SCIENTIFIC ABSTRACT FR:GZYRYAN, M.S. TO:GZOVSKIY, M.V.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R000617800052-6
• Release Decision: RIF
• Original Classification: U
• Document Page Count: 99
• Document Creation Date: November 2, 2016
• Sequence Number: 52
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTR

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AP`I'YUSIi>+;NitO, Z.T. ; YASIL'Y3~;V, I.V. ; G~7AA~�5..;..._GOLOVACH, A.d. ; GRUBOY,
V,I.;LAMY`~~Ti1IN, ~e.N.; PIDO~mI, O.A.; PIGIP~NKb, F.S.; POLS~IX:O,
O.M., kand�biolo~.~eauk; RODIOI~FNKO, G.I.; RUSAI~V, F.N.; SAAKOY,
S,G,; SOKOi'AV, S,Ya., prof., doktcr biolo~;.aauk, red.; FFDUROY,
A1,A,; 5E{Il?C1{INSKIX, N,V, ~dACeaged.~; SH[JL'GINA, Y,V.; SHUKHOTj~ODSKIX,
B,A,; GOI,O1lNIN, M�I,, red. izd--va.; KRUCrI~IKUYA, N.A., tekhn.rAd..
Trees and. ahrubq cf the U,S.S.R,; wild, cultivated, and promi.si~
exotic tr~-~~s and shruhe~ DerAV'ia i. kl~etr~rmiki SSSR; dikcrastctehchie,
lnal.'tiviru~gmve i pereppktivnyc! d1iP~ introdukteii. t~ookra. [Yo1.4.
An~inapgreus : I~e~~minoeae - Funicacc~aA] Fokr~tot3emenr>f�: Sr,mPit~ttva
bnh~vvA-~TltinAtnvy-~. 195A. 97~ p. (1dIR.A 11:J.?)
1. AN SSSf(� Botanf cheekiy institut�
(An~rioeperma) (Trees) (Shrubs )
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APPROVED FOR RELEASE. 06/23/11 CIA-RDP86-005138000617800052-6

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APPROVED FOR RELEASE. 06/23/11 CIA-RDP86-005138000617800052-6

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APPROVED FOR RELEASE. 06/23/11 CIA-RDP86-005138000617800052-6

APPROVED FOR RELEASE. 06/23/11 CIA-RDP86-005138000617800052-6

APPROVED FOR RELEASE. 06/23/11 CIA-RDP86-005138000617800052-6

APPROVED FOR RELEASE. 06/23/11 CIA-RDP86-005138000617800052-6

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A~ ntethod for measuring the mobility of ions in dielectric ' ~ ~. -
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scrHxd for measuring mobility of current carrirrs in dielec.
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denser In series with the cell, and from this, the time for Iona
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thu valtagt across the cell, and d the distance bctwCen the ~
r tlectrotles. For hexane, the meaxnrccl mobilities are: ~
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cf ~,r~o~hvsics o�~ the AS ~, ,~U~;; c;e ,c;heinat-
plast~v~;~ros~meter and a dynam�~,:~eri.c t,tatEsrialre5sure, was ~i1e ~~an~er.tial :i ~I'r:SS i2:t,~al:~i.ty ~ %ilc',
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1?tay~~i ;~ ~ Ltac~3;"y cif.' ~ ., �
1~,'~'ft;ty ;01

t)�00? ~~~f the ,hear modulus of. rocks� Hence elast,lc elcng~~.jti.on
:end elaptlc s.2ears in r.oc:ks are always 1e.s tr:,_in i;~ and jo re:~pe~ ,~,,.~-
ti~vel.,y4 The author proposes a con~ple}: physi�a1 theory for tectcn~-~
fray�tu::'e fox�mation, which contains 6 basic princ:iples~ ~) Iza eacri
material. two types o.f rupture -PW tearing and shearing ~~ � crud their.
two c~~rrespondin@; strengths are ~~oss~.bleo In each speczf:~c, c~~se
x�upture is deterrr~ined by the character of the str~iin state and by
thA oorrelation between the material�s ten3le and shearing
strengthso 21 The tenacity values do not remain ronstan.t but change
in relation to the duration of the action, the manifold compro~~iorA
anal the temperatureo This p.ri.nciple is corroborated by numerous px-
per:~ffienias and the:aretical researcha ;~) The stren~;tha of rocks may
~{,rzTy widely de~aending on their 1.:itho~lo~;~{.~ ~irrd petrogrc;pha.c� pec~ulza
t�..tl~~~r~ 4~ t~tien ~~tudying the laroce:~s of 1'r~:~rtGur�e 2'vr�rnut;ioia a.t i~>
rae~~e7sc~~�y too taker into r~.c:courat the inf:luc~nc::~: 4,f ttlc se~1 fe~mer'~~1t~i
rupture surfaces on the strained state o.t' thei.r .~urra~.znding cirer;~~~
In Some casea.5 a weakening oi' thy; str. esae:~ occurti .~ but lr} othF~rs
they cir+~ stren~;~i~hened� 5 ~ The p.roces:?e ~.~I r,~~~k ru~~ture drv~:~1o1
~, ~r~~~� f~ :iong ~acaz�1ot~ nf' timt, 1~~regu~far�ly; i,~~~,('~~lt'r ;:~; t -, }~~~;~~~t it� ~i~lc7

