SCIENTIFIC ABSTRACT VORONOV, P.S. - VORONOV, T.F.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R001860920016-8
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: March 20, 2001
• Sequence Number: 16
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

A001/A101;
AUTHORS: Voronov, P. S., Ushakov, S. A.
TITIE- Some problems of studying processes of isostaiyin the Antarctic
PERIODICAL- Referativnyy zhurnal,,Astronomiya i Geodeziya;r no. 10, 1962, 39,
abstract lOG199 ("Inform. byul. Sov. antarkt.I~ekspeditsi.ill, 1961,
no. 30, 5 - 8)
TEXT: The most explorers consider isostatia equilibrium of,the Antarc-
tic as a result of Earth's crust sagging under the ice load weight. Main prdb-.''
lems in stAidying -the mechanism of isostasy are as-follows:,: A establishing Vhe~;
character of reaction of various structural zones.of the terrestrial crust to
cover glaciation; 2) determihation of the area of the peripheral:zone of the
antarctic continent free of continental ice and sunken considerably below the
rmal level, which will make possible to determine more pirrecisely the values
.no
elastic-plastic properties of the terrestri )Iestablishing*geo-
f al crust;, 3
o
physical evidence of isostatic rise of Eastern Anbarct4 block mountains, as a
result 6f which it will be possible -to determine .-the mechanism f spreading of
the substratum.
Abstracter's note: Complete translationi B 131-yusov.,
krd 1/1

I 1 1. HIM 11 !11101 ~I I it ~1'11 I 141111A. I HIM 11111.1% 11~4
I'll! A I 11*11111"I
Mpg
PossibiUties of finding Devonian potassium AM Uman sults
In the area of Khatanpi Bp-.v,, . Trudy. NIIGL 80--182---J Ua 158. OUP 24-11.)
(natanga Bay region,--$a1ts)-
J
TR
FIN,

VORONOVI P.S. kand.geolog-mineralogicheakikh nauk
.9
Absolute age of rocks and the strueture of Antara!I-,I,ca,, lnf~orm.
biul.Sov.antark.ekep. no.3lsl5-21 161o
OMA 15:4)
1, Nauchho-issledovatellskiy institut geologii Arl,.Iiki"It
(Antarctic regions- --Geology., Structu-~al) (Geoll:Ogical time)
-1 -IF

VCRONOVv kand.geologo-mineralogichookLkh nauk; KARASIX, A,,M., geofislit
Physical properties of the rocko of the vestfcad~lffilla,
their goolo-leal int arpretation. Infoni. tiul. $ov. aMArk.
I
eksp, no.33:10-14 ~HMI -16:2)
1. Nauehno-isaledavatellskiy inst Iitut geologii irktud
(Vestfoid Hillet Antarotlca-Rocke-T,~stirg)

u
Ll
I

VOROVOV, P.S.; YEGOROVAO T.S.
Analyzing tho orientation of linear seefiona of river toille'-/8 In
the oautheastern Taymyr Peninsula for purpos I*a of'recerit tectonic
studies, Trudy MIGA 80-.139.-JJA 158. 1. NIM 14! 11)
(Taymyr Peninaula--Geolog7, Structu~al)
Ji

,.t r, vt ~ ii imi ii i V1 I HNInN.'"N."Am Ill.
'111111111 !!flli I 1111;111
--- --- --------- .......... .. ..
VORONOV #-P.'-'~-w-)--kandogeo2ogo-mineralogichoskikh nauk; YM iBLEMM.. ya.p.
kand.tekhnicheskikh nauk
Using the drift of icebergs In studying the relief of~the
Antarctic shelf. Inform. biul. Sov,antark. ekIip'. no'o'27:9-13
161. if (MI11k V*t7)
lo Ilauchno-isoledovatellskiy institut geologillli kitilit (for
Voronov). 2. Arkticheskiy i anitarktidheskiy nauch-nol-issledova-'
tel'skiy inptitut (for Koblents)s,
(Antarctic regions-Su6irine topography).
(Icebergs)

