SCIENTIFIC ABSTRACT VAKHRAMEYEV, V.A. - VAKHROMEYEVA, N.I.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R001858410014-9
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: August 31, 2001
• Sequence Number: 14
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

VAKERMEYN, V. A.
Now bigh-capacity WS-0, 8 machine for cleaning the need of
fiber flax. Sellkhozmashina no.8:8-10 Ag 156. (HLRA 9:10)
(Flaxseed) (Agricultural machinery)

VAMUSIM, V.A.
Postore dikes of quartz porphyries In the Shal7m deposit of
Cromaya Shoriya. Trudy Gor.-geol.inst.zap.-Sib.fil.AN SSSR
no-17:49-52 156. (KIRA 13:5)
(Shalym mgion (Gornaya Shoriya)--DIkeB(Geolog7))

SAFIANO. Tat!yana Alekseyevna; KGRZ TV KIY, D.S.. alcademik, redaktor;
BOMMAN, I.D., doktor geologo-mineralogicheskikh nauk, redaktor;
VAAMi�W&mLv&jA doktor geologo-mineralogicbeskikh nauk,
remm-0:r; ma",-T. L. doktor goologo-mineralogichaskikh nauk,
.edaktor: MIA, B-X., doktor geologo-mineralogichaskikh aauk,
redaktor- IABSIW, A.F.. doktor geologo-mineralogicheakikh nauk.
redaktor: KHAIII, V.Ye., doktor goologo-miueralogicheakikh nauk.
redaktor; SHMTS. N.A., doktor goologo-mineralogichookikh nauk,
radaktor; TABUZOV. V.S., kandidat geologo-mineralogichookikh nauk.
redaktor; OMAN. R.L., kandidat biologichpokikh usuk, radaktor;
VAYSMAV. L.3., nauchnyy sotrudnik, redaktor; SIAVIANOVA, N.Y..
nauchn" sotrudnik. radaktor; IZMHINSXATA, Ye(ITO, redaktor;
TUMARKINA. 5.A., tekhnicheskiy redaktor
[Inglish-Russian geological dictionary] Anglo-rusekli geologichaskii
slovar'. Pod red. D.S.Korzhinakogo i dr. Xoskva, Gov. isd-vo
tekhniko-teoret.lit-~-ry. 1957. 528 p. (XLRA 10:7)
(English language--Dicti one rise --Rus 9 ian)
(Geology--Dictionaries)

!._~ --!7 'T -,- f! ! F 1 t_ -, -i V, i , ,,
AUTHOR: Vakhrameyev, V.A. 11-11-7/9
TITLE: Development of Botanical-Geographical Regions During the
Paleozoic and Idesozoic Eras on the Eurasian Territory and
Their Significance for Stratigraphy (Razvitiye botaniko-geo-
graficheskikh oblastey v techeniye Paleozoys i Mezozo a na
territorii Yevrazii i ikh znacheniye dlya stratigrafii~
PERIODICAL: Izve8tiya Akademii Nauk SSSR, Seriya Geologicheskaya, 1957,
11, p 82-102 (USSR)
ABSTRACT: The study of botanical geographical zones and their division-
ing into respective areas and provinces of geologic history is
not only of theoretical but also of practical interest. In
the history of climatic developments and botanical geographical
areas of Eurasia throughout the periods of the Upper Paleozoic
and Mesozoic eras, two cycles can be distinguished: the first
covers the Lower Carboniferous up to the end of the Middle
Triassic, the second starts at the Upper Triassic and ends at
the Lower Cretaceous epoch. The author subdivided each cycle
into two stages. The first halves of these stages were charac-
terized by gradual diminishing of the zones of arid climates,
which resulted in a smoothing-out of climatic, botanical and
Card 1/3 geographical zoning. The temperate-humid zone transits directly

11-11-7/9
Development of Botanical-Geographical Regions During the Paleozoic and
.Mesozoic Eras on the Eurasian Territory and Their Significance for Strati-
graphy
into a warmer humid zone in southern direction. During the
second half of the Paleozoic cycle a narrow belt of arid climate
appears, separating the Tunguska and Westfalian regions of this
era, without having a definite influence on the nature of vege-
tation. During this stage the growth of trees, especially
those of the southern zone reached its climax. During the
second stage a quick spreading of arid climate over formerly
humid-hot areas was experienced. At the end of the second stage
and throughout the entire cycle a renewed narrowing of the arid
belt was experienced, widening the area of humid climates of
the southern zone and giving rise to new types of vegetation,
which soon covered the entire territory of Eurasia. During
the Paleozoic era the arid belt practically disappeared, while
at the end of the Mesozoic cycle it continued into the Upper
Cretaceous period, confined primarily to eastern Asia. The
second stage began during the Eocene epoch when vegetational
differentiation of Eurasia became more noticeable. A.N.
Card 2/3 Krishtofovich classified the two basic regions into: North

11-11-7/9
Development of Botanical-Geographical Regions During the Paleozoic and Meso-
zoic Eras on the Eurasian Territory and Their Significance for Stratigraphy
Turgay and South Poltava. Subsequent aridity and cooling-off
led to the formation of a steppe belt in western Eurasia. The
author is of the opinion that the explanation of the zoning
of the Upper Devonian period ir or% of the most important future
tasks for Soviet Paleo-botanists by using macro-fragments as
well as spore-pollen complexes for their research work.
There are 1 table, 4 maps, and 42 references, of which 41 are
Slavic (Russian).
AVAILABLE: Library of Congress
Card 3/3

3(5) PHASE: I BOOK EXPLOITATION SOV/15o6
Vakhrameyev, V..A.
BegionalInaya stratigrafiya SSSR. Tom 3. Stratigrafiya i iskopayemaya flora
yurskikh i melovykh otlozheniy Vilyuyskoy vpadiny i prilegayushchey chasti
Friverkhoyanskogo krayevogo progiba (Regional Stratigraphy of the USSR. Vol. 3.
Stratigriphy and Fossil Flora of Jurassic and Cretaceous Deposits of the Vily-
uyska*a Depression and the Adjacent Part of the Priverkhoyanskiy Peripheral
Downwarp) Moscow, Izd-vo AN SSSR, 1958.
PURPOSE: This book is intended for geologist-stratigraphers, paleontologists
and paleolatonist8.
COVERAGE: This book contains the results of studies the author conducted between
1950 and 1954 on the stratigraphic series of the middle course of the Lena
River and its tributary the Vilyay. Fart I describes the stratigraphy of Juras-
sic and Cretaceous deposits, and Part. II - the fossil plants of Upper Jurassic
and'Lower Cretaceous times. No recognizable Lower and Middl Jurassic fossils
were discovered. The Jurassic and Cretaceous deposits of the middle course
of the Lena and its tributary, the Lindya, were studied by the author in co-
operation with Yu. M. Pashcharovskiy, and the Mesozoic deposits of the Aldan
Card l/ 4

Regional Stratigraphy of the USSR (Cont.) SOV/l5o6
River in cooperation with V.A. Smwlina. The following geologists, working in
the area of the Vilyuyskaya Depression and on the periphery of the Priverkhoy-
anskiy [Verkhoyansk] Dcrvinwarp, participated in collecting informtion presented
in this volume: G.V. Barkhatov, T.I. Bedrina, G.I. Bushinskiy, V.S.Vysbemirskly,
.N.P. Yegorova, G.K. Zemskova, N.A. Ignatchenko, A.Ye. Kiselev, A.G. Kossovskaya,
Z.K. Korollkova, A.I. Kyanno, V.M. Yellnikov, V.I. Muravlyev, L.A. Nazarkin,
V.D. Nikiforova, S-N,. Panov, Z.M. Starostina, I.I. TUchkov, N.M. Chumakov. In
addition, outstanding contributions in collecting, identifying, classifying and
describing plant fossils vere made by senior laboratory assistant Ye.L. Lebedev,
G.T. Petrova, N.A. Bolkhovitina and V.A. Samylina. In addition to the 32 plates
depicting fossil plant specimens, there are 16 figures and 2 tables. There are
101 references of which 86 are Soviet, 10 English, 4 German, and I French.
TAJ31H OF CONTENTS:
Introduction
PART I
STMTIGHAPHY OF JURASSIC AND CBETACHOUS SEDIMENTS OF THE VILYUYSKAYA
DEPBESSION AND TER ADJACENT PART OF THE PRIVERKHOYANSKEY DOWNWARP
Card 2/ 4

Regional Stratigraphy of the USSR (Cont.) SOV15o6
I. Histo4cal Outline of Studies 7
II. Stratigraphy 13
A. Jurassic formations 13
1. Lover Lias (Mugutskaya series) 13
2. Middl Lias 17
3- Upper Liao 19
4. Middle Jurassic 22
5. Upper Jurassic 27
13 . Lover Cretaceous formations 35
0 . Upper Cretaceous formations 45
III. Certain Natures in the Development of Upper and Lower Cretaceous Floras
in North and Northeast Asia 58
IV. Geological History of the Vilyuyakaya Depression and the Adjacent
Part of the Priverkhoyanakiy Peripheral Downward in Jurassic and
Cretaceous Times 64
Card 3/4