~`-1~'(~ ~/ ~
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'}~i`(~~,}? 1}ly".; i..a 1 t~tt'~:l~y t:, f' tr'.: ti~rtl .: I't� t t;;','t ', ,~`~:.~; i ~~t.
PL~tIUllICE>
~~ eferatitn~lyy Ltlurrlals Ucof_i,~~_~k%I, ri~~ ~';~`:~;~. "0, ~ ,
Ii
. .
itiJ.~tl'~t:., f: 2.A68 (V sb., Yrab1 0 �t;iit~tiC!f-~.'l i',_:. 1'i., , Go~g;'_..
t ek>'1i ~~~d.t `~:}lE' .~t.r~ltin e:11i1t:>,t.iii trlc~:; ;~ ~;t.�lt_t ttry~~'~;_ /
r1.- k:~~si~ ~r, the geollletLic ~ticnsideraticrl cf ~~.ri~; }lum:)genecus def~~~
m~;~ Sono T?1e s~tr-~lin ellipscid calm t}lercfcl~e,; re ust~'d to descr~br '~
:mp ~e tF_ 'rlc~m
' a~;eneaus dFforln~l t:1on ~ :l_t ~ (~t.~';e.1t}pmE?nt- and &
. ~;,~-~a._ ~c ~~i ~~a-:r: ~_ ~~,~.~~ ~.~. ~ ,a .. ~ :.'~.�f. ;_~z �,t' s~�;.sm1:3.ty a.nd the ge~llog~.cal
~t~ir~ `.;;,~ t: '~::ki +_, 5t r i.!~ ~ t}. ~- ,~ , ,,;.~~ x�'~~.~ ?.,,__ F{~r~w~~rd ma.*at ~~~~-s Academic:j.an.
(~ ~ A ~ ~a~a a.t~ r �~~~ ~ de ~Ya>.~~c~' 4Jpl : 1.a i~ t ~e~ .~ �~lI'1(~.a+alozls for this work when
he wa.~ d~'~e::;'__ ~ '~,�= ~'~;,~~� 1~1~ .~ad~.~%~.d~aa:1 chapters of t�hF bank Were
wr:~t,}e.~ byy , 7�tr.:~~.;t,Y `,. ;, ~7c1 ;.:yap�.N/x-~~Iy._ Z., L,N7ar~q~s.a~vi' and Yu_ V Riz/n+i~-
,'.'~F�~i.~.i~ ~., ~'sapt;.eC c,', "- ' i`. ;``~'.~'~,ny�'1'.,t'y 141a~f 4.~~~ ~} ..~ .l 1:~., ,l ~i ~.i;; F,~;i ~.'v ~i~l~ T. lr�
~t�illl el~ ("'tl=~~?'t~~ ,, .. `l' .� fi~;,lt 1.~i;i1, C(?~:1~?~t~t' _. ._ K,. :K ~1,~~~~.1`'sltiy rlnd
~, i ~, ~.~~,+~:.1.'1ll~'~il, + ~lFl~..' ~' - v 1. '~".,1 �'-~ii "~~ if ~J~ I.: ~ ~'iti..a.~71JV84(f.tyt~,
~.~ Pa~~~.'_-~~rtia aru~. t' I. K`~la.~kuP�:~n� l:?~a}~,ter '~ ~- V., ~. i�~?,~ie~ I. L: lVersQsav
,ara Yu '^~ R~~~ni+..h~~ali~,'~., i ~ie.E;�, ~f ~? ,-_ 1`t ~'~ G,.ovsk~.~r; V.. 1.J. Krestni.kc:v,
,nn.c~, G %, i(e~.J,1~;. t,17tt~:,r{ '~ -' V i~ kstz_-~e~A4�.._..a.._ -,zovsk:~ and I~ L, Neise-
s,.~=~ 'thy: are ,.~~ :~+:.=h�:F1_.-.. ~ 1~5 ``~;~eta..,,~~ Ea:~g;lis~~� a:td 1k ~erman~

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sPy~m~~l~^g~i~ .A:N' '1'~~~~~hiksk~y ~>5It ~Tnst.itute ~~f Seismology o.f the AS Ts3~hik
SSft? dux~~g the 1:.~ri~~ 1~7~;,;..ira5ry Amon, the t,opi~s discuss�d are:. s�ismic
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;>us:i..~:z v~' a.i'or~, niel~;c~1 ..uc'L eat~F, 1.
u.~:, ~ ~ ~ on ci.eTis:i.ty one.
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APPROVED FOR RELEASE: 06/23/'1'1: CIA-RDP86-005'1380006'17800052-6
Conforc~nce on tech}n~~4?ily~ic:~.

