SCIENTIFIC ABSTRACT PETRUSHEVSKIY, B. A. - PETRUSHEVSKIY, S. A.

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• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

PETRUSIEVIA 1Y, B. A. Doc ~eolog-jlineralog 3ci
Dissertation: Ilh-Lstory of the Development of the Vral-3iberian %pi-
Hereynian Stage During the Mesozoic an-i Cenozoic Eras.
10 June 49
Inst of Geological 3ciences, Acad -,ci U.
CNO F f, r, I
C-1-jr-" M031kva
(y lyl
Sum 71

FMUSHIVSKIT. B.A.
-
Mesozoic and Cewsolc structure of the West Siberian nals.
Biul. MOIP. Otd. geol. 26 no.4:3-40 '51. (K= 11:5)
(Vest Siberian Plain-Geolog7)

USSR/Geophysics Seismic classification FD-758
Card 1/1 Pub 44-6/11
Author Belousov, V. V.; Gorshkov, G. Ts.; Petrushevskiy, B. A.
Title Concerning I. Ye. Guvin's article "Seismic regionalization of
southwest Turkmenia"
Periodical Izv. AN SSSR, Ser. geofiz., 443-450, Sep-Oct 1954
Abstract Discuss recent statements of I. Ye. Gubin concerning his proposed so-
called seismotectonic method of seismic classification of regions.
Establish that these statements are but slightly connected with the
author's earlier remarks on the given problem. Show that it is im-
possible to talk about the existence of a new seismotectonic "method."
Eleven references, all USSR (6 by Gubin, and the rest by V. V. Belousov,
G. P. Gorshkov, and Ye. F. Savarenskiy).
Institution Geophysics Institute, Acad. Sci. USSR
Submitted April 12, 1954

PE-TaH,Ss It It tt,'%'S 1-7. 1 Y ,A. 1,r) 1c, I
USSR/Geophysics Seismogeological characteristics
Card 1/1
Author Petrushevskiy, B. A., Rezanov, 1. A., Rastvorova, V A.
Title Seismogeological charac,~eristics of western Turkmnia
Periodical Izv- AN SSSR, Ser. geofiz. 2, 160-18.), Mar/Apr 195L
Abstract Consider the structure of western Turkinenia and its seismicIty, an-J
to explain the various seismic interrelationships Arrive at the
that the west Kopet-Dag is characterized less by high degree of seismi il-y
than the regions adjacent to it on the west and east. Twenty-fivx-
ences, all Soviet, including A. A. Shreyder, "Basic results of
geophysical survey of the western part of Central Asia," PrikladnaYs Gee-
fizika (Applied Geophysics), No 4, 1943.
Institution Geophysics Insti,-ute, Acad .;c~ USSR
Submitted March 11, 195---

laOPOTKD:' F.!!., rtv. red.; BELOUSOV, V.V., red.;
N.A., red.; LiGGLAINU,', A.A., rec.; %L'ETSKI'.,*,
GU- BD' , I.Ye. , red. ; LE', E-, A.!-. , red. ; MAZA:-CVICT;, O.A.
red. ; MbFIATOV, V.V. , red. ; I IKOLAYEV, N.I. , red. ;
F-A~~LOVSKF.', Ye.V., red.; FEYVE, A.V., red.; FEll,,LSll-l;I:.-J.Kz.1
A. -, red.; TUSKI:k~OV.-rTY~ Yu.:..,
.e0.; IN'.A., red.; vOISHIN, A.L., red.
F
LS*-n-.cture anr3 the development of the ea-r-this cr-usl '
materials! Stroenie i razvitie z~-mnoi kory; maLevial":.. '.':o-
skva, Nauka, 196,,. 199 (MI,-~A 18:2)
1. Vseso-.-uznoye soveshchanie po problemarn tektonilri.
1-~O:~Cow' 1~-)( 3.

PETRUSHEVSKIY, B.A.
Pacific m7ving ring. -'cv. ge~~-'. - nc-':3-2? Mr ',,4.
I X7 % ; d
1 .4, ~A , -:1-
1. ~nstlltut, fiZAK'- I~Vrlili iM. C.YU. --Imidta AN SSSR.

PMUSHEVSKIT, B.A.; REWOV, I.A.; RASTVOROVA, V.A.; LIONOT. N.N.
Tectonics of western Tarkmenia. Biul.NOIP. Otd.geol. 29 n0-4:3-35
JI-Ag 154. (MLRA 7:9)
(Tarkmenistan-Geology, Structural) (G*ology. Structural-
Turkmenistan)

PETRUSIMSKIL B.A.; -YABSHIN, A.L., redaktor; MIZAK(N. I.A., redaktor;
AMMENYWA, T.Y., tekhnicheskiy redaktor.
[Uralo-Siberian api-Hercynian platform and Tsien-Shan; history
of development in Mesozoic and Cenozoic times and problems of
seismicity] Uralo-SibirskAia spigertsinskala platforma i Tian'-
Shan'; istoriia razvitiia v mezozoiskoe i kainozoiskoe vremia I
voprosy seismichnosti. Moskva, Izd-vo Akademil nauk SSSR, 1955.
551 P. (KLRA 9:4)
(Siberian platform--Geology) (Tien Shan--Geology)

