SCIENTIFIC ABSTRACT AYZENMAN, B. E. - AYZENSHTAT, I. I.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R000102710015-4
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: June 6, 2000
• Sequence Number: 15
• Publication Date: December 31, 1967
• Content Type: SCIENCEAB

ATZMOUN, B.13.
Antibiotic substances of microbes as an indication of evolution
and adaptat
Mikrobiol.shur. 14 no.3:78-86 '52. (HLRA 6:11)
(Microorganisms ) (Adaptation (Biology))

ATZINXkN, B.TtL-
Uynergetic effect; of eyntomycin with other antibiotice and certain
compounds
upon the typhoid fever bacillus. Iflkrobiol.zhur. 14 no.4:36-45 '52.
(MLRA 6:11)
(Antibiotics) (Typhoid favor)

AYZgM4A.N, B.Yif,; SHUYGER, M.O.; ZIELNPUKIbi, S.I.;
M&NIRIK, T.P.
Classification of antimicrobic alibEtan.,es: remarks
on the article
by Kh.Kh.Planelles. Mikrobiol.zhxtr. 15 no.1:77-79
'53. (MLRA 7:3)
1. Z Institutu mikrobiologii Akademii nnuk URSR.
(Bactericides) (Planel'es, Kh.kh.)

Chemical Abst.
Vol. 48 No., 9
May 10, 1954
Biolop,ical Chemistry
Sbme cbmu-micterlatics of the metabolisf~ of the tyiiii-ol'd
bacillus. ". YA-., Alzennian. AUkrobiol. Vim, Akad.
Natti Ukr. R.S.R. 15, No.3, 17-2Nin Russlan,20XI953).-
rryptophan wa% neres-utry in ZI strains of typhoid bneillm,
liot requited 111 7. The requirtnivrit (Or tr~rptophnn Is
specific. but the Imcillus can synthesize It oin indole.
The straimq tot requiring it are nliparently capable of syn-
thesizing tile ludole ting. B. Gutoff

iL
ATZMTMF, B.T11.
]tffect of loycluWastin on Salmonella lyphosa in vitro
and on am-
perimental typhoid fever in whilte mioe. Mikrobiol.
sh., Kiev. 15
no.2:260-34 19!i3. (GIML 25:5)
1. Of the Institute of Microbiology of the Acaden7 of
Sciences
U=ainJaA SSR.,

-AYMENMAN. B.Ye.
OMMOMM" NFL
Certain eharact*ristiee of the pbleiology of
nutrition of the
typhoid bacillus. Second report: Formtion of thiamIne
and
biotin bir the typhoid bacillus. Kikroblol.zhur. 15
no.4:20-25
'53. (MLRA 7:2)
1. Z Institutu mikrobiologii Akaeismii nauk
Ukrainallcoi RSR.
(Nberthella typhosus) (Vitamins)

AY~~!NM-WIV Berta Yefiroimn
(Inrtt of Illicrobiolo,gy of V-c J!,Iin.Istr:i of Yealth
UBSP.) - Acade. ic elegree
-f Ioctor of Piolof-imil Sci-nnc-7~s, ba tel -Ti I -r
def-mse, 13 ',-~a--r 1955, in
the Council of the Fiev Veterinary Dist, of ler
Oisse-tt!tion entitled:
"Scns~ tivit f Vie TThoidi Fever NAllus to Aiit'.biotloe in
Connect'on
L y o
~.,ith C~!rtnin Characte~istlcs of It's ~`(ItF!bolisr.
Acw`,~!--'c derro,~ an(]/(-)r title: Doctor of Sclri;ices
SO: D,?cisi.ons of VAY3, List no. 27, 24 rec 55,
Bpill-etenl '-70 SSSR,
Uncl. JPRS/NY 548

AYZBNKRH, B.Yu.
Second conference on the problem of phrtonicideB.
Mikrobiol.zhtLr.
18 no.4:65-69 156. (WIRA 10:2)
(IIHYTONCIDBS)

AUMEAN, B.Yu.
Study of the eubject "Antiblotlai frots higher vlants"
nt the
Institute of Mllicrobloloa of the Acadomy of Sciences
of the
Ukrninifin S.S.R. Vienyk AE URSR 28 n-3.1o:61-64 0 '57.
(MIRA 10:12)
(An-bibiotics)

SOV/20-121-5 -4 5/50
ALUNORSt Boldyrev, B. G., Drobot1ko, 1'. G., Ayzenman, B. Ye.,
Z-3lepukha, S. 1.
TITLE: On the Antimicrobic Activity of Alkyl Esters of
Thiosulfuric
Acids (0 protivomikrobnoy aktivnosti alkilefirov tio-
sullfokislot)
PERIODICAL3 Doklady Akademii nauk SSSR, 1958, Vol. 121, Nr 5,
pp. 924-927
f~'USSR)
ABSTRACT: The above mentioned prapert:11es of the eaters (1)
of the thio-
salfuric acids were only recently properly investigated for the
first time. According to the authors the synthesis of these
esters and the study oT their bactericidal properties is prom-
ising (Refs 1, 2). Thi:3 is supposed to be the way to develop
new active medicaments. First of all, alkyl esters (V) of
alkane-thiosulfuric acids which correspond best to the natural
antibioticum "Allizyl" werv synthesized by the first author
(Ref 3). The antimicrobic ixtivity was studied on Sta2hylo-
coc-cus aureus, B. coli, Myoobacterium Bq, and on various spe-
cies of fungi, also on w~Z_tar Infusoria,"on the dysentery bac-
Card terium, on blight spores, and on others. The activity of
the

13OV/2CI-121-5-45/50
On the J.ntimicrohlc Activity of Alkyl Esters of Thiosalfuric
Acids
Academy of Sciences, Ukrainis.n SSR)
PRESEIITJ:',D.- March 20, 1956, by V. N. Shaposhnikov, Member,
AcadeiV of
S,ziences, USSR
S UBMITT.',D s March 20, 1958
I Card 3/3