8/169/62/000/1066/013/093
228/D304:
D
AUTHORS: Voronov, P. S. and Ushakov, S. A.
TITLE: Some questions of the study of procf.A~sses of isostasy
in Antarctica
PERIODICAL: Referativr.yy zhurnal, Geofizika, no. 6t/19062, 19, ab-
stract 6A133 (Inf6rm. byul. Sov. antarkt. ekspeditsii,
no. 30, 1961, 5-8)
TEXT: Most research workers recognize the iso6tatiP equilibrium
of Antarctica as the result of the crust's war6ingunder the weight
of the ice load. The chief problems ofL*the study-of the mechanism
of isostasy are as follows: 1) Establishing the nature of the reac-
tui-on of different crustal structural zones on~'the glaciation cover;
2) determining the area of the Antarctic mainland's peripheral
zone that is devoid of continental ice and has sunk well below the
normal level, which will allow the values of'the crust's elastlc-
plastic parameters to be defined more accurately;~and 3) obtaining
-99ophysical proof of the isostatic uplift of,,J;East,~Antarcticals
Card 1/2

11 fit I'll Wild
RE M
~006/013/093
S/169/62/000/
Some questions of D228/D'304
block mountains, as a result of which it.will be 96ssible to fix
tkie mechaniam of substratal diffluence. /-A:bstraoterfonote: Com-
plete translation.
Card 2/2

AUTHORS:
TITM:
S/169/62/000/004/0,59/103
D228/D302
Voronov, P. S. and Kruchinin, Yu. A
The finding of marine sediments on t,he surface of
the Lazarev shelf glacier
no~1-4
'1962 58 ab-
PERIODICAL: Referativnyy zhurnal, Geofizika,
stract 4V343 (Inform. byul, Sov. aniarkt.ekspeditsii,
no. 29, 1961., 22-26)
TEXT: The examination of one of the ahelf glacie~re iidar Stn. Da-
.zarev led to the discovery on the vertical surfa"oe or one of the,
fissures in the glacier of shapeless dark spots'!wit4gm area of
200 - 300 M2; these consisted of disseminations,of shingled silt,
some organic remains in the ice. The study of their composi-
tion indicates that traces of chemical weathering processes are
practically absent in these remains; and that bottom material
'which belongs to the category of normal iceberg sediments, has
been found. The results of geologic and ~oologia comparisons lead
Card 1/2

S/169/62/000/004/059/103
,:The finding of marine D228/D302
to the conclusion that recent marine sediments were encountered
on the surface of the Lazarev shelf glacier; it is noted that this
kind of discovery also applies to other places in'Antalretica. There
,is some doubt about the hypothesis, according to whichthe con-
:tinuous movement of the mass of the ic'e layers foiming.the shelf
glacier takes place upwards at the expense of froozing,below and
the intensive melting and sublimation of ice fromIthe glacier's
upper surface, since no bedding is observed among1he organic and
the terrigenous.inclusions. The assumption is made that it is pose-
ible for such inclusions to be formed at the expense of the arti-
culation of a whole row of icebergs,,*ome of which could have been
inverted. 7 references. /-Abstracter's noto: Complete translation.1
Card 2/2

i
f
KAPITSAI A.P'. VORONOV, P.S'.. kand. geolo go-minerel. Ugo red.;
-K.-K. ',red.
FILIPPCT, MOZHZMWA L P tekhn red.
(Transactions of the Soviet Antarctic Expediti' i 19551
Trudy Sovetskoi a~tarkticheokoi a editaiip 19 3- ler
Vol!
grad., Izd-vo "MorskoilraneWrt is. ce 4wA
DynMi
Morphology of the ice cap in the~cmtrsl Oector 6f o4o"ra
Antarctica] Dinamika i morfologiia :Lednik6vog6 kro"
P6 Po
teentralluogo sektora. Vostochnoi~Antarkti4ym 4iredl P.S.
R
Voronova. 1961. 92 p6 iml .4 350Y
1. Sovetskaya antarkticheskaya ekspeditei;~aj 195!~-.
(Antarctic regions--Ice)

VDRONOVJ Pas, kand,geologo-mii,-iralogichealcikh nauk
Quaternary deposits of Antarctica. Inform. biull Sov,~` antark.
ekap. no.26:5-8 161. (MIRE 24t7)
1. Nauchno-issledovatel'skiy institut geologllArktikic
(Antarctic regions-Geology., Stratigr4phic),
it

1 11 1.11 f 1 11 1 V1 :
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d: ;

