SCIENTIFIC ABSTRACT ZUBTSOV, P.A. - ZUBZHITSKIY, YU.N.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R002065610012-8
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: September 1, 2001
• Sequence Number: 12
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

ZUBTSOT, P. A.
ZMTSOV, P. A. ---"Investigation of an AG Tachometer Generator.: Method of
Calculation." *(Dissertations for Degrees in Scienee an(lUgine"ring Defended
at USSR Higher Mucational Institutions) Kin of Highsr Mlar~Atioa USSR, TAnItWraa
Polytechnic rnst imeni M. 1. Ealinin,'laningrad, 1955
SO: Knix lotopis'. No. 25, 18*Jun 55
For Degree of Candidate in Vichnica-1 Sciences

SPIZHARSK-TY,, GRONVW Yu,,Ya.; T-~,Inimcli whploi-ij ti 3p(,Wvlxovp 44,6;
0014-7,TSAMA., T~ . lil u L.T.41MITALI)
L 11"llig olaih,, Me tod1
r-a,:kj a' fo r
ploogoog. 10310 (MIPAii8.6)

15-1957-12-17069~
Translation from: Referativnyy zhurnal, aeoldjiya,:l957$ W.12,,~
P 53 (USSR)
AUTHOR: Zubtsov, Ye. I#

TITLE: Shan
Structural-Facial Zones of Tyan16 -:and the,Deep
Fractures (Reported at the i6~'Seialon'of S~iintifio
Council VSEGEI on April 5, 1955Y. [Strukturnolfatiiall
nyye zony Tyan'-Shanya i glubinn~ye razlomy (DOklad na
godichno sessii uchenceo soveta, VSWEI 5 aprelya:
1955 971
PERIODICAL: Inform. ob. Vses* n"i,, geol. ih-4a, l956, Hr.4,, PP 38-45
ABSTRACTs It has been assumed::until now ti~fat Plileozoio deposits of
'
,be 0defly a~facjal
the Chatkal-Naryn Zone appear t6
variety of Middle Paleo oic for~atidns (Sil~~an,! Denovian
th
eP
d
ih
if
d
b
l d
e
n
and Lower Car
on
ero
a
evelope
JA
''
t
T
S
t
h
-
van
geo-
Pergana-Kokshal zone of
ern
he sor#
hAn
syncline, Only in the northweat,, Iii i6 Karatauiand
Dzhebagly Mountains was therea known section of a dif.!.
t
f
t
t
eren
arruc
ure wi
h a lar discontinuity ahd an angu-
f,
~th
l
f
it
i
ar uncon
orm
e lower
the Silurian and,
n place o
y
Card 1/4

15-1057-12-17PO
Structural-Facial Zones of Tyan'-Shan' and th
OL, iep!Practurei (Re-
ported at the Annual Session of Scientific C i V.~EOEI on
April 5. 1955)
lower half of the Devonian* Thid section was not,conside;~~ed
7
typical for the whole Chatkal-Karyn zon6, but on!IV for iti
northern margin. The author and other geologist" explain4d-Oiat
Te-
such a structure of the Paleoz6ic section exists''bLlso inithe:
maining territory of the Ghatkal-Naryn,zone~ which fact sha dy
.0 rp
contrasts the latter with the Pergana-Kokshal :bone and a,soi'with
the southern Tyan'-Shan'. The author coniidersithe Chatkal-, !
Naryn zone (together with Kurandnakaya. zon4~ (zone)] as aniindividual
structural-facial zone separated from the:6outh~and north!TY#.n
Shan' zone by the large and deep marginal,fAulte (see the~'diqL-
gram). Overthrusts lying nearthese sharp bordors are considered
as local and without any influence on bringing together -of thb faclede
The Whok arphsaftes the great value of a study pf,ithe deep marginal frictures
for qlarifying the,,de-mlopms~t_of active crustal zotte, for solving the problems
t
of i0taMaPnesisAnd,fok guldlig the exploratory a~tiviiiosw
Card 2/4 A;'Id 1. Suvorov

Structural-Facial Zones of Tyan'-Shant and th6 Deep Fracturos (fte-
ported at the Annual Session of Scientific C04XII IISIMEI on :April 6j.
19mat
70
W
Al -A U
I
k I I
ovy A

42

N.4 Ale
A
AS

10
2 OKA
7 5

Card 3/4

-lgr -12-17069
1
5 'P7
Structural-Faoial Zones of Tyant-Shan' and~the De;ep Fractures (He-
ported at the Annual Session of Scientific ObuxiAl VSEGEI, on April 5j.
3 4 5 6! 7
1 Northern Tyant-Shang; ? Central Tyanf',-6han I aa C ha tih: al
Naryn. zone,, b -, KuramjnsWWa zona;!, $, - SoutheA T.Y! an I ~_Shan
4 - Faults: ABC -,"Most Ijhportant Strae'tur'al Line" 'of T A.
Nikolayev, BD - 'Talasti-Ferganam.1! faultj EFryff - Faults a; the
border of the northern and thu southern Tyapl,-Shanl, 1E ~'. Faalts,
at the border of Chatkalt,-Naryn- and XuraminskA3a zones;
5 - Intrusions controlled by the deep:Paultsl
Card 4/4

BOGOYAVLENSKIY, Nonstantin Nikols7evich; UALOBDVp ~J.ktor
VladWrovioh; DMGACM p VI ,adWr 1vancpf1$chj ZU11T
4MMhail Yef movich- UNDIKHOV, Alekoandr 1 1"! 0b;
___ J' ";Nikv1(qav1ohj MILLER, T,.Ye. red.;
KOV.
KOV, N
ELIKIND, L.H., red.iod-va; ISLENTIYEVAy NO., tokhnered.
(Working nonferrous metals and alloya by~*aswwe] Obra-
botka tsvetnykh metallov i splavov davledem. ['By) K.Nv
Bagoiavlenskii i dr. Izd,2'' ',porer. i dop;~.,,Moskvaj Me-
tallurgizdat, 1964. 564 p. [IRA 17:3)
d

i I
7
II i
11 i i
ZtTil"iOVApfe.l. ;
_LtK�QV -1

SMIYAN, Yu.P., veterinarnyy XORMTSEVA, L.~*
Aotivo and pavoive immunization of ducklinga agaInst viral h6patitis.
VeterinAriia 41 no,3t40-42 Mr t64# (KI4 1~tl)
1. Ukrainskaya reepublikanakaya veterinarta~& laboratoriya Ministerstva
sel'okogo kbozvaystva Ukrasa (for Smiyan) 2* t1javVy veterinarMy
vrach Gosudarstvannogo nauchno-kontrollnogolinstituta veteritarnykh
preparatov (for Zubtsova).

