SCIENTIFIC ABSTRACT GZOVSKIY, M.V. - GYULAKHMEDOV, A.N.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R000617810004-4
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• Publication Date: December 31, 1967
• Content Type: SCIENCEAB

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Conference on tectonophysics. (Cont.) 49-7-13/14
in benzyl alcohol and it was proved that '~his plus~ic,
optically active material is suitable for modelling
tectonic processes. New instruments were demonstrated
which were recommended for investigatin8 physical properties
of the materials of the models.
N. V. Hikhaylov, Moscow Scientific Research Institute on
Building (Noskovskiy Nauchno-Issledovstel'skiy Institut Pc,
Stroitel'stvy) devoted his paper to investigating the
physical and mechanical properties of those materials which
are equivalent to rocks from the point of view of modelling
tectonic phenomena. For materials with crystsllisation
and strong, "high structured" coagulation structures, he
recommended determining of the curves of the kinetics of
increase of the deformation with time when stressed with a
consta~ tangential stress and the drop in deformation
after relieving the stress. Materials with low strength
coagulation structures should be studied by recording the
changes in tangential stress for a given constant deforma-
tion speed of the specimen. He described ~ new instrument,
the electron-selsyn elastoviscosimeter which he designed
C&rdlO/18 and some new methods of determining ~he coef�icient of
viscosity of the material.

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Conference on tectonophysics. (Cont.) 49-?-13/14
The following physicists dealt with the problem of modelling
the tectonic phenomena: L. E. Kachanov, Ye. I. Edel'shteyn,
G. V. Vinogradov, G. N. Kurznetsov, ~,~. P. Volsrovich,
A. V. Stepanov and also the geologists F. I. Vol'fson,
V. A. Aprodov, N. I. Borodayevskiy, Yu. S. Shikhin. It was
mentioned that the fund,~mental difficulties in developing
modelling techniques and definin$ more accurately the
condit.tons of analogy are due to the inadequate knowledge
of the physical and mechanical properties of rocks and that
much a~;tention should be paid in the near future to
improv!ng the theory and methods of modelling. The
geologists mentioned that from ~he practical ooint of view
the ex~.~eriments with non-uniform models of sections of the
ore fields are of greates~ interest. Tn-~ho resolution
of the conference it was mentioned-bhat i'~ is possible in
principle to simulate on models tectonic phenomena and that
the wo.~k carried out in this field by the Geodynamics
Section of the Institute of Physics of '~he E~rth is
promis �ng.
(Note: Up to this point this is s co~olete translation
except for the initial introductory paragraph).

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C&rd

Conference on tectonophysics. (Co[it.)
The mechanism of formation of large structursl elements
of the Earth's crust was dealt with by t;)ie following
authors:
V. V. Belousov (I~ti~te of Physics of the ~rth) mentioned
the variety of reasons of ~old formation snd~the necessity
that in each concrete c~se the locsl csuses o~ such ~
phenomenon should be investigated. He considered fold
formation as a reaction of l~yered plastic s~rat~ to the
differential verticsl movements of the underlying blocks
o~ the ~th's crust.
G. D. Azhgirey, ~oscow State University (~toskovskiy
Gosud~s~e~ Universitet) drew attention to the necessity
of usi~ e~ensively geological methods for detsiled study
of the long term history of formation of concrete
structural elements o~ the ~th's crust.
P. N. ~opotkina, ~stitute of Geologicsl Sciences (Institu~
Geologicheski~ Na~ ~ SSSR) deslt with compression and
stretohing in the ~rth's crust and possibilities of study-
' se henomena. � '
~ng=tii~=~, W~oscow Geological-Pr�spegting ~?ti~u~2
1~/18 %~_ ~f~s~d,,ing the mechanism of iorm~xon ox -u

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gonference on tectonophysics. (Gon~.) 49-7-15/14
folds ~nd fractures which d~veloped in l'ece~l; period.s,
on the ex~ple of the ridges of Ksrat~,u in Southern
Kaz~hst~. .
V. I. Keylis-Borok (Institute of Physics of the ~rth)
described the method which he developed for determining
the elements of location of fract~es in the depths which
bring about e~thqu~es and elucidated the direction of
displacement of their e~remities- The resolution
empha~ized the importance of 'She exteusive study of the
deformation of the Earth's crust within individual large
resions carried out by the Geod~CS Section of the
~sti~ute of p~sics of the Ear'~h. A number of papers
were devoted to methods and tasks of detailed investiga$ion
of tecto~c fractures.
~. V. ~ovskiy proved the inconsistency of ~he hypothesis
of G. Becket w~ch is widely used by geologists for
inte~preting the fract~e tcctonics~ he reco~ended use of
a conplex of modern conceptions on the strength of
mate]~ials which would permit to re-establish the basic
feat~=es of the tectouic stress field acting d~ing the
time of formation of the cracks. ~-*~tute of Geology of
1~/18 I. P. Kus~arev ~d L. I. Lukin~ ~=~ ,
Ore Deposits (Institut GeoloGii ~destorozhdeniy ~ SSSR)

---u, -,--,--,- un-un aesearch LusoiUute of the
......... Gold ='GeologiCal Prospecting Institute (Vseso)u/znyy Nauchno--
Card 14/18 Issledcvatel'skiy Geologo-Razvedochrgry Insbitu't Zolota)

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Conference on tectonophysics- (Cont.)
outlined those practical problems, I'or t~e solution o~
i~ is ~dvisable ~o study the 'mechar~s~. of for~ati�n of the
. . � Research ~sti'bute of ~ineral Raw
st~ct~e of deposits of gold ores.
V. ~. ]~e~r, All U~.o~.~+itut Minersl'no~o Syr'ya)
~,~taterz~ls Lvseso~ ~Y ..........
sides on the character of thc tectonic frsc~res and on the
craci~ distri~tig~ .... =~olo~ of Ore Deposits) demons~ra-
ted materiaZ inaica~zn~ '
deposits of iron, nickel and cobalt in the weathered crust
depends to a l~ge extent on the direction, density and
character of the crack ~stribution and of the larger
fractt~es in the basic rocks.
A. A Belitskiy, Tomsk Pol~ec~ical Institute (Tomskiy
Poli~e~cheskiy Ins titut) ch~act eri ze s the c omplic at ed
crack structure of coal bearing deposits on the example of
the Kuzbas �
G. V. Charushina, ~st Siberian Branch of the Ac.Sc.
15/18 (Vostoc~O-~ibirskiy Filial ~ SSSR) ~alysed '~he method
of studying fractures in s~llow sedimentar~ rocks on the
sample of the South Siberian platform, mentioning Ch~t

--. ~v~aoze
..... u~o~-zcaszon of th~ interpretation of fractures
...... '-- is inadequate and in some cases doubtfuli ~n p~ospect~ng for

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Conference on tectonophysics. (Cont.) 4~7-1~/14
ores the mechanism and history of deformation of the
investigated parts of the Earth's crust should be considered
as one of the basic scientifically justified methods.
The problem of cleavage was extensively discussed by
various authors. A. V. Pek, Novocherkassk Polytechnical
Institute (Novocherkasskiy Politekhnicheskiy Institut)
dealt with the method of microscopic investigation of the
rock structure for elucidating -bhe character of the
inves, tigated deformations (petrotectonic) and emphasized
the practical importance of this method from the point of
view of deciphering the structure of ore deposits in
dete~mining the displacements along large tectonic fractures
and also i~ other cases. The various problems of the
physical and mechanical study of tectonic deformation o~
rocks, which are impcrtant from the point of view of
engiz~eering geclogy were considered by I. V. Popov, Laboratory
of Hydrogeological Problems (Laboratoriya Gidrogeologicheskikh
Problem AN $$$R). The problems of tectonophysical
investigations relating to search for oil and gas with
analysis of concrete examples were dealt with by
C~rdl?/18 P. P. Ivanchuk, All Union Gas Research Institute (Vsesoyuznyy
Nauc~mo-Issledovatel'skiy Institut Gaza). It was recommended

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-~ :[- ' :-~':~;~' ':'-:'~;i- - I'~':~ i , ~! Ii'Ii. ~!l~!~! :ll'}l:~:~l!~:'~l~'l'~ ~! I"~i~?~l~'!~;',F

Conference on tectonophysics. (Con~;.) 49-7-1~/1~
to orgsnize a perm~nent tec~ono-pb, ysical se~zinary and
the o]?ganization of such s semin~y wss entrusted to the
~odyn~ics Sections of the Institute of Physics of the
Earth, Ac.Sc.