PBMSMSKff. B.A. BRIDUSOV. V.V., rodaktor; RXZAMV, I.A., redaktor;
10 AINKOUTiLl- T.W., tekknicheskly redaktore
Significance of geological phenomena in the division of a region
into seismic zones. Trudy Geofiz. inst. no.2813-58 155.
(Geology, Structural) (Seismology) (KUU 8-5)

PATRUSHUSKIT. B.A.; TAIISHIV, A. L.
- - e. &-I
---'-=f ~erenc"a on tectonics in Baku. Biul.140IP.Otd.gool. 30 no.2:116-11)3
Mr-Ap 155. (MIRA 8: 8)
(Baku--Geology, Structural)

- i
PRMUSHNSKIT.B.A.
Mesozoic and Cenozoic struct-ure and hostor7 of development of the
Ural-Siberian opt-Hercynian platform and Tien Shan. Blul.MOIF. Otd.
geol.30 no-3:17-38 vf--Je'55. (MIRA 8:10)
(Tien Shan--Folds (Geology)) (Siberia--Folds (Geology))

PETRUSHRVSKIY_ B,A.
-
Relation of seismic phenomena in the Ural-Siberian Platform an:!
Tien Shan to the geological conditions of these regions. Bi;.!.
MOIF.Otd.gool.30 no.6:31-53 N-D 955. (MLRA 9:4)
(Kazakhstan--SeIsmol*gy) (Tien Shan--Seismology)

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AUTHOR: Petrushevskiy, B.A 5-5-4/6
TITLEt Some Current Problems of Seismic Geology (0 nekotorykh teku-
shchikh zadachakh seyamo-geologil)
PERIODICAL: By-ulleten' Moskovskogo Obshchestva Ispytateley Prirody, Otdel
Geologicheskiy, 1957,* No 5, pp 99-125 (USSR)
ABSTRAM The author sets forth his conceptions on the connection be-
tween geologic and seismic phenomena, basing it on the fact
that seismic phenomena and various large-scale structural
complexes on the Earth's surface are the results of abyssal
processes. The contemporary abyssal processes are in most
cases manifestations of the trends which have been character-
istic for a given region during the preceding span of time,
which was sometimes rather long. Thus, a genetic connection
can be established between the seismic events which repre-
sent consequences of recent abyssal processes on the one
hand, and the large-scale structural surface complexes which
also represent consequences of abyssal processes proceeding
during considerably longer times, on the other hand. How-
ever, connections between the Seismic and geological situ-
ations are rather complicated, the intricacy of the proces-
Card 1/6 ses causing the differences in the geological structures of

5-5-4/6
Some Current Problems of Seismic Geology
various regions. In some cases the geological peculiarities,
with which the intensification of seismic activity is con-
nected, consist of the presence of those zones which link
large structural complexes with different build-ups and
movements. In other cases, these geological peculiarities
consist of the tectonic mobility of a given region, which
characterizes its development during a very long geologic
time. Still in other cases, geological peculiarities con-
8ist of the combination of their low mobility in the past
with the high intensity of movements at the present time.
All these cases pertain to the regions related to plateaus
with Pre-Me8ozoic folded foundations. On the territories of
the Alpine folding in the Southern USSR, the seismic act-
ivity is connected with other geologic peculiarities. Above
all, the zones of recent, Pliocene-Quaternary volcanism in
the Caucasus must be mentioned. Then, there is a connection
between the high seismic activity and the zones of intensely
developing Quaternary depressions superimposed upon the
elevation$ of the preceding stage of development. There is
also a group of earthquakes associated with the zones of the
Card 2/6 largest transverse elevations. Movements resulting in the

Some Current Problems of Seismic Geology 5-5-4/6
formation of folds in regions not affected previously by
folding are of importance for the intensification of seismic
activity. Thus, both for the plateau structures and for the
Alpips folded.-zone of the Southern USSR, seiamic phenomena
are connected with various geological peculiarities which in
the most cases have one or another reflection on the surface
of the Earth. It is probable that seismic-geological con-
nections in the Far East are characterized by a still differ-
ent special type or types. Following the ideas of G.A. Gam-
burtsev, who started investigations in the Geophysical In-
stitute for establishing geological criteria of seismicity,
the author proposes some general concepts of his own. He
considers seismic phenomena as a reflection of contemporary
(in the literal sense of this word) tectonic developments of
a given area. For the Urals-Siberian region the author de-
rived the following regularity: the younger the age of fold-
ing of the foundation is in a given area, the oftener occur
in this area movements leading to activation of seismic act-
ivity. The second regularity found is formulated as follows:
the intensification of seismicity is usually observed in the
areas in which recent intensive movements lead to the form-
Card 316 ation of active elevations (anticlines) of relatively small

