure for observing earthquakes by means of an azimuthal set-
up with inclined seismographs. Demonstrate the superiority of set-ups of
this type in comparison-with azimuthal set-ups with horizontal and one ver-
tical seismographs. Present examples of the recording and determination of
the direction of the displacement vector of soil for local earthquakes in
the region of Pamir in 1953. Two references, both in Doklady Akademii Nauk
SSSR, 1953-1954, by G. A. Gamburtsev.
Institution : Geophysics Institute, Acad Sci USSR
Submitted : January 7, 1954

6o-29-1//14
AUTHORS: Zapol'skiy, K.I., Gallperin, Ye-I., Borlsevich, Ye. S.
TITLE: Mobile Experimental Low-f re(jUe-fi-cy -Seismic Stations
(Opytnaya peredvizhnaya nizkochastotnaya seysmicheskaya
stantslya)
PERIODICAL: Trudy Geofizicheskogo instituts AN SSSR, 1955, Nr 29,
Pp. 3-10 (USSR)
ABSTRACT: The authors describe apparatus developed to investigate
multichannel registration of near earthquakes In the frequency
range of 1-25 cps. The station consists of a low-frequency, 12-
channel seismic unit "O/7HC" motmted on a "TAZ-51" truck. Each
channel consists of a seismograph, an amplifier and a galvanc-
meter. The general characteristics of the filter-amplifier sys-
tems and auxiliary measuring and registering instruments are
described in detail. Field experiments conducted in 1950 In the
area of northern Tien Shan demonstrated the effectiveness of
these stations. The station may also be used to register explor-
atory explosions. There are 7 figures and 4 references of which
3 are*USSR and I English.
AVAILABLE: Library of Congress
Card 1/1-

GAIPERIN, YL L, MIRONOV, A. V. and SHEFOV, N. 14.
"Spectographs for the Study of Atmospheric Emission During the LG.Y. of
1957-1958.11 paper read at the 7th International Astrophysical Colloquilim,
Lie#e, 12-14 Jul 1956.
A short description of spectographs or large focal ratios for
studies of the night sky and aurorae is given.
so: 568946

GALIPSHIN, Ye.I.
Solution of'io-46&rd space problems of a geometric seismic ways for
multistrata media with arbitrary demarcation boundarlen. Jzv.AN
SSSR.Ser.goofiz. no.4:391-403 Ap '56. O= 9:8)
1. Akademiya nauk SSW, Geofizicheskly institut.
(seismology)

GALIPHRIN, Ye.I.
,-,_ - I- 'Azimuthal declination of seismic rays. Izv. AN SSSR,Ser.geofiz.
no.11:1282-093 N '56* ( KLRA 10:1)
1. Akademiyz nauk SSSR GeOfi2icheskiy institut.
(Seismic waves)

GALM IN) Ye . I . , -_`a3YACTjEV A . 'V . and ZV.ITZ V, S . N..
"Crustal Structure Researches in the Transition ReSion from the Asiatic
Continent to the Pacific." (Sub-title - "The Pacific Goologo-Geophyeical
Expedition.")
IBM Academy of Sciences, 1957; XII Seismology, No. 1, 31 PP. (Russian)
Special Commtttee for the International Geophysical Year.

44
AUTHOR: Aksenovich, G. I., Gallperin,"(E. I., Zayonchkovskly, M.A.
TITIE: Special features of an apparatus for deep seismic pro-
bing and results obtained in testing it. (Osobennosti
apparatury dlya glubinnogo seysmichesicogo zondirovaniya
I rezul'taty ee oprobovanlya).
ITRIODICAL: Izvestiya Akademii Nauk S I Geofizicheskaya, 1957,
(U.j.,er. a
No.2, pp. 184-189. R T
ABSTRACT: Apparatus Is described for recording seismic waves pro-
duced by relatively small explosions, using 50 - 300 kg
explosives, at distances of up to 400 km from the
explosion point. This apparatus is based primarily on
work carried out In Northern Tyan'-Shan' in 1949 and
1950 by the authors and other members of the Geophysics
Institute of the Ac.Sc. Information on the experimental
apparatus has been published previously (10). It was
found that the predominant spectrum of the frequencies of
seismic waves at distances of 150 to 300 1cm changes
little and the predominant frequencies vary between 8
Card 1/2 and 15 C.P.S.

44
TITLE: Special features of an apparatus for deep seismic pro-
bing and results obtained in testing it. (Osobennosti
apparatury dlya glubinnogo seysmicheskogo zondirovaniya
I rezul'taty ee oprobovaniya).
The individual components of the apparatus are briefly
described, namely, the seismographs, the amplifiers and
the time marking circuit. A few seismograms obtained
at various locations (Tyan'-Shan', Bashkiriya, Turkmenia,
Pamir) are given
The text includes 2 graphs, 1 diagram and 4 sets of seis-
mograms. There are 18 references, of which 17 are Slavic.
ASSOCIATION: The Academy of Sciences of the USSR, InstJtute of Terres-
trial Physics (Akademiya Nauk SSSR, Institut fiziki zemli).
PRESENTED BY:
SUBMITTED: 5/23/56
AVAILABLE: Library of Congress
Card 2/2

VEITSMAN, P.S,; GALIPIRIN, Ye.j.
- ~'.
Studies on the structure of the garth's crust on the territor7
between the Asiatic continent and the Pacific Oceaa. M9zhdunar.
geofiz. god no-3:76-82 157. (MM 11:5)
(Sakhalin region-Urth-Surface)
(Kurile Islands-lkrth- Surface)

AUTHOR; Gallperin, Te. 1. 49-9-1/13
TITLE: Grouping of the fir t type and method of obtaining multi-
component azimuth seismograms. (Gruppirovaniye pervogo
roda i sposob polucheniya mnogokomponentnvkh azimutallufth
seysmogramm).
PERIODICAL: Ivestiya Akademii Nauk SSSR, Seri a Goofizicheakaya,
1957, No.9, pp.1081-1098 + 3 plates. ~USSR)
ABSTRACT: The objebt of this paper is to describe a method of
grouping of the first type based on changing the directioAal
diagram of the first type, i,e. on the displacement of a
particle at a given point during passage through it of a
wave. Such grouping is referred to as point or azimuthal
grouping and in such grouping the signals are summed of
seismograpUs located in one point but orientated in
different directions in space. Whilst grouping of the
second type is linked with the direction of the approach
of the wave, grouping of the first type is linked with the
direction of the displacement of the particle. Fundamental
equations in grouping are the equations determining the
directional diagram of the group,which in turn is determined
by the shape and direction in space of the axis of maximum
Pard 1/4- sensitivity and by the amplitude. A method of grouping of'
-Tip

49.9.1/
Grouping of the first type and method of obtaining multi-componen
Y
azimuth seismogram .
the first type (azimuthal grouping) is proposed which permits
changing the direction of the axis and the sensitivity of
the directional diagram of the group. Equations are derived
of azimuthal grouping and a method has been worked out for
obtaining multi-component azimuth seismograms by means of
small component (3 to 4) azimuth equipment. A brief
description is given of the apparatus (polarisation seismic
analyser) and azimuthal seismograms are derived which were
obtained by the proposed method. In para..1 the direction
of the axis of the directional diagram of the group is
considered as a two-dimensional and as a three-dimensional
problem, investigating methods of changing the direction of
the axis of the total directional diagram. With changing
of the direction of the axis there will also be a ckange in
the amplitude of the diagram which is determined by.the
sensitivity of the reference seismograph. Pars.2 deals with
the problem of the amplitudes of the directional diagrams of
groups. In para,3 some particular cases are studied whick
are used for analysing the derived equations, namely, the
following: four-component conical set-upwjth7S450tnClinatIon
'ar-I 2/kangle td the horizontal of the seismographs; three-component

49-9-1/13
Grouping of the first type and method of obtaining multi-component
azimuth seismograms.
set-up of seismo6q.-aplis xyz; three-component symmetrical
arrangement of inclined seismographs; example of comparison
of multi-component azimuthal seismographs by the method of
azimuthal grouping. Para. 4 deals with the possible
applications of azimuthal groupings; in para. 5 a brief
description is given of the apparatus used for azimuthal
grouping showing the block schematics of the polarised
seismic analyser (Fig.11); Fig.14 shows a comparison of
twelve-component real azimuthal seismograms (channels 1-12)
and of reference seismograms (channels 13-24), whereby the
angle of inclination of these seismograms is 450. It was
found that in grouping of the first type., azimuthal grouping,
the diagram of the direction of -the group coincides in shape
with the diagram of the direction of each seismograph
included in the group and can differ from -the latter only
in orientation and amplitude. The azimuthal grouping
permits increasing the effective sensitivity of the apparatus
and it also permits obtaining multi-component azimuthal
seismogTams corresponding to an arbitrary distribution of
the reference seismographs in the set-up. In addition to
.Card 3/4 purely theoretical interest, these proper-ties can be

49-9-1/1_3
Grouping of the first type and method of obtaining multi-component
azimuth seismograms.
utilised in seismology and seismic prospecting. In
seismology azimuthal grouping can be applied for qualitative
determination of the direction of displacement of longitud-
inal waves and also for studying the parameters of
polarisation of micro-seismic waves for -the purpose of
elucidating the relations between the direction of displace-
ment of the particles and the direction of propagation of
the waves. In seismic prospecting the aximuthal grouping
permits combination of positional and azimuthal correlation
of waves on the seismoSTams and a more detailed study of
the wave chart, particularly for sections having complicated
geological structures. Acknowledgments are made to
A. V. Frolova for carrying out the basic calculations.
There are 16 figures and 13-references, all of which are
Slavic.
SUBMITTED: November 2, 1956.
ASSOCIATION: Ac.Sc. U.S.S.R. Institute of Physics of the Earth.
(Akademiya Nauk SSSR Institut Fiziki Zemli)
AVAILK'BLE: Library of Congress
,-',-Card 4