AVAI~BLE: L~b~ of

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(;ZOlr$/[I1r, ~'.V.

The development of teCtOm~phyet�~; conference tn the In. tltute of
Earth ~stc~. ~eet.~ SSSR 27 no.4:11~116 Ap '57. (~ 10:5)
(Oeolo~, St~ct~l)

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GZOVSKI�,

Modeling method in ~ec~onophysice [wita summary, in English]. Soy.
geol. 1 no.$:%3-72 Ap '58. (MIRA 11:6)

1. Im~ti~ut fiziki Zemli AN SSSR.
(~eological modeling)

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i~!il~i~ l~'J~:~:':~~' ' f;' ;, ' ~., .; :~!~- j ;: : :.~l~' ~j!! ::tll~:liJ

AUTH. ORS:
TITLE:

PERIODICAL:
ABSTRACT:

C~,zdl/5

~ r7

V.N. ~eL' sesov I.L. ~d.
._~G~!yski_~ku ~i.V. , Krestnikov, , ,
Reysner, ~i
Tectonic and Seismic Conditions oJ ~skiy ~yOn tn
Tajik SSR (Sopostavleniye tektoniki = seysmku, uuusu'yu
~ms~go l'~kyona ~adzhik~ko~' SSR. I) Paint. I.

Izves~iya Akad mil Nauk SSSR~ Seriya Geofizichesksya,
1958, Nr 8~ pp 959 - 976 + 2 plates (~SR)
A ;~unction of tl...~ vast Asi~n mountain chains, Himalaya-
P~air ~eosyndine and the T'~n-Shan ~nge v~ith the Ta.jik
depression represents tei'rJ.$ory o~' very active seismic
activities. P~ticularly, the Ga~ly rayon is ~o~ for
its highest concentration of the epicentres [Fig~es 1
and 5).
The history of its alpine~ tectonic movements and the
formation of iSs geological stz'ucture can be represented
in tb~ form of diagrams. The structural chan~es v;hich %~'ere
un(l~rgone during the periods of the ~esozoic and the
Kainozoic in the eastern p?.~t of the region alon~ tke
line NW--~ are shown in Fi~re 2, while Figure 5
represents the same cross-section running through Garmr
skly rayon.

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............. ' ................................ '"'"'" ' ' ........ ' ........

Tectonic and Seismic Conditions c~Gau.~iy Rayon in Tajik SSR

Some of the data given in the diagrams were interpolated
from the places situated �arther away (Figure 4) but it
was a~sumed that the possibility o� error could not affect
the general character of the graphs�
A clear difference in the tectonic movements between the
geosyncline and the plateau areas can be clearly distin-
guished in Figures 5 and 6.
The present structure (Figure 7) of the Garmskiy rayon and
~E part of the Tajik depression is characterised by several
divisions of which the most important is the alpine district
of Psm~ir and Darvaz.
A maiz~ feature of the structure of th~ Garmskiy rayon is a
vertical displacement of the isolated blocks separated by
the tectonic faults which break through the Earth's core~
The traces of these faults can be found even in the
Palacozoic base. A change o~urred in their direction in
comparison with that in the Neogen and Quatern~ periods
at thE, time when an inversion took place of the pre-Pamir
depression and when the region of the Kabudkrin rose above
the s~roundtng areas.
Card2/5 At thE: same period in the ~orth-west of the Kabudkrim

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SOV/~9-%-8-3/l?
Tectonic and Seismic Conditions of C~mmsk~ R~yon in Tajik SSR

Uard~/5

anticline, a series of faults developed, the depth of
which is characterised by the long and narrow grabens
filled with small rocks (Figure 1). These grabens could
not be independent structures as those in other areas
(Figux'e 7). It can be assumed ghat they are the remnan'~s
of the, changed direction of the movements of neighbouring
regions. Originally, a rise of one of the regions caused
the formation of a fault. The faults, in turn, caused a
break in the general movement of the area. Thus, at the
boundary of two neighbouring tectonic regions, the faults
can be, found, usually at the narrow ridges (Figures i and 3)~
The fc.rmation of new faults in relation to the dislocations
are em~lained by the faults being not vertical. They -are
mostly inclined towards its lifted side.
A noticeable feature is a ~ry well-maintained range of the
young faults and folds of ~eogen-Quaternary origin~
Their large number signifies a horizontally directed course
of the tectonic regions. Also, it can be assumed from
their general orientation that the shear effect was directed
along the Meridian.
The Palaeozoic foundation of the Garmskiy. rayon was e��ected

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~-~ ~f/Lr 9- ~r~-8- ~/~.. ?
Tectonic and Seismic Conditions of Ga~mst~y Rayon in Tajik SSR

by both the strong, vertical forces and the weaker,
horizontal shearing stresses, thus being subjected to
a deformation which was of plastic character. This can
be .~leen on the surfaces where the Pala~zoic is found
clo~e to the ~esozoic rocks. Where this ~y~e o� deform-
atic. n occurred with great speed, the faults were formed.
It could be said that all the blocks of Palaeozoic origin
behooved not as rigid bodies but as O~ plast~ic medium
with some parts of the Earth core being somewhat~of
gre~ter viscosity in relation to the ~!esozoic and the
Tertiary sedimentations.
The general character of the mechanism of formation of
the alpine structure of tb~ Garmskiy rayon could' be also
applied to the regions of Taji~ dep~:ssio.n
It can be assumed that the developments in the Garmskiy
~ayon took place during the second half of the Quaternary
per~.od and lasted about 120-230 thousand years which can
be compared with 600 thousand years of the total ti~e of
the Quaternary period.

Card ~/5

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Tectonic and Seismic Conditions of Garmskly Rayon in Tajik SSR

There are 8 figures and 28 references, 25 of which are
Soviet and 3 German.
ASSOCIATION: Akademiya nauk SSSR Institut �iziki Zemli
(Ac. Sc.USSR)Institute of Terrestrial Physics)
SUBMITTED: August 28, 1957

Card 5/5

1. Geology--USSR

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AUTHORS~~, Krestnikov, V. N., Nersesov, Io L.~
' ' Reysner,
TITLE: Comparison between the Tectonics and Seismicity of Oarmskiy
Rayon of Tadzhik SSR. II (Sopostavleniye tektoniki s seys-
michnost'yu Garmskogo rayons Tadzhikskoy SSRo II)