ZATULOVSKIY, B.G. [Zatulovalkyl, B.H.J.
kand.biolog.nmik; ArL3NKU,
B.I., doktor biolog.nauk, glEkvnyy red.
(Antibiotics] Antyblotyky- Kyiv, 1959. 43 p.
(Tovarystvo d1la
poah7rannia. litychnykh i naukovykh snan' Ukrainalkoi
RSR.
Sere5, no~3.350 (min 12:12)
(AWTIBIOTICS)

6OV/21-59-3-21/27
"L
1.UTHORS: Ayzenman, B,YU., Mandrik, T,P. and Shvayger, M.O.
TITLE; A Quick Method of Primary !3election of Inhibitors
of Ascitic Cells of Ehrlich's Adenoca--cinoma (By-
st:ryy metod pervichnogo ot')ora ingibitorov astsit-
ny:,ch kletok Adenokartninom:r Fh:-lichla.)
PERIODI"dAL: Dopovidi. Akademii naul: Ukrains:koi RSR,
1959, Nr 3,
pp 317-321 (USSR)
ABSTRACT: The authors recommend',AsirgtvoIiiethods Of
microscopic
examinations for finding aead and damaged cells,
for the primary selection of preparations for
ascertaining ant1blastomous ac,".-ivity with respect
to the ascitic cells of Ehrlich's adenocarcinoma.
Both methods are simple and can ascertain antiblast-
omous activity within 5-30 minutet3. Both methods
are recommended for testing other c~:].la of animal
and human tumors, where the nature of -the growth
permits it.- The firs'; method is worked out by
Drobot'Ico /Ref .57, by way of borrowing the ideas
of Japanese sc '~`ntists Mijamura. ~R_ef 2-7 and
Card 1/3 i

so-v/101 -59-34-21/27
A Quick Method cf PrimaU 6election of inhatitors o,.F
Ascitic
Cells of Ehrlieb's Adenocarcinome,
Yarr.azaki ZR-ef
_37. The ,4eccnd metl oa. hu-- been worked
out by the authors. IL consisti of the foll3wing:
OnE. drop of 0.1% water solul-io:i of Congc-red is put
on the glass plate and it drcp of the ascitic aiquid
to be examined in admixed The plate is
covered by anot.her i_,,-laqs Plate. AfTer 1-5 hours
the plate (still d[Imp ') is tiulijectt~d I-o a
microscopic
examinaticn. The live. cel- ~, :,hov, no .:olor. The
dead and semi.-dead (injured) ce-"-,-: appea-r 14n ruqset
-:or of various intens,_ti~~-.. The ul,)-,e the oell is
c
o.,
damage.,zi, the brighter is the col.cr. Of four varie-
ties of Congc-red, +he bep-, Yo8ul't,; were obtained
with the vse of Congo-red applied in the fluorescein
microscopy. There are 7 rs?ferences, of which are
Ja-oanese and 5 Soviet.
Card 2/?',

SOV./2*L - 5 9 -.3 -21127
A Quick Method of Primary Selec-tion of Inhibitors of
Ascitic
Cells of Ehrlich?s Adenocarcinoma
AS50CIATION: Ineititut mikrobiologii AN CkrSSR (Institute
of
Microbiology of the AS UkrL~-.~SR)
PREbENTKD: November 22, 1958, by V-G~ Drobot'ko, Member of
the
AS UkrSSR
Card 3/3

RABINOVICII, A.3. [Itabinovych, A.S.]; AYZMMII,
13-Ye. [Aizenmn, Bau.];
zRT muh, S. 1.
Iaolat!ion and inveatiption of antibactorial
proparationa from
wild homp (Cannabia ruderalis) growing in the
Ukraine. Hikro-
biolahur. 21 no.2:4o-48 '59. (MIRA 12:9)
1. Z Institutu mikrobiologii AN UFM
(PLAIUS) (AHrIBIOTICS)

I Ma
AY'MIMN, 13-Ye. Wzenruin, B.IU.1; WOMIUK, T.P. L ndr.-,rk,
T.P.1; SIMAYGER, M.O.
[Shvai'Ier, 14.0.1
Stiuliea on methods for the determination of antitumor
properties
of antLbiotics and synthetic preparations. Report No.l: Rapid
Tinthod for the primary selection of Ehrlich aecites carcinoma
call inaiibitors in vitro. Hikrobiol.zhur. 21 no.2:49-56 '59.
(141RIL 12: 9)
1. Z Institutu mikro'biologii AN USSR.
("fIBIOTICS - pharmacology)
(ANTINHOPIASTIC ACHUTS - pharmacology)

DERBEETSEVA, N.A.; RABINOVICH, A.S. [Rabinov;-ch, A.S.];
ArgzNw. zae,
CAYEenman, B.IU#]; ZFJJIPUKHA. SJ.; ILUMIK, T.P.
~?.&ndryk, T.P.J,-
SHVATGHR, X.O. [Shvalher, K.O,]
Antimicrobial substancee of Hyper'icuai perforatum.
IRikrobiol.zhur.
21 no.5-.52-57 159. (MIRA 13:2)
1. Is Inetituta mikrobiologii AN USM..
(AIVISMICS pharmcol. )
(PLANTS MIGINAL pharmacol. )

AYZBNIIAxs BeYet, [Ayzenman, B.rU.]; MANDRIK, r.P.
[Mandryk, T.P.1;
. . SHVAYGIM, M.O. [Shvalher, M.O.j-, KIFRIANOVA, Ye.A.
(Kiprianova. O*A.]
aapia method for in vitro detection :)f injured and dead
cells of
Ehrlichlo adenocarcinoma during primiry selection of
antiueoplastic
aubstances. MI-krobiol.zhur. 21 no.5;66 '59. (MIRA 13:2)
(NMPUSMS exper.)
(ANTINEOPLASTIC AGNO'S pbtrmacol.)

