SCIENTIFIC ABSTRACT NERESESOV, L.L. - NERSESYAN, A.B.

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• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R001136620001-1
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: January 3, 2017
• Document Release Date: August 1, 2000
• Sequence Number: 1
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

S/169/61/000-/O!O/1007/05-i
D228/b3O4
AUTHORS-z Hersesov, I. L.9 and Khalturin, V. I.
TITLE: The Karatega earthquake of January 7, 1956
PERIODICALs Referativrqy zhurnal, Geofizika, no. 10, 1961, 109
abstract 10A.118 (Tre-In-ta seysmostoyk. str-va i seysmol.
AN TadzhSSR, 7,j 196o, 87-96)
TEXT: Instrumental and macroseismic data are stated concerning the
six-mark earthquake which occurred in the Garmo district of the Tadzbik
z3R. Z-Abstracter's notes Complete tranalation.2
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3/519/60/000/008/003/031
D051/DI13
AUTHORS3 Riznichenko, Yu.V.; Nersesov I,.L1
TITLE-. Contribution to the development of the principles of a quanti-
tative method of seismic zoning
SOURCE. Akademiya nauk SSSR. Sovet po saysmologii. Byallaten', no. 8,
Moscow, 1960. Voprosy seysmicheskogo rayonirovaniy& ? 36-59
TEXT: The authors discuss the basic features of a quantitative method of
close saismio zoning, which was developed by the Tadzhikskaya komplekenays
seysmologicheskaya ekspedit-siya (Tadzhik Large-Scale Seismological Expddi-
tion) (TKSE) of the Inatitut fiziki Zemli AN SSSR (Institute of Physics of
the Earth of the AS USSR) and the Institut sayamologii AN Tadzhikskoy SSR
(Institute of Seismology of the AS Tadzhikokays SSR). On the basis of data
obtained by observations from 1955 t.-) 1957 in the Garmskiy and Stalinabadakiy
rayons,a-map of seismic activity of these territories was plotted, which per-
mits calculating the mean times of recurrence of earthquakes of different in-
tensity *n individual arsaa. The quantitative method of close seism4c zonijl&
whose development is still in the initial stages, is intended to fAl
a gap
rard 1/4

S15191601000100810031031
Contribution to the development ... D051/Dll3
in presint Soviet saiemic reaearc.h, in which the methods of genezal zoring
kon a ~45-000,000 scale) and microzoning (is100,000) are mainly used. Quan-
titAtive c1cise seismic zoning, which ia carried out on a 1.500,000 scaleg is
an attempt to combine nomprehensive seismic and geophyeical reaemrcch~ so as 'Dr.
entirely satisfy the needs of earthquake engineering. Basic features of the
new method are the quantitative characterization of earthquake intensity by
frequenoy speztxa and large-scale consideration of microearthquakes,in order
to extrapolate strong ones. Discussing the method in details the authors
first present some basic results obtained through the study of frequency
speeatra and the fading of vibrations with increasing distance from the earth-
quake center, i.e. dyr-amic chara:.;teristics of earthquakes, propagation of
Beismic waves depending on geological structure. They cozsider that the best
quant4&tative method of representing seismicity is using earthquake tracury-Orice
N and seismic activity A as charaoterizing quantities. N 16 the ueual ordi.-
4
nate of earthquake reourrence graphs (in regard to the surfaoo of a region
cr the volume of a space it is called "normalizad") and A designates the
"level" of seismicity in these graphs. A graph, for instancep showing, de-
pending on earthquake intensity, differe-A earthquake recarrence cuzves for
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Contribution to the development... D051/DI13
various areas will, consequently, for a given earthquake intensity present
different earthquake recurrence levels of these areas. The unit Of A (A Gan
be indexed Alf A29 etcog according to the seismic intensity E w 10192j..o
joules) corresponds to the annual recurrence of one earthquake on an area of
100 kno Rendering of the activity In A umits proved useful to the TKSE,
7
viluioh,-vith a dense network of stations, worked on limited territories of
high seismicity. Another important characterizing quantity is
4 log N 4
6 log E E - earthquake intensity), which is constant for r-ec"Alinear
recurrence ourves,.i.se for curves depending on seismic intensities up to
1016 or 1017 Joules, The knowledge of the law of earthquake recurrence
ff- N(E) for a given district,permits calculating the mean densi&y of the
energy flow of all earthquake centers in this region. In this connection,
the authors dqrived some formulae for W (energy flow) and f.-(tootonic move-
ment)9 which, however, due to the insufficient knowledge of X(E) regulaxi-
ties are only relatively important. Turning to the mapping of seismic acti--
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S/519/60/000/008/003/031
Contribution to the development... D05l/D113
ityg the authors give a detailed account of how to determine the density of
epicenters of a region in units of seismic activity and how to establish
the seismic activity of the area according to the epicenters of earthquakes
of various Intensity. The concluding part of the article contains informa-
tion on plotting and on an analysis of the initially aentioned map of seismic
activity in two Tadzhik rayons. The folloviag Soviet scientists are mention-
ed in connection with seismic resoarcht A.G. 11azarov, S.V. Madvedsvp VJ.
Buns# Te.Fe Savarenskiy,, G.A. Gamburtsev, and S.A. Dzhibladae. There-gre 8
figures and 36 referosoess 18 Soviet and 18 non-Soviet-bloo references. The
four nost recent references to English-language publications read as followas
B. Gutenberg, C.F. Richter, Magnitude and energy of earthquakes, Nature, IT6,
no- 4486v 1955; P.S. Axandq Two proposed measures of seismicity, Bull. Saian.
Soco Amep 469 no* 1p 19561 C* Tsuboi# Energy account of earthquakes in and
near Jspan. Journe Physe Earth.9 5o no- lo 1957; J.V. Riznioheako, On quan-
titativo.deteraination and mapping of seismic activity, Annali di Geofisica,
Roma, v. XII, no. 2, 1959-
ASSOCIATION; Institut fiziki Zemli AN SSSR (Institute of Physics of the
Card 4/4 Earth of the AS USSR)