Some Current Problems of Seismic Geology 5-5-4/6
size and of conjugated active and equivalent scale ainklngB
(synclines). In the areas of unidirectional elevations,
although very considerable in extent of lifting, the seism-
icity is somewhat weakened. For the region of the Caucasus
the author formulates the following conclusions the great-
est seismic activity is characteristic for the zones which
suffered multiple reconstructions of the tectonic structure,
and moreover, the highest intensity of seismicity occurs in
the areas where this reconstruction took place only recently.
The seismic activity of the Turkmen-Caucasian section of'the
Alpine folded region is connected with the zones of the most
recent activation of tectonic movements. The author con-
cludes that regularities of connections between seismic and
geological events are different in different zones which can
be classified into 3 large groups;
1. The Alpine folded zone of the Southern USSR,
2. The plateaus, and
3. Those portions of the former plateaus which have been
reconstructed (and continue to suffer reconstruction) as a
result of manifestations of very intense tectonic movements.
It is probable that the greatest earthquakes arise just in
Card 4/6 these regions. In the regions whose structure considerably

Some Current Problems of Seismic Geology 5-5-4,'6
differs from these groups, such as the Pacific ring and modern
synclinal regions, geological criteria of seismicity may be
characterized by some new, still unknown properties. The
author evaluates M.V. Gzovskiyls fRef. 11, 122 highly poe4t_
ive,new,physico-mathematical approach about the seismo-geo-
logical phenomena. The author discusses a possible depend-
ence between earthquakes of maximum intensity and geological
factors, and comes to the following conclusioni that the
maximum intensity of earthquakes occurs in the reconst-ructed
plateaus, followod by the Alpine folded zone, and the 'Lowest
intensity has earthquakes in the recent plateaus. Here the
maximum is understood on the average. The absolute maxima
of earthquake intensity in the Alpine folded zone and in the
reconstructed plateaus are almost equal, but their frequency
in reconstructed plateaus is higher. The author cites the
map of epicenters of the earth akes in Asia compiled by Gu-
tenberg and Richter LRef. 50:rand finds there the confirm-
ation of his theoretical results. The author recommends the
method of historico-structural analysis for investigating
seismo-geological correlations which should be supplemented
Card 5/6 with sei8mic-statistical data.

Some Current Problems of Seismic Geology 5-5-4/6
The article contains 2 maps, 2 tables and 50 references, 46
of which are Russian,and 4 in English (us)
AVAILABLE: Library of Congress
Card 6/6

AUTHOR: Petrushevsedy, B.A.
TITLE: Conference on Dividing Central Asia :ntc Te-t~r.--
Held in Tashkent (Scveshcnaniye
vaniyu Sredney Azii v Tashkente)
PERIODICAL: Izvestiya Akademii Nauk SSSR, Seriya 3eologJ1chesxaya,
1, PP 107-109 (USSR)
ABSTRACT: A conference held in Tashkent from 1114 May to 1~3 May
dealt with the task of dividing Central Asia into tectonic:
districts. The chief task of the conference was to compare
the available opinions on this question with the u:timate
aim of preparing a scheme which could be used as a relia'--
basis for the preparation of metallogenetic an! progn3sti--
maps. The conference was attended by numer~,us
ganizatlons of the foliowing Central Asian re,--n.ics: A--~u-
demies of Sciences of Uzbeki s tan,T&dzhjkjs tan Kirgizia, "'Li-
zakhstan, organizations "Sredazneft" and "Turkmenneft', !,.a
trusts "Sredaznefterazvedka", "Sredazneftegerfzika" ani
others. To coordinate the efforts of ge(,logiLits
ent republics was one of the principa, suhliect3 ,f the ~ n-
ference. Although the ultimate goal of the conference, t!.e
Card 1,12 establishment of a certain scheme of divid;.r.g central Asa

Conference cn Dividing ~-entra.' As-'a Tectonic :J,stricts
into tectonic districts could not be achieved, it ~aveJ t.,.e
road for such an undertaking. One of the most 4mportant
lectures was held by Professor V.1. Po~ov, of tne UzL-ee, A-a-
demy of Sciences. Other lectures were held b~- Ya..N.
coworker of the Scientific Research Institute of Apiliei
logy (N1IPG) , B.B. Tal ' -Virokly, B.S. Vol 'V0V9K1.y , k A.
Ryzhkov of the Uzbek Academy of Sciences, Prrfessor D.i.
Rezviy, L.G. Zhukovskiy, V.G. Korolev and F.T. kas-irlna
the Kirgiz Academy of Sciences, S.A. Saknarov and M.M.
Kuktikov of the Talzhix Academy of' Sciences &r,!
AVAILABLE: Library of Congress
Card 212

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a r

AUTHOR: Petrushevskiy, B.A.,
TlTLEi To the Probl em of the Trarisl ) teration of
Names in Central Asia and Kazaehstan (K vuf.rosu o trans~rf-
tsii rnestnykh geograt'icheskikh nazvaniy v 3redney Azii
zakhstane)
PERJODlCAL: Izvestiya Vsesoyuzriogo Geograficheskogo Qbshchestva,
Vol 90, Nr ", pp 18') - 186 (U,*)SH)
ABSTRACT: The author criticizes irregularities in the transliteration ol
Central Asiatic and Kazakhstan names in the great "Norlt MaT-
published recently. ne quotes various examples and
the eliminating of these deficiencies by the Seographa7~I_
Society.
AVAILABLE;: Library of ~'on6ress
Card 1/1 1. Cartography-Determination