AMMU.N.. B.Ye.1 MLNDRIK, T.P.;..SHVAYGER, M~Ojj;
KIPRIANOVA) Ye.A.
Rapid nathod for theln, vitro detectlon of inju: d and
46d oel3j
of L"nr3ichls aarcinuma. Autibiotiki 5 no.3397-4,;
MY-Je 960s-
WRL 14#6)
1, Institut mikrobiologii AN USSR.
(CANCO (STAIRS AND STAINING (?g(4tOjlCCFY))

ZELF
RABINOVICH, A.!;.; AYU
E~. TUEHA S. 1.
Antimicrobial substances In Ukrainiaa hemp. Antibiotiki 6 no.1;
74-76 &"a 161. (MIRA 14:5)
1. Institut =Lkrobiologii Akademii nauk USSR.
(HEM?) (BACTMA)

AYZIOMAR, B.Yq.; MAPDREK, T.Pa; SHVAYGER, F.O.;
KIPRIAIOV.A, Ye.A.
Sensitivity of Ehrlich cancer cells to dyes* Vopwonke 7
no.81133-90 161. (MIRA 15:1)
1. Inatitut inikrobiologii AN USSR (dir - akad. AN
UkrSSR
V.G. Drobotlko).
1:CANCER) (STAINS AND STAIREG (MICR3SOOPY)) (DYES)

AYMIFJX~ D.Ye. (Aizenraany B.IU.]
Variability of ricro-organismakunder the influence of
environmental
conditiona. Mik-robiolaburi Ukno.31:50-56 162. (MIRE'
151C)
MICIM-BIOIOCY)

HUMAN, B.Ye* [Aizenman, B.IU]
- L -11 __
Variability of microorganisms under tie influence ar
the condi-
tions of the medium. Mikroblol. 2,hur. 24. no.4244-50
162.
(MIRA 1615)
(BACTERIOLOGY-CULTURM AED CULIURP, MEDIA) (VARIATIOV
(BIOIDM))

[Aizenr-m., B.IUJ; MAMR1K. T.F,'[Mandryir, T.P.);
SWAYGIRs M.O. [Shvaiher, 14,0*1; BIM]II9MU,, A.11,
[Bredi3china..A.M.1;
BONDARENKO J, *43
Testing the antitumorigenic activity of extracts; h,om higher
plants in vitro. Mikrobiol. zhure 25 no-4346-52163.
(MIRA 16439)
1. Institut mik obiologii AN UkrSSR.
(MATERIL MEDIGAp V19GLTIBLE) (CYTOTOXIC DRTICS)

JUZEMAV. B!Ye; [Aizenman, B.IUJ, SINAYGM, 11.0.
(Shvaiher, M.O.J;
iWOMP T.P. [Mandryk,, T.P.1; BIUMMNA, A.11.
[6-edikhina) A.M.)
Testing the ",ntitumorigenic activity of alkaloids.
Mikrobiol,
zhur. 25 no,402-57163. (M:RA 16:9)
1. Institut mikrobiologii AN UkrSSR.
(ALKALOIDS) (CrTOTCD[IC DRUGS)

D4131OT".-:0, V.G., otv. red.; MZEM-Ydi, Mo.,
md.;MAJlDRTK,T. P. red.,
BEL ITMOVA, K. I ru U, S. 1. , red.
A.K.p red.: KULIKOVSMYA, M.D.p red.;
11-1AWSIEWSKAYA, IN.5.1
red.; FOCIdNOK, P.Ya., red.; SINAYGER, IM.0.0
red.-,
KUZNETSOVA, A.S., red.
[Fliytono ides In the national e~~ononyj
Fitontsidy v mnc.,nom
khoziaistve. Kiev. Naukova duinka 1964. 350 p.
(VIRA Vill)
1. Akadem.1~7a nauk UIL~lt, Kiev. lm~tytvt
ullkrobiologii -.1 vi-
rusologi.l. 2. Inottitut milkrobiologli .4%
Ukr-S.111H (for
Zolepukba, Pochinok: Nigrrash, Kulikovskt~ut).

AYZENIRN, B.Ye. [Aizenman B-IU-]; SHVAYGER, M.O.;
MANDPIK, T.P.;
BREDIMINA, A.N. [BrediYhina, A.M.); OR1SIIChIJK, L.F.
[Oryshchuk, L.F.j;
KOLESOVAP E.A. [Kolesova O.A.1; MISHMIKOVA, Ye.L.
[Mishenkova, G.L.];
GALKINA, T.A. (Halkina, T.O.]; ZA191AROVA, I.Ya.;
RASIIBA, Ye.Ya.
[Rashba, O.IA.1; IAUSHNIK, G.M. [lauijhnyk, H.M.];
PRFOBRAZHENSKAYA, N.Ye. (Preobrazhemilka, 11.111.1
Effect of substances of bacterial orAgin on Ehrlich's
carcinoma.
Mikrobiol. zhur. 27 no.6:61-67 165. (MRA 19:1)
1. Institut mikrobiologii i virusologii AN UkrSSR.

T- ~71UT -------
'-'Ipcl,ric Ciibhs,
Delivery of cil.blen Trovi. !~;wrC. 7", no.
MonLhlz , -I-, I Librrxy :T Con.-res--:, April T ~C I
- . 14LU :) ' L . ., ~ IF!i~D.

RODZEVICHY V.; ~
Group production practices Frof.-to,'Ch.obr. 22
nc).B.-')-30
Ag '6!~. (MIRA 18:32)
1. Intipektor Gortkovskogo, oblastnogo upravlanlya
prof e-sair-nal 'no-
tiWmichaskogo obramviinlyn (for Rulzovich). 01. Dimktor
Gorl-Atovskmvo sollskoflyo uch.111-01C.11"i
No.8 (for Ayzenshtadt .

-AYMMATAT, A.I.; LISIDIEVSKIY, S-M-; DUBAS, D.K.
Progrossive osteolysis. Ortop. trarn. protez. 24
no.7148-51
,11163 (MIRA 1712)
Iz RiLhskogo instituta travmatologiL i ortopediii (
dir. - dotsent
V.K.Kidnberw [Kalnberzop V.D i tranmtologiches~ogo
otdeleniya
(zav. - zasluzhennyy vrach Estonsko~7 SSR - B. Kh.
&,iline)
Talliziskoy respublilcanskoy bollnits-ir. Adres
a%toxvv-. Riga, u1.
Duntev, d.129 Institut travmatologiL i ortopedii.