GALIPERIN, Ye.I.
Method for processing observations on three-dimensional sounding.
Prikl. geofis. no.17:67-75 '57. (MIRK 11:2)
(Prospecting--Geophysical methods)
(Seismic waves)

GORYACHW. A.V.. ZYMM.S.M.; FEDTNSY11T,V.V.,doktQr.
fizUro-matematicheskikh nauk, otv. red.; SILKIII,B.I.. red., izd-va.;
RTLIVA, Tu.V., tol-chn. red.
(Studies on the structure of the Earth's crust in the transition
region from the Asiatic continent to the Pacific; work: of the
Pacific geological and geophysical expedition of the Acade~xy of
Sciences of the U.S.S.R.] Isaledovanis zemnoi kory v oblasti
oerekhoda ot A21.atskogo Irontinenta'k Tikhomu okeanu; rsboty
Tikhoolreanskoi iro=lgkmnoi geologo-goofizichesirni. ekspeditaii AN
SSSR v 1957 g. Moskva. Izd-vo .11md. nauk MR. No. l.LTwelfth
section of the International Gaoohvsical Tear Droeram(selamoloicr)l
III razdel nrogramE7 MGG (sei'mologila) 1958. 25 P. (MIRA 11:10)
Geo-j1.7SJCJL1 Year, 195-e-1958)
(Seiamology--Observat ions)
(Soviet Far East--Geology)

i
2 A A
go
st
i J
Ail

7b. f.11-1,4g Vpers Wre r"4 at tho p"ttAg of tM gaincla"Cel
Ccuslauloo In Utrqcht, Sollsod, 8-12 April 195at
-A ~, 4
i.=t9l. P. (Itscur)
,,at
Crustal dt~t~ According to Us FLON."
.de:
SAVARMKrY, Ye. F. (Vineew)
"teteralmatim of T&rtb*m" Plagaltubs wd latwalty In the tM.'
Rrjicnmm, x . Y. OiLecow)
q~aotltttw Determination and MWtag of Selftle Activity.'
nYLIB-Omm, V. 1. (%Neow)
lutimattom f Displacement I- an ftrtbq-Ww - -9 and of 9muce Dimensions.'
FARE, To. V. (WW, )
'Aboorption cr Statli. mastle Vikestims In lacks.,
(rive or abo stboosse tb* Conference)
go. enroakd4me, a4l IVA, uncl.

T T T -7
"Corplex 'Jeologica and -oloviev an ~,,)Dplex `,,oloE-ica
-jc--,ohysical investigations of the Crustal ';tructure in tl~le
Yone of Transition t,,etween the Aiiatir (,ontinent and the
?,~-cific Ocean."
Paper ~~`resented at CL)AGI Feet:Lng, 30 Jul - 9 'Aug Ff . i'-03,col.-I
11,ailable in Library

70.-:e of Transition "etween the Asiatic
f.
I'Leep ~-eisidc Sounding if, t,
.,C
Coi.-ti ent anri the ~`acific Ocean."
Paper Presented at ,'.7;AGI Eeeting, 30 Jul - 9 Aug 5F, Moscow
Wailable in Librlry

GKLIPERIN, Ye.l.
- oojs_~, - - -
, ~05-30 Studying the structure of the earth's crust In the zone of transi-
e , tion from the Asiatic continent to the Pacific Ocean. Mezhdunar.
geofiz. god no-5:66-73 158. (14IRA 11:10)
(Soviet Far Eaet--lastb--Surface)

I . . .- I I Ir."IWilpliff
SOV/49-58-7-3/16
AUTHORS: Gallperin, Ye.I. and Kosminskaya, I.P.
TITLE: Methods of Seismic Depth Soundings at Sea (Osobennosti
metodiki glubinnogo seysmicheskogo zondirovaniya na more)
PERIODICAL: Izvestiya Akademii Nauk SSSR, Seriya GeofLizicheskaya,
19582 igr ?, pp 833 - 847 (USSR)
ABSTRACT: The best results in determining the composition of the
Earth's c
,rust ere obtained in the USA by employing a
method of th~seismic-depth sounding (S.D.S.) with the
mobile points of detonation and the stationary registration
stations. This method is one of the many which generally
can be classified as follows;
The Method of a Stationary Point of Detonation is used in
the majority of seismic surveys on land and sea. Several
kinds of this method can be distingui.~;hed:
A) Continuous Profile Method - is the most comr-on, also
used in S.D.S. (Figure 1 I-A). This method offers the
foll W1 advantages: 1~ the differentiation of a single
wave. 2 Determination of the wave travel time.
3~ Determination of the wave relative velocity.
4 Continuous recording along the line of observation.
5 Construction of a continuous odo6raph.
(;ardl/10

Methods of Seismic Depth Soundings at Sea SOV/49-5a-7-3/1(5,
B) Partly Continuous Profile Method (Figure 1, I-B) is
employed mostly over large territories, mountains, etc.
The seismic survey is based on the separate tracks with
distances between them much larger than the wavelenEth.
This method gives only the first three of the advantages
listed above.
C) Pointed Registration (Figure 1, I-C) gives the time of
wave travel only by offering tile second and. third of the
above advantages. This method is employed with the stron~-r
detonations.
A quite different method is obtained when the mobile
detonation points and the stationary registration stations
are applied. This method can be divided into tro main
classes, depending whether one or more points of registration
are used:
1) One Point of Registration.
a) Continuous shooting (Figure 1, II-l-A) can be employed
together with the continuous profile mthod. This method
is not largely used due to the difficulties of obtaining
the detonations frequently ~-? nou5h'.
Card2/10b) Partly Continuous Sh6bting kFigure 1, II-l-B) gives

14.ethods of Seismic Depth Soundings at. Sea SOII/49-58-7-3/16
the first three advantages listed above with the possibility
of obtaining a partial wave odograph. It can be employed in
place of the continuous profile method. However, this
method is not much in use owing to ma technical difficulties.
c) Pointed Shooting (Figure 1, II-1-~C has only the first
advantage, i.e. it gives the total travel time of one wave.
2) Multi-point Registration.
This method can be used effectively when there is a
sufficient frequency of the point-to-point registrations -
then the third advantage could be obtained.
Figure 1 shows the above systems grouped as follows: the
top row - stationary point of detonation. The middle and
lower rows - mobile points of detonation. The left column
gives the most efficient methods: the continuous profile
and continuous shooting - the right column - the least
efficient methods: the pointed profile and pointed shooting.
The mi&le column represents the intermediate methods: the
partly continuous profile and partly continuous shooting.
When the detonation and registration points are situated
on land, the best methods employed are 1-A,B. When the
both Doints are at sea the methods II-1 and 11-2 are the
Gard3/10

Methods of Seismic Depth Soundings at.. Sea SOV/49-58-7-3/16
best (especially II-1-0). The method II-2-C is the best
for the work carried out partly on land, partly at sea.
Two methods (II-1-0 and (II-2-C) were applied in the S.D.S.
of' the Caspian Sea in 1956 described below.
Methods of Observations - usually a greater area can be
covered by the mobile detonations method at sea. This,
coupled with the better odographs, better interpretation of
the longitudinal and other profiles -and the DOSsibility of
carrying the survey with fewer points of detonation
(Figure 2), decided in employing this method for S.D.S.
df. the Caspian Sea. Several other points were observed:
the length of profiles ~the length of odographs) was taken
in relation to the depth of the sounding datum, which was
deeper on land (30 - 40 km) and shallower (10-15 km) at s-eaz.
The distance from detonation to registration points was
kept &a 250-300 km on land and 80-100 km at sea.
Distance between the points of detonation and the observation
ships was chosen to allow a group correlation between waves.
This distance was changed along the line of profile. The
Card4/10 distances between the observation ships were determined by

Methods of Seismic Depth Soundings at Sea SOV/49-58-7-3/16
the type of odographs in use - usuallY 50-100 kv. Figure 3
shows one of the odographs prepared for a profile oP the
Caspian Bea.
observations at the detonation point - Experience shovied
that the registrations of the soundwaves received from the
detonations were very useful for the determination of the
various data of sounding, thus helping to separate the field
of the secondary shocks.
Determination of places for ships and detonation points was
carried out by means of the radio,-eodesic methods if the
distance from the shore was not great, otherwise the
c'
velocity of sound in water was applied with SDecial investi-
gation of 1.4ydrorlogtoal conditions of the sea (temT.,erature
and saltiness).
In the intermediate regions between the land and deep sea,
the length of each profile was 3-5 km.
The apparatus used. ror the registration of the seismic
waves at- sea, 'the hydrophones with the amplifier placed next
to the piezo-unit were used. For the secondary intensi-
fication, the usual low-frequency amplifier -was employed.
Gard5/10 A multi-channel registration was applied for the pointed

Methods of Seismic 1jepLh Soundings on Sea S07/4-9-58-7-3/16
method of observation (Figure 4).
Inter-oretation of Sea Observations.
Interpretation of seismic observations was carried out
in two stages: the analysis of seismograms together with
production of wave odogra-phs and the reading of odo~--ra-ohs
~determination of seismic velocities, plotting maps e~c.),
the character of work and the data collected by the mobile
method of detonation is given below.
Types of wave correlation: The analysis of the seiSMOLTPLIS
was based on selecting and detecting of the main seismic
oscillations. A soecial feature of the depth-sounding at
sea was an application of the group vrave correlation, i.e.
working with a Whole group of waves instead of a
wave. This method proved to be much superior in the irivesti-
gation of the crustal thickness.
Detecting of the Main Wave on Multi-channel PositioninC,
Seismogram.
One of the more important methods of detecting tl-,,e wave on
the seismogram was the determination of apparent velocities,
The main wave or a group of waves on the printed seismo-1-ams
Uard6/10

Methods of Depth Soundings at Sea SOV/49-58-7-3/16
was characterised by the quasi-sinusoidal shape of its
tracing and could. be distinguished by its amplitude
(Figure 5). The group of waveE was distinguished by both
the absolute time of travel and the intensity.
Correlation of the Wave Groups on the Joint SeismogrEms
Due to the distances between detonation points at sea being
greater than the length of waves, the correlation of phases
usually was not practical. However, it was i)ossible to
obtain a group correlation by observing the kollowinE
points:
a) Pointed Recordings. To select a group of waves from a
series of pointed. recordings, a method of absolute time
was applied. The travel times of the first waves of a
group were PlOttE-d along the straight line on the odograph
for the longitudinal profile or, along the hyperbolic
curve on the transverse odographs.
A similar shape of the wave group had an equal period of
oscillations; the sa-me length of the group had an equal
number of the separate waves of similar intensity. The
intensity of each composite wave gradually decreased with
Card?/10 an increase of distance.