GORTACHEV, Arkadiy Vasil'yevich-, PETRUSHBVSKIT, B.A. I.otv.red.; KELINI-
-va: - _
KOVA, N.B., red.izd V., to red.
(Mesozoic and Cenozoic structurea, tectonic development, and
seismicity of I-eke lasyk-Kull region] Me20ZOisko-kainozoinkais
struktura, istoriia tektonichealcogo razvitila i seiemichnost'
raiona otera Issyk-Kul'. Moskva, lid-vo Akad.nauk =R, 1959.
178 p. (MIRA 12:11)
Ussyk-Kull region-Goology)

RZZANOV, I.A.; RTRTT5" A tv.red.; KUN. N.R., red.izd-va;
!&ELI* te khn. red.
AVROV, A.V., -edjzlL_V=8&;'5FP5TAFIT3VA, G.A.,
[Tectonic pattern and seismicity of the Turkmen-Khurnann
Ranges] Tektonika i seismichnost' Turkmono-Khorasanskikh gor.
Moskva, Izd-vo Akad.nauk SSSR, 1959. 243 p. (MIRA 12:12)
(Turkmen-Khorasan Rnnges-Geology, Structural)
(Turkmen-Khorasan Rangos--Seismic waves)

S/5l9/60/OO0/0G8/,02/'G51
D051/Dll3
AUTHOR: Petrushevskly, B.A.
TITLE: The association between earthquakes of maximum intensity and
the geological environment
Akademiya nauk SSSR. Sovet po seysmologii. By-ulleten,,
no. 8, Moscow, 1960, Voprosy seysmicheskogo rayonirovanlyti,
28-35
TEXT~ In a previous paper (Ref- 5: B.A. Petrushevskiy, 0 nekotorykh te-
kushchik.h zadachakh seysmo-geologii [some immediate tasks of seismic eeo-
logy]. Byull. MoBk. ob-va isp. pri.r., otd. geologii, no. 5, 1957) the
author outlined three groups of geological criteria of seismicity likely to
help find the association between heavy earthquakes and geological condi-
tions. Without indicating the special features of these groups, he points
out that, for the Western USSR, the regularities of association between
seismic and geological phenomena differ for the following three J.&rge struc-
tural areas% (1) the zone of alpine folding (Caucasus, Turkmeniya); (2) the
areas of recent platforms with a paleozoic folded foundation (Urals, Kyzyl-
Card 1/3

S/519/60/000/008/002/031
The association between earthquakes ... D050113
Kumy), and (3) those sections of platforms of any age of foundation fo~j_qg
which are still undergoing structural changes (Tyan'-Shan'). Comparing the
geological conditions of these regions and the frequency and intensity of
the earthquakes occurring in them, the author concludeB that the alpine
folded zone can be considered as a standard of seismicity, the recent plat-
forms being considerably below this standard, and the transformed platforms
(particularly in sections of early stabilization) a li*,tle above it. Some
asgumptions on the geolugical reusons for this phenomenon are given. A map
and tables are included Illuatrating the distribution and intenalty of
earthquakes in Eurasia from 1897 to 1957, most of the data boing dorived
from American sources. For the indicated period, the most intense aeisoi~_
shocks occurred in the area of transformed platforms. The author mentiGns
N.V. Gzovskiy for his recent efforts to establish the relationship between
the force of earthquakes and the geological environment and Huang io-chlin.
A.D. Arkhange"skiy, and V.V. Belousov in connection with the structural
determination of Tibetan earthquake areas, There are I figure 2 tables,
and 13 references: 8 Soviet-bloc and 5 non-Soviet references The four most
iecent English-language references read as follows- B. Gutenberg, Great
Cazd 2/5

S/5l9/60/:=/OG8/X2 /~.z I
The association between earthquakes ... D050113
Earthquakes 1896-1903, Transazt. Amer. Geophys. Union, 57- no- 5, 1916;
Seismol"cgical note-; Bull. Seism, ~"oc, Amer,-ca, 46. no. 4. 1956, id, 47,
no. 1; 1957~ :Ld. 47 no. 4, 1957.
ASSOCIATION. 1astitut fiziki Zemli AN SSSR kInstitute of 1~h~rsl~s of the
Earth of the AS USSR)
Card 3/3

RE,ZANOV, I.A.: RA~M)ROVA, V.A.; LEOWV, N.N.; Prinimali uchastiye:
AU1)Rh"J_V, S. S. ;'PERIN, Ye. I. ; DORABRWV, A. T. ; KATS, A. Z
KOSMINSKAYA, I.F., LWWV, N.N.; M"SKIT, S.I.; MKOV11M,
B.A.- HCHKOV, S.V.; RASTVQROVA, V.A.-,
nz"Ov, IA.; SAVARE14SKIY, Te.F.; KHARIN, D.A.; Red karty:
GAMBURTSM, G. A.
Betablisbmaut, ofcbtailed seismic regions as exemplified by
a region of western Turkmenistan. Biul. Sov. possism. no.8:
131-141 1~0.! (MIRA 13-10)
1. Institut f~ziki Zemli AN SSSR.
(Turkmenistan---Seismology)

