SCIENTIFIC ABSTRACT VYALOV, O.S. - VYALOV, O.S.

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• Collection: Scientific Abstracts
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• Original Classification: S
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• Document Creation Date: November 2, 2016
• Document Release Date: September 1, 2001
• Sequence Number: 8
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

MR/Oeolog7 Ileaeontology
Q-- rd iA Bib. 22 - 37/51
Authors I Vyalov) 0. S., Act, '!bT-b. of Lead. St., Ulm SM
Title Hew data on the paleogenic mters from Ushowit
PsriodicO. i Dak. AN SSM 101/5, 921-923, Apr 11, 1955
Abetract Now geological data are presented on paleogenic oywcers diacovered
in Kashgara Genixal Asia. EiW. retemacest 6 MMJ1 I Svedish and
1 French 1,1936-1948).
Institution *,o*o
Oubmitted t December 20,, 1954

VYALOV, O.S., professor; VINGLINSKIT, I.V., nauchnyy votrudnik; OOLBV,
asaistent; GORETSKIY, V.A.. dotijent; GORBACH, L.P.. aspirant;
XUDRIM, L.11., ussiatent; GHLOYAND, X.J[h., redaktor izdstellstva;
MALIAVKO, A.Y., tekhnicheskiy redaktor
[Geological museum of the Iv.7ranko State University of Lvov; a
grief handbook) Goologicheskii muBel Livovskogo gosudarstvannogo
universiteta im. Xv.lrranko; kratkii putevoditelf. [LIvov] 1956.
29 p. (MLRA 9:8)
1. Lvov'.'Univeraytot.
(Lvov University) (Lvov--Geological museums)

VYALOV, O.S.
~
trati&aphy of the Miocene of Transcarpathia. Gool.sbor.[LwoyJ
no.2/3:5-17 156. NLRA 10:3)
1. L'yovskiy gosuniversitat imeni Ivan& Yranko.
(1franscarpathia-Zeolorr, Stratirraphic)

VTAWV, O-S-i PASTEUAK, Sol*
Nov di2coveries of laocer-mus la Transcurpathian flyach. Geol.sboro
[LvovJ no.2/3:203-2" 1569 (MiaA 10:3)
1, Liveyokiy gosunOTersitst imeni Ivan& Iranko (for Vya1ev).2.L1vov-
skiy nauchno-pripodevedcheakiy ruzey AN-USSR (for Pasternak).
(Transearpathia--Lamellibranchiata, Yossil)

VTA10T. 0.S.
In memory of Z.Y.Gorizdre-Kullchitskaia. Geol.sber.[livoyj no.2/3:338-
342 '56. (KM 10: 3)
1. Livovskiy gosunivergitat imeni Ivan Franko,
(Gorizdro-Kullehitakata, Zinaida lFeelctistoyna, 1884-1949)

VYAWV, O.S.
. 1611~ urvey of some new works on the Carpathians and the
Carpathian piedmout. Geol.xbor.LLvovJ no-2 /3:362-370 156.
(MLRA 10:3)
1, LlvoTskir gosuniversitst imeni ITana 7rankoo
(Carpathian Mountains-Beology)

TTALOT, O.S.
Conditions of the formation of the calcitic band In Kimeridgian
deposits of the Izyum region. Xin.sbor. no.10:341-342 156.
(KM 9:12)
Gosuniversitst Iment, Ivans, Franko, L'yov.
(Isyum reg"Lon-Calcite)

VIYAWV, O.S.; VORONOV, P.S.
Geological structare of the Bangor *oasis* In Qmeen Xar7 Land
in the Antarctic. Visnyk AN URSR 27 no.6-.39-42 is 156.
(Antartic regions-Gaology) Wn 9--9)

VY.ALOV. 0.3 -
Faleogene of southaastern Kopet Dagh.Biul.MOIP.Otd.geol. 31 no-15:75-
83,S-0 156. (MLRA 10:3)
(lopet Dagh-Geolog7, Stratigraphic)

14-1-410
Translation from: Referativnny Zhurnal, Geografiya, 1957, Nr 1,
p. 40 (USSR)
AUTHOR: Vyalov, 0. S.
TITLE: Flight over the Dzhungar Depression (Perelet cherez
Dzhungarskuyu vpadinu)
PERIODICAL: Nauk. zap. Llvivsk. un-tu, 1956, Nr 39, pp. 115-127
ABSTRACT., Results of the author's observations made from a plane
flying across the Dzhungar depiession in September 1940
are given. The roundtrip flight was made from Urumchi
to the Kok-Togay village in the upper reaches of the
Irtysh River.(Kara-Irtsys) near the confluence of the
Ku-Irtsys and Ul'kun-Kairty Rivers. Points of 'observa-
tion were clocked from the start of the flight and en-
tered in numerical order on an attached schematic map.
Card 1/4 Having mapped out the direction offlight and calculated

Flight over the Dzhungar Depression
14-1-410
the average speed of flight, it.was possible to deter-
mine the location of these points. As a result of these
observations the line of dislocated mesozoic formation
may be considerably further extended to the west of the
Guchen meridian into the Dzhunigar depression and a
schematic drawing made of the limit of the expansion of
the horizontal tertiary layer which directly covers the
paleozoic formations. Paleozoic formations reach the
surface in the Kara-Irtsys and Urungu River valleys.
At times, small paleozoic mounds rise above the terti-
ary plateau. The intermediate mesocainozoic deposits
are absent' in such cases. The northern par 't of the
Dzhungar depression can be considered to have such a
terrain. The formation of this part of the'depression
appears to be as follows: the tdrtiary plain stretches
south from the Urungu River and an extensive mas 's of
Kobbe sands covers the tertiary atkata. The'paleozoic
formations stretching from the east come iri dire 'ct con-
Card 2/4 tact with tertiary ledges and appear on the surface
I

Flight over the D'Zhungar Depression
14-1-410
only where tertiary deposits have been washed away.
Tertiary strata also come in direct contactwith
paleozoic e'leotions at the western edge of the
Dzhungar depression. The southern boundary of this
region is not known because a solid layer of sand ex-
tends in this direction followed by a bare plain con-
tiguout to the mesozoic edges of Tyan'-Shan. several
lines of dislocation of mesozoic formations were found.
one of them corresponds to the btrongly broken line of
the northern foothills of the Bogdo-Ula Mountain. It
was established that the inner part of the depression
has a~plateau-like formation bordered by steep ledges.
Dry river beds, cutting deeply not only into the sands
but also into the tertiary plateau, were discovered at
the northern edge of the sands and almost in their
central part. Possible changes in sand dunes are con-
Card 3/4 sidered. The author supposes that the basic source of

Flight over the 0zhungar Depression
the sands are alluvial deposits.
ASSOCIATION: Llvov University (Llvivsk.un-t)
14-1-410
Card 4/4

