SCIENTIFIC ABSTRACT ZVEREV, P.I. - ZVEREV, V.A.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R002065710008-2
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: September 26, 2002
• Sequence Number: 8
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

USSA/Xicrobiolory - MicroorEpnisns Pathoj;cnic to Humna au.
Animls
Abs Jour Hof Biol. No 12,' 1958, 508V
Author 2;~Or`e"vi P. x:f
vatenAgricultural Vicititutc,
Inst Dar
Title Erroct of Abbe'ato~~ J161-Activit,
of Biopr-ap,arations Foltored Tli~o~di Thbid*6 I
tIa1956, 8 144.14~.~
Orig Pub Tr. Dadestanski sa;-Idi. in-
Abstract Typhoid and paratyphoid aCe6i:Utinatfing tbera wdre rilterel
at! thdr til ~
through7 small, asbe os -,.ltct,* ;Or ws~.dotcrmi-~
nod bef6re'the, beginning of he.' expoiliment iand overy.,W
minutes thereafter, L i' the first 'pbitiona of Uic ~ f iltra-
to the titer-.fell 2 t6 3 tims.,4ndloitly on; the 3rd-5th
'tost 'was the. irdtial:titckf,o~i~in6d.:,i~tBactciiiaphaGe ofS.,
abortus equi. vas filtercd'throuGh a ;13imLlex filter anC its
Card 1/2

P.H., insh.-polkovnik
War years of *Artilleriiskii shurnal.0 Artill. zhur. no.5.*16-0
My 158, 1(migA llt6)
(Artillery~-Periodica~v)

AUTHOR: Zverev, S 4-5816 2~/37
TITLEi Underground Fertiliziation (Podzemno 6~:udobieniye)
y
PERIODICALt Znaniye - sila, 1956, Nr 6, p 44 (UsSO
ABSTRACT% The co-workers of the Kishinevskiy ee11'skokhozyaystvennyy. in-
stitut (Kishinev Agricultural Tnstitute) hnve been investigat
ing for several years the possibilities of.underground irri-
gation, heating and fertilization of sugar-beets, vineyards
and gardens by means of underground pipes.
1. Irrigation systems--Applications 2. Agricul-ture--USSR
Card 1/1

VARVs Sot inshener,
Device for 'separating shelled grains In moving ear corn.~Kuk.vbelsv.
prom 22 no,9:29-30 S '56. (MLRA'10:8)
I.Krasnodarskeya. krayevays, kontore. Zagottierno.:.
(Corn handling machinery)'

S. I

I

z ut S.# inzhenaro
Ifficiency,pronoters' sWoutione vhich have been pnt into ~effect
at grain receiving points of Krasnodar Territory. Muk.-eleli. prom.
23 no.4:25-26 Ap 157- (MIRA 10:5)
10 Krasnodarakaya ~rayevaya kontora Rooglavzorno,
(Grain-Drying)

Suggqstioas of issevators put into effect Im.:thsj mechanization of-
rtu*21 is.10.42&-27
loading sad unloading p
0 155. (KM 9;1)
sks
1.1rasnedAr .7a kAyevaya kesters Zagstseres,6
(Loiding and unloading) (Grab-Irihnsport4tion)

AUTHORt Zverev, S. $0V/4-59-1.18/42
TITLE: The Descendants of a Noted Barrel (rotomki znamenit~oy boohki)
PERIODICALt Znaniye oil&, 1959,.Nr 1, p 30 (PSSR)~
ABSTRACT: Reinforced concrete has become today's principal bti.ilding
material. To many specialists it w4o a surpri ej:when4t
the Conference of Architects and Enginea .ra whi:h took Place
in the Leningradskiy filial Akademii Stroi.tellstva,i Aikhi-
tektury SSSR (Leningrad Branch of:the USSR Academy.of Build-
ing and Architecture) it was stated that reinforced con-
orete is hot the ideal combination~'of metal and cohorete.
"Armocement" (armoteement) - a thick steeli netting;pouied
over with concrete - was indicated~ae a far better .material.
The Kolkhoz Market Hall 3n Leningrad was covered with an
arched roof of armocement, the span being 15 m and:'the"thick-
ness of the roof only;2 cm.
Card 1/1

IVANOV-DYATLOV, Ivan Gavrilovicho doktor teklm. nauk) prof.; AGEYEV,
Dmitriy Nikolayevich; ZVERE
.L Sergey Aleksandrovieb;
- ~LOW4*,k%~ g(WX;u4wff glT i.pior
KONOVALOV, Stepan Vasillyevi in I P I Gi~keyrconovna;
FOCHTOVIK, Gennadiy Yakovlevich; RADKEVICTI,'Boris Loonardovich;
SHCHEKANENKO, Rostislav Arkadlyevich; GORLOVA, N.B., red.;
BODANOVA, A.P., tekhn. red.
[Using claydite concrete in road and bridge~construction] Pri-
menenie keramzitobotona v dorozhno-mostovom:stroitelletve. (By]
I.G.Ivanov-Diatlov i dr. Moslcva,, Avtotransizdat, 1963. 271 p.
(MIRA 16:12)
(Lightweight concrete) (Bridges, Concrete)
(Favementsy Concrete)

ZVEREV, Aleksandr Yevgenlyevicb; KIJRWIOV, Viktor Daitriyevich;
red.
8.A., dots..
(Electron-tube and transistor pulse signal amplifiers; a
textbook] Elektronnye i poluprovodnikovye usiliteli im-
pullsr.qkh signalov; uchebme posoble. Moskyat Mosk.
aviatsionrWi tekhnologicheakil in-ty 1965., 219 p.
(WRA 18:11)

Use of flasks In bottling standard sera. Fliabl. gamut. I perel.
krovi 10 no.1:54-55 Ja 165. 19.1)
1. 3-ya Leningradskaya gorodskaya stantsiya perelivaniya krovi.