FATEUSHUSKIT, B-A. ___
Selsmogeological characterintice of mountain structures In southern
Siberia arAnorthern Mongolia. Blul. Sov. po seism. no.10:108-120 160.
(MIRA 13:W
1. Institut fiziki Zemll AN SSSR, Moskva.
(Siberia--Seismology) (Mongolia,--Seismology)
(Geology, Stmotural)

YE
Structural position of the Greater Balkhan. Biul. 1401P. Otd.
geol. 35 no. 3:1C5-128 MyJe 16(. (NIF.A 14:2)
(Greater Balkhan Range-Geology, Structural)

PHASE I BOOK EXPLOITATION Sav/5127
Petrusnevskly, Boris Abramovich, Doctor of Mineral Geological Sciences
Zemletryaseniya I vozmozhnosti ikh predskazaniya (Earthquakes and trie Possibility
of Forecasting Them) Moscow, Izd-vo "Znaniye", 1961. 44 p. 22,500 copies
printed. (Series: Vaesoyuznoye obanchestvo po rasprostraneniyu politicheskikh
I nauchnykh znaniy. Seriya XII, 1961. Geologiya I geogrefiya, no. 2)
Ed.; Z.A. Siannik; Tech. Ed.: L.Ye. Atroahchenko.
PURPOSE- This booklet is Intended for the general reader.
COVERAGE: The author discusses in simple language the various types of earth-
quakes and their causes, with special emphasis on tectonic earthquakes. Examples
are giver, of the most powerful earthquakes over a period of several decades, in-
cluding earthquakes causing tsunamis. The cmpilation of seismic regionaliza-
tion maps is also discussed. There are many illustrations in the text, including
.a world map of seismicity. No personalities are mentioned. There are 12 ref-
erences, all Soviet.
C %rd-lft-

GORSHKOV, Georgiy Petrovich; PETRUSHMKIY B.A., doktor geol.-minera.1
nauk, otv.red.; WIKOdRvi~~~~-va; ROMANOV, G.P.,
tekhn.red.
[Problems of seismotectonics and seismic zones of the Union of
Burmal VoproS'y Beismotektoniki i seismicheskoe raionirovania
territorii Birmanskogo Soiuza. Moskva, Izd-vo Akad. nauk SSSR,
1961. 124 p. (Akademiia nauk SSSR. Sovet po seismologii. Biul-
letent, no.12). (MIRA 14:12)
(Burma--Seismology)

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r
turblient
mz~-2 a. V.,
e.,,tAbtL- of fixl~g fl-- i. I-
Tepr-kla=' M. A.,
cretaem-a deposits f
it
tT. -ete- p-t
(S-ttoo VTIX.I)
it It. -f F-b MY-. r- 3'.~' Zt
of the P~clflc bs~&!Z- C
-,the- pet of u.
Z01--lM. L. A-, 1-% i '-. -
brideo rrsa tb& e
rM;rW-Q I-May, ru, .4.,
1. the
d-1c. ror r::M
of
da-slolment of)-. ri-I 1.~ t..
(S..tt- rlt.c Q-,
bott~ ss~ L-et. Ul
I tt, Z-1 i~ J~
3-t-
FTAGW. of- c.t I, A- 5-
31.t, U.;--ty, --Y -
T~. r-*..t,-,, -t.-! r, ~c .
-"kjPQL&. Eh'
LL- Fzrlnlf:~& I.o t!~A northe: , P-t r t.- 0-
the re. p, .6 . ~ (S-L', r.:
3"3DYLE:=. r 0--j.
ih;.ry of f-tl- cf t-m t=;-Tt- rs,- -s
S-tt.. VII.A)
it.
re~-' t, --k~-
XQ_c1"'t ~t".: ~r Ge~ :-2 'P-'-~--
i.. ar. ) -
SHVIIZY, A. E..t 1 t-
Al
;J,t- of the P-:f~ 3, n
SEC. r'; Orr=~:.-L- ~f L-:-!
j~ ce ~t
of h- LU~:s phy ~j ttwlr vny:-.4,
t I
-dt.1- (So
SMH=T, z r.v~ttw-o'
k%'A S__ S-d-
D I)
:1. N. Lnatttote ~' C r --r!~ d,er
. L. tb. -, -4 .- ,, ~.l '-t4
ftciftc Ocommo (S~tion vir.B.5)

LEONOV, hikolay Nikelayevich; FET'-%IJSI:EVSKj7i,-B-"--,otv. red.; N2RAKOVA,
L.V. , red. izd-va; UKAMM-A, I.A., tekhn. red.
(Tectonics and the seismicity of the Pamirs-Altai zoneil Tektonika i
seismichnost' Pafairo-Alaiskoi zony. Moskva, Izd-vo Akad.nauk SSSR,
1961. 162 p. (MIRA 14:1-1)
(Pamirs--Geologj,, Strictural) (Seismoloq )
I I
(Altai Vountair-s- Geology, Structura )