VORONOV
5028 geomorphological featurso of'
208 r6o. Antarctica. i.'rnd,, iITTru

-Y-O-F,91-074~~

FAN 11,1111[!, Tilllitlll
rd MUM, P.S., kand.geol.-mineral nauk
d
An attempt to restore the Antarctic,ice sbeptilof th4 epoch of
earth's maximum glac'iation.1 Infom.,.biul. S~r, ani~irk., eksp. no.23;
15-19 '60. 14:5)
1. Nauchno-issleclovatellskly institut geologli.Artild,
(Antarcti Cial e '04)
a regiond-Gla PO
MATIVII 'PIP, I I'll
I V1111 I 111fli M

SOV/169-604t-645
~4JUSSRJ'
Geofizlka,:1960, Nr',11,
Translation from: Referativnyy zhurnal,
p
AUTHOR: Voronov, P.S.
TITLE: The Operation of an outlying Station
PERIODICALz Inform. byul. Sov. antarkt. ekspeditsii, 1959, Rr 4, pp 37 41
A
k\Y
ABSTRACT: In the region of the\"MiMV.V"-obse_ atorfy (Anta~ctlc~), the
runoff of cooled lower luytl s of air MM
\!! Ll n =d, 3~ '~ Ing dff) from
the sides of the ice dome Is observed J_ e MAY of ~tbese run-
off winds was carried out from August 1 to lk ig,56,,by four
outlying stations (OS) located along the meridUrk at4ifferent
altitudes and distances from the coast. The 6p~ratidn of the VS-3-
outlying station (Chief P.S. Vor6n!pv) is detcriibltd. iThe staticn
performed measurements of the temperature -of ajr~.at altitudes of
0.0, 0.5 and 2.0 m and the velocity of wind at-'~Itit~d(~s of 0,5.
and 2.0 m every three hours, and moreover, glac~Lologj.c observ3Lttcrj_q,
It was ascertained that two predominent winds oian be~slngled out In
Card 1/2 the region of the station: a cyclonic easternJor easterA- south.-

The Operation of an Outlying Station i~~5,
eastern wind in cyclones incoming from the west, and a 13 of southern
south-easterm wind,which blew during 65% of time. The hlgh~st vstoaitleo
were found in cyclonic winds with gusts up to 42 v/seo Sn4vwau~tvansported
in the. main by winds running off. It Is noticed that the ahowdrifts isettle
in the windless region of the coast barrier.
1.P.
Card 2/2

VORONDT,_P.S., kand.geologo-cineral.nauk; MCHINIM, Yu.A., mlactshly-
nauchrU7 ootradnik
Brief pl7elcogeographical characteristicc of the ;rqglou ofthe
'Lazarev SouthoPolar Station. lnform.biul.Sov*anW!'kj?kqp.
no.12:5-9 159. (MI34 1 .6).
1. Mauohno-iseledovatelliskly iustitut geologii Axktiki Uor
Voronav). 2* Arktichaskiy i antarktichook3y j~sucbzO-issl~dcvatell-
skly lutitut (for Kracbinin)e
zarev region, Antarctica-Pbysical gepgray4)

SOMOV, M.M., otv. red.; MAKSIMV, I.Y., zameatitall otr.red.; TRESHNIZOV,
A.Y., zameBtitell otv.red.; ANMIYASHEV, A.P.i :Led.; RNNI TSKIY.V.Kh., red-;
-YOROMV-,-P-.S., red.; DOWIN, I.M., red.; YA=11K, H.Irv, redo;
KOHOTMIC11, Ye.S., red.; NIKOLISKir. A.P., r(b'd.,;RAVICH, X.G.,
red,; TLUBER, G.M., red.; ]ROWT. V.V., red.;'SUTICH, S.B.,
red.; KAPLINSKAYA, L.G., red.izd-va; MOM=X1.. L4?., tekhn.red.
[Report on observationo completed by the Soviet Antarctic Nx-
pedition in 1957 and 19563 Otchet o nabliude'altakh' vypolnenrqkh
Sovetskoi antarktichenkoi ekspeditaisi v 1957A 1956 gg.
Sovetqkaia antwrk~,iche~lmia ekspeditaiia. 1955~1195801 Leningrad,
Izd-vo "MorOkol t-~~n vort," 1960. 39 p (Inforuatsionnyi biul-
letins, no.15) OMU 13: 6)
tAntarctic regions-Ibissian exploration)
I 1 11 Ni! 'I'I 111H, '11111111 [111M, 1r, Ill 1i III