AYZEN3HTATY A.I. (Riga)
Clinical significance of hiatal hernia. Klin.
ruid. 41 no.4:
18-2:5 Ap 163. (MIPI 17:2)
1. Is rentgenovskogo otdeleniya (2av. A.I.
Ayzenshtat)
3-y -)b"yedinennoy bollnitsy (glavmyy vrach A.A.
Durov)
Ministerstva zdravookhraneniya Iatviyskoy SSR.

AYZENMITEYN, A.] .
High-voltage dividers for vibratory and electronic
oscillographs.
Prib. i tekh. eksp. 9 no.ltl32-135 Ja-F 164. (KRA l7t4)

A)2Er43HTADT, A.Ya,
. ~~2-
Semisiraraex semigroups of andomorphisits, of
ordered sets. Dokl.
AN SSSR 142 noil-.5-11 Ja 162. (MIRA 14:12)
Id Prodstavleno akademikom A.I. Mailtsovym.
(Groupaj Theory of) (Aggregates)

VAGAtlEii, V.V.; (',I,IJSUNP L.M.; qZENSHTAT, A.Ya.
Evgenl.~ SergefivichiJapin, 1914-; or his "0th
birthd&y. Usp. mat.
nauk 2.0 iiu.l*.244-24,5 Ja-F 165. (MJRA 18:4)

MUMINCV, Fatikh Abdumalikovich; AYZENS11TAT E A.
kand. fis.-mat.
nauk, red.; EELF.NIKAIX-,- A.G.,
tekhi.red.
[Themal balance and meteorological characteristics
of a
potato field) Teplovoi balanm i meteorologicheskii
reshim
kartofellnogo polia. Leningrad, Gidrometeoizdnt,
1963. 149 P.
(MIRA 16:8)
(Uzbekistan-Potittoes)
(Uzbekistan-Meteorology, Agricultural)

ACCESSIM NR-. A24018345 8i,"03/00/016/000/000

AUMOR: Aponabtato Be A*

TITLE: Diurnal variation and co"arstive charsaterif Alas of the-
tarbalonso Cost_

ficient for c4irtaia region@ in Central Asia.

SOURCE:
Tash%tent. Brodneaziatakiy a,-i. gid"a*1W-oj!, lastitut. TrW j no

16(31), 1963. Voprooy* aktinometril, matoorelogil i agromtoor#14,gii
(pr"10104

of actinonotjqrl nateprology, and agricultural
n9to**i)logy)$ %-60

TOPIC TAGM jostoGrologys turbulence eseflislonAl
0twepberio t%AMlsna*j air

t*wp*r&tur*, toapsratw-e inversion

ABSTRACT:
A study van made of dl%~wnal variability of the turbulence
coefficient

for various geographic are" in Central Asia *(,-cupiqd by
samy deserts, o*aid*-

sort, uAirrilstod landa, irrigated fields and
muntain regions. In all the mn-

.tioned areas KI -turbulence
coifficient at 1 isater sibove surface) Vag high
the daytime said lover -at night. In the desert and 4somidenert Kl
is 0.25-0.40

sea during tkis day and near go" at night@ Near
Loidagrad duriAg'daytime in sun-

mar Ki. - 0. 2"-30 m2/sec. Becawn of
strong tranapiration by plants over irri-
!
s, uhich in wintalited throu&sut the days ?her*-
atod fi*lds an inversion develo

g
p
.
V2

Cwd

ACCESSION NR: AT400-4729 S/ft'12/63/007/000/0230/0240
AUTHOR; Aysonslitaft B. A.
TITLE: The heat balopice of Uis principal geomorphological areas of
Central Asia
SOURCE: Wee. nauchn. meteorologich. soveshch. Trudy*, v. 7. Fizika
prizemnogo
SIOYIL. Leningrad, 1963, 230-240
TOPIC TAGS: meteorology, micrometeorvlogy, microclimakilogy,
boundary layer., beat
baltuice, desert. heat balance, mountainow3 area heat balance, oasis
heat balance, valley
heat balance, bDundary layer dynamics, Central Asia geomorTihology
ADs,rRACT: The heat balance of an acUre surface appears an effective
method of
inveatigating the interaction between the surfaco and the
atmosphere. Research has
established a series of significant thermal and dynamic properties
of the lowest atmos-
pheric layer. 'During it period of 12 years the I)epartmenta of
Meteorology and Clima-
I tology of SANIGIMI organized special expeditions to study the:
heat balance in CQntral
Asia.. Areas Included In Uds study were isandy deserts, Kara--Kum,
Kizil-Kum, clay
deserts, irrigated territories located in oases, and mountainous
regions. Complete data
characterizing the nature of the best balance in the lowest
atmospheric layer were
obtained. These &ta elucidate the mochanism governing the formation
of a meteorological
Cwd 1/2

ACCESSION NR: AT4004729
regime. Research data of stationary stations wEa also utilized. The
totals of heat for
day wid night in calories per square centimeter mad the intensity of
the currents in
calorLes per square centimeter per minute are shown. For
measurements of the radiation
balance R, thermoelectric balance meters were used. The turIbulent
heat current P was
measured by a inethod of heat compensatics. I'm heat losses In
evaporation V were
calculated using; the equation for the heat balanco
R'- P + B + V
it is concluded ithat during war= semiannual periods the plains of
Central Asia serve as
a sigaificant saarce for heating the air a=l for sative
transformation of the air masses,
Orig. art. has: 1 figure and]. table.
ASSOCIATION: 8ANWKI
SUB14ITT Dt. 01) DATE ACQ; 271)eqa ENCL: 00
000
BUD CODE: ZA NO REF SIN: 018 OTHEP.
Cwd 2AI