Regional Stratigraphy of the USSR (Cont.) soVl5o6
PART II
DESCRIPTION OF UPM JURASSIC AND LOWER CRETACEOUS FLORA OF TO
VILYUYSKAYA DEMSSION AND THE ADJACENT PART OF PRIVERKHOYANSY-TY
PERIPH&RAL DOWNWARP 64
1. Algae 70
2. Ferns 72
3. Equisetacese 103
4- Cycadophyta 103
5. Ginkgoaceae 105
6. Coniferse u9
Bibliography
125
Notes to Plates 1-32 Depicting Upper Jurassic and Lover Cretaceous Fossil 129
Flora
AVAILABLE: Library of Congress
Card 4/4 *Vfal
5-5-59

i-
VAMIRAMEYNY, V.A.; SAXYLINA, V.A. `\1
71rat, find of a repreaentative of the genus Pachyptorle in the
U.S.S.R. Bot.zhur. 43 no.11:1611-1612 N '58. (MIRA 11:11)
1. Goologichoskiy inatitut AN SSSR. Mookvn t Botanicheakiy
institut im. V-L. Komarova AN SSSR, LeningrAd.
(Baraka.vevskeya--Pteridoopermae)

3(0)
AUTHORS: Vakhrameyev, V. A., Ya_--oshcnko, 0. P.
J
TITLE: The Upper Jur~as* flora of the Southern Re,-'~ions of the USSR
(0 verkhneyurskoy flore yuzhnykh rayonov Sr,!)R)
PERIODICAL: Doklady Akademii nauk SSSR, 1958, Vol 123, Nr 5,
pp 925 - 920 (USSR)
ABSTRACT: Macro-remains of Jurassic flora rarely occur in the Ukraine,
Crimea, Caucasis, and Middle Asia (Srednyaya Aziya). Even
where continental sediments are prevalent (Middle Asia) only
one locality rich in fossil flora is known: the villages of
Galkino and L-,ikhaylovka (-outheast end of the K~~ratau Mountain
Range) (Refs 2,8-10). The rocks which contain this flora
are assigned to the Lower Jurassic on the basis of Lower
Jurassic plants (Ref 10). On tile contrary, the finely bedded,
limy shales, containing plant, fish, and insect remains, were
considered as Middle 'Ref 6) and even Upper Juracsic (Ref 2).
Since the well known Upper Jurassic leafy plant remains of
the southern part of the USSR are lacking, elimination of
this unclearneas was impossible. In spite of previous un-
Card 1/3 successful attempts to extract spores and pollen, thu authors

The Upper Jurassic Flora of the Soutl,ern Rej.ono of the 207/~9-127~---43/50
USSR
were successful, (sample donated by A. I. Turutanova-Ketova,
village of Mikhaylovka). The pollen consisted of 94.6,04
Brachyphyllum (of various species, Fig 1), and 5-4~~j Pinaceae
and Cupresmecae together with rare Coniopteris spores. The
authors compare this with cimilar pollen assemblages of the
USSR (Ref's 1, 3-7, 11,12). They -irrive at the following
conclusions regarding the age of the calcdolomites of Karatau:
1) They belong to the Upper Jurassic according to 0. P. Yaro-
shenko. 2) The firn and Ginkgoacoae declined strongly around
the boundary betueen the 11-liddle and Upuer Jurassic and were
replaced by an abundant development of conifers with awl
or scaly formed needles. zit the same time Bennettites with
leather-li'~e leaves developed. 3) The origin of these floral
changes may be found in thedry climate, which prevailed over
southern Europe, Kazakhstan, and Middle and Central Asia
during the Upper Juras2ic- 4) In the regions of Eurasia
farther to the north (Ref 1), a distinction between the flora
of the Middle and Upper Juraf--.qic is scarcely recogniz,7ible;
there, the climate remained moderately arm and damp. 5) In
Card 2/3 this connection, a study of the Up-,er Jurasoic spore-pollen

The Upper Jurassic Flora of the Southern Rejons of 5011/2o-12. Z_5_47 /50
the USSR
assemblages of southern Europe would be of interest. There
are I figure and 12 references, 10 of which are Soviet.
ASSOCIATION: Geologicheskiy institut Akademii nauk SSSR (Geological Insti-
tute of the Academy of Sciences,USSR) Moskovskiy gosudarst-
vennyy universitet im. M. V. Lomonosova (Moscow State Uni-
versity imeni M. V. Lomonosov)
PRESENTED: July 25, 1958, by A. L. Yanshin, Academician
SUBMITTED: July 24, 1958
Card 3/3

BOLKHOVITINA, Hatallya Androyevna; VAKHRAMMV, V.A., otv*rmd.;
PECHENYUK, I.L., red. izd--*-v~;'-UL-TAMTA-, -0.G.. talchn.rad.
[Spore and pollen complexes In Mesozoic deposits of the
VilyW deprossion and their stratigraphic significance]
Sporovo-MrIlts.avye komplakey mezozoiskikh otlozhmnii
Viliuiskoi vpadirq I Ikh znachanie dlia stratigrafii. Hoskwe.,
Izd-vo Akad.nauk SSSR, 1959. 184 P. (Akademiia nauk SSR.
Geologicheskil institut. Trud7, no.24) (MIR& 13;2)
(VilyW Vall"y-Palynology)

MJBINSHTEYN, G.A. [tranalatorj; VAKHRAKS-7ZV, V.A., red.; YAKOVENKO, M.Ya.,
red.; ARTEMOVA, Ye. , tekbn-.-r-e-d`.--
(Stratigraphic guidebook: Japan] Stratigrafichaskii spravochaik:
Uponiis. Moskva, Izd-vo inostr.lit-ry, 1959. 2o6 p. Translated
from the English. (MIRA 13:9)
1. International Geological Congress# 22nd.
(Japan--Geology, Stratigraphic)

ORLOV, Tu.A., glavnyy red.; RAUZXR-CHXRNOUSOVA, D.M., otv.red.toma;
FURSKUKO, A.V., otv.red.toma; XARKOVSKIT, B.F.. zan.glaynogo red.;
RUZHKNTSKV, V.Te., zam.glavnogo red.; SOKOLOV, B,,S., zam.glavnogo
red.; VAKHRAXMV. V.A.. red.; GXXXXCH, R.F., red.; (ROMOVA, V.I.,
red.; DAVITASHVItr,-L.3h., red.; KRTMGOLITS. G.Ta.. red.; LUPPOV.
N.Po, red.; GBRUCHEV, D.V., red.; OVECHKIN, N.K., red.; PGMYSKAYA,
I.M., red.; PCHBLINTSEV, V.P., red.; RADCLUKKO, G.P., red.; RODEN-
DORF, B.B., red.; ROZnESTVZNSKIT, A.K., red.; SARYCHEVA, T.G.,
red.; MBBOTINA, N.N., red.; TAKHMADZHAN, A.L., redo; rLNROV~ K.K.,
red.; KHABAKOV, A.V., red.; CHEMSHEVA, N.Te., red.: EBERZIN, AoGo,
red.; KOTLYAREVSKATA, P.S., red.izd-va; MOSKVICHEVA. N.I.. takhn.
red.; POLENOVA, T.P., tekhn.red.
[Fundamentals of paleontology; reference book in fifteen volumes
for paleontologists and geologists of tho U.S.S.R.] Osnovy pale-
ontologii; spravochnik dlia paleontologov i geologov BSSR v
piatuadtoati tomakh. Moskva, Izd-vo Akad.nauk SSSR. Vol.l.
(General part. Protozoal Obahchaia chaet'. Prosteishie. Otv.red.
D.M.Rauzer-Chernousova, A.V.Fureenko. 1959. 481 po (MIRA 12:7)
(Protozoa, Fossil)

VAKDAMM, V.A.; VASPIA, R.A.
Lower Jurassis and Anlenian floras of the Northern Caucasus.
Palsont.xhur. no.3:125-133 '39. (WRA 13:4)
1. Geologicheakiy institut Akademli nauk SSSR.
(Caucasus, Nartbern-PalisobotarV, Stratigraphic)

Lower Cretaceous plants from Lake Khanka (Maritime Territou).
Bot. shur. 44 no.7:997-1000 J1 '59. (KRA 12:12)
I,Geologicheakiy institut AN SSSR, Moskva.
(Khanks, region--PaleobotanT)

MATVETZVSKATA, A.L.; IVAHOVA, Ta.F.; VAKHRAMETZT,._V.A.. otv.red.; ZATTSKY,
N.S.. otv.red.; KULIKOT, H.T.. red.ird-va; KRUGLIKOVI, B.A..
takhn.red.
(Geology of the southern part of the West Siberian Plain in
connection with its oil and gas potentials] Geologicheskoe
stroenie iuzhnoi chasti Zapadno-Sibirskoi nizmennosti v aviazi
a voprosami neftega2onosnosti. Moskva, Izd-vo Akad.nauk SSSR,
1960. 263 p. (MIRA 13:7)
1. Zapadno-Sibirskiy filial AN SSSR (for Matvayevskaya. Ivanova).
(West Siberian Plain--Patroleum geology)
(West Siberian Plain--Gea, Natural--Geology)