PERIODICAL: Izvestiya Akademii Nauk SSSR, seriya geofizicheskaya~
1958, Nr 12, pp 1~25-1~42 and 2 inserts (USSR)
ABSTRACT: It was observed t~t more than 9000 epicentres of the
energy from lO~ - l0 ~ j showed activity during 1955 and 1956
in Geamu,kiy rayon of about 15 500 km~ (Figs.2, ~ and 8). The
earthquakes were registered in sufficient detail to give a
complete picture of the seiamicity of this region (Fig.1)~
This region, therefore, was chosen for the investigation on
the relationship between seismicity and tectonic structure�
A quantitative method of investigation was chosen so that the
analysis of tectonics could be utilised in the determination
of seis.micity. The mean gradient of the velocity of vertical
tectonic movements of the e~rth crust was calculated from ~
Eqs.(1) and (2). Some results are shown in Figs,*, 5 and 7
and Tables i and 2. The cross-sections I-I and II-II
employed in the calculations can be seen in Fig.6. The com-
Card 1/~ pariso~, showed that in aarmskiy rayon the a~eas of higher

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SOV/ ~9-58-12-1/17
Gomparison betw~een the Tectonics and Seismicity of Garm~y Rayon of
Tadzhik SSR. IX.
seismi�.~ activity coincide with the banded structv~.e, for which
a mean gradient of tectonic movements in the Quaternary peried
was high (Figs.5 and 6). Therefore, it' can be stated that the
velocil;y of seismic activities increases with au increase.of
mean tectonic gradient. In order to verify this relation, a
method was devised which could be applied to any region having
seismic, activity of short duration (2 to 3 years), provided
weak earthquakes and the measurable gradients of tectonic
moveme~.ts are of recent origin. This method is based on the
deteiled analysis which showed that the correlation between
the frequency of earthquakes (Fig;l) and the tectonic grad-
ents ~'ig.6, is maintained in various areas of the Garm region
Table 3, ~ - frequency). As the above relation was found
for one region only, it is possible that some modifications
Card 2/3

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SOY/ 49 -58-12-1/17

Comparison between the Tectonics and Seismicity of Ga~skiy Rayon of
Tadzhik SSR. II.

are necessary for the different tectonic structures or for
various depths of the earth crust. Therefore~ the investi-
gations in this matter are not yet concluded and the addit-
ional information will be presented at some future date.
There are_ 3 tables, 8 figures and 28 references, of which 23
are Soviet, 3 are German (2 translated from Hungarian)~ and
2 are English.
ASSOCIATION: Akademiya nauk SSSR, Institut fiziki Zemli (Academy of
Sciences, USSR, Institute of Physics of the Earth)
SUBMITTED: August ~ 1958.

Card 3/3

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GZOVSKIY,._ ~Ltkimil_~lad~mir.~o�ich; BELOUSOV, �,V., otv.red.; FEDOT'YEV,
K.~(., z'ed. isd-va; MAKUNI~ Ye.~., tekhn.red.

[Basic tasks in studyihg ~be formation dynamics snd tectonics
of the Baydzhansay snticltne] Osnovnye voprosy tektonofiziki
i ~ektpnikaBaid~hansalakogo antiklinorlta. #os~va, Izd-vo
~d.na~ SS~. Pts. I and 2. 1959. 254 p.

1. Rukovoditel' otdela geoclJ.~amiki Instituta fiziki ~emli AN
3~'SR (]for Beleusov).
(Eara Tau~GeoI~gy, Structural)

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B~.OJ~O?, �.V.~ red.; G~-O~-~_~_H_Ho?, ~ ~nd.~ol.-~ner.n~, red.
~SH~, T.T., ~d. izd-v~ ~OTA, O.A., te~.~d.

[Tectonop~eic~; tr~ne~ct~one of t~ ~ll-Un~on Coherence on
Tectcnop~cs] � ~oble~ tektonoff~zik~; t~dy Pe~o~ Yse-
eolugnogo tektonofiziches~ogo soveshc~ntia. Pod
~l~aova [ H.g.O~ov~ogo. ~o~a, ~s.nauc~2e~n.~zd-vo
[~t-ry pO ~01. i ok~ene nedr, 1960. ]6] p.
(a~ zq:~)
1, Veeso~zno~ tektonoffizicheakoye soveshchani~, let, Moscow,
19~7. 2- C~en-kor~apondent ~ ~ (~or ~lou~ov).

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PHASE i BOOK KIPLOITATION

$0V/5096

Bune~ Vo I~,~ ~~ K~ K~ Zapol'~skiy~ Vo Io Keylis-Borok, V~. No Kr~tnikow., ,,0 N~ Malinovskaya.~ Io Lo~ersesov~ Go It Pavlova.~
T~ Go Bautian~ G,~ I,~ Reysnsr~ Yuo V~ Riznichenko~, and V. I o Khalturin

Metody detai~nogo !zucheniya seysmichnosti (Methods of Detailed Seismic Research)
Mosc~n~ Izd-vo J~ SSSR~ 1960~ 327 po Nee of copies printed no~ given�
(Series~ Akadez~ya nauk SSSR~ !nstitut fiziki zemli~ Trudy, vyp~ 9 ~176])

Resp~ Ed~:~ Yuo V.~ Riznichenko~ Corresponding Member AS USSR; Ed� of Publishing
House~ So Io Mosarskiy~ Tech~ Edog 0o Go Ul~yanova

PURPOSE~ This book is intended for geophysicists, particularly seismologists.

COVERAGE: The book s,,mm~r'izes the prinoipal results o� the work of the TKSE
Instituta fiziki z~mii AN SSSR (Tadzhik Complex Seismological Expedition
of the institute of Physics of the Eat'th of the AS USSR) and the Institut
seysmologii AN Tadzhikskoy SSR (Institute of Seismology of the AS Tadzhik
SSR) during ~he period 1955-1957o Among the topics discussed are: seismic
apparatu~ usod~, new methods for determining the coordinates of earthquake

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Methods of Detailed Seismic Research

sov/oo

foci, detailed methods for determining the structure of the earth's crust,
some results of these de%erminationss, methods of determining seismic energ~
on the basis oi s series of criteria~ analysis of dominant frequencies; the
u~o of froquonoy-,~ol.oot~v~ ~pparat,u~ a goner'al do~orlpt:ton ami a~a!yolo
of seismic conditions in the Garm and Stalim~bad areas~ tim gool.ogtcal
structure of the Garm region and the history of its development~ and a
comparison of the spatlal distribution of seismi�ity and the geological
and tectonJ.c str~tume of the area� The Foreword mentions Academician
G~ Ao Gambu.rtsev [deceased] who laid the foundations for this work when
he was director of the TKSE~ The individual chapters of the book were
Mritten byx Introduction aud Chapter I -- I. LoN~rsesov and Yu~ Vo Rizni-
chenko~ Chapter 2 -- !~ Lo Ner~,~sov~ Chapter 3 -- Io Lo Nersesov.and T. C.
Rautian) Chapter 4 -- T,. G~. ~autian; Chapter ~'-- K. K,, Zapol'skiy and
V~ I.. Khalturin} Chapter 6 -.~ �. [o Keylis-Borok~ L~ N~ Malinovskaya~
Go Io Pavlova~ and Vo I~ Khaltu_rin; Chapter 7 -- V. Io Bune~ Io L. Nersesov
and Yu~ V~, Riznlehenko~ Chapt,r 8 -- Mo Vo Gzovskl~, V. N,. Kres~nikov,
and G., i~ Reysner$ Chapter 9 -- Vo I o B~ne~__M. V. Gzovski~ and I~ L~ Nerse-
sovo There are 272 references~ 185 Soviet~ 73 English, and 14 German�

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~ h
Detailed Seis~i~ Researc S~V/5096
Methods
of
5. Seismic reg./of the Stalinabad region 239
239
Study of ,~rthquake frequency cur~.es. . 242
Study o~hange in time of the seismic regime
On ~/means for further investigation of the seismic regime 244
in ~he Stalinabad region
Ch. 8. History of the Geological Development and the Present
Structure of the GarmRegion 247
1. History of Alpine tectonic movements and the formation of 247
the geological structure of the Garm region 249
Triassic and Jurassic 252
Cre~aceo~s 253
Paleocene and Eocene 253
Oligocene and Neocene 256
~uatezm~r~...peri~d:
~62
2. Present structure of the Garm region 263
Internal structure of Paleozoic formations 263
Form of the upper surface of Paleozoic formations

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Methods of Detailed Seismic Research

SOV/5096

Internal structure of Mesozoic and Tertiary deposits
Form of the upper surface of Mesozoic and Tertiary deposits
General arrangement of the present structure of the region

Mechanism of the formation of the Alpine structure
Structural results of change in direction o� the movement
of teetoz~e zones
Indications of additional weak horizontal compression
Mechanism of fold for~ation
Formation of transverse faults
Form'of tectonic zones

Ch. 9.
1.