VOROWV, P. S.
Clouds as a cause of mountain disintegration in Am-tiLrat,lea.
Inform.biul.Boveantark.ekep, no,14:37-)O 160.
(XIU 13t6)
(Conrad Mountains -Weathering)

VORONOV,I-P.S.,
Relationship between the relief of bhe northorin pari. of central
.6
Siberia and.neotectonic processes.. Trud),r NIIGA' 7:94-103 158.
OURA 12:10)
(RuBuia, Northern-Geolog7, Structurial)

I 1 '11,11 rq 11 1 HIT ; [VI I! I i I !1 1 1 1111; J~j fl!; I I
PHASE I BOOK EXPLOITATION SOV/4339
Sovetskaya antarkticheskaya, ekspeditsiya, 1955-
Pervaya kontinental1naya ekspeditsiya 1955-1957 gg;; nauchnyye remaltaty (First
Continental Expedition, 1955-1957; Scientific Results) Leningradq Izd-vo
"Morskay transport.," 1959. 161 p. 2pOOO copies printed, (Seriess Itai
Materialys tom 2)
Sponsoring Agencys Arkticheskiy i antarkticheskiy nauohno-i~sledovateltskiy
institut.
Eda M.M. Somovp Doctor of Geographical Sciences; Tech. Zd.~ L.P,. Drozhzhina.
PURPOSEs This book is intended for polar specialists, geographers, geologists,
meteorologistsp and geophysicists.
COVERAGM This book is Volume 2 of a multivolume work contalming 'scientific da-ta
collected by the First Soviet Continental Expedition to the Antarctic (1955--
57).. sent out under the auspices of the Arkticheakiy i antarktlcheakiy nauchno-
issledovateliskiy institut (Arctic and Antarctic Scientifie Remearch Institute)
as part of the IGY program. The purpose of the expedition wan'to survey an
area between 74 to 1110E longitude and 59 to 700S latitude (an:area of about. 1
Card 1/4

First Continental Expedition.(Cont.) SOV/4339
million square kilometers),, to develop methods and teehnlcjues~for field studies
applicable to local conditions; and to initiate a systematic atudy of the
natural phenomena of the region. Ground and aerial observations were conducted
in the more interesting areas around and between Mirnyy and Pionerskaya$ In
the three cases of Griersong Bunger, and Vestfoldq on the Sbackleton Ice Shelfv
Drygalski Island, and a number of nunataks (Amundsen, Gauss, etc.). Geological,
geographiev and geophysical observations were made at the Mirtyy Observatory
and at the Pionerskaya and Oazis research stations. No personalities are men-
tioned. There are no references.
TABLE OF CONTENTSt
Introduction
5
Korotkevich, Ye.S. General Physical Geographic Gharacter4st,ics otthe Expedi-
tion's Area of Operation 6
Voronov, P.S. Geological Structure of the Expedition's Area of Operation 19
Rusinp K.P. Some Characteristics of the Radiation and Thermal Balance of
East Antarctica 39
Card 2/ 4

r.J!
First Continental Expedition (Cont.) SOV14339
Tauberp G.M. Synoptic Conditions in the Indian Ocean Sector of the Antarctic 46
Tauberv G.M. Characteristics of Meteorological Conditions in tho,Antarctic
in 1956 49
Rusin., N.P. Meteorological Characteristics in the Region Around the Mirnyy
Observatory 55
Gusevo A.M.0 and N.P. RaBin. Meteorological Characteriatico of t~a Glacier
Slope of East Antarctica 68
and
Vtyurin,, B.I., L.D. Dolgushiny A.P. Kapitsa./Yu.M. Model'. :~Gont4zporary
Ice Cover of-East Antarctica and Its Dynamics 73
Korotkovich, U.S. Ice Regime of the Davis %,a and Adjacent Regions of the
Ocean 93
Korotkevich, Ye.S. Biogeographic Characteristics of the Rxpedition's Area of
Operation 104
Card 311,

First Continental Expedition (Cont.) SPV/4339
Bukin, G.V. Ionospheric Observations
Sen'koj, P.K. Magnetic Field in the-Region of.Mirnyy- 115
Senlko., P.K,.,, and V.A. Troitskaya. Investigation of Telluric Currento in the
Region of Hirnyy 135
Sytinakiyp A.D. Seinde Observations in Mirnyy 153
Paleyev, N.R. Medical Studies in last Antarctica 157
AVAILABLEs Library of Congress (0860.S58)
Gard 4/4 m
T-1
17 71i
I l7t, I, Tr

Letest tectonic movements in the Arctic portion of the Lens-
Tenisey region. Trudy MIGA 105:92-415 159. (JURA 13 :5
(Russia, Northern--Geoloff, Structural)
111 -11111' Id 11,111"111,11111 J!"111111 11 111 fl]

VORONOV, F.S.
Snow "volcanism.0 Informo biul. Sov, antark. akup. 110-W75-76
159. Q~au 12:11)
(Antarctic ragiono--Snow)
F
!I*' Id! 111 111T
!