OPLOV, Yu.A., glavnyy red.; MARKOVSKIY, B.P., 28M.glavnogo red.;
RU=.NTSHV, V.Ye., zam.glavno--o red.; SOKOLOV, B.S., zam.glavnogo
red.-, URYCHEVA, T.G.. otv.red toma; VArmalwXly A.A.. red.,
GRUM. R.F., red.; GROMOTA. V:I., red- -; DATITASHVILI-. L.Sh.. red.;
KRYMGCL'TS, G.Ya., red.; LUPPOV. H.P., rod.; OBRUCHEY, D.V.i red.;
OVECHKIN. N.K., red.; PCKROVSKAYA, I.N., red.; PCHELDITSEV, V.F.,
red.; RADOIDMO, G.P., red.; RAUZIM~CMUIOUSOVA, D.M., red.;
ROISNDORF, B.B., red.; ROZflMSTVENSKIY, A.K., red.; SUBBOTDA,
N.H., red.; TIUWAD2HAH, A.L., red.; FLEROV, K.K., red.; FM-;P 0,
A.V., red.; KRABAKOV, A.V.. red.; CHONYMWA, N.Ye., red.;
NBERZIN, A.G.; NZVESSKAYA, L.A., red.izd-va; POLENOVA, T.P.,
tekhn.red.
[Fundamentals of paleontology; manual in fifteen volumes for
paleontologists and geologists of the U.S.S.R.] Osnovy paleonto-
logii; spravochnik dlia paleontologov i geologov 330 v pistnadtsati
tomakh. Moskva, Gos.nBuchno-takhn.izd-vo lit-ry po geol. i okhrane
nedr. Vol.7. [Polyzoa, Brachiopoda. Supplement: Phoronideal
Mshanki, brakhiopody. Prilozhanie: Foronidy. Otvet.red.T.G.
Sarychava. 1960. 342 p. plates. WRA 14:4)
(Polyzoa, Fossil) (Brachiopods. Fossil)
(Phoronides, Fossil)

CHLOV, Yu.A., glaynyy red.; RARKOVSKIY, B.P., zam.,,,,lvvnogo red.;
V.Ye., zameatitell glavnogo red.; SOKOLOV, B.S., znmotitel' glavno-
go red.; REERZIN, A.G., otv.red.toma; KIPARISOVA, L.D., red.;
SHIMANSKIY, V.N., red.; VAKHRAKEYEV. V.A., red.; GEEXM, R.F._, red.;
GROMOVA, V.I., red.; DAVITAM7rLT-,-L-.`S1T., red.; KRYMGOLITS, G.Ya.,
red.; LUPPOV, N.P., red.; OBRUCHXV, D.V., red.; OVECHKIN, 11.K.,
-red., POKROVSICATA, I.M.. red.; PCIMIDTSEV. V.P., red.; RADCHEMO,
G.P., red.; RAU2M-CfDWOUSOVA, D.K., red.; RODENDORF, B.B., red.;
ROZHDESTVENSKIY, A.K., red.; FTMOV, K.K., red.; FURSENKO, A.V..
red.; THARA OV, A.V., red.; CHERNYSTAVA, N.Ye., red.; KORBE, K.B.,
red.izd-va; POLENOVA, T.P., takhn.red.
[Fundamentals of paleontology; reference book in 15 volumes for
paleontologists and geologists of the U.S.S.R.] Osnovy paleonto-
logii; spravochnik dlis paleontologov i geologov SSSR v piat-
nadtsati tomakh. Moskva, Izd-vo Akad.nauk SSSR. V01-3. [Mollusks:
Loricata, Bival7ia, Scaphopodal Holliuski - pantsirnye, dvu-
stvorchatye, lopatonogie. Otvet.red. A.G.Bberzin, 1960. 299 p.
(Mollusks, Fossil) (miRA 14:1)

KOSSOVSXAYA# A.G.; SHUTOVt V.D.f MMV,'YEVj V.I.j VAKWUME)ZVj V.Aej
otv.red.; GALUSHKOp Ya.A., red,izd-val GUrMApT.V-.q*WbftI.I*d.
[Mesozoic and upper Plaeozoic sedi~nsnto in the western Verkhoyansk
Range iEnd Vilyuy Lowland] ?4ezozoiskie i verkhnepaloozoiskie
otlozheniia Zapadnogo Verkhoianlia i Viliuiskoi vpadiny. Moskva,,
Izd-vo Akad.nauk SSSRp 1960. 274p, (Akademiia nauk SSSR,
Geologicheakii institut. Trudyp no. 34) .(NM 14:2)
(yakutia--Sediments (Geology))

MASLOVq Vladimir Fetrovichj SHATSM, IT.S.# akademikv glavnyy red.;
otv.red.; ZELENOVI K.K.9 otv.red.;
IIIIHAP N.S., red.izd-va; KUZIMIN, I.F.9 tekhnared,
[Stromatolites; their genesisp mothod of study, relation vith
faciesp and geological significancep based on studies of
Ordovician deposits of the Siberian Platfom] Stromato2ityj ikh
genezial,metod izuefteniia) aviazI a,fataiiami I geologicheskol-
znachenie na primere ordovika Sibirskoi platformy, Moskva# Izd-
vo Akade wukSSSRj 1960. 186 p. (Akademiia nauk SSSR,
Goologicheskii fnatituto Trudyl no. 41) (MM '14:2)
(Siberian Ratfom-Strcmatolites)

BEZATIVSKIY, N.A.; VAKHRAMEYEV, V.A.; GORSKIY I.I.; NALIVKIN, D.V.;
OVEGHKOI N.Ko; 5616100 V'. __
Reoults of the An-China Stratigraphic Confbrence; Poking, llavember
13-21, 1959. Sov. geol. 3 no.2:149-160 F 160. (MIRA 13:11)
1. Ministerotvo geologii i okhrany nedr SBSR AN SSSR.
(China-Goology, Stratigraphic)

,-VAXHR"1E1MV, V. A.
Stratigraphy of Jurassic and lower Cretaceous continental oedi-
mente In Zastern Siberia lind the Yar Zaqt based on paledbota-
nical data. Sov. geol. 3 no-7:82-94 J1 ;60. (MIRA 13:8)
1. Geolcgicheakiy imtitut AN SSSR.
(Siberia, Eastern-Phledbotany, Stratigraphic)

VAKKRAMM, V.A,, doktor geolvmin,nauk
All-Chinass Confarenoo on Stratigraphy. Vest.AN SSSR 30 no-5i
75-77 Vest.AN SBSR 30 no,5:75-77 mr 160
(MiRA 13:5)
(China-Geolo". Strattgraphle-Congresses)

VAKHRAMEM, V.A., doktor geol.-mineralonauk
- ~- -, . - ;- 1;'~ -t
Conference of the Czechoslovakian Society of Geologinto and Mineral-
ogists. Yest.AN SSSR 30 no-12:82-83 D 160. (HIPA 13:12)
(Czechoslovakia--Geoloe7, Structural-4ongreseea)

all
0.
FH L
PA
~i i
la.
6
fi.
far
2

VAKHIWSYEV, Vsevolod Andreyevich; DOLUDENKO., Mayya Prokoflyevna;
-------OT-L-YA&VSKAYA, F*S. redeizd-va; GUSIKOVA, O.M., tekhn.red.;
MAICOGONOVA., I.A... teL~.red.
(Upper Jurassic and the Lower Cretaceous flora of the Bureya
Basin and its significance for the study of stratigraphy]
Verkhneiurskaia i nizhnemelovaia flora Dureinskogo baBseina
i ee znachenie dlia stratigrafii. Moskva, Izd-vo Akad.nauk
SSSRt 1961. 134 pe (Akademiia nauk SSSR. Geologicheakii
institute Trudy, no,,54). (1,aRA 15:3)
(Bureya Valley-Paloobotanv, Stratigraphio)

BOLKHOVITINA, Natallya Andreyevna; SHATSKIY N.S. I akademik (deceased];
VAKHRAMEYEV, V.A., otv.red.; POPOVA: S.T. red.izd-vaj SHEVCHENKO.,
[Fossil and recent spores of the family Schizaeaceael Iskopaeuve i
sovremennye spory semeistva skhizeinykh. Moskva,, Izd-vo Akad.nauk
SSSR) 1961, 175 P. (Akademiia nauk SSSR. Geologich~skii institut.
Trudy,, no.40). (MIRA 14:5)
(Ferns) (Spores (Botany))

DRUSHCHITS.,Vladimir Vasil 'yevich; YAKUBOVSKAYA, Tamara Antonovna; --VAKMU,
--HMOML,-Y,A.y otv. red.; POMALENIKAYA, O.T., red.; LAZAREVA,
tekbn. red.
(Paloobotanical atlas) Faleobotanicheokii atlas. Moskva, Izd-vo
Mosk. univ... 1961. 178 p. (MIRA 14:10)
(Paleobotww-Laboratory manials)

VAKWMYEV, V.A.; MASILOV, V.A.
---
Domerian flm~a in the Horthern Caucasus. Puleont,.zhur.
no.3:103-108 961. (MIRA 15:2)
1. Geologicheskiy institut AN SSSR.
(Caucasus, Northern--PaleobotaxW)

