SCIENTIFIC ABSTRACT USHAKOV, P.V. - USHAKOV, S.M.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R001858120015-0
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: March 14, 2001
• Sequence Number: 15
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

L) 1~ // o ill, t-v 17 V-
AX M-SHKIN, I.I.; BARANDVA, Z.I.; BRODSK1T, X.A.; VIRKETIS, M.A.;
VOLODCIMO, H.I.; GALKIN, Tu.I..; GURITANOVA, Te.F.; DOGW
V.A.; DITAKONDV, A.M.; ZSVINA, G.B.; IVAIJDV, A.T.; KIRITANDVA,
To S.; KOBTAKOVA, Z T.; KOLTUN, Y.M.; KORZRMVA,Ye.D.;
KOROTKICVICH, V.S.;KLTUGB. G.A.; LOZINA-LOZINSKff, L.K.:
LOIL&KINA, N.B.; NAUM07, D.V.; PICHGAMMIT, T.S.; RISHITXTAX.
V.V.; SAY-BLITNA, T.S.-, SKARLATIO, O.A.-, SOKOLOV, I.I.;
STRKLKOV, A.A.; TARASOV, N.I.; USHAKOV. P.V.; SHCMRINA,Z.G.
TAKOVLXVA, A.M.- USHAKOV Lj., obsbchly rakovoditall-,
PAVLOVSKIY, Te.i., ~5o'mlr -redaktor; STRIUXOV, A.A. redaktor;
BRODSKIY, K.A., redaktor; ARONS, R.A., tekhnichookiy redaktor.
[Atlas of invertebrates of the Far East seas of the U.S.S.R.]
Atlas bespozvonnchnykh dallnevostochnykh morei SSSR. Kooky&,
Izd-vo Ahmd.nauk SSSR, 1955. 240 p., 66 plates. (HLRA 8-10)
1. Akademiya nailk SSSR- Zoologicheskly institut,
(Soviet Far Easu-Invertebrates)

USHAKOV,P.Y.
........
Aphroditidas (Polychastae) of the Kurile-Kawhatka Trench.
Trudy Inst.okean. no-12:311-321 155. (N1RA 8:9)
1. Zoologicheskiy institut Akademil nauk SSSR
(Kurile Trench--Polychaeta)

UsaKov, P.V.
lwv~ ~,~
New species of polychaetes from the family Aproditidae (Polvchaeta)
from the Far Eastern seas. Trudy Zool.inat. 21:170-173 '55.
(KLRA 9:5)
(Pacific Ocean--Polychaeta)

V'-17- - 11 -
USHMOV,P.V.; PAVlA)VSKIY,Ye.N., skademik, redaktor; BTKHOVSKIY.B.Ye.,
'-~re4gfrovi; VINOGRADOV.B.S., redaktor, STRItTXGV,A.A., redaktor;
SHTAKKLITM A.A., redaktor
Polychaeta of the Far Eastern seas of the U.S.S.R. Opr.po fauns
no.56:3-443 155. (MLEA 8:11)
1. Direktor Zoologicheskogo instituta Akademii nauk SSSR (for Pay-
lovskiy)
(Soviet Far ]Cast--Polychaeta)

USHAKOV, P. T.
d"Aakab ".-
Role of the L& Porous@ Strait in the fauna formation of the
Bouthwamtern part of the Sea of Okhotsk. Dokl.AN SSSR 105
no.6:1371-1371# D 155. (IIIRA 9:4)
1.Zooldgichookijr institut Akadenii nauk SSSR. Predstavlene
akademikem Ye.N.Pavlovskim.
(La Perouse Strait-Karine fauna)(Okhttek, Sea of-Karine fauna)

USH"OL6p'V- -
Atlas of the invertebrates of Far Eastern so". Trudy Probl.i tem.
(am 9: 1.1)
sov. no.6:155-156 156.
1. Zoologicheskiy institut AN SSM.
(Soviet Far last-Invertebrates-Mps)

USHAKOV, P.V.
Polychaetes of the family, Fisionidae Ievinsen inhabiting the seas
of the U.S.S.R. (with InEliah summary in insert]. Zool.zhnr.35
no.12:1809-1813 D 156. (MIRA 10:1)
1. Zoologicheski7 institut Akademii nauk SSSR.
(Polychnota)

usmov, P.J.
Pblagle Poii~hasta of.the northwestern Pacific. Isal. WInevast.
por..SSOR 1;o.4:267-290 157. (MINA 10:4)
i
1. Zoologiobieskiy institut All SSSR.
(Pacific Oceez-Folychasta)

USH-A F CIT" , -1, . v .
USHAKOV, P.V.
-
Oceanographic Institute in Kiel. Zool.zhur- 36 no.1:158-159 Ja 15?.
(MLRA 10:5)
(Kiel--.MmLrine bi ology--Re search)

USHAKOV, P.V.
German Avgustovich Kliuge; obituary. Zool.zhur. 36 no-9:1433-1435
S '57. (MM 10:10)
(Kliuge, German Avgustovich, 1871-1956*
(Bibliograph.v--Arctic regions--Marine fauna)
(Arctic regions--Marine tauna--Bibliography)

I'L7 -3 H /T i~ 1~ V, 1 , L.,
USHAKOV, P.V.
'40j7'.~,A4 -:?, ~ -.; - ,
--'- -4~' 2iblychaeta of the Arctic an& Antarctic [with ffumMR17 in Inglish].
Zool. Shur. 36 no.11:1659-1672 5 157. (NLRA 10:11)
1. Zoologicheskiy institut AN SSSR (Leningrad).
(Arctic O~ean--Pblychaeta) (Wilkes Iand-Polychasta)

USHAKOV. P.V., professor.
~
In New Zealand and Australia; from the notebook of a hydrobiologist,
member of the general artarctic expedition of the Academy of Sciences
of the U.S.S.R., 1955-1956. Priroda 46 no.2:61-66 F '57.
1. Zoologichaskiy institut Akademii nauk SSSR (Imeningrad) (MIRA 10:3)
(New Zealand--Description and travel)
(Australla---~escription and travel)

BIKLYAYXV, G. M.~"H~Ryujja-~
Certain regularities in the quantitative distribution of bottom
fauna In Antarctic waters. Dokl.AN SM 112 no.1:137-140 Ja 157.
(KM 10:2)
1. Institut okeanologii I Zoologicheskiy inatitut Akademii nauk
S=. Predetavleno akademikom Ye.N.Paylovskin.
(Antarctic regions-Narine fauna)

Gi -~, ~ A 1(,, v)P, 0,
13(5.-7) FRABE I BOOK EXPLOMATION BOV12193
Sovetslaya antarkticheakays ekspeditsiya, 1955-1958
Informatsionnyy byulleten', VYP- 3 (Tnformtion Bulletin of the Soviet Antarctic
Expedition, Nr 3) Imningrad, Izd-vo "Morskoy transport," 1958. 102 p.
1,500 copies printed.
Sponsoring Agenciess USSR. Ministerstvo morskoy flot. Glavnoye upravleniye
Severnogo morskogo puti. Arkticheskiy i Antarkticheskiy nauchno-
issledovatellskiy institut.
Ed. of this Vol.z P. V. Ushakov; IL-sp. Ed.: M. M. Somov; Editorial Board:
A. P. Andriyashev, V. Eh. BuWnitskiy, I. M. Dolgin, S. V. XhIesnik, Ye. S.
Forotkevich, I. V. MLksimov (Deputy Resp. Ed.), A. P. Nikollskiy, M. G.
Favich, G. M. Tauber, A. F. Treshnikov (Deputy Hesp. Ed.), S. B. Slevich
(Resp. Secretary); Ed.: L. G. Kaplinskays; Tech. Ed.: L. P. Drozhzhina.
PURPOSE: This book is intended for natural and earth scier4tists interested in the
research activities of the diesel-electric ship "Cb4V in the Antarctic. It
Card -*i~-

Informtion Bulletin of the Soviet (Cont.) SOV/2193
is of particular interest to marine biologists., meteorologists, and
geophysicists.
COVERAGE: This issue of the Information Bulletin on the Soviet Antarctic
Expedition reports on the fauna found in various re-gions of the Southern
Hemisphere, the hydrology and hydrochemistry of Antarctic and Subarctic
waters., and the geomorphology of the Antarctic shelf. The reports vere
read at the First Conference on the Study of Antarctica's Marine Fauna in
December 1958. No references are given.
TAME OF CONTEWS:
the Editor 9
Andriyashev, A. P.s K. A. Brodskiy, and P. V. Ushakov [Doctors of
Biological Sciences]* Biological Investigations of Soviet Antarctic
Expedition Aboard the Diesel-Blectric Ship "Ob"' 32
The following research workers, associated with the Zoological
lustitute., Academy of Sciences of the USSR, the Institute for Ocean-
ology, Academy of Sciences of the USSR., the All-Union Scientifi( Re-
search Institute for Fishing and Oceanography, and the Paleontological
Card 2*