Methods of Depth. Sounding at Sea SOV/40'--58--/-3/16
A particular difficulty of the pointed method of regi-
stration was the~eparation and detection of waves on some
recordings. In this case, a shane of the recording and
the intensity were considered.
rigures 6 and ? represent the pointed seismoZ:xams obtained
on the transverse ZFiGure 6) and lonGitudinal (FiGure
profiles. Figures 3 aud 8 show the group odographs coti-
structed from the pointed seismograms.
b) Multi-pointed recordings. For detecting the wave
groups and separatinS them from a series of multi-pointed
recordings, the equal apparent velocities and a similar
shape were considered. The straight line odograph was
obtained from the longitudinal profile while the hyperbolic
S-2
odograph was obtained from the tran v_lrse profile. The
apparent velocities from thie separate seismograms were
related to the apparent velocities of the wave front
spreading along the sounding datum.
Change of Wave Group.
The best correlation usually was obtained of the first
waves recorded. However, there were cases when the first
Uard.8/10

Methods of DeDth Sounding at Sea SCV/49-58-7-3/16
waves were changed, i.e. at the inters~-ction of odographs
when the gradient changed or in the case of the fading
wave. The latter case was due to the changes in the
boundary of the sedimentations (Figure 9, group t2) or to
the variations in the core structure (Figure Q., 6roups t-
and t 4)'
Construction of Seismic Cross-section
The other interDretations of the S.D.S. odoeralphs did not
differ much from the usual methods employed in the seismic
survey. The problem of selecting of the medium and strati-
fied velocities was of special importance. More experiments
are needed in this matter but it can be said that the
graphs showing the ratio of the mediwn velocity v to the
depth H and the vertical odograph t(H) could be employed
with advantage.
It should be mted that the method of mobile detonations
was very productive, allowing the analysis of seismoCirams
Card 9/10

Methods of De-Dth Sounding at:. S(-a SOIT/49-58-7-3/16
to be carried out du.-.-ing the periods of obserwition. This
involved an advance 1-lanning and the corrections irade on
the spot for each pr(file, thus improvinc, greatly tLe final
resulls.
There are 9 figures ~.nd 15 references, 13 of vhich are
Soviet and 2 English.
ASSOCIATION: Akademiya-nauk LSSR,Institut fiziki Zenili
(Institute of TErrestrial Physics of the -AS USSR)
SUBMITTED: August 20, 1957
1. Seismic waves--Al.-plications 2. Seismological stations--
Card 10/10 Applications 3. Seismic waves--Recording devices
4. Earth--Wave transmission

, GALIPERIN, Ye.I.; KRASILISHCHIKOVA, G.A.; MIRONOTA, V.I.; FROLOVA, A.V.
-~
Techniques in using stereographic projections for solving three-
dimensional problems ingeometriml seigimolog7. Prikl. geofiz. nD.18:
3-29 '58. (MM 11--5)
(Seismometry) (Projection)

.; owl-i ;yiz u ii u, i !i n, it : ~ !, ,, : , ,, , 4:~. -I -
...
AX33NOVICH. G.1.; G&L'PFARIN, Ye.I.: ZAYONCHKOVSKIT. M.A.; KULIKOV, S.A.
Recording the moment of explosion indeep seismic prospecting.
Razved. i prom.geofiz. no*23:21-30 10. OGRA 11:12)
(Prospecting"Oeop4sical methods)

'rI'i
A-li T EOR S: Gagel I ga..tz! A. Gal Y;~ 5 0 T 2 1
Kosminska-yE., 1. P.
TITLE- The Structure of tha Earth'S Crust the Cr-n'.ral Part- of ~.he
Caspian Sea ag DetEnidnee. by D,7-ep S~IiDlril
zeinnc~y kcry chast-i Kaspiytik,.,E~-, mrrya po dar.--~'lr-
gl,abirmugo seysmich-askogo zc,-.,dir-::-iran4yEj
T) L) ~'O 2 2
PERIODICAL: Doklady Akadem-1-4 mak SSSF, 10--fl, Vol 7
(USSR)
ABSTRACT. Un-ler the In-' e--)
_a+,4 :-1,7.1
AN SSll:.l (.L
U S Sri 4- -1 ~' c. I, e:,-,1 t2wi th t iie 7se uzz r.-yy
.Ls,31edl-vatell~kiy -st4-tul-l (All- i 4 c-, n '17, z ie
ti: Ai~~: 9,i

I is i-.i T)r. 1"".7 0. A a~

AN SSSR
k
AS USSR) dr~vi3ed tsB-', ap-a:.~atvsDs ancl
.
I s
F) fro r
bc
t (F
,
i
m .e
a
a
"
Hle

f t 3 c Ei. D .2 Sc
t Th e e,-. u F
f
f m c: t h the ani b,
fold, n
j
u r
E.
J - 71 f
1
1 1
C) L In' 2 of 20-251 th-*--l'
ai-aa c-..C t ~;.n I is all-out
k:i In
e. u n t a,. 1 d ol-dtad
Ca-~! 2/13 s 1;

of 'he Earth's Cris~. in the Cer~-re7
Pa::,t of t-he Caspian Sea as Dete:mined by Deep Soisr.f.r. Sounding
the sedimentary (r.:,re than 20 km and 't",-,e The
great thickness o '' the sedimentary layer and the thin
granite layer may be characteristic of oertaf_n Zones of slp_:-D.~_
"alding which haw in the past intense -'old-;.,-.g and
even now are unde:tgoing folding. There are 2 figures and
Soviet references,
PRESEDITED: Ju-na 26, 1958, by N. S. Shatsk-Ly, Lcadmician
SUBMITTED: Jume 9, 1959
Card 3/3

S/169/61/000/012/001/089
D226/D305
AUTHOR: Veytsman, ~-? S Gallperin, Ye. I., Zverev,
Kos-ninsi~y-a-,71. P., and Krakshina, R. M.
TITLEP: Sote data Dn the structure of the crust in the
transitional zone from the Asiatic Continent to
the Pacific Ocean
PERIODICAL: Referativmyy zhurnal, Geofizika, no. 12, 1961,
5, abstract 12A34 (V sb. Geol. resultaty prikl.
geokhimii i geofiz. Razdel 2. M.p Gosgeol-
tekhizdat, 1960, 37-42)
TEXT: Complex geophysical research was carried out on the
structure of the crust in the transitional zone from the Asiatic
Continent to the Pacific Ocean. The complex of methods included
seismic surveying, aeromagretic surveying, and gravimetry. Geo-
logic investigations were rlso made in coastal districts. It
was possible from the procfsaing of preliminary data to expose
Card 112

Some data on...
S/169/61/000/012/001/089
D228/D305
3 main types of crustal structure: continentalo oceanic, and
intermediate. A schematic zoning of the study region Nvas made
from the crustal types, and transitional areas from one type to
another were distinguished. The transitional region from a
continental- to an oceanic-type of crust in the vicinity of the
Kuriles Depression, where both the thinning-out of the supra-
basaltic stratum and the rise of the surface of the basalt layer
and the Mohorovicic surface are observed' is especially noted.
Z-Abstracter's note: Complete translation.,7
Card 2/2

s/o4g/60/000/02/002/022
oo E131/E459
AUTHORS: Gallperin, Ye.I~ and Frolova, A.V.
TITLE.- The Azimuth~Phase Correlation of Seismic Waves with
Elliptical Polarization
PERIODICAL: Izvestiya Akademii nauk SSSRj Seriya geofizicheskaya,,
1960, Nr 2, pp 195-208 (USSR)
ABSTRACT- A method of "azimuthal correlation", based on observing
in one point the waves or their individual phases as a
function of the direction of the axis of maximum
sensitivity of the seismograph, was described by
G.A.Gamburtsev in 1952 (Ref 1). This correlation can be
applied for determining the direction of the seismic
waves when related to their polarization. The azimuthal
seismogram of a wave can be characterized by the phase
and the amplitude. The phase characteristic determines
the relationship between the phase displacement (P) on
the azimuth seismogram and the direction of the
selsmograph's axis (w - azimuth of seismograph's axis,
40 - angle of the selsmograplis inclination towards the
horizon). The axis of equal phases in the azimuth
Card 1/3 seismogram is defined by the equation P = P(wjy) .