RASSKAZOVA, Yelena Stepanovna; VAKHRUEYEV, V.A., otv.red.; CHEPIKOVA,, I.M.,
red.izd-va; SUSHKOVA,, L.- ~-p -
[Fossil flora of the Kata series in the Tunguska Basinj Iskopaemaia
flora katakoi svity Tungusakogo basseina. Wskva, Izd-vo Akad.
nauk SSSR, 1962. ~5 p. 32 platep (Akademiia nauk SSSR.
Geologichoskii inBtitut. Trudy, no.67). (MII(A 150)
(Tunguska Basin-Paleobotany., Stratigraphic)

VAKHRAMYEV V A
-
New Lower Cretaceous cycadophyte of Yakutia. Palsont. zhur.
no.3:123-129 162. (MA 15:9)
1. Geologicheskiy institut, AN SSSR.
(Yakutia-Cycadophytia)

ORLOV, Tu.A., glay. red.; YAXRC)VSKIY, B,P,, zam. glav. red.,
RUZHENTSEV, V.ye., zam. glay. red.; SOKOLOV, P,S,, zan.
glav. red.; VAKH k otv. red. ; RADCHENK0,
G.P.P red.; NOUN, A.L., red.; KOTLYAWVSKAYA,
P.S., red.izd-va; LAUT, T.G., tekhn. red.
(Fundamentals of paleontology; manual for puleontologi6ts
and geologists of the tn 15 volumes] Oanovy paloonLn-
logli; spravochnik cilia palcontologov i geologov SSSR v plat-
nadtsati tomakh. Yoskva, Izd-vo AN SSSR, Vol.14- (Algae,
bryophy-tes, psilophytales, lycoplda, arthrophytes, fernal Vo-
dorosli, mokhoobraznye, pollofitovye, plaunovidnye, chlenisto-
stebellnye, pnporotniki. Pod red. V.A.Vakhrameeva, G.P.Radchenko,
A.L,Takhpadzhana. 1963. 697 p. (MIRA 16:10)
I.Paleobotany, Stratigraphic)

MASLOV., Vladimir Petrovich; GOLLERBAKH, M.M., otv. red.; VAKHRAMEYEV,
V. A., otv. red.; PEYVE, A.V., glavnyy red.; MARKOV, M-.S'.', red.;
MENNER, V.V. , red.; TIMOFEYEV, 1I.P., red.; VANYUKOVA, O.Mj. , rod.
izd-va; CUSIKOVA, O.M., tokhn. red.
(Introduction to the study of fossil charophytes.] Vvednie v
izuchenie iskopaemyAh kharovykh vodoroslei. Moskva, Izd-vo Akad.
nauk SSSR, 1963. 103 P. (Akademiia nauk SSSR. Geologicheskii
institut. Trudy, no. 82). (MIRA 16:11)
1. Chlen-korrespondent AN SSSR (for Peyve).

ORLOVI Yu.A., glav. red.; TAKHTAIYLHYAN, A.L., otv. red.;
VAKLHM=X,-M-A., red.; RADCHENKO, G.P., red.; SHVEDOV,
red.; VASILEVSKAYA, N.D., red.; TUR[JTANGVA-KEMVA,
A.I., red.; MURAVIYEVA, O.A., red.; POKROVSKAYA, I.M., red.;
YATSENKO,.KHMELEVSKIY, A.A., red.; GOROKHOVA, T.A., red. izd-
va; GUROVA, O.A., tekhn. red.
[Fundamentals of paleontology; manual for paleontologisto
and geologists of the U.S.S.R. in 15 volumes] 0snovy paleon-
tologii; spravochnik dlia paleontologov i geologov SSSR v
piatnadtsati tomakh. Glav. red. IU.A.Orlov. Moskva, Izd-vo
AN SSSR. Vol-15-(Gymnosperms and angiospersm) Golosemennye
pokrytosemennye. 1963. 742 p. (141RA 16:11)
(Gymnosperwi, Fossil) (Angiosperms, Fossil)

ZAKLINSKAYA, YelenA lkpitriyovna; VAKHRAHEYEV, V.A., red.; GOLUBEVA, L.V., red.;
CHEPIKOVA, I.M., rediizd-va; KASHINA, P.S., tekhn.red.
[Angiosperm pollen and its stgnificance for the stratigraphy of the
Upper Cretaceous and Paleogene] PylItsa pokrytosemiannykh i ee znachenie
dlia obosnovaniia stratigrafii verkhnego mela i paleogena. Moskva,
Ixd-vo Akad. nauk SSSR, 1963. 255 p. fo'd. diagrs. inserted. (Akademiia
nauk SSSR. Geologicheskii institut. Trudy no.74). (MIRA 16:10)

VAKIIRAI T.A.; PEYVF, A.V., glavnyy red.; KIIZNETSOVA, K.I., red.;
SIM-1EMi
wrPFIR) V.V., red.~ Tl,'.IOF7Y"I, P.P., red.
P
[Jurassic and Early Crotaceous florns of Furnsin and tho
paleofloristic provinces of this period]. IUrskie i
rannemelovye flory Fvrazii i paleofloristicheskie pro,iintsil
etogo vremeni. 14oskvrt, Izd-vo "Nanka," 1961~. 260 p.
(Akademita nauk SSSR, Goologicheskil Ingtitut. 102)
(MIRA 17:6)'
1. Chlen-korrespondent AN SSSR (for Peyve).

v ~ -1, 11. 11
rIv v ti.
"Recent studies on the Devonian floras of Siberia."
report submitted for 10th Intl Botanical Cong, Edinburgh, 3-12 Aug 64.
AS USSR, Moscow.

V=WNEYEV, V.A., otv. red.; SHVEDOV, N.A., otv. red.; VANNUKOVA,
red.
[Gondwana] Gondvana. Mosl-va, Izd-vo "flauka," 1961,. 139 p.
(Its: Doklady sovetskikh geologov, Problema 9) (MIRA 17:9)
1. International Geological Congress. 22d, 1964.

VAKTROIE-YElly A.
F( leogs, CF.

JEAMi, doktor geol.-mineral.nauk
W
Marjan RaciborBki; on the 100th wmivereary of his birth. Vast.
AN SSSR 34 no. 1:98-99 Ja 164. (MIRA 1715)

YAROSHENKO, 011ga. Pavlovna; VAKHRAMEYEV,, ~_, otv. red.; PFYVE, A.V.,
akademik, glavnyy red.; KUZNETSOVA, K.I., red.; MENNEER, V.V.,
red.; TIMOFEYEV, P.P., red.
spores and pollen complexes of Jurassic and ToWer Cretaceous
deposits of the Northern Caucasus and their stratigraphic
importance.) Sporovo-pylltsevye kompleksy iurskikh 1.
nizhnemelovykh otlozhenii Severnago Kavkaza i ikh strati-
graficheskoe znachenie. Moskva, Nauka, 1965. 107 p. Illus.
(Akademiia nauk SSSR. Geologicheskii institut. Trudy, no.117)
(MIRA 18:11)

LEBEDEVP Yevgeniy Leonidovich; Y_AaiaAa'XLN,,- V.A., otv. red.i PEYVE, A.V.,
akademik, glavnyy red.; EII/I&TSOVA, K.I., red.; MENNEIR, V.V., red.;
TIMOFEYEV, P.P., red.
(Late Jurassic flora of the Zeya River and the Jurassic-
Cretaceous boundary.] Pozdneiurskaia flora reki Zei I
granitsa iury i mela. Moskva, Nauka, 1965. 141 p. illus.
(Akademiia nauk SSSR. Geologicheskii institut. Trudy no.125)
(AIRA 18:11)

VAMWIEYEV, V.A.
------- . -
Sffu Haing-chien [11. C. Sze], 1901-1964; an obituary.
Paleont. zhur. n0-4:113 165. ('effiv.. 19: 1)

VAKI[RAMFYEIV) V.A..
First find of Jurassic flora in Cuba. Paleont. zhur. no.,-,:
123-126 165. (MIRA 18:9)
1. GEoljgIcheakiy institut AN SSSR.