ACCESSION NR: AT4004729 8/2922/63/007/000/0230/0240
AUTKOR- Ayzeiasl%U4, B. A.
TrMig: The hent balance of the principal 1pomorphological miss of
Central Asia
SOURCE: Was, nauchn. meteorologich. eoveshch. Trudy*,. v. 7. Fizika
prizemnoso
sloya, Leningrad, 1963, 230-240
TOPIC TAGS: meteorology, micrometeorWogy, microclimatology, boundary
layer beat
balance, desert heat balance, mountainous area heat balance, oasis
heat balance, 41ley
heat balance, boundary layer dynamics, Central Asia geomorphology
ABSTRACT: The heat balance of an active surface appears an effective
method of
invesUgating tho interaction between the surface and the atmosphore.
Research has
estaUlished a series of significant thermal and dynamic properties of
the lowest atmos-
pheril: layer. During a period of 12 years the Departments of
Meteorology and Clima-
tology of SANK'11M1 organized special expcditious to study the heat
balance in Cqntral
Asia. Areas Included In this study were sandy Ceserts, KaraACum,
KIZil-Kum, clay
deserts, irrigaled territories located in osa6s, and mountainous
regions. Complete data
characterizing the nature of the beat balance in 1;he lowest
atmospheric layer were
teorological
obtained. These data elucidati-) t1emechanism poverning the
formationofame
Cwd 1/2

ACCESSION NR: AT4004729
regime. Research data of stationary stations was also utilized. The
totals of beat for
day and night In calories per square centimeter sad the Intensity of
the currents in
calories per square centimeter per minute are shown. For
inessuremients of the radiatloa
balance R, thennoelectric balance meters ivere used. The turbulent
heat current P Vag
measured by a niethod of heat compensation. The beat losses in
evaporation V were
calculated using the equation for the heat bodance
R - P + B + V
It is ODneluded that during waim. semiannual periods the plains of
Central Ae~& serve as
a significant sou.rce for heating- the air and for antive
transformnUon of the air MaSses,
Orig. art. has; :I figure &W I table.
ASSOCIATION: IMMMI
SUMMED: 00, DATE ACQ: 27Dtc63 ENCL: 00
NOREFSOV: 019.
SUB C:ODE:. ZA OTHCR.. 000
CWd 3/;

AYZENSHTAT, B.A., kw.d. fiz.-ratem. wuuk
Climatic factors of landscape diffo.*-enves of
moitntain slopes
of earntern and westorn wq)osuro. Motoor. i g1drol.
no.11:22-2u
F 166. (MIRA 19: 1)
1. Srodneazint.9kiy iiaiic-lino-i.ssledov3Lt(,Ilskiy
gidrcmeteovologicheskiy
inotitut. Submitted October 25, 1965.

",YZFNSPTAJ)T, !~J%
1~xfwnisivf, introduction of advanced experience on
dust elimination
i
in tho refractory Industry. Ogneupory 30 no.9sl--3
165.
(MIRA 18:9)
1. Vansoyuznyy institut ognsuporov,

AMMMADT, V.S.; ARSENIM, A.A.
Bradics,tion of gray rate in sewer orjalse Gigs I
situ, , no~8:45-47
Ag 154. (MLRA 7:9)
1. Is eanitarno-epidemlolceicheskogo otryada I
Odevskogo gorodskogo
otdelerlya profilaktichaskoy desinfelitsit.
(RATS$
control in city canalisattim In Russia)
(SANrTATIO9.
canalization, control of rate in Russia)

As *-4 't,56T 'n OIT c T" 7(--.-,' T-01,
. . TT") 'M'11C.':1117 MiC,"ITS-11CF7 - )t
- SITTr-(YT Palsa-10~1 V UT SqUOI)ON JO UOTj'~'-IT%uop7:r
.:~ '(7 ',!(~iT. 0--lif
i

AYONS11TADT.D.S.; ARSXNIYICV.Ji.A.
line phoaphide for poisoning the Norway rat. Trudy
probl. i tom.
Gov- no-5-93-98 '55. (KLRA 8:12)
I. Sanitmmo-epidemiologiohaskiy o'.1del Odeaskogo
voyannogo okruga
CRnts-Exterminntion) (PesticV.se)

PIONMOVSKAYA. S.F.; SIHOHOYICH, Te.N.;
AYICNZHrAX,-D.S.
Posuibil.ities of contact between man and the
ectoparasitegi of
rodents., VopArsev.,obe i ekep.paritz. i med.zool.
9:50-64 155.
(RODENTS AS CARRIERS OF DISUSI) (KERA 10: 1)
(PARASITES-RODINTIA)

AYZENSITADT, D.S.., RUSSUKH, P.A., and PIO]MMVSKAYA, S.P.
"The Faunc, of Extoparasites of Mouselike Rodents and
Hnsectivorse of Thans-
carpathis", Problems of Regional, General, and
ExperimentalL Poraw-'tology and
Medical Zoology, Vol. 9, 1955.
Division of Parasitology and Medical Zoology, Inst.
Epidemlology and Microbiology
imeni N. F. Uscialeya, MI8 USSR
Sum- 1305

- - - --- - -- ---- - -- - 11-- - - -- - - V~-~kwm~ - -~Mm
AYZENSHTADT, D.Sw SIMONOVICH, Ye.N., t)nd PIOTMOVSKAYA, S.:.)
"The Conditions for the Man's Contact with the Ectoperesites of
Rodents",
Problens of Regional, General,, and Experimenial Parasitology and
Medical Zoology,
Vol, 9., 1955-
Mvision of Parasitology and Medical ~~oology, Inst. Epidemiology
and Microbiology
imeni N. F. Gamaleya, MSS USSR
Sum. 1305

IYZIINSHTADT, 11.3.
I ; -, -"
History and routes of settlement of Ihe common braim
rat (Rattus
norreglaus aarfbgicuo Darken.) within the bou'adarios
of the
U.S.S.R. 2ool.zhur. 34 n6-5:n45-115:! 8-0 155- (KLRA
9:1)
1.8anitrano-apidemlologichaski otrynd.
(Rats~

SOSNOVSKIT, I.Y.; AYMSHTADT, D.S. (Wessa)
Doublo-headed serpents. Priroda 45
!50-3:2.19-120 Xr 156.
(MLILA 9:7)
I.Nookovskly seepark (ter Ssonavski:r)
(Serpents)