(Antarctic regione-Xrosion)

VORONDY, P.S. , kand.geologo-minoralog.naulr.
Geomorpboloff of the eastern Antarctic. Inform.Mul.150r.antark.
eksp, no.1:35-39 1580
1. Nauchno-iseledovatel'skir institut geologilArktiki.
(Antarctic regions--Ph7sical geograpb7)

VMR, V.A.- VORONOV, P.S.; IMMITITSKAYAP R.M.
Regional faults in the northern part of central Siberia. Trm17
NIIGA 67:87-93 158. li (MED 12:10)
(Russia, Northern--Faults (Geology))
"I I[I 111 1 Ilk IT! 1, 1, 111 Iii;

3(518) s0v/11 59-13-2/17
AUTHOR: Voronov, P.S., Klimov, L.V., and;Aavich, M.G.

TITLE: Late Pre -C.Ambrian. -N~pcjsit a1-of the.i!A=ndsan. and'.3andau
Mountains on queen Mary Land in the Eastern Ant-
arctic.. (Pozdnedokembriyskiye otlozhoniya gor
~
j Meri v vostochnoy
Amundsenai Sandau na Zemle Koroler
Antarktide)
PERIODICAL: Izvestiya Akademii Nauk SSSR, Ser~ya Geologicheslmyaj
1959, Nr 3, pp 3-18 (USSR)
ABSTRACT: The authors describe in d0tail the rellults of the
cameral treatment of materials gatherild. by the Soviet
Antarctic Expedition in 1956-19W6 The extremely
rare group of late Cambrian metamorphic rock of green
schists, encountered in the Centr~al sector of the
Eastern Antarctica for the firatl;timei, is dealt with
in particular. Exact data on th6.loaiation of the
fur~nished. The
Amundsen and Sandau mountains are,
geological research of both these mou~ntains was start-
Card 1/5 ed in January 1957 by L.V. Klimov and P.S. Voronov

Pr e - sol'/11159-3-2/17
Late/Cambrian Deposits of the Amundsen and San&Lu Mountains on
Queen Mary Land in the Eastern Antarctic
who systematically described the laminar cross Sect-
ion of the terrigenous rock stratU!~ and a total of
70 samples were takon. The collected material was
examined by the Nauchno-issladovatb-I'ski-y institut
geologii Ark-tiki (Scientific Resear'ch Institute of
Arctic GeoloKy). The petrographic jdesdription of
rock was handled by M.G. Ravich. with the assistance
of Ye.M. Orlenko. A complete silicate analysis on
the green schist of the Sandau mountain was made, by
A.Z-Shpindlev. The absolute age evil's deltermined at-
the Laboratoriya geologii dokemb~riya AN SSSR (Labo-
ratory of Geology of the Pre-Cambrlian Period, AS
USSR) under the direction of E.K. 'Gerling. Orographic-
ally, the Amundsen and the Sandau'~aounta_ins represent
typical nunataks, the first one being 50 m, the other
150 m above the ice shield of thei Anta:rctica (Figures
2 and 5). The absolute.height of~~the Amundsen moim-
tain is 1,445 m and that of the Sa~adau!mountain,,
Card 2/5 1,380 m. Judging from the configu~ratibn of ice cracks,