~, F., c, ~, t t i, ~~ c~; r i. c)d ;~ ,
1,t~~; ,Xr
folds ,~r~(~. fracturcy. v~~r~zt-lt .t, ~ .
,, t~F~t~ a its ;,ou
a.n the e~;,azc~,ple of the z'i~ll,c;~~ of ;.~
Kazakhstftaa.
fey la.s-Barok ~ ~Ils~+.L but 11 of Y~IY ~ia~' f o~r diet exn z, nine
V. I� ~ ~T ~ cievc.lol.c
descri.beii fi;he metplc-cl whi~~h Y1':. ~~l~a ~~rlich
the elements of 1oc;�~'rion^o~' t~t'~i~%d~ ~ea~ t~lie~~.ia ECt:iOYl of
brink ab~aut earthgtz~lces Und eluc Mlle -~,osolution
d~.sp~.f~c�.uiQa1~ of ttl~air. e:~t,x'`~la. theJ~~~~:i>Cl,.i.vo .:-l,ll~i.y c~1.' talc.
emphac~ized file 1lll~u.L ~~-~t1(,~
the Earth.' S C1"uSt wii,tiirt il~lciiviu.u:1 l,.~x,~f,
clefor~.natian of ~;;1~e C~Godyne.mics Sec~ti.on of ~ttic;
re~ians cE~rried out by ,, ~1 tramUe~~ of ~~~,per. s
Institute of Physics of the Lal til,
~- ~, tq rne'tho~l.s ant tgs~:' o-~ det~:ileu :~rivesti~;Gt;ior~.
We1''C c~eV'4 re
of tectc)n:i.c fractures. ~� ~~)~,iies~.~~
y, G~,a,vskiy proved the inco~lsis~en~~aoio~i~l:,al,for.
1VI. u:~ ~~a by l~
of G. BE;c:ker which is w:iclel.y
k10 X'e00I11t;1GS1C?OC! t1SE i)i
intez~preting the fractu:re t~;ctonic,s;
~ 1 x of wadez'n c;onc;evtions on thy: strel~~;til ox
a cox p e est~~Ulish i~hc b~~aic
r~~:te~~ia~ls which ~~oulci permit to re-
t gg of the tectonic stress field actin, ~:ariri~ the
feat ~r
-time of formation of tl;.e cruclcs� T.l~titute of Geology of
P. Kushn~. T. l,u:t~.n, ~ nip S~ai{)
arev a.nd :G. ' r r
Ci81"CI 13~~�~ I' .[.I1~t~Lltt l~('~?~.~'~~-1 i,if.:'~ 1;.~ 1'~~ r.,ililGlll~
0~.'e Depasita ~
___,, , ial.L ~~.l.t.~v11 ~~tese~rcil l.,i:; ~i~ute of -c tie
Vold Geol~~~;ico1 Yrospcctirt~, Institute (Vse.;~~~u~,nyy Tiuuc_-Zno--
Ca:rd ~.1E/1.8 .Cssledcv~~i~el.' .,l::iy Geolo~;;~~ ~ is I ~.~ _i.~ ~ - j
_i1~,;.,v~ tiort y,Y I ~ltL ~o).(,t~.~
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~~9-~t-J.3/1~F
Conference on tectvziol:~hys:ic~,. (Cvrlt,. )
ThE~ m.e~chani~3rn of f~~rraf.~ t~.c~z1 o:f lr,r~;;e s Lr. uc i~ur~ ~! eleu;~;nts
of they Earth' ~ cri~.st~ w,~~ c:l.c~~r:1.1; ~~v~i.l,}~. ley t,}zc; foll.a~vi.n~,;;
Guthors:
V, V. Bel.ousov (InstitutE: of Physics o~' Lire 'z;arth) raentior~ec
the v~~rie.ty of .reasons of .fo].ci forll,~ rc~ji.,esau:i'rl~uc 1c~s~ity
that ~.rz e~aczi conc~~ete c4.,_~c. tl:ic lvct
};~ lie c~~r~,~i~~.E~.rc~cl fold
pizenomenan should ire ~.rive~s 1.~,u tc`i .
f ormat;iorl as a reactiuu of l,zyorvc:~ `'~~:~und el~l.ri:li, blocs
d~-ffez~ent;~.al verticG~l movE,:a,.llts of ~, ~
of ti1E; EF~rt:h' S crust .
~,, D. Azllg~.rey, Moscov~~ S~i;a to Univers:i_ ty (r~}os~:.ovs~.i~~r
Gos,~d~zrsl;vE:nnyy Uni.versitet) drew attention ~t;o ~che neces5i..t;,~
of us~.zi ' e~:tensive].y geological methods for detriled stud~~~
of thE: glong term history of for~~ij~ 1~ioi1 of concrete
struc~.ur~al elements ol: tLie L~~-�~tl`z ~ crust.
~. T1. Kr~opotkina, Institute v:t Geolo~,icel acierl.ces (Ins~l:L~'juc
~. ~ a It ~.vith cuL~pression az~d
GeoloE,ic:~eskikh Nauk ATE aSSR) aou
stretc~hin~; in the Earth's, crust and loos: ibil~~l;ies of stud,~-
ing these phenomena.
N, I. N~.kolayev, I~Ioscow Gevlo~ical-Pros~?ectin~ Tzisti ~,ute
(irlosk~avskiy Geologa-R;.sv"edochnyy Insti~tut) cozi.~idored tz.e
CI~-rd 12~1~ ~t1ze mcct,.~.ilisr~ of 1'uz:~~~r tion of t'aose
methods of studying
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C onf er E:nc; e an t e c t onopi~ys i c s. (C ont .) 49-7-13/1~~
The fo].lc~win:g physicists dealt with tale prabl~;r:: of r~odellir
i;he tectonic phenomena: 1~. T~~:� I~actiG.riov, Ye. I. T~a.el.'sr~teyr~,
G. V. Vinogrndov, G. N. I~iurznetaov, ~~. F. Volaravich,
A. V. ;itE;panov and also the p;eolo~,ists F. I. Vol'fson,
V . A. ~lprodov, N. I. Borod~lyevsl~iy, Yu. S. Shiktiin. It wa s
mentionec, that the fund~itlent~.~1 cliff:icul-ties in developing;
modella.n~; techniques ank definin" more accurately the
condit:~ons of analogy are duE: to ~~lie ins deyuate :nowled~;e
of t~~e pY:~ysical zrlc]. i,iecl~anic~.]. ~propert=i~;s ~~r roc~-~s Utlci f;h~ t