SHAVIMSHTETN, V.L.; Ar4XXq4T4pT,.P.S.
Studying the susceptibility of Norvity rats to Infection
by lepto-
spirosis in the southwestern Vkraino; authorla at)etract.
Zhur.mikro-
biol.,epid.1 immun. 30 no.llt116 11 159. (MIRA 13:3)
(I&,FTOSPIROSIS) (MMAINII--RATS AS CARRIKRS 0? DlSFASB)

AYZENSHTADT, D.S.
Nature of relationabip between I;he black rat (Rattus
rattue L.)
ard the brown rat (R.norvee;icus Berk.). Zool.zhur. 38
no.9:
13196-140,5 8 '59. (MIRA 132-1)
1. Aserbaydahanskaya protivochuinnaya stantisip,
(Baku).
(Rats)

AY'4" 1F, N S i i T.-%
013ame Relplarities in Distributica of Petroleum In
Southern Embe. Regioap" G. Yo. ApaiwMadt, All-Uniam
Petroleum Solentiflo Ressaroh Geological Prospeeting
Institute, 2 pp
Obok Ak Nauk" Vol LTE3:Ep No 4
DIscuooos results of isme 335 anayssa omdueted to
detezvWie petroleum-bearing area In southern Ibba
2*4gicn. Lists general areas vhere tbase tests verip
taken. Submitted by Madeadolem, S. 1. Mronov, 28
Apr 1947.
)W92

AYZENSIITAU',', 0. Yo -
"Condl.tions Governing the Sedbnentation-A ccumulat ion of' the South
Embe in the Jurassic Period." Dokl. AN SSSR) 68, No.5, 1949 1
AlL-Union Petroleum Sci,Res, Geol.Pmepecting Inste

BAKIRDV, A.A.,doktor nauk, redaktor: VASS)YLVICH,
N.B., doktor nauk;
VEBREL, V.V. , doktor nauk; IHILI, t4.F., doktor
nauk; DOBETANSKIY,
A.Y. , doktor na)tk; MATNU, S.L., loktor nauk;
HIRCHUX, M.T.,
reduk-tor; ANDRRTKV, P.F., kandidat nauk; AXZM
kandidat nauk: B000HOLOVA, A..I.. icandidat nauk:
GORSKAWYAJ."iI.,
karididat riauk;ZIIABREV, D.V.. kandidat nauk,
redaktor; KAZMINA,
T.A.., kandi(lat nauk; nssiuvu, M.A., kandidat nauk,
PETROVA,
Yu.11., kandidat nauk; ROCENKO, D.A., kandidat nauk;
TATARSKIY,
V.T,., kandAdat nauk; TIKHIY, V.N., kandidat nauk;
USPOSKIY, V.A.
kandidat nauk. DTAKOV, B.F., rndaktor; SAVINA, Z.A.,
redaktar;
TROTKMOV, A.V. , toftnicheakiir redaktor.
(OrIgin of oil) Proiakhothdanie nefti. Pod red.
M.F.Mirchinka i
4r. lloskva, Gos.nauchnn-tnkhn.12d-vo neftianoi i
gorno-toplivnoi
lit-3-7, 1955. 483 P. (MLRA 9:1)
1. Chlen Icorrespondent 0 SSSR (for Mirchink)
(Petroleum geology)

AYMIhSRTADT. G.Ye.-A.
......
Some nawdata on the tectonics of' sall.ne domes.
GeD!.abor.no.3:
215-21B 155, (M-RIL 8:6)
(Jeology, Structural)

AYZENSHTADT, I.Te.-A,
On the DOcurrence of salt cornices in the Imba
domcs.Geol.abor.
no.3:219-M '55. (KLoA 8:6)
(Kazakbstan--Geology, Structural)

f~Y-LCLW o \i -v (I ~1) T, ~V- .
AIZKRSHT&IR,G.Ye.A.
Oil-bearIng series of the southern Bob% region.
Tntdy VNIGRI
n0-0:1)0-1-139 '55- (KLRA 8:10)
(11abs, Vallay-Patroleum geology)

ATZENSHTADY, G.E.-A.; AVTONOV, K.V.
FactorB in the formation of slat domea and oil poolB in
the southern
part of the Emba oil region* Avtoref, nauoh. trud. VNIGRI
no,17:
214-4).19 156. (MIRA 11:6)
(Kazakhstan--Petroleum geology)

AMONOV, X.V.; AYZENS11TAX, O.Y*.; GRACHN, R.I.;
DZUMAGAI,IYFV, T.N.; KOWYPIN'
S.x. bwmm,,
"Oil-bearina strata of the 36~a region and the-orIgin of oil
pools,*
N.K.Chukesv. Reviewed by X.1'.Anteso-Y and others.
Neft.khes.34 zo,W5
Ag 15 6. (KW 9110)
(Emba region-Petrolem geology) (Chukeev, N.M.)

ATZEN.1311TADT, G.Te.-A.
%41,,- ~
Classification schna" of oil po,)ls in the Imba isalt
domes.
Trudy VNIGRI no.95:21-30 '56. (MLRA 9:12)
(Imba Valley-4etro%eum geologr)

15-57-5-5997
Translation
from: Referativnyy zhurnal,
Geologlya, 1957, Nr 5,

pp 42-43 (US"~'R)
AUTHOR:
Ayzenshtadt,
G.Ye .-A.
TI Tl.*jE
An Outline Classification of the Stilt
Domes of Southern

Embil (Skhoma klassi.fikatsli solyanykh
kupolov Yuzhnoy

Emb Y )
PERIODICAL:
Tr. Vses, neft. n.--i.
geologorazved. in-ta, 1956, Nr 95,

pp 214-221.
ABSPRACT:
Ten
types of salt; domes are differontiated. The type

"Suyeshbeic" is associated with the zones where salt

tectonic
movement Is nearly ended and a transition to a

platform
structure is taking place; the salt core is a

gently sloping,
doine-shaped bulge with its apex at a

depth of about 3 kin.
Ihere are but weakly defined

anconformitivs. Dips cf limbs
are up to 50. There are

few faults; the grilben may be 5 kni
to 6 km wide, but

may be completely absent; sections of limbs
are similar.
Card 1/4
The type "Karaton" is cijaracteriZEid by
IA slightly