80941
s/o4g/60/000/02/002/022
E131/E459
The Azimuth-Phase Correlation of Seismic Waves with Elliptical
Polarization
The amplitudinal (dynamic) characteristics of the waves
define the relationship of the amplitude A and the
direction of the axis (w1,) . The equation A = A (w,811)
is derived for the azimu h seismogram. Both equations
can be applied in order to determine the various types
of waves and their parameters. The axis of equal phases
for the wnve elliptically polarized cart be derived as
Eq (1) and the equation of amplitudes is defined as
Eq (2). The direction of the normal to the equiphase
plane can be derived from Eq (4) and (5). Fig I to 6
illustrate examples of some particular cases where a
collection of the equiphase planes of the polarized
waves are given. The axes of equal phases are
illustrated in Fig 7. The relationship between the
polarization plane and the equiphase plane can be derived
from Eq (6) and (7). The parameters of the waves
elliptically polarized are defined by Eq (8) to (13),
where
*1, 01 and +2, 02
1 () 4 *2. , 0 ,,
Card 2/3 *1 1 -

'4
S/049/60/000/02/002/02-,;
E131/E459
The Azimuth-Phase Correlation of Seismic Waves with Elliptical
Polarization
are the coordinates defining the direction of the axes
of the pairs of seismographs. The plane of
polarization can be determined also by the graphical
method, as shown in Fig 8 and 9. There are 9 figures
and 8 Soviet references.
ASSOCIATION: Akademiya nauk SSSR Institut fiziki Zemli
tAcademy of Sciences USSR, Institute of Physics of the
Earlh
j
SUBMITTED. June 3.7.) 1959
Card 3/3

S/O 11161,1000100 1/00 1/001
A054/A133
AUTHORS- Voytsman. P.S.; Gallperin, Ye.I., Zverev, S.M.; Kosminskaya. 1.
P.; Krakshina, R .M- and Tulina,1u.V.
TIMY:. -Some results of studying the Earth's crust in the area of the Kuril
Island are and the adjoining areas of the Pacific Ocean based on
deep seismic sounding data
PERIODICAL: Izvestiya Akademii Nauk, SSSR. Sariya geol6gicheskaya, no.1, 1961,
81 - 86
TEXT- In 1957-58, Soviet geologists 'surveyed.by deep seismic sounding the
geology of the region between the Asiatic continent and the Pacific, the area of
the Kuril Island are and surrounding parts of the Pacific. These latter regions
are particul-arly interesting, because in a rather narrow (300 - 1~00 km) zone the
Earth's crust here shows great variations which can be classified in three main
groups: 1) continental type crust, conslo'ting of an upper sedimentary and two
lower: A granite and a basalt layer. This zone is 20-30 km thick, the average
velocity of longitudinal waves in'this zone is not more than 6 km/aec. 2) The
oceanic part of the crust consists of a thin sedimentary less than 1 km thiak and
Card 1/ 4

3/011/61/000/001/001/001
Some results of studying the Earth's crust ... A054/A133
a 5 - 10 km thick basalt layer. The wave velocity in this zone (outside the
sedimentary layer) is about 7 km/sec. 3) The intermediate zone has an intermediate
character both as regards thickness and structure of its layers (in general the
sedimentary-basalt structure prevails). The classification into these three groups
was b,~&ed on the time-distance curves of primary waves and the ratio of average
speed v to depth h. The geological map of the surveyed area shows that the
intr#ate alternation of these three types of crust-structure cannot be observed
in the direction from the island to the ocean only but also along the entire area,
from the Hokkaido Island to the Feninsula of Kamchatka. The most intricate crust-
structure is-found in the area between the island are and the Kurile-Kamchatka
deep trench. According to the crust-sti-acture this area can also be divided into
three parts: a) its northern part shows a continental, b) its southern part part-
ly a continental, partly an intermediate character, while c) the central part also
consists of two structuresi one of an Intermediate and one of an oceanic character
and seems to be the continuation of the deep-water area of the Okhot Sea. In order
to establish the changes in propagation velocity in the -transition zone of one
typical area of the crust into another, the average T-values have been determined
at a height of 7 km from the bottom. The c,~mparison of the velocity .-;urves with
the relief of the bottom revealed a strict regularity in the relations: the oceanic
qird 2/4

310111611000100110011001
Some results of studying the FArth a crust A05VA133
plateau corresponds to the highest average
the direction from the oceanic plateau to
southern direction as well, in the area of
The lower values of V in the tabular zone
layers, (near Kamchatka). The areas close
of the arc display high V values and the high
show a stable character (about 7 km/sec).
trench however, there are also extensive low-water
bathymetric data referring to this area and
established that the low-water areas of the
regions of the are correspond to the continental
deep-water areas of the central part of the
mediate type of the Earth's crust. The same
western-coast of the island are. Gravimetric
continental type crust structure the anomalies
values as compared with those registered for
intermediate crust structure the anomalies
and continental anomalies. The boundaries
values correspond roughly to the boundaries
values of V, which drop sharply in
the tabular zone, in northern and
the eastern slope of the deep trench.
are connected with thick sedimentary
to the central and the southern part
V-values for the oceanic plateau
Between the island are and the deep
areas. When comparing the
the structure of the crust it can be
Pacific at the northern and southern.
type of the crust, whereas the
island are correspond to the inter-
regularity is also observed for the
data show that in regions of the
of the gravlty_force display low
the ocean, while in the zones of
also have medium values between oceanic
between the zones of various A g
betwene the zones of various crust-
Card 3/4

S/011/61/000/001/001/001
Some results of studying the Earth's crust A054/A133
structures. Themoat-intense volcanic activity for the past 200 years was record-
ed for the central part of the are, with an intermediate crust-structure, while,
the highest seismic activity was observed in areas with a continental type struc-
ture of the core. In the Kuril are remarkable and intensive recent movements
have been observed, according to which the area can again be divided into three
part: in the northern and-southdrn parts a remarkable up-lift is established,
whereas the central part - bordered by the Bustol' and Kruzenshtern. straits has
subsided. There are 4 figures and 9 Soviet-bloc references.~_
ASSOCIATION: Institut fiziki Zemli AN SSSR, Moskva (Institute of Geophysics.. AN
USSR.. Moscow)
Card 4/4

00 0
AUTHORS: Averlyanov, A.
Zverev, S. M.,
I. P., Kraks'3ina,
Yu. V.
22423
S/049/61/000/002/001/012
D242/D301
G., Veytamant P. S., q-allper-in,-ye, I.,-,
Zayohchkovskiy, M. A., Koeminakaya,
R. M., Mik%ota, G. G., and Tulina,
TITLE: Deep seismic sounding in the transitional zone between
the continent of Asia and.the Pacific Ocean during
the International..Geophysical Year
PERIODICAL: Akademiya*nauk SSSR. -Seriya geofizicheskaya.
Izvtstiya, no.2, 1961,.169-184
TEXT: As part of the.IGY program.scientists..of..the.Institut
fiziki.zemli..AN.SSSR (Institute'-of.Pliyeics.of.the-Earth AS USSR),
the.Vsesoyuznyy nauchno-issledovatellskiy.institut..geofiziki
.Ministerstva geologii-.i..okhrany.-.nedr-SSSR-(All~-Union Scientific-
Research..of.the.Miniistry.of..Geology.and.14ineral..Resources.of the
-USSR) ardother-organizations..investigated.the..crustal structure
of--the Olkhotsk.Sea by.means.-of...deep.seismic.sounding...The area x
Card l/ 11

224211.
S/OA'a/61/000/002/001/012
D24~7D301
Deep seismic sounding...
was.chosen since.very.little is known of.the-nature of the crust
in such transitional zones.between continents,and oceans. It is
separated from the Pacific.by the Kurile Island Arc which is
bordered by a deep ocean containing seismologically-active zones
with-deep foci..and-large.positive-gravity.anomalies. The main
observations were..undertaken.along..-profiles-with.lengths of
.about.8000-km, orientated.-transve'rsely..to-the.supposed.structures
of.the.study area,.as described.by.Ye. 1. Gallperin, A. V..Gorya-
chev and S. M. Zverev (Ref.A: Issledovaniye.zemnoy kory v.oblasti
perekhoda-ot-Aziatskogo kont~nenta.k Tikhomu.okeany (Investigation
of-the Crust.in..the.Area-of Transition between-the-Continent of
Asia.and.the Pacifilb-Ocean) Sb. XII razdel programmy MGG (seysmo-
logiya), No. 1. lad. AN SSSR, 1958) and by V. G. Vasillyev et al
(Ref. 2: Issledovaniye zemnoy kory v oblasti perekhoda ot Aziats-
kogo,kontinenta k.Tikhomu okeany (Investigation of the Crust in
the Area of Transition between the Continent of Asia and the
Pacific Ocean) Sb. "Seysmicheskiye issledovaniya v.period MGGII
Card 2A1

22423
S/049/61/000/002/001/012
D242/D301
Deep.seismic.sounding...
No. 4, Izd. An-SSSR, 1960).. The area near Iturup Island was also
investigated-on.a special grid. The data was collected by the
method of.movable..explosion points with.single-point.recording
at fixed stations;..the.details.are.given.by.Ye.,I. Gall.perin and
1. P. Kosminskaya-(Ref..-3: Osobennosti.metodiki-.glubinnogo
seysmicheskogo.-.zondirovaniya-.na-m6re-(Features.of.the-14ethod"of-
Deep-Seismic.Sounding.-at..Sea).Izv..AN.SSSR,.Ser..geofiz., No. 7,
.1958).-..Use was.also.made-of-the results..of.-experiments,.conducted
by G. A. Gamburts6v-(Ref...6:.O.glubinnom.seysmicheskom.zondirovanii
zemnoy kory.i nekoto-rykh dru*ikh,prilozheniyakh.metodom...vysoko-
chuvstvitelinoy zapisi..seysmicheskikh-kolebiLniy-.-(The-Deep.Seismic
Sounding-of-the Crust--and-some-other..Applications.by-the.Method
of Highly...-$eusitive.Recording-.of..Seismic..Oscillations)..Izbr. tr.,
Izd.-Akad..Nauk.SSSR, 1960.).and P. S. Veytsman.(Ref. 7: 0 resull
tatakh rabot po glubinnomu..seysmicheskomu zondirovaniyu zemnoy
kory v odnom iz gornykh rayonov Sredney Azii.(Results.of the Deep
Seismic.Sounding of-the Crust in.a.Mountainous District of-Central
C ard 3/11