� , ~Stalinabad
C ar,d~(5~

S~iamicity of the Region and Its Comparison With the
Structu~:al Geology
Map off epicenters
Method: for drawing a map of epicenters
General �,haraoteristics of the composite map of epicenters
Co~l~arisc,n of the epicenter maps for 1955 and 1956
~arm regd.on ..
region

265
269
270

274

274
276
~76
278
278

279
279
280
282
283
286
288

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S/ l /60/O00/OOO/O0 /O)l

AUTHOR:

Gzovskiy 9 M.Vo

TITLE: Tectonic physics and seismic zoning

SOURCE~ Akademiya nauk SSSR. Soviet po seysmologii. Byulleten'~ no.8,
Moscow, 1960. Voproey seysmicheskogo rayonirovaniyae 67-72

TEXT: The author discusses the character and compilation of seismotectonic
maps9 and shows how the parameters essential for compiling these maps can
be determined. In the author's opinion9 seiemotectonic maps must separately
define zones of t,resent and possible future earthquakes differing in depth,
energy~ and recurrence. The total amount of seismostatietical data for each
point or uniform zone can be most fully rendored by the main parameters of
~he lqgarithmic curve of recurrence of earthquakes of different energy�
The main parameters of these curves, which were compiled by Yu.V. Riznichen-
kom IoLo Nergeaov, and V.Io Bune for a number of Central Asian districts~
are ag followg: (!) the upper limit of earthquake energ~ (Usmax); (2) the
angular coefficient ~ of the rectilinear section of the curve in the area

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S/~19/60/000/00~/005/0~1
Tectonic physics... DOS1/Dll~

of micro-~arthquakes; (~) the location level of %he r~ctilinear section of
the a~rve, fixed by the recurrence of earthquakes of any definite energy
(Nj)o' TN author considers that seismotectonic maps should bmsically ~how
zones wit~ different U_ of earthquakes with a definits focus depth.
Within the zonoe~ aeot~ characterized by seismo~ta~i~tical data a,~d
sections establi,~hed as a result of extrapolation and in~erpo/ation accord-
ing to geological features should be distinguished. The recurrence of earth-/
quakes Ni must' represen~ the second (~uperpoaed) sign. For USmax~ the
author developed a formula which contains quantities (coefficient of propor-
tionality between earthquake cen~er volume and cube of faul~ extension~ ve-
loci~y gradient of tectonic movements~ coefficients of viscosity and li~
berated ene~gies~ etc.) with peak values in each sec~ion~ the ~otal number
of peak values determining the upper limit of earthquake energy. For some
eections~ this limi~ is established seismostatis~ically~ and for others,
in which seismostatis~ical data are interpolated or extrapolated~ the upper
limit can remain unaltered or vary depending on constancy or change in the
values of %he quantities of the formula. The an~ular coefficient ~ of the
rectilinear par~ of ~he curve of recurrence permits calculating how ma~

Ca=d

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S/519/60/000/008/005/0~1

Tectonic physics..,
times (m) the number of faults will decrease when their length is increased
r times: l~ . (3)
lg m = ~ V lg r; � = $ lg r

The author further derived the formula
i (lg (6)

where L is the coe�fYctent of proportionality between the cube of the length
of faults i and the energy of earthquakes US caused by them. It shows that
'for sections with uniform conditions for earthquakes, the logarithm of the
length of faults causing the shocks is a linear function of the logarithm
of the earthquake energy, if L can be determined for some earthquakes. The
amthor also shows this dependence diagrammatically and proves that, on the
basis of seismic data,'the empirically established curve of recurrence and
coefficient L permit the size of faults and the characteristics of their
historical development to be evaluated� The remainder of the article is

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Tectonic physics.,,

S/519/60/000/008/005/031

devoted ko recommendations for the compilation of tectonic maps� The prin-
ciples and methods of compiling standard tectonic maps are being developed
by V.No Krestnikov and G.I~ Reysner using the Garmskiy rayon and other
sections of Central Asia as examples. Soviet scientists V.V, Belousov~
GoPo Oorshkov, A.Vo Goryachev~ I.Ye. Gubin, I.V. Kirillova, V.No Krestnikov~
B.A. Petrushevskiy~ I.A. Rezanov~ and A.A. Sorskiy are mentioned for their
efforts in developing seismotectonic maps at the Institut fiziki zemli AN
USSR~Institute of Physics of the Earth,AS USSR)~ I.Mo Kuznetsova and T.A.
Tikhomirova - for having calculated, together with tH& author~ certain geo-
physical coefficients belonging to the U~ma� formula. There is i figure.

ASSOCIATION: Institut fiziki zemli AN SSSR (Institute of Physics of the
Ear'~h of the AS USSR)

Ca=d 4/4

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S//169./62//000//002//0'13///072
D228/D301

AUTHOR:

TITLE:

Physical theory of tectonic fracture formation

PERIODICAL:

Referativnyy zhurnal, Geofizika, no. 2, 1962~ ~0.-11,
abstract 2A68 (V sb. Probl. tektonofiziki~ M.~ Gosgeoi.~
tekhizdat, 1960, 78-96)

TEXT: The notion about the strain ellipsoid finds a strict tecto-
nic basis in the geometric consideration of any homogeneous deform.
msilono The strain ellipsoid can~ therefore, be used to describe
complete homogeneous deformation and also its plastic and elastic
components. The method proposed by Becker for comparing fissures
with the strain ellipsoid does not always give accurate results.
In the study of fissures and large tectonic fractures the author
proposes the use of 'the complex of contemporary notions about the
strengths of materials. It is noted that the nominal momentary
~ensile strengths of rocks is about 0.000! of the modulus of elas-
ticity~ and that the nominal, momentary shearing-strengths are aboui

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$/169/62/000/002/0~5/072
Physical theory of .o. D228/D301

0.001 of the ~hear modulus of rockso Hence elastic elongatione
and elaetic shears in rocks are always less than 1% and 1o respec-~
tivelyo The author proposes a complex physical theory for tectonic
fracture form~tion which contains 6 basic principles� 1) In each
material two types of rupture -- tearing and shearing -- and their
two corresponding strengths are possible. In.ch specific case
rupture is determined by the character of the strain state and by
the correlation between the material's tensile and shearing
strengthBo 2) The tenacity values do not remain cohstant but change
in relation to the duration of the action, the manifold compression
and ~he temperature� This principle is corroborated by numerous
periments and theoretical research� 3) The strengths of rocks may
vary widely depending on their lithol0gic and petrographic peculia.-
ritieso 4) When studying the process of frac'~ure formation it is
necessary to take into account the influence of the selfemerg~ng
rupture surfaces on the strained state of their surrounding areas.
In some areas a weakening of the stresses occurs~ but in others
they are streng~thenedo 5) The processes of rock rupture develop
over a long period of time irregularly, together with plastic and