TTAIDTVv,0.0~~,
"~ .
Nov data on tha Palsocene fauna of Kas,hgar. Dckl. AN SSSI 106 no.6:
1065-1067 7 156. (HLRA 9:7)
l.De.vstvitelin" chlen AN USSR.
(Xashgar--PalAontology)

TTAUW,-0,S.t;V0R0F0V. P*S;
'Preliminary nots, on the geological structure of the reCion of "Oasis'
I
on:ICbman Kar7ls land at the Antarotic Continents Dokl. AN SSSR 108
no,5:916-~919 Ja t56o (XLRA 9s10)
I* Akadsmlk Akademil nauk USSR (for Vralov). 2.0beervatoriya MirD.Ty
AntarkticheskfWa ekspeditsiya A)mdemil nauk SSSR,
(Antarotlaveglone-Geologr)

v 'u, /
" 66 v i C), S.
M 049
ItW'6ier the Dzungarlan depression. Ilauk.zap,, Llviv un,
39:115-127 '56. (ULU 11:1)
(Dzungarian Ala-Tau-Physical geography)

VTALOVP O.S.;VORON.Ove P.S.
.Granite outcrops at the Knox coast In Antarctica, Dokl, AN =R
log no.6:1187-1190 Ag 156. (HLU 9:11)
1. DeyetviteliW chien Akademii, nauk UMM (for Vyalov). 2. Observa-
toriya MirrWy, Antarkticheakaya, ekspeditsiva Akademii nauk SSSR.
(Knox Coast--Granite)

SUBJECTt
ANTIRCTICIGeology
lo-6-1113
AUTHORt Vyalovo O.S.
T
ITLEo On Geology of the Mirnyy S~tation Region (K geologii rayons, stant-
I aii Mirnyy) ob
PERIODICALs Izvestiya Akademii Nauk SSSR# Serlya Geologicheskaya, 1957, #6,
PY 3-13 (USSR)
ABSTRACTs The author took part in the Soviet Antarctic expedition and
gives a geological description of the regions investigated in
the Antarctic, beginning with those in the vicinity of the Mirnyy
settlement. He prefaces his description with a brief character-
istic of the geology of the Antarctic.
Two main structural components are distinguished in the Antarc-.
tic: the folded zone of the Western Antarctic and the Eastern
Antarctic plateau.
The most complete cross section and the main peculiarities in
the atructure of the plateau are revealed in the Queen Maud
ridge which goes over into a mountainous region of the Victoria
Land coast. Foundation rocks consist of various gnsisses and
Card 1/5 crystalline slateaq including biotite gnsisass, micaceoua and

io-6-i/i3
TITLE: On Geology of the Mirnyy Station Region (K goologii rayona,
stantaii Mirnyy)
hornblende slates, granulites, etc. Their age is the Pre-
Cambrian epoch.
The sandstone series Beacon was discovered in the Victoria
Land# but it is to be found also along the Rose Sea coast and
in the Queen Maud mountains. The.age of this series is eati-
mated to be Devonian to Permian. In the Bangor "oasis" located
in the eastern part of the queen Mary Land outcrops of ancient
crystalline rocks were discovered.
The Gauss mountain In the Wilhelm II land was built of leucito
basalt and represents an extinct volcano of the Upper-Tertiary
age. There are also recent volcanos, as for instance Terror
and Erebus in the Rosa Island, of which Erebus iu still active.
Thus, the Eastern Antarctic represents an ancient plateau
whoso foundation is built of a crystalline complex covered main-
ly with the Paloozoic sandstones of the Beacon series. The
presence of Cambrian limestones was also established.
Vertical shifts were of enormous significance in the develop-
Card 2/5 ment of the relief of the Eastern Antarctic. The Ross Sea is

io-6-1/13
TITLEt On Geology of tho Mirnyy Station Region (K geologii rayona
stantaii Mirnyy)
a giant graben, The mountainous ridge of the Victoria Land and
the Queen Maud mountains are a big horst uplift which occurred
probably during the glaciation time of the quarternary period.
The Western Antarctic represents a folded zone which is an ex-
tension of the folded system of the South-American Andes. The
territory remains still unexplored. The presence of dislocated
metamorphic rocks of an unclear age was established in the
Rockefeller mountains# Edward VII peninsula and Edsel Ford
mountains,
On the Coast of "Pravda" in the Mirnyy regiont 4 small eleva-
tions or mounds protrude from under the ice cover. They are
located at the very coast and were named Mirnyy-1, Mirnyy-2,
Mirnyy-3 and MirnYY-4. The distance between the extreme mounds
is about 3 km.
The Mirnyy-1 mound Is the largest outcrop of rocks occuring in
their place of origin at the Pravda Coast# It is about 400 m
long and 34.8 m high. The Mirnyy settlement is located imme-
Card 3/5 diately south of this mound. The mound in built of charnockits

io-&i/13
TITLEs On Geology of the Mirnyy Station Region (K goologii rayon&
stantaii Hirnyy)
&rtnitoida, gneisses and crystalline slates. A small vein of
pyrite was discovered at the eastern slope of the mound. There
gre also several quartz veins. South of the Mirnyy-1 mound
there is the largest moraine of this district.
The Mirnyy-2 moundq or the "Radio" moundq is the highest
elevation on the coast. It is located.500 m south-west of
Mirnyy-1. Its height is 50,9 m. It is built of charnookite
granitoide.
The Mirnyy-3 mound has dimensions of l20xl5O m. Its height in
41.1 m above sea level and 15 m above the ice cover. The main
rocks composing this mound are dark-grey h7perathene plagiog-
neisses and hyperethene granitoida.
The Mirnyy-4 mound is only 20A m above sea level and a few
meters above the ice cover. Its dimensions are 75 x 20 m. The
mound is built of olivine pyroxene granonyonites with xenoliths
of gneisses and crystalline slates. Near the western side of
the moundp there is a vertical crossing vein, 40 am thick,
built of biotite granite, There is also a 2 to 5 cm thick band
Card 4/5 of leicocratic charnockite granite with films of iron oxides

1o-6-1/13
TITLE: On Geology of the Mirnyy Station Region (K geologii rayona.
stantaii Mirnyy)
and pyrite inclusions which arose due to the hydrothernal pro-
cesseso
A small island@ Fulmarg is located about 1,200 m north of the
Mirnyy-1 mound. Its top is 38.6 m high. One sample from the
island proved to be olivine-pyroxene granosyenite. Pegmatite
veins were discovered.
The author came to the following general conolusiones
The territory explored was Initially built of gnetesoe. Later on,
a large-scale intrusion of granitoid magma occurred. All the out-
crops of the primary rocks in the coastal mounds and islands re-
present the remnants of the single gneice-granite massif. Quartz
veins and sulfide minerals were created as results of the sub-
sequent hydrothermal processes.
No references are cited.
INSTITUTIONt L'vov State University.
PRESENTED BYt
SUBMITTEDs On 26 February 1957
AVAILABLEs At the Library of Congress#
Card 5/5