22423
S/049/61/000/002/001/012
D242/D301
Deep seismic sounding*,.
Asia) Stud, - Geophys. et Geodaet. , No. .2, 1958) in. continental
areas-of-the.Soviet Union...In.contrast.to foreign-practice, it
was.possible-by-employing several-recording.stations-on-the line
of.observation-to.obtain-.the types.of time-travel-curves shown
~.in Fig. 2 during a..single.boat journey. Mave recordings were
also made.on-the,explasion.vessel.-..The.bottom of-reflections
provided.'information.-on.-the..depth.,of.water.and-the.structure of
bottom sediments.in.accordance.with..the.-procedure.mentioned by
S. M. Zverev (Ref. 10: 0 stroyenii-osadochnoy.tolshchi-.uekotorykh
uchastkov-.Tikhogo.okeana po dannym seysmicheskikh otTazhennykh
voln (Structure-of the Sediment Layer of Certain.Parts of the
Pacific Ocean-from.the Data.of-Reflected Seismic Waves) Izv.
AN SUR, ser. geol., No. 2, 1960). The explosions of charges
weighing-about loo-kg-were-.recorded.on.a low-w-frequenpy seismic
device.with..a-filtration.range..of.0.7.- 15 hertz at distances of
up to-200.-.250 kn-on the sea and..100-- 150 kn on the ocean. The
receivers.consisted.of hydrophones with cascade,i-ntensification.
Card 4/11

40
Deep seisr~ic j#
sounding... 10
Fig. I.-
Examples of
hodograph
systems ob-
tained in the
Okhotsk Sea to
(14-111 6-11)
and Pacific
Ocean (6-0)
Pr fi* 14 M
2242~
S/C)49/61/000/002/001/012
D242/D301
0 ..k
I P. 5 pe, ~fwl,
t P
t4 2
j
A7 IMS-H
P 41
P1. VII
P
-t:p
11!1r. Z-.- Rpumepw CIICTCINI ro;torpatpoit, ittiay-temiux B OXOTCHOM )10pe P4-M,
it Timm oneiiiie (6-0)

221R3
S/049/61/000/002/001/012
D242/D301
Deep seismic sounding...
The wdves were separated.and correlated by.recording,their inten-
sity simultaneously i%~ith..the..construction-of.ttic hodographs-which
were set out in such a.way that the coordinate origin corresponded
to the position of the rdcording station,,the time of wave-arrival
being plotted over the positibns.of the.explosion sites.. Despite
the complexity of the rebordings, 'especially in island.and-littoral
areas, several types of waves.related.to crustal discontinuities,
bottom sediments and the water layer were distinguished on the
seismograms, including refracted longitudinal waves associated
x-ri~h boundaries in the sediment layer (Psed) and the actual crust
(I?' and P*) and T,7ith*the Mohorovicic discontinuity at the base of
the crust. 'Waves of the first type have speeds of 5 I'M/sec and.
were observed near the Miriles and on most sea.profiles. The
velocities of-the.PO.and P* waves mainly recorded.in island areas
and near Kamchatl~W_ire 6--and 6.5 - 7.1=/sec respectively. The
leading P waves refracted from the,llohorovicic.discontinuity
Card 6/1.-L

S/049~/61/000/002/001/012
D242/D301
Deep seismic sounding...
traVel*at speeds of.about 8.5 IM/sec. Waves (PR) reflected from
the Mohorovicic..and other discontinuities were also noted in
addition-to.-the refracted-waves, although it was only possible
to distinguish them with. any clarity in certain regions - mainly
the northern and central parts oE-the Okhotsk Sea, where their
amplitude is greater than that of the other wave-types. Analysis
of the hodographs discloses.the existence of.three main wave-types
defined.by differences in the arrival.and transit.time of the
waves, by the areas where they were rec6rded and by the presence
or absence of the PO and P* groups (Fig. 9). By plotting the
values for the relationship of the mean velocity v to the depth-
h, three types of velocity curves corresponding-to continental-,
intermediate~-and--oceanic~type.hodographs-were-also..obtained.
Contiuental=type.hodographs-are-characteristic-of-large areas
iu-the northern-ancl..central.parts-of-the Okhotsk.Sea-and in the
northern.Kuriles,.where.work.by P. S. Veytsman et al (Ref. 11:
Nekotoryye rezulltaty.izucheniya,stroyeniya zemnoy kory.v oblasti
Card 7/11

22421
S/049161/000/002/001/012
D2427D301
Deep seismic sounding...
Kurillskoy ostrovnoy dugi i prilegayushchikh uchastkov Tikhogo
okeana podannym glubinnogo seysmicheskogo zondirovaniya (Some
Results of the Study.of-Cr-ustal.Structure in the Kurile Island
Arc and Adjoining Parts of.the Pacific Ocean from the Data of
Deep Seismic Sounding) Izv. AN SSSR, ser. geol., No. 1, 1961) has
already indicated,that the.crust.-is.of the..continental type. In
the-continental-ntype.hodographs..the.arrival.times..of the PO, P*
and..P_waves are at a maximum, the transit time of-the P waves
being 18.- 19 sec. There are two forms of..hodograph; one repre-
sents,.a-three~layer.crust.(sediments.-.-Igranite'-Ibasalt') for
the region near- KEauchatka- and Sakhalin, while ..the. other corres-
ponds to.a granite.crust (with local basait.layers) in the north
of.the.Okhotsk.Sea. According to.the.velocity-depth curves the
continental-type. crust, whose thickness throughout- the, study area
may vary from.-20 to 30 km, includes thick or thin sedimentary
layers. Oceanic-type hodographs cover areas approximately out-
lined by the 5 km isobath. The arrival time of the P* and P waves
Card 8/11

Deep seismic sounding...
Vig. 9. tsm Gec,
Principal
hodograph
types.
1-continental
2-oceanic
3-intcrmediate.-j,
striations
denote areas
where there
are different
types of hodo-
graph waves;
Type 3 charac-
terizts hodo-
graphs for the
P,
Bering and
Okhotsk Seas P
Card 9A1
.S/049/61/000/002/001/012
P242/D301
, - ,
Pr
Oil. F
ON
,HIelo
Piz
7

Deep seismic..sounding...
22423
S1049V61100010021003-1012
D242/ r'301
is at a minimum and t~e.transit-t'inte'.for.,the.latter waves is
t 14 sec. The presence.bf a thin.basart crust with a thickness
of about 5 - 12 1cm may be inferred frqm.the observational data.
The intermediate-type-hodographs are.representative of.the south-
ern part of the 01thotsk Sea a~d the neighborhood of the,Komandor-
sitiye Islands. They are aistinguished by.the existence of P* and
P waves and by the large area in which waves of the first type
viere recorded; the transit time of the P waves is 15 - 17 sec.
The velocity-depth curves rdsemble those-for the continental-type
crust in abyssal parts of the Okhotsk Sea, where the sediment
thickness.appears to be cqnsiderable,.and those for the oceanic-
type crust in the Bering Sea. The authors conclude by stating
that a-composite intc~pretation of the data of deep seismic
sounding and of gravimetric, aeromagnetic and*geologic observa-
tions in this region will be made subsequently which may.possibly
expose the patterns of development of crustal structure and also
clarify the conditions and sequence of transition from one type
Card 10/11

Deep seismic sounding...
S/049/61/000/002/001/012
D242/D301
of crustal.structure to another. In addition, they emphasize the
desirability of comparing.-their data with those from other global
zones.- There are 13 figures and 12 references: 10 Soviet-bloc
and 2 non~Soviet-bloc. The references to-the English-language
publications read as follows:.R. W' Rditt - Seismic-refraction
studies of the Pacific Ocean Basin, p. 1. Crustal thickness of
the central.equatorial.-Pacific,.Bull. Geol..Soc. Amer., 67, No.12,
1956; M. Talwani, G. H. Sutton and J. L. Wor2el -,A crustal section
acroas-the Puerto Rico Trench, J. Geophys. ges.,. 64, No. 10, 1959.
ASSOCIATION: Akademiya nauk SSSR, institut fiziki zemli (Institute
of Physics of.the.Earth, AS USSR)
SUBMITTED; July 24, 1960
Card 11/11

S/049,/61/000/006/001/014
0239/D306
AUTHORS- Gal'perin, Ye, 1. and Froloya, A.V~
TITLE, Three-component seismic observations in boreholes. 1.
PERIOVICAL Akadvmtya natik. IzvemCipt. Seriya geofizicheskayn, 1961,
no- 6i 793-809
n=.~ Two e:ztensions of well-shooting technique are discussed and
supported by field results obtained in 1959-60 by the Inatitut fiziki
Zemli AN SSSR (Institute of Physic* of the Earth of the AS USSR).
These extensions are (a) The use of correlation principles to follow
arrivals out to the end of the traceag obtained in ordinary, reflexion
shooting by adding three-component information from a neighboring bore-
hole shoot and (b) the use of polarization data to assist in the qualita-
tive evaluation of strata. The necessary elementary theory for the case
of a borehole penetrating a single horizon is developed and the case is
illustrated by field dato on arrivals P, PP7 PPII and PPS from two shots V/
about 200 m from a single borehole. A clear figure is drawn of the data
Card 1/3

S/'049~/61-/000,~"006-.'001,'OI 4,
Three-component seismic D239/D306
from both the vertical prof-Ae and the horizontal arra, In as6ist lb-
explanation which is de!ailed. Fieldwork was carried out -v Ocrar-
pathin (Stan~slavskiy oblast) where there is a -harp horizon between
4he gypsoanhydrite-layei and the overlpng argillaceotis sandsloop. flx~~
Aservat;*ons were inade with a apparatus typ-e CC-26-51-IR
iss 26-5! 0) using seismometors type CrIJ-1011 iSPA614).. The X.-compr-
nen*s had a resonance a* 20 c/s and the Z-componen*l at 50 c/,Q. A N!-
description of the results and their analysis is g-iv?n,, ~411ustrated
b
y five photographs of seismograms. The net result was the detection 01
a slope and its strike at the interface. To Kulichikhina, FQ Vinogradow., V,
P. Yudin and L. Khudobina are mentioned for their contributions. There
are .1 tabte,* 12 figures and 23 references- 17 Soviet-blot and 6 non-
Soviet-bloco The 4 most recent references to English-language publica-
tjons read as follows~ FoJ. McDonal, F,A. Angone, Attenuation of the
shear and compress~onal waves in pierre shale. Geopkys. 23, 1959-, E.M.
Riggs, Svism-lc wa-ve types in a borehole. Geophys. 20; 1955. F.K, Levin,
R,O. Lynn. Deep hole geophone studieso Geophyso 23, 1958. F,~ Collins,
ca rd 2 -,

a ! v A t-,ri
ASSOC I AT I ON Akadomiyn mink
scietif c." 1
0 19 6 001 y 1101)
D239 D-Mfi
ital. I ot, v h,,it ar I c K- it t om Ill I i p,-r
14.14.1411 I"StIfill I" oliem% 0
ItI.-'t i liltv W, I'llyst, ~)l lilt, Fro I Ili
toi rrrFD f ~ ml) e) 15 1960