An Outline Classification of thE, Salt Domes (Cont.)
asyrimetrical salt cove. Its cap bre9ks'through the
Permo-Triassic
at '-.-.he depth of about 2 km. Depth of erosion in the layer
above the
sall: reache:3 60 m to 70 in; walls sloj)e at anglen not
exceeding 81.
Aside from the faults in the graben and the radial faults,
there are
Yr.an,,, faults In the limbs. This amplitude is froin 3 m to
15 m. Width
of the grabon is from 2 km to 3 km. We obsorve clear-cut
differences
in -~he sectlons of the limbs and of the graben. The type
"Narmun-
danak" is characterized by asymmetrizal salt cores at a depth
of
900 in to 1200 m, where they pierce the Permo-Traassic and, in
part,
the Jurassio. Erosion in the portion near the nap reaches 50 m
to
60 in. Slopes of limbs are up to 100. The grab,)n is 1.5 km to
2.5
km ivide. The sections are not oqually complete on the upthrow
and
the downthrow sides. The type "Kulsary" is cha:racterized by a
narrow, markedly asymmetrical salt core with it:3 cap at a
depth of
250 m to 3 00 m. It breaks thrOUgh the layers above the salt
to the
Ap t'. an. Erosion in the parts of the raised walls near the
cap reach
100 m to 150 m; slopes of limbs are ap to 250- The graben Is
300 m
to 500 m wi d e. The depressed 1!.mbs show a relatively full
section,
while in tho raised ones, sepELI-ILte horizons, series and
layers are
mis3ing. The type "Dossor" has a horizontally 3tellate salt
core
Card 2/4

An Ciatline Classification of tile Salt, Doines (Cont.)
15-57-5-5997
witl,,. a complex rE)J.tCf at a depth of 2~00 m to 500 in.
Slopes of limbs
are up to 100. The system of narrow criss-cross grabens is
charac-
teristic for this typp. Unconformitlas and erosional.
features reach
100 m to 150 m. The type '%ychunas" has an oval salt core
with
gently sloping sides, at a depth of %500 m to 500 in. The
slope along
its long axis may be vory steep. Tho layer above the salt is
pierced
through to the Aptian. Erosion reaches 500 m to 600 m. Whole
systems may be missing. Dips of strE.ta are up to 150. There
are
few faults. The type "Iskine" has a flat, tal)10-shaped top
of the
salt; core at a dopth of 100 m to 200 m, and the sides of
the core
sloping at 400 tc. 701. The layer above th~ salt, is brokbn
through to
the Upper Cr-etacoous and Tertiary deposits. Tho total depth
of
erosion may exceed 1000 ni. At the top of the dc(ne whole
systems
are lacking. Slopes of' the layers are up to 700. There are
numerous
transverse and longitudinal faults. The subtype "Chernaya
Rechkall
is distinguiShed by the outcrop of the cap rock. The type
"Kuttubay"
has a salt core with comparatively gantly sloping sides (300
to 450)
and a flat ~,ome up to 150 km2 in extont, and iying at a
depth of
Card. 3/4

AYZENSHTA,-Z, G.'fo,-A.
,
Mastarn Callplan Npression. Trudy VNIGRI no.96;5-27
1,56.
(Catipian Lepression-Goology, Stratigraphic) (VIM
10:1)

*I. '~c. -A.
"The HIS*;'Dry of the Tectonic Development of the
(Prjkarpi)rskiy)
I're-l.'aspinn Pe:presslou." p - 179
Geologichoskiy aborn:UK, 3, (Collection of Articles In
Geology, Vol- 3),
Leningrad Gostoptekhlzdat, 1958, 471pp. (TmAy, v)lp 126,
Vsei;o)uznvy neftyanoy
nauchno-Iscledovat.--j'skly geologorszvedochny), institut)

AYZINSHTADT, DNIUMOV, V.S.; KOLTr."IN, S.N.; SOROLOVA,
Ye.I.
Oil and gas potentials of the southirn Jm1xh reg!;on and
adjacent
soutbern territories. Geol.nefti 2 no.9:19--25 S 158.
(MIRA 11:10)
l.VsesoMny7 neftyanoy nauchno-istledovatiollskiy
geologo-razvedochnyy
institut.
(Kazakhstan--Gas, 1iR%ura1---Geo1vg)r)

AYZBNSHTAM,_G.YFt-t.A-4--MFONDV, N.K.; ClU2WjNDV,, hT.N.
Basic problems relative to oil and gas potentials of
western
Kazakhstan. Sov.geol. 2 nn.q:fi6-6q 3 159. OCIRk 13:2)
1. Veesoy-uzw ~qftyanoy nauchnn-issledovittel.19kiy
goologoraz-
vedochnyy institut (VNIGRI).
(Kazak-hatan-Pevrolewt geology)
?,al--GeolojO,)
(Kazakbetan-Gas, xatu.

AMA511TOT, G.To.-A.
.-1 11 1-1 .; I t -';', - I---,k
Zorutl structure of salt dones in the northern part of
the Caspian
Sea region. Geol.2xofti i raza 1 no-8:13-18 4' '59.
(141RA 12:11)
1. Vaosoyusnyy neftyunoy nauchno-Isaledovatelloldy
goologo-
rtx2,jcdochrqy inatitut (VIIIGRI).
(Canplan Sua region-Geolog-f, Stru.,tural)

AYZENSHTADT, G.Ye.-A.
... I .
Geology and oil potential of the southern Exiba
region. Trudy
VIGGRI no.132t29-43 159. (HIRA 17t1)

i;'027 ~BC 7 '6
AUTHORS: Gr:.nberg, I. G., Dlyakov, B. F.,
4evolln, N. %F., Trof-1mov, 11. K., Cherepanov, N. N.,
Eventov, Ya. S.
TlTLE: Petroleum and Gas ProspectE of Western Kazakhstan and
Principal Trends of Regione.1 Exploration and Prospecting
PERIODICAL: Geologiya nefti i gaza, 1960, No. 2, pp. 10 - 15
"'EX' .: In accordance with the resolutions of the XXI 'Party
Congress of the
,FSU, the petrDleufr. industry in Kazakhstan was assJL:-ned the task
of
pr-,ducing lax-go industrial petroleum and gas stocks wLthin the
Seven-year
Plan. Western Xazakhstan includes the Ca3Dian depression with one of
the
largest salt domes in the world. Prospecting for petroleum and gas
in this
territory is to be carried out in four d1rections cor:?esponding to
geo-
IcEical formations: 1) in the complex of salt domea above the salt
layer,-
2) in the Paleozoic zone beneath the salt. layeri 3) in the Yesozoic
zone
of North Ustyirt and the Buzachi peninsUIU; and 4) in the Mesozoic
zone
Card 1/3