ZUBTSOVv Te.j.; ZUBTSOVAt U.I.; HIKLMOAAJUAY,,~A.D,
Now hids of marine Permian deposits In Tion, 86an, Dokl, AN SSn
116 no.4:681-683 0 157. (MIRA 11t3)
1 Vaeanyusnyy nauchno-inalmdovatellakly,,#-,Oologlahomkiy listitut L
i;ningrAshy gaeudarstvannyy universitat im. A.A-v Shdanov&. Prod-
stavlonu almdevdkom D.T, Waliftinym,
(Tien Shan- Pals ontology)

2o-119-4-41/6o
AUTHORS: Chirkova-Zalesokayal Ye. F., Zubtso'y? Yei. I.
TITLE: New Pounds of Stevphanian Stage Flor!a in Central Tidh Shan
(Novyye nakhodki stefahakoy flory V~~Srednem Tyan'-Shane)
PERIODICAL: Doklady Akademii Nauk SSSR, 19% vfil,, II 9j lir 44
ppo 776 - 778 (USSR)
ABSTRACT: M. D. Zaleaskiy (Reference 1) described in,1920 fossil flora
from the region in question which is very sirailar to the'
complex of the Stephanian f lore, of Vastem Europe - On 1he ~ strength
of this single found the late Paled%laic aInd Plaristi~o distri-
bution of zones of the !whole earth ~waa retionstruct4di,(Re'feren-
ce 2). In this connection further fo4nds,,2oo km wesi of the
first site (Naryn-Tau),i.e.in the goic-Irim-Tau-chain:0955)
are interesting. The found was made 1)y Y6. 1. Zubtsoy and
Ye. I. Zubtsova and was investigated! 1by Yts.,F. Zales4ksy~&.The
containing rook is described. Then the author repeats the de-
tails of the first found of the florm in que-stion (Reference 1),
Card 1/2 and describes the composition of the1lora from Kok-Irim-Tau.

2 o- 1194.41/160
New Founds of Ste'phanian Stage Flora in Central Tian Shan
A strange lycopod C~nopqdiaceae);MA'iroesia rhotboidoft
Goth.and Jong.(Reference 3) is at Ig -here* This type was
described from north west Sumatra. Then:t1le single'sitos-
of St4phanian flora are enumarated.1he founds were~mado in
Kok-Irim-Tau in three different plad,ea, however, in.approxima-
tively the same horizon, A description of the last',mentioned
plant (figure 1) follows. Then the position of theilaye a is
compared with the flora in questionIn Kollc-'Irim-Tau and~in
Sumatra.There are 2 figures and 3 referenbas, 2 of which are
Soviet.
ASSOCIATION: Institut nefti Akademii nauk SSSR (Ntrolhum lutit-atej
AS USSR)
PRESENTED: December 6, 1957, by S. 1. Mironovp Hember, Academy of
Sciences, USSR
SUBMITTPD- Mmvember 28, 1957
C"xd 2/ 2

I

AUTHORSs Zubtsov, Ye. I.j Zubtsova, Ye, 1. 4g/~i
MikTu_kR_o_-15k_1ay , A . D
TITLEt New Discoveries of Marine Permian DepOsits in the Tion-Shan
(Novyye nakhodki morskikh permakikh oflozhoniy v Tys.O-Sh4ne)
PERIODICALt Doklady AN SSSR, 1957, Vol. 116, Pr it$ pp. 681-683 (USSII)~
ABSTRACT: It is customary to consider the northern margin of the Fergana
aInd Tarim depression as the northernboundary of the'v*rine Per,
mian deposits in Central Asia. There~is an assumptioit according
to which the coast line of the Permian sea:took its course some-
what northwards in the east of the liAe BoSbu-Tau mountains -
south eastern slope of the Chatkal chain. Since this~4ssumption
was up to now not confirmed, the diacoverj~of marine lower Per-
mian deposits in the north west of the Ferganat i. e.:in the dis-
trict of the Naryn depression by the two first authors in.1956
is interesting. The finds are of two diffevnet places'(their dis-
tance is 6o km). a) in the eaetern pult of the Daybiche-Tau chain
(Ulan river valley) and b) on the soathern slope of the lloryn-
Tau chain. At the Ulan river the expo~ureu have a breadth, of Boom
and 3 km. They are covered by unconf6Vui red
-colored tortiary de-
.
posits in the north and border in thO.Aouth along thelfracture to
Card 1/5 a thick chalk mass of lower carbonif orou3- The real charaoter of

New Discoveries of Marine Permian Deposits in the 1,ien-Sban- 2o
the Permian-carboniferous-relation isinot quite clearlheie. The
cross section is described in detail and the names of,thd fossils
of single horizons are given. The total thickness of the lower
Permian amounts here to 470 m- In the14aryn chain a thick com-
plex of terrigenous deposits of the upper palaeocoicuu' is devel-
oped. Final conclusions. According to~lthe quantity and the syste-
matic composition of the foraminiferw~the Permian exp4)sures of
the Baybiche-Tau chain are much richei than those of~the same age
of Naryn-Tau. The differences are appirently connects ILad. with the
facial peculiarities of the sites. The knowledge given in!the pa-
per concernin3 the systematic amount of the fusuliniaen 4n the
Baybiche-Tau exposure shows that the two fauna zonesi(the.lower
with a paraschwagerinp3quantity; the upper with a lot.of parafu
sulines) on the whole correspond to the central Karadhatyr hori-
zon of Ferganaa( according to the strAigraphic scheme,by-Miklu-
kho-Maklay). Any original species whicli do hot occur ih the early
Permianof the Fergana depression lac~'~hera~ The occur ~ena e of a
rath er great quantity of forms is *triking; they aru isiraiiir to
those of the upper part of Tayyuan' ser~ds of Vorth China~and to
those of the Chuant-Shan' aeries of South China. Verj, interesting
is the discovery of 3 species which are.described from the Car-
Card 2/3