or
S/51 60/000/008/019/031
D051YD113
AUTHORS: Bune, V. I.;
TITLE: Some results of a study of the seismicity of the Stalinabadskiy
rayon
SOURCE: Akademiya nauk SSSR. Sovet polseysmologii. Byulleten', no. 8,
Mosccw, 1960. Voprosy seysmicheskogo rayonirovaniya, 157-165
TEXT: A report on an investigation of the seismicity of the Stalinabadskiy
rayon is given. The investigation was carried out from 1955 to 1957 by the
Stalinabad section of the Tadzhikskaya kompleksnaya seysmologicheskaya
ekspeditsiya (Tadzhik Comprehensive Seismological Expedition) (TKSE). This
expedition was organized in 1954 under the guidance of G.A. Gamburtsev.
Using a network of seigmic slations, the section recorded about 300 micro-
earthquakes (energy 100 - 107 joules) without taking into account the recur-
rent shocks of the Hurek earthquake of September 22, 1956; for comparison,
the authors state that only about 150 earthquakes were recorded in the years
1907-54. The results of the observations are shown on maps of epicenters
and seismicity, both included in the article. The latter was compiled by
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Some results of a study D051 D113
the authors together with Yu.V. Rizaichenko, who proposed and described the
method of compiling maps of this type in two publications. The maps permit
two basic epicentral areas in the Stalinabadskiy rayon to be distinguished:
W The Gissar (northern) zone which lies along the southern slopes of the
Giis'sar Mountains and (2) the southern zone which lies along the southern
slope of the Gissar Valley. Both areas are distinctly confined to the faulte
which bound the Gissar Valley from the south and north. The focus depths of
these zones vary from 5 to 30 km. The central part of the valley has only a
limitea number of epicenters and divides the epicentral zones; on the basis
of geological and strong earthquake data, these zones were also distinguish-
ed by I.Ye. Gubin and L.B. Vasillyeva. The distribution of earthquake cen-
ters determined according to instrumental observations over the past 27
years basically confirms the existence of two seismic zones. Their activity
is characterized by local variations so that they constitute unusual mosaieN
of seismically active sections. Another feature is the occurrence of strong-
er earthquakes in regions of reduced seismicity or of microearthquake epicen-
ter accumulationt this phenomenon, however, still needs further study so
that a regular correlation between micro- and strong earthquakes can be es-
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Some results of a study D051/D113
tablished. The rest of the article is devoted to problems of earthquak-e
recurrence in the Stalinabadskiy rayon. As can be seen from two graphs, the
recurrence curve plotted according to strong and microearthquake data of
different observation periods of various duration, essentially coinoides in
linearity and direction with the curve representing earthquake recurrence,
exclusively on the basis of data obtained from 1955 to 1956. This shows
that data on microearthquakes can be used for judging the seismic activity V/
of a given territory. The earthquake recurrence for the northern and south------
ern zones is also graphically illustrated. The problem of the -ossible
maximum earthquake intensity for a given seismic zone could not yet be re-
solved. Seismologists S.A. Zakharov and V.A. Nechayev are mentioned in the
article. There are 6 figures and 12 Soviet rcferences.
ASSOCIATION: Institut seyamologii AN Tadzh. SSR (Institute of Seismology
of the AS Tadzhikakaya SSR), Institut fiziki Zemli AN SSSR
(Institute o- -Physics of the -7arth of the AS TMSR)
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D228/D304
AUTMRS I Bune# V. I., GaoTakiy, K. V., Zapolfakiy, K. K.,
Keylis-Borok, V. I., Irestnikov, V. It., Vhlinovoka7a,
L. N.V- Versesov, 1. L., P rlova-9-47-r.-, Rautian, T. C.,
Hey3ner, 6-.7-.-,-Xrr-,nI-cRenko, TU. Y., and Khalturin, V. 1.
TITLEs Uathods of the detailed study of seismicity
PERIODICALs Referativnyy zhurnal, Goofizika, no' 10, 1961g 12-139
abstract IOL144 (Tr. In-ta fix. ze~li AN sm, no. 91
19600 327
TEXT* The Tadzhik complex seismologic expedition was organized with
the at= of studying the nature of earthquakes and the condi4ona of their
genesis. The most soismically-aotive zones of the USSR (Garmo an& Stalina-
bad) were chosen an the work areas. The specific conditions of working
and proosdaing the data demaadedL the development of:special systems of ob-
servo,tion and methodip of interpretation. The large amount of recorded
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Mithodn of the detailed... D22a D304"
seismic p Ihonomena permitted the use of atatiztioal methods for studying IJ
their distribution in space and time; thano methodn, in their turn, pr~-
vided the basis for introducing the quantitative indicas of 'he sciamicity
characteris Lien of the soit;mIcally-aotive areas. The actun) noicmic ob-
aervations were closely coordinated rith Caoloz;ic --iona, and thia
mic
pro,.rided the posuibility of exposina the tectonic b.-tqia of the spin
phenomena. A eenoxal review of the rorl: aroa ir. ~,,Ivon in Oli:apter 1, and
concise data an major earthquakes are cited to-et'-Ier with thi General po:;i-
tion of the expedition stritiona. A dencription of the starrl:--rd r-ain and
auxiliary apparatus =od at the otatiowt and also trio layout and dc..-crip-
tion of n(~wly developad equipmant-inrluding an r-ato=atic se-isr-lic otation
-.Tith a ma,-notic memory-is cited In Chapter 2. Oi,~ methods developed and
utilized in the expedition for atud,,ing the crustin structure in the area
under investigation from the record* of nearby oarthquakes are described
in Chapter 3. Horizontal and vertical hodographs were constructed. The
resulting mterial enabled the crust to be represented-an a one-layer,mass
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~~1116V-511000,101010091053
Methods of the detailed-.. D228/Dr-~
with a loncitudinal-wave. velocity of 6,.O.e. 6*1 km/"o. At the 1:ohorovicio
boundary, the velocity suddenly changed Co.6.0 km/scc. an4 then aorowhat
decreases. but at a depth of 300 Im lt.subsequently increases to 9.2
ko/soo. These data underlay the construction of.isochrone charts used to
localize the epicenters and to determine the focal depths. "the isochrons
charts were constructed with an account if the hoteroCencity or the vrork
areals geoloGio structure and thojecultaritj of the scismic stations'
location. This enabled the preoioion of hypooenter localization to be
substantially Increased, reducing It to I - 2 k= at the center of the
work area's topographic map., In Chapter 4. the definition of the concept
of seirmia energy at the focus Is givep,?nd the basic forcalas are de-
rived for its calculation. On the basis of experimentally obtained laws
for the dying out of energy with distance, nomograpbA were constructed
to deteraIns practically the anargr at the focus from the records of nearby
earthquakes. Appraisal of the precision of calculation of the energy In
relatioa to different factors shows that It W be determined accurately
to thd order of its magnitude. Ta thisconnection, the value K a Ig E
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511691611CO3101010r,91053
Xethods of the detailed... D228/D30.4
Is introduced for characterizing the enera class of earthquakes. The
value of K is compared with th6 earthquake magnitude M. The study of
the too-energy I;no3 shown that the different dagroca of the dying out of
seia~io energy aiong and across the strike of geologic structures exort
a decisive influence on the form of the Isoneisms. In Chapter 59 the
frequencies of seismic vibrations arc studied--in relation to the earth-
quake energy, the distance from the source, the Coologic corAitions at
the point of observation and at the hypocenter, ete-from recordines at
both the customary stations and a special 4ACC (ChISS) seismic-atation
intended for frequency analysis of seismic waves directly at their place
of registration. A detailed description is given for the frequency-
selective seismic-station 4ACC- M4 (CU4S-1954) and for the results of
the investigation of its recordings. Cerimin opiconiral zones with an
anomalous frequency are thereby revealed. The procedure for theoretically
calaulating the focal -charsoteria tics, and also for appraising these
latter from ampir'oa'Ld&t*t is given in Chapter 6. Several formulas are
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Uathode of the detaile4*.. D22BID304
cited for detarnining the Site of a focus ln*rolation,to its onorgf on t1te
basis of different physical propositions. The dynamic parameters of the
fool are determined; there appear to be definite predominant directions
for both the strike and dip of the fracture planes. The chiractoriatic3
of the seismic conditions of the Go=* =4 Stalinabad aoinstically-Motive
reGiona--both a3 a whole and in individual arees--are quoted torother with
the variations in the parameters of the conditions In time. The quantita-
tive Mrsesion of the saiamiaity 4uring con3tmat seismic canditiona is
datermirad by the seismic aotivity. The possibility to shown of oonatr4at-
ing graphs of the recurrenco-of earthquakes from short observations of
weak shocks, and methods are given for determining the period required to
obtain the parameters of the aelonia oanditions with a pro-sot precision
In relation to the energy of the records& earthquakes. The Statistical
constancy of the seigato conditions is determined by the So-called waaure
of dispersion of the frequency of earthquakes. A brief,description of the
area's stratigraphy and the history of its geologic development is given
in Chapter S. The structuraLl'achauxes aal descriptions of tha zoat importdat.
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Uothods of the detailed... D226/D304
deep faults are cited. The contemporary structure of the Game area Is
dopioted%3 two main regions# the alpino goosynalinal zone in tho south
r.nd the notivatod opi-Iteroynian platform in the north. In section, it is
drawn as several stops of Paloozoic, baserant adjoinlnC ench other mlong
deep faults. A comparison of the seismicity with the tectonica of the
study areas is made in Chapter 9. The construction of maps of isolines
of seismic activity and aradionts of the rate of tectonic movements is
recoozended for appraising the 00tWootion the seismicity and the
tectonic*. Vothode are cited:for constructing such'map3. 'Ahe con,-;monco
between these casnitudes is established for the regions under investiGa-
tion, and aroaa.with th2 maximun gradient values corres pond to those with
the hienest values of seismic activity. 272 references. fAbstracter's
notes Complete trazolaiion-1
Card 616