Informtion Bulletin of the Soviet (Cont.) SOV/2193
Institute of the Academy of Sciences of the USSR,, took part in the ex-
pedition: in the first voyage - A. P. Andriyushev, V. A. Arsenlyev, G. M.
Belyayev, K. A. Wodskiy, M. Ye. Vinogradov, A. K. Tokarev, and P. V. Usbakov;
in the second vdyage - V. A. Arsenlyev, V. V. BLrsukov,, X. V. Baklemishev,
A. V. Gusev, V. S. Korotkevich, F. A. Pasternak, and Yu. Ye. Pernitin; in
the third voyage - A. P. Andriyashev, K. A. Brodskiy, B. A. Zenkovich, A. A.
Kirpichnikov, V. M. Koltun, A. G. Naumov, F. A. Pasternak., and Yu. Ye. Permitin.
I-Toroshkin, K. V. [Senior Scientific Worker]. Hydrological Investigations of
tbaSoviet Antarctic Expedition Aboard the Diesel-Electric Ship "Ob'" 1T
New data on the structure of the Antarctic divergence zone vere
obtained by Yu. A. Ivanov and B. A. Tareyev.
Bogoyavlenskiy, A. N. [Senior Scientific Worker]. Oertain Feculiaritiej in
1heDistribution of Oxygen, Phosphates and Silicic Acid in Antarctic Waters 19
Zhivago, A. V., and A. P. Lisitsyn (Candidates of Geological Sciences].
Bottom* Halicr and the Deposits of the Southern Ocean 21
Card 3/4

Information Bull tin of the Soviet (Cont.) SOV/2193
Brodskiy, K. A.- [Doctor of Biological Sciences], K. K. ~hrkov [Professor],
and V. I. Shillnikov [Jkmior Scientific Worker]. Zoning of the Temperate
aad High latitude Regions of the Southern Hemisphere 23
Brodskiy, K. A. Plankton Investigations of the Soviet Antarctic Expedition 25
Vinogradov, M.Ye. [Candidate of Biological Sciences], and A. G. Naumov
(Aspirant] . Quantitative Distribution of Plankton in Antarctic Waters of
-the Indian and Pacific Oce s 31
Beklemishev, K. V. [Candidate of Biological Sciences]. The lAtitudinal.
Zoning in the Distribution of Antarctic Phytop2ankton 35
ImaM , N. B. [Candidate of Biological Sciences], Imphausiacea Collected
by the Soviet Antarctic Expedition 37
Usbakov, P. V. Benthonic Research of the Soviet Antarctic Expedition
-'-)Eo-iL-rW-U-e--Diisel-Electric Ehip "Ob 39
Card 4M

,a+ 4 Dn 3
Investi,g c-P Fa,ina In Far 'bast; b(. th~.~ f
of Scienc,~,!3, USJR.
ton species in the cone of tlieccrfluence -.r--r,:! an:i a-3 r e -
sults obtained in 1954 by the sc-called North-Kurile Exploratinn the%-
Kamchatka El-anch of the Pacific institnte of Piscatoloay M 1jRO) 4 r
.0 , nolla!-_-ati~,,in w'-t-'; the
Institue of zoologry and the Institute of Cceanology (ICA11) , bcth of the Aca~!'~7'-Y 'f _'2ienees,
USSR. As its bast! the exp-~~dition us-?d the motorbuat Vitya7'. Thr~ f:--11(,-,rI'ng parti
cipated: V. Kcitun, V. Korotkevich, i-1. Le:-_-z, and 11. Spirina. Th.,! article Jis3ussej tlie ze.--
geography of the region in question and analvzes rf the prblem-_ of fainafc,rrnati~~n _-11~1
fauna distribtiticn. 'Di-! article! urges a conl~inuatkn o.~ this resuarch.
This collection of articles reports the results of cbseinratiuns mar~,,~ -n tleracific by the
Institute of OceanoloGy for the Academ, the institute
y of Sciences, USSR. In 1,,)49,
a systewtic five-year progra-i of scientific exploration of certain hydroraohir- pt.-cullaritie
of the Soviet Pacific Area. The operatictis were carried out as a
LI-Cped
- iton," using the Mot(--)rboat Vityaz' as its hase. 11he Expedition worked In c,illal,oraticn
with the hydrographic Institute of the S..)viet Navy (VMS), the Pacific Inotjtut-3 of Piocat~:log
and Oceanography, and some 40 other institutes of tht-, Aoademy of S:!icnce!-- Betwe,-2n 194) and
1954, 18 trips were made, coverinS about 130,001) miles. Among the subjf~cts of dir~,c" ccn~cer
were: Meteorolugy, hydrolngy, octanography, hydrochemlotry, ae1j1mo-ntrit1i)n, j.,ri.,()j!raVhy of flj'~-
littoral, geology and contours of the ova br)tt(,z, fauna, plankton, m1croblology, and Vravi-
metry. Twenty-eight authors contributttd to the collection which consists of 27 articles.
6 gables, 23 diagrams, 3 illustrations (photographs of the littoral), 1, ~IZTs. 1;c- references.
Research of the Northwestern Part of the-Pacific Ocean, Moscow, Izd-vo Ali USSR, -19'J-8.

L-1 "FTA I I-
t
A
00 0
R 1A ii.M' - h QQ
ndh 4
10 00 0 10
A 1
000 :9. 0 :mi Uft 3
ot- 0,3 1. j -01
V
D.
.%4 -H -H if
a
CS -0 .4
14
0J.111 1-4V
Ao' a
so
d,
"Al
-m -- - I
Ila -w U41
oil
40
u
c6
14
vi 0,3
.d
53 V. 0
103 j
1b 0:1 S 10 1
.0 -.1111 Ismos.
1j
i -g, I aw
-A

ANDRIYASHEV, A.P., dok-tor biol.nauk; BRODSM, K.A., doktor biolonauk;
USHAKOV, P.V., doktor biol.nauk
Biological i3tudies undertaken by the Soviet Antarctic Zxpedition
on dieeel-electric ship 80b'm in k955-1958. Infromoblul.Sov.antarko
eskp, noo3:11-16 158o (MIRA 12:4)
1. Zoologicheekly Institut AN SSSR.
(Antarctic regions--Hydrobiological resenrch)

USHAKOV, P.V-, doktor biol.nauk
Benthonle research made by the Soviet Antarctic Expedition on the
diesel-electric ship wOblw In 1956-1958- Inform.biul*Sov.antak.
e)MP. no-3:39-42 '58- (MIRA 12:4)
1. Zoologicheakiy institut AN SSSR.
(marine fauna)

.-U.SHAKOV,-P.V. .
low and interesting species of Polychasta from the region. of
southern Sakhalin and the southern lurile Islands. isol. aallbevost..
mor. SSSR ne.5:78-89 158. (MIRA 120)
(Sakhalin-Pol7chasta) (Kurile Islands-Polychasts.)

USMOV. P.V.
now species of Pblychasta of the family of Phyllodocidae from
abyssal depths of the Kurile-Kawhatka Trench. Trudy Inst. okean.
27.-204-207 158. (KIRAL 11:4)
1, Zoologicheakiy institut AN SSSR.
(Polychasta) (Okhotsk. Sea of)

GURIYANOVA, Ye.Te.; USHAKOV, P.V.
On the Ninth Pacific Scientific Congress in Bangkok and'the marine
littoral fauna of the Gulf of Slam. Zool.zhur. 37 no.10:1586-1-591
0 158. (MIRA 11:11)
1. Zoologicheskiy institut AN SSSR (Leningrad).
(Pacific area) (Slam, Gulf of-1/hrine fauna)

AUTHOR: Ushakov, P.V., Professor SOV-26-58-3-10/51
TITLE: The Subantarctic Islands of Macquarie and Kerguelen (Sub-
antark'ticheakiye ostrova. Makkuori i Kergelen)
PERIODICAL: Priroda, 1958,'Nr 3, PP 58-63 (USSR)
ABSTRACT: In 1956, the author in his capacity as a hydrobiologist
went with the Complex Antarctic IExpedition of the AS USSR
in the dieselelectric vessel "Ob" to the Islands of Macqua-
rie and Kerguelen. Here, cold Antarctic and comparatively
mild oceanic currents meet. The two islands are about 3,250
miles apart, the waters in oetween attain depths of 3,000
to 4,000 m. However, 'the fauna and flora of both islands
are very similar. The littoral fauna and flora of both is-
landa containod up to 50 vj'u of tho snmo qpoviea. This indl-
cates the existence of a single biogeographical area, in spite
of a diverse geohi3torical development of the islands. A
parallel phenomenon has been observed in the northern hemi-
sphere with respect to the Commander and Kurile islands.
There are 2 maps, 1 chart, 4 photos and 3 references, 1 of
which is Soviet, I German and 1 Swedish.
Card 1/2

The Subantarctic Islands of Macquarie and Kerguelen SOV-26-56-3-10/5-1
ASSOCIATION: Zoologicheskiy institut Akademii nauk AN SSSR-Leningrad
(zoological Institute AS USSR-Leningrad)
1. Animals--Macquarie island 2. Plant s--Mac quar ie island
3. Animals--Kerguelen island .4. Plants--Kerguelen island
Card 2/2