BUD
Pra- VI 1--;59-3-2/17
Late/Cambrian Deposits of the Amundsen and Sand,"M Ma.iixittains on
Queen Mary Land in the Eastern Antarctic
the Sandau mountain is circumflown~~.rrom~ SW by an ice
stream heading NW. This ice stream is,located approxi-
mately 1,5 km from the:mountain sJunrilit.~ An analogous
stream circumflows the Amundsen moiintain. from the S
and SE. This ice stream is about L) kmraway from the
Amundsen mountain peak. A petrographic study of these
2 mountains disclosed that the met~:morphic rock could
be classified into 5 principal grloups:'l) metamorphic
baltoids, converted into epidotic-_~Iilovite slates
vrith quartz-epidotic and chloritic!veins; 2) meta-
morphic quartz conglomerates; 3) various metamorphic
quartz-feldspathic, and quartz sandstones, in places
resembling quartzites;:4) met-amorphic dleurolites
and argillites; 5) sericitic slates., These 5 groups
are fully de *alt with. The authors.conclude that by
comparing the me-t,-amorphic terrigenous mountains under
discussion for composition, geological.istatus and
character of metamorphism with rock series in Siberia,
Card 3/5 it may be assumed that the most pr~(Aable time of their

Pre- SOV/11-59-3-2/17
Late/Cambrian Deposits of the Amundsen and Sandag Uo-untains on
q,ueen Mary Land in the Eastern Antarctic,
formation was the lato Pre-Cambriant per iod. The green
slates of the Sandau mountain may bO identical -aitkh
the green slate formation on -the TalpyrTaninsula, a
number of regions in Eastern Siberirit, on the Kojjj
Peninsula and in Kareliya. In all these regions, IV-'_ue
green slate formation is considered to originate from
the Proterozoic period. The same holds'true for the
green slate deposited in the 6andau~imountain. PBam-.
mitic sediments are prevalent in the cor~position of
terrigenous deposits, whereas psephitic aleuropelitic
sediments are less developed. Judging from the litho-
logical peculiarities of metamorphic terrigenous rock,
the elastic material was deposited by water streams
and partly by wind under conditions~~of a,littoral-
continental environment. There are,4 photographs, 1
map, 2 sketches and 2 references, li'iof which is Soviet
Card 4/5 and 1 English.

Pre- SOV/11-59-3-2/17
Latq'Cambrian Deposits of the Amundsen and Sandau Mountains on'
Queen Mary Land in the Eastern Antarctic-
ASSOCIATION: Kompleksnaya antarkticheskaya ekspe4itsiya AN SSSR
(Comprehensive Antarctic Expedition':of the AS USSR);
Institut geologii Arktiki Leningrad (Institute of
Arctic Geology, Leningrad3.
SUBMITTED: June 21, 1958.
Card 5/5
T

I h2.L;Ej pul-Arm"I ~A
TI F, 3 M., FF,f~, R: I I
M--
.1; T I F E M., MP M-1
VORONOV, P.S., kand. geol.-miner. nauk
On the'. zone of buried block structures supposed to be bet7veen the
South Pole and Olaf P~rvdz Bay, in!,iastern Antarc:tica..Inform. biul.
Sov. antark. eksp. no.4:19-22 159. OURA 12:11)
1.Nauchno-issledovatellakiy institut geologii irktilci.
(Antarctic regions--Goolog7, Structural)

VORDBOV, Y.S., kand. geologo-mineralog. nauk
Geological significance of the discover7 of now m,ount&imx south of
the Prince Charles mountain chain in Eastern Aztarcti~&4 Inform.
biul. Sov. antark. ekep. no.5:15-17 159. (HIRA 12s10)
l.Nauchno-iseledovatel'skl7 institut geologii Arktikli
(Antarctic regions--Mountains)

geol.-minoral. nauk
Work of the carry-out station. Inform. biul. Sor,. antark. eksp. no.4--
37-42 '59. (KM 12:3-1)
l.Nauchno-iosledovatellokl7 institut geologli'Arktikit
(AntArctia ragiow--Mataorolo&--Observatio~d)
p

VOROIUV, P.S.. kand.geologo-mineralog.na:Wr
----------
Structural acbere of the Antarctic. Infor-m.biuI.5ov.'PAntark.
skep. nool:21-25 158-
1. Hauchno-isslarlovaitallsidy inabitut 9601op
(Antarctic regions--GeologF, Structural)
Tj

I'M
;I F7 jE I I I
vo~o
kand.geol-min.nauk
Current problems in studying the atructura of th4 Antarctic.
Inform. biul. Sov. antarkt. ekep. no.2:17-20 '5~. -
.01IRA 12:8)
LITauchno-issledovatel'okiy institut geologli Ark-tiki.
(Antarctic regions-Osologrt Struo~'urai)',
ii Ilk