BUTOVSWAq Ye.M,; KONIKOV,, A.T.;,IML
IF-401r-TvLw; PAK# V.A.;
TROSTYARSKIX,, G.D.; ULOM07,, V,I,; SOKOrMA,, A,A*., red.;
GCRIKOVAYA,, Z.I.,, teklm.red.
ESelsmism of Uzbekistan] Seismichnost' Uzbekistam. Tashkoxxt,
lad-vo Aked.nauk Uzbekskoi SSR. Vol.l. [The Fergana Vauey]
Zerganskaia dolina. 1961& 97 P. (KERA 15:5)
1. Akademiya nauk Uzbekskay SSR. Institut matematiki.
(Fergana-Seismology)

BAGDASAROVA, A.M.; ISLAMOV, X.Sh.: KORIDALIN, Ye.A.; KUZNETSOV, V.P.;
KUZIMINA, N.V.: NEUILINA, V.S.; NERSEWV, I.L.; SULTANOVAt Z.Z.;
KHARIN, D.A.
Seismicity of the eastern part of the southern spurs of the Greater
Caucasus and some problems of methodology in studying the seismicity
of individual regions. Report No-3. Tzv.AN Azerb.SSR. Ser.geol,
geog.nauk i nefti. no.4:13-24 161. . (MIRA 15:1)
(Caucasus--Seismology)