BEZPALOV2 K.M.j__jAKffOM -,-~S-
)W
new stepless electric drive for the vertical glAso-draving machines
Stek. I ker. IS no. 3:4-7 Mr 161. (YJFA 14:5)
(Glass manufacture-Meotric equipment)

ARTES, N. A.; VASSKRWp L. M.; VAKROMEV, V. B., master katodnoy
sashchity .............................,
Group installation of electroch6mical protection anodes on
parallel pipelines. Suggested by K. A. Artes, L. M. Vasaerman,
V. B. Vakhromeev. Stroi. truboprov. 8 no&4*.28 Ap 163
(MIRA 161:0
1. Starshiy lnzh,, Zapadno-4libirskogo nefteprmWelovogo
upravleniya (for Artev). 2. Nachallnik uohastka tresta No. 8
(for Vasoorman).
(Petroleum pipalinse-cathodic protection)

170)
AUTHOR; Vakhrameyeva, I. A. SU'1/20-123-3-48/50
TITLEz 5velo~pment -ofth~e ~tioned Motor Reflexes of the Type of the
So-Called Voluntary Movements in Babies During the Fii-st Months
of Their Lives (Razvitiye uslovnykh dvigatellnykh ref..eksov tipa
tak nazyvayemykh proizvollnykh dvizheniy u detey pervykh mesyatsev
zhizni)
PERIODICAL: Doklady Akademii nauk SSSR, 1958, Vol 123, Nr 5,.Pp 944-9471 (USSR)
ABSTRACT*. The author has made it her task to clarify at which age the develop-
ment of the type of reflexes mentioned in the title is possible.
Furthermore, the peculiarities of the development of complicated
motor reflexes of this type in children during the first months
of their li'ves, and the degree of analyzing possibilities with
regard to motor activity a-t this age were to be studied. For the
study of the motor analyzer the modified device by Zhakoakiy (Figi)
was used. The baby's forearms were tied to rulers so that he could
bend his arms only at the elbows. A gentle rhythmical blowing of
air into the eye was us-ad as a conditioned stimulus. If an arm
bending angle of 1800 was obtainedg blowing was discontinued. If
0
1800 were not obtained, the arm was passively bent to 180 , Thus
Card 1/3 the unconditioned stimulus for the winking reflex was transformed

SOV/20-123-5-46/50
Development of the Conditioned Kotor Reflexes of thel~Ve of thc So-Called Voluntary
Movements in Babies During the First A"onthd of Their Li,,es
into a conditioned reflex, viz. into tt.u signal of the motor
reaction of the arm (Ref 7). The children's ages varied from
2 weeks to 8 months. It was shown that children up to the age of
1.5 months are unable to develop the reflexes mentioned in the
title. The author explains this phenomenon by the absence of a
functional connexion between the kinesthetic cells and the cor-
responding motor elements,~ However, even in 3-4-week-old children
the actual recipient part of the motor analyzer is sufficiently
far advanced tv develop a conditioned reflex to a proprioceptive
stimulus (Ref 2). The author has succeeded in developing motor-
conditioned reflexes in all the 50 children examined (ages 1.5 to
8 months). She differentiates among 4 successive stages of the
transformation of a passive movement into an active one. They
depend both on the degree of development of the conditioned motor
reflexes and on the age of-the child: 1) Slackening of resistance
to passive movement; 2) emergence of individual insignificant
(40-800) bending movements; 3) emergence of movements of consider-
able range (150-180?), with the "idle" arm in sympathetic motion
(stage of generalization); 4) stage of independent activity of the
Card 2/3 arm tested. In 1.5 - 2-month-old children, stages 1) and 2) are

JO V/20-12.'J-5-48/50
Development of the Conditioned Motor Reflexes of the Type of the 3o-Called
voluntary Movements in Babies During the First Yonths of Taeir Lives
very marked. This corresponds with a most primitive, rough analysis
of the proprioceptive stimuli. In 2 - 4-month-old children, stages
1) - 3) are clearly visible (Fig 2), In 4 - 5-raonth-old children,
all 4 stages had been developad, although stage 2~ Was less clear-
ly visible. In even older children ( r- -- 6 months), stages 2) and
.10
3) are less marked. Table I summarizes the results.- There are
3 figures, 1 table, and 11 references,, 10 of which are Soviet,
ASSOCIATION: Institut evolyutsionnoy fiziologii im, 1. b1, Sechenova Akademii
nauk 5SSR (Institute of Evolutionary Physiology inieni I.M.Sechenov
of the Academy of Sciences, USSR)
PRESENTED: August 4, 1958, by L. A. Orbeli, Academician
SUBMITTED: July 25, 1958
Card 3/3

VAKHW4EYEVA, I.A.
Develomenta-1 characteristics of the motor analysor in children
during tlhhtdr first months of life. Mat. po evol. fiziol, 4:5-13
l6o. (MIRA 13:10)
(INF~'IJITS) (MOVEMENTj PSYCHOLOGY OF)

and ex tensor m, usc--D~s of t~ lii~ -2
zhur. 49 no.4:/.49-.'.56 1- 7
1. From t1le Laboratory of WL,~,.qr
thlo Child, Sechpnciv In-3l't'ufA- ,f
Len~ngrad.

VAKMAMEMA. L. A.
"Precision of Plotting Isolines." Thesis for degree of Cand. Tectmical Sci. Sub
28 Apr 50, Moscow Inst of Engineers of Geodesy, Aerial Photography, and Cartegraphy
Summary 71, 4 Sep 52, Dissertations presented for Degrees in Science and Engineer
in Moscow in 1950. krom . Jan-Dee 1950.

Design4
VAKHRAMEYVIA, L. A. Cand Tech Sci -- '4WWwmbW of topographic viaps in the USSR
and various foreign countries." Mos. 1960 (Min of Higher and Secondary Specla-
lized Education RSFSR. Moo Inst of Geodoay, Aerial Photography, and Cartography).
(KL, 4-61, 195)
-a-

S/154/60/000/02/14/018
B012/B123
AUTHOR: Vakhrameyeva, L. A., Senior Teacher
TITLE: Some Investigations of the Formulas for Rectangular Coordinates
of Lambert's Conformal Conic Projection
PERIODICAL: Izvestiya vysshikh uchebnykh zavedeniy. Geodeziya i
aerofotos"yemkat 19609 No. 2. pp. 119-130
TEXT: Lambert's formula (1) for topographic mapmakin is often used
outside Russia, 'Since in the conformal conic projection the length dis-
tortion is quite large, the territory has to be divided into many small
parts..In this respect the author compares the formula of Driencourt (5)
with Roussilhe's formula (8), and states that the former is more advan-
tageou 8~ since the abscissas come out with greater accuracy than in for-
mula (a . ALrther development leads to formula (14). The author gives
an example for B 0 - 540 , and computes the values from formulas (1), (5),
(8), and (14). From this comparison the author concludes the following:
1) If one uses'Lambert's conformal conic projection in zones not exceeding
Card Card 1/2

S/154/6o/ooo/004,/006/007/XX
B012/BO54
AUTHOR-. Vakhrameyeva, L. A., Senior Teacher
TITLE: Comparison of Projections Used for Modern Topographic Maps
PERIODICAL: Izvestiya vysshikh uchebnykh zavedeniy. Geodeziya i aero-
fotos"yemka, 1960, No. 4, PP. 93-101
TEXT: In the present paper, the author compares three projections ueed
at present for topographic maps: Gauss-Krfiger's projection, Lambert's
conformal conical projection, and the stereographic projection. The form;;
las for these projections are compared. This comparison shows that
if the origin of coordinates coincides with the origin of the axial
meridional zone - the formulae for the orthogonal coordinates are nearly
equal, only differing by terms of the third order. It is also shown that
the introduction of an additionnI series reduces the accuracy of ortho-
gonal coordinates. With the aid of an example, it is shown that the ortho-
gonel coordinates of the stereographic projection are equal to the arith-
metic mean of the coordinates of Gauss-KrUgevs and of Lambert's projec-,
tion. The comparison made shows that the otareog-raphic projection exhibito
Card 1/2

Comparison of Projections Used for Modern 3/154/60/000/004/006/007/Xx
Topographic Maps B012/BO54
a smaller diatortion and a smaller linear and angulai reduction than the
two others. All projections studied exhibit small angular reductions in
absolute terms. They can be neglected in low-accuracy surveys. On the
other hand, Gauss-KrOger's and Lambert's projections are superior to the
stereographic projection as to the area represented, Gauss-Kruger's pro-
jection exhibits an additional advantage over the zso others, namely the
full identity of all zones. This advantage gave rise to the compilation
of detailed tablea to facilitate the use of this projection in the prac-
tice. In consideration of the merits of Gauss-.Xrflger~s projection, it is
expectpd to be used to a far greater extent in the future. There are
3 tables and 5 references: 3 Soviet and 2 French.
ASSOCIATION: Moekovskiy institut inzhenerov geodezii, aerofotcs"yemki i
kartografii (Moscow Institute of Engineers of GQodesy,
Aerial Photography and Cartography)
SUBMITTED: Pebruary 29, 1960
Card 2/2

VAKHRAMEYEVA,-L.A., starshiy prepodavatell
Prof. M.D. Soloy'sylo method for obtaini perspeetive
projections with multiple representations* Trudy HIIGAIK
no.47:117-126 161. (MRA 15:7)
1. Kafedra zatamaticheakoy kartografii Mookovskogo
institute, inzhenerov geodeziio aerofotos"yemki i kartografii.
(Map projection)

VAMMAVIE=A, M. G., Candidate Biol Sr'i (diss) -- "on the bioloor of the lFham-
Icafed'rAcer platanoidesjmple under various conditions of existame". Moscow,
1959. 18 pp (Moscow Order of Lenin an(I order of Labor Red Banner State U Im M. V.
Lomonosov, Soll-Biol Faculty, Chair of Goobotany), 120 copies (KL, No 23, 1959, 163)

VAKMUJMMA9 M.G.
Some observations an stands of the Norway maple (Acer platanoides L.)
grown from seeds of different geographical origin.Nauch.dokl.vys.shko1y:
biol,nauki noA152-156 160. (MIU 13:11)
1. Rokmendovana kafedroy geobotaniki Moskovskogo gosudarstvennogo
universiteta imo MoVeLomonosova.
(MAPLE)
(BOTANY--ZCaVJGr)