New Discoveries of Marine Permian Deposits in the hen-Shan. 2o-)#.42/51
nic Alps (A. Shellvin), here in great~number of individuals.
There are onlj few species which cou.14 be tound in the schwage-
rine layers of the Russian Plateau at~l in the near-Ural egion.
From the occurrence of the same specion in~the,Carnic.klps, Per-
juana , and China it can be concluded to especially favorable mi-
gration conditions of the fauna in thd~.. latitudinal extention.
There are 3 Slavic referencea.
ASSOCIATION: All-Thd- Scientific Geological Researoh. Inatitute, State Uni-
versity imeni A, A. Zhdanov in Leningrad (Vsesoyuznjy~nauchno-
issledovatel I skiy geologicheskiy institut, Leningradskiy gosudarst-
vennyy universitet iui. A. A. 6hdanova)
PRESENTEDi May 11, 1957, by D. V. Nalivkint Academician,
SUBMITTEDi May 8# 1957
AVAILABLE; Library of Congress
Card 3/3

o.l.; ZUBTSOTA, Ye.l.
Pro-Carboniferous deposits of the Takhtelyk-Ridgd, Xok-Iriw-tautj
and the northern edge of the Marjrn Valley iii thelian Shan. Inform.
abor.VSZOBI n0-3-3-9 156. (HLRA-iOll)
(Tien Shan--Goologro Stratigrapixte)

A=MI.-Y's =1
Formation of the eastern, Fer&%nm coal basin*: KAt.Y.MAI no.1
32 156.
OKLRA :1)
(Fergma-Cota geology)

Z~u B T S ~O~v
On the most important faults of the Tien Sbanl~. DokI. AN SSSR
ill no.3:673-675 N 156. 10-.2)
1. Vaesoyusn" vancbno-inaledovatel'skly geolOgicbenkiy InetWitt
Leningrad, Predstavlano akadaudkom H.S. shatailm,
(Tien Shan--rhultt (Geology))

AGEYEVA, L.S., w1adshiy tiauchnyy sotrudnik; SINrM11(IKGV,, Ira.D.; ZURMYVA, R.A.
Testing virus vaccines agains~t Nswcastle'.4!aaaso'an poultry faris
with a year-round system of dhicken raising'. Veterinariia'
no.9t42-45 S 162.
16010)
1. Gosudarstvennyy nauchno-kontrollnyy Institut vleterinarny~h
preparatov (for Ageyeva). 2. Glavnyy.vater'inarl vrach Uprivlea~jva
ptitsefabrik Moskovskogo oblastnogo soveta taroOogo khozyay~tva'
(for Sinallnikov). 3, Glavnyy vaterinarniy-lyrach p'titsefab~iki
Moskovskogo oblastnogo sovnt6 narodnogo kho'~IyaystlvaI(for Wbtsova).

ZUBTSOVt To. I.; ZUBTSOVA, To. I. MIXUMM)-KAmrl k D.
Naw ffids of mrine Pormian deposits In T1 emll Shall', Dlokl, ANJSSR,~
116 no,4:,681-683 0 157. (HIU 1193)
1. Vaeanyusnyy nauchno-I.Raledavat4l'okly g6hogichaskly inat'i.tutA
Ienirgrankly goftdarlobve=Y7,universitat Iij. A.Ai. thdanova.' Prod-
istavlenu akademikom D.V. lallvkinym.
(Tien Shan-PhlaontolOA7)

AUTHORS: Zubtsov, Ye. I.t Zubtsova) Yet I.
1
D~.,~~
Miklukho-Maklay,-W7
TITLEt ~ta ih the Tien-Shan'
New Discoverieo of Marine Permian Depos
,
(Novyye nakhodki morskikh peraskikh otl*zheniy v Tyan'-Shan,e)
PERIODICALi Doklady All MR, 1957) Vol- 116, lir 4, pp. 66i_'683 (USSO
IBSTRACTs It is customary to consider the norther#i tuartin of the Yergana
and Tarim depression as the northern boandarj of the makine' Perv
mian deposits in Central Asia. There in Ian dasumption 6ccording
to which the coast line of the Permian 4ea took its course some-

J -Tau mountains', -
what northwards in the east of the line~Bogbu
south eastern slope of the Chatkal chain. Since this asdumption
was up to now not confirmedj the discovorj of
uarine lover Per-
,
mian deposits in the north west of the1l,erganap i. e. in the dis-
trict of the Naryn depression by the two firot authors in 1956
is interesting. The finds are of two alfternet places (their dis-
tance is 6o km)z &I in the eaatern part of the Baybiche-Tau chain
(Ulan river valley and b) on the soathern slope of the Uarjn-
Tau chain. At the Ulan river the exyosar~aa have a breadth of 8oom
and 3 km. They are covered by unconform red-colored tertiar;r de-
posits in the north and border in the souAh along the fracture to
Card 1/3 a thick chalk mass of lower carboniferout3. Th~:: real character of