PW~ 0.1%,ttted for the Oth P,.rL.
5.0 2961.
or
=tIVA4 f -r
the horLzontal ~,~~ vertt i:,! -Iltioa If -tern d-Ing, the vL,"r
period I. the -rth,, i,~. the P-Lri, vi:.z))
-Pres.m.twn of 5.t_., of sciences -n, ro~~ of
the birds of S11wria seA U,o Fa~ E-t Df 'he oz ~snttl*
spreaders or vims and rlc!~%ta-L diecone" (Se-:tloo 111-D.Ii)
ZZZRWM;Sxly, B. L., or A-~,v or Gi-e.
WZR . -,ho -InL3 of some cL~rsctertatlc prcea- Of atwo~hvrtc
.1roul.tion -r-&t Ant-tt-," (Section M.D.1)
"'VC,twYA, X. A., lz.ttlt~t. of Cclocy - "Adrute. In recent maj;ne'.1m
of the rucirtt &harts of the t.Sll- (SeitioA
or - "on the
of level ..or -he -lest. of -.he raclftc' (Section VII.B)
M-131MV.r- P., of 0-~CrA;J:y - "ril ft-t-1.4 11o the
wz~so~ c~Giie of -he Mr Ust &-A the Infl,-nae of re-ent va'cscivm~
orrtsefft Isterlt.3 -A 14-er.-IT Gait.- (Soctm 1.0
00FITACM7 A. ., :_ttvt* of rArth physics 1-1 0. ra. rth,11t. -
of 'he K,artle Ka-hitkift tine se sa
or st,otur%l of the emx-.h's c-st In -he ncrth--tern
Psart of the P-i.", b-in' (5-tI..
:-st.'tute cr 0:-alcm, - ~Spc:lrll frutures In the
distribution 0: -,Iw.~~tot In the tmpi-nl part of the PaLfIc
Ocean, (Section. :-.C)
GLM.'k,f_~. _S. The Croll"'It.1 M,- I_.I A. P. y'--pin.uy"
Aced-7 of Ki-es L=n - %1~km' teeth found a' th~ totto,% Or
t.h. Ncifll. Cc-, (S'etice 111.0
n1a, Lmbarst-f of vclc~lov - "Pctml~heodc.l
ree'tures of "IC-4- In relAtIon to the t)~* of the earth's crust"
C5ec%1= M.C.2)
G=Z, A._P., Zst.t-4-.e of 0:t-oiogy - '-he stratig-piq of bctt..
jA'r`seU.-e,1i- -A the condit.... of 1.
the Pseiri., (Sez%lo.
-MKAZ!yr:" of G~.grnrhy .., siterl. and -%a Fe,r D-t
~:rhe origin%! tret0a wt re-1to of telic%1 gt~t;ra;hlce. reseorch in
the S-lat Fax r~-t' CIT.c-lor V11:.B.4)
PGALO _q~ P~Irl: C-06i Stien Lric Res-ch tn.tttute or
_ jSM_A - t
K~Ine 1-shir.; -1 Olesnc~ruphy - -h, Ichthyl~&Iml mat.ri.1b
mU#lt ed during the B*rl..Z Sea expedition opot3orid by the k' I.
sol Pacific Ocesc ~~.Itntiflc R",eorch ln3tituta Of Mthing
am ~kaa~grap_y 1. 19',t~59" [Sc~tioft 7ZI.C)
X&%C"=J7TCj~L._&.j Institute or 0:eorojoar - *Reth~d of cc -tIng
statlozar7 eorrects irto "20=t the effect or isiwW
(Section T'11.2)
X&=La_T_F., Imati-ute of' C-ology sut-iAe re"Ler of
the Wril -' (Sectl.. 7-Z.C.1)
XASS, Institute or - "Deep-sem fichea or the
=,the- pr, of th, rulfit a,,d Jj..ent at." (5e~tt.l 111,C)
JM.~Cacmy'-Y., sal F, V_ Institute of Z"Lofzr -
-POITCt-ta Of the Sn~ In the torthwat Pacific -1 problems
of smphl-Pmcific ilstrlbtioo~ (Section 111,C)
rp C=,-M7A- G.-Z., Moccow state 1~niverolty, piy5tcal Ficulty - "The
cmacuittion, or t~rttaeot eufruion coefficients t-i upon the
recordings of eiectrocon~ojtlvlty fjuct~t-.ou w.1 c~orrrn- rnte
.. see (Section TIZ.B.5;
.9T"AT7,W9DT=, Se I-, Inst!tt, or *Scv. r-Rularitif. of
the th,rwcl.. 'Imtti., 1, tho Ole-" (S-tio. VILB)
1-titute of Oc-ul~a~
Ulefitblt) "Llef or the continental shelf of t:ie ~atern stabo-I
to southern ni.c.0
Institute or Oce=oloa - "ie %-;w;raPhIc&X unat0n
In the ~tcra 0.1 atQ=er.. nrcus* (Zettion VJ.D)
Inztitute f exn31oM( - "A D~rty of data
cot.amea with -,rlmw7 ;~.-u:tton in the northern pnm of -he Pacific"
(section 11;.A)

LINDBERG, G.U.; SHCHEMINA, Z.G.; DOGEL', V.A.; RRSHRTHYAK, Y.T.; STRILKOV,
A.A.; KOLTUN, V.M.; IIAU14DV. D.V.; IVAIMV, A.T.; BYKHOVSKIY, B.Ye.
ZHUKOV, Ye.V.; F121GAMEWT, T.S.; KORDTKIVICH, V.S.; USHAKQV_, Pt-'K,_;_
KLTUGI, G.A.; ANEROSOVA, Ye.I.; GOSTIWVSKAYA, M.G.; PRODSKIT, K.I.;
G[JSIV, A.Vj; TAMSOV, N.I.; GURIYANDVA, Ye.F.; TAGIN, V.L.;
WKAKINA, N.B.; BULYCHEVA, A.I.; KOBTAKOVA, Z.I.; WZIND-WZINSKIY.
L.K.; UKOVLEVA. A.M.; G&LKIN, Yd.I.; 9KARIATO. 0.A.;
AKIMUSHKIN, I.I.; DIYAKONDV, A.M.; BARANDVA, Z.I.; SAVBL$TBVA, T.S.;
SKALKIN. V.A.
List of the faum of mrine waters of southern Sakhalin and
southern Kuriles. Isol.dallnevoot.mor.SSSR no.6:173-256 159.
(MIRA 13:3)
1. Zoologicheskiy institut AN SSSR.
(Sakhalin--Marine fauna)
(Kurile Islahds--Marine fauna)

TICH, L.A.; MOKLK7SKIY, O.B.; USHAKOV, P-V-; FIIATOV, S.Z.
At the Yirst International Oceanographic Congress in the United
States. Zool. zhur. 39 no-5:797-80D W 160. (MIRA 33:10)
(oceanography-congresoes)

USHAKGV, P.V.
Some specific features of the hydrological regime and fauna of the
flooded volcanic crater of LIvinaya. Past' Bay on Iturup Island
IKurile IslanA Isol.dallnevost.mor.SSSR no.7:344,348 161,
(KM 14:5)
(LIvinaya Past' Bay)

USHAKOV, P.V.
Acelimati;ation of the Kamchatka crab in the Barents Sea.
Trudy MMBI no-4:250-251 162, (MIRA 15:11)
1. Zck6logicheakiy inatitut AN SSSR.
(Barents Sea-Craba)
(Animal 4ntroduotio,n)

USHAKOV, F.Y.
"Biologic oceanopaphy and marine
life,- by J.M.Pgie's. Reviewed by
2 no.3073-575 OW -
(Marine biology)
biology. Part
F.V.Ushakov.
(Firls, JX)
1: Benthonic
Okeanologiia
(MIRA 150)

-USHAKOV, P.V.
Polychaetous annelids of the fandlies Phyllcdocidae and Aphrcditidae
from Antarctic and sub-Antarctic waters. ISS1. fauny mor. 1:129-189
162. 4URA 17:9)
1. Zoologicheskiy institut All SSSR.

USHAKGVP P.V., doktor biolog. nauk
Some fleatures in the distribution of bottom fauna off the
shores of eastern Antarctica. Inform. biul. Sov. antark. eksp.
no.400-13 163. (MIRA 1637)
1. Zoologicheskiy institut AN SSSR.
(Antarctic regions-Marine fauna)

USHAKOV, P.V.; U BAO-LIN [~.~ Pao-ling]
Free -s wimaim, PolychaeW of the Yellow Scu. fauriy
0
3:145-258 165. (141PA 1P:9)
1. Zoologicheskiy institut All SSSR (for Ushakov). 2. Institut
okennologii Akadaidi muk Ki.-Wyskoy Narodnoy ReormblAki (for
U BAO-LIN).