17 (4,10)
AUTHORS: Vakhrameyeva, N. A., Neyfakh, A.A. SOV/20-128-2-58//59
TITLE: A Comparison of Radio- and Thermosensitivity in the Process
of Egg Segmentation in MisgurnU3 f089iliS
PERIODICALi Doklady Akademii nauk SS3R, 1959, Vol 128, Nr 2, PP 429-432
(USSR)
ABSTRACT: The clarification of the effect of ionizing radiation on the
cell is principally based on the understanding of the specific
effe of this agEnt. On the other hand, the similarity of the
final ffect (mutations and chromosome aberrations) after such
manifold kinds of action as radiation, temperature increase2
or radiomimetic substances, prevents a judgment on its
specificity. The differences can only be determined by such
method which can inform on the real nature of interaction of
the harmful factors with the cell structures. Such a method
may be the comparison of sensitivity to various agents in the
course of cyclic changes, e. g. of those proceeding during
cell division. If the primary object of damage are chromozomes
while the result is the fracture of the latter, the differences
of interaction may be expressed in an unequal dependence on
Card 1/4 the state of damaged structures at the moment of action. At the

A Comparison of Radio- and Thermos ensi tivity in the SOV/20-128-2-58/59
Process of Egg Segmentation in Misgurnus fossilis
same time, the kind of change in radiosensitivity during the
mitosis has hitherto remained completely unclear. In the
present paper, the X-radiation was compared with the short-
termed effect of increased temperature. The experiment was
carried out as follows; from a vessel containing the spawn of
Misgurnus fossilis, 2 portions (of 200-250 eggs each) were
taken every 7 or 8 minutes at exactly the same time. The spawn
was in a stage immediately before the appearance of 2 blastomers.
One portion of spawn was irradiated while the other one was 0
heated. The further development of the spawn took place at 18
After the unfecundated eggs had been removed (stage of early
until medium blastula), the number of destroyed eggs was
determined in the stage of beginning mobility and before
slipping out. The radio- and thermosensitivity were expressed
in % of survival in comparison with the number of fecundated
eggs. Part of the material was fixed in the stage of gastrulation,
and the chromosome aberrations (Fig 2) were calculated from this.
This and figure 1 show that the sensitivity of eggs to radiation
Card 2/4 and increased temperature changes periodically. The rhythm of

A Comparison of Radio- and Thermosensitivity in the SOV/20-126-2-5_e/59
Process of Egg Segmentation in Misgurnus fossilis
these changes is in strict agreement with the division rhythm
of the egg. On the other hand, the periods of maximum radio-
sensitivity and radioresistance do certainly not agree with
those of thermosen3itivity and thermoresistance, respectively.
The kind of chromosome aberrations (Pig 2) was not very different
for these two effects. As had been ascertained before (Ref 9),
the curve offrequency of chromosome aberrations followed- also
in this paper - rather exactly the curve of mortality and the
frequency of deformations. This applied to both radiation and
heat. Figure 3 shows the dependence of the survival on the
frequency of chromosome aberrations. The number of destroyed eggs
is directly proportional to the frequency of chromosome aber-
rations. Thus, both radiation and heat, in low dosage, act upon
the nucleus. In case of high dosage, they also act directly on
the cytoplasm. V. N. Belyayeva and G. V. Pokrovskaya (Ref 9)
are mentioned in the text. There are 3 figures and 10 references,
6 of which are Soviet.
ASSOCIATION: Institut morfologii zhivotn,,kh im. A. N. Severtsova Akademii
nauk SSSR (Institute of Animal Morphology imeni A. N. Severtsov
Card 3/4 of the Academy of Sciences, USSR)

GOLOLOBOVP A.D.; VAKHRMIX.MrA, N.A.
Photometric determination of cobeIt in soils, va ers, and
plants using pyridylazore3orc:Lnol. ibchvovedenie no. 2-.
81-88 F 165 OURA 1931)
1. Vseaoyuznyy naucbno-issledovatellski-y institut zhivotno-
vodstra. %bm-Itted June 2, 1963.

VAKHRAMEYEVA, N.I.
State of the gums during pregnancy. Stomatologiia 41 no.4:24-27
Jl-Ag 162. (MIRA 15:8)
1. Iz kafedry terapevticheskoy stomatologii (zav. - prof. Ye.Ye.
Platonov) Moskovskogo meditsinskogo stomatologicheskogo instituta.
(GUMS-DISEASES) (PREGNANCY)

BUKHTANOV. I.M.; TSARIKOV.. G.A.; nMMOV, Y.K.; KATSHR, B.M.;
VAMIRLNUMA. T.M.; TRIT'TACHEM, S.Ya.
Rubber coatings and belts for draw boxes on spinning machines.
Tekst.prom. 19 no.2:20~24 F 159. (MIRk 12:5)
(Spinning machinery) (Rubber coatings)

USSR/Geolog~ " Georbemistry
Card 1/1 jub. 22 - 25A0
Authors iVakhrameyeva, V. A.
Title 1The-1,,4ihesfs' 'of glauberite in salt deposits of the Kara-Bogaz-Gol Bay
Periodical :Dok. AN SSSR 99/2, :281-284, Nov 11, 1954
Abstract i Geological data are presented regarding the genesis of glauberite (calcium
sodium sulfate), discovered in the salt deposits of the Kara-Bogaz-Gol Bay.
The three stages of formation of glauberite crystals are described. Nine re-
ferences: 6-USSR; 2-German and 1-USA (1877-1953). Illustrations.
listituti6n All-Union Scientific Research Institute of Halurgy
Presented by: Academician D.S. KDrzhinskiy, September 8, 1954

15-57-7-9.314
Translation from: Referativnyy zhurnal, Geologiya, 1957, Nr 7,
pp 81-82 (USSR)
AUTHOR: Vakhra . A
TITLE: The Mineralogy and Petrography of the Salt Deposits of
the Gulf of Kara-Bogaz-Gol (K mineralogil I petrografii
solyanykh otlozheniy zaliva Kara-Bogaz-Gol)
PERIODICAL: Tr. Vses. n.-i. in-ta galurgii, 1956, Nr 32, pp 67-86
ABSTRACT: A mineralogic and petrographic study of drill cores
from Kara-Bogaz-Gol has shown that the Caspian Sea
stood at a high level for at least two long periods of
time and at a low level for three periods during the
interval when this investigated section (up to 40 m
thick) was being formed. During the highest stand of
the salt water, carbonate-ciay rocks were deposited.
At this time, despite the high salt content (and the
periodic precipitation of mirabilite), there existed
an abundant fauna and full-grown seaweed. Glauberitic
Card 1/3 rocks began to form during evaporation of the brine.

The Mineralogy and Petrography of the Salt (Cont.)
15-57-7-9314
Further evaporation was accompanied by precipitation of halite,
followed by astrakhanite (bloedite) and, locally, by epsomite.
Between the modern period of dryin -up of the gulf, beginning
with the twenties.of our era Isic.1i and the two pre-
ceding periods, there occur marked facies changes and fundamen-
tal differences. Detailed mineralogic and petrographic descrip-
of the salt-bearing rocks--carbonate-gypsam, glauberite,
hali.te, astrakhanite, and epsomite--have permitted the author
to interpret their genesis. Despite the complexities in the
origin of glauberitic rocks the author, at the present stage
of study, has already noted several ways in which glauberite
crystals may form. These are: 1) seasonal deposition from the
brine of fine-grained glaugerite, simultaneously with, or
immediately after, deposition of calcium and magnesium carbon-
ates; 2) early diagenetic formation of medium and coarse-grbined
light-colored glauberite, derived from other minerals (mirabi-
lite or natrosyngenite); 3) rapid recrystallization of massive
precipitates (in several examples) of unstable forms of sodium
and calcium sulfates, resulting in unbedded white fine-grained
Card

The Mineralogy and Petrography of the Salt (Cont.)
15-57-7-9314
and extremely porous glauberite; 4) formation of unstratified,
coarse-grained, highly porous glauberite, apparently forming by
slou solution of massive precipitates of mirabilite (especially
in "fruitful" years); 5) growth of glauberite crystals from
solutions which are supplied from bottom sediments (carbonate-
gypsum rocks underlying brown clays). Differences in form
between the pores in glauberitic and halitic rocks indicate
that the causes of each were independent. The astrakhanite
rocks formed both by direct precipitation from the brine, in
small crystals, and by early and late diagenetic processes,
in large crystals ranging up to 5 cm and 7 cm in beds up to
1 m thick.
Card 3/3 S. M. Korenevskiy