15-67-5 16815D.:
Translation from: Referativnyy zhurnal, Geol'ogiy6, 19570 Nr 5,
P 157 (USSR)
AUTHOR: Zverev, S, Me
TITLE: Improvement o "p aratus and Mothods;Usod in Wine
Seismic Explorations (Usoversh6qstvovahiye app6ratury i
metodiki morskoy seysmicheskoy~razvedkl)
ABSTRACT: BiblJographic entry on the author's dissertation for
L
IV-he degree of Candidate,of Geological and Mineralogical
Sciences, presented to (no institution given), Moscow,,
1954.
ASSOCIATION: (no institution given)
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GALPERIN,YLP. 1.J, X GCPYACM, A. V. and ZVMMiV, S. M.
/V1
"Crustal Structure Researches in the Transiti6n Region from the Asiatic
Continent to tbePacific." (Sub-title- "Ibe Facific Geologo-Geophysical
Expedition.
UM Academy of Sciences, 1957; XII SaismologY, No. 1., 31 PP (RUB'sian)
Special Committee for the International Geophysical Year,

GALIPK~Rl, -To-I., ~GMYACJW,
fiziko-mateuaiicheskikh neuic, otv. red.; ZIIJ1W,B.1., red., !z4-ya,;
RY10A, Tu.T., takhn, red.
[Studies on the structure of the Earth's ortint in the transition
region from the Asiatic.continent to the Pacific; ifork of the',
Pacific geological and geophysical expeditioa of the Academy,of
Sciences of the U.S.S.R.] Isisledevanie zemnoi.kory v oblasti
j)erelrboda bt, Azia takogo kontinents Tik~om*u, okeam; rab o ty
Tikhookeanskoi kempleisnei AspeditsiL4N
SSSR v 1957 g. Moskva, Xzd-vo .11.md. nauk.SSSR. NO i LTwelftb
aection of the. International Geo-ohVilical Year prog;amzse1smo1OqV)1
XII raidel rogrammy- MGG (sei~mclogiia)'1958. 25 P. (MIRA 11--10):
Unternational Geonlj.7siml Year, 195V-1958)
(Seismology--Ob'servatlons)
(,Soviet Far Eastm--P~ology)

V z P_ E V 5, MI
14(5) MO I BOOK UPWITATTON SOV/2818
Vsesoy=W nauchho-issledovatelskiy institut geofizicheakikh metodov
rezvedki
Fazvedochnays i ptwWalovaya goofizika, vyp. 21. (Exploration and Industrial
''112 P. (Series:
Geophysics,, No. 21) Moscow, Gostoptekbizdat, 195B.;.
Obmen proizvodstvannym opytom) Irrats slip inserted. 4 500 copies printed.
f
Xd.t A. 1. Bogdanov; Exec. Ed.: ff. P. Dobrynins; Tach. Ed.., I. G. 1redotovs,
PURPOW: ;This booklet is intended for geophysical engineering and technical
personnel in tAw petroleum ind-astry.
COVERAOt Individual articles of this collection dis6uss ImprovementsAn
methods of luttaprating seismic and,gravimetric data, testing of seismic
recei,mrs, and, the refimment of seismic station ='Plifiero. A nowavla
is described for the rapid computation of magnetic properties of rock .
sWlesp and a sum=7 is provided of experience in mrking oil contacts-
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Exploration and Industrial (Cont.) SOV/26189'
Maproved methodB and equipment of radioactive methods of surveying
boreholes are also discussed. References accompany individual.articles.
TABLE OF CONTIMi
W*blinskiyo G. N. Study of Boundary Velocities In the Basement of tba'
W#st Siberian Piain
T&I'Virskiyj D. B. Peculiarities of Seismic Recording and.Tive-
Distance Curves of Refracted Waves in Crose-Sections of them Downwarped
Parts of tW Sibirskoys Priural lye [Siberian Urat Baft "int
Zvare!,__A._& Selodc lxplomtion Surveys,on West Sibtrian Rivers 16
Andreyevj V. A. Approximative Methods of Iatarpratinl:g Tiow-Distanee
Curves of Flefracted Waves 23
Voinoy, V. A. Houiogram for the Transformation From Isonozaas to
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Exploration and Industrial (Cont SOV/2818
Urupov, A. X. Corrections for the Effect of rAy Fafraction in
Determining Velocities by Time-Distance Curves of Plefracted Waive
Shlykov.. M. 0., and V. V. Bogdanov. Tmproving the Characteristics
of an Amplifier Of SAmmic-Station SS-26-51D 41
IvanovP M. P. Voing a Cathode Oscillograph to Check Seismic
Station Baceivers .43
Yezho,r,, YU. Yo. Filling a Cistern With the Aid of &~Tractor 49
Khomenyuk, Yu. V. ProcessingAV. Osaillograms of VeAical Electrical
Soundings by the Three lbadings YAthod t5l
Nikoneakop L. M. Device for Standardizing ElectriCal Exploration
Equipment 54
Kotlyarevskiy, V. Utilizing Vertical Gravity Gradients, for
Geological Interpretations 56
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Exploration and Industrial (Cont.) sorv/2816
Avehyan., 0. K. Nomogram for Computing 9. and I r in ~&suring
Kagaette Properties of lWak Somples Ath the X-2 *4detometer 68
Fiytel.'son,, A. Sh. Example of Comparing Pasults of Geophysical
Investigations in the Nortbern Priurallye
Blankov, To. B., A. H, Bly~mntsev,, and T. N. Rlankova. Co"rative
Ifficleacy of Various FMioaative Metho,de of Determining ths
Position of the Water-Oil Contact in C&aed Wells
Man v, Ye. B. and T.;,N. Blank v&. Applying the Method of In-
diced Aotivity.in Oil Wells
Gol'skiy, 'Ya. Y&. Iml seance Counters and SpeciAl h Stureb in "Mir
Applie,ation to Butiometric Equipment 16).
AVAIIABIX: Library of Congress
card4/4 3.-T-59:

_ZVERE-V, SA,
PHASE I BOOK EXPLOITATION 1031
Prikladnaya geofizika; sbornik statey, vyp. :19 (Applied Gpophysics;
Collection of Articles, Nr. 19) Moscow, G,osto*ptekhizda't, 1958.
253 p. 3,000 copies printed.
Sponsoring Agency: Vsesoyuznyy nauchno-issledovaitel'skiy institut
geofizicheakikh metodov razvedki
Ed. Bogdanov, A.I.; Executive Ed.: Dobrynina, N.P.; Tech.'Edi:
Polosina, A.S.
PURPOSE: This collection of articles is intended for professional
geophysicists'engaged in scientific research or working inAndus-
trial enterprises.
COVERAGE: The articles are devoted to a discussion of methods of in-
terpreting various types of electrical logs, methods of :determining
the porosity, permeabilityand specific surface characteristics
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Applied Geophysics (Cont.) 1031
of water bearing rocks, and methods of determining the physical
properties of sediments and the characteristics of vari.ous,phy-
sical parameters. A.description of piezoelectric pressure re-
corders used in seismic exploration is also given. Th Ie articles
are accompanied by graphs, tables, and bibliographic references.
TABLE OF CONTENTS:
Rudakovskiy, G.I., Zverev, S.M. Piezo-crystalline Pressurd-Recorders
in [Off-Shore) .9eismic Exploration 3
Al'pin, L.M. Transformation of Electro-logging Curves 23
Zavadskaya, T.N. Notes on the Tranaformatiomof Electro-logging'
Curves 47
Berdichevskiy, M.N., Zagarmistr~~A.M. Problems in, Interpreting.
Multi-Stage Electrical Logs with Dipole installations 57
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Applied Geophysics (Cont.) 1031
Faradzhev, A.S. Investigating the Effects of Non-borizontal;Plane
Boundaries on Electro-logs 109
Shapiro, D.A. Discussion of Theoretical Problems on Diffusion-
adsorption Potentials (Diaphragms) in Borehol6s~ 129
Morozov., G.S. Methods of Determining Porosity,":Permeability.and'
Specific Resistivity per Unit Area of Water Conducting.Surfaces',
from Electro-log Data 170
Keyvsar, Z.I. Relationship Between Relative Resistivity, Pordsiey,
186
Permeability-and Specific Surface
Avchyan, G.M. Determining Magnetic Susceptibility wIith Dolginov's
Astatic Magnetometer 195
Kalinina, R.V. The Correlation Between the Velocity of PropAga-
tion of Elastic Waves and the Relative Elastic~ Constants of'Rocks' 216
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Applied Geophysics (Cont.) 1031
Filippov, Ye.M. Investigation of the Diffused Spectrm of Gama:
Radiation in-Rocks of Different Mineralogical Composition and
Densities 230
Veselov, K.Ye. Golomb, V.E., Kalisheva,L.V,, Kudymov, B.Ya.,;
Lozinskaya, A.I. Review of P.I. Lukavchenko's* "GrAvimetric Ex-'
245
ploration for oil and Gas"
AVAILABLE: Library of Congress
Card 4/4 MM/sfm
1-22-59

-Lug", ",luawly P. S. GALPERIN, I.,
MY, 1,
KOSMINSKAYA, 1. P..,YICffO`l`A,, G. 0.
"Deep Seismic. Sounding' in. the Zone of Transition*~.etw'en the Asi~tic
Continent and the Pacific Ocean.".
Pp_per Presented at CSAGI Yeeting, 30 Jul lei Moscow
q Aug
Ivailable in Library

SPY/49..59-4-7 20
AUTHOR: Zv~erev, S. M.
TITLE; The kiglicati,9n of Bound Recordings for Determination or
Distances in~7 4�smic Soundings in the ..8ea (Ispollzovaniye
zapisey zvuka d1ya opredele'niya rasatoyaniy pri rabotakh po
glubinnomu. seysmicheskomu zondirovaniyu na,more)
PERIODICAL: Izvestiya Akademii nauk SSSR, Seri .7a goofiziche.skaya,
1959, Nr 4, pp 560-569 and 2 'plates (11SSR)
ABSTRACT: Two methods of exact determination,of d;Lstance fvom the
recordings of sound waves are describod. One of th6 methods
is based on the first recording of the* sound wave axid 6a its
velocity in water in relation to the,4epthand profile'of the
sea-bed, The accuracy obtained in uoing this method was 0.4%.
The second method is based on the recordingd of thelirst
group of sound waves. The accuracy ia this case was 0.~7%,
The results of experiments are illustrated i-a Figs I to 10
and in the table on P 568. Figs 1 and 2 show photographs of
the seismograms. Fig la illustrate's 't-lie 6uocession,of entrance
waves at different impulses of sound 'at various points (shown
in 19) along a.profile. FiS.2 illustrates succe-ssive seismo-
grams obtained when the distance from' the:points of ~ detonat-
ion was gradually increased. The firat entering impulses are
Card 1/3 framed. The datalobtained from the seismograms Figs 1 and 2