much a7~telntion should be paid iri the near f'u(,urc:~ to
improv:~ n@; the theory anu. rnetl~~ods of t~~ouellici~. '.~~he;
~eolot:i.st;s mentioned that; f'rara ~;he ~?r~:c~ic~~l_ t?oint of vie4~
the experiments with iivn--uz~i:f'o.ru: tnouels of scctionti, of tYzE~
orE fields are o;[' ~reate:ct irit~:rFSt;. In tic resolution
of the conference it was ment,ionea tiiGt it; is passible in
principle to simulate on models tectunic pzie~.zo:;~ezla and th~~~t
~~ 1Z/.i8 the ~~ro.rk carried out in this field by ~Ltle Geodynam~ics
Section of tine Institute of Physics of ~iie E~~rc1i is
promis ink;.
(T~u~te: Up to this point t.tlis is a calrln]_ete t:rlt~ti;~.~,tian
except for the initial i.ntruductor~~ 1~~:~~~~lt off.
viscosity of t1.1c uiateri;:~l.
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~n~r ~f rl~/~T
Unferer:cE; orl -tect;vno~iiysics. (Coll~� }
c, e ,u,~it;iol:~.s curr~.st~~~lu.~ :.o,~t, closel.;j tc;
-~
U~ilis~~~l;ion of t~l sE; .
lll_Lt5 Uf .l. ~~ ,(',:~~1;(~:C.' ~ .Li1VC::~u:Lz,,.~t;1Url., u~ r.'OCI;:.-;, ti~
the re~ ~, u- .,
:result of s}oecial irives~:i~a~l;:iol~..> '~1 ;!~.._~r~, ~~_~ ne~v 1.1.~:,1~~!"titiEnta
it ~vae found tYra-t ~~ n~t~riber o:e ;r~~:: ~~.~1: i.~ls possess ~th(~ ~~~~,; sica-
+!lE;cll~{lra.cl~l l~t'Gpez`I:,ic;~ tvlziE:h ,::~huirl~.l l':C~.;~I~ vr> i,~u; i~f,c~>~~ of
zinc to �t?r1C~..1.~~1Ot1::3 :i.il dill; AtOC:tC'Z.A~. '.i.'~.lU.:l ~ 1 ~~ '..'~.{:~ "'l`vVc'i~ t~l~'t
t'`~ '^ ~ 1:L c~Uiicei.vc.:~lc iJUt ~~laa Ur.'^ctic~ally
i~t is ~ZOt only tn~v:ck~t,ic~~~ y A
possible to simul~ t~e an ::EO1els -tE,ctor~ic t~llcnoluen~.
~rlastically ae.formi.n~, ;no~~e1 fx'om ~. c;;.~ce:ntr~:~ed solu~,:i.on of
l~En�' l 41c o~ln l ~;~:~ a,- l.;u.(is t;x'~+tt,ci i.l:l v1l:lic~i
eta . +~ellulo~e in ~~,~
the stress distribution ~~r~.s dc,t~'c~i,~.%1{~.u. by uai,ic~:.L ;~E; t,~iou_a.
~'xa.in~ples ~ver~; liven o.F ~+,c~~~1ya_.u,; i;il(: ;i~t~~h~~~a, ul slulul~~~ta:ioi1
~-1.1;~ dcr:ive(1 phy;~-i.c>.u.~i~~c:l 'o~.lld:i~l~, ~n~. lv�~,ituuir~~~1
c_l_dr~L:~.jl Luc ;.~~,.JJ~.ble: allsE.
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.4g-i-~.3/1~}
(Cant
tectonuuhysi.cs. �
Conference an l'tc)r_~I~:ov:.;':E~.y
.1.J. iJ. ~i~y~iUXlf3()1'1 JVii);aCi1~'1 ~tW
~ic,~ a 11 ~~l.t. ~.~ i i t, t'~
Lner~et;j.c;hr,~lci;y :~nati t~~t) , ~ ~� :I c r l ,rur e:;:~E;c, .r~o:i:'
(J :E' ~ 11,E .~ ~ {:
o.~ 5i~u:l�ctin~, an ~riouc;ls, , , in TTiodt.ls ~ n~1 iii
r simile+rity of ~~~huilu;;�i~>u~.:
Tna~teria~l.~.si.n~ ,,,-1d suf:ki.c.ient to lu1.f i1 coizciition'
nature it z.s necessory ~:~a~i. for t!?e n~~tur�1
ideu-tity fo.r� tll~; rl~~ciel
titrhicli en,~ux'e ~ ~,lu~x~., :~ u.l c~ini~~r~:~ic~~1~:s;~
ouject o:E the clit~Ctls~.uTi1_e~~-~ a ~rocesa, `.Clze ~_.utb.or
the :~~udieu 1
,~ up:~l~,ed ~ ~.
c;`.;uatic~n:s desaribit~.l,
cr;.l.~t?r~a:i.zed l;tTt~ t �~l,tt7.f, rrti' L"tluc.i c,.;rl t' c:
4=rhict~ it :t~:; rlut pc~s:;iU1i; i,i) co~rll)ly ~ti~it,il ~.:.1~. t~lu
1T1 CaSE.S iIl C,t c~ri,~i].O~y )Jilt U1?~L,~j~ ~�Il-til`.~-
~theorei;ically ~.eriveu. cunci.iti.otls
the IAa:ln. conditions oz ~.nal.cl~;;l� of i,i?e ;E;~~1~t11, ~~c.~c%, ,
~~z~ovskiy (Institute of T'~ys ~-c `' ~ a.nc>.
IuI. V. 1 justific~.tion of nec; ;:l~tuocts
USSR, ciVe ~- tlieoretic.G_ r of 1;ec~o1?ic procE:s:~es.
certGirl results of simulutin~ on moc_el~ a er:~
`' corice~~t:i.on.; eluci d~,Ifed in ~reviaus p P
un the t~a.~is o:L ~~ Gnr~.l,~sin~;
~ r o:C c~n~;lo~,y rr~~:i�e detexl:~inc;a y
tl-~e coniitio~~~ ~~t 1T1 E11?j'~1C0-clleiriic~.l
( Lick"t j.0I1S ~s'i1:LCl? ~. rE` 1'r:L~ie1~ l'~
't;1105E: e ~ ~ , ~i "~+ i)1- :J.eiUl';ii~:tlOnS
mechanics wYiicli cle.~cra.be ~ti}e ~ ~v~.luui,.~,,,t ,., .
to ccnsi~ierati~.,rl file aepencience u~. ~~~~ viscosity
in , c:;:..sileratian its
~,nd fr~.c~ture C-
on tl?F; stresses) ~-
8 1g c nce on the ~ {urn 1;icz1 of t11e ~~ctiori ~,.~ sae stresses .
depen ~.e
APPROVED FOR RELEASE. 06/23/11 CIA-RDP86-005138000617800052-6