.. AUTHORs Vyalovj O.S. 5-6-5/42
TITLEs Faleogene of the Kyurendag Type In Turkmenistan (Paleogen
kyurendagakogo tips, v Turkmen1l)
PERIODICALi Byulletent Moskovskogo Obahchestva, Isiytateley Prirodyt Otdel
Geologioheskiy, 1957, # 6# pp 81 - 92 (USSR)
ABSTRACTo The author has studied the stratigraphy of Paleogene depos-
its in Turkmenistan since 1938.
In the present article he describes the Kyurendag type of
Paleogene deposits which is characterized by its considerable
thickness. The columnar sections of this type are similar to
the Kobystan typeo differing from the latter by the presence
of fauna.
The author tries to correlate Caucasian columnar sections
with those of Central Aaiay and holds that the Kyurendag co-
lumnar section is of great importance as the first link be-
tween them.
lie classifies the entire section into 6 suitee, character-
izes each of them in detail by petrographic and paleontological
data, and compares his schemes-with the earlier classification
schemes proposed by the other investigators.
The hrticle contains 1 figure, 1 columnar section, 1 table,
and 15 Russian references,
AVAILABLEt Library of Congress
Card 1/1

TYAIA)V, 0. S.
~ '
.0 ~ ,.
Seismotectonice of the western Carpathians and adjacent areas.
%o1. zhur. 17 no.2tl6-20 157. (HLRA 10:11)
(Carpathian Mountain region-Gbology, fftructural)

I" t'll, -) ,
TfALO',~, O.S,
I , - ..
Geolog7 of the Hirzy Station region (the Antarctic). Izv. il;
SSSR.Sor.pool. 22 no.6:3-13 Je '57. 10:8)
l.L'vovekiy j-,osudarstveuny7 universitet.
(Antarctic regions-Goology)

TTAWT, O.S.
mr of
U: S.S.R.
6
the Antarctic XxpeditlQn Of I the Aca"m7 of &Iona@# of the
Vlanyk A URSR 28 no.6t4)-47 Jo '57, (MM 100)
~(Jhitarctio regions)

VTAWV, 0. S.
International Geological Congress in Mexico. Izv.Vses.geog.
ob-va 89 no.3:289-291 MY-Je 157. (MIRA 10:11)
(Mexico (City)--Geology--Gongresses)

26-58-6-39/56
AUTHOR: Vyalov, O.S., Profe ssor and Tkachuk, L.G., Professor
TITLE: Lime Crusts from Antarctica (Izvestkovyye korochki iz Ant-
arktiki)
PE.RTODICAL: Priroda, 1958, Nr 6, P 113-114 (USSR)
ABSTRACT: The author tells of the observations he made at the Mirnyy
station in the Antarctica. Among the protruding granitoids
and gnoisses of the omall volcanoes he found large quantities
of grey lime crusts of peculiar shape, none of which was over
4-10 Mm thick. Under the microscope they were found to con-
sist of fine-grained calcite containing small quantities of
quartz, feldspar, bornblende, pyroxene, garnet and iron. Some
of these crusts are covered by irregular bud-shaped calcite
cryatals (Fig. 2) which, nccordinF to the author, probably
originate from sprays of non water containing calcium colts.
Since these crusts have faint indications of glacial scratch-
ings, it must be concluded that their origin dates back to the
preglacial epoch. There are 2 photon.
ASSOCTATTONt Tnatitut. geologit poleznykh iskopnyomykh Akndemii nauk MR
(L'vov) (Institute of the Geology of lip'ineraln of tho Ukr.3',3R
Academy of Sciences, L'vov)
Card 1/1 1. Geology-Antarctica

VIA~Ollf 0.".
New Arallocarlia frGm the 0' Two-er,'.-~n.
Tr-',Ir,y VSFG-I IC-9a2-9t>.-'0a 163. (!-' i I " i ". - , e i

VrALOV 0,3*
Probleme on tha Silurian of Kazakbutan, Biul. XO'l'?. W. greol.
38 no.6slOO-105 N-D 163. (MIRA 17?8)

MMA', O.S.; GORW-Cll, L.P.
Alla-morphic sculpture of the Lower Faleocene oysters of
Inkerman (Crimea). Vest. Llvov. un. Ser. geol. no.2:25-31
,64. (MIRA Y-): 1)

*VYALOV C.S., akade-ilk
------ -~-p .-- ~,, ~ "'. -
V I ... I
Ronam!ng certain Faleogpne U.-.
1
1359-1362 16.2. ~ M7 i-i I S.,.~ ~,
1. Institut geologil gcryuo~;hikh 4-skopf-p~m,,AY. AN i
All UkrSSR.

VYALOV O.S.; GOLEV, B.T.
. ----Z p
Faleodictyon of the Crimoa. Izv.,i7,*.uch,,mb.zav,; geol. I rdzv.
7 no-3:24-36 Mr 164. (MIRA 1813)
1. Institut geologii goryuchikh polcznykh iskopavemykh A14 UkrSSR
i Universitet druzhby narodov im. P.Lumumby.

GORSACH, (11'-%-N1Ch, rjuTovo.-,srAYA, T,,.
(Dobrovolln'ka, T.T.1
. j
Fossil atar-shaped prints of the activity of marine org.Anlaffis In
the ea5tern Crimea. Gsol. zhur. 24 no.4-.92-9'7 164.
1. Ina"itut geologii i gcokhlm.2. goryuchikh Jskopayem,,kh At.'
UkrSSR.

VYALOV, O.S. -
Nature of the Paleogens Cylindrites tuberosus Eichwald of the
Ural Mountain region. Biul. MOIP. Otd. geol. 39 no,ltl63-167
Ja-F 164. (MIRA 18s4)

VYALOVJ O.S.; GOLEV, B.T.
Detailed subdivision of Palodictyonidae group. Biul. HOIP. Otd.
geol. 40 no.2:93-114 Mx-Ap 165. (HIPA 18:5)

VYALOV, O.S. , akademik; r.FJSIiK*--'VICII, G.11.
Age and volume of the Miocene Puglovka layer3. Dckl. ~';
160 no.6:1361-136.1. F 065.
I.,k-h r"'All SSS,.
1. Institut geologli i geokhImii goryuchikh lskopaywwr P
2. All (for Vyalo7).

VYAILV, O.S., akademik; GORETSKIY, V.A.
Stratigrapiq of Tortonian sedizents in YoRynia e-nd Podolia.
Dokl. All SSSR 161 no. 1; 175-178 Ur 165.
(MIRA 18:3)
1. Institut geologil i gcokhimii goryuchikh iskopayomykh AN
UkrSSR i Llvovskiy gosudarstvennyy universitet im. I. Franko.
2. AN 'JkrSSR (for Vyalov).