13O1r/49--59-4-?/20
The Application of Sound Recordings for Determination of Distances in
Seismic Soundings in the Sea
are tabulated in the table on p 568 where Colilmn,l gives
:- ime of; first entrance
the seismogram number, Column 2 6. 1
Column 3 - time of group entrance, Column 4 - approximate
distance for V =-14?0 Column 5 - velocity of first entry
as in Fig 6 Column 6 distance calculated from first entry,
distance caculated from group recording. 'Fig 7 represents
the sound velocity in relation to the,'idepth,of the Pac3':fic
near the Kuril Islands. Fig 4 sh.ows'the &~4pft of sound velo-
city V in relation to the various di8taA008 foUnd'froM tile
impulse of entry (1 - layers-of mnif6rm i5radient 2 -, lowest
layer); Fig 5 - trajectories of sound rays accoraiag to their
entry; 1 - first arrived, 2 -:second.~~3 - :third 4 -, touching
the sea-bed. Fig 6 represents the vLocities coIrresponding.
-to the first entrance vf sound waves along, the profile,5.8 km
d:eep. Fig 8 gives the time dif f erence of entry of the 8eparate
impulses; Ag 9 amplitude of the first entries from the
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SOV/49-59-4-7/20
The Application of Sound Recordings for Determinat.ion of Distances in
Seismic Soundings in the Sea
seismogram in Fig 2 and the projectories~of the corresponding
rise. Fig 10 shows the relationship~'of the velocity :V and
the distance from the source of the r'ays x to the' depth H.
There are 10 figures, 1 table and 11 Soviet referehoes.
16SOCIATION: Akademiya nauk SSSR, Institut fiziki:Zemli (Ac~ademy of
Sciences USSR, Institute of Physics1of the Earth)
SUBMITTED: August 18, 1958.
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S/169/0/000/012/001
..~I~~00010~12100~1~~
~9/
D228/M5
AUTHOR: Veyteman, P. S., Gallpering,"Ye. ;1.# ~Zverev,
S M. Kosminskaya, L P.,' and Krak;hina,_ft7M.
TITLE: Some data on the structure7'6f the crust:in the
,transitional zone from the!:Asiatic Continent to
the Pacific Ocean
PERIODICAL: Referativnyy zhurnalq Geofizikaj no, 1.2i 1~61,
5, abstract 12A34 (V eb.,.teolo; resultaty prikl.
geokhimii i geofiz. Razdel 2. M., Gbdgeol-
tekhizdat, 1 960j 37-42)'
TBXT.- 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 com Iplex,'of methold,s included
seismic surveyingv aeromagnetic surveying, and gravimotry'. Geo-
logic investigations were also made in~*coastal distri6tsa It
was possible from the processing of preliminary data'.to expose
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S/169/61/000/012/001/089::
Some data on... D228/D305
3 main types of crustal structure: continental, oceanic, and
intermediate. A schematic toning of the study region was made
from the crustal types, and transitional areas from,one type to
another were distinguished. The transitional Iregion from a
coutinental- to an oceanic-type of crust in the vi'cinity of.the
KurileB 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.
,CAbstracter's note: Complete tranalation,l
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113/014/61,/000/061/001/toi
7
A054
/A133
AUTHORSt Veytsman, P.S.;-,Ga!'perin. Ye.I.; Zverev S.M I Kosminskay6 1.
P.; Krakshina, R.M.,-. Mikhota, -Yu.V.
TITLEt. Some results of atudying the Earth's cruist in Ule area of the Kuril
Island are and the adjoinin~g areas of tho Pacific Ocean b6sed.on
deep seismic sounding data
PERIODICAL: Izvestiya Akademii Nauk, SSSR. Seriya geoldgichoskaya, no.1, 196.1,
81 - 86
TEM In 1957-58, Soviet geologists surveyed-by deep' seismic sounding the,
'
ar'ba of
geology of the region between the Asiatic continent and the Pacific, the
the Kuril Island are and surrounding parts of the Pacific. These latter: regions
are particularly interesting, becalase inIa rather nar.row (300 - 1~00 km) zone the
Earth's crust here shows great variations which can be':olassified in three main
groups: 1) continental type crust, cons I18tIng of an upper aedimentary and two
lower: q 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 k~/sec. 2) The
.oceanic part of the crust consists of a thin sedimentary less than I km thick and
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01
S101116110001001100110
Some results of studying.the Earth's crust A054/Ai"
a 5 - 10 km thick basalt layer. The wave velocity in this zone (outside the
sedimentary layer) is about 7 kin/sec. 3) The intermediate zone has an i'ntormediate
character both as regards thickness and structure of its layers (in general the
bedimentary-basalt structure prevails)., The classIficationinto these three groups
was b4ffed on the time-d1stanoe curves of primary waves and the ratio of average
speed v to depth h.. The geologicil map of the surveyed areat .shows that.the,
intri~,ate alternation of these three types of crust-structure cannot be observed
in th~ direction from the island to the ocean only but also,along the entire area,
from the Hokkaido Island to the Peninsula of Kamchatka, The most in-tridate.crust-
structure ~s-found in the area between the island ara iind tlje~Kurile_Ka~ehatka
deep trench. According to the crust-struature this area can also be divided Into
three partal a) its northern part shows a continental, b) its southern ipart part-
ly a continental, partly an intermediate character, while c) the central part also
consists of two structures.- one of an intermediate and one or an oceanic character
and seems to be the continuation of the'deep-water area of the Okhot Best. In order
to establish the changes in propagation velocity in the transition zone of one
.,ypical,area of the crust into another, the average V-;yalues have been determined
at a height of 7 km from the bottom. The comparison of the~.velocity curves',with
the relief of the bottom revealed a strict regularity in the relations: the oceanic
qa~rd 2/4