GALIPERIN, Ye. I.; FROLOVA, A.V.
Three-component seismic observations in boreholes. Report No. 2.
lzv. AN SSSR. Ser. geofiz. no.7:979-993 Jl 161. (MIRA 14:6)
L.Akadamiya nauk SSSRP Institut fisiki Zemli.
(Seismic prospecting)

~ 1:` , lir WPF~1,111 "', , 1- :~ W11 C! I'1 I I ~ ! ~ ! ~ ~ *1 - if -~ !
GALIFERIN, Ye.I.; TURCHENKOV, V.I.
Ring phase detector for high output voltages. Priborostroenie
I
no.11.21-22 N 162. 1 (MIRA 15:12)
(Voltage regulators)

, 1 * : Ik I I ~ I lil- ;V11 1" 11
GALIPERIN, Ye.i.
Studying the direction of the vector of displacement in seismic
waves during observ&.ions in boreholes. Izv. AN SSSR. Ser.geofiz.
no.21278-292 F 163. (MIRA 16:3)
1. Institut fiziki Zemli AN SSSR.
(Seismology)

-
Using the directions of the displacements in the initial waves,
as observed in boreholes,, to determine the bedding factors of
the refraction discontinuity. Izv.kN SSSR.Ser.geofiz. no.41
513-524 Ap 63-. (KIRA 16:4)
1. Institut fiziki Zeali M SSSR.
(Seismlog7-Graphip methods)

GAOPERIN, Ye.I.; ZAYONCHKOVSKIY, M.A.
Methodology and technique of deep-sea seismic prospacting
using submarines. Izv. AN SSSR. Ser. geofiz. no.12:1833-1836
D 163. (MIRA 17:1)
1. Institut fiziki Zemli AN SSSR.

GALIPERIL, Ye.I., otv. red.; KOS-IINSKAYA, I.P., otv. red.
(crustal structure in the transitional area from the
Asiatic continent to the Pacific Ocean] Stroenie zemnoi
kory v oblasti perekhoda ot Aziatskogo kontinenta k
Tikhomu okeanu. Moskva, Izd-vo "Nauaka," 1964. 307 p.
(MIL4 17:6)
1. Akademiya muk- SSSR. Institut fiziki Zemli.

ACCESSEN NRs Aonmq S/0049/64/000/00WO456/0474:
AUMMs Oallperln# Too 1e
TIMM Detailed study of a velooity model for the upper part of a seation vith
weak velocity differentiation
SOURCEs AN SSM. Isvestlya- Sarlya soofisicheakwas no. 4v 1964s 456-474
TOPIC TAGSs velocity model,, seismic amdell, head wave,, refra*cted wave, vertical
profiling
JABSTRACTo The ordinary method used in a drill hole (measuring velocities along the
i shaft of the hole by recording f irst-arrival times) does not alwaWs permit the
!construction of a velocity model of a medium that corresponds to the basic f"tur**1
!of the observed wave picture. Through a combination of vertical and horizontal
,profiling and a study of the displacement directions the different kinds of head,
irefracted, and reflected waves in successive parts of the record may be distia-
!guished anA traced,, opening up the possibility of using the dominant wave in the
actual medium (according to W. Utude) to construct the saismic model, The best
system of observation for constructing a proper velocity model of a medium we
i-Card 1/2

:-ACGWSION NR: AP4033019
I
correlation systems in vertical planes. This technique has permitted the construe-
,tion of a model with weakly differentiated velocities in the modium. For technical
Ireasons, systems of observations in vertical planes have been used previously for
!constructing velocity models of the uppor parts of sections, chiefly in connection
:with the study of wave noise, Under those conditions only direct head and re-
Ifracted waves could be used (their first arrivals on the record). With more
!thorough studios,, the munber of usable waves is increasing, wA more effective use
lof the possibilities of the system is being realized. Orig. art. hass 12 figures*
ASSOCIATIDNa Akademiya nauk SSSRpInstitut fisiki Zemli (AcadeW of Sciences SSMP
Institute of Pbgmics of the Zarth)
SUBK=M t ~3 DA73 ACQt, IM&A. IMM 00
ISUB CODRe in ND PJW Offs M3 MMI ON
i Cam 2/1

GALIFERIN, YO.I.
InfluerrA of tbel upper surface and the upper par' of a cross -Qfction
L,
on tht character and structure of seismograms. Vop.din.teor.raspr.
seism.voln no.7:201-214 064. (MIRA 171 U)

T, 11816-65 3v`T(1)/9WA(h) Pob OW
AV4045250 BOOK EXPLOVATICH S/
Almdamlya nauk SSSR. 106titut fislkl seall in, 0. 1u, Shaidto
3tructure of the earth's crus in the zone of transition from the continent of
Asia to the Pacific Ocoan (Stroyenlye zemnoy kory v oblasti perokboda ot Ast-
.takogo kontinenta k Tikhom Ckeanu) Moscow, Izdmvo *Naukamp 1964. 307 p.
iliu'.' biblios, foldin charts (in portfolio), Errata slip ineert*de 1200
copies printed, Responsible editores Ye. L Gallperin, L P. Kcmainakaya;
Editor of the publishing houses S. 1. Masarekiy; Technical aditcres Ye V.
Uakuni, S. 0. Tikhomirara
TCFIC TAGS% area seismic sounding, earth trust, geopbysics, International geopby-W
oical year, ocean, seismic wave
PURPOSS AND COVERAGEt This monograph in devoted'to studies b7 the method of deep
-/qaiamie soundi
ic awndin (GSZ) in the zone of transition fron the Asiatic continent to
the Pacific Ocean (Kamchatka, the Karile peninsula, Bering See, etc.) during the
International Geophysical Year (MDO)s The material is presented as a collection
of individual chapter#, although all are devoted to a single probles and are
C.M 2/

L 31816-65
AR4045250
lally parts of one book. The authors express their gratitude to Professw
absont
V. V. Fodmakly, Chairman of the working subgroup of the Sawstakly Hatsioullray
Nomitat, Initiator and. organizer of complex geophysical research, and also- to
Corresponding Vember of the AcaderW of Sciences pr the USSR V, V, Belau* r0
The concludW chapter we prepared by A.G. Avertm-ow, P.-S. Vertaman, to, Z.
_-GLI-IsArin, So V* Zverev, wd Z. P. Kosainsksys.
TABU (W MUM
Introduction (A, I.
_A,Samburtsev 3
Ch, 1. Brief information concerning the research methodoloa and &Mrstus (To..
1. Callperin) - - 7
Ch. 2. Dividing the region for Invest4ption into some aecording to types of
asimic material (L P. KosaInskaya) - ~ 12
Ch, 3. Special kinematic "rectoristics of sultiple isves cowwated with deep
6iscont1rultive (To. L Gallperin) - - 21
Ch, .4. Dynamic characteristics at deep way" for certain models of the earth's
crust (A. 0. ATWIYNW# L ?a KOWIM"t Os A- Yaroshow 39
coni

L 31816-65
AW45250
ch. 5. Results of studying a sedimentary stratum In the Ses, of Ckhotsk and the
Kurile4amchatka Zone of the Pacific ocean (S. N. Zverev) QO
The magadan-KoUm continental contour (j,.-1L.RLv-vdsn, Ta, B, Shva -
Ch. 6. 8) - I
Ch. 7. The northern and central parts of the Sea of Ckhotsk (Sections 117
9-9 - 14-M) (L P. Xosainskays, R. V. Krakshins, L N, pay-lova) - - 128
Ch. S. The southern part of the Sea of Ckhotek (L N. Parlows) - - 180
Ch. 9. The southern and central parts of the Pro-gurile Zone In the Facifle
Ocean (Yu. V, Tulina V, VIronowa) - - 199
Ch. 10. The northeastern part of the Xurilia-Kafthatka Zaw of the Pacific Ocean
(P. S. veyteman) - - 229
Ch. 11. Pr"cmandor sectlons of the BerIng Sea and the Ficific Ocean (I. F,
KonsIMMYS) - - 264
Ch. 12. General features of the stmature of the earth's crust In the transition
sons (I. P. losalmakays, S. V. Zvorov, P. a. vsytmn, Tn. V. Tauns) 274
Concluslone - - 294 ' I - I
bittal treatment of selamographs (T. L 91ronvA) (Appendix) 299
Uterstum 302
Cwd

i: I ~ ~ III I, - .." ..
~Mmm."Wwl~
AU; NM AP6011952
SOURCE CODE: UR/0387/65/000/012/0001/0012
AUTHOR: Gallmin, Yee I*
ORG: Institute of Physics of the Earth j_ Ak WW (Institut flaiki 7
_.Zali AN SM)
TITLE: Study of multiply reflected waves in vertical seipm oci!~ro*riling Z Z
SOURCE: AN SSSR. Izvestiya. Fizika Zemli, no. 12, 1965, 1-12
TOPIG TAGS: shock wave reflection, seismic wave, stratigraphv,,seismology
ABSTRACT: On a vertical profile, in contrast to a horizontal profile, multiply
reflected waves differ sharply from singly reflected waves and in particular there
is a difference in the regions where they occur. Vertical seismic profiling affords
new possibilities for study of multiple waves: determination of their naturep pathas
relationship to stratigraphy, conditions of formation, etc. In this respect vertical
seismic sounding has considerably_greater possibilities than horizontal pr,.ofiling. In
order to determine'the- niture *of waves recorded at. the surface and de-
tection of singly reflected irtaves among a large number of multiply re-
flected waves it is of particular importance to combine observations by L
the horizontal and vertical. profiling methods. The use of a multipoint
probe with independent spring devices has considerably improved the
;possibility o~ correlating ,mves on the vertical profile. On the seis-
imograms for a vertical profile, the last part of which is free of
I wave
!interference, it-has been found that there can be phase correlation not
UDC: .550.834