WALC4r-Or&vj akademiks otv. red.; WGDANOVICH, A.K., red.;
BONDAREVA, T.P., red.; P101VANOVA, L.S., red.;
SUBBOTINAp H.N.p red.; FELIBIK, A.F., red.
(Faikop sediments and their age analogues in the Ukraine
and Central Asia; materials) Maikopskie otlozheniia i ikh
vozrastrqo analogi na Ukraine i v Srednei Azii,- materialy.
Kiev.. Naukova, dumka, 1964. 299 p. (MIRA MO
1. Kollokvium po mikrofaune i biostratigrafJi maykopskoy
tolshchi i yeye vozrastnykh analogov. lat, LIvav, 1961,
2. Institut geologii goryuchikh iskopayemykh AN Ukr.SSR
(for Vyalov).

VYALOV, O.S.1 GOLEV, B.T.
Prinolples of' lalaodiotyon aubdIvislono Izve v7so uahabb %av.;
geol. I razy. 7 no*107-48 Ja 164 (MIRA, 2,W)
1. Llvovskiy univeraltet Iment Tvana Franko i Universitet
druthby narodov imani P, Lumumby.

c.oF,c,jffrlj,', I. lya Davidovich; VYALOV, 0. S. sakademiky otvo red.;
1,1WNIK, A.F.p red. ~rvlll- ~'
fliacent tectonlcs of the Carpathians] Ileotektonlkn Karpat.
Kiev, Izd-vo AJ4 U= , 196,1. 181 p. (MIRA 17:6)
1, All Ukr.Sqt (for Vyalov).

VYALOV. O.fj., akademik
1-1~
Relationship between the first and secondlayers of Oligoeene-ostra-
cods in the CaucAsus. Dop. AN URSR no.2:242-245 164. WRA 17:5)
1. AN UkrSSR.

VIALOV, O.S., ikademik
Correlation between ttm first and second ostracod layers
in the Oligocene of the Caucasus. Dokl, AN SSSR 153 no.4.-
895-898 D 163. (MIRA 17:1)
1. AN ~krgSR.

VYAL(YV, 01eg Stepanovicb,, akadem1k; ANDRUS079 Dimitry Ilikolayevich..
akiiddd-Ye
On the'r'ecessity to divide the Paleogene of the F2jisch zone
into tvo main iseriest Carpian end OmbroniomaGeol,.1 abor. 14 no.11
169-173. 63.
1, Inctitut geologil gryucbikh iakopayemykh, Akadmaiya Vauk
Ukraynakoy SSSR, Kopqpika 15, Vvov (for Vyaloy),.'2, Geo-
logichookaya labomtoriya Slovatekoy Akademii Naukp Bratislava,
Cbrancov mieru 41 (for Andrusov).

VYAWVI O.Si, akademik; DANYSH, V.V. mmunwSKIY, S.F. (Kotsiubynolkyl.,
S, P ); KULICHITSKIY, Ya.0, [Kullchytslkyi, 1A.0.1; LOZIJffAKj, F-Yu.
[L~;;Lak, P.m.)
Cretaceous deposits of the western part of the eastern
Carpathians. Dop, AN URSR no.8:1081-1084 163. (MIRA 16:10)
1. Inatitut geologli goryuchikh iskopayemykh AN UkrGSRj Ukrainakiy
nauchno-iseledovateliskiy geologoraztedochnyy Institut i Nauchno-
prirodovedcheskiy muzey AN UkrSSR. 2. AN UkrGSR (for Vyalov).
(Carpathian Mountains-Goologyp Str%tigraphic)

VYAL akademik; BUFLOT, V.S.; MURAVETSKU V.ff,
p
Character of the basoment,of the wrestarn Transearpathian trotWb.
Dokl.l AN SSSR 150 no,428744r Je 1630 (KIRA 16:6)
1;,Iwtitut geologii goryuchikh iskopayemykh AN UkrSSR i
L rov-skaya geologopoi8kovaya kontora treBta. *Llvuv,aftegaz-
razved3m". 2. Akadeiniya nauk UkrSSR (for Vyalov).
(Trar,scarpathia-Goology, Stratigraphic)

VYALOVS O.S.,
Significanco of the find of Faleodictyon In tho Chukchi National
961s
Area. Sov. geol6 4 no.8,106-109 Ag (MIRA 16:7)
1. Inst#ut geologii J~2ul~*kh iskopayemvkh AN UkrSSR.
(Chulcehi N;9.tion&l4iK&-P&leobotaxq, Stratigraphic)

V'YA L OV pO.S.; VEIIGLII:SKIYI I.V. (vonblinalkyip I.V.11 UITIOBIII, V.11.
--- -,- (Utrobin, V.M.]
Corrolation of the oil and gas potentials of a cross section of
well No, 1 in the ziauzhe area. Pratoi Inst, geol. koro kop.
AN URSR 3:102-3.14 161. (MIRA 16:7)
(Zaluzhe region---Petroleum geology)
(Zaluzhe region--Qs,. Natural-Geology)

VZALOV.. 0.3.[Vyalov _MI; PISVABOVA, L.S. (Piahvanova,, L.S.1;
GRT iN~G.V. lGrishkavich, G.N.)
Sketch of the Transcarpathien Riocens stratigrapby. Amlele geol
geogr 17 no-4.-58-68 O-D 163.
1

VYALOV O.S.
Renarks on the clas;sification of tentaculites. Visnyk Llviv.un.
Ser.geol. no.lt66-69 162. (HI.RA 1607)
(Tent,iculitidae-Classifioation)

VYALOV, O.S., akademik
Phenomena of intravitam i=uraticn in nature. Dop. AN URSR no.11:
1510-1512 161. (MIRA 160)
1. AN UkrSSR i Inctitut goologli poleznykh iskcopq~pnywl
AN UkrSSR.
(Paleontology)

VTALOV O.S.
Soma problems of the Miocen stratigraphy of tha cis-Carpathian
Tegion, Pratai Inste geol kor. kopo AN URSR 3:3-18 161.
(MM 1617)
(Carpathian Moantain roglorr-Geologyp Stratigraphlo

PASTERNAK Severin Iyanovichl LEVITSKIY, Vladimir TeodotovicA
tLevytalkyls, V.T.1; IrYALDY 0 S akedemik, oty. red.;
ZAVIRTUKHINA , V. M. , r'~. '~zd-W;~'RBAWVA, N. A. , tekhn.
red.
[Monographic collections of palentological fonds in the
Museum ot Natural History of the Academy of Sciences of the
Uk~ainlan S.S.R.] Yonografichni kolektaii paleontologich-
nykh fondiv naukovo-pryrodoznavchoho muzeiu AN URSR' Kyiyp
Vyd-vo Akad.nauk URSR, 1963. 36 P.' Wii 16:6)
1. AN Ukr.SSR (for Vyalov).
(Ukraine--Paleontology)

VYALGV,t 0,6.
CUssification of the traces of vital activities of organisms end
structural marks in molasse and flysch layers. Geol.zhur. 23 r,-o.L;16-2.'q
163. (14IRA 16:4)
1, IGGK AN UkrSSR,
(Paleontology)