New Discoveries of Marine Permian Deposits in the Ti6n-Shan- 2o-4-42/51
the Perinian-carboniferous-relatioli is,rtot quiLe clear,here'. The
cross section is described in detail arid the nanes of~.t'he fossils
of single horizons are given. The total thickness of the lower
Permian amounts here to 470 M, In the lfaryn chain a t4iQk com-
plex of terrigenoue deposits of the upp'er palaeocoicum1s devel-
oped. Final conclusions. According to the quantity and the :syate-
matic composition of the foraminifera the Permian exposures', of
the Baybiche-Tau chain are much richer, :~hari Olose of 010~ 06',ue age
of Naryn-Tau. The differences are apparontly~aonnected *fith~ the
facial peculiarities of the aitea. The.Acnowledge given in the pa-
per concerning the systematic amount of~~Ithe fuaulinidea~izi the
Baybiche-Tau exposure shown that the two ftiatin zones (the l6wer
with a garasch-wagering.iquantityl the uplier with a lot of R&rafa-
sulines) on the whole correspond to the,central Karachaiyr hori-
zon of Perganaa( according to the strati6raphic scheme~by Miklu-
kho-Maklay). Any original species which do not occur in~the'early
Permian of the Fergana depression lack here. The occurrence:of a
rather great quantity of forms is striking; they are siLlilar to
those of the upper part of Tayyuan' serOs of.1forth China and to
those of the Chuan'-Shanl series of Souii'i Chitia. Ver.1 intere~sting
is the discovery of 3 species which are ilescribed from the Car-
Card. 2/3

New Discoveries of Marine Permian Deposits in the Tien-Shan. 20-442/~i
nic Alps (A. Shellvin), here in great number of individual6.
There are onlj few species which could ~O found in the 6chwage-
rine layers of the Russian Plateau and in the near-Ural~region.
From the occurrence of the same species~~,in the Carnic Alps,'Fer-
igana, and China it can be concluded to especially favorable~mi-
gration conditions of the fauna in the latitudinal extettion.
There are 3 Slavic references.
ASSOCIATIONs AU-VaLm Scientific Geological Reaearch In3titute, State Uni-
versity imeni A. A. Zhdanov in Leningrad (Vse13OjUZUy nauchno-
issledovatel Iskiy geoLlogicheskiy institut,~Leningradskiy gosudarst-
vennyy universitet iia. A. A. 1,hdanova)
PRESENTEDs May 11, 1957, by D. V. Nalivkin, Academician.;
SUBMITTEDs May 8, 1957
AVAILABLE: Library of Congress
Card 3/3

SOYA, Te.I,
Pro-CarboniferoUd deposits of the TAkhtalrk ~idgej Kok-Irin-Tiu.
and the northern edge of the YAwyn Valley in~~ the Tion Shan. tuformo
sbor.VSEOZI no.3:3-9 136. (MLRA 16:1)~
(Tien Shan-Geoloff, Stratitraphic)

UGIA)Y. F.G.. professor (Leningrad, Kirovskly pro, d#2,, kv,4 26); MTSOMM
V.I.; PUTUTOTA, N.G.
KpPhode for the early diagnosis of lung cancerl[with summary in"
Ifiglioh, p#151-152) Yest.khir. ?7 no.12:27-34 3) 1561 (NLRA 10,02);
1, Is gospitallnoy khtrurgichaskor kliniki (za*. - prof* Y.G.Uclov)~
1*-go Leningradskogo neditsinskogo institute in'o~ akai4 I.P.P'vivlovas
(IIJNG NZOPIASMS, diag,
early diag.)

ZUBTSOVSKIYI V. N., Cand of Med Sel (diss) "Dlmgnosla of cancer o f the
lungs by cytological inveatifgations." Lf.-:ranr-rad~ 1957 2.,'-,
pp
(Kir!t Leningrad Medical Institute Im 1. P. Pavl~-~Vo C1111 I rof 110'spitill
Surgery), 200 c-)pies (KL, 37-57, 104)
C2
wr Him!
i tF minn ~~HY7 I'I

(Leningrad, P-P22. a. Wya Tolat4go,
Diagnosis of lung cancer 'br cytologic examUlaillon [with summary in
English. p.1603. Teat.khir. ?8 no.$;93-103 Ply. '57,' OLRA 101-7)
is Is gospitallnoy Wrurgicheakor kliuiki (sav. prof. Y-G1:MClo#)
1-go, Laningradskogo wditsiuskogo instituts im". akmd.~
MID NW-1-ASKS, ding.
cytodiog.)

ZGTSOVSKIY, V.N.
in-lung cancer, Veot, khir. zi~d 6s2,3-35
165. (KUM 18 112)
I*. Iz-gospitallnoy-.khir=-gicbeikey Irlihiki 0; ohlen-
4".
1my,rasmt%rAfmt AMU SMit ~.i nrnf _~ V~111_ Iffflowl I-DIft T.0114 n-

POOMNOV, N.I.; ZUBTSOVSKIT, Y.N.; TORKOVICH, I.L.
Some Aspects of methodia used In ge6logical piompecitag for coal
in the buried easternsection of the greater bonatelmain. Ra~v6d.
I okh.nedr 22'no.12:23-26 D 156. W~A 10:2)~
1, Rostovskaya geologichaskays ekspeditolyat
Musts Basin-Coal geology) (Prospectin

Unc% F.G.p prof.;_LUBTSC~ ,,,V,.N,.j_KARTAVCVA, V.A'oj TSAUD-,1F,, L.O.J
NIKITWA~ N.I.
Late results of palliative surgery In tetralogy 0t Fallot.
111A 18-7)
Kardiologiia 5 no.2:35-1,0 Mr-Ap 165.
1. GospItalinaya khirurgiohe3kaya klinika (PAr. jwpf, F,G.
Uglov) I Leningradskogo meditsinskogo inatWita lmi,ml t.P.
Pavlova.