So K'O V, S
Subject USSR/Aeronautics
Card 1/1 Pub. 135 - 2/19
AID F - 2238
Author Ushakov, S.*, Maj. Gen. of Aviation, Hero of the Soviet
UnTrIll ' ,
Title Anti-fighter maneuver of h1gh-speed bomber aircraft
Periodical: Vest. vozd. flota, 7, 8-14, J1 1955
Abstract The author considers problems connected with those
evasive actions of bomber aircraft which consist of chang-
Ing speed alone and of changing speed and direction
simulianeously. In order to simplify the problem, the
author supposes that fighter aircraft start from one
airfield only, This is the second article of this
series. The editor does not agree with the author in all
his opinions. Examples, diagrams.
Institution; None
Submitted : No date

AID P 2202
Subject USSR/Aerodynamics
Card 1/1 Pub. 135 - 3/18
Author : Ushakov, S., Maj. Gen., Hero of the Soviet Union
Title : inteiceptor maneuver by changing course of bombing
aircraft
Periodical : Vest. vozd. flota, 6, 17-23, Je 1955
Abstract : The author expresses in this article his personal views
on the problem of bombing-aircraft maneuvers. The editor
does not agree with the author on a number of his state-
ments, in particular, those relative to the time neces-
sary for the determination of new flying data of bombers,
or on the transmission of orders to fighters. Diagrams.
InstitutiOn s None
Submitted : No date

S
AID P - 1844
Subject USSR/Aeronautics
Card 1/1 Pub. 135 - 5/18
Author Ushakov, S., Maj. Gen.
Title High altitude bombing
Periodical Vest. voz. f2ota, 4, 31-37, Ap 1955
Abstract The author considers general problems of bombing and
describes in some detail high altitude bombing from
hori4ontal flight. He analyses errors and gives
geiieral advice on training. Some names are
mentioned.
Institution None
Submitted No date

F1
85-58-5-25-38
1
AUTHOR: Ushakov S. Major General of the Air Force, Hero of the
Sovief -Union
TITLE: Strategic Aviation (Aviatsiya dallnego Ceystviya [ADD]); In
the Battles for the Soviet Homeland (V boyakh za Sovetskuyu rodinu)
PERIODICAL: Kryll.ya rodiny, 1958. Nr 5, pp 20-21 (USSR)
ABSTRACT: In the second of two articles, the author relates the
exploits of Sovietc. airmen of the ADD during the Second World War.
The personalities mentioned inlu4e: Navigatqr Nikolay Georgiyevich
Al I shevskiy, now GuardaLt Col; Lt Col Vasil~y. SezAlko, Hero of the
Soviet Union. There are 2 photographs showing Al'shevskiy and
Sen1ko.
AVAILABLE; Library of Congress
Card 1/1 1. Aviation-USSR

USHAKOV, S., general-mayor aviataii, geroy Sovetakogo Soyuza.
...... "'star. .0481111~
Long-range aviation in combat for the homeland (conclusion).
Kryl. rod. 9 no.5:20-21 My 158. (MIRA 11:6)
(World War, 1939-1945--Aerial operations)

65-58-4-18/36
AUTHOR: Ushakov.. S., Majar General of the Air Force, Hero of the 5oviet Union
TM : Strategic Aviation in the Battaes for the Soviet Homeland (Aviatsiya
dallnego, deystviya fA_M
7 v boyakh za Sovetskuyu Roclinx)
MIODICAL: Kryllya rodiny, 1958, Nr 4, w 17-19 (U`SSR)
ABSTRACT: The author relates the exploits of Soviet al ~ of the ADID, all Heroes
of the Soviet Union, during the Seiond World War. The personalities wn-
tioned include: Nikolay Fvantze-rilch Gastello, pilot, vho perished ramming an
enwW; Seasen Mikhaylovich Alashla, fligIit comnnzAer on the Leningrad front
vhoj when hit, made a suicidal d1w in-to an amminition dump near Chudovo rail-
road station. A,Xotj navigatvor; I. I. Starzhinskly,. navigator) nov Lt Col;
Yevgeniy P. Pedorov, now Maj Ge:-,; f=xs for precision night bombing;
Dmitriy Baryshev, vho, first imereased bombing loads; Aleksandr Ignatlyevich
Molodchiy, nov Maj Ger., one of tbe first to bomb Berlin in 1942; Feodosiy
Karpovich Parashchenko; Lt Gea G. N. Tapikov; Gen I. V. Georgiyev;
Syatcbilrhin, aircrarc, cacm%ander; )%j Ax-11-Juorov, aircraft coamander. There
axe photographs of Generals lvedorov; 14olodchiyp and Tupikov. Th be continued.
AVAnAZZ: Library of Congress
Card 1/1
1. Air Force USSR

AID P - 5120
Subject USSR/Aeronautics - training
Card 1/1 Pub. 135 - 5/26
Author Ushakov, S. F., Maj. Gen., Hero. of the Soviet Union
Title : Who knows and dares is ahead
Periodical : Vest. vozd. flota, 10, 23-29, 0 1956
Abstract : The author strongly critizise5 the behavior of such
commanders who do not dare take risks during the training
of flying pe.-i3,j.!rel under adverse we3ther conditions.
The article is of some interest.
Institution : None
Submitted : No date

USHAKOV, S., Gercy Sovetskogo Soyuza, general-leytenuni, avialljii
,
.
Long-dis
tance bombers are in operation. Av. i k0sm. 47 n0-5:36-46
My 165. (YIPA 18:4)

USIIAK(V"S.-,, gene ral-leytenant aviatsii, Geroy Sovetskogo SoyuzEL
Fighting nights. Av. i kosm. 48 no.12:79-83 D 165.
(mLqA 18:11)

BARSXATA, N.; USHAKOV, S.; XATSEV, I.. rodaktor; HATISSEN, Z., tekhni-
cheskiY"PWMT&rr-
[gari A.S.S.R.; sketch about a documentary filnj Mariiskaia. ASSR;
ocherk o dokumentallnom fillme. Moskva, Goakinoizdat, 1952. 26 p.
(Mari A.S.S.R.) (KERA 8:5 )

USHaOV, S., uchonyy leeovod (Vladivootok).
NEWAM%MV
Iron birch (Betula Schmidtii). Vokrug eveta no.2:39 F 154.
(MLRA 7:2)
(Birch)

POLYUSMN, V.; USHAKOV, S.
Upedition-reaearch vessel 'Vitiaz." Xor.flot 15 no-5:19-21
MY '55. (MIA' 8:6)
("Vitiaz"(Ship)) (Oceanographic research)
0

USH&M, S.,1uud.tekhn.nauk
Important problems in raising railroad freight capacity. Zhel.
dor.transp- 36 no.6:9-13 JS '55. (NM 12:4)
(Railroads-Fraight)

USHAKOVS S., starshiy prepodavatell
Problems without complicated calculations. Nauka i zhizn' 30
no. 5: 50j 109-110 My 16". (MMA 16: 10)
1. Kafedra fiziki Vsescy-uznogo zaochnogo mashinostroitellnogo
instituta.

Of 1;Gin,- ~ilr---T ~~t prose cc "inp. Inf-:,
4-7 ei7 o s u n i7m r u i t (~t i:o o 1 f) i i a s Idy f ~zl, 11 t t
-,Ctho~s)

-US.UKOV, S.A., aspirant;IAZLROV, G.Ye., mladshiy nauohnyy sotradnik
Certain conclusions based on seismic and gravimetrIc observations
along the profile Little America-Byrd Station. Inform. biul. Sov.
antark. ekep. no.9:17-20 '59 (MIRA 13:3)
1. Moskovskly gosudarstvann" universitet.
(Marie Byrd land--Ice)

USHAKOV, S.A., aspirant; IAZAIM, G.Ye., mladshiy nauchnyy soturdnik
ThiOmess of the earth's crust along the meridional profile
Davis Sea - Pionerskaya Station. Inform. biul. Sov. antark. eksp.
no.10:9-12 159 (XIBA 13:3)
1. Moskovskiy gosudarstvenrn universitet.
(Davis Sm,;egiou--Geology, Structural)

USHAKOV, S.A.; mladshiy nauchnyy sotrudnik; LAZAM, G.Ye., mladshiv
-nau-c-hny7 so trudnik
The inostatic equilibrium of Antarctica. Inform.biul.Sov.
antark.ekep. no.11:17-21 '59- OTIRA 13:5)
1. Moskovskiy gonudaretvannyy universitst.
(Antarctic regions--loostasy)

3(6Y
AUTHORS Lazarev, G. Ye., Ushakov, S. A. SOV20-126-2-20/64
TITLEr An Attempt at Determining the Thickness of Ice in the Antarctica
From Gravimetrical Data (Opyt opredeleniya moshchnosti l1da v
Antarktide po gravimetricheskim dE=ym)
PERIODTCAL: Doklady Akademii nauk SSSR, 1959, Vol 126, Ur 2, PP 299-302 (USSR)
ABSTRACT: The seismical determination of ice thickness must be supplemented
by gravimetrical, measurements because of the large distances
between the points of seismic probing and because of the probability
of considerable errors being caused at some points. These
gravimetric methods may supply valuable information vith respect to
the thickness of the ice. In these zeasurements it is necessary to
separate the influence exercised by the e1ifference in ice thickness
from the influences of the lower factors. The ice proffile
investigated by the authors extends over a distance cf ^5 km from
the shore of the Mirnyy-Rayon into the interior of the mainland.
The points distributed on this profile at distances of 1 - 2 km
from one another either coincide or are not more than 500 m distant
from one another. The large difference in density (1.9 &/cM3 Y
Card 1/3 between the core layers and the ice is very favorable for the

-An Attempt at Determining the Mickne3s- r,-' 1ce ir-
Antarctica From Gravimetrical Data
application of the Eravimetrical method. The inves'%1-:U--ti'cr-s
out by the authors lead to the follo,.-,in& conclusiox.3- -1) 7cr
determination of the thickness of antarct4C iOC- --4r
1 1. . -
investigation must be carried out in ~~crjunctior- w4-th
investigations, In this way, not oi.1j, r-zrat ditta
thickness, but also some infon7x-tion
crust of earth below the ice may be obtai,.cd. 2) '11,P-a
gravimetrical data it is -possiblc to deter,:;ire t%e r4c j:;i c i
background by con7erting EUE;e's anc-maliez for Lei6`ht. If L.ere iZ
an isostatic compensation of t,ie covar of ice or. a
area of the eastern Antarc~-;~,'
represented bv the curve of 'Lie ic-~
above seal level (however 7r tl ed SiLr 7 -licn, 4 c~~. of
i I ci , AQ~ -
me-thod developed by B. V. Yumerov inerea3es the --cc.1-.-'CcY of ice
thicla,.ess deter-,nii;atirnzi from L;ravimetric data. The most rationall way
of caloulatinb~ thi c' neswo ac cord in~., to thio method i.,j by ~,o for
such distances betw1-.;c.. ~&,e e,,ra,.vimetric roiiits t,3 aro riot E;rer~tcr
t.'-i,; z-'four times the thickness of t1le ice. The authors th,=.k
Professors 77. V. Fedyns'Kiy, 11. A. YaLriitzl-kiy, and F. A. M-MLskj~' frr
Card 2/3 their help and advice, as well as Professor S. S. Vyalov,