L 21130-66
ACC NR: AP6011952
~Only of the domihant waves, but also of
waves with a relatively small
:amplitude. The use of the methods of directional reception considerably.f:,
-improve the possibillties-9f correlating waves on a vertical profile.
;Even at relatively great depth - 2-2,,2 Im -- there is a strong influ-
ionco or the surfaqe and the discontinuities :Ui the upper. part ot the
cross section on the wave field recorded at inner points of the mediume
IThe overwhelming part of the energy on records obtained at these depths
is related to multiple waves which are reflected from the surface or
idiscontinuities in the upper part of the cross section and are propagatedq
downward in the medium. The next objective in the study of multiple
:waves in vertical profiling is the study of the dynamics of multiple
S waves and the properties of the media in which they arise and are prop&-
:gated. The results already obt;ained and those expected in:the future
:'Justify the broadening of investigations in this direction. It*can be
speculated that vrith a further developnent of the methods of vertical
isei=ic profiling the possibi3ities of enerimental study of seismic,.
waves in real media, and especially multiple waves, can be so decisive
j that it may be desirable and economically advantageous in areas -where
ManY seismic investigations are _"ing made to have special: drilling f
a borehole for vertical seismic
Rrofiling purpoaaa, Orig..,krt, has:
8 figures and 2 formulas. [JFRSJ
SUB COIOEi 08, 20 SUBK DATEI :3.lJun64 ORIG IREF M7
Ccwd 2/2

4 1! 1 1 11 ? f. F: I I II. ~1-1 ij!' i Tit
L 29883-66 T ( 1
ACC NRs AP6005550 SOURCE CODE: UR/0030/66/000/001/0055/oo6o
z
AUTHOR: Gal'Derin, Ye. I. (Candidate of physico-mathematical sciences)
ORG: Institute of the Physics of the Earth in 0. Ya. 91midt, AN SSM (Inst*t Fiziki Zeml~
TITLE: Investigation of seismic waves in real media
SOURCE: AN SSSR. Vestnik, no. 1, 1966, 55-6o
TOPIC TAGS: seismology, seismic profiling, seismic wave, seismic modeling,
seismography
ABSTRACT: This paper presents a brief historical review and a summary of the
present status of Soviet studies on seismic wave propagation in real media. The
Institute of Physics of the Earth im. 0. Yu. Shmidt of the Acadewj of Sciences
USSR began work in 1959 to improve methods for the experimental investigation of
seismic waves in real media. The main task was to make the transition from inves-
tigation of wave pictures which already had been formed to investigation of the
actual 'processes of the formation and propagation of seismic waves. This again
required changing from surface observations to observations made within the earth's
crust (borehole multichannel registration of waves with shot points located at
various distances from the mouth of the borehole). The importance of combining
observations carried out within the medium (vertical profiling) with surface obser-
Card 1/2

L 29883-66
ACC NRj Ai
vations (horizontal profiling) is emphasized. The author points out the need for
further investigations of the correlation method of refracted waves as one of the
most important methods of carrying out regional geophysical studies. He also
emphasized the need to attempt to improve on Petrashen's theoretical treatment of a
simple model to more accurately reflect.the propagation and behavior of seismic
waves in more complex models. Orig. art. has: 4 figures. CERI
SUB CODE: 08/ SUBM DAM. none
Card 2

ACC NRs AP6032422'
SOURCE CODE:
:AUTHOR:..Gallperin, Ye. I.; Frolova, A. V.
PG: Institute of Earth hysics. AN SSSR (Institut fiziki zemli AN SSSR)
.!TITIZ: Investigation of exchanged waves by the seismic vertical profiling method
SOURCE: AN SSSR. Izvestiya. Mika Zemli. no. 9, 1966, 93-104
..:TOPIC TAGS: seismic wave, stratigraphy-, transverse wave
~ABSTRACT: At present, the main difficulty in developing this method lies in the correc
linterpretation of the composition of the ground and in the separation of individual
.waves. knong other difficulties, the great number of possible wave types and the wide
,~r~hge of the velocity ratios of the longitudinal to transverse waves should be mention
ed. The difficulties mount even in the simplest of seismological cases. In complex
cases, the problem is hardly soluble. The method of vertical profiling affords the
ifollowing: 1) determination of the nature of waves; 2) identification of waves with
,the 6orresponding strati"graphic units; 3) identification of waves as longitudinal or
transVerse--within limits of the stratigraphic unit; 4) construction of the simplifi-
ed model; and 5) evaluation of the wave parameters. The exchanged waves are most pro-
nounced when propagating upward. The improvements in the method should be along the
~
Card
UDC: 550.834
UR/0307/66/000/009/0093/0104

ACC NRt AP6032422
lines of mi-relation of waves throughout the entire vertical profile. Orig. art. has:
7 figures, 2 fomulas..
SUB CODE: -08/ SUBM DATE: O8May64/ ORIG REF: 020

------- OW
ACCR ~,M6035594 i66WC~6DE's UR/0387/66/0(
'
AUTHOR: Gal
perin, Ye. 1.

ORG: Institute of Physics of the Earth_,,Acadepy._q( n fisiki
jj~jq_ cgs_.SSSR (Institut
Zemli, Akademiya nduk SSSR)

TITLE: Intensity of head waves and reflected waves incident at angles exceeding
the critical. angle, bii-e-don ~eitlcal seismic-Prof-41-ng data

SOURCEs AN SSSR. lavestlya. Mike Zemli, no. 10, 1966, 9-24
TOPId TAGS: seismic profiling, wave propagation, seismic wave, vertical seismic
profiling, heat wave, reflected wave
ABSTRACT: The intensity of head waves and reflected waves incident at angles exceed-
ing the critical angle is investigated inside the medium by vertical seismic pro-
filing. These investigations are a continuation of those initiated by Ye. I.
Gal'perin and A. V. Frolova [Izv. AN SSSR. Ser. geofiz., no. 9, 19631. The advantage
of observations made inside the medium as compared to ground observations in
investigating head waves is that the waves are recorded in different regions in
horizontal and vertical profiles. In horizontal profiling the first head-wave
arrivals can only be recorded at relatively great distances, making it difficult to
analyze them. In vertical profiling the first head-wave arrivals are tracked directll
from the point of origin and from the refracting boundary, making possible the

_L 29261~;&6-- -EWT(l)JPn(m)/FGC/EWPLt-)/Er1 -- IJP(C I-- GWIWV/JD
ACC NRa AM19297 SOURCE COMt Lqt/0203/65/005/004/0728/0734
AUTHORI Gallperin, Yu. .; Sobeltman, I. I.
ORG: Institute of Physics of the Atmosphere. AN Institut fiziki atmosfery
AN SSSR); Physics Institute im. Lebedev, AN SSSR krizicheskly institut AN SSSR)_.
TITIE: Possible role of metastable states of neon and argon in processes of
-post-luminescence of.auroras
V/
SOURCE: Geomagnetizm i aeronomiya,, v. 5, no. 4, 1965, 728-734
TOPIC TAGS: neon,, argont aurora
ABSTRACT: A study has been made of the role of the processes of collisions
f 02 M01' ules with leading to,
'0 ec Ne and Ar,#toms in metastab 1e statea
Idissociation of the 02 molecu 1with the formation of excited oxygen
latoms. The' oxygen lines A 8446and 7774 A are emitted at,the time of;
collisions with neon; the lines A 5577 and 6300 A are emitted at the
t
time of collisions with argon, The duration of post-luminescence at
[hheigk~s -200 km can attain several see q.
- j Orig. art. has: 17 formulas and
1 table. (JPRS1
SUB CODE: 04 SLJBK DATE: 120rt64 MIG MF: 008 OTH OF: 009
Cdrd 1/1 -UDC. 550-388-8

: : ! 1 1 11 ~- .. : - 1 , 1
KUTITS, Y.Te., kandidat meditsinskikh nauk; GALIPMN. Y1.1. student
TI k-urva.
Immediate and late results of treating chronic osteovVelitis
by continuous Intraossal penicillin injections. Khtrurgita no.6.-
71-75 Je '55. (KLRA 8: 10)
1. 1z kafedry faltulltetskoy khtrurgii imni N.M.Burdenko (sav.-
zaalusheaW dayatell nauki prof. N.N.Yelanakly) I Moskovskogo
ordena Lenina meditsinskogo instituta.
(OSTWWIILITIS, ther.
penicillin, Intra-ossal aduln.)
(PMICIUIN, ther.use
ostsoarelitis, Intra-ossal admin.)