PHASE I TREASURE ISLAND BIBLIOGRAPHICAL REPORT AID,507:- I
BOOK Call No.'* ~: QC1942.Z8
Author: -ZIWAN, ZH. D.
Full Title: OR!-OI-U--]M DEVELOPMENT OF CYCLONES AND ANTICYCLONES
Transliterated Title: Vozniknoveniye i razvitiye tsiklonov i
antitsiklonov
PUBLISHING DATA
Originating Agency: None
Publishing House: Hydrometeorological Publishingillouse (Gidrome'teo;-
Izdat)
Date: 1949 No. PP.: 52 No.,of copies: 50001
Editorial Staff: None
TEXT DATA
Coverage: This monograph belongs to the,"Synoptid.Met~eorologistls
Library" series. It is written in a popular form to summarii6Irecent
Soviet achievements in the study of cyclones and~anticyclones., Ac'-
cording to the author., modern Soviet methods have left far behind
western progress in meteorology. The booklet d6als With the fundb-
mentals of the advection and dynamic theory of the development of
cyclones and anticyclones. This theory was worked out by
Kh. P. Pogosyan and N. L. Tabarovskly, and is bined on I. A. Xibel's
hydrodynamic theory of local changes in atmospheric pressure., The
author maintains that this is an original Soviet theory unknown to
2/3

V6zniknoveniye I razvitiye tsiklonov I antitsiklonov AID 507 1
foreign scientists. Fundamentals of this theor~'are given in them
following works:
Taborovskiy, N. L., Hydrodynamic Theory.'or the~,Baroclinic Atmosphire
and Basic Problems of Synoptic Meteorology,, 1947.
Pogosyan, Kh. P., Seosonal Fluctuations or the4enerll Circulation
of the Atmosphere, 1947.
Pogosyan, Kh. P.:and Tabarovski N L Advection and Dynamic~Bases
of Frontological Analysis, 1946.
T~i6 monograph is provided with many charts.
Table of Contents Vages
I Introduction
HiA~Ory:;'-;Origin and development of baric form~tiohs;- Klbel0d,
formulas and qualitative deductions concerniq, preseure
changes.
II General Analysis of Pressure Changes 11-31
Geostrophic wind; Non-stationary movement; Local changes in.
pressure and temperature; Advection and dynamic changes In
pressure and temperature; Changes in the absolute altittide
of the 700 mb isobaric surface; Charts of isallohytsed of
the relative 500/1000 mb. topo raphy,, and their us6 in
2

Vozniknoveniye i razvitiye taiklonov i antitsiklonov AID~50-( I
j
practice. How to forecast dynamic pressure changes from
the structure and charts of the thermobaric field;
Problems of frontogenesis and frontolysis and dynantic
pressure changes; Interrelation between dynayhic changes
in pressure and advection changes in temperature..
IIII Origin and Development of Cyclones and Anticyolones 31-52
.'Cydlogenesls'li-and "anticyclogenesis". Evolution of cyclones
and anticyclones and structure of the thermobaric,field;
Some specifications for forecasting; Critical value of
temperature contrast; Changing of altitude d4tormation
fields and processes of oyclo- and anticyclogeneals;
Movement of cyclones and anticyclones.
Purpose: This monograph is intended to improve the qualifications of
weather forecasters in their routine work.
Facilities: None
No. of Russian and Slavic References: 7 (1940-1948)
Available: A.I.D., Library of Congress.
3/3

ZMANt 0. D.j CAND PHYS-WT
USSR/14eteoroloa - Frontal Zones
ii.JUL
"Planetary Altitudinal Frontal Zone," G. D iZubyarij:
Cand Phys-Math Sci
'Neteorol i Gidrol" NO'7., PP:10-16
States that analysis~ of synoptic maps or ~i4a and!
bArle tnmography shows that in the nortberl~'6ml~-
aphere Vie asic devel6iment of att pvoaas6i~s- depinaw'
not on one frontal zone as assumed by V. A~ I~Ugayev
ana V. A. Dzhordzhio (cf. 'trudy TsIPII NO'95 OP-L
bound and,,~inter
1951), but on at least 2 clasely~
acting planetary altitudinal frontal zones~41~
23

ZUBIAN.,, G?vorg Davidovich; POGWTAIT,lh.P., redaktor; BRATNINA,14.1.,
t
(Synoptic and aerological studies of atmospheric frontal
Sinoptiko-aerologicheskoe iseledovanis atuomfenfth froutov.
Leningrad, Gidrometeorologichaskoe isd-yo, 1955. 120 po
(Hateoroloa) OWA 9:2)

Name:
Dissertation: Synoptic Aerologiog I 10tudy of Atmo-
spheric Fronts
Degree: Doe Geog Sci
Affiliation: Zn-ot indicatog
Defense Datep Place: 15 mar 55, Council of thu Central,
Inst of Prcgnosis'
Certifiention Datat 28 Apr 56
Source: 3MV0 4/57

KRICHAK, Oskar Grigorlyevich; ZMYAIT. G.D..* otv9tstv*mW rodaktor;
TASNOGORODSXAYA, M-X., H.14'', taktzicbesildy
redaktor
[Synoptic meteorology] Sinopticheekals mateoroloCiiao laningrad
Gidrometeorologichookoe iud-vo, 1956. 530 P. (ma loll)
(Meteorology)

A~"TAVRI4Wb?KK' , P.D., kazid.geograticheakikh nauk; BURTSBY A. Lit'kand.fisiko-j
matematicheokikh nauk; MOV, Top., kovd,fiziko-Mattewticheskikh i
nauk; ZVMV, A.S., kand.fiziko-matematichookikhnnuk;-ZMULAP,.P~e
doktor geogrefichoskikh nauk; HIIIIIIA, LPS., knad,gnografickepleikh iaauk;
MOROMIN, A.A., Inshener-meteorolog; RUPPART i! L.L.'. kand.geogrifiche-
Okikh nauk; BIRGHYMV. B.H., Inthener-mateor6log; SANDYLOY, A.I., ;
kand of iziko-me tome tichaskikh nauk; TURKMIpI.L.j~,bnd*geogftfichPj-
akikh nauk; CHERNOVA, T.F., starshty nauchnyy motrudnik; CHISTYAKO*.
A.D., kand.fisiko-matematiche6kikh nauk; POGOBYAN, 1b.?., profe,red.;
YASNOUORODSKAYA, X.M., rea.; BUYNINA, H.P., tskhn~riodx
[Synoptic study atlas] Uchabnvi sinoptiobeekli atlas, Loningrhd.
Gidrometeor. izd-vo. Ft.2. (Soot, PsD.Astapoinko I'drj 1957.'
90 fold. maps (in portfolio)._ _ _ (Practio6l recammendation4
and aasignments for students using the Osynopitc Owly atlas* L
Metodicheskie rkomendatoii t sadantis dlia attAentov k "Uchabnomu
sinoptichookoma atlasu,s chest' 2. Soot. A-S~"Zveravp 1957 8 Pe:
1. Mentrallnyy institut prognozov (for Ghernava)
(Climatology--Charts, diagrams, StO.Y