An Attempt at Determining the Thickness of Ice in the WY/20-126-2-20/64
Antarctica From Gravimetrical Data
0. K. Kondrat"yev, G. S. Lopatinand S. A. Manilov for placing
data concerning glaciology and seismic research at their disposal.
There are 1 figure and 8 Soviet references.
ASSOCIATICK: Moskovskiy gosudarstvennyy universitet in. k. V. Lomonosovs.
(Moscow State University imeni M. V. Lomonosov)
PPMENTED: February 14, 1959 by D. 1. Shcherbakov, Academician
SUBUITTED: February 12, 1959
Card 3/3

67257
3 (1e) 3- 9000
AUTHORS: Ushakov, S. A., Lazarev, G. Yes SOV/20-129-4-19/68
TITLE: The loostatic Downwarping of the Earth Crust in the Antarctica
Under the Load of the Icecap
PERIODICAL: Doklady Akademii nauk SSSR, 1959, Vol 129, Nr 4, pp 765 - 788
(USSR)
ABSTICXT: According to 1. D. Zhongolovich (Ref 2) and Tanni the platforms
are essentially isostatic in equilibrium. Up to being iced the
inostatic anomalies and the anomalies averaged by Fay which are
similar to the former with respect to its magnitude (according
to S. V. Yerseyev (Ref 1) and E. Jeffreys (Ref 10)) must nearly
be equal to zero. The radius of this averaging was assumed, ac-
oording to S. V. Yevseyev (Ref 1), to be 118 km. The results ob-
tained by the Soviet Antarctic expeditions, which the authors
had available, indicate the existence of an isontatic compensa-
tion in the region under investigation. This leads to the fol-
lowing problem: It must be found how completely the isoetatic
compensation in the other investigated regions of the Antarctica
are realized. According to G. P. Wollard the thickness of the
rocks below the icecap varies Byiism-aikally from the periphery
Card 1113 of the Antarctica towards its center. Such a systematic variation

67257
The Isostatic Downwarping of the Earth Crust In the BOV/20-129-4-19/68
Antarctica Under the Load of the Icecap
is# according to the authors'oRinion, very improbable. The non-
agreement betweenNseismicl"Wnd ravimistriol%epth is essentially
due to the downwa-r-pi-ng- under the weight of
the ice. The existence of isostatio equilibrium in the profile
extending from Little America to Byrd may be concluded from the
analysis of Pay's anomalies. In the isostatic compensation of
the ice load Bugs's (Bouget's?) anomalies illustrate the in-
fluence exerted by the following factors: 1) The density relief
of the,layers below the ice. 2) The anomalies densities of the
rocks under the ice, 3) The regional gravitational background
duo:to the-isoptatic downwarping of the,--earth crust. If the ex-
06'86'ice 1oad I' isostatically fully compensated, Bugs's anoma-
liess after colderation of the regional background are nothing
but.P&yls anomalies.. Basing on this assumption-the authors cal-
oulated the depths of the lower layers in the profile Little
America.- Byrd. The good agreement between the gravimetric and
the seismic depths on the aforementioned profile confirms the
assumption-that the;excess ice load is essentially inostatically
compensated. The same also applies to the eastern part of the
Card 2/3 Antarctica. The existence of an imostatic equilibrium is also

67257
The Isoatatic Downwarping of the Earth Crust in the SOV120-129-4-19,168
Antarctica Under the Load of the Iceoap
indicated by the fact that the Antarctic shelf is, on the
av*rage, 200 m lower than the shelves of other continents.
The minimum of Pay's anomalies in the Pacific sector is pointed
out. The 0&us* of such anomalies hasp as yetp not been found.
It is further mentioned that the authors thank V. V. Fedjnskiy,
V. A. Magnitskiy, and P. A. Shumskiy for discussing this paper,
and that they also thank 0. K. Kondratlye , S. S. Lopati!!, and
-0. A. Manilov for making the data of seismic probing available.
There are 2 figures and 14 references, 9 of which are Soviet.
PRESENTED: May 4, 19599 by D. 1. Shcherbakov$ Academician
SUBMITTED: April 29, 1959
Card 3/3

5"C'. ~,,ICIO/Ci
T:TLZ: Chmol.l.
I
TEXT; Fr- s:.r IC-14. 1763 the
10
50 97rsvl~vlril (Slith
-1r:11try
moktsix. r".t & gv.d..11 1 j..fl. 1k, -k ~%R 'or
G-46.7 of the cormitte. of ;Qo--*3Y and ceoptYsics of t1if .-levy of
3eioncos MR) and the Aerm;r-i-tricreakayt latoratjriy~ :---utut, J
f131ki -21L AN SZSB (Laboratory for L*ro,;rxv-.=,try of t%- lm.~-titut,!~-,cf~-
rhZsles of the Earth of the A:; z,16 ropresont,tives of t,
org-saticna took vart in tti. conference: poduction
research contw:wo testing and constmetLon orrmnlzstl~rm, eSucatic-1
Instilutlons. &nJ org.misations o: the Akadonlys nauk -314 of
S.1-C-9 MR). Siblr.k*y. otJ.l.oLy. A." S359 f the
C--d 1/6
AS C'a ), &W.zll mnoak Zkratmskoy. ratimakoy, Lita-kay L
.Sr
At SZR CAC.d,oi- of of th~
;Msia.keya, LitovskAya, and At-b~yl-.hanskzja :2R), "el.t-atmo
.7.8h.Co I r do a ly,
~d S..-d ry'S;:.otl MI. i~ft the C53R).
okb6raA3r medr SSSS (21nistry of Geoloa and irouerv,tion of
ctct*t r letz,~ Injkh pribortv pet Zov,.%*
.1, . t :rittl
ILl *I" SH = t * 0 5 nd4rd . aou-s. &.14 ::aaxurirv~.
TAst~eutx of %be Coua%ctl or L'Unlaters ":S3), -.,:I IT'.
xQO1t:%cs--t. Lict.tr.v S=R p0 .1t-tit.tali i
(at.%ocost % ..0L.tometion trl. :..Ohit. co-t-tti- f %h, C-n-jj of
glnt*t.ra VSZR)s &2 well as reprejontntives of the factorlog of t~*
Xoakzvskiy so-r"oz (Uosoov 3-arkho-) and th* Leti-,rit.%17
;00-rkho. gravimetrie %pparatus.
at. be ld. Zh_ _. 01.1 h (lzWt.t
atr.. OaI4 Al I-F I~L,111,It. 1 Z--t--l Altro-Y or -h~
t . 4,
tmu% h -Fxporience
he TArth Proi Obm-~ tIot aof t -d
Card 216
ThlrJ Artificial Smtellj-e~ y1no-kly xtout he
Gr-Ilt-t-.1 Ac-lorati- or the
rolnt of V,
~1:1. In
p It tl:,:L.
7,-11~AIK- A 7tI
u1 n
-ZILA", L. A. ~bn-~t of -,I,.
H.C.M1.6 IrN-Tvnlu;~ '-'-mur-n-
and the
b.
All ZSZ;?, klulz
L. -~,e k1,14 of
n
the 1e -T.? Theory of Deqrm.-n1r,; :;-vit%t4.-1
Accelvr~tlon on the oeOtv Vomro ofvz;ravl=ot,rm-.
error. already i,qbli.h. :2
or u.it%ej
fo~ rublteation by .0ma authorm. A=one theae are paper. by
Vvovskly polltskh~lchvskly inatitut (Llvov ?olt,ctzrjc ~.njtj-u-,I~,
-2;dz (Femskiy Goeudxrntvenzj7j universLto. kll-lrv- lt~t,,
4 5. T. (L-ineml.kijr ~o.. I.r.t-.yy n1,er.lt.t
V~l C.~d 316

c hr.. I
r
-, TI.
R*~r-vntat- -4
r.;.rt.d on of L'al-"t;z
kat-tl
or t he Lftrtt 'Mot In the Antar~tira A C
Do I r %t,
*b..t In* paratlon I
,1,.n y te Conference are mentioned. Fro= Arrjl to 22, 1)"
ch~nlcal Confwr&nc* or U,o jirk.rs or t ~..
3,1-1~ S-I- .1 11. ~I-oy. t'pr., 1. Ily.
I Ckhr&~7 nair rri S-ote NInletrov Ckl."lk.y SIR (1., .1"
_I or
and 1 B--.. or th. C.
ssR I,I. I, of I
to
phlo-C.1d.tic and ...k In th. If th.
V3a CkrZZI) and the of n..
C.r4 'L16
_,k,.t I d 04,tot he
extent or I I
d be -Irk =,,i Ired
. In t,
.14 *;tlacroos#4 no"
.Ith
orai~ ""a. N r IIr., In*
fo'lo.i,tC dr..bck. -..d ..t: TA. -t"j- -P,11. 4N
1,*I,
"'a Crol_ical orq;,ni-obtlone are r-,
q.1 p -d 'In- ob.-rl.ti.n. th.'mf.-
PhQto,cr..~; end top.ir.p.-tt 1. - . '-K~ r. no.
Thl. t.t. I, by ln.ffj~j- .:.Ic,-
a -1 f,OL~nt t:Ch%lt anl tat,r1*1 2up;Ij, by a
I.-k
It.. 10 1 in tb at Z" loCiya CkrS~fl ftni tr,-~
I OL~--Y ft~dr SSER ..... of
lita.r.1 U--% or th. crm A t - d -.. p.,
I
%hIN For Tb. -k.r. IT
con f ran- su4;C* t-8 to catr4rt scientile and tec!,nl-I
'a. For i~ v , h
at r:Cular ;r. In In'. it d for th. cf
,l..- I.I.. -1't.1I.I board or tl. r _t ;or j o
fur:1.2, for -4 4..A.t. or' '
Ob**rv&tIM3. Uo "rtIct;&n-m In the C~nfermnc# to th: ork...
card 5/6
at the ht. an)
su"ey.lo.c ;N.Tlcq of I GY. .krjsg) to -r7thin,; ;-,lbl.
in order to ce.rry out the to uti- of th -lot F-t "cOtc-413 I' th4
C%l
I the cp
C Sty and -.he ?I.... of the of su I. J_..
card 616