a
16 1/001/1001
'~00/t'o
'~/A
Some results of studying the Earth's crust AO 13
plateau corresponds to the highest aver .age values of V, which drop sharply-In
the direction from the oceanic plateau to the tabular~~zone,,,in northern and
southern direction as well, in the area of the eastern slope of the deep trench.
The lower values of V in the tabular zone are connected with.thiok sedimentary
layers, (near Kamchatka), The areas close to the oeniral and the southern part
of the are display high V values and the high V-values for the oceanic plateau
show a stable character (about 7 km1sec). Between t he islandarc and the deep
trench however, there are also extensiv 'e low-water areas. tdhen comparling the
bathymetric data referring to this area and the structure df the crustit can be
established that the low-water areas of the Pacific at the northern and southern
regions of the arc correspond to the continental type of the crust, whereas the
deep-water areas of the central part of the island are correspond to the inter-
mediate type of the Earth's crust. The same regularity is also observed for tfie
western-coast of the island are. Gravimetric data show that in regions of the
continental type crust structure the an 'omalies of the:gravity-force display low
values.as compared with those registered for the ocean, while in the zones.of
intermediate crust structure the anomalies also have medium values between oceanic
and continental anomalies. The boundaries between the zones of various A g
values correspond roughly to the boundaries betwene the zones of various crust-
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S/01 1/16 1 /000 /00 1~ /00.~ /00 1
Some results of studying the Earth's crust A054/AI33
structures, The.most-intense volcanic activity for -the past m0 years Was record_
ed for the central part-bf the arc, with an intermediate crust-structure, .while
the higheat seismic' actIvity was observed in areas Willi a c6n-tinental type otruc-
ture of the core. Ifi t4e Xuril arc remarkable and intensive recent movefffents
have been observed, according to which the area can again be divided into thi~ee
part: in the northdrn. and -sbuthdrn parts a remarkable up-lif ~ is established,
whereas the central part - bordered by- the Bus-sol' and Kruztnishtem straitsf had
subsided. There are 4 figures and 9 Soviet-bloo refar%ences.-
AOSOCIATIONj Institut fiziki Zemli AN SSSR, Moskva.(Institute of Geoph~sics) AN
USSR, Moscow)
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S/011/61/000/002/001/001
A05J/A129
AUTHOR: Zverev, S. M.
TITLE: On the structure of the sedimentary mass in certain sections of the
Pacific Ocean according to seismic reflected wave data
PERIODICAL: Akademiya nauk SSSR, Izvestiya. Seriya Geologicheskaya, no. 2 1961,
8o - 86
TXKT: The Institut fiziki Zemli (Institute 6f the'Physics of the Earth) of
the USSR AS conducted a study in 1957 - 1958 on deep seismic sounding in the
earthts crust of the north-western section of the Pacific Ocean:and adjoining.wa,
ter areas. The main method of investigation was primarily based on observing
seismic waves from the deep-lying interfaces of the eart-h's crust to the s~urface.
Data were obtained on the structure of the upper thickness of oceanic sediments.
Investigations
carried out simultaneously of the vertical reflections from
were
the ocean bed', surface and interfaces in the Wiments using,two majob methods:
Reflections were registered by one channel in the exploding of. high charges mount-
ed on a moving ship. The experiments showed that the reflections were registered
favorably at frequencies of 50 - 70 cycles (Fig. 1). A multi-channel floating
Card 1/ 11

s/011/61/000/002/061/001
On the structure of the sedimentary mass in certain ... A051/A!29
set-up was used during brief stops,of the:vessel, similar to that used in.marine
seismic explorations of petroleum. It was found that the multi-channel set-up
was more effective and sensitive than the single-channel~apparatus. The~multi-
channel set-up was used to register the raflections from1the interfaces in sedi-
ments both In the region of-the ooean floor as well as in the deep depressionand
various parts of the shelf. It is pointed out that the yertical reflection cuts
obtained by observations may be distorted by phenomena of Pul~i~le refledtion'of
waves in layers by Interference of waves,the length of which'im.the same'as the
layer thickness. The observations of the vertical refleotions were conducted.at
all depths of the deep seismic sounding carried out in 1958 and the obtained data
for the Pacific Ocean near Kamchatka and Komandorakiy Islands are submitted.
The present #I-ticle deals with the layers of sedimentation thickness expressed in
time of the vertical reflection rather than layer strength. Recordings of multiple
reflections of waves in the water depth obtained on the selsmQgrams weroused to
evaluate the rate'values in the sedimentations as well as the reflection coeffi-
cients of various multiplicity. Favorable~coincidence ot experimental data with
the corresponding theoretical values (Fig. 6) lead to the conclusion that.the:rate
value 1.89 - 1.91 km/sec was the rate of the transverse i~i4ves, and in deeper layezu
of the sediments the rate value of the longitudinal waver, was about 3.2 - 3.5 km/
Card 2/11

S10111611000190210011001
On the structure of the sedimentary mass in certain ... A05,1/A129
/Sec. The following average values of the reflection coefficients were obtained
from the ratio of the amplitudes of the lst and.2nd order vertical refl6ations:
for the floor surface -0.17, for a sharper interface -0-58, for the deepest re-
fleeting surface -0.34. Estimations of the vertical rerlection coefficient using
Raleigh's formulae showed that the following rates V and.densities f in the sedi-
mentation layers correspond favorably with the above-givoin datai a) ocean: bed
sediments (not compressed)z V 1.65 km/see f - 1.35g/cm3; b) deeper,sediments
(compressed): V = 3-5 km/sec, 2-5 9/clr~~, c) sole of thesediments (crystal-
line ores): V = 6.4 km/sec, f 2.80 g/cm3. It is further seen that in all three
profiles investigated the nature of the sediments change~labruptly when passing
through the deep-lying depression. At the No. 9 profileo passing in the south-
eastern section from the southern. edge of the Kamchatka Peninqula and on the
western slope of the deep-water depression, there are three main reflecting~
horizons with intervalsof time At between the first and last* reflections - 0.2
0.4 see (Fig- 3). Tfie No. 7 profile layer is similar to thmt of 9 (Fis.~ 4).
The author draws the following conclusions from the data obtained:. 1) the deep-
water depression separates the horizontal-laminar, comparatively slow-changing
sedimentation layer of the ocean bed from the complex layer of the shelf sediments.
The thickness of the sedimentation ores of the ocean bed changes slowly with an
Card 3/11