3(7)
AUTHOR: Zubyan, G. D. S07/50-59-1 -1/00 i
TITLE: The Intarlatudinar ftchango of Warm ana. Cold Air 11asnoo in!; the
Stratosphere In Winter (0 mezhshirotn6ni obmcind teplykh'4 kholo-
dnykh MA88 vozdukha v atratoefera 2imo.0
PERIODICALt Meteorologiya i gidrologiya, 1959i lir, I j pp~!3!02 (USSO
ABSTRACT: This is an evaluation of results of 9~ri~opti~al investi~,ations
f
made at the and of January - beg nninjr,io F6b~uary 195$ on.the
station Sevornyy PolY1113-T(SP-7) whilo"At dtitted at ii~out:
~
ngit Iild(t. For cb~parisont
850 nor-th latitude and 156-1530 west'la
the measurements of Station Saratov 01,0 34'. north latitude',
460 031 Vtat longitude) are added, Thb'~tempwrtituro di6iribution
characteristic of au=er with gradient.b'dir" Lated from~the pole
to the equator is disturbed during the'polat night. I~nlthei~
stratosphero, a warm belt -with reIntivoly high temperaturep
forma which comprises the whole hemis0hare.iLargo graalento
directled towards the pole'are built UP,[north of this belt.:
They cause a strengthening of west wiWis at!am increaB~ in:
height, and a stratospheric Jet streAm~on the margin of the
polar night. - A disturbance of thin winterly normal condition
Card 1/3 occurred in the period of time observe(L. The following was'

The Interlatudinar Exchange of Warm and,Cold Air SOV/5P-59-1-1/?O
Masses in the Stratosphere in Winter
found: 1. An extraordinary increase in, tempOrature in the
central arctic due to advection of wnlrj~ Pir~ftom temp6tatu're
zones. 2. A great decrease in temperatiire iii the temperate,
latitudes due to a spreading of cold air from the arctic b,asin
towards the south. 3. An inversion of~the vertical at-roti-,
fication of temperature over the central arctic ani the
temperate latitudes in contrast to the,one characteristic of
winter. 4. A considerable shift of the~'wnrm belt in the
Pacific and North-American section to the north, and 4~shift
of the arctic "cold cap" to the south-~owards Europe i;~i Voist
Siberia. 5. A concentration of large h6rizontal tempe~~tur'p
gradients over the pole, and an appros~ailh of~the stra,O~pheho
jet stream to the pole. 6i A splitti 9'0f the polar c~olon6,
the formation of a zone o~ increasTpiessure over th6icent.ral
arctic, and thus an essential chugo tit alronlating obiditions.
A general regularity for this process aouldInot be ascertained.
,between
Also ofher variants appear well possible. A connection;
atmospheric processes in the middle a 'ttatosphore an4 those'in
other layers can be explained for every- concrete case'o*nly:by
Card 2/3 means of a synoptic analysis of the totiperature fields$

The Interlatudinar Exchange of Warm and Cold Air SOY150-59-1-00
Masses in the Stratosphere in Winter
the geopotential and the Rir currenta it diffetrent hekkst$,~
The disturbance observed Is caused by the specific wln~eriy
radiation conditions. There nre 5 figures and 10 referonoeb,
5 of which are Soviet.
Card 3/3
J I

ZUBYAN, G.D.
Aerological study of the penetration of cold aii~ nasses imto
Armenia. Dokle All Arm. SSR 40 no.3:183-188' 1654;
18: 12)
1. Inatitut geologicheskikh nauk All Arr4SR. SubmItted August
Up 1964-

I-L 021~8-62 I,',JT(1) GW
NKs AV7002325 OR/02'' /66/042/0'
SOURCE CODE: 52 0.3/0i~9)lO`65'
I
AWHOR: Zuby
,in. G. 1)
ORG : 1Lqqtitutc, q - Geological Sci nc s,. Arm!;SR (Institut p N' ArrASSH)
. . . r - - . - - . __ - - ~ P~ _ P'. . . ijologi6heskikh n4qk Aj~
TIT18:. Burgos of con3iderable a -tratospheric templerative fluctuatior.3 ovcr~Armet4a
SOURCE: AN ArinS!3511. Dolclady, v. 0 noi.-Y,'-i~66, 159-165
ITOPIC TAGS: troposphere, atmospheric temperature
ABSTMICT: The paper cited below gives some results of inv6atij,~itilon of th~ istr&to-
sphere over Armenia on the basis of daily acroloGical observations at Ycro~j
van in 1961. Aperiodic temperature changes in Armenia ocletir not. only in t1i 10
troposphere and lowcr atratospheral-but alao in the highcr1aycra of the lot,*
.ter, possibly ~o its upper boundary. Viese variations arc~abaervddfor thq~
most part in the warm season of the year an& in the middle Intratosphere fro-`
.quantly attain 10-150 in 1-2 days. The most important cautIntive factor ap--;
parently is vertical air movements induced by the stratospIkeric nubtropical~'i
:frontal zone. Ilia article gives an extremely well-expresai.1d case of this
:stratospheric temperature change in tho occdnd half of Augu'at 1961. At thdl I
same time, the temperature fluctuatione in the tropospber6Jwcrc up to 10-14P
but the temperature changes in the stratosphere and troposphoro vere oppo-. i
a i to in sign. . Thin 'cane. was associated with penetration 6f a coW air wool,
but not all such stratoophoric temporature changes are cautiod 'bY4uch event6o'
iThe key factor in vartical',air.movements, which arc discusilad in general,
and in application to the particular case considered. Thi6 artidle was presented
by Academician AN ArmSSR S. S. M(rtchyan on 18 October 196~, Orig. art. has:
3 figures, 1 formula and 1 table. 1JPRS; 370971
SUB CODE: 04 SUBM DATE: none ORIG REF1 005
Card 1A nat