VYALOVt O.S. ; PASTEMAK, S. I.
In memory of B,3. Kok-oshinskaia. Faleont.sbor. [Lvcrvl
no.1:157-158 161. (MRA 15:9)
(Kokoshinskaia,, Bronislava Sigi=undovna, 1897-1959)

VYLLGV: O.S.
Critical study of the Gryphaea brongniarti Brom group,
Paleont.sbor. [Imov) no.1:3-18 161. (14M 15:9)
1. Institut geologii poleznykh iskopayemykh AN UkrSSR, L'vov.
(Oysters, Fossil)

VYALOV. MTRASIMETICII, 11,1.
GR- r7lCll, G.R. fitryshkav7sh, H.M.
c1 ~,r 1.'!~
Stratigraphic pattern of the IYanscarpathism Mocens. Do
AN UISR 16-ift (MIRA 31,~M
1. Institut geologilb. korimikh kopalin AN URSR i UkrDI-IGRU.
2. Akademlk AN bWR (for Vyal(ri.10
('11'rans ~~arpat hia- -Poe clogy, Stratig-raphic)

VnbDV. O.S.: ZEIIKEVICHI II.L.
Traceo of a crawUng animal on the flocr of the Pacific. Izv.,~ 11
SSSR. Ser.geol. 26 no.1:52-58 JTa t6l. (HIRA, 15:6)
1* Institut goologii poleznykh iukopayomykh AN U58R. L'vov i
Institut okeanolo i All SSSR.. Moskva.
Pacific Ocean-Palenotolo&7)

VUWY-PI-Q.ST--
Outline of the tectonics of the &Btern Soviet Carpathians.
Mat.Karp.-Ba.lk.assots. no.1:5-30 160. (MIRA 11+:12)
(Carpathian Mountains-Geology, Structural)

VYAIA)V, O,S.
Formation of oil poola in continental layers of Dzungaria. Geol.
abor. (Lvov] no.7/8:263-281 161. (MIRA 14-12)
1. Institut gaol giLpole=ykh iskopaysmykh AN USSR, L'vov.
(D-.ungaria-Patroleum geology)

VYALIDV, O.S.
Stratigraphy of the Faleogene in the &tdkhyz region. Geol.abor.
(Lvov) no.7/8:489-503 161. (MIRA 14:12)
1. Institut geologii poleznykh iskopa.-remykh AN USSR, Llvov.
(Badkhyz region-Geologyp Stratigraphic)

VYALOV, O.S.
Trip to Poland., Hungary and Rumania in 1959. Geol-sbPr.
[Lvov] no.7/8:541-554 161. (MLM 14:12)
1. Institut geologii poloznykh iskopayemykh All USSR, L'vov.
(Geology-4ongreoses)

VYAIDV) O.S.,. akademik; DABAGYM., N.v.; KULICHITSKIYp Ya,O,
Recent data on the age of the Shipot and Dusino series in
the Eastern Carpathians. Dokl, AN SSM 142 no./,:896-8" F
162. (MIRA 15t2)
1. Institut geologii poleznykh iskopayamykh AN USSRli
Ukrainakiy nauchno-inslodavateltakiy geologormododayy
institut. 2. AN USSEL (for Vyalov).
Chernogora Range region--Goology,, Stratigraphio)
Malyava lPegion-Geology,, Stratigraphic)

VYAIDV (SSSR); GLUSHKOO V.V. ( SSSR)j KULICHITSKIY, Ya.0. (SSSR)-
P
SIAVIN 0 V. 1. (SSSR)
Stratigmphy, of the Eastorn Soviet Carpathlaze Mat.Karp,-Balk,
asooto. no.3t5-26 160. imm 341v)
(Carpathian Hountaine-Geologyp Stratigraphic)

VTALOV.. 0.S. (~WR); MULOV, V.P. (SSSR); 'WDOVIARZ, St. (Polska);
OLEWIGZj, Z;R. (Polska); NOVAK* V. (Polfsha); SIAVIN, V.I. OM)
MAS=VA N.r. (SwOR VYALOV A,G, (=R)
BONDAMHUK, V.G (SS tj
Participation in discussions. Mat,KezVe-Bd1koas`sotse no#3:257-
179 160o (MIRL 14:12)
(Carp~thian Mountaing-iGqology)

GOFSHTLMI, Illya Davydovich; VYAIDVJI O.-S.,,_ akademik, otv. red.;
CHEKHOVICII, N.Ya. [ChMOvycE, A.3j, red.; LIEERMAN, T.R...
tekhn. red.
[Recent tectonics and morphogenesis of the upper Dniester Va-Ueyl
Neotektonika i morfogenez Verkhn'oho FTydnistrovlia Kyiv Vyd-
vo Akad. nauk URSR, 1962. 130 P, imIRA IP5:6)
1. Akedemiya nauk TJSSR (for Vyalov).
(Dniester VaUey-Goologyj Structural)

--V-Vnovs 0. 0 rof., akademik
Snakea buried alive* Friroda 50 nooll;216-117 N 161o
(IOU 1010)
1. Akademiya neuk USSR, L'vov.
(Hungary-Serpent43, Fossil)

AIJASTASIYF.VA, OX.; VYALOV, 0,S.; SANDIER, Ya.M.
'I-% -----------
Jurassic stratigraphy of the southwestern border of the Russian-
Platfoxv and the Carpathian piedmont fault. Trudy VNIGIII
no.29:161-166 vo3. 2, 161. (MIRA 24:7)
(Ukraine, Western-Geology, Stratigraphio)

FORFIRIYEV, V.B., akademikp otv
ff_Ajg~j_gjeg 4~4 a red.;
CHEKHOVICH, red.; YEF1240VA, M.L, tekbn. red.
[raleogone flyacb on the northern slope of the CarpathianalPa-
leogenovyi flish severnogo, Alone, Karpat. Kiev, 12d-vo Akad.
nauk Ukrainskoi SSRp 1961. 234 P. WIRA 1511)
I.Akademiya nauk Ukrainakoy SSR (for Porfirlyev).
(Karpathian Mountains-Flysch)

MLOV 0. S.
Development of the studies of the tectonics of the eastern
Carpathians during the Soviet regime. Fratsi Inst. geol.
kor. kop. AN UPZR 1:3-28 159* (MIRA 14-6)
(Carpathian Mountains-Goologyo Structural

VYALOV, O.S.
Brief s~tudy of the structure of the Carpathians. Pratsi Inst,* geol.
kor. kop. All URSR 20-22 160. (1-ap-A 1" : !,)
- (Carpathian Mountaim-Geology)

VYALOVP O'S,
__ - -- ---- - -
Lower Faleocene 'Polovetokw Limestone In the Crimea. Biul.
. MOIP. Otd. geol. 36 no.1:99-105 161. (MM 14:5)
(Crime&--Limestone)