EXCEIVU REDICA Sec.13 Vol,1/9 Cardiovasadar SePt 57
2687. HALPERIN E. 1. Determination ol portal blood Pressure by spleen Puncture
(Riissian text) Khirurgija 1957, 4 (109-114) Tables 3
On account of the development of the operative treatment of cirrhosis of the liver
it is of great importance to measure the portal pressure !.)cfore t lie oporation. Estima-
tion of portal pressure gives the opportunity of early correct diagnosisand determin-
ation of expediency of surgical intervention. Taken into consideration the fact that
the medullary sinus of the spleen is connected with the veins of the portal system
in the spleen, it was suggested that the pressure measured in the spleen must show
the correct value of the portal pressure. In order to check this statement 22 measure-
ments of the venous pressure were taken in dogs and 6 in rabbits. Simultaneously the
measurements of the pressure in the portal vein were taken. The results were ident-
ical. The pressure in the spleen was from. 100 to 220 (average 147) nun. of water
column. The portal pressure was from t02 to 220 (avera e 144) nun. of the water
column. The same evidence was obtained on measuring tke pressure in dogs. Later
this method of measurement of the pressure by puncture of the spleen was tested in
9 patients who suffered from cirrhosis of -the liver. There were no complications
noted either in the patients or in laboratory animals. (Xvill, 9)
Zl~

Xhe
i9Y,(',F,TT'T'A * Ml~;A Sec 9 *'ol 13/7 Siir,,Pry JU'-Y 59
I
4014. PORTACAVAL END-TO-SIDE ANASTONIOSIStITH THE AID OF DO-
NETSKY'S RINGS (Russian text) - Galperin 1. - EKSPER. KHIR.
1958. 4 (40-44) Tables I
A portacaval end-to-side anastomosis was performed in 15 dogs with the aid of
bonetaky's metal ring. Thia technique of the procedure is described. Suture of
vessels with the aid of this method never caused any great technical difficulties.
There was no haemorrhage-. Vasograms; taken from 17 days to 2.5 months after
the operation showed the vascular anastomoses to be fully patent. One dog died
immediately after the operation from air embolism. Two dogs died, one after 17
days, the other after 2 months, with symptoms of meat poisoning. All anLmals
~ 51
-7
ee s- AIS1 141 I'V

GALIFERIN, Ye.I.
Induction of liver cirrhosis and gscites In experiment. FkBper.
khir. 5 no-1:46-49 Ja-F 160. 0\11RA 13:12)
(LIVER--CIRRHOSIS) (ASCITES)

PETROV, B.A.,, prof.; GALIPERIli, Ye.I., kand.ried.naA
Diagnosis and treatment of nonalcerative gastrointestinal hemor-
rhage. Vest.khir. no.10:87-92 161. (IMIRA 14:10)
1. Iz Moskovskogo gorodskogo ordens. Trudovogo Krasnogo Zanmeni
nauchno-issledovatellskogo instituta skoroy pamoshcbi IM. W.V.
Sklifosovskogo (dir. - zasluzh. vrach USSR M.M. Tarasov).
(MNORRHAGE) (Dir.P.STIVE ORGANS-DISEASES)

A manual on s peel N c-ttiori reuuiremi(irits Cor metril-wor'l-in, a -I-,
nauchrio-te-khn. izrl-vu :mi2hinoptr~-jit. lit-ry? 1949. 119 3';412~i'
TJIIB-.G25

GAL'PERD, E. I.
Naladka zub,)reztWkh stankov.
Moskva, Mashgiz, 1951. 172 p.
(Setting up grear-cutting machines.)
SO: Manufacturing and Mechanical Engineering in the Soviet Union, Library of
Congress, 1953.

/v /Y,
KOROLEV, F.K., dotsent, kandidat tekhnicheakikh aauk: BONDARI, M.P.,
kandidat takhnichaskikh nauk, redaktor; ag'FARIN. Te.I., inzhener,
reteenzent; KHAYMOVICH. Ye.M., professor, do-k-t-o"r-,t-e"k~6"r,-cheakikh
nauk, retsenzent; XISTMNIO, D.M., takhnichookly redaktor
(Calculations for transverse planing machines] Raschet poperechno-
strogallnykh stankov. Iriev, Gov. nauchno-tekhn. Izd-vo mashIno-
strolt. lit-ry, 1952. 100 P. (Microfilm] (HLRA 7:10)
(Planing machines)

SIDOBEMO, A.K.; K&MEV, A.K.; SlUTSKIT, Ye.;S.; GAL' PERIN,, jq2.,_j,,
otvetstveanyy redaktor;IZMA., V.I., vedushcl~l~~r*~d.~Vlctar-' RU-
MSKIT, Taj., tekh-aicheskiy redaktor.
CManufacti=e of cog and worm gear] Izgotovleaie zubctlatykh I
cherviachn,vkh peredach. Kiev, Goa. nauchno-.tekhn, lzd-vo ma-
shinostroitellnoi i sudostroit. lit-ry, 1954. 117 P.
(Gearing) (MIRA 8:1)

KARISEV, A.K.; URPOV, V.F.. inzhener, redaktor; GAL' IN, fe. I , inzhener,
redaktor; 1EMA, V.I., inzhener, redaktor; UD=l tekhni-
cheakiy redaktor.
[Production of worm gears; from the practice of the Novo-Kramatorok
machine shop] Proizvodstvo globoidnykh peredach. Pad red. V.F.Kar-
pova. Kiev, Goa. nauchno-tekhn. lzd-vo mashinostroit. lit-ry, Ukrain-
skoe otd-nie, 1954. 134 p. (KM 8: 1
(Gearing, Worm)

.i~adB-e-a, AlekAandr Hoyseyevich- "WSRU YO.I., Insherier rvtoeazent;
LYAPUNOV, M.A., kandida im nauk, loteent, rell-sonze-it:
GLUVGHlbl6KlY, Ye.V., kBndi4at takhnichookikb neuk. redairtor;
LV.UTA, V.I., inzhoner, redaktor izdatel'stva; MUMMY, Yaj.,
tekhnicheskiy re"ktor
[Anginsering precision of gear cuttLug vachines and means of
improving It] Tokhnologlaheeknia tochnost' suborozaykh stankov
oposoby so povyshentia. Kiev. Go~.wuchno-t9ktui.i%d-yo mashinotit-rit.
lit-ry, 1957. 190 to.
(Gear-cutting, machines)

PHASE I BOOK EXPLOITATION so-'~/4602
Gallper1n, Yevgeniy Iovelevich
Naladka zuboreznykh stankov (Setting-Up of Gear-Cutting Machines)
2d ed.Y rev. and enl. Moscow, MashSiz, 1960. 214 p. lo,ooo
copies printed.
Reviewer: 0. A. preys, Candidate of Technical Sciences; Ed.:
N. P. Onishchenko, Engineer; Chief Ed. (Southern Department,
Ma3hgiz).- V. K. Serdyuk, Engineer.
PURPOSE: This book is intended for skilled workers and foremen
working in machining shops.
COVERAGE. The book contains basic data on setting-up Soviet-
made gear-milling and gear-shaping machines for machining
spur and worm gears. Essential information is given on
gears and on cutting methods with various tools on milling,
tooth-milling, and tooth-shaping machines. No personalities
are mentioned. There are 20 referenmes,, all Soviet.
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Setting-Up of Gear-Cutting Machines SOV/4602
TABLE OF CONTENTS:
Foreword 3
Basi(,, Information on Gears 5
Types olf gears 5
Profile of a gear tooth and the elements of gearing 6
Properties of involute gearing 8
Basi~~ definitions and dimensions of spur and worm gears 9
Requirements imposed upon gears 17
Gear-Cutting Methods and Tools 19
Gear-cutting methods 19
Gear-cutting tools 2 42
Review of modern methods for machining spur gears 26
Concise information on tooth-finishing operations 28
Setting-Up of Machine Tools and the Related Calculations 31
Se"Iting-up of a machine tool 31
Speed 31
Feed 32
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Setf,lng-Up of Gear-Cutting Machines Sv~/4002
Kinematic scheme of a machine tool 33
Gearing ratio 39
Change gears 43
Cutting of Spur and Worm Gears on milling Machines 45
Division heads 45
Cutting of straight spur gears 53
Outting of helical spur gears 54
Cutting of worm gears 56
Determination of feed., speed, and operation time 57
Gear-Milling Machines and Their Setup 57
Setting the milling cutter and the blank on gear-milling
ma,_,hines 61
Type 532 gear-milling machine 66
Type 5D32 gear-milling machine 104
O%att-ing worm gears with a f lyeutter 126
Mac;hining spur gears having a prime number of teeth 130
Setting up a gear-milling machine without differential
.r.
lor maahinIng helical gears 132
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Setting-Up of Gear.-Cutting Maochines sov/4602
Setting the operation time for gear-millIng machines 133
Produ,:'1V-1v1ty 1mrease In gear milling 134
Generating Gear Shapera and Their
Sett"Jng the shaper-outter and
'PYPe 51-4 gear shaper
Type 5A.1,21 gear shaper
Type r5V12 gear shaper
Setting the operation time for
Cutting Nonst-andard and Modified(Corrected)Gears
Setting 138
the blank on gear shapers 140
144
163
179
gear ohapera 188
Inspection of Maohined Gears
Gearing toleranoes according to GOST (All-Union State
Standard) 1643-56
Me-1hods of inspection of gears
Appendix
Bibliography
AVAILABLE~ Library of Congress (TJ187.G3 1960)
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200
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VK/wra/ec
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i
REZAHOV, I.A.; lUiSTVUROVA, V.A.; LEONOV, N.E.; Prinimali uchastiye;
ANDRELS, S.S.- GUIPIRIN, Ye.I.; DDIIABYMV, A.T.; Yk2-,S, A.Z.;
KOSMINSKAYA, I MASARSKIY, S.I.; KOM3T,
S.V.; PETRUSIERVSKIY, B.A.; FUGHKOV, S.V.; RASTVOROVA, V.A.-,
REZANOV, I.A.; SAVARENSKIY, Ye.F.; KHARIN, D.A.; Red karty:
GAMBURTSEV, G. A.
Establishmett ofdatailed seismic regions as exemplified by
a region of western Turkmenistan. Biul. Sov. po saism. no.8:
131-141 1~0.1 (MIRA 13:10)
1. Institut fiziki Zemli AN SSSR.
CKirkmenistan-Seismology)

AK-SENOVIC119 G.I.; ARONOV, L.Ye.; GAGELIGANTS, A.A.; q4~'Mijl'
ZAYONCHKOVSKIY, M.A.; KOSMINSKAYA, I.P.; OAKSHINA, R.M.;
VERES) L.F., red. izd-va; TIKH%IIROVA, S.G., tekhn. red.
[Deep seismic sounding in the central part of the Caspian Sea)
Glubinnoe seismicheskoe zondirovanie v tsentrallnoi chasti Kas-
piiskogo moria. (By] G.I.Aksenovich i dr. Moskva, Izd-vo Akad.
nauk SSSil, 1962. 150 P. (MIRA 15-8)
(Caspian Sea-Farth-Surface) (Seismology-)