ASTAPENKO, P.D.; BELISKAYA, N.N.; BUSIMi V. I. I- BUS119t)l O.A.~ GUROV V
ZIMYAN- r.-D-;-KATS, A.L.; MININA) LOS.; MDROZXyp A.A.; PAVLOVSt,AYA
A.A.; POGOSYANO Kh.P.; SAMOYLOV,:A.-I.,~ S91EINOV" P. I. T RAKANOV,i
G.G.; TURKETTIO Z,L.; CHERNOVA,, V.F.j,GH1STYAW10 A,,)i~
(Symptic atlas for'schools]Uchebnyi sinaptichdiskii ~tlfts. Pods
red. Kh.P.Pogosiana. 3, perer. i dopa, izd, Lenilngrcj
J (M,,GIdromete4-
izdat, 1962. 217 gold.col.maps. RA 16:3):
[Assignments for atuaents)Za&miia dlin uch4shchikhain. Pod!;'
red.Kh.P.Pogosiana, 138 p [Methodological:linstr~ctions and~~
recommendations for teacheral-Reiodicheakie uka~:aniia!i-rekomen-'
dataii dlia prepodavatelel. Pod red. Kh.P.Pogoiliana.:'73 P.
(Meteorology-Charts diagrams, etc.)

POGOSTAN, Khoren Petrovich. Prinimali uchastiye: VGAROVA, K.F., mladably
nauchnyy sotrudnik; SWILISIXOTA, M.T.. mludWy nauchnyy
sotrudnik; PAW4TSUTA, A.A., *l&d:hiynauchn;'ry sotrudnik; FAVWTA
U.N., insh.; GMVLTMINA. A.C. tar hiy takhnikl HOSTAGINAO!
U.N., starshly takhnik; SXXNNOVA, A.V,l stavshiy takhnik. _20
G.D., oty.red.; BLINNIKOT, L.Yd# red.; 71MOYA, TA,, tekhn.r6d.
[Jet streams in the atmosphere] Strainye tacheniis v otmoafe".
Moskva, Gidrometeor.izd-vo (otd-nia). 1960. lB2 p~
(jet stream) (MIRA 13: 8)

BOGATOV, Anatoliy Danilovlchp katul, tekhzi. nauk; ZUBP:[N
Leonidovich; BASHCHENE0, II.T.p Ived, red,`
[Ore concentration in Plov launers) Obogashchan'le na
struinykh zhelobakh. Moskvap Nedra, 1965. 97 P.
(1111RA 18:4)

ZUBYNINA, A.V.
Classification and the clinical aspects of cicatricitil pyloric
stenosis. Sbor. nauch* truds Ivan& gose med. inst. no.25:86-91
162. (MIRA 17:5Y
1. Iz kafedry fakiLlItetskoy khirurgli (zav. - P~Iof. N. A. Blago-
veshchenskiy) Ivanovskogo gosudars-tvennogo medilainskogo inatituta
(rektor dotsent Ya.M. Romanov).

u y v V. 11 k, F C I f 2u E~
Nev data un mode, 4)f
wolf rp,!.-.J fxj. t~oM AN
"go)

*'!-:J'-~;,7 - - _- I= f
fill
2557Q746 W. (d)/WPLh)/
ACC Nk: AM6007923
h gakharov
Zubtitskiy,_ 04 Ivanavle u Oer VA
Iva 6vi6"
Transportatioltithin a port (Vautriportovy7 transport) Otdscow, lzd-vo "Ttavaiiort'.1j
1965. 165 p. Lllus. Errata slip insetted. MO copies grinC44-
TOPIC TAGS: marine engineering, railway ongineeritig, highway Paginceringo r&Uway
transportation, ship, port
PURPOSE AND COVERAGE: This book Is intended for studddto in opera-
tions, and hydraulic- engineering specialities in highmi.- edociLtional inotitiltiord
of the Hinistry of the Merchant Harine; it may also Ue used by port and planning-
organization personnel In the merchant marine. Problems relating to the deMign,
construction, and operation of rail lines In port aream, sit$ mhort-diotmuce ac-
cess rail lines connecting ports to trunk lines and toxhistri.p.t complestets are re-
viewed. The planning and construction of port facMeles, vorftng facilities,
sorting yards, motor transport access roads, and roads connectioR various port
areas are also discussed.
TABLE OF CONTENTS: [abridged]:
_7'
'Card 1/2
.... ........ ......
._LLi

7
7-
t rt
L* 25r'?0.66
ACC MR: A96007923
Ch. 1. the general character of intrapott transp6rtadioft
Cit. 11. Rail tranaportation
Ch. 111. Automotive transportation 91
Ch. IV. Port veosels -- 156
SUB CODE: 13/ SUBM DATE: I ';Ju 16 5
Card 2/2 60
7 '17

ZUB2HM
Agglutinant property of Shigella sounsi as t~lelatefl to the PhANG of
their growth in a liquid culture inodium. Tri* L$OKI 3 0:63-12T '36.
(MIRA,10:8)
1. Xnfedra mikrobiologLi Ieningradekogo sakiltarno~Siglyentobaskogo
moditsiaskogo instituta (gav. kafedroy - prof. H.S.fisher)
(SILIGAIJAs cultare,
o=el, agglut. properties in liquid medium & growth
;
actor (Run))

7- Y /Y 6'. N,
DIPHTHMIAI
"An attempt to Use Fluorescent Microscopy for the riagiwsis of
Diphtheria", by Yu.N. Zubzhitskiy, Laboratornoye De16,~!No 2,~ March-
April 1957, pp T5-~-38
The author adopted Keller's test (fluorochromiftg vith cotlyphoaphine;;
1939) and, as a result of his experiments, asserts that the,method by
fluorescent microscopy of the diphtheric bacteria rendibrs it possible
to accelerate and to obtain more accurate laboratory diagnodis, of diph-:
theria. This test is quite accessible for daily use 'i~ every bacterio-
logical laboratory.
Card 1/1 5