15-57-8-11309
Translation from: Referativnyy zhurnal, Geologi:,a, -1957, lir 8,
p 171 (USSR
-V jhrama*&ua,_V. A.
AUTHOR:
TITLE: Stratigraphy and Tectonics of the Verkhne Kamensk
Deposit (K stratigrafii i tektonike ~erkhnekamskogo
merstorozhdeniya)
PERIODICAL: Tr. Vses. n.-i. in-ta galurgii, 1956, Nr 32, pp 277-
313
ABSTRACT: The author gives the results of macroscopic individual
study of strata A, B, and C, and also of the upper 16 m
layer of the "lower" rock salt of the Verkhne Kamensk
deposit. The study was conducted from cores of a
number of Solikamsk and one Klepikovskaya skvazhina
(bore hole), at the mining operations of the Solikam
and Bereznik mines. The stratigraphic (but not
Card 1/4 lithologic) cross section of the productive series is

Stratigraphy and Tectonics of the Verkhne (Cont.) 15-57-8-11309
maintained over a distance of about '00 km (from Klyepikovo to
Bere,zniki) in many cases with exactness up to one annual layer; in
the clay seams the accuracy of correlation is as high as 1 mm. The
thickness of the annual layers of the lower rock salt is from 2 cm
to 10 cm, Half of the annual layers (51 percent) are represented
by four seams: 1) clay; 2) halite (skeletal-crystalline, smudged
with clay); 3) halite, skeletCal crystalline, clear; and 4) halite,
colorless or rose-colored. Other annual layers of the salt consist
of a smaller number of' these seams, rarel-- in a different sequence.
Stratum A in all operations of both mines Is represented by banded
sylvinite. It is composed of 40 annual layers consisting of laminae
as follows: 1) clays U mm to 3 mm); 2) halite (10 mm. to 30 mm); .
and 3) sylvite (10 mm to 30 mm), with sometimes an additional lamina
of halite, or more rarely, sylvite, on top. Slight facies changes
are associated only with the size, the form of crystal, and the
difference In shades of coloring of the sylvite and halite. Stratum
C is composed chiefly of carnallite and, in the east and southeast
deposits, of variegated sylvinite. Its lower layers are sometimes
Card 2/4

15-57-8-11309
Stratigraphy and Tectonics of' the Verkhne (ConL.)
composed of carnallite, sometimes of variegated sylvinite. (Cl is
often composed of variegated sylvinite, while C2 and C3 are usually
different * In all strata the amount and even the thickness of the
clay and halite Layers Is maintained, and only the thickness of the
sylvinite and carnallite seams varies. Shearinp
,, ands in part, tile
second phase of shearing, that is, flow and gradual destruction, had
the greatest importance in deformatiun of saline minerals of the
Verkhne Kamensk deposit. As a result of greater 'plasticity of the
carnallite, the proces,-,/of'fold formation occurs more intensively in
the carnallite zone than in the zones of sylvinite and rock salt.
The secondary folding of the carnallite is of a chevron form. In the
anticlinal parts of the large folds, the accumulations of the
chevron folds increase the thickness of the separate layers. For
example, the thickness of stratum C increases five to six times. In
the synclinal parts, on the other hand, a squeezing out of the rock,
occurred, chiefly from the middle part of stratum C. In the area
of the Bereznie mining district, located on the anticline of the
Card 3/4

15-57-8-11309
Stratigraphy and Tectonics of the Verkhne (Cont.)
large Churtanskaya brakhiantiklinall (brachyanticline), the original
carnallite layers are thin, and the dislocations ended with formation
of fblds which 6nly slightly faulted. In the area of the Solikamsk
mining district, located on the western limb of the brachyanticline
of the same name, the carnallite rock appears at first glance to be
irregularly brecciated. Detailed study has shown that disruptions
of the annual layers and of their separate sections, and also second-
ary folding, occurred here as a result of gradual migration of the
latter into the anticlinal parts of the large folds, In layers
removed from the more inert sylvinite zone, the carnallite rock had
a-greater mobility and drew with it layers of rock salt. Under the
action of tectonic deformations in the carnallite rock, however,
real changes of the mineralogical composition did not occur. The
secondary carnallite and halite were formed only in small sectors
around the mass of the brecciated stratum C--D and sometimes in the
limbs of the folds.
Card 4/4 S. 14. Korenevskiy

VAKHW=A, V.A., M.L.
VOROITOVA I
Luneburgite from Kara-Bogaz-Gol and Uzun-Su. IrLCiy VIIIIG
no.40:330-336 160. (MIRA 14 - 1-1)
(Kara-Bogaz-Gol(Guef)--Luneburgite)

VAKHR.41EYEVA, V.A. ; GORIWN, O.Y.
Petrography of rocks in the underlying and lower salt Layers.
Trud,v VNIIG no.Wi.371-391 160. WIIM 14: 11)
(Kama Valley-Salt deposits)

ALEKSANDROVA, M.A.; ASIIIOVSKIY, E.I.; BALANDIN, V.V.; BRODYANSKIY,
V.M.p kand. tekhn. nauk; VAKHPAK e.A.; VERBA, M.I.,
kand. tekhn. nauk; VORONII., T.A., kand. tekbn. nauk;
GIRSHFELID, V.Ya., kand. tekhn. nauk; DEYCII, M.Ye., prof.
doktor tekhn. nauk; IVIN, F.A.; LAPSHIYj, M.I.0 kand. tekhn.
nauk; LIFOV, Yu.M.,, kand. tekhn. nauk; LYUBARSKAYA, A.F.j
MAKARENKO, I.D.- MIRIMOVA~ V.M.; NZVLER, S.Ye,; ROZANOV,
K.A., kand. tekhn. nauk; ROTACH, V.Ya., kand. tekhn. nauk;
KHMMINITSKIY, R.Z., kand. tekhn. nauk; SHEVCHENKO, E.G.;
BOGOMOLOV, B.A., red.; VAYNSHTEYN, K.N., spets. red.;
LICHAK, S.K., spets. red.
(German-Russian heat engineering dictionary] Nemetsko-
russkii teplotekhnicheskii slovar'. Moskva, Sovetskaia
entsiklopediiaj 1964. 512 p. (MIRA 18:1)
1. Moscow. Energeticheskiy institut. 2. Moskovskiy energe-
ticheskiy institut (for all except Vaynshteyn, Lichak).

t~l L- ~E- iM ef- - f I
USSR/Cultiva'.-:~C. rlaonvs Frui-~s. ~ xri-.S.
U 44270
Abs Jour -".'Lo2.., Ilo 1-0, 1~52,
Author in,
Inst P- ~.---:,navcOsk Uiafversj. y.
Titl-~- C,2.-, .~-. .,-.,.clding wit.i '~- -~ T~s- A-L,.;dnes.
Or i Ig Elf 1 namic'-n. ra)ot s*6--c. l--.-;:c)wv.,:,dskogo
37-95
-j -tr wern. Co.. ek,,-c .-0.. at -'&*Ile sulanz
s act,
~71',) witil V'(2 u,:
!7=o]:dinr,0 cja d -lo-ped by
W~47) and R.H. (1049). A-'U- tl-~~- .:,"A
J,, c it r- -)laced in C, fl wf-
(57 c 1) cm oi~ noil a-A C
W-r. r, li~- averagL i,c
Card 1/2

s jour 276
---d in L -:v wa.; 2211
.or,.. va,'.
0-L'
17 -ea cu, i',Ligs al-, -.-aC...
lar ve~ it i la on w-:; niarl
fra G were U~
c- v ic i -orjk r), wo.3 -lrlv
(con-trol
Aj k'ap
case- o'L it-as 31" (c:).l-r,-l
'tl' anc'. in cct""-~ ci-- percolli-a--n, IfIns 1:121
(co-,-rol
Car(I 2/2
I Sj 7

TAKHRAMFMA; Z.H.
Structure of the head in now forma and Its relation to the genetic
propinquity of the parents. Trudy Kar.fil.Aff SSSR no.17:38-46 159.
(MIRA.13:4)
(Grain brooding)

VADRAWMA, Z.H.
Some data on variety test,& ior new types of wheat in 1957. Trudy
I Kar. fil. AN SSM no.2993-7 161. (MIRA 15:2)
(Wheat. -Arleties)

VAFjjp.Ay,n,j,
A t-l'uhment fo-:- grinairip 1'~jrx cj ' tern. MaPM I ioitrc, I tel 1 rv~-&t
26 Apt 64 It 141 RA I? V7 )

-Y-gTtATVj P.P.
Reducing auziliary time in machining special pins.
Mashinostroitell no. 509 Yv 164. (MIRA 17:7)

P.!'~
c1.c-, for sInaz-penina fo-aing IJ.
nn.'12.,21. 164.