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~T'~! ~ .: ::~[,-!~'.::;J~ ~lli :(J;~i-: :7 'J. i : : !'[ Ilt ~lil:f JlJ~"JJl~J ~.JJ~-JlJJ~',~J:~,~,J~J~JJ~!frJ-~J!~f~'~II:IT'~''''~''*I'IIr'''- ' '" '

ee/ /ooo/oo /o 0/o 3
S/1
D228/D30~

.... ~,::, ~',Iodelling of tectonic orocesses

PEitlODiCA]]: Re�era~ivnyy zhurna!, Oeo_~z~ka, no. o, - -
abszract 6A58 (V sb. Probl. tektonofiziki, M.,
geoltekhizdat, 1960, 315-344)
TEXT: The modelling o� tectonic processes is based on zhe prin-
ciples of: 1] the similarity of the models of natural objects;
2) zhe choice (zke selectivity) of naZural processes; 3) the
azzze, en~ factors (of Zhe separition)'on models;
paraze szudy of ..... ~ * '
successive approaches (the approximation)aeducz~o,.to aabouznazuralthe objeCt;results
~I the statistical substantiation of ' ~ ~s
of model tes'~s. Proof is given for the oossibility of modelling
zectonic processes -- ~he formation of ~olds, boudinage ruptures,
and oZher macroscopic manifestations of crustal deform~ion a~)d
disinzegration Conditions of similarity are derived from dif
� ' the fields of Zectonzc
_e.~m~l or integral equations, describing
car~ ~/3

j/

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Modelling of tectonic processes D228/D304

stresses. A sJ. milari~y condition, illustrated by numerous
is derived mathematically. The question of the extrapolation of
laboratory data to notions about extremely long geologic processes,
!a~ting for thousands and even millions of years, is considered.
Conditions of similarity are deduced for the processe? of plastic
and e!aszic deformation and rup2ure formation, both statistical
and inertial forces being thereby taken into account. The coeffi-
cients of viscosity are considered as functions of the temperature,
the manifold pressure, and the tangential stress intensity, the
coefficients of durability being regarded as time functions; the
shearing strengths depend on the normal stresses. Besides the ge-
neral conditions of similarity, allowance was also made in a spe-
cific model for the boundary and the initial conditions. The prac-
tical feasibility of modelling is demonstrated. In addition to this
.oc~s and
� ~ '~:~ ~ ~.S
a co~.~._son given for the mechanical properties of ~
equivalent ma~;erials. The opzicai method of studying stresses in
moacis is also examined. Examples are quoted flor the use of models
in solving gec~!ogica! and geophysical problems: 1) ~ae ~o .... a~ion
mechanism for longitudinal flexure and lamination folds in vhe
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~L�' ~.�., ~.~k~. V.~.~ J~ l.b. a~ ~o~n~, ~.I.
~ pr~eipl~ of o~ bo~Y~ for amt~l T~'~' II
~I~s ISv~tL~ A~t ~k 8~i, 8~ g~flsie~, 19~. Ir 3,

~nt of ~ow of ~rtnG ao~t~on.
rmto of tect~le moY~m~ as d~er~b~ b~ G~ou~ ~ al. (R~ 6).
~: .,p ,h~ ~n ,,g1 --' cmg, l~ on ~e ~i. of ~e r.ul~ ~'
ob~n~. Tho noth~ of soimic pro~os~s co~istd of ~ so~to

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BI' ~, ::;' CIA-

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New l~ineiplo8 of -qeLem~c Zon~G Derived for Central Tyun~-3han. TI

As an muuplo, tho ~oblbilit7 p{ 0.001 of oc~ .
(once or l~e in 1~ y~l is s ........ rr~ee of
dum~e It~e~r~ ~d -/ ~ ~,~oAe z'o~ ~o oreo~ of l~a /
r~ v.~A ~onee or A~a in 1~ y~) for /
lo~-~tAng at~c~rm. Det~t~on of auch a
~e ~ ~ ~e above son~n. ~..+ ...... P~bill~ ~

3o~ ~i 2 ~G~ah. ~A~fm a~ ~9 r~oncm, 17 of ~l~ if0

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AUTHORS:

TITLE:

Shchegolevska~a~ N. A., 0sokinat D. N.t S/153/60/003/01/047/058
Gzovskiy, M. V., Soko!ov, S.I. BOll/BO05

Polymeric r,',a~erials With Different Physicomechanical Characteristics
for Stress Investigations by the Optical ~e~hod

PERIODICAL:

Izvestiya vysshikh uahebnykh zavedeniy. Khimiya i khimicheskaya
tekhnologiya, 1960, Vol 3, Nr 1, pp 172-175 (USSR)

TEXT: The authors pm~ved ~he possibili~y of producing pho~oelastio substances
wi~h high optical activity and a wide range of elasticity moduli (up ~o gel-like
substances of the gela'~in-Jelly type). These substan~zes are produced o$ the basis
of copo}ymers of unsatlAra~ed~polyes~ers, of p~yrene,~and of glyph~halA~an~epoxide
resinsJ~These material,~ had manifold, given ph~sicomeohanical propertie~AThe
authors paid special a'~tention to the production of plastics with a vi~-cosity
(~) of 104 .- 107 poise,~ an elasticity modulus E = 10-1 - 101 kg/cra2, and a high
optical activi~yo Produc~s of copolymeriza%ion of unsaturated esters and vinyl
monomers have a reticular structure. Products with different optical and meShani-
cal properties can be obtained by changing the number of chemical bonds between
the molecules. For this purpose, ~a%urated dicarboxylic acids (e.g. sebacic acid)
are introduced besides unsaturated maleic acid, and the number of individual
monomers (e.g. s~yrene) is varied,. In con~ras~ to previous papers, the authors
investigated polyesters obtained with the use of reduced amounts of maleic acid
Card 1/~

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Polymeric Materials With Different Physicomechanical
Characteristics for Stzess Investigations by the
Optical Method

09680
5 o/oo ,/o4 5e
~o~ VBO05

and an excess of diethylene glycol (according to Ref 3). It' was proven that the
maximum amount of sebaoic acid must not exceed that of maleic acid' (1:1), or
the product would become opaque. Benzoyl peroxid~ (O.1 - 1%) was added to the
mixture. Polymerization was carried out at 20-40�. The polyester - styrene ratio
was varied between 2:! and 500:1. Optically active substances with
E = 0.2 - 20 kg/om2 and a coefficient of optical activity Bo = 100-1000 brewster
(10-13 cm2/dyn) were obtained with styrene at a ratio of sebacic and maleic acid
in polyesters of 2:1, m~d acid : diethylene-glycol of 2:3. Even at a polyester -
styrene ratio of 1:500, they remained gelatinous. The figure (p 174) shows that
both the modulus E and 'the optical activity of the polymer considerably increase
with increasing styrene content. Modified glyphthal resins are condensation products
of.pol[a~omic algohols.(pentaerythrite' glycerin, diethylene glycol with phthalic
ana maxcie acid (Ref 4), T~ey are called '~gl~ftamal". They are suited for work
at room temperature, having E = 50,000 kg/cm and BO = 36 brewster~ Very trans-
parent substances with ~ = 104 - 107 poise, and B~ = 2.103 brewster can be
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Polymeric Materials With Different Physicomechanical
Characteristics for Stress Investigations by the
Optical Method

S/15 5,/~0,100~/01/047/051]
BO~ 7/3005

obtained by changing the acid - alcohol ratio, adjusting the thermal treatment~
and using plasticizers. Previously (Ref 5) the authors had produced an optically
active, solid, elastic material "epoksiftamal" from the epoxide resin E-40.
In the presen~ paper, the amount of hardening agent was reduced to 3-5%� The
resin became Jellylike but remained brittle. At a content of 2-5% of maleic
anhydride and 30% of dibu~yl phthalate, an op~ically active, highly viscous
liquid without a noticeable yield point was formed. At 5~22% of dibutyl
phthalate, the resin has the maximum shearing stress~ By combination of epoxide
resin with hardening agent and plasticizer, it is possible ~o produce optical-
ly active substances with manifold physicomechanical properties: Trom elastic
bodies to viscous liquids. There are 1 figure and 5 Soviet references.