88844
S/026/60/000/0 I 2,/V,;2/r/C9
(/6 Ai66/Ao27
AUTHORz Lazarev, G.Ye.; Us
.~akov, S.A.
TITLE: The Earth Crust of the Antarctic
PERIODICAL: Priroda, 1960, No. 12, pp. 17 - 22
TEXT: The article gives an account of the earth crust of the Antarctic
from data recorded by Soviet geophysicists in 1955 - 1958. Studied of the ice
cap were made in the Eastern Antarctic from the Mirnyy observatory to the inland
stations at Vostok and the Pole of Inaccessibility and also at intervals along
the coastal area of the Eastern Antarctic from longitude 55 - 1650E. Seismic,
gravimetric and magnetic observations have been made and an aerial survey car-
ried out along a U-shaped route from Mirmyy-Pionerskaya-Parr Bay and also in the
coastal area of Wilhelm II Land and Queen Mary's Land. Seismic studies of the
thickness of the ice cap were also made in these anas and gravimetric and mag-
netic research performed in other coastal areas of the Eastern Antarctic. Tt
was found that the mean thickness of the ice cap In the Eastern Antarctic varies
from a minimum of 2,000 m to a maximum of 4,000 m. The figure shows the sub-
glacial relief (top) and the thickness of the earth crust between Mirnyy and
KOM60MOliskaya. A subglacial upheaval detected in the central part of the Weet-
Card 1/5
LIX

ern Glacier is of the fault-block type and is probably the northern end of the
block mountains situated to the east of Olaf-Pruds Bay. The calm gravitatlonal
and magnetic fields detected between Mirnyy and a point 200 km towards Pioners-
kaya indicate that beneath this sector lies a plain with slight rises and de-
pressions. The proterozoic foundation is overlaid with low-magnetic rocks, Sim-
ilar to those which compose the bed of the Davis Sea. South of the 200 km
point an upheaval of the block type has been detected which, together with the
Banger and Obruchev Oases and the Stratkon and Amundsen Mountains, forms a sin-
gle system of upheavals stretching towards the north east. According to Soviet V,
observations, the eastern area comprises two separate structures; King George V
Land is part of a platform, while Oats' Land is probably a Caledonian fold
structure with component rocks no older than 300,000,000 - 400,000,000 years.
According to the values of Bouget's anomaly, determined along the meridian frcm
the Davis Sea to Komsomollskaya, this strip may be divided into 3 sections: 1)
from the Davis Sea to 100 - 200 km from the coast Is a section of transition
from a typically oceanic crust to a continental crust of the continental slope
type; 2) the maritime 100-km strip in the Davis Sea, and the land up to 50
km inland from Mirnyy towards Pibnerskaya is a shelf zone; 3) the section be-
tween the 50-km and 1,000-km points from Mirnyy, a little to the south of Kom-
Card 2/5

88844
S1026160/0,X/o 1 2,,TC2_,/CC0
The Earth Crust of the Antarctic A i 66/A 10 2~_
somollskaya, is a zone of platform depressions and slight plateaus. The zero
Bouget anomaly corresponds generally to a sial crust 33 km thick. The general
conclusion of the calculations is that the earth crust increases in thickness
towards the center of the continent from 32 km at M1rnyy to 37 km at Pionerskaya
and 40 km at Kom5omol'skaya. By its crust the Eastern Antarctic is, therefore,
a continent. In the coastal areas, however, (100 - 200 km inland) at depths of
2,500 - 3,000 m the earth crust is definitely of the oceanic type. Observations
have shown that the glacial loading in 'the Antarctic is fully compensated, com-
pensation which could only take place through a sagging of the earth crust. This
sagging is confirmed by analysis of seismic and gravimetric observations along
the stretch from "Little America" to Station Bird, and by the fact that the Ant-
arctic shelf is, on an average, 300 m lower than the shelves of the other conti-
nents. There are 4 photos, I diagram and 2 Soviet references.
ASSOCIATION: Moskovskiy gosudarstvenny universitet im. 14.V. Lomonosova (Moscow
State University imeni M.V. Lomonosov)
card 3/-5

88844
S/026/6o/ooo/oi2/oo2/ooq
The Earth Crust of the Antarctic Ai66/AO27
Figure (~D
111M,

Card 4/5

88844
The Earth Crust Of the Antarctic
Figure S
S/026/6-0/Cr,c/C !
A 1 (,'6/.,', G 27
Card 5/5

USUkKOV, S.A., aspirant
Soma structural features of George V Coast and Oates
Coast according to geopkvsical data. Inform.biul.Sov.
ant,Ark.eksp. no.18111-14 160o (MIU 13:7)
1. Mosko-.skiy gosudarstvenryy universitst.
(George V Coast-Geology, Structural)
(Oates Coast-Geology, Structural)

USHAKOV9 S.A.
Thickness of continental glaciations and the reaction of the
earth's crust to their weight. Biul. MOIP. Otd. geol. 35 no. 3:162-
163 my-je 16o. (MM 14:2)
(Glaciers) (loostasy)

USHAKOV, S.A.
Reaction of the earth's crust to the load of continental
glaciations. Dok:I.Aff SSSR 133 no.1:205-207 Jl '60.
(MIRA 13:7)
1. Moskovskiy gosudarstyennyy universitet imeni M.V.
Lomonosova. Predstavlano alaidemikom D.I.Slicherbakovym.
(Isostasy) (Glaciers)

N%
USHAKOV, S. A.9 CAND GEOL-MIN$p SCIl GEOPHYSICAL INVES-
TIGATIONS OF THE STRUCTURE OF THE EARTH'S CRUST OF 'NNW
ok.,~
EASTERN ANTARCTIC G"44"W- MOSCOWt 1961- (MOSCOW OR-
DER OF LENIN AND ORDER or LABOR RED BANNER OTATE UNIV IN
We Ve LOMONOSOV. UEOL FAC). MO 2-619 202).
-54-

0
S/1 6 62/000/006/0'- 3/093
D228YD304
Voronov? p. S.
AUTHORS: stions of.the study of processes Ox- isostasy
TI12LE: Some que
in Antarctica no. 61 19621 19, ab-
pBjaj0DjCAL: Referativnyy zhurnalg Geofizikaj VGiij
stract 6A133 (Inf6rm. byul. Sov. antarkt. ekspedit
no. 30, 1961, 5-8)
ecognize the isostatic ec
TEM: I.,ost research workers r C. uii4brium
-L V ca as the resu-It of the crust's warping under the weight
0- n~arcti of %he mechanism
load. The chief problems of the study' e of the reac-
of the ice 'j) 13stablishing the natur
of isostasy are as follows:
1 .0 zones on the glaciation cover;
ti-on of different crustal structural mainlandIZ Peripheral
2) determining the area of the Antarctic sunk well below the
Zone that is devoid of continental ice and has
ues of the crust's elastic-
normal level, which will allow the val Ia4
lastic parameters to be defined more accurately; and 3) obu ~-ning
gophysical proof of the isosta-Vic uplift Of Fast Antarctica's
-9
card 1/2
Some questions of S/169 62/0
block D228 D304 00/006/013/093
t'~; e as a result
Of Which it V/
zechania,m Of 'Ubstratal diffluence. Ostracter,s note: COM
be p6s8i ~le to fi
Plete translation.-7 A
Cax-d 212

S/035/62/bW/010/117/128
AOO11A1O1
AUTHORS: Voronov, P. S., Ushakov, S. A.
TITLEt aome problems of studying processes of Isostasy In the Antarotio
PERIODICAL: ReferativnTj zhurnal, Astronomiya I Ge~dezlya, no. 10, 1962, 39,
abstract 100199 ("Inform. byul. Sov. antarkt. ekspeditsii", 1961,
no. 30, 5 - 8)
TrAT: The most explorers consider isostatic equilibrium of.the Antarc-
tic as a result of Earthts crust sagging under the ice load weight. Main prob-
lems in studying the mechanism of isostasy are as follows: 1) establishing the
rust to
character of reaction of various structural zones.of the terrestrial c
cover glaciation; 2) determination of the area of the peripheral zone of the
antarctic continent free of continental ice and sunken considerably below the
normal level, which will make possible to determine more precisely the values
of elastic-plastic properties of the terrestrial crust;: 3) establishing geo-
physical evidence of isostatic rise of Eastern Antarcti~ block mountains, as a
result of which it will be possible to determine the mechanism of spreading of
the substratum. B. Bryusov
,~Abstracterls note: Complete translation]
ard 1/1