~ ~VYAWGV 0 S ak&demik
, W ~,~ * - 0 ~,CIA,
Recent fossil footprint of a bird In the Miocene of Ciscarpathia,
Dokl. AN SSSR 135 no.5#1237-1239 D 160, . (HM 13t12)
.1. AN USSJI-~ Institut, geologii poleznykh iskopayemykh AN USSR.
I IDelyatin region-Birde, Fossil)
(Nadvornaya region-Birdav Fossil)

TANSHIN. A.L., akedemik, rod.* VTALOV. O.Sap red.; DMOOPOLOY, X.N.,
red.; KMM, V.T., red.: ROSSOVA, S.M., red.izd-va;
MAKOHNOTA, I.A., takhn.red.
(Paleogene sediments in the southern port of Buropean Russia]
Paleo&9novye otlozheniia iuga Irropaiskoi chasti SSSR. Moskva.
Izd-vo Aked.nauk SSSR, 1960. 311 p. (mm 14a)
1. Akademiya nauk SSSR, 2. Inistitut goologichookikh nauk I
poleznykh iskopsysmykh AN USSR (for V781OV). 3. Inatitut geologi-
cheskikh nauk AN SSSR (for Kenner).
(Russia, Southern--Geology, StratieraDhic)

VrAWY, O.S. , akadem!Lk; GOLEV, B.T.
Classification of Palsodictyon.
S I6o. J)okl 'AN SSM 134 no - 1-' 175-178
(MIRA 13:8)
1- V86607uzWY za0chWy politekbuichookiy inatitut. 2. Akademiya
nauk USSR (for Tyalov).
(Paleontologr)

Dg St OPEL h T.J&]LAw,.,O,Sj,, prof,, doktor geol.mineral nauk,
40VIO
akademtk
Expedition to the Antarctic, Ilauka I ZhYttla 6 no.9:1-4
S 156. (14IRA 13:5)
1, All USSR. Llvovokiy universitet. Uchautnik Antarkticheskoy
kowlekenoy ekspeditaii AN SSSR.
(Antarctic regions)

VYALOVO Ovs*
Some Paleogene ovoters from Turkmaistan. lzv,Al Turk.SSR no.6:
102-104 159. (KIRA 13:5)
1. Inatitut geologii AN Turkmenskoy SSR.
(Turkmenistan-0yeters, Yossil)

VTAIDT, O.S. (Vialov. O.S.], akademik
Indications of the volcanic activit;r In flysch and molasse
formations in the northern slope of the Carpathians and the
cis-Carpatbian region. P~t.geol. no.9:5-19 158.
(MIRA 13:4)
1, AN USSR.
(Carpathian Mountain region-Volcanic ash, Tuff, atce)

VTALOV, O.S.;,IVAROVA, L.Y.
Age of rocks in the Bitkov t-qctonIc window, C"thlan KountaIns.
Gaol. abor. LImovJ no.4:43-46 '57. (MIRA 13*2)
l.Inatitut geologii roleznykii iekopayamrkh AN SSSR, LIvov.
(B7stritea Valley-Yoraminifera, Fossil)

VrALOT, O.S.
Yreliminary data on the geoloff of the Antarctic coastline
betwoen 89 and 107th degree I.L. Geol. s~or. LLrvvj no.4,.*187-195
157. (MIRA 13:2)
I.AN USSM 1,1vovskly gosuniversitat imeni Ivana Franko.
(Antarctic regions--Geology)

VTALOV, O.S.
Our impressions of the International Geological 00utreGG in MexitO-
Geol. sbor. Llqovj no.4:355-360 (HIRIL 1312)
1.1natitut geologii poleznykh iskopayerqkh AN USSR. Llvov.
(Mexico (City)--Geology-Oongresses)

VTAWV, 0. S.
Miocene stratigrapby of tbn Transcarpatblan trough. Geol.
nefti i gaza 3 no-8:39-43 Ag 159, (MIRA 12:11)
1. .411 USSR.
(Transcarpatbia--Geolog7, Stratigraphic)

.3 (4, 5)
SOV121-59-8-15126
AUTHOR: Vyalov, 0. S., Member of AS of the UkrSSR
TITLE: History of the Development of Antarctica
PERIODICAL: Dopovidi Akademii nauk Ukrainstkoi RSR, 1959, Nr 8,
PP 878 - 880 (USSR)
ABSTRACTs In connection with research studies conducted by various
foreign geologists during the 3rd International Geophysical
Year and with the conference hold in Wellington in 1958
[Ref, 43, the article presents additional nomenclature
suggestions in respect to the history of geological develop-
ment of Antarctica. The following basic stages of the geo-
logical development of this territory may be outlined3
1) The Precambrian stage of the accumulation of sediments
(Maud complex), folding, metamorphismp and the formation of
intrusions which ended in the formation of the old East
Antarctic platform. The Victoria cycle (granites, etc.) and
the Mawson cycle (chiefly charnokites, etc.) are distinguished
as two main cycles of intrusion aotivity.
Card 1/4 2) The Upper Proterozoic and the Lower Faleozoic stages are

SOV/21-59-8-1-/26
Tectonics and History of the Development of Antarctica
characterized by the development of the Rose geosyneline at
the Western edge of the platforml the deposition of Re3s
system strata, the development of the Rossid folded system
(which probably continues in the Flinders system in Australia),
the formation of the Admiralty intrusive complex (granodior-
ites [Ref. 53, etc.). On the platform - the deposition of the
Sandow series.
3) The Paleozoic Stage, not yet subdivided, is covered by
the development of the Falkland geosyncline and its branches
the Orkney, pasaing through the Shetland Islandsp the Western
Edge of Antarctica and the AustralianAlps, and the Maronian
which lies between Antarctica and Africa [Ref. 11. Probably,
the Caledonian folding and, for sure, the Hercynian. On the
platform there are the Beacon deposits. As the result of
closing of geosynclines and folding, Antarctica became united
in a single platform with Brazil, Africa and Australia. More
recent folding processes were not noted there.
4) The Mesocainozoic stage also not yet subdivided! develop-
ment of the geosyneline of BellinshaVsen which unites the
Card 2/4 Andes and New Zealand, the Mesozoic ~Pacific) folding, the

SOV/21-59-0-15/26
Tectonics and History of the Development of Antarctica
intrusive activity (Graham's cycle), the closing of geosyn-
cline, the formation of the Antarctic Andes system. Splittings,
volcanic activity, and formation of dolerite sills (Ferrarla
volcanic cycle) on the platform.
5) The neotectonic stage (Neogene - Quarternary times)i
large block rising and sinking, formation of the Great
Antarctic horsts and of the South Pole graben, the shaping
of the Antarctic shelf contours, and (in its general aspect)
of the continent, the large morphological elements on the
bottom of the adjoining oceans [Ref. 1, 2], recent (up to
the present) volcanism (Mac Murdo's cycle). Eastern Antarc-
tica is the only continental massive with a very complicated
relief broken up into a number of grabens by young movements.
The South Pole is located within the borders of a deep graben
since the fundamental bed is only 275 meters above the sea
level. For solving the most significant basic problems
connected with the structure of Antarctica, the study of the
zone between the Queen Maud mountains and the Shackleton
crest, and particularly of the coast of the Bellinshausen
Card 3/4 and Amundsen sea is of exceptional importance.