21734
S/026/61 / ~)00/ D03/0
3, ?3ao A166/A127
AUTHOR: Petrushej~~~ Doctor of Geological and
m~inera~ojcal sciences
TITLE: Earthquakes ana their Causes
PERIODI(,',iL. Priroda, no. 3, 1961, 15-2b
TEXT: The articles describes types of earthquakes, tneir
relation to movementb and faults in the earth's crust, the propa-
gation of earth tremors, the 6eographical distribution of eartil-
quakes, the phenomenon of tsu-naiLi, the power liberated by earth-
quakes, the damage they cause and ureasures of protection againSt
them. Much researcia is now being devoted to predictinb the place
and time of possible earthquakes. Seismologists can now predict the
site of an epicenter to an accurancy of' 1 3-5 km. uompreherisive
6eolo6ical and geographic studies in the seiswic regions o1 Lhe
USSR have enabled scientists to indicate the maximum earthquakt
force probable for each particular zone. Each zone is asbigned za
Card '112

21734
0
S/02b/'1/00O/003/003/M,
Earthquakes and their Causes A10--u/A127
ratin6 of 6, 7, 8 or 9 balls Earttiquakes of' a l'orce 61-eater ti.an
9 balls are extremely rare in the USSR, however vaiere an avea is
liable to quakes breater than 9 balls this data is indicated on
seismic maps. The Institut fiziki zemli AN SSSR (InstituLe of Geo-
physics, AS USSR) is compiling a map of the seismic zones in th~
USSR. After government approval the map will become an obli6atory
document for all construction enterprises. The laLter will have to
conform to anti-seismic measures in reinforcing installations unaer
construction to standards established for each of' the 6-9 ball .-a'u--
ings listed on the map. Soviet practice in this respect is now be-
ing followed Ln uhina, Rumania anct Bulgaria. Rcs~,arch on methods of'
pred,Jcting the time of an earth4uake continues. 2here are 4 maps
and 4 photos-
ASSOCIATION: In s t i t 1,1 tf4 ZjK; ZeL!~, 1111. C'~. ~U Sill jUt ( 111SL1 Uj,tf, (i
I I - IL i
Geol,hysics im. 0. Y,,, Shmidt), YloscoA
Card 212

PETRUSHEVSKII.-, B.A-
Tectonic characteristics of the Pamixs, , OU.geol
36 110-4:122-154 J1--A9 -61, (1-:L',A 14:9)
(Pami-ra-Geology, Structural)

REZANOV, I.A.; ZAhUDNYY, 143 MRUSHEVSKIY lbl*AA~otv. red.;
'-'-L , T.V~ -ed.
GALUSPRO, Ya.A,, red. iz~d-vaj-'~ .9 tekhp.. z
(History of epeirOFenic movements in the northeastern part of
the U.S.S.R.] Istoriia kolebatelfnykh talctonichoskikh dvizhenii
Severo-Vostoka SSSR. Moskva, Izd-vo Akad. nauk SSSR, 1962. 173 il.
(MIRA 1~:6)
(Soviet Far East-Earth movements)

GARMSKI-Y, R.G., otv. red.; YA143hlN, A,L. ukacevili, ctv, "O1.;
BEWUSOV) V.V., red.; BELYAYKMIY. N.A., red.; BOGDAJI,~-',,
A.A., red.; GUi,*III, I.Ye., red.;
LEYTES, A.M., red.; MAZA-((jVlCfi, 0,A., red., KURATOV, V,V~,
red.; NIKOLAYEV, N.I., red.; PAVLOVSKIY, Ye.V., red.; ITY17E,
A.V., red.:- PETRU
red PUSHUAROVSKIT , Yu. V..,
red. ; SIIMms Y..M., rA.iSMSYS N.A., rod.
[Young ~Iatforrrs, their Te--tor.ics, axiL prr~spectc 1")r !,,na-
ing oil and gas; materials' Moloiys- platf'C~rry, ikt, t,jet(.n:k~,
i persp(-ktivy neftegaz-riL;sr,(j:Ii; mtkler~a'v.
1965. 223 P. (141:,-A IP.3)
1. Soveshchardye po prc-bieinaz taktci,iki, ~-'c-z-ow, !'~O

PETRU51EUL,
PrinciplP r-f thc- succession of ~Levslopment, vqr--.-q~ = 7--7:r=7--c
the problem of large horizontal ds!-.--;catI, -,na. . ~~-P. ~-- ". -, .
39 no.1-3-Q Ja-,I 164. , V, I R A. 'A q - ". ~
i1a -

MU;iATOV, M.V., otv. red.; PUSHCFW~OVSKIY, ~u.M., red.; KIIAB ,
V.Ye... red.; MAZAROVICH, O.A. . red.; BELOUSOV, V.V.,,
red.; =AYEVSKIY, Ii.A. '. red.; BOGDAIiCV., A.A,, red.;
GARETSKIY, R.G., red.; GUbBi, I.Ye., red.; FROPOTKIN,
P.N., red.; LEYTES, A.M., red.; NIKOIAYEV, N.I.., red.;
PAVIDVSKIYP Ye.V., red.; PEWE, A.V., red.; PETRUSHEVSKIY,
B.A.,. red.; SMNMANN, Yu.M., red",
TAWSM , A.L., red.
[Folded areas of Eurasiq- ma-,er-'alsj Seadchatye oblasti
Evrazii; materialy. Moskva, Nauka: 1964. 375 p.
(MIRA 17tll)
1. Sovesbchaniye po problemam tekt.--,niki. Moscow, 1963.