ASSOC IAT ION:

Moskovskiy institut khimicheskogo mashinostroyeniya; Kafedra
fizieheskoy khimii
(Moscow Institute~r the Construe%ion of Chemical Machines;
C~f Phy,ical Chemistry)

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Polymeric Materials ~i~h Differen~ Physicomeohanical
Characteristics for 8~ress Investigations by ~he
Optical Method

69680
s/'5!/60/oo3/o,/o47/oss
BOll/BO05

SUBMITTED: April 10, 1959

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GZ.OVSKIY, M.V',; ]~3rLEs~IIKOV, ?..'q.; Id{O}BV, N.N.; ~OV, I.A.; }{.B'TSI[]{~{, O.I.

~a~ of recent toctonic movements in Centra~ A~i~, Izv, Alt 38311. 8er.
geofiz, no.8:1168-1172 Ag '60. (MI~A 13:8)

1. Akad~emiya nauk S~SR. Institut fiziki Zemii.
(Soviet Central Asia--Geology, Structural~#aps)

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85707

AUTHORS:

TITLE:

S/069/60[022/004/004/005/XX

osok o ovski , V..,and
Pavlov, V. P.
investigation of the Processes of Plastic Deformation by
Means of Eth~lcellulose~Solutions and Gelu and Optical
Polarization
PERIODICAL: Kolloidnyy zhurnal, 1960, Vol. 22, No. 4, PP~ 454-442
TEXT: The investigations described in the present paper deal with the
problem as to whether it is~ in principle, possible to study shear stress
and rate of deformation in plastically deformable soft bodies by the
method of optical polarization. The results obtained may be usefully ap-
plied in the mechanics of disperse systems, of tectonic physics, etc~
~he measurements were carried out in a device designed by V~ P~ Pavlov
cted b the Institut fiziki Zemli AN ~SSR
(Re�~ 15) and constru Y ..... ~ ..... u~l., fulfilled the func-
o'? the AS USSR), wn~cn smmu-~a-=~ - ~, schemat-
of Geonhvsics
tion %f a plastoviscosimeter and a dynamooptmme~er. The device

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8~707

processes of 'Pla. tic S/06~/67~0~2/004/004/005/XX
investigation of the gthylcelluloSe Solu- BOOa/BObb
Deformation by Beans of
tions and Gels an& optical Polarization - . the original paper oon-
_~eA ~n detail ~_~ =% gs well as
_ ~ and descr.~uy]~ ~ :~co~e /~Dr-T/~
ically -"__~ ~the'r thzn~ a~-~.~JZ~ optlca~ ez tic
deformation-kine
tains, amo~ ~. ~or
Berek compensatOr ~ well as the
shear stress on d.eforma%ion as s elmStoplastoviScosimeter
were ascertained with the help of pavl�V:thylcellulOSe of the tYPe K-290
%0~ and a subs%ituti�n degree of
(Ref.~ 14)- The matermal used was soviet ~ . lutXOn was -290 centipoise
(K.290) with a molecular .eight of 7~7"
4�'%{~% mhe ethyl celiU~ --trations) and/Or --ed in a ~0~
-~ohol k�i ~'~ / .~se mixing '~ ~--rams oI e~
~ - ~- m~xtures k~ ' ---n in the ~l~ � --s was betwee~t �
= -~d resu~ _. _~ ,ellUzU=~ __1
modulUS of snu~.
v~scosity between 10' and 107 poise
alcohol co - "'

cal properties, a
.sscouS ~ewton ~quidS having completely

Card

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Investigation o� the Processes of Plastic S/069/60/022/004/00~/005/XX
Deformation by ~eans of Ethylcellulose Solu- B003/O56 '
tions and Gels and Optical Polarization '

~he blrefringen~e (~ ~ bcth on the shear stress as also on the deforma-
tion rate� The solutions containing dibutylphthalate acquil'ed plastioal
consistence with an increase in the dibutylphthalate content,. The afore-
mentioned dependences are, in this case, not linear but exponential. The
coefficient of optical activity ~- (Vw = A~U; A'n - amount of the double
refraction of light, ~ - shear stress) is in the case of !O to 35~ ethyl
cellulose solutions practically independent of the concentration, and is
between 5_7.104 Brewster: W decreases with an increasing dibutylphthalate
content in the mixture, as well a~ with decreasing temperature.. Among
others, a paper by G. V~ Vinogradov and V. N. Manin is mentioned. There
are 5 figures, 1 table, and 13 references: 1! Soviet, 1 US, and I German,

ASSOCIATION: Institut fiziki emli im~ O~ Yu,~ Shmidta Moskva (Institute
of Geophysics imeni

SUBMITTED: April 19, 1959
Card

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GZOV'SKIY, M.V'.; OH0][INA. D.N.
Model stuc~ of theological processes in soltds, with stress
determ[natio~ by oottc~i polar~zationo ~o11. zhur. 22
no. 5',:560-568 8-0 ;60. (MLRI 13:10)

1. ln,~titut fiziki zemli AN S3SR ~m. O.Yu.3hmtdta.
(Deformations (Mechauics)) (Rheology)

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~'.dfj,~:;!~!.~.T ~-t .q, ;i'; ~? ~';~-.~.JJ"F~:~l~,~ ~J' ~ t~i~i~':.~: -t.' ~: ,: ~li~lill~ ['~S~.~tJll.~*ll~',;~'lm'l~':r~'~''*~'~''~-' .... ' ....

PETRUSHE~SKI�, B. A., geblog; BELOUSOV, V. V., geolog; GZOVSKIY, M. V., geolg;
GO~OHEV, A. V., geolog; KIRILLOVA, I. V., geolog; KRE,~OV, V.
geolog; RASTVSROVA, V. A., ~eolog; REZANOV, I. A., gsO~og; SORSKIY,
A. A.., geolog.
Geolo'gic principles of seismis division into districts. S%udii
as~ron seismol 6 no'2:181-186~ '61.

1. Institut fiz~ki Zem%~i AN SSSR.

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D363/ 07

X.TiTLE: ' Problems of magnetism and tectonic physics
abstract 3G7 (In .Collecti�n: Vopr. " -
~ SSSR, 1962~ 297-518)
A discussion is give~ of the tecto~ co~dition~ of
: tectonic ~a~a the caus~s
T]~T: , _ cossider~ Lrom. binatlon, bflmag"
= 'on of u~a~a, inz ~ the co~l~ -
-he zo~tz _,, -sure exam ~ .~ -t of thc Lo ..
the cha~e_ of ~_ , 'e~nts a~d e?tz~a~ ~{~_ ~k v~-zous ma~mas:_
--,4~m ~.~th. tectu~zc ~ov .~_ ~,,~ ~ t~e ~o~u~u~ ~ - most bas;kc
~--'i ........ A~ ~ ol-essuru =~o .. . sho~ed that for .