3161V 1/000/017/001/002
D239 302
AUTHORS: yedvedev, 3,V&l Bune, V,I.t Yvedenskaya, N.A., Gayskqy,
V.N. Kirillova, I.Y., Nersesov-1.L., Rizaichenko,-
Yd-.-V.. Savarenskiy, L.F. a Sorsk-ly, A.A.
TIT12t Instructions for reGional seismoloiJcal au-=aries
SOURCE: Akadezalya nauk 533R. Inatitut fiziki Z_-Mll. Trudy no.
17 (184) uoaaow 1961. Voprosy inzheaernoy seyamologii
no. 5, 128-145
TBXTI These instructions were confirnedby the director of the
Institute of Geophysics All SSSR, M.A. Sadovskiy, on February 27,
1961.. Their objective is clearly to secure a unifora system of
recording all soismoloGical data pertinent to building construc-
tion, obtained in future in the USSR. The instructions are divi-
ded into six parts, containing 64 numbered articles I the follow-
ing being an indication of the scope of each part: 1) General
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Inutruotions for robional ... BA 19A 1/000/017/001/032
Oection. This definen the purpose and ucept, of th~) -mork. The
seismoloGical map of the USSR cstablish~La in j957 is beint, kept
up to date by nontinuing observations. Its scale is 1 1 5 000,000.
The mau is to be uned to raake scis.aoloLical forccauto both for
the epinentral 7one and for the viiiole earth'a surface. 2) Inatru-
mi~ntal data on earthquakes. Thiu to defined a.4 dutd obtainad
now from both fixed and expeditionary stations no opposed to the
study of past earthquakes. Uethods of classification by magnitude,
precision of e3icqntral location and frequency of recurrence
are definl)d, 3 En4gineering seismology, Under this heaOing ia
defined *he format of an atlas of strong eurthquake with isonels-
mala. This should be or, a scale of It 1,000,000. It is also
hoped, to include data on the energy density distribution of the
frequency spectra. 4) Seismcgeolo6ical d.~ta. Since some regulari-
ty is discernible in the distribution of shocks, a "seismotek-
tonic" map should be a possibility. Thin would be particularly
hnlpful In rek;ions where seismological data up to this time are
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lr.qtxu~tlons fVX
E,pa1:sP,. ljrn;.vitational data could alao be uueful here. 5) Prc-~e-
dlirps fcr manng seisaolo6ical sum;a~try mups and their dccum4~v~
-1:ation. are to be of two types, correoponding to i and 7
atove, i.e. acislacloGical mapa and xads of iocseis;aala shcvirzE;
ertergy and attunvation. nhara~,teristLcs of the rej~,ion. The -vay
In which these should be prepared is described in considerable
detail, oL~,thqr wit-h CoMe #Suldance about what is envisaged for
the a,ismotekl~onic~ mapn. 6) Arranvement, duration of and 1)3xti-
-,-,pan-!a ill the fulfilmant of the project. The names and addres-
sea of the participating Inatitutions for each re6loll are
z1,venithe end of the-, first term will be at "he ~nd of 1962.
The wap In oxpeotod from the AIL SSSR (AS USSR) in 063. There
are 60 So,riet-bloa references
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V
31920
B/619/W000/017/002/002
-s,9300 D239/D302
AUTHORSs Nerseso I.L., Rautian, T.G., Khalturin, V.I. and
Riznichenka, Yu.Y.
TI ME a Instructions for dynamic measurements on seismograms
SOURCE-. Akademiya nauk- SSSR. Institut fiziki Zemli. Trudy
no. 17 ('184). Moscow, 1961. Voprosy inzhenernoy
seysmologii no. 5, 146--167
TEXT; The term It dynamic" signifies measurements of amplitude
and period of oscillations, directions of first motion and du-
ration of the trace, as opposed to kinematic measurements of
I.-imes of arrival of phases. The objective is to obtain informa-
tion of the strength and type of movement at the focus. Data
frcm. a long chain of stations are necessary and these data must
be strictly -omparable~ on a uniform basis. It is assumed that
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31920
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Instructions for dynamic ... D239/D302
all such stations are fitted with typecry(,SGK) --~-Ctl< (SVK)
se-48mcgraphs cr others of similarly wide bandwidth. The ir-struc-
tions are based, on-exoerience of near earthquakes Cup tc 700 km)
i_-- Central Asia,' but recomaendations are also given for dealing
with earthquakes outto 100 epicentral distance, where diffrac-
ti.-:)n begins tc affect matters. The instructions are divided ir--
ti -!ight sections as followas 1) Dynaaic quantities determi.-
rable. from seisacgrams. These are 'Lj~k Tj; the amplitude and
period of first arrivals of each phases Amax, Tmax the maximum
amplitude and correspon.ding periods of each phases Am; TM; the
the mear. dit*to,*T the duration of each viave-group. A distinction
is made between relative durection whioh is measured between
points of amplitude one third the maximum, and the absolute du--
ration. which is measured between poir-ts of fixed amplitude. The
latter clearly depends on the energy. 2) measurement of
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Instructions for dynamic ... D239/D302-
amplitude and period of first arrivals details). 31 Separa-
tion of basic wave-groups on the trace Rllustrated by examples).
41 Measurement of maximum am9litudes and the corresponding pe-
riods (details). 5) Measurement of mean amplitudes and mean
periods (details). 61 Determination of total duration of seis-
mic oscillation (definitions). 7) Calculation of seismic energy
ed
density. The formula evolv 12
Al A2
0.085 + :.'L - . .......
T22 2
I
2
2n .'rn erg/cm.2, where the sy,-.jbols are: v = velocity of
T n
given wave-group, Vs.= velocity of 3-waveal A = ground amplitude
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5/619 61/000/017/002/UO2
Instructions for dynamic ... D239rD)1302
in mm, T = period in seconds of first arrivals of phases
... n. a.-nd*r = duration of phases 1,2 . ..... n. This section is
also illustrated by examples and a nomogram for rapid calcula-
u
tion is given. 6) Galculation of 'he seismic nerty at the fo-
cus. This simply involves evaluation of 4'K IL). Another
nomogram is given for this. A third nomogram ca-n be used for
estimating magnitude. All these data should be reported on a
special lorm designed for the purpose and a completed example
is given, There are 13 figures.
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sA69/62/000/011/006/077
D2213/D307
AUTHOR: Koridalin, Ye.A., Masarskly, S.I., Nersesov, I.L.
and Kharin, D.A. ----------------
TITLE: Trial study of weak local eanfthquahes by means of
temporary seismic stations
PERIODICAL: Referativnyy zhurnal, Geofizika, no. 11, 1962, 18-19,
abstract 1IM2 13tudil qi cercetari astron. qi seis-
mol.1 6, no. 2, 1961, 101-172 (summary in Rum.))
TIMT: The seismicity of various districts of the Soviet
Union is being studied by means of the investigation of weak local
earthquakes. Investigations are being conducted in two directions:
seismico-geologic and engineering-seismic. In the first the aim of
~he research is to obtain the general regular relations of the dis-
tribution of weak and strong local earthquake epicenters to the tec-
tonics. The chief plan of the second is the problem of seismic loc-
al and micro-zoning. Work of this. type was begun. in 1927 in connec-
tion with the study of the seismicity of the Turksib Route. Next it
was carried out in the Crimea, where the outline of the epicentral
zone of local shocks was obtained;.in T-arkmeniya, where distribution
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ial study of weak local earthquakes ... D226/D307
patterns of the multiple shocks of the iishkhabad earthquake of 1948
and problems of the seismic microzoning of the city of Ashkhabad
were studied; in West Turkmeniya, with the aim of the detailed seis-
mic zoning of the territory; and in other regiona. The method of
using mobile seismic stations, which was first applied in the Shemak-
hinskaya zone in 1953 and in the wridest volume in the Tadzhik comp-
lex seismologic expedition, was specially practised. Here the ques-
tions of'quantitatively studying the parameters of the seismic re-
gime and the energy of. weak earthquakes are being investigated par-
ticulwly carefully. 'Electromagnetic B3rVIK (VEGIK) acismogrzaphs are
being used in the work, as are methods unrelated to the supposition
that the crust is homogeneous, for determining the position of an
epicenter; the ad-curacy of such determinations thereby reaches
1-2.Icm. The method of mobile stations with their locational profile
As,also being emploed to study the depth structure of the crust.
9 references.
Z7Abstracter's note: Complete tranalation_.7
Card 2/2