USSR/Microbiology GaneralMerpolology F-IJ
Abo Jour:
Author i
Inst
Title
Orig Pub:
Abstract:
Card 1/2
;Ref Zhur,-Siol,, No 18 1,190 IWO+
Zubzhit, skiy midi
.1'e
Fluorescence Microsc6py:11of Tuberq DO 111. and.
its-Evaluation,in Cofinectioftvit4, 0S~ibt e
P
Errors of!:thd Method and,Va iabi~~,ty"6 the
Vector.~
Labor. delo, 1957, No. 61 22-25 J
In the preparations of materials! tested with
fluorochromated acridin orange b:tl the:detailV
were dyed greenish-yellow and only tOborculosi~
mycobacteria (TM) fluoresced with a bright
.mord specific;
orange-red color; this method ii
than treatment by auramine. InliteSting 600
smears by the fluorescence method, 6% more

ZU.BZHITSKIT* Th.M.
Substitute for immersion oil In fluorescence Microscopy [with
summary in English). Mrobiologiia. 26 no.3086 ~V~-Je 157.
(NDU 10:10)
1. Uningradekly oanitarno-giglyanicbeskiy mediteinAir inatitlit
(MIGROSGopr,
fluorescence# substitution of Immersion oil with
anisol in microbiol. (Run))

I

ZUBZHITSKIY, Tu,ffs, MALTUKOVA. 1.T., MANIMMISHTAK. U.Te
in 0 13
viv tudy 0 the sensitivity of nerve d'sU protoplRam t6l
novocaine s Trudy LSGMI 45:172-183 '58 (MIRA li:xl)
Is lafedra obahchey biologil,Laningradakogo eanltarno-giglyenl-~
cheakogo maditsimakogo instituta (save. kaftidroy ahlaa--kori~Ieapdadent
AMN SSSRb prof. P.V. Kakarov)o'
(MMS)
(NOVOCAM)

UDINTSIV, G.R.; ANAVINA, Z.N.; ANDRVEVA, A,G.; BLOk V.Bip:'~GAVAN'
v 0
TAGOR'KOTA, A&S,; 'ZVBZHITSKITO Yu.1r.; IIIINAp N.D.-- KAMM, I.Tf;
ICAJM, LeMo; MIRDYZ'VSIaYi~o';':t:OT4010"0;-~nCHAYVAq te.A.:, PAR11OV, 18,S
Influenza in 1957 from data of the hospital thlarapoutic clinic, of
the Ieningrad Institute of Sanitation and Hyglens. Boy.wd. 23,
:no.loz67-70 0 159. 13:0
1. Iz goopitalluoy terapevt1chegkoy kliniki (214veduwanhehiV - chlen-
korrespondaut ART SUR prof. O.No Udintony) U;n1ngrikdukogo gwaltarU6-
glg4yenicheskogo meditsinskogo, instituta.
(TNYLUJMZA statistics)

Q~ZHMSKIY, Tu.W.; BARSKIT, I.Ta.
------------
Combined luminescent audphaae contrast m1cr6ucopT,6 Zab.dsla
6 no.3:42-43 W-ja t6o. (MIRA 13:1)
loni lmdakago
1, TAboratoriya Iyaminestsentaoy r1kroskopit U41.
sanitam-egiyenicheakogo maditainskogo LnAltuta~ V lAbora-
torlya ekotsitofisiologii Botanichookogo inailtutw1uni
T.Le Iromarova.
(PffASR MICROSCOPA)

ZUb'f-9,1L;:,KiY. Yjr-.y Nw-umovirb, TOEM, 1.1j., rod.
vl r.:)I,)i!Y a:xJ lmiuriol f7 Ile t od lludiliv t-LientAirl
akt)pA v mikrc,,.AtAfogF.li, virvsologil i immoAcg.1,11.
Leningrad, Vleditslna~ 19#':k4', 152 p. (MIRA a: ci

ZUBZHITSKIY, Yu.N.; YAKOVLEVA, G.S.
Detection of virus antigen in cells by the.indlrp~ct fluorescent
antibody method. Trudy LSGRI 66000-306 162. ~MIRA VtO
1. Kafedra mikrobiologii Laningradakogo sanitarm-gigiyonicheakago
maditsinskogo instituta, (zav. kaNdroy prof. M!.~.Fil:her).

,,ZUBZ ITSKIY, Yu.K.
H

ZUBZHITSKIY, Yu.11.
New possibilities to use fluorescent irtiornscopy. Tr,,;Liy T.SG14I
66t90-303 162.
Production of precipitin sera for the indirect fluore-ncent anti'Lody
m, thod. lbid.:104-109
Una of acce'Lerated methods fcr the parificatior, of tmiril~ from
fluorescein lsocyhnattj dcvtvativt~s. IbLd.ill.0~1,119
D( tection of enterapathogenic Zscherichia coll. ,by tim indiiree t
fluorescent antibody method. lbid.il,35-145
Use of fluorescent antibodies in~the study of'li-wt withods of
diagnosis in virus hepatUle (Botkin's diseaso):.. IbLd.007 317t
(YIRA 173d
1. Kaeedra mikrobiol.agii T-f-iningradskogo sani tAr:no-g 1~ I~e niche skog')
wditsinskogo instituta (zav. kaffedray - prof. MJIA.3~.,er).

ZIJBZHITSK
Studiss of the diatribution and fur-ation of he-143rologms Firotet4a
in the tissues of a nonimune arp-anism by thc~ iniothoc~ cf lumine;rdlent;
antibodies. Dokl. AN SSSR 155 ~no.jj234-237 H.- '64.
OCRA 17~4)
1. Ins"itivt eksperimentalinoy med.itsiny AMN 0,133MR. Rrcdstnv1fnO
akademikom NJI.Anichkovym.

ZUBZHITS
Effootive method for obtaining precipilat:W''g! sera vith a hi"' Ah tit'er
for work with luminescent antibodies. Iab.i del*;6 l6o.
1399)
1. Wedra mikrobiologii lieningradskogo semitarna-gigiyani0hoskog'o
meditsinskogo instituta.
(ANTICOV AND AITTIBODIW) (SIU61