8/011/61/ooO/002/001/001
On the structure of the sedimentary mass in certain A05j/Al29
increase in its distance from the deep-water depression.- '2) the surface of the
ores covering the sedimentation layer of the ocean within the borders of the '
regional embankment of the Kurilo-Kamehatka deep-water depression.has a complex
surface. With an increase in the distance from the depreasion.the surface of the
sole becomes more calm. At distinces of 150 - 250 km from the~axis of the de-
pression, high fault throws are .noted,"cutting all the sedimeptation layers and
are expressed in the floor contour. These faults are comIdered to be the results
of-comparatively recent tectonic movements, oc *curing at the edge'of the Ocean bed
in the Kurilo-Kamchatka deep-water depression. The thickness of the sedime~atations
within the limits of the regional embankment of the Pacific Ocean at tire Aleutes
deep-water depression is two to three times greater than the sedimentations of,the
Ocean bed near the -Kurilo-Kamehatka depression. This indicates that the conditions
are quite adverse for sediment accumulation in the outer sectio .ns of these two
regions. There are 6 figures and 3 Soviet.references.
ASSOCIATION: 'Institut fiziki Zemli AN S88R, Moskva (The~Institute of th61hysios
of the Earth of,the USSR AS, Moscow)
Card 4/11

.9/011/61/000/-302/001/001
On the structure of the sedimentary mass in certain ... A051/A129
Figure 1: Records of waves reflected from the surface of the floor (A)Iand the
interfaces of the sediments (1,2,3) obtained on a movint; vessel, 3 and 4 u~p:er
tracks signal recording at various'amplifications
U
4 1~ t'
R,
L
Card 5/11

s/oli/6i/000/002/001/001
On the structure of the sedimentary mass in certain A051/Al29
Pigure 1 continued:
lit;
Card 6/11

S10111611000100210011001
On the structure of the sedimentary mass in certain ... AD.5!/A129
Figure 2: Recording of the reflections from the floor aurf ace and the inter-
faces in sediments (1,2,3) obtained with the aid of a~mlilti-aliannel set-lip"
Route 1-5 above- recording of various hydrophones of,th6 Muiti-charinel se't-up;.
At 8 routes-recording of the Ist, 3d~and 5th hydrophones with a lowered 6ensi-
tivity.
wi-EP-1
N1JJ Vt
17,01
- ~Ik U zlx_ --Z,4
Card 7/.11

S,/O I 1/61/000/002/COI/00 I
On.the structure of the aedimentary mass in certain ~05.1/AI29
Figure 3: '-time of reflection, see. Times of vertical refl6ation at profile 9,
transgressing the Kurilo-Kamehatka Deep-Water Depression from the southern end
of the Kamchatka peninsula. 1 - times obtained in observing . the reflections on
a moving ship, 2 by multi-channel set-up, 3 - places on the profile with sharp
change of the time of beflection from the bottom and interfa~ces in the sediments
fit 'VI
(D;
J-j
__-_ ~_MTI
Q
Onr, Bptmexs OPUXOAA UPTRKSAMMI OTPAMONNA MA PP44HAS 9. * HePeCtMAjoLuem Kypwjw-Kswvacyi* my6oldlomyw us-
AIIHY Or IOXHOM ONO"SAPIO nQfi)OC?PG$8 Kawtows,
NPINIMI. MA"OXMI pVV g1 WACNM%X MgAMft WX An;~.rn."U -0.6.9. A- -~A-4 V414.~A. A-4 upwo
M-4 A*- 0 M6-4 4
Card 8/ 11

-9/011/61/000/002/001/001
On them structure of the sedlmdntaz7 mass In certain A 05.1~ A129
Figure 4: 1 times of reflections, see, 2 - ocean de:pth,lm~ Times of the
vertical reflection on profile 7' *transgressing the, Xurilo-yamchatka Depp-Water
Depression from the region of Petropavlovsk on Kamchatka. Symbols of Figure 3
t.1yG"OGOAN$1C WANdY OT PliUl T. ntrINMIS-
AOUX its KIM-tallm.
Card 9/11

5/01 1/61/000/002/001/m,
On the structure of the sedimentary mass in certain 4051 A129
Figure 5: 1 - oceaa depth, km' 2 - time of reflection, sec., Times of.the~
vertical reflections on profil; 8, transgressing the Aleutes-Deep-Water'Depressio
from the Komandorskiy Islands.
in 'ISO Its
7.
J.4
Card 10/11

S10111611000100210011001
Onithe,structore of the sedimentary mass in certain A05j/Ai2g
1~kgure 6: Comparison of experimental and calculated~amplitude graphs' for three-
fold reflected water waves in the" 'ocean for determining the rates in the sediments
I-experimental data, 2 - calculated data for the firsit~.oritical angle,~ (sec6nd
maximum of the graph corresponds to the'value of theirate in the floor layer of
about 1.65 km/sec, the first maximum-to the value of ~ the rate of the longitudinal
waves in a deeper layer of sediments of about 1.90 km/sec), 3 calculated data
for the second critical angle (first
maximum corresponds to the rate of the
transverse waves in a deep layer of 20-
sediments'of about 1.90 km/&ec).
Val
~3
:47 3 59 75 189
Card 11/11