S/058/63/000/002/062/070
A1601A101
AUTHORS: Zorkin, A. F., Tereshcheako, A. I., Vakhraneva, L. F.
TITLE: Dispersion equations for uniformly bent waveguides of a complex
cross-section shape with lugs on the plane wall sides
PERIODICAL: Referativnyy zhurnal, Fizika, no. 2, 1963, 25, abstracT, 2Zh156
C'Uch. zap. Eharkovsk. un-t", 1962, v. 121, Tr. Radiofiz. fak. 5,
74 - 83)
TEXT: Or. the basis of the solution of Maxwell's equations, dispersion
equations were obtained for uniformly bent H, r1, T and cros!~-shaped waveguides
with lugs on the plane walls of the bend. The characterisLic equations for de-
termining the critical frequencies were obtained as a particular case of dis-
persion equations. The obtained equations are true for any bend radii. The cal-
culations of the critical frequencies were experimentally checked. The checking
confirmed the correctness of the theoretical conclusions.
[Abstracter's note: Complete translation]
Card 1/1

BARASHKOVI G.K.j VAKIHO,2HINA,
-- I n the Zelorel-311-aY-~L B-Y
OvergrOvIL.h Of a raft b.,-v !.azDiarla saczla-jna ' Irl
~-l -,-n
f>,,, tha Barantr, -Sea. 49 no.1111-651- LC~..C H 164. OcaA
:.1, Murmwiak,'y morskoy blologiche5kiy inbUtut, Dallniya Zelontsy,
Rurmanskoy ob2ast'.o

"-jnvint of nitrcran frjbctanv~sc in =a-;rrzh-.yte- -i-grt~ tf
Mi~--zw-n Coast, F~rikl. -:)!.(,khim. i
165.
.i. Mjrm,-r)zk-:.y iavrckc-.~, blolcg~ch-~ekiy Jwltltut il'.cl lislvrog:,
f I .:,-a la AN SSS R.

T. 2473R-M rtjT(l) A(iTg -M
ACT W D6015521 SOURCE CODE: UR/0411/65/001/004/0469/0471~
AUTHOR.- Barashkov,, G. K.; Vakhras 3-5
hina, A. V.
ORG: Murmansk Marine Biolo cal Institute$ Kolfsk Branch AN SSSR (Hurmanskiy morsk-4
biologicheakly instiEut ol'SkOgO fillala AR 03M-
TITLE: Content of nitrogenous substances in large Murmansk 2~&ae
SOURCE: Prikladnaya biokhim.' 469-471
-Lya i mikrobiologiya, v. 1. no- 4, 196
TOPIC TAGS: algae, nitrogen, colorimetry, protein, photosynthesis
ABSTRACT: The authors report on the dinwAc's bf seasonal -changes in the
content of nitrogenous substances in 12 species of brounp red and green
'algae investigated by the wdified colorimetric method of determining
nitrogen with Nessler's reagent. A pattern of changes was noted in most
!
-:of the species. In the brown and red algae,, the maximum content was noted
at the end of spring-early summer and was followed by a decrease, In the
green algae,, however., the maximum was in J4nuary-
In all.the algae,, the general nature of the changes in total nitrogen
varied largely with changes in the protein content. Fluctuations in the
amount of nonprotein nitrogen were manifested only by the appearance of
additional small. peaks, eege., in Lo. aaccharina. The ratio of nonprotein to
'total nitrogen in all the brown algae fluctuated widely - from 0. 7-23.9% in-.
Fucus vesiculoaue and from 3*2-22oO% in Le digitatao It fluctuated much
;Loess In the red _algae - from .7#0-10. 6% in Porpbyra umbilicalie and from
Card 1/2

020,53x
L 24738-a
ACC MR& AP 15521
;6.4.16.9% in Modymenia palmata. In the gri'm algae "the amplituds' 0
0
-Inuctuations was comparatively wide (from 11 6-27-R.
The authors link the observed fluctuationa mainly to photosynthesis.
IStarting in January, light in the polar regions starts to increase oharplypi
reculting in marked intensification of photosynthesis* The algae begin to
take up nitrogen ealts from the medium and thereby alter the Wrochemical,
indices of-sea watero, The seasonal changes are also related to the Physip-,
lojicaf'kit~e 4 the pl~ntss-*_Origo arts has: 1 table, PPRSI
'-SUB CODEt 06,, 007 SUEM DAM 2lJan65 ORIG REFS 010 OTH REFS 010
Card 2/2

VAKHRIN, A.
We build rapidly, well, and economically. Sell.stroi. 11 no.12:
6 D 156. (MLRA 10:2)
1. Brigadir stroitallnoy bridady kolkhoza "Fobeda",
Mokshanskogo-viyona, Penzanskoy oblasti.
(Building)

SOKOLOYSM, L.O.; VAKHROMEPTER I M.N.; KAPALIN. A.G.: ALITMAN, 9.-B..
kandidat teihTnI'C"Vs8kikh nxik, redaktor; UVAROVA, A.I?.-, tekhnicheakiy
redaktor.
[Casting with aluminum-magnesium alloys AL8 and AL133 Lit's 12
aluminievo-magninvvkh splavov AL8 i AL13. 14oakva, Gos.nauchno-
takhn. izd-vo, mashinostroit. lit-ry, 1955. 63 P. (MLRA 8-8)
(Aluminum founding)

BLYWOERY G.N.; VAKHROWYEV, G.S., -FOMIN, M.M.
Using geophysical methods in prospecting for carbonatite deposits.
Biul.nau,:-,h.-tekh.inform.Vli,Fj no.la28-32 160. (IORA 15-.5)
1. Kontors, "Vostsibneftegeofizika" Urkutskogo goologicheakogo
upravleniya'
(Proupecting-Geophysicall methods) (Rocks, Carbonate)

S11321601000101010021004
Aoo6/AOOI
AUTHOR% J!~ chrome ~ev ~G.S. ly
TITLE: The Possibility of Applying Geophysical Methods-in the Search
and Exploration of Rare-Metal Carbonatites
2(0-
PERIODICAL: Razvedka i okhrana nedr, 1960, No. 10, pp, 25 - 28
TEXT% Extended geophysical exploration was carried out on a carbona-
tite rare-metal deposit composed of alkali rocks and carbonatites having
a concentric-zonal structures its periphery consists of alkali rocks of the
melteigite-urtite series and the central part of calcite carbonatites,
bordering carbonatites of ankerite composition. Rocks of the lamprophyre
effusive type have been preserved in the carbonatite nucleus in the form
of irregular-shaped xenolythes. The main ore mineral, the pyrochlore, is
attributed to a series of linerarly stretched enriched zones. The geo- V/
physical operations included: magnetic exploration; gamma survey, metallo--
metrical and biochemical sampling; electrical exploration and emanation
survey. At the beginning of exploring the carbonatite deposits the magne-
tic method may be considered as the basic mode of investigation. The dif-
ferentiation of the magnetic fields observed over various rocks correspond-
Card 1/ 3

S/132/60/000/010/002/004
A006/AOO1
The Possibility of Applying Geophysical Methods in the Search and Explora..
tion of Rare-Metal Carbonatites
ed to differences in the magnetic properties of these rocks. However, the
contacts between the rocks could not be accurately discerned so that in
some cases micromagnetic survey was used. Results obtained by gamma and
metallometry provided additional data for the interpretation of results ob-
tained by magnetic exploration. The intensity of gamma fields was estab-
lished and it was found that a higher radioactivity of carbonatites was due
to the presence of pyrochlore containing uranium and thorium, Metallome-
trio survey was preceded by investigations on the optimum depth and proces-
sing of sampling. When applying metallometry for the purpose of revealing
the basic element of carbonatites, namely the niobium, it is expedient to
take the samples from a depth of 15 - 20 am and to analyze grains of not
less than 0.25 mm. fraction. Metallometric methods and gamma-survey should
be included into the complex of geological exploration of aero-magnetic
and aero-gamma anomalies where carbonatites may be expected. This helps
to determine the geological nature of the anomalies. Emanation survey and
electrical survey methods are recommended for detailed investigations.
Card 2/3

S/132/60/000/010/002/004
A006/AOOI
The Possibility of Applying Geophysical Methods in the Search and Explora-
tion of Rare-Metal Carbonatites
Electric exploration by the method of symmetric profiling yielded satis-
factory results in mapping the external contacts of the massif and in re-
vealing the xenolytes of lamprophyre effusives. The biochemical method was
used to determine the content of rare metals in vegetational samples which
were dried, incinerated and subjected to spectral analysis. Thus it was
stated that such metals were contained in the ashes of some plants; barium
and strontium were found in the bark of fire, niobium in the bark of cedar4
phosphorus in cedar needles and zinc in fir needles. The results obtained
by geophysical and geochemical investigations reduce the mining and geo-
logical routing operations to a minimum and ensure the checking and speci- V/
fication of geophysical data. There are 1 table, 3 figures and 5 Soviet
references.
ASSOCIATIONa Kontora "Vostsibneftegeofizikall (The "Vostsibneftegeofizikall
Office)
Card 3/3

VAKHROWVS. O.$.
Metallometric survey of the scattering flave in deposits of rare-
metal carbonati-'ea,.. Izv. vys. ucheb. say.; geol Urazv. 7 no.10:
75-83 o 164. (MIRA 180)
1. Irkutakiy politekhnicheakly institut.

VAKHRa4EYEVA, N. I _aspitant
Case of Bowen's disease involving the oral mucous membrane.
Stomatologiia 42 no.2:93-94 Mr-Ap'63 (MIRA 170)
1. Iz kafedry terapevticheskoy stomatologii (zaveduyushchiy -
prof* Ye.Ye. Platonov) Moskovskogo meditsinskogo -tomatologi-
cheskogo instituta i patomorfologicheskogo otdela(zaveduyu-
shchiy prof. Ye.F.Belyayeva) TSentrallnogo kozbno-venerolo-
gicheskogo instituta Ministerst-va zdravookhraneniya RSFSR.