li
~~,
G o r~ is t; ' C t l c~ t; o rl L' r ~ ~, ~ .. ,. ,~ ~ ��~ ::, ~~ a
,~ , :ice U� ~; r 1 j ~., ~~ ~ ~ ', .L 1 j
tjlc18 uraiN i~ Ci. t .ti ' i1S1-`'v1Ui1 i. J: !~,~ - '..
disruntion n � ''- r; .J�~r~.~. ~_u I.cc~:.,.>~.--~; "~~
~I;ypc 3i.sru~~~~- z -�,~u; "i,l,,l.l u.~~ r,:~~,;V, - _ . , . ~ .~E _ ~:,
~iiStiTl~;uiS.t1 ~JJ ~~ .., , - - ;; i-� - ~
f; v to ]_u L a. t~ r 1 cwt-' 1. ~, .. ~ ~ ; , :~ ~.) ~ ~. ; ,
ti j , ,
.P '1; 1, r; ~'d111.t'i1 ltr:c'8 ~:~ ~ i _~,,,,,,,~ ~,,i �,lit;
r P (l E::~~;t'i-'il.l.il(.., Ill ~~, ;~ :~ .,,1L'�; ...~. .f r..
~~.r;:l ~ttt ~~.lr~~ ii,l -;.i '.',,~~t_~u 1)~ ; ;, ~;i. i.t~
l; t if I;1c ~ i f; a. ~ ~ ~ ~ ~ ~, U T.1 O' !. !.:.i .i.. ._ ~ rl
~~ 't 1,IZe stz~es~ stoma t,c i ~ , , ~ .,~ ~ .1 1 c ~'~~,~�~ y t>~- F:
u~.I,u.(~ , incl. a1s~ i,t~~ :l.,,ex' i~ i~1~ , _ i ~ ) ;~' i;iiCiaC
G1.'l~.J.J i31.''.C (,1.011 ~ r. 1'_ ": ,_ ~ .l.CliJ V.1-~~.L l~~i `~ .1 ~.L.+- ~J,� `
GLE;:~ OIL C)Tl. c1,.1C1 t~;iC: _ ,.
~ ~ 1.:1
D0:.11.OS tid't'I.:LCiI tY'i'Y1S r -�~ ~ .l~?} L;at-',rlC;^ i,~_.~~ !~,_~t: z, _ L`1
~' 111 U ~ i~- I..: (.:' }
;;~ i~ L't.a:~C%S ~iC'L:L u ~ '~. ;.illU',11_i1. ~ ,i
~) j ~ t) f') U :i (1 u. 't~ l ~ 1,
.,. , , l: ~ rr 11e ull'~i1:1G r + ' lli.l ti Il :' ! ~ ., ~ ~ ;~ ~~ -~ ~ ~ ~::L' '~
u ~ ;.. 1
~lv~ ~ ~~_..~, 1-~ 0~1 ~_ 1t, ~t.~ ~~...1, ~ ~,:_ or -1 ~ .~r
iu~ ..~> ~.~ not cle~~ez _l `'- ~,~;_~zltu.r.. ~ .; k ,. ~:~c coll;
`7s4~ l )L ~f~ lit~rla
IIlEl~l;];'a ~,~It C'I,;� �Cr~i)i(' :'lljl~,i ).1., c ..
liyr?e ~.~ (~1:~1_'Llj)f):Ll)rl:i ~I:llt_'r'i)`~ i; I, l~:Ll:l~:l!SlOil�^ilU
11,h;~ c a�. ~~ I: ! , i_ . E~ c. olrt;v..., I'
i~lzndr ec 1'il _ _ t ~: 11.:~ . ~ e I.:~ ~t c:i' i. ~, ,
1 '.'~' ~,Y7 J
01 ~Cl(? ''x'~tlC1S Ctr~ill~'10a1.i.l. 1,~1G 4-u- .` `' Uil, (~I~+CL'~):.~t;~~ )1C
~~ ~t-l C: :C'U" ~ j (., Vi'i', .L I...;I.'ill)~/1. I' t y ~~
~); :c~~ic,~zlarly `�" ~ t, :.` uy .;l,vC~a: ~l c).r.lle.r.'~s
,~ ~ U ~:LOila, ~,11~, a.E,.u.t,~,l t_IL ,~~'l..C- i �.; l.tll.'i.~ ' .. .. ,`~
~JlLla ,LLllu:le l/llc.ll l/~.tl; l: .I.~ltf/Zt.>J_:)il:~ ./.l ~ ~=> ~ i
_ CL 1i t)L' Lire(', ~ilU:~."!1
~hE, ;ut~~~teri~l. ~, y c.. is 1t1.~ , .. .. .`,
U~. 1 , ~ Ili_.' ''J `~ lt.' i :.Vl:::i u 1. t. I l�1t.1 ,3~11,(;.lI?iF.'11 Oi' ,.t.l~~.
1';r ~,)�~;inG i':['~- c1,u.c'C'S 1C c.! ti~ C;
I'i: !v~::~ ~)u.intea ou, ~ ' }1L' , >, :.~~ie~~s ~~f
c~~, se ~~~ Ua: ruE' ~lij,;a.~e ,_~a_ ~c.l.' ;: be
venal orde~.~ ~ . i.~ i.iutl s,lou.l~.
u,~ C~ G Ic; incliv.i~~uzl crr~ci. ~; ,'~ .~ ' - n~~ion
~ f' l,) j
~i8t-ll ~~1-`~ p - j ~ ia::) ..t lll.:~:,'~l ~. ~~ L L.,I~ ,lF t), ~ `~1{~ . .ti~i V
c'.~zl.,i~.e1.e:~.
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Coat.) t}9_7_1.3/1
Conferer.,ce on tc;ctoraap~~,,ysics. C ,,tart to develo
developn~ent of tectonolaiy~ics, it; is im~~az
g the plastic a.nd strength propertiF=s ~f
methods of studying;
-uni:eorm layers of rocks under ~'heins11og~e~ox~mutiuno:ns.
non
New con~septions on thiousnuolidrer~' liquid bogies v~iiich
and disruption of var ortcd in the papers of
also extE-ndder andl~YaWe13P Fri.dman�
P. A. Reba.n ~ ~ ~ sic;]. CIiE~~,ais tr~1, Ac .ac . ,
P. .~. gel~inder, Institutlu of lhJ .-~.:~c~:~ozlce
;l~~l~
.:,,L ;,~ `,
1�;~,s ex~Lre;1~lc1y irui~txul_.