2242)
~vl
/.goo S/049/61/000/002/001/012
D242/D361
erlyanov, eytsman, P~*l %, allperin,.Ye.' I.,
Zayozichkovskiy, b4~ A.', Kosminskaya, ,
I. P., Krakshina, R. M., Mighota,~ G.'G., And Tulina,
Yu. V.
TITLE t Deep seismic sounding in,the transitional zonetbeiween
the,continent.of Asia.and.the Paoifit Ocean duping
the International...Geophysical Year
PERIODICAL: Akademiya*.nauk,SSSR.~ -Serlya Sepfizicheskaya.:
Izvbstiya,,no_2,.19d1,.169-184 i
TEXT: As part of.,the..IGY program;.scientiats...of.,'the.,Institut~
fiziki-zemli.-AN-SSSR- (Institute'.'of_PhysicB..;0f_ the- Zarth, AS, USSR),
the Vaesoyiiznyy'rauchno-issledovateliskiy..inatitiit.geof iziki ~
Mini st eratva . ge ologii - i.. okhran~r_ziedr - SSS R _(All 4zii on Scientific-
Research...of- the -.Mitiiiitry..6f,.'Geology.-atid.,Xiueral..Resources. of ~ the
-USSR) an4.other.organizationd..investigated.~the-crustal,stmcture
of--the-Okhotsk, Sea. by,means..of .-deep. seismic-sounding. The, area
.Card I/11

2949X,.
49/61/000/002/001/012
42/D30
E
Deep-seismic.soundingo*e
was,chosen since,.very.little.is-known.of the...nature-of the,crust
in such-transitional-zones.between.continents.ancl.oceans.~!Itlis
separated from the Pacific.,by the,Kurile Island,Arc which is
bordered-by.& deep ocean containing.sciamoldgically..active,zones
with.deep foci-and-large-positive.-gx-avity.atiamalies. The main
0b servati an s..were.. undertaken. dla:.~g_ profile a.. with I lengths of
-.about..8000-kmv orientated-tranaveteely-to.the,,supposed..structLires
of-the-study area,.as-described,-by.Ye...I..Ga.11pering A. V.,Gorya-
chev and S. M. Zverev (Ref."1: Issledovaniyq*..,zemnoy kory.v:oblasti
perekhoda.ot-Aziatskogo-kont~nenta-k-Tikhomu,.okeany ~(Inveatigation
of -the Crust, in -the.Area. of Transition, betwee'n.. the Continent of
Asia and-the-Facifi~..Ocean) Sb..XII,razdel ~rogramy.MGG (seysmo-
logiya), No. 1. Izid. AN.SSSR, 1958).and,.by . G. Vasillyev et al
(Ref. 2: Issledovaniye.iemnoy kory v oblasti.perekhoda ot Aziats-
kogo.kontinenta.k.Tikhoma okeany (Investigation of the Crust in
the Area. of Transition between the Continenti.of Asia and the
Pacific Ocean) Sb. "Seysmicheskiye..issledovaniya,v.period MGG1'
Card 2Ai.

22413
S/0'49/6L/000/002/00,L/012
D242/D30i
Deep.seismic..sounding...
No. 4, Izd.,An.SSSRt:1960)._..The area,near-Iturup.teland wad also
inv.estigated-.on.-a..-speciaL,grid. The data was.',coll6ated by the
method of.movable.-explosion..points,with.-single!.?.point..recording
at fixed stations;..the detaiLs.,are.given by.,Ye..I. GaLlperin and
I..P. Kosminskaya-(Ref...3:..Osobennosti.,metodiki...gLubinnogo
seysmicheskogo,.-zondirovaniya--na.-m6re - (Features .,of. 6e Xethod'of
Deep.Seismic..Sounding..at..Sea)..Izv.,AN,.SSSR,.Ser. geofiz.,.No. 7,
.1958). _Use vas.. also - madd..of.. the,.results..of..e~.13eriments..condUcted
.....by.G-.A.,Gamburtsov'(Ref...64.-.O.glubinnom..seysnacheakom-zorLdirovanii
iemn;y 'kory. i ' nekoto-tykh-.drugikh...priLcizheniyakh.-.met6dadL..vyaotca- ~'
chuvatviteL!noy.zapi'si.,aeysmicheskikh..kolehaniy..~Tlie-Deep.Seismic
Sounding., of_ the. Crust.. and.,some- other.Applications ..by--.the -Method ~ *
of.HighLy.-$eusitive..Recording-of,.Seismic-OacilLations),.Izbr..tr4I
Izd.-Akad..Nauk-SSSR L960 ) and.P. S.,Veyt9mmn,(Ref.;7: O,resull
tatakh.rabot po glubinnomu,'.seysmicheekomu.zondirovaniyu zemnoy
kory.v oduom.iz g6rnykh rayonov Sredney.,Azii.(Pesults.of..the~Do-ep
Seismic-Sounding-.of-.the.Crust in..a.Mountainous District,of-Central
C ard 3/i1