50Y/21-59-8-15/26
Tectonics and History of the Development of Antarctica
There are 6 references, 3 of which British and 3 Soviet
ASSOCIATION: Institut geologii i poleznykh iskopayemykh AN USSR
(The Institute of Geology and Mineral Resources of the AS
of UkrSSR)
SUBMITTED: March 25, 1959
Card 4/4

3(5) SOV/21-59-9-16/25
AUTHOR; Vya.lov, O.S.,-Member AS UkrSSR
TITLE: On a Change in the Scheme of Miocene Stratigraphy of
the Transcarpathian Region
PERIODICAL;. Dopovidi Akademiyi nauk Ukrayinslkoyi RSR, Nr 9,
1959, pp 998-1001 (USSR)
ABSTRACT: In this article,* the author discusses the results of
a detailed analysis of the Miocene foraminifera of
the Trans- and Fore Carpathian depression which in-
duced L.S. Pishvanova / Ref 7-7 to give a new inter-
pretation of the age of certain koc,-~.ne suites of
the Transcarpathian section. Analyzing the new micro-
paleontological materials presented in the paper of
this scientist, the author arrives at the conclusion
that some 3uites of the basic scheme, located in its
various parts, have expressed themselves to be mono-
secular, which means that they reoccur in the sections.
This calls forth the necessity to revise the geological
Card 1/4 map considerably. The age and the location of dacite

SOV/21-501-9-16/25
On a Change in the Scheme of Miocene Stratigraph.- of t-he Transcarpa-
thian Region
tuff horizons is of basic importance for the new stra-
tigraphic structures. On the basis of the data of
Pishvanova, the author concludes that the Novosolitsa
tuffs of Novoselitsa district and the Danilove tuffs
discovered by the Danilove borehole are one and the
sam,e horizon, called the Novoselitsa tuff. This re-
sults in the fact that the sections of the central
parts and outskirts of the depression start vrith
these Danilove and Novoselitsa tuffs. In such a case,
the lowe:T strata earlier considered as the strata
underlying the Novoselitsa tuff Z Ref 8-7 (Tereblya
and Solotvino series) do not drop out of the section
in the outskirts of the Solotvino depression; on the
contrary, these strata lie above the tuff. Therefore
the #p1asse series of the Solotvino derressior cnnnot
be subdivided into the lower and upper Holassi for-
mations lying under and above the Novoselitsa 'v-uA'fs.
This also does away with the subdivision of this de-
Card 2/4 pression into two zones of different age - an outer

SOV/21-c9-9-16/25
On a Change in the Scheme of Miocane Stratigraphy of the Transcarpa-
thian Region
zone with a complete series.of molasse and an inner
zone with only upper M61asue depos4ts. Then, the
Tereblya salt containing stAte of the Golotvino region
and the section of the Danilovo borehole will to some
extent correspond to the Khustets clays of the Novo-
selitsa village which directly cover the Novoselitsa
tuff. The tuff horizon outcropping on both vings of
the anticline of the Danilove region as well as on
the river Tereblya, Mount Xopul'no and other places,
and this discovered by the borehole in Vishkovo, are
not Novoselitsa, as usually considered, but an inde-
pendent, younger Upper Tortonian horizon which the
author named Nankovian. At present it is impossible
to express a definite consideration concerning the age
of the Nankovian tuff, as there are no accurate and
revised data available. If the above consideration
were correct, it could be assumed that the Nankovian
tuff lies between the analogues of the Verbovets and
Card 3/4 Pruth strata. Finally, the author emphasizes the need

SOV/21-59-9-16/25
On a Change in the Scheme of Miocene Stratigraphy of the Transcarpa-
thian Region
for a collective elaboration of a new stratigraphic
scheme and for the establishment of a basic standard
section. There are 1 table and 8 references, 7 of
which are Soviet and 1 Czechoslovakian.
ASSOCIATION: Instytut heolohiyi korysnykh kopalyn (Institute of
Geology of Mineral. -Resour,619)~-
.SUBMITTED: -March 2.5, 1959
Card 4/4

VTALOV, O.S.
- Oil In the Antarctic& Geol.nefti 2 no.3:70-3 of cover Xr '58.
04MA 12:6)
1. Institut poloznykh takopayomykh All USSR.
(Antarctic regions-Oil ftnlds)

3 (5)
AUTHORS: Vyalov, 0. S., Academician AS UkrSSR, SOY/20-126-4-40/62
1-1,
PfifiFa:novi~j
TITLE; New Data on the Fauna of the Lower Tortonian of Podoliya
(Novyye dannyye o faune nizhnego tortona Podolii)
PERIODICAL: Doklady Akademii nauk SSSHj 1959P Vol 126j Nr 4P PP 834 - 837
(USSR)
ABSTRACT: In the Nikolayevskiy karlyer (Nikolayevskiy open-cut mine)
close to the highway of L'vov-Stryy, near the town of Nikolayev,
about 30 km south of L'vovj where the platform slants to the
Zubzha river, fossils were found which hitherto were unknown
in the
western areas of the Ukraine. The following faunistic
'
horizons were separated in this Lower Tortonian sand mass (from
below to the top): 1) bryozoan-horizon - 4 m. 2) Ser ula-hori-
zon - 7 M. 3) Heterostegina (Pig 3)-horizon - 2 m- 45 Serpula-
-bryoioan-sandstones (1-5 m). In the second horizon beside
Serpula gregalis and*Ditrupa cornea aloo a great number of pa-
culiar rod-shaped, sandy, formations were found. They are known
in Soviet publications as rhizoliths or ophiomorphs (Figs 1,2).
The authors hold the opinion that they*are traces of the vital
Card 1/3 action of decapod crustaceans. In spite of their wide distri-

New Data on the Fauna of the Lower Tortonian of BOT/20-126-4-40/62
Podoliya'.
bution they were almost not described. Their nature was not
determined for a long timep they were even believed to be the
roots ~f lana plants. Finally, the true nature of the rhizo-
lithe was determined (Refe 2,4,8)- In this connection also the
claws of higher crustaceans were found. In the entire sand
mesa bryozoae, ser ulids# and opins of urchins are rather wido-
-spread. Ostraoods are found everywhere (Bairdia,.Cythera).
Different parts of the send mass mentioned, do not sharply
differ from one another, the quantitative interrelations, how-
ever, between -the individual elements differ rather strongly
so that the ceparation of the 4 independent horizons mentioned
was pos3ible. The Tortonian sea is supposed to have had normal
salt content. This was probably a shallow area near the coast
with moved water. In the stratie:raphio scheme of the Miocene-
-molasses (molassy) of the Predkarpatlye (Cis .-Carpathians) the
Globigerina-horizon (or accordir-9 to the second author, hori-
zon with Candorbulina universe, was separated as a horizon
with pseudomussium denudatum (Rouss.). It is true, in the Pred-
karpatskiy progib (Cie-Carpathisn Depression) a much greater
Card 2/3 manifoldness and a strorger predominance of the plankton forms