KEYLIS-BGROK', Vladimir Inaakovich; NERSESOV I LeonowichL-YAGIDH.
u"
Akiva Kaboyevich; SADOVSM,3~.Apc U. red.; MEDER,, V.Kp'
red. ixd-,m; ITPIrAWTA# Lvp~ tokb*4
[Ket" of Symauatirti. thw scononid - offset of earthquakeproof
ou]Katodika otsenki okonoidchookogo offekta asisno-
stolkogo stmitoP'stw. Moskva: Isd-vo Akad. nauk SSSR, 1962.
45 P. (MIRk 16:3)
1. Chlen-korrespondent Akadenii nauk SWR (for Sadovskly).
(Earthquakes and building)

IWTIVIOT, V.N.; Ovr I.L,
Tectonic pattern of the Pax' and Tien Shan and its relation
to the mwface relief of Mahorovicie. Sov.geol. 5 no* 11:36-69
N 162. (KM 15:12)
1, Institut fiziki Zemli AN SSSR imeni Ojul Shmidta.
(Tien Sban-Geology-Struotural) Usufrs-Geologyj, Struaf#ra4)

NEMSCV,, I.L.; NIKOLAYEV, A.V.
Relation between the dominant frequencies in blasting and the size
of the charge. -Trudy Inst. fiz. Zem. n0.25:95-100 162. (HIRA 15:11)
(Blasting) (Seiszolog7)

KONDRATENK09 A.M.; PA95DY4-1~.~
Some results of a study of a cbange in the velocity of longitudinal
waves and the relation of the velocities of longitudinal and trans-
verse waves in the focal xone. Trudy Inst. fiz. Zem. no.25:130-150
162o (KM 15:11)
(Seismic waves)

IrEFSESOVI I.L.; TCIQ-'IJLIN, M.Kh.
Graphic method for the selection olf frequency-Pumplitude and
phase characteristics of a seismic channel. Trudy Inst.ftz.
Zem. no.32:20-33 164. (MIRA 18:2)

NMESOV, I.L.; RAUTIAIT, T.G.
Kinematics and dynamIcs of seismic waves at distp-n,-es -f ul; t.0
3..500 km from tbg epicentre. Trudy Irst.fiz.Zem. no.3.. :0-31
164, C111RA 18:2)

off-kX1 1uff
ACC NR: AF6O262% Sou-I"'e Couz: U!C/Ujo-t/oofuuij/uu.:~luu.),~lu-,
AUVIM: SavarensLdZ. Ye. F. (Doctor of physicomathematical sciencesh Nersesov.-I. L.;
AL- R. M.; im-A -L. 1k., I
ORG: Institute of R~Vsics of th) Earth, All SSM (Institut Miki Zomli All SSSR)
V~
TIM: Long-period waves of the Aleutian earthquake of 4 February 1965 recorded by
quartz extensometers
SOURCEs All SSSR. Izvostiyao Fizika zomli, no. 5, 1966. 33-42
TOPIC TAGS: earthquake, Rvyloieh wave, internal friction
ABSTiU=: 'Ehis paper*giires an' 'analysis of long-period oscillations from the
earthquake of 4 February 1965 'which occurred in the Aleutian Islands.
The tremor (H - 8.5) was recorded by extensometers at Talgar (Kazakh SSR)
and Dzherino (Tadzhik SSR). It was possible to detect groups of Love
:wav~es from the 2d to 9th order with periods from 70 to 720 see and groups
Of RaYleigh waves.fran the 2d to 13th order with periods of 120-330 sec.
The dispersion curves of the group velocities of these waves were obtained.
The authors determined the amplitudes of the displacements in the R and L
'wavesp the coefficients of decrease of the amplitudes Y and the parameter
Q, characterizing internal friction in the earth* The value Q agrees with
the data obtained by other authors. The values Q, determined fr= love.,
'waves, vary from 60 to 120 %ften T - 300-500; the values Q for Rayleiah,
'wa,~ea vary ~n.the range 150-200 when T = 200. Orig -art* has: 7 figures.
7 formulas. a* - S: 36,5~2-
and 3 table Lk%
50 C~~E 1 0% SMI DM: 03AU65 / OM W-F: fo cm
.----A