USHAKOV., S.A.., starshiy nailchnyy sotrudnik
preliminary results of geomagnetic studics in western Enderby Land*
Inform, biul, Sov. antark. eksp. no.37:X-37 162. (MliU 16:4)
1, Moskovskiy gosudarstvennyy universitet.
(Enderby Land-Magnetism,, Terrestrial)

USHLKGVP S.A.
Relation between the gravitational filed and the geological
structure of investigated antarctic regions. Dokl.M! SSSR 145
no.6:1275-1278 Ag 162. OURA 15:8)
1. MOBkovskiy gosudarstvennyy universitet im. 14.V.I4monosova.
Predstavleno akadeiftikom D.I.Shcherbakovym.
(Antarctic regions--Geology, Structural) (Gravity)

LAZAREV., G.Ye.; USHAKOV, P.A.. - ,
Gravity field and subglacial relief of Alm central part of eaotern
Antarctiout Dok:L. AN SSSR 152 no.2.-4-00-403 S 163. (MMA 16:11)
1. Institut fiziki Zemli im. O.Yu. Shmidta AN SSSR i Moskovskiy
gosudarstvennyy universitet.im. M.V. Lomanosova.' Predstavleno
akademikom D.I. Shcherbakovym.

GIADUN, V.A.; DEMENITSKAYA, R.M.; STROYEV, P.A.; USHAKOV, S.A.;
FROLGVp A.I.
Some results of geophysical studies of the crustal structure
in Antarctica to the north of Novolazarev Station. Dokl. AN
SSSR 153 no.6:1398-1399 D 163. (MIRA 17-1)
3. Moskovskiy gosudarstvennyy universitet im. M.V. Lomonosova
i Nauchno-issledovatellskiy institut geologii Arktiki. Pred-
stavleno akademikom D,I. Shcherbakovym.

FEDYNSKIY, V.V.9 doktor fiz.-mat.
nauk,, otv. red.; ISAKOVICH, T.D., red.; IJL"YANO'VA, O.G.,
tekhn. red.; DOROKHRIA, I.N., terkhn. red.
[Collection of articles of the Intergovernmental Committee
for the Execution of the 17ternational Geophysical Year]
Sbornik statei Mezhduvedomstvennogo kamiteta po provede-
niiu Mezhdunarodnogo geofizicheskogo goda. Moskva, Izd-vo
AN SSSR. No.4. [Geophysical studies of the crustal structure
in the eastern Antarctica] Geofizicheskie issledovaniia stro-
eniia zemnoi kory v Vostochnoi Antarktide. 1963. 91 p.
(MIRA 17:2)
1. Akaderiya nauk SSSR. MezhduvedomstvenMy komitet po pro-
vedeniyu Mezhdunarodnogo geofizichaskogo goda. XIII razdel
programmy MGG. Gravimetriia.

GLADUN, V.A.; STROYEV, P.A.; U'SHAKO-Vo S.A.; FRcLOV, A.I.
Geophysical studies of the eartn's crust in the transitirn zcn--
from Antarctica to the Indian Ocean in the area between 550 and
1000E. Dokl. AN SSSR 153 no.2:427--428 N 163. (MIRA 16:12)
1. MoBkovskly gosudarstvenny-y iiniversitet Im. M.V.Lomonosova.
Predstavleno akademikom D.I.Shcherbakovym.

L 16149-65 E19(1) Pa-4 ESD(t)/3SD/AFWL/.'.c T-P G11
I _1
ACCESSION NR: AP4045632 S/002J!641158/002/c34510347
AUTHOR: Gladun, V. A.; Ls ev Ye, N. ; Koryikin,___Ye,__D. ; qtrqyqy,__P, A.;
Ushakov S. A. : Frolov. A. 1.
TITLE: Results of geophysical investigations of the s of the Antarctic
in the Enderby Land region
SOURCE: AN SSSR. Doklady*, v. 158, no. 2, 1964, 345-34?
TOPIC TAGS-- isostasy, earth crust, Antarctic, Enderby Land, geology, geophy-
sics
ABSTRACT: Antarctic is, on the whole, in a state of isostasy insp-..te of the ex-
cess of the ice load. This is, however, not true with respect to certain sections
of morphological structure. One of these sections is the Enderby Land where the
Soviet Antarctic Expedition conducted in 1961-1962 geological and geoph I I
investigations of the earth crust. The map of the kiravitational_ anomal as pre-
pared, and the depth of the Mohurovicic surfaces determined. The measurements
indicate that the young block mountains in the west of Enderby Land are far from
carcl 1/ 2

L 16149-65
ACCESSION NR: AP4045632
isostasy. The authors are grateful to R. M. De"nitsk-ay-a for discussions.
Orig. art. has: 3 figures
ASSOCIATION: Moskovskiy gosudarstvenny*y universitet im. M. V. Lomonosova
(.Moscow State University); Nauclino-issledovatellskiy institut geologii Arktiki
(Scientific- Research Institute of the 9!~ ~Io of the Arctic)
SUBMITTED: 29Feb64 ENCL: 00
SUB CODE: ES NO REF SOV: 006 OTHER: 001
ard2/2

Z111VAGO, A.V.;
J,r-n zcne of "oni-arctics
st.-,1,-ture an(i enr~'-.'a c-ri.-'3t. Dokl. A"I
SSSR 155 no. 3.,565-568
u1 17: 5)
I Is t Vf foi I.-!. r i i A N j-otndav.-.Lvnnn,vy
i I I. a I to t' i ill,! :' . V. 1 -014 0 fl.) i1 6kadomlkotr,
D.I.Shcherhakovym.

L 24823-65 FYr (1 Ak F F,M r_'W
ACCESSION NR: AP4046375 0-~002n/64/158/003/0594/0597_
AU'rHoR. Ga~Manov, A. G. ; d_Lh2.,kaK,5, &
TITLE: Isostasy and plutonic structure of the zone of the transition of the Asiatic
Continent toward the Paciric Ocean in the reainn of the (7hishirna-Kamchatka
Dept-ession
SOURCE: AIN SSSR. 1-11', K 'La'j-e~ v 15B. no. "15, 1",64, 594-597
TOPIC TAGS: Qa.Lth cru.�t, isostatic deflection, Chishima Kamch-atka depressie_-n,
geology
ABSTRACT: Recent investigations have disclosed thpt tho P;irth c-rliqf ha!2 n- -1911'-
derable plasticity M A. Heiskanen and F. A. Vening -Meinst, The Earth and its
Gravity Field. N. Y. 1q58) The )resent paper investigates tile isostatic state of
a given region by the rriethod suggested b- Lyustikh, Tr. Geofiz. inst. 38, 2 (1951
in which the pressure P = Z C-- H, ronczt. where e~ is the riensitv off the i- !a-,-e
i s t Jh;~! de ryt h o r t h Prm w n Ez i rrAc 7, express on
is valid f r) r H10 'k. rrT r-f-, .k; q p 7 r rC3 t t j r- r) s T a tt A t e

Kamchatka depression, Orig. art. has: I figure
ASSOCIA7101N- Mosknvskly gn_qudar3tven.,vv*y -uriversitet im. M. V, 1,ornonosc.va
%lyluuVOW, 51"Cat-e
SUBMITTED: 29Feb64 ENCL: 00
Sula COD& E.S %_"C) =14 F sov~l ollig OTHER- 002

IISII,IKQ-V, ~ .13hly ?I,-Illc-hnyy sotrudrilk
, - A., mln(I
Thickness of the earth'3 cru--t in th!~ Enderb-I r~--Pi,:n
according to gravimetric data. Iniorm. biul. Sov. antark.
eksp. no.47:50-53 164. OMIRA 1~11-4)
1. Gosudarstwnnnyy astronanicheskiy instLtut

ACC NRs AT6016944 (A)
SOURCE CODE: UR/2639/65/000/000/0053/0060
AUTHOR: Lazarev, G. Ye.; Ushakov, S. A.; Bugayev,-Yu. G. (Professor)
ORG: none
TITLE: Methods and basic results of geodetic and gLav~i~metric investigations of the
ceutral sector of eastern Antarctica
N'Y
SOURCE: AN SSSR. Mezhduvedomstvennva komissiy~i yo igljcbLqa~~
_Aalarktiki. Antarktika
_Z~~ 9
(The Antar t c -,--jo-kl-a-ay7W6iWssir,-*I~~64.-K6-dc-o-w, Iia-vo Nauka, 196~ ~i-60
TOPIC TAGS: gravimetric survey, geodetic survey, sea ice
ABSTRACT: Measurements (begun in 1959) of the altitudes of the ice surface and the
force of gravity in Antarctica are described. Absolute altitudes were calculated from
the mean sea level of the Davis Sea; the Vodomernyy bench mark, served as the basic
land station. In the gravimetric survey, differences in the force of gravity were mea-
sured using several gravimeters in order to minimize observational errors. The er-
rors along the Mirnyy-Komsomolalkaya, Komsomollskaya-Sovetskaya-Pole of Inaccessibili-
ty, Vostok-Polyus, routes do not exceed 12, '1, '2, '4 mgal, respectively. The er7.
rors in the determination of the force of gravity at Mirnyy, Pionerskaya, Komsomol'-
skaya, Vostok, and Sovetskaya do not exceed 12,5 mgal. The geodetic observations
show that 1) daytime is the best time for geodetic surveys because refraction is at