A theore~%c~s~=~ ..... e pressure
mamas the loweri~ of st~roundi~ this factor plays
their fo~ion ~l~le in most cases of acid magmas
conda~ pa~. ~e.l.ysia of cxisti~ ma~-~ -__., .~ation o~
a se .... ~Z cn~ection ~z~een tectonic mov~ts ~ ~
to deep physical and chem-
magma. >Io~t ~eetonie motions ~e relatea
.... �

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L~ I~,,~I~ i;'.l::',~!i'yy .~t � .':]!,~-:it~N"?~ ;I~! !l::'. ;: I~~t ~ : q'itllU

D26~/DS07 i :
Problems of magmatism ....
� bcrustal ].ayer,ialth�u~h: in some.'
� .. roceedzn~ zn the su snondi sa~.gz~
~ reactzons, P . ses corse , ng ... :
.ca~ . - f m wa can e~

~ ~�~n o� t~.e martb's surf. au,~. .~-[,~,..~�e�~t.,~ is tzecessary for' ~t~e
~mbination of. physzcal aua cnemzcaz ~ .... am ....
tectonic movements pIa2 important but not a

formation of magma~
critical part',. (99 references).
~-AbstraCter!s note: Complete translation_/

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Ii~'~,i~,~[ il~t;:l;~ ,{~:':f! ~1 ~! ;1- ; :;~' ~i-i~ ::~ ;~1' i :::1 ;*~ " { , ;!:l!ii '~IE3iI:[~J~H~:If~E~! ~li'.U:~l~'lr~t"''?'' ' :'''' ' " '

GZOVSKIY ~ M.�'.
Role of tectonics in the origin of magma of various compositions.
Biul. ~IP. Otd.geol. 37 nee3:122 My-Je '62. (MIR~ 15:10)

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OSOKINA, Doi'ial~ra Nlkolayovna; ~j~.~SKI~v~M~V~r-otv. ~od. 4
MIL;.~,R, Yu.G., red.; ~D~, V.~., red. izd-va; ~LINA,
YuoV., ~ekhno red.

[Plastic -~ elastic lo~-module optically-ac~iw materials
for studying stresses in the earth'e crus~ by the modeling
metho~i~ Plastichr~e i uprugie nizkomodul'~ye op~icheski-
aktiw~ye materialy dlia issledovaniia r~apriazhenii v zem-
noi ko~e metodom modelirovaniia. Moskva, Izd-vo ~d~ SSSR,
1963. 195 p. (~tIRA 17:1)

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qZ~'S'-~-'~"~6-I~O~�-~iNA, T.V., red. i~.d-va; A~'I'~ ~.-a, .... , ~
red.
[~sic p~blems in the tectonophysics ~d tectonics of ~he
~ydzhansay anticline] Osno~e vop~sy tekto~o5i~i~ i tekto~ka
~id.~nskaisko~o antiklino~ila. ~osk~, Izd-vo ~ SSSR. ~s.~-
(~ ~6~0)
1963. 543 p.
1. C~en-korrespondent AN SSSR (~o~ ~lousov). (Xaratau--Geology, St~ctu~)

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~Peb'-'~OW:' "-:':. ;'- : . '.4 i:~! ! -;: : :, i i::':~;:~.: ,'..
~cEsSI0.-~: ATqO~225- '-- ..:': ... ;. s/O000/6~/O00LOOO/~OS8/O0.77 / ,: .
- : - .. :~ ;.-.._:...'.~ ,: ;H ;'.~ .. ................
'" � ' :''. ' ' ' - ' '-. 'J. ' . : ' :' : - ~: :,'." : :I i: '.L -:':,;;.

' A tect0no-h'sical co. arisen'of recen.~-~tonl~ m~en~s'~s~. . i; ~ '- ' ''
TIT'~E. ' . P Y: � . '. .. ' ~, "L" � thin the'.;'~-
seism~clty, gravitational an~al~es, magmat~sm and deep proc~sses~!. : : : ~-, -

limits of-.the SSSR .: .~ . . .'. ~ :: . -: ~ - ':~: ~. ~,: .. :"~"'::
~ - . . - : .::_ - . .' . . - ' _ ::... : ::.:~ :- ~ .:~ ~.~ .' t'} ~: ~ '
0uRCE: Vsesoyuznoye tektonlchesk0~e sOve'shc~aniye;': 2d,--Dush~nb~; :1962, i .
nov~YghiYe':tekt~nl~He~iYe ~d~izhenlS zemn'oy ~ry*, ~= --- ' ya{ t.'
Akt i vl zi rovanny*ye- Z�n~:~
--' -~ .... 'h~s crust latest :tectOni~ ~ov~en~t� .~:~ - -
seysmichnost~ (Activ~ated zones o~ ~.u ~ ...... : : ...... i
, � y,~..soveShchaniYa.:: HOsco~;. Izd-vo~Nauka, 196h,;58-7~71
an~ seismicity); material - ... � .... ...... :' - ~ -
TOPIC TAGS: Heogenei-~uaternary ~v~ent, _tect0n?phxsi~ Lmz~en~:,~'_~}~.~c~ ~v~.
� - ~msostatic~v~ent, earthquake Focus~' iana uplitt :~aEe~. ear~~.-
ment~ ant . . ' . :. : ~ .:': A

'~ 'An att~pt has been made tO' pro~e -that' the i01u~i:on of ;v:,arious 'anSi,near..
ABST~ : '. ' . - � ''- ..... (~:'nc-0~ ~bai'thqua~es I
' -. "~ ::~ -~ .... diction of the .force and freq ~ y . j
~ g P ' ' :;houid be based on. the physlcal -lnterpr~t;ation~O[ !:ecco~l~[;~-~
a articular area, t, - � d" e~lOn:' the
~e~ts. The fol~i~in9 c~parisons are discussed in th~s.,c~n . ~ ,
~ion of the 9e�logi~ai ~v~ents ~i~h Lhe resUit~ of abyssa~ ~seis~hi~ ~soUndip~s,
~ard/z~hel~rLical and ho~-izontal: speed~ .�f such '~v~ents, the ~l~pse ra~~e ,and ~he~:

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L 17585,65 ' ;-~
J~CCESSIOIq NR:. ATt~O/~3225 - ' : ' ' ' :ii i; ' '
; spatial 'distribution of earthquake !foci, etc. The uplift ra~;, o~ the~latest
"- : merits within, the ~er~ricory-of the. S~SR.ls'onlY 0.25 m/yea~ ~[es an auerage
30-milllon year periled). -The lapse-~ate dist~ibU[i�n ~f':th~lat~qt~vertic~t}
ments in the SSSR as a whole appears to conform tO the seismic zoq~qg ~maPs
earthquake ep~cente~ maps c~ptled by the AN SSSR..The m~O~'lty
porary abyssal fracture zones are'.s~eeply Inclined (60+7~ahd mo~e), :ext'endihg~
~uch deeper than the base of: the eairth's crust. [nasmuch'~g the :~a~th'S cru�~.
~ [sostat[c, It Is assumed that the Convor~enco. rate:o~ th~}upl!fg and
- of the ~rth~s crus~ is at' lea~t. the same a~'~he.hl~he*t'lOp~e ra~e:}of
ment c~ onent, 'A d~ arisen'of t'eetonic.~vemeh~s ulth~ma~n~tid~��easses :r~vea~18'
that the relationship between~th~ is'paragenetic~and not:me?ely causative.
currently ~o~n geological and geophysical ~acts ~upport. t[e:.hypoghes!s:that.:.
- "phYsic6chemical 't'ransformatlon~of matter-~n-the upper mantte~-'Of ~e~*earth
' major- Cause of tectonic movements. The'average up ll ft ~:rate ~t: .'tfi~:~ i~alth's '~r~
must be related to the gr~ing cru~:~l thlckneS~ produced b~[:~he~a~e~lon:
qu~ntlt,e- : . ~ :~ . ~.~ .....
acld igneous rock-.to the crust.~'Or~g=.'art~: has.::
creasing
bared formulas, 6 figures and one table. : ":=: ~ : ......
ASSOCIATION: none
SUBHITTED:
Ca'rd ~/~ NO REF S(~V: 055'

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GZOVS~IY, S.Ys.., l,mncl, tekhn, nauk

Kinematics of ~he stream iurtng the mixing of the liquid b7
radial blade impellers. Ehim. mash. no.6:13-20 NvD '%9.