ACC NRA AMIN33 SOURCE COD41
UR/0425/66/009/012/0020/0023
Amu Katoic, Ai-'i;g Gaxkfy, V. N-; Mors= Hirsayevo K. M.
ORGt btatitute of Satanic Resistant Canstru~.tlon and Seismology* AN
TsdshSSR OnStitut X075100071090 str0ItGI9stVM, I sirlsoologil AN TadshSSR)
i121,91 Analysis Of fluctuations Of the seismic to In*
SOUMs AN U&bSSR. bakladyo v- go he- 12o 1966o 26-23
TOPIC TAM 641"Ologre earthquake
SM CODES 08
ABSTRACTS The accuracy and reliability of determining the mean long-term
frequency of earthquakes Is dependent on the value and character of
variations; of the seismic regine at the tirie of observationse The
available approach Is Inadequate and t%,* authors therafore have developed a
method for defining the charactiRristics of temporal variations of the seismic
regine which makes it possible to estimate the accuracy of determination
of tim long-tom frequency of earthquakes of different energy classes and
detect the pertods of systmatic changes In the course of the process. Data
accumulated id recent years Indicates a sore complex depeadence between R
(the measure of *dispersioa of the frequer4y of 'earthquakes) and the
gWeylies of the selanto pcooses -than believed to exist earlier, contrary to

I - - - .. - -
. ACC INts AP?013733

L 38523-66
ACC Nits
AUTHORi Alekseyevj, A. So; Mersenr.-A&IL.
ORG: Computer Center, Siberian Department, AN SSSR, Novosibirsk (Vychialiteltnyy
tsentr'3161-r-aVogo otd. AN W5K); Institute or Ueophysics, AN SSSR, Moscow (Institut
Fiziki Zemli AN SSSR)
TI779: Travel tims and amplitudes of waves in Central Asia - theory and
experiments 6-
SOURCE: Studia geophysics et geodaetica, v. 10, no. 2" 1966, 172-176
70PIC TAGSt seismic wave.)0/shock wave analysis
ABSTRACT: The article presents a new interpretation of the results of observations
of body wavesp obtained In-deep seismic sounding and In observations of earthquakes
Central Asia* Origo art. has: 4 figures. (Orig. art. in Eng.] (JMS9 36o8441
SUB CODEt 08 / SUBM DATE: 28Aug65 / SOV REF: 005
S()URCE CODE:
card

IAUZ=GVO S. K., and NEnSESOV, L. G.
('Technological Diagrams of Contemporary Processes in the Working (Processing)
of Petroleum.," Moscowv 1950
xxx

FIDMV. V.6.; ELYABCHIKDT, T.R.; FOLTAKOT, I.S.; SMKIN, U.I.; RTABYKH, P.M.;
NOVIK, R.G.; SWUM, ?.Jr.; MASHOVSKIT, K.H.; IAL&IMMY, S.K.;
AMWIYZT. A.?.; YSTSTAFOYZV. V.V.; ZVJM. A..P.; ERMSOT, L.G.;
GROSSNAN, Z.11.; HIRM, A.0.
Fetr Alakaandrovich Smirnov, 1902-1958; obituary. Kkim. i takh. topl.
1, masel. 3 no.12:68 D 158. (MIRA 11: 12)
(Smirnov, Petr Aleksandrovich, 1902-1958)

MOMOV, P.V.
Designimg~stael rods for the joint action of flexure and
axial coWession. Trudy GPI (Gras-] n0-5:81-89 '62.
ODA 15;12)
(Stealt Structural)
(SlAstic rods and wires)

EATONGHKOVSXIY. P.A.. professor. radaktor; RIMISOVAr N.A., kandtda-t-
IstorichaskM aaak, redaktor; SIK0d7TI.P.'W.M%"aMt pedagogiche-
skikh naylk. reda Kor; TIRXKE[OTA, D.Y., takhatcheskly redalctor
[Dissertations for doctoral and candidate degrees defended at
Koscow State University from 1934 to 1954; a bibliography]
Doktorskie i kmadidatekle dessertatsti xashchishchannyo v Moskov-
skoa gosudarstvannom univeraLtate a 1934 po 1954 g.: bibliagrafi,
cheskil, ukazatelf. Pod red. P.A.ZaLonchkovskogo, I.A.Keressovot,
1L.R.Simana. CI(oskva] Mo.l. [Departments: Kschanics and mathematics,
physics, chemistry] IFakulftety.- Makhanilco-aatematichookit..Ifiziche-
skit, Ihimichesicit. 1956. 254 p. (MM 9:8)
1, Moscow. Universitst. Nauchnsys, bibliotaka iment A.M.Gorlkogo.
(Bibliograpby-Science)

~J
7-AYOUGMTSKIr, ?.A., prof,, red,; imad.ist.nauk. red.;
LT *K
SIMON, X.R.. kaud.ped.nauk, V..-ft AKOT. H.S., tekha.red,
[Doctoral and candidate dissertations accepted at Moscow University
from 1934 to 1954; bibliographical listj Doktorskis i Twadidatskis
diseartataii zashchishchannyo v Koskovskom goaudaretvennom universt-
tote a 1934 po 1954 g.; biblicgrafichaskii ukazatelf. Pod red. ?.A.
Zaionchkovok6go i dr.. Koskva. Pt.2. [Yaculties: Geology, Geograpby,
Biology-soll,scleu~*] Fakulltety: Geologicheekli, Geogrefichaskii,
Biologo-!pochvem7i, 1057. 217 p. (MMA 11:3)
1. Hsocow. Univerattat. Biblioteka.
(Bibliogrepby-Geology) (Bibliograpby--Geography)
(Bibliography-Biology)

PATEMUNg A. (Baku); MMMOVAp H. (Baku)
Formation of production funds on coUective farms. TOP. ekon.
no.12:142-V44, D 161. (CoUective farms) I (KM 24: 12)