L 38687-66
ACC NRs AT6016944
a minimum; and 2) the errors in the determination of mean altitude values (employing
direct and reverse leveling) are of a random nature. The gravimetric data show the
presence of several anomalies of positive and negative types, ranging from 30 to 100
mgal. Analysis of the data revealed the following relief zones: 1) from the coast
line to 680 S, relatively small highs (up to 400 m) and small depressions (to -300 m);
2) 680-710 S, sizable mountains (up to 1000 m) and depressions; 3) 711)-750 S and
870-1000E, where the relief of hard rocks is almost at sea level with extreme alti-
tude variations of +500 m to -150 m. Orig. art. has: 1 table, 2 figures.
SUB CODE: OW SUBM DATE: none/ ORIG REF: 006/ OTH REF: 001
Lc-,d 2/2 2fC

USHAKOV, S.A.; KHAJN, V.Ye.
Structure of Antarf-IJcki based on veolovical -~nrnrq~lcql
data. Vest. Mosk. un. 3ar 41 Geol. 20 no.1:3-27 Ja-F 165.
(MIRA 18: 3)
1. Kafedra geofizlki i kafedra dinamichaskoy geologil Moskovskogo
gasudarstvonnop

L 2761Q--��.. EWT-W- -SW
A C C N R i A F -6'o-- 1-6- SOURCE CODEt UR/62 15765-10- 0 -0762 Zoo 3776651
431
AUTHORi Demonits~ga, go It#; U _W
ORGt Scientific Research Instit otic G2010gy (Nauchno-iseledovateltakty
institut goologii Arktiki); Moscow State Universkty (Moskovskiy gosudarstv9smyy
univoreltet)
TITIZi Relief, isostasy. some characteristics of structure of the uppor mantle in
Antarctica
Yr
SOURCEt Sovetskaya goologlya, no, 12, 1965, 37-51
TOPIC TAGSt Hohorovicie discontinuity, upper mantle, Earth crust
ABSTRACT: The article cited below is a summarization of intormation on
-relief# icootasyp crustal structure and the mantle; more than fifty
Soviet and foreIgn sources are cited. Figo 1 in a sketch map showing
the extent of geological and other studies in Antarctica; Fig. 2 is a
sketch map of the bedrock relief of Antarctica; Figo 3 in a sketch map
of averaged Faye anomalies; Fig# 4 is a uketch map of iaostatic anomalies
.in Antarctica; Fig. 5 is a sketch map of bedrock relief in Antarctica
after deglaciabion; Fig, 6 is a sketch map of the depths of the Mohoro-
vicic discontinuity in Antarctica. These maps are cited here since the7:
form the basic forthe text and indicate in part the scope of the mater- .~

L 27610-66
ACC NR. AP60243-1
iial covered* Within the entire Antarctic region covered by continental
and shelf ice there is a cruet of the continental type and only in indi-I
vidual sectors is it possibly of a subcontinental type. The amplitudc.
of the relief of the surface of the mantle in Antarctica in about 40 km,
Within Antarctica the temperature at the surface of the mantle varlea
from.150 to 9001C and pressure from 1-2 to 15 kilobarso In all proba-
bility the matter of the ourf,,ce tlo,is in a crystallino state*
qf the man
Orip art#, hast 6 figm7aso DPR-S7
SUB COM 08 / SUMI DAM none / ORIG REFt 029 OM REF: 024

ACC NRI A116036761 SOURCE CODE: UR/0020/66/171/001/0091/004
!AUT11OR: Ushakov, S. A.
;ORG: 'Moscow State University im. M. V. Lomonosov (Moskovskiy gosudarstvennyy
iuniversitet)
,TITLE: Dynamics of the Earth's crust in the transition zone from continents to
I
~Atlantic-type oceans
i
ISOURCE: AN SSSR. Doklady, v. 171, no. 1, 1966, 91-94
jTOPIC TAGS: earth crust, geophysics, oceanography, ocean floor topography, geodynamics!
ABSTRACT: The dynamic forces in the Earth's crust in the transition zone between the
continental mass and the ocean basin are analyzed. The author evaluates some
geodynamic characteristics of transition zones: sediment thickness, ocean floor
topography, and shoreline formation. Recently acquired knowledge concerning the
Atlantic-type transition zone shows that the continental slope and the continental
shelf of the Atlantic and Indian Oceans have a definite form, that the relief of
the continental slope and the continental shelf are symmetrical reflections of the
boundary relative to the free surface of the mantle, and that the granitic layer
wedges out at depths of 5-10 km. All these phenomena can not be explained solely
by the slow movement of the upper layer of the Earth's crust above a typical ocean
floor. Experimental models have shown that creep determined the forms of the
Card

ACC NR. "6036761
internal structure and surface of the Earth in the Atlantic-type transition zone.
Thus, it is assumed that the Earth's crust has a certain threshold for crustal
creep along the mangle because complete leveling out of the Earth's relief would be
observed otherwise. The existence of a threshold the creep implies that the latter
process must take place in a layer of limited thickness at the level of the free
surface of the mantle. The diversity.in the vertical thickness of blocks of
the Earth's crust, continental and oceanic, gives rise to considerable horizontal
forces that reach a maximum at the level of the free surface of the mantle, Orig.
art. has: 2 figures. [BA]i
SUB CODE; 08/ SUBM DATE: 03Jan66/ ORIG REF: 010/ OTH REFs 0031
ATD PRESS: 5109
CardL 2

SOV/1 Z4-57-4-4497
Translation from: Referativnyy zhurnal. Mekhanika, 1957, Nr 4, p 91 (USSR)
AUTHOR: Ushakov, S. A.
TITLE: The Possibility of Employing the Method of Circular PS Measure-
ments in the Determination of the Direction and Approximate Rate of
Seepage Flow (VozmozhnosV primeneniya krugovykh izmereniy PS
dlya opredeleniya napravleniya i priblizitellnoy skorosti filltratsii)
PERIODICAL: Sb. nauch.-tekhn. inform. M-vo geol. i okhrany nedr, 1955, Nr 1,
pp 62-64
ABSTRACT: Utilizing the proportional relationship existing between the intensity
ofan electrokinetic field and the rate of seepage, the author demon-
strates that, by means of measuring the radially projected intensities
of the electric field and plotting a locus in the shape of a figure eight,
it is possible to establish the direction of the seepage flow and evaluate
the absolute magnitude of the seepage velocity (within the limits of
accuracy of determination of the electrokinetic properties of the soil).
The method described was employed in the field investigations carried
Card 1/1 out by the Severourallsk geophysical expedition. A. V. N.

IVANOV, A.G., inzh.; OKERBLOM, Yu.I., inzh.; USHAKOV, S.G., inzh.;
GROMOV, G.V., inzh.
Results of the studies of a turbulent ZIO burner with a radial
twisting apparatus and regulated twist of the flow.
Energomashinostroenie 9 no.9t8-11 S 163. (MIRA 16:10)

BOKOVP A.S., inzh.; 711ADAN, N.Ya., inzh.; PANKRATOV, G.M., inzh.; USHAKOV,
S G. inzb.
-.1 - ~~ I
Burning of Bashkirian coal in ejector burners with gas drying.
Elek. sta. 35 no.6:11-15 Je 164. (141RA 18:1)

Ju
AA
'if
00
of a
00 a Laminated jillistic S. 1. 1 Y, M 1,,L .... #40
00 8 Anti S, 1. KtwhutvnL,,
00 a 110.1 1"K01w. I.v I'Al,tr will] 4,1 AO 0
00 1 .1.1. If Asti)'. ial 1, qn. ..I thr OVIt, plu 11.4
4fill llh~ 9414 1191tift. "IIP b .-I" M- 1-1-4JI-A M OW 1-41-1 111. -09
00 tit, It'll 0
coo
00
0
oil
00
--go
moo
it
00
%00
=00
woo
a L inaii t, a.. 46C too
v -4v -F-6-
a Air 00 is AM I I a 04 0 1 W of- --I a 4j
R w " a ff
w
0 0 * 0 0 0 0 0 0 0 0 0 0 0 0 0 0
0 Ce a 0 6 0 0 0
0 ::o 0 0 0 0 0 0 0 0 0 9 0

The CommIttee an Stalin Prizes (of the councii or Kinisters USSR) in the fields of
science and inirentlons announces that the folloving scientific works,, popular scien-
ttfic books., and textbooks have been w1haitted for competition for Stalin Prizes for
the years 1952 and 1953- (FAwetskAya Kulturap Moscow, No. 22-40, 20 Fob - 3 Apr. 1954)
Nam Title of Work Mosinated by
Us'-~!Aov, S. 1. "Coltoi Cro-wUN 11 Mi.nistr,., of Ai-ricultur, 'U%bek
T Ib o )k SBR
SO: W-30604,, 7 JaY 1954

usimov,
R T 11 1- _i a', -
1 -892 (Penzyl dihydrccja'-ie ate - , w-w ~Jastjcizer) Novyi Plartifi-kator - 'cerzil' c'
ietat.
PusrlCliS3KI--'*' IIIIAS3Y) (3): 4-8, 1935.