r'-' 'v. red.
;-t-c .
7ed . i: Iv,Ln'y E;
red .
Y 1'~ A
!lectonic.-, uric I r i tFUI i
r.m air r.; L -.7 4:-
ITJI t.,
1'. !a F
Vc-: W.

i3ELDUSOV, V.V., red.; BELYAYEVSK1' , red.; ;kGDANCT, A.A.,
red.; GA--F'1~21Y, red.; -l*.zl!l*, IT.Ye., red.; K
-.N.j red.; L..-!"ES, A.X., red.;
O.A., rod.; rod.; NiKld.AYEV, red.;
~AVLOV3EIT, Ye.V., red.; A.'-, red.; J-j ENS K I','
~".A. , red. USIT,', Yu--., red. ; Sli:17blXA'1,, Yu.1M.,
red.; li.A., red.; A.L., red.
[IrobJen,; of' the comparative tw,tonic:i . finclont pifltl"ormn;
materitAsi '.oprosy -rr.vi:ite!lnL)i I.ekt.aniki tweirnlkh 1.1atr(fm;
materialv. IlJoskva, Nauka, I'otv.. 152 p. Wl~-,A 17:9)

. -F~~USHEVSKIY , B.A.
[Problems in the geolog-ica-I hiEtory and tector-ics of EaE-,,ern
Asia] Voprosy geologicheskol istorii i tektoniki Vostochnol
Azii. Moskva, lzd-vo "Nauka," 1964. 299 p. (MlRA 17:~j)

-2ZET-RUSHEVSK11. B. A-j geolog; BELOUSOV, V. V., geolog; GWVSKIY, M. V., geolg;
GOIUACHEV, A. V., geolog; KIR-,LLWVA, I. V., geolog; KMTIrIKOV, V. W.
geolog; RASTVCRDVA, V. A., geolog; REZANOV, I. A., geolog; SCIRSKly,
A. A., geolog,
Geologic principles of seismis division Into districts. Studii
astron seismol 6 no.2:181-186 161.
1. Institut fiziki Zemll AN SSSR.

VARSANOF'r,u-VA, V.A.; BOGI)All(,,V, A.A.; KlUZNT,,TSOV, Ys.A.; LANGE, O.K.;
MRKMN) R.L.; P;U.hJ--TOVJ, M.V.; 1-YarLAKOVA, A.I.; PETRUSnVS)MI
B.A-.; SOKOL4DV, D.S.; SHVEnOV, M.S.; YAYEHIN, A.L.-
Nikolai Sergeavich Shatskii. Biul. MOIP. Otd.gool, 16 no.4:
3-6 n-ag 61. (MI-RA 14:9)
(Shatakii, Nikolai Sergeevich, 1895-1960)

RUDICH, Yevgeniy Markovich; otv. red.; MIRAKOVA,
L.V.,, red.izd-va; POISIOVA, T.P.9 tekhn. red.
(Basic characteristic-a of the tectonic development of
Sakhalin, Japan, and the Maritime Territory as the transition
zone froir the continent to the ocean]Osnovnye zakonor.ernosti
tektonocheskogo razvitiia Frimorlia, Sakhalina i IAponii kak
zony perekhoda ot kontinenta k okearm. Moskva, lzd-vo Akad.
nauk SSSR, 1962. 271 p. (MIA 15:11)
(Soviet Far EaEt-Geology, Structural)
(Japan-Geology, Structural)

BYKHOVSK,kYA-Pi*VljOVSKAYK, I.Ye.; PFTIIUSHEVSKIY, G.K. [deceased]
Trematode larvae in fishes of the Soviet Union. Trudy Rov.Ik~,t-
kom. no.9:198-201, 159. (11411RA 13:5)
1. Zoologicheskiy Inatitut Akadomit nauk SSSR i Vnnso3,uzznyy
nauchiio-18aledovatellskiy institut ozernogo I rechnogo rybnogo
kbozyaystva.
(Parasites--Fishes) (Tromatoda) (Larvae--WorriB)

BYKHOVSKAYA-PAVLOVSKAYA, I.Ye.; PETRIISHEVSKIY, G.K.
Distribution of fluke larvae in fishes of the Soviet Union. Paraz.
sbor. 21:14G-202 163. (KIRA 11:4'
1. Zoologicheskiy institut AN SSSR.