New Data on the Faun4 of the Lower Tortonitn of SOY/20-126-4-40/62
Podoliya
which indicate the greater dopth of the water, were found. It
may be maintained that the ofia of the Nikolayevskiy karlyer
was a very shallow coastal part of the Lower Tortonian waters
which was connected with a doeper part in the Predkarpatakiy
front dapresoion. There are 3 figures and 11 references, 5 of
which are Soviet.
ASSOCIATION: Institut geologii poluznykh :Lskopayemykh Akademii nauk USSR
g.Ltvov (Institute of 06010g;r of Mineral Reoorarcea of the
Academy of Sciences UkrSSR, L'vov)
SUBMITTED: January 9, 1959
Card 3/3

3(5) MWE I WOE EXPLOITATION 1 my/7302
Akadentra nauk Ukrainakoy SSR. Inptitut geoiogli polernykh iskov^70-
m7kh
magratsit Wet I foralrovanlya nertyanywk I lazovyk2l sko-
Plenty; astartaly Larovskay d1skusal 18-12 says 195 A.
i
ono;
Or 07.1 Migratlon and the Formation of 01'. and 043 Accumulat
Material* or the Discussion Hold in L,vov, May B-12. 195T) Moscow.
008toptekhtsdat, 1959. 422 p. 1,100 copies printed.
Ids.8 V. S. Forneyev, Academician of the Ukrainian 3= Academy Or
Balances, and X. 0. bred, Professarj ZX&O. Id.2 P. a. Y*rwwv;
Tech. Z4.1 A.S. Polosina. Zdltorisl boardi 1.0. Bred, r-olessor.
U.N. Ladythonakly, and V.D. PorfLr9yev, Academician or the L"s-rain-
lan Academy or Sciences.
PURPOSZs This collection or articles to Intended for a wide range Or
geologists and research workers interested In all problems.
COVIPAORt Articles contaln2d In thin book deal with the proble%x Of
Migration and accumulation or oil and gas. Thee~ problems were
discussed in RAY 195T at WvOv State University Is. 1. Frank* at
a meeting orSanized jointly by the Institute of O*ology and Xlner-
ax Resources, Academy or Sciences or the USSR, the Department of'
00ology and Oil Exploration or the L-vov Polytechnic Institute.
and the L'vOv Goo], steal Society. Theories on the origin OC P*-
trolaus daVomtts kn4 the conditions surrounding their occurrence
A" treated. There are 32T reforencest 232 3ovl*t. 86 M4116A.
5 French, and 4 German.
?ABU OF COXTVffS&
Introduction 3
Opening Address by the President of the Organization Committee
of the Conference T.R. Forftr-yow 5
Xmas
Av"v W.Ya. JVWIGRIJ Basic Regularities in the Formation of OIL
Doicialti-In the Pril.-plyakaya Salt Dome Region III
Linetakly. V.P. 11OPI, Am Vkrssa) Anomalous Formation Pressure
as a T--xw Criterion In th. Formation or Oil Deposits 121
Eadrysvtoev, N.A. (TWIGRI, Leningrad) Mechanics of the Formaticwt
of Oil mad gas Deposits 136
Ir"atkIn. ?.M. and r-A. Shakhvarstava jOeologicheekly Institutl
Solid Bit%vanne. 011. and lot Gas~& In Ultrabasic Intrusions,
Traps mad Volcanic mocks
Forfir'yev. V.S. [InstItut g*ologll poleznykh Iskopsymakh AM.
UkrS3R1 The Tise Problem in the Formation or Oil Deposits X65

Kakhtt"v, Sh.p. jrhatitut
9e0101911 IA. I.M. Oubklna, AxerbAydtan)
ThWS*u"* Bad Characteristic or the Lower Part Depo#lt. In the
Productive Series (Middle Pliocene) or Azebydgh,.~n
K0z1*nRO. 3-t- and K. A. MashkovIch. (VWIOMI Branch. 3ALr&tovl Th.
Age or oil and 048 TrAP"l 4 Criterion for Forecasting Their Cl_
:O"ring capacity 2M
11"0n. X-X, IMJRI, Moscow] Distribution of Heavy Hydrocarbons
n"ar Various aeologloja Condition.
'Xt!2!L-0_3- on the ojestion or oil LA the Antarctic fteglon 210
'T*b*rs v-v- (vxlaml* R0840w) Formation or oil Deposits and Feel.
or Sedimentation
211
Tydrin. b.r, (Krasmod
arh;ft:ra#v*4k~j M*W Data on the Ooology of
the oll_&nd C&*.b4Lrt
ng as ibiliti.6 I, the W..#Lorn Caueasue and
-
P"dkavkaX
j,e
217
CW-d J/10

VTALOV, O.S.; XMKOV, L.V.
Composition of moraines on %~wsn Xary LwA and Wilhe2x II Coast.
Trudy Uuch.-Isslolnetegeol.Arkto 95:123-139 '57.
(MIRA 12: 1)
(Antarctic regions-Noraines)

15-1957-3-2629
Translation from: Referativnyy zhurnal, Geologiya, 1957, Nr 3,
p 12 (USSR)
AUTHORS: Vyalov, 0. S., Babayev, A. G.
TITLE: Some Data on the Cretaceous and Tertiary Rocks of the
Zeravshan: Valley - __ (Nekotoryye dannyye o melovykh i
tretichnykh otlozheniyakh Zeravshanskoy dolihy)
PERIODICAL: Zap. Uzbekist. otd. Vses. mineralog. o-va, 1956, vol 9,
pp 63-75
ABSTRACT, The paper describes sections of Upper Cretaceous rocks
in the Zeravshan River valley at Khshikat (Tadzh33R),
near the Stalinabad--Ura-Tyube railroad, and of Upper
Cretaceous-Paleogene rocks at Vishist (middle course of
the Zeravshan River). The Upper Cretaceous rocks con-
sist of marine and lagoonal deposits. In lithology and
environment of deposition they are similar to the-Upper
Cretaceous rocks of Fergana. The upper Paleogene rocks
Card-1/2 are chiefly marls and clays, but some limestones and

15-1957-3-2629
Some Data on the,Cretaceous and Tertiary Rocks of the Zeravshan
Valley (Cont.) :
I
dolomites are presento- Similar rocks occur in the Tadzhil-
depression, especially on the northern and northwestern border.
Card 2/_2 A* V* Go

VYALOV, O.S.; TKACHUK, L.G. [Tkachuk, L.H.)
Sedimentary rocks from Cape Town and Antarctic moraine. Geol.
zhur. 18 no.1:39-45 158. (MIRA 11:5)
(Cape town-Roclai, Sedimentary)
(Antarctic regions-Rocks, Sedimentary)