VORONOV, P.S.; KLIMOV, L.V.-, RAVICH, M.G.
late Cambrian deposits of Mount Awmdsen and Notint Saniow on
Qaeen Nary Coast In the eastern Antarctic* Izv,,'Aff SM-Ser.
geol. 24 no.3o.3-16 Mr 159. (MXJR4 32 -.4)
1. Komplekenaya antarkticheakays ekapeditelya AN 88SHo Inatitut
geologii Arktiki, Leningrad.
(Antarctic regions--Geology, Stratigr~phic)

FF7
mm
VOROMT, 1).S.
Nov data on the goomorpholog7 of eastern Antarctica.:Nmuch. dokI,
vyo. shkolr; geol,-geog. nauki no-3151-54 1580~ (HIRA 12:1)
I.leningradokiy gorw indiltut.
(Antarctic regions-Gpology, Structural.)
(Geophysical research;

VORMOV P.S.
Zangential stresses and regional shifting deformatlons of the
eartb's crust in the Northern part of central Sibeiia. Inform.
biul. HIIGA no.17-.13-20 '59. (AM 13: 11)
(Siberia--Bartb-Surface)

-PHASE I BOOK EXIWITATION SOV/1464
Voronov,, and Dmitriy Andreyevich Yawner.
Uralmmahzavod--pervenets tyazhelogo mashinostroyeniya (Tlle~ Ural Heavy Machinery
Plant., Oldest in Heavy Machinery Building) Moscov., MA311giz, .1958. 114 p.
(Series: Iz istorii mashinostroyeniya na, Uralep vn-~ 0 5',060 copies printed.
Ed.; A. A. Volskov., Candidate of Historical Sciences; Ex4-cutl ve Ed. (ural-
Siberian Division., Mashgiz): M. A. Bezuklednikov., Zng$,neer;~Tech. Ed.:,
N. A. Dagina; Editorial Board of Series: A. 1. Aleksaxldrov,,'Candidate of
Technical Sciences; I. R. Bogachev, Doctor of TechnicaJ, Sciences.,
A. I. Volskov,, Candidate of Historical Sciences., V. I.. Dovgopol,, Engineer,
A. G. Kozlov, Scientific Worker of the Archive Section, and 14. 1. Sustavwr,
Engineer.
PURPOSE: This book is intended for engineering - technical, an'd scientific
personnel and students. It may also be useful to propagandists and agitators.
COVEWE: The book r 6 of a serlej of 10 entitled~"Fraii the History of
n=be
Macb.ine Building in the Urals". describes construction'and &.velopmnt of
the Ural Heavy Machinery Plant imeni Sergo Ordzhonikifte, ow of the lea&ng
C ard 1/~
h Ill IIIJ 111111 11,11:1111 !~!111 11111~ 11111111 Ill!! "I'l! Ill 1`1111N.'.
D

The Ural Heavy Machinery Plant (Cont.)
Soviet machine builders. Principal stages in the develoyment of machines
and equipment built by the plant for metallurgical., mining and other branches
of industry are presented. Engineering achievements and advanced experience
in casting., pressforging and thermal, welding and mechmnized'assembly processes
are generalized, and the main trends of future engineering progress at the ~
plant are indicated. No personalities are mentioned. There are no references.
TABIZ OF COMIMS:
Introduction 3
Ch. I. The Birth of a Giant 6
Ch.I1. With the IMIW (Ural Heavy Machinery Plant) Trademark 15
F=avators 23
Crushing and grinding mills and sintering furnaces 32
Blast furnace equipment 39
Rolling mills 41
Card 2/3

The Ural Heavy Nachinery Plant (Cont.) SOV/1464
Drilling and perforating xachines
Ch. III. For Advanced Technology 55

Caoting 6o
Preon-forging 73
Welding ~80
Mechanized assembling 87
Ch. IV. Under the Ban r of Competition 1013
AVAIIABIZ: Library of ConMos
GO/Mi
5-15-59
Card 3/3

711/5
71--l
.75
Voronov, Parfeniy Yefremovich
Uralmashzavod pervenets tyazhelogo
msinostroyeni,ya tThe Ural Yachine
Building Fla'it, leader in heavy mchine
buildin.g, byj P. Ye.Voranov fil D. A.
Yasenev. Ibskva, Sverdlovsk, Yashgiz,
1958.
114 p. illus., diagrs., tables.
(1z Istorii Fashinostroyeniya na Urale)
vyp.6)
-mmIUMIDIM JAM m
1111 M
. ml
ITWII

qM,_Pargsuiy-- Yef removich-,- 1ASIUMV, Nitriy Andreyevich: DMINA, N.A.,
tekhn.red,
(Ural Heavy Machinery Plant, first of the heavy mschiaery Industryl
Uralmoohzavod - pervenote tiashelogo mashinostropUiLS s, MOGkVS,
Goo, nauchno-takhnsizd-vo mashinootrott. lit-ry,' 1958$1- 114 P.
(~.MA 11:5)
(Sverdlovsk--*ch!i~,;.~tog"iia~itl7)