22423
S/0'4?/61/000/002/061/012
D242/D301
Deep seismic,soundinge&j,
Asia).Studt.Geophys..et-Geodaet., '.No -2,-1958),in.,continenta,l
.areas-of..the-Soviet Union.-In-contr;st.-to forleigm-practice,, it
was.possible-by.-employ.ing-severaI recording.station~.-on.-the.:I:ine
of.observatiou..to.obtain.-the.types.,of..time..?t'ra'vel.durves shown
in Fig.. 2. during.. a- single -,boat Journey. _'Wave 'recoi:dings. were
also,made.on-the..explosion..vessel,..-The..bottoni,.of..reflections
.provided--A*.nfomation-on..the-depth.,of.,water-and-the:,str,ucture of
bottom-se'd3"ments-in..accordance.with-the.-procedure.merLtioned by
S. M..Zverev.(Ref,,,l0: O.stroyenii...osadochnoy..tolsbchi-nekotorykh
uchastkov-Tikhogo..o!ceana.po.dannym seysmicheskilch ot-razhennyIch
voln.,(Structure-of.the.Sediment..Layer..of Certain-Parts of the
Pacific,.Ocean..from-the.Data of.RePlected Seismic.14aves) Izv.~
AN S.SSR, ser. geol., No. 2, 1960)..-The-exploslons-iof charges
weighing,.about,loo-kg..were..recorded..ou..a.low-!.frequenoy.seismic
device. with. a. f iltration.-range.-of..0.7.. .! 15.hertz..at distances of
up to.200 .-. 250 -Ian, on, the. sea - and.-100.,-. 150 - kmL,on the.ocean. The
receivers..consisted,.of,.hydrophones-with-caseade,.intensifi--ation*
Card 4/11

3/040/61/000/002/001/012
Pr g* 14,
Deep sciame -ft D242P301
sounding...
A7
Fig. I,
Examples of,
/M w av
hodograph .3 %"2
systems ob-
tained*in the
Olchotsk Sea
(14-M, ~_11)
4 ~70
and Pacific- Av
e ~'Po'
P4
Ocean (6 0)
rt.
P P.
'~j
Card 5/'LL -ITP11110PU CIt"eit rOAOr aloft' Itaity,tetutwxa030TOICOM 110pe (14-.xi, L-.Nt)
It TIIXO%t WHO

22103
S/049/61/600/002/091/012
D242/001
Deep seisraic:sounding.,.
The w4ves were..separated,and-correlated byirecording.their.inten-
sity simultaneously with-the.. construction.. of -thel.hodograp~hs- which
were set out in such-a..way.that.the coordinate~origin.corresponded
to the position,of..the,rdeording station,.the time-of-wave-arrival
being plotted over the.,positibns-of the explosion. sites.,. Despite
the complexity of the.. retordings,-'e specially in islarid. and -littoral
areas, several types of,waves.related-to orustal, disconti-nuities,
bottom sediments and the water. layer.were! distitiguished on the
seismograms, including refracted longitudinal.waves.associated
i-rith boundaries in the sediment layer. (Psed) and the actual trust
.(PO and P*) and with'the.Mohorovicic discontinuity at.the.base of
the crust. Waves of.the-first. type. have.. speeds I of..5. Ian/see and.
were . obse*rved near. the Ktwiles and. on most i's'ea., profiles.: . The
velocities. of -tho.1?0. and F* waves,mainly re*corded. in island areas
and near Kamchati~W-a'r-e 6-and 6.5, - 7.1t-m/see-reopectively. The
leading P waves refracied :Crom.the,llohorovi'cic.discontinuity
Card 6/11

S/01,09/61/QOO/002/601/012
D242/b3O3_
Deep seismic sounding...
tra,~el,'.at speeds of.about.8.5 km/sec.- Waves',: (PR)~ ref lecte& fr 6M
the Mahorovicic-and other discontinuities were,also noted in :
addition-to..the.refracted-.waves,;Ialthough it,'was only possible.
to. distinguish them. iTith- any-.clarity- in certain regions . - 6ainly
the northern and..centrAl.parts of,--the Okhotsk,,Sea-Vwhere their
amplitudeAs..greater-than that of.the other.;~oave-types. An alysis
of the hodographs..diseloses-the.-existence.of,three main,wave-types
defined.by.differences.in the ariival',.and tr~nsit~;time of the '
waves, by the areas where they were rec6rdedand by.'the'pref3ence
or absence of the PO and P* groups (Fig. 9)., By plotting the 2
values for.the relationship.of the mean..velocity v to the depth-
h, three types of velocity cUrves. corresponding.. to.-Coatinental-
intermediate.t....and-.oceanic~"type-.hodographs.were..also '-obtained.
Continental.~type.-hadographs..are-.characteristi.c.. oflarge.areas
..in.the.northern-and..central..parts-of...the-Okhotsk..Sea-and in the
.northern.Kuriles,...where-work-by-P..S*. Veytamah.et.,aI.(Pef. ll-.~
Nekotoryye.rezul!taty.izueheniya.stroyeniya.zemnoy kory..v oblasti
Card 7/11

22423
S/049
/61/000/002/001/012
D242/D301
Deep.seismic sounding...
Kuril1skoy,ostrovnoy.dugiA prilegayushchikh,~ uchastlcov Tikhogo
okeana podannym glubinnogo-.seysmicheakogo,zo6dirovaniya (Some
Results.of.the Study.-of,Crustal.Structure.iii.the Kurile Island,
Arc and Adjoining.Parts-,of.the Pacific Ocean from'the Data~of
Deep Seismic Sounding)..Izv..AN SSSR, ser..gedli.,.No. 1, 1961) has
already indicated..that,.the.crust.-is.of.the..continental.,type,. In
the..continental-!!type,.hadographs..the.arrival...times.:of.the PoVP*
and,.P,-waves. are .. at - a maximum, the. transit. tite., of. ~1 the P waves I
being,l8__-!.l9 sec. There are-two-forms-of..h.odograph; one repre-
sents.. a - three, layer.. crust.