L
~i l
~Ilt:~ SL"�~l~a.;;; t, lc ;i1Gci1~ I1:ic~..
-;
C1.
ituC.11 ~~~eI11,lUi1 4Vc'S i)c1: ,
~
properties of ruc:~s.
(Ins~Li.Lu~e v
)l~rovicl~
V
' ., ,_ -~
:i t'hy~lcs of c.r~e Lurch ~`~c.~~c.,
.
t
.
a~. ~
J. ~ ) ~~E'~)L~1~~Ut.L Ut.). IiIU.L~.L'~I
. ~ . 1Z 1~ ~ ;;zlc:l L~eslll_t~, ~)f' i;ile
ii~t,; ~,ll)f~..,
1 i 1 ~ ~.
't) G I'"~11.5 O.L 1'~ C',.~, lIl.
I
l
'
StuC:.y Gj' Ill' U~1~~:LC;L11. c' 11i:i. iliC;C
' ~
_ n
.
~ .
l1~+I11~
i X11 si~Li;v~r republics, ~~IIt, r;iini:,try of G~'v.i.~:~y
a.ad Const~rvation of Putinc:a.~~~l ~~esources (l~ln~.sterstvo
Geolo~ii i Ukhrally Nc;dr SaSR~, tnG i:~~inis tr.y of idon-~~'errUU;~
i,'eti:~llur,~y (I~linister~~tvo Tsvetno~y iile~tuli.ur~;ii S~SR) a:~d
~.nc; iulini.,~~Lry of l~iiatlF'r.ika.ucation (~`Ii.n:i:~ ters'tvo Vysshe~,v
Ubr~~zova;cli,ya SS~l~). The confererlc~; Nres ~::1so at~t~~lded by
5pecia].i:~ is frol!~ (;IIiI1u ~~nd (;.,cclluslclva,L:i.a ti+r'lo wez ~: ~.t til~~~
cilne in .~Ioscovr. Twc;Ilty-ll1.I1u utt~!i.l.~>~l p~:.pcrs wexbe read ~y
Carcl 2/13 s~ec~.~:lis-L-s oil vtlysico-me;cii~`iaicUl properties of roclts, o:
~eolo~;ical conditions of foriaU~~i_on of folds an~>. frac~ure.~
iIi 'the Earth's crust, tia.e s~cructurc of or.e t nu cap 1 del)c~,:t.-t.~,
APPROVED FOR RELEASE. 06/23/11 CIA-RDP86-005138000617800052-6