IWMESOVAj, Z. L.
uTemperature Variation of Ground Iciness," Dak Ak Nauk SSSR, Vol 75, No 6.,
u
.p 845, 846, Dee 1950.
Inste of Permafrost im, Ve A. Obruchev, AS USSR
U- 1528j, 10 Oct 51

IlefisESIOW,J3,
!:Mll- L fic~ ~ 4 -,
Nrrac*,,v4. e'.A. (II.A. I$$,, ,, J,W Ill.ill,le 4,1 14t*frlg, 1 AJI.Iss, U.S.S.R. ACAdClIly "I 51tellk CO,
46v- ,iiii0lorAt tho jJ1,1410 Ott 1.4 6,% 0"(:. sol-d
AkA40alls Muk S.S.S.R.,p rook'AAdy Voi, ~q N,, j 11 1 -r,

- HER SOTA, Z.A.
--- -Qi~
Phase states of water in ground freezing and thawing. Hat.po
labAsel.meml.grunt.107-51 '53. (KLRA 7:2)
(Frozen ground) Ofater)

e A.
z
"cniorlinetric Method of Determination uf the iciriess o.
Sb. po -,-erzlyx.- ..;run
0-C~p 1900
A2 a result, of' the. como.-xi.~,-,ri or tho ci~)ta :roin dilr;to,-.q,-Ar`c ani calori-
metric methuds -)f Investii,,Alori LLe !~ut,or recu,ruien~i,, as -iiuc-t rell-
able the vilorimetric irietiod ior trie, Irv-,resti:;-,it,'.on of froven -,rounds.
He r-conmends also th-,-, c~~iorlme,ric raetaod for L-e deter Alri,~tloici o: lee.
(RZhGeol, lio 6, 19541)
SO: Sum. 4J2, 12 55

112MOVA.Z.A.. starshly nauchW notradnik
Directions for determining the quantity of unfrozen water and ice
in frozen ground. Nstpo labAsel.nersl.grunt. no.2:55-57 '54.
(KMA 8: 8)
1. fSentrallWa, laboratorlya Instituta rierslotovedenin Akadesli
nwlk SSSR.
(rrozen ground)

HEMSOVA,Z.A.. starshfy nauchay sotrillalk
- - Wstea4:
Direct-Lone for determining the heat capacity of frozen ground.
ffat.po lab.lssl.merzl.grunt. no.2:100-110 '54. (MM 6:8)
1. TGentrallmWe laboratorlya Institute, serslotovedenlya Aka-
demli nauk SSSR.
(Yrozen ground)

r u..'j",kandidat geologo-mineralogichaskikh nauk, otvatetvanayy
r
,.- - radartop
(Basic concepts and terms in gookryalogy (the science of
frozen:cround).] Osnovnys P'onlatils, I termirq gookriologil
(acrslotovedealla). Moskwa. 1956. 15 p. (MM 10:5)
1. Akadenlya nauk SS4R. Institut marzlotovedeqlya.
(Prozen ground-Torminologr)

IN L
TSMVIGH, N.A It TA, S.A.; BOZMKOVA, A.P.; IfATTUNOT. I.A.; DOMMOT,
B.11,; ;b~l r-Y~X--,--BAMIN, F.G.; SATUOUT : B.A.; ZHMOV. V.I.;
WMNOT. G.A.; VTA1OV, S.S.; ITA, Ye.P.
Physical phenousna and processes In freezing, frozen, and thawl1w
sol.Elal general coments. gat. po 100 isel. maxxl. grunt. no-W-
114, 157. (MM lot1l)
(7-rozen ground)

/Y,F, A6 E'S j /// 1, / /.
=ff= A
. XOOA.Ijj*, ,
M&W ~n the active surfe i of soils at temperatures below and
above freezing point. vat, * lab. isal. mercl. grunt. no.3.-163-
167 157. (min 10:11)
Mom ground) (Cations)

N ~- (2, S ~- 5 o IV' A- -k-
MOWMTA* S.A.
Iffeat of exchavgeable cations on water phase composition in frozen
soils. Ikt, po lab, Isal. mrzl. grunt. no.3:i6&176 157~
(Prozen ground) (Cations) (Soil moisture) (KIU lOrll)
6

NERSESOVA
Effelof exchange
heaviptg of ground
grun.~ no.4-22-52
1
cations on the migration of water and the
during freezing. Issl.po fiz. i mekh. merzl.
161. (MIRA 14:12)
(Frozen ground)

MT(SESOVA., Zinaida Aleksandrovna, TYSTOVICH, flikolay Aleksandrovich
"Concerning unfrown water in frozen 6oilso
report to be submitted for the Intl. Conference on Permafrost, Purdue Univ.,
Lafayette, Indiana, 11-15 Hav 63

TYUTTU , Ivan kleksayevich, doktor geol.-miner. aauk; KERMWVA,
STOLYAROV, A.G. . red
Zinc
RTLIVAp Tu.V., takhn. red.
(The nature of the movement of vater in soils during freez-
ing, and the bases of,physical and chemical methods of
controlling heave, Priroda migratsil vody v gruntakh pri
promerzanii I oanovy fiaiko-khimichookikh priemov bor'by a
puchenism. Moskyag Izd-vo AN SSSR, 1963. 157 p.
(KIRA 16:10)
(Frozen ground)

PIMOVSKIT. B. T.; A.A.; RYBKIN, I.N. (Noskva)
Bilateral ligation of the internal mmary artery In stanocardia;
preliminary report. Klin.med. 37 no.11:52-55 IF 159. (MM 1-3:3)
1. Is gospitaltnoy khtrurgicheakoy kliniki (direktor - deystvitell-
nyy chlen AM SSSR prof. 3.T. Petrovskiy) 1. propedavtichaskoy terapev-
ticheskoy kliniki (direktor - deystvitelivy chlen AMU SSSR prof.
V.Kh. Tasileako) I Noskovskogo ordena Lentua maditsinskogo instituta
iment Sachenova.
(ANGINA PICTORIS surgery)
(THMM blood supply)