(Nixing) (Hyd. r odznamics )

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GZOVSKIY, ~,�a~; PLANO�SKIY,

Invsstigatin& mass transfer in the solution of the solid phase

(Nasa transfer) (Solution (Ohe~istry))

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ll~:.;l:~' ~*f,I,~; -*"~ ' ': ~ " ~ t ~. ! ~! !~ '1~!:'

gotor~lning ~t~eaees and angles of arr~ngemen~ of drivin~ ~nd
~upportin~ guidinE roller~ of ball mills havln~ fric~ion drives.
Trttdy MIKHM 14:3-18 '~7. (MIRA 11:9)
(0rushing machinery)

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~ ';' 5 :; ~'~:q'' " ! '~:11: 'q!!' tlt~;~l ~lJt~t~'~l~illi~g~l

GZOMSKIY, S.Ya,~, kanci.~ekhn.n~uk

HydrodFnamics of the flowing stream during the nixing of
liquids by radial flow paddle impellers. ]Dnim.m~sh. no.l:
17-20 Ja '60. (~([RA 13:5)

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DIN VEY [Tin~ Wei]I_GzOV~KIY, S..Ya.; PLANOVSKIY, A.N.

Sttu~y of the kinetics of solution duri.ng m~xing by mechanical
mi~:erso Khim. prom. no.4,286-292 Ap 'o3, (MIRA 1618)

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i

/ ,l, method for me~,surlng the mobility o! lone In dielectric
tlqttlds. ~L~and Jozef Terl~kl (Odansk Eng.
CdJ., ~oland). ~lda Phys. Pdon. 18. 191-8
(lgSO~in gnglish); cf. CA 32, ~7a.~A methml is de-
~ri~ for me~uring mobility of cu.ent carriers in diel~.
liquids. A pl~ne of Ions Is prmluced In the liquid by x-
re}s. A volta~ is appll~ to 2 d~tt~es in the ilquM,
O~:liloKmms ~ the voltap-tl~ cun'e aet~ a con.
d~in ~ri~ wi~ the ~ll, and from this, the time fm to~
to move to the el~t~e Is detd. The m~lllty ~ is calcd,
Iram the ~htlon; ~ - ~(V/d}, whKe ~ h the vd~lty, g
th~ v~tnlc acm~ the cell, aM d the dhtan~ ~tw~n t~
elec~, gm hexane, the m~cd m~llit~l ~
~ - 4.1 x 10-e~.cm./v.~. and~ - 1,3 X 10'~.

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GZOWSKI, J.

Complaints and grievances, p. 3.

ROL~,IIK SPOKDZi/~,GA. (Ocntrala Rolniczej Spo!kzielni "Sm,~popomoc Chl�pska'')
Warszawa, Poland. Vol. 8, no. h3, Oct. 1~55.

~Bnthly list of East European Accessions (EEAI) LC, VOL. 9, no. 2, Feb. 1960

Uncl o

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GZRF,~D^LA, J.
~eeut~on or t,r~e Pl.~n ~n mn~t im~-~rt.~nt technical ~r~ eenn~m~e ~te!d~ .~n the
tst half' oe 19~;]. n_. ~k.
SO: Mont, h].v L~t. o.~ E~.~t, F, urcre.~n Acces.~en$, (ZEALS, LC, vo~, ], No. 17, Dec.
195~, Uncl.

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T~RLEGKI, Jo~ef~ dr. tnz.; FIG%~q, Jan, mgr. inz.; GZOWSKI, Olgierd, dr.
A fire alarm system based on radioactive isotopes. Bud okretowe
Wars~a 7 no.7~228-231 J1 '62.

1. Polit~clmika, Gd~n~k.

CZA-RDP86-00513R000617810004-4

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;~' I".:~['?'~ J?::-fi:~;.~t I ~!: ! ~ ! '! Ti:II:

GZULYA, F. I_._.,~.spirant

Pathonorphology and pathogenesis of grave forms of Botkin's
disease. Zclrav.~zakh. 17 no.10/ll: ??-?9 '57. (MIIIA 12:6)

1. Iz }~fe~rypatologichesko� anatomii Kazakhskogo gosudar-
stvennogo instituta.
(H~PATITIS, IliI~0TIOU~) (AI~iOI~--PHTSIOI~GXCdLLIg~FIICT)

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� ?~ 'i :";:'E~ ~: !i.'--!.ql'i 'El ~ ' ~ ~ " I I~17:

8}[AKIMOVA~ BoSh.; GZULY. A~ F..Io -~ !~"

Itsenko-Cushing disease with plu~lglandular insufficiency. Zdrav.
Kazakh. 21 no.2:28-32 '61. (MIRA 14:3)

1o Iz kafedry gospital'noy terapli l~av. - dotsent R.A.Satpayevm)
i kafedry patologicheskoy anatomii %zav. - pro�essor PoP.0chkur)
Kazakhskogo meditsinskogo institu~a.
(CUSHING SlgmROME) (DEFICIENCY DISEASES)
(E mOC Ns Om ,S)

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! ! ''L ~ ';! '~':~t I ; ! ~ T!II ~l~;' i!l~'~J~i'

CTA-RDP86-00513R000617810004-4

IBRAYEV, Sh.Z., kand.med,nauk; GZULYA, F.I.

Case of typhoid fever in a child of 4 months.
no. 4:79-81 '61.

Zdrav. Kazakh. 21
(~a~i ~:4)

1. Iz kafedr detskikh bolezney i patologicheskoy anatomii Kazakhskogo
medits'~mkogo instituta.
(TYPHOID FEVER)

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IBRAYEV, Sh.Z.., ka_~t_.med.nauk; GZULYA, F.I.

Case of cirrhosis of the liver in au infant.
21 no.12:55-57 '61.

Zdrav. kazakh.
(~A 15:3)

1. Zz kafedr detskikh bolezney i patologicheskoy amatomii
Kaza~skogo meditsinskogo instituta.
(~w~--cmm~)

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KATSrUB~, K.A.; GZULYAs F.I.

Hepato-c~rebral dystrophy in children. Zdrav. ~akh. 23 no.~:
61-64 '63. (MI~ 17: 5)

1. Iz n~vrologich~.skogo otde.leniya I det~koy kl~ni,:he~koy b.!'nitsy
i kafed~y p~to!ogl~h~,~koy anatom�i Aim.,~-lt[nskog,:, ,~:,ii l.s!m,.~ogo
ins titu t a.

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ee ~i

CTA-RDP86-00513R000617810004-4

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 "APPROVED FOR RELEASE:
~, '[~"1 ~.' ~-~ '~ i I !'~ J i~': q-"!l~ i :1 : '

09/17/2001

Electrical Eugineering Abet.
Vol. 57 ~�,. 675
Mar. 1954
Electrical Engineering

C1'A-RDP86-00513R000617810004-4

621.313.17-004-5
.~ ,. ---.--~.,,J II.V. oI'ef'~
' tn~k~on lin~. t. ~-,,~ , M~K0

AND ~- ~OMIA~SKI- ~cr~c,]- , ' ,

0953) fn Polish. 's oF a few p~i~ ~th~s-
~ tlon is gt .eh -
tX dc~'P - -~,-tr t~mi~ton hn~
operating at ~oltag~ up lo I lO kY for t~ting
~nsion and pin-l~ insulator,
tact {m~ista~ of ~ndt