rr~ ~ ~ ~ f i .M ~~ 1 ~~~~ V .
l.1
AUTi-~GR : G~ ovskxy, Ni � V .
'.~T'~.~: Conferer~cl~ can ~t;~cGon~>prlysic;s. (Sov~;~kici~r:+rz~i.,yL Ego te~~tor~oi'i~iY~�~
P;F.,~ZUDIGAL:r Izves~tiya Akademii NTaTuk~pjaSR, Se:ciya Geofi~iclles~ay"a,
.~SI~kkCl~': Un a sai;all scale, te~~Lonoptlysical inv~;sti~,ati.or~s have ucl~1
carried o,.~t fora 1on~, ti~~~~ :ire t.i~: U.j.~'1. and .E'r~r1Ce.
Durirr~; the last tU~o decades r�pl.d ci.cvelo~~l~~ents ti~:ve been aide
in this field in the U.S.a.R., Uhiila and Czecl~oslov~a~Lia.
wince there has been no cooc>erat,ion be~t~veeri the scientific
or~~~anizatior~s and the indiv~.dua]_ scientists ~,~o~.~kinG in the
Soviet Union in the field off' tectonophysics, there has also
tjE;E;n no a3eguate coordination rind t~~c re has been a great
divergence both in tie pr.'o~;~-'cn~~F~ of .~nvest,i~,~.~t~ivns ~.~Zd in
a adtz:; The Tnstituce of Physics
. ^i r~ ri
t1i; interpretation of fact~zU _ ,
of the "r~arth of she ~1c.Sc. USSR (Tnsticu~ Fiui:~i G~.yr:li xN ~a~R
la:; organised the first All Uni~~n ouiif i;reiice on teCtozlO-
pl:ysics, which had the following; aims: to i'orrnulate pore
.precisely the tasl~s of the t;ectonop~lysical investigations;
to elucidate the probler~~s ~vtlich ~~re of E;rtc.test interest
from the point of view of a,r.~pliod ~eolo~,y; to outline the
litost proR;isiil~ methods of t;ect:onopk~,y;;ic~ l xnvr;sti.~~Uian., i.a
Card 1/1~ i;norove the relations bet~veeri lnaiv_;_duGl .roses rc:i workers
APPROVED FOR RELEASE. 06/23/11 CIA-RDP86-005138000617800052-6