STARIKOY, G.M., dotsent, otv.red.; TUDENICH, V.A., prof., red.; OGLOBLIN,
A.A., prof.. zasluzhennyy de7stel' asuld, red.; PATRIAMA. 4.T.,
prof., zooluzherinyy davatel' nauki, red.; ANISIHOYA-ALM-~HMGVA,
VJ., dotsent, red.; MARGOLIN, prof., red.; KAIUATINKO, A.N.,
prof., red.; KISXLL?V, M.S., tokhn.red.
(Forty years of the Smolensk State Medical Institute, 1920-19601
40 let Smolenskomu goaudarstvennomu maditsinskomu inatitutu,
1920-1960 gg. Red.kollegiia: G.M.Starikov i dr. Smolensk. Izd-vo
Smolenskogo goa.med.in-ta. 196o. 189 p. (MIRA 13:7)
1. Faisaia (1917- R.S.F.S.R.) Hiniaterstvo zdrevookhraneniya.
(SHOUNSK-MEDICINN-SMY AND MCHING)

PETUKHOR. R.H.
Economic calculations in determining size. degree of epectali-
sation and dislocation of repair plants. Izv.AB Kazakh.BSR.Ser.
ekon., Mos.1 prava no.2:29-41 159. (KIRA 13:4)
(KiLzakhata,n-Kachinery--Kaintenance and mpair)

PITUK90V, B.S., doktor tekhn. nauk
Contemporary state and perspectives of the development of hA-at
exchange rosearch. TePIDOnorgetiks 6 no.12:)-13 D 159.
(MIRA 1-11:3)
I.Moskovskiy oner eticheeki3r institut.
Mat engineering)

AUTHOR: Petrija~Bv8kiy, iJ,.A_
TITLE: Investigation of the gpiiriii, k' v? in China
PERIODICAL: Izvestiya Akadetnii nauk -~ZSSR Seriya geofizi0it-t5K-i,t
1959~ Nr 12, pp 1729-173d ('US51()
ABSTRACT: A short description of rh(-
in North-West China (Gan sity,sk Corr-)dor) 1.s
the author who, together with D A, Kharin and
N. V. Shebalin of the Institi,te -if Physiza of tit-k-
Earth, Ac.Sc., USSR ' in-ent tr~ Ct.ina as Soviet
tives on 'seismic resf-ay.c-h)Ht~ The general charatm!
the territories descr:.bed :an be seen in thE c!..irt
(Fig 1), which gives the fcllouing Jata
I zone of the Epi-Droterozoiz. Platform
2 Epi-hercynian Platform
3 zone of the Epi-hercyni3n Pla-tforni changrid
high mountain con8riu,li:)n during *ch-a Neogeri-
quaternary Period,
4 transitionary region bevween the Epi-prot~-.
Platform and the high mouritain constr-Acticri
Cardl/2 produced on the Epi-hercvn-an Platfcrm
5 zone of the Upper M(:sozvi,~ fold-.i witl~in ,tic

c
F. I
Investigation of the Seismicity in China
Epi- pro terozoic Plat form wtii.-A-, underwent xt
motions in the Ter'.iarv Period
6 - epicentres of the magriti-(!e M> 7 1/4
7 - M 7 to 7~3,4,
8 - m = to 6Z'4
9 1-1 = 5 t 0 5 Y4.
10 M < 5,
11 approximat e zone o f th e ea r ~ hquak e :,n 'L )1i w I
M 8 ,
12 earthquake in 1954 with M xz~~ 8 - 9
Investigations of this retrior. have been Start-I Ir.
collaboration with Sovtet 5eisai,--logisti-s and ir I!,
that their methods of res.-arch w--11 b,:-come a molt-
seismic work in the rest of China Thanks are
expressed to the Depully DireL-tor .)f' the Instillitf
Geophysics and Meteorology, AC Sc.. China. Chi~n I
to Professors Li. Shan-Pan. Fu Chcn and Se Yuv-m(~ i;1'1
to Professor (if -the-
for organizing the work
Card2/2 There are 1 f igure and 1; . e I f-I ell es 21 of* W h I C 1, ~' I a~
Soviet and 3 English
ASSOCIATION: Akademiya nauk Sz).')R Ill!it-ltut 117,11c1 Zemli
(Ac.sc. , USSR, Institute of Physics of the Earrill
SUBMITTED: May 11t, 199~9

GAIUL, Ye.S., irizb.; PETRUSHEVSKIY., I.N., inzh.
Testing of TV2-100-2 turbogenerators whicb use JLGF-l
automatic field quenching apparatus. Slak.sta- 31
no.407-89 Ap 160. (XIBA 13:7)
(Turbogenerators)

II.-A.,A, , i r.2,. . - t -'K, ', , " - - A , . i -, ., , . . P!, -I ., * ~'V , ,, : --
L . , , . I . I . I . . I . - . . .
-1 )me s ") e . ,I - : t, ;, * i r --~ = : , :.-- . , _. - ~~ , ~ --f- - rt- - - -,- . X - - -_
- t T. - r ) - ~ ~ :- 3 : :- .~ y 7. '.:' . n . , ~,'- :- - ' :1 ~- ' - ~ . ". :11r. r 9 . I F, - - - ~ * -'e),:~ . . - -1 .
n,, . , : . i'i - ~ ') It ~. .0m i R A 1 -4 , '-,

GABA.Te.S., inzh.; PETRUSHEVSKIY. I.N.
Posaibility of vrong oper.tion of directional averload protection.
Elek.sta. 29 no.8:88-90 Ag 158. (MIRA 11: 1-1)
(Blectric networks) (Zlectric circuit breakerB)

(A) ui