._, HMM,~q A.A
,:----, nL==-,
lUrgical treatment of chronic coronary insufficiency by blUtijea
ligation of the interwl mmmary arterypurvey of foreign litiMime.
Ehlrurgila 36 no.3t225-IZ Mr, f6O. (MMA 1342)
(WRONART HVM DISMIC) (BPJWT-BLOOD SUPPLY)

MSESM A A - R=IN,, I.N. (Mbakval
rnmediate and late results of bilateral ligation of the Internal
thoracic artery in stenocardias Klinomed* no.lt44--~48 t62.
(KMA 15:1)
1. Iz goopitaltnoy khirurgicheekoy kliniki (dir. - daystvitellnyy
chlen AM SWR prof. B.T. Petrovskiy) i propedevticheskoy terapev-
ticheskoy kliniki (dir. - daystvitelln7y eblen AMN SSSR prof. V.Kh.
Tesilenko) Y Nookovokogo ordena lenizin meditainskogo insiftuta
Imeni T.H. Sechenova,
(ANGINA PEGTORIS) (THORACIC ARTERY)

16(1)
AUTHORSt Dzhrbashyan, 31.M. and Yersesyan, A.B. S07/22-1---j5-71/9
TITLEs Criteria for the Possibility of Expanding Functions into
Dirichlet Series (Kriterii razlozhimosti funktsiy v ryady
Dirikhle)
PERIODICALs Izvestiya Akademij nauk Arqra4i~-Irmy SSH, SerkW,
maticheskikh nwi k;p 1958.0 Vol 11, ITr 51 PP 65 - 106 (USSR)
ABSTRACT: Let F(6) be defined and continuous on (6',+ 00), a,-.> 0
Then let 0
d-,CF
a (e e-u) e"uF(u) du
d e r (41) (e
Lot the sequence satisfy the conditiont /U0 ~ 0,
0 , 1
(Pk) d845 f I.
The function L F( 6~) is called continuous on ( 670,+06) if
1) it iZ c3ntinuous on (i~`o,+
r~ kj and 2) there exists the limit
(IV
value L F(+0o 1i% L F( G'). Let F( 115) e L( rn;
(Plc)
if on ( 60 +003there exist all functions L F( 67 ) end a
continuous and If on ( 616+00) the functions e6 d L
QkW
are continuous and absolutely integrable, where 61 >G'0 is
arbitrary.
Theoramt If F( 6')6 L( then for every n.)P-0 and 6C.( Go
there holds the formula
Card 2/3

On the Application of Some Integro-Differential Operators SOV/20-121-2-4/53
n L Qk-) F(+oo ) -& G' +00 fn+1_1 u (N+1)
Z r(l+;%k) o + r f (e- Gle-u e- L F(u) du.
k-o 6
Two further theorems contain conditions for the developability in
the Dirichlet series if the function belongs to certain subclasses
of LQAn; 60). Further results are combined with the introduction
of certain generalized differential operators and with the use of
Weylls integral of the ordert)(.
There is I Soviet reference.
ASSOCIATION:Inatitut matematiki i mekhaniki Akademii nauk Arm.SSR (Institute
for Mathematics and Mechanics of the Academy of Sciences of the
Armenian SSR)
SUBMITTEDs April 21, 1958
Card 3/3

S/022/59/012/05/02/009
AUTHORSt -Dzhrbashyan# N.M., A.B.
Tome, \\O
TITLE% On the Construction of Some Special. Biorthogonal Systems
PERIODICALs Izvestiya Akademii nauk Armyanskoy SSR. Seriya fiziko- mate-
maticheskikh nauk, 1959, Vol.12, No. 5, PP. 17-42
TEXTt Let y(xok) and z(x, ~.) be entire functions in A which belong
to the class L (0,1) together with their derivatives with respect to
for every fixed with respect to x. Furthermore let all functions
I
z(x, A411 (r,s = 0,112....
) X*8
belong to L1(0,1), where A Ai~ are arbitrarily fixed. Furthermore let
-U(N ) be an entire function and
(1.2) Y(X, Z(X, A e)dx (AA
A - A k.
for all Let the function a A0 possess denumerably many zeros
Card 1/3

On the Construction of Some Special S/022/59/012/05/02/009
Biorthogonal Systems
~i $ 0 '4 1 ~ 11 '.,
k.o r(A4.+k,3-
It is stated that the expansione in terms of these functions converge
-.simultaneously with the ordinary Fourier series. On a finite interval the
authors formul4te conjugated boundary value problems for differential
equations of fractional order-S
,,i), the adjoined and eigenfunctions of
which for special parameter values agree with the considered biorthogonal
Card 1/2

86820
5/020/60/135/005[005/043
C111/C222
AUTHOR-.
TITLE: Expansion in Eigenfunctions of Some Non-Selfadjoint Boundary
Value Problems
PERIODICAL: Doklady Akademii nauk SSSR, 1960, Vol-135, No-5, PP-1050-1053
TEXT: Let a(x), b(x) be complex-valued functions of bounded variation on
Ox let K(z,t)E-E-0).
Lot
(18) 4A 0 ~ 0.
In this case all oigenvalues of (A) and (A*) lie in the strip
Card 619

86820
3/020/60/135/005/005/043
0111/C222
Expansion ja Sigenfunctions of Sons Son-Selfadjoint Boundary Value Problems
- Re X'r - . Let
6
1 T2 (6 1< log I'Lo 1/1 OW'.-e- erd
a(x) - al(z)+a2(X)+a3(x),
(19) b(x) - bl(x)+b 2(x)+b 3(x),
where Yx), b,(z) are absolutely continuous; a,(x), b 2(x) are jump
functions; a 3(X)P Yz) are singular functions. Let
1 1
(20) A - V(a2+a ), B - V(b +b
0 3 a 2 3
Theorem 1: Let
(21) jPjA+jwjB+AB