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.,J~jm 1. I'MRIMIR In. P11 T.
THT TM TV nnri "PArTm IA V
"High Strength Low Alloy Carburizing Steels," clItait6 (IW) pp 181/188.
B-73331, 1 Apr 54
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MII-31'Cll %1CV1 Writ 111111101 tO (let., thrir
maki"S orms. The rejult4, (if ph)-,. te,tot Sri.
'
rlmw siterls were found suitable w rulow-j! Cr.-Ni for nij ik-
ing Nem. Most flesiralAo wcre the loccU ?ZRAIGs 11
Mr-Nin-S-3,10 land =KhOsVii (Cr-".%lti-N-Cu). 71s .
, St
Steds hail the hq-it mlibillation of telwle StIC71ii h.
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K
V- -7
-P
"On the PclarizOtiOn Of Light by Roflectioll cit Diffuse
Bodies, Zeltsct=ift fur Physik, 1524, Vo.l. 301, 1,7 2, pp

"On the Jolective Reflection of Light at Diffiir,,c Rofli!cHxil, 13I.Jilies,
Ze-itsch-rift fur Physik, 2.10211, '101- 30, "'Ito. 6j PP325(c',-370.
LIJ., 11 id
T!' A
A 1Tm
iTit i i

"The De-nolarization of LiZht in Diffuse -IM.ection," ZvaitBr-1=--Lf1.
fur Physik, 1925, Vol. 33, pp 86g-C6(,).
IL III 1,HAIIII WIMUIMB111

"The Light Scattering in Coarsely Dispersed I~Ldia, off H1811C.'r C(I*n..
contration," Zeitschrift fur Phy$ik, 10 6, Vol. 35, tio. 6-9: w 63
2
641.

=sing MA
J.1 I I ~~ !
M-4
"The Optical Properties of DIsly!rzed I.Scrcuxic' Slut'ide, 2~.AII(I'lil -
7p-itschrift, 1927, Vol. 43, PP 78-61,
"Hydrosols of red 1[g3 vere 'DrelW3. In SeVCT01 dt2oreeS of~ fllzl>~i~rzior
by means of colloid mill. T'hese vere illuminated by a bu.1,1dle df paral-
lel rays of light an an examn. vas made of the light scattered:ut
right angles to the illuminating ray and of, the transmit~,t~,-d lir~ht.
For coarse particle a the scattered and trapamitted lighti~tjre nvarly
the some, but as the degree of disperBion inarcaaes they 11~tcome! Cori-
tinuously more nearly complementary. The transition setr3-;in wMn-. the
particles are still relatively cotjvoo. It was dbservable~lvith
particles ltAin radius."
1k; 11 In',

"Optical Examination o1L substar..,ces of Powder or Fiber
Kolloid-Zeituschrift, 1920, '101- 45, 1-7.
Hl 1,1*1;1~ III 111] liNw" 1111 `11 11,~ i'll IN"1111, IiIIII IT III

"Experimental Investigation of the Absorption KDility Of:SOM
Materials for Light of Different Wave Iengths as a Functiou of
Particle Size Kolloid-Zeitschrift
1930, Vol. 50Y pp'7-19#
"The r3tio of the transmitted light to the incident light ties ~Ietd.
for I%S and ultramarine suspensions at various wave lengtI 'is and f or
particle sizes detd. by Stokes I law, from 675 to 475 M q~lia e: Al.
values of the absorption coeff. approach those required by;ithe Mq-
leigb theory as the particle size ddcreases.~ Thedifficulties of
accurate duplication are the irregular sizes of the particles and the
magnitfication of errors by the graphical dL ifferent is'. ion 66e d .The
color of the suspension changes when the effective radius it; less than
the wave length of the incident li6ht.
VI

VIYALOV, O.P.: VORONOV, F.S.
Geological structare of the Bangor "CASISO In;
i