APPROVED FOR RELEASE: 06/23/11: CIA-RDP86-005138000617800052-6
Tecto;rzo-physical ~us'l;ificati.or~ of ~eo:lo~icel s~,isnz:icity
crite:^ia, II. (Cont.)
necessary to determine t;:b.e contours of the assLiz:~leG. ret;.o�~~
of maatima of tangential str~~s;~es, ~Lo ev~~l.l~ate ~~p~~x~o~ci,~t~~,trf~(,~~
by us'l.ng eq. C5) the rel~~tive+ ma~;rzitude of ttae l~iaxi.tnuzu
tange~~t~.al stresses acti.n~; inside 'the maxima zones ani- t+~
indicate the genetic types G~nd the maximum dimensions of
the f~1actures which develop and can be anticip~~ted in th~;se
regions. The seismastat~ic data should be camp~~red wi'til:,
the mFZgnitude of the def'orme.tion si,ruc'turs 1 e1e~-ents of ~,:r~e
Earth"s crust and 'tale tE~ctoz~,ic fracture; ussoc�it,tod ~~i t,~z E i~c~es ,
YrAR
(nul].et~.n o~ ~k~he Ac�"' ='~S3 (U.-~.~.~�)
pp ~ ~?73 ~-
to l;he, iorecas~L-
to~~o.~.physical. f.nvest1~~a.ti,ons re.Lat~.n~ .. , ~,
. .,, r ~t,uC,~yl.lt~'-; Ilcl'ti11Z.'~~= (~.~;~Or[!%t`s1t.1~071s
A.ii~`.I.FZ,EI~`~ .. T~:c
i.n~ of ear.^th~~u~.~~es consa.s#, ~.c~ ,~ ~ ~ra~r:ial~t~ n-`~ i~:t~e
r t'ra~~tures i.n the ~;ar~t;ki' s crust; ct ucl. ~ }. ~ overni.n~,
and 1~rie reld~tions t;
.. pse str~~ssei~ wYla.cr~. are linked with
~~tudies as-need at ~lucid.aG'~r~~; .., ~ ~ ~ st ar~d Ux~in
distribution off. ~ a~ carrylri�
q. in the structure of tl~e ~`A~Ytike necessity r i,n
,.,han~e wakes . ~l;1ie author
about f'rac~ruz"es arid, ear. ~nq 1~~~~.~.~~:~~})
vesti~at~.c~n.~ .has teen ex~?~urdal,bNa. ~., Y~4.~ � _,
out such ~.n a er (saxna ~l eria ai
the i3.~`s~; part of this :P ~ of ~eolo~ica7. crit aintec~
in ~~~hac;h the physical >ne~.nin�; ortance wa_~ p
se~.si~l_ic~:ity wt~s deter.~iii~lect anc~ the ~i~p
oi;~~es~.s wh~c~;ka ~.:tnlc.s ~t~~~iel~~`1ec.~~l. atl~i
~arthqu~~kes In i;i~ue ~rri i;~i. t,eo E.. }
out o~ c].evelo~~irl~ a hyp �~t,hErSis :~,
et,ition of In th:LS paper suci~ a hy~~. .o ;.-
the r~P
,- ~; cri~t,erautY~or ;grid :is e.~~:>xe;~sc:ct in2the:mUtic~~~ .-y ~~
t;~~.#~. ~,~?~ s e a. sz~t~ o ~. Y l~ lie
press~^~i~fac~. by
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APPROVED FOR RELEASE: 06/23/'1'1: CIA-RDP86-005'1380006'17800052-6
~~~
� Tectonophysical explanation of the gecheskoeloboano-ia
TITLE. Part I. (Tektonofi2l
of sc:ismicity.
vani~~ geologicheslcikh kriteriyev seysmichnoeti. ~: �
studied, it
In r�egiona which have not been ade~onallgeologica~. in-
will be advisable to carry out reQ, _
vegtigationa together with seismh~,stahto~teetapoasiblei
gations so as to detect: within t
time regions for which the ~aaaeBl1erticaggmovemen'ta of
gradients of new and pr. eser- Y
the Earth's crust take place and t~lerexig~enceaofainid
already occur; in these re~iona the e
~eaea!s is mo~~t likely and these
crea,aed tangential etr~~
regions should be cona:idered as t;he mo~tion$gwhich ha e
the point of view of s~eiam.lcity. In r g
been studied more exte:naively in ~icala~ieldtwork and
necessary to Carry out tectonophy
inv+sstigatione'`on models, with the aim utionrofitheat al~
hyp~~theaia on the moat prructuredandrtrend of develop-
max:tma, their internal at
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SUBMITTED: 10/2/55
AVAILABLE: L:~bra:t?y of Congress
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1
~a..
AUTHUR: aza~rskiya M. V.
_--..--. _

TITLE: _..,..
_ - ~._ ,V........~~ ---
Teci;onophysical explanation of th~> geological criteria
of :~eitsmicity. Part I. (Tektono:~i~icheskoe obosno--
van:le geologichesk~kh kriteriyev seysmichnosti. I).
PERICDTCAL: Izve~stiya Akademii l~aui~, Ser, aeo:fizicheakaya, 1957
No.~?, pp. 1~1m16C- (U.S.S.R.)
ABSTRACT: The physics of geological criteria of seismicity are
described and their im~~ortance is pointed out in
com~)lex geologica.l~geo~phys:lcal forecasting of earth-
qualces. In this paper the author is concerned only
witl~ the tectonophysic,~,l point of view of considering
the geological criteria of seismicity. He defines as
the geological critE~ria of seismicity of a given
reg.lon the geologiGa.l characteristics of the degree
of ~~eismic danger characte~nised by the maximum farce
of ;future .seismic tremors and their anticipated re-
Card 1/~F cur:rence as a function of timeo
be necessary to c;han~,e over Zn ~. inun~ the"presc,nt ;;tats
forecasting based can the knowledge
de the of the Earth and on tY~e eesndency ~7f
of the p
rd 2 4 development of deformations and stress
Ca / .~ -�
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