Petroleum and. Gas Prospects of Western
S/009/60/000'002/001/002
Kazaklistan arid Principal Trends of Regional B027/B076
Explori,Aion c.nd Prospecting
of South MaiVy~hlak and South Ustyur-L. Two million meters
of deep drilling
will be neceEsary. The most promising directions and
regions for the
expl:)ration are now being determined. These are: 1) the
Mesozoic structures
and. the sea bottom at Karaton; 2) the region north of'
Dossor-Makat where
high-quality fatty oil is suspected; 3) the north-eastern
part of the
Caepian depression in the direction from Makat toward
Shuburkuduk; and
4) the region between Volga and UraL where abundant natural
escape of Etas
has already been attracting the attention of geologists for
a long time.
Of the other regions, South MangyshLak and South Ustyurt
are the most
promising petroleum deposits. In the time of the Sevon-year
Plan a number
of scientific explorations are planned in %7estern
Ka,:akhstan, geological
~iorveying of the entire territory of Ustyurt and most of
the Caspian
J----pression ort a scale 1 - 200 000, c;eisiric
exploration, trial drilling
-,,~Iectroe):ploratory work according tc the, telluric
current method with
-,ich the Presence of tectonic elements of first and second
order has been
i stied. For the exploration of PalEozoic deposits In the
central part
'.;i(! Caspian depression 10 drillings are planned, one of
them to be to

" ~ tL('1LLZ1i'1 11111, Gas Preospects of' Western
i/009/60/000/002/001/002
Kazakhstan and Principal Trends of Regional 13027//B076
Exploration and Prospecting
a depth of 6 or 7 kms. The main aim of --,he regional ivork
is the explora-
tion of the facies and of the petroleum-- and gas-bearing
Faleozoic
Mesozoic and Cainozoic deposits in the various tecto-.,.Iic
formations.
Further the determination of the large twopected salt plug in
the central
part, of the Caspian depression and also the geological and
geophysical
inv-,:,stigation on the Ustyart and Mangyshlak in order to
determine the
peculiaritiea, physical properties, depth, and age of the
folding of the
beds and the general construction of large tectonic
formations in these
reFions. There is 1 figure.
ASSOCIATION: VNIGRI (All-Union Petroleum Scientific Research
Institute
for Geological Exploration), VNIIGeofizika (All-Union
Scientific Research Institt.te of Geophynical Exploration
Methoda), VNIGNI (All-11nior. Petroleum Soientific Research
Institute for GeoloLical Eyploration)
Card 3/3

AI'ZEN3HTADT, G.Yo..-As; NSVOLINj 14.V,,- VENTOVt U.S.
Drillizig extradeep weUo in the cent,-al Gaspian
Lowland. Sov. geol.
3 no* 32:33-43 D 160. (MIRA 14-.2)
1. VseEiovuzzVr neftyanoy nauchno-ios.Ledovateliskiy
geologorazve-
dochrinr institut, Vsesoyuznyy
namahm-issledovatellskiy institut
geofizichaskilch metodov raEvedki i Vwaoyuznyy
nauchno-issledova-
tellskly geologorazvadcohnyy nefty&nV institut.
(Cag-pian Lowlind-Boripg)

AIZXNMTADT,, G.Te.-A.
PrD11PeCtG for finding heaTv oil 13oole In wester,
Uzakhatan, Geol.
nefti 1. gaza 4 no.9:1-5 3 100. (KIRA 13:8)
1. 1rseaoyuzny7 neftvanoy natwhnc-loaledovatellakiy
institut.
(Kazakhatan-Petroleum geologV)

ANUSHTAIN, G.Te.-A.; XDLTYPIN, S.N.; TRIFONOV, H.K.
HAictonie structure and historizil development of the
Caspian lowland
and. adjacent regions in connect.",)n with gan aril oil
potentials' by
M.P.Kazakov and others. RevieweL by G. X-A. Alzenshtadt.
S.N.Koltypin,
andl H.K.5?ifonov. Izv. AN SSSR. Ser. geol. 25
no.4:109-112 Ap 160.
(MIRA 13:11)
(Caspian Lowland-Geolo Structursl)
(Kazakov, M.P*f

AIZENSIITAD','P G. Ye.-A.
Problem
area of
255 160.
of evaluating the oil and gas potentials of the salt
dome
the northern Caspian Sea region. I~rudy V14IGRI
no.163:233~-
(Cuspian Sea region-Petrolem (;eulogy) (MIRA 1416)
(Caspian See region-Gas, Naturttl-Geology)

A72;ENSIITADT, G. Ye-A.; YAKUTSENY, V.P.
Us.'Lng the characteristics of free and dissoloved gaves in estimating
tho outlook for petroleum in the southeastern dispian Lowland.
Trudy VNIGRI no.163:571-575 160* (MIRA 14:6)
(Caspian Lowland--Petroleum geolft7)
(Ca,splan Imland-Gas, Ritural-Analysis)

AYZEb[SHTADT) G.Ye.-A.
Stratig.caphy of the lower and middle Jurassic of
the southern
Emba ofl-bearing province. Trudy VNIGNI no.29:64-71
vol. 2., 161.
(MIRA 14:7)
(Embs, region-Gealogyj Stratigraphic)

AYZI'.NSHTADT, G.Ye.-A.; GRATSIANOVA, O.P.; NEVOLIN,
N.V.; EVENTOV, U.S.
Efficient methods for geological mapping ard
prospecting in
salt--dome regions. Sov.geo*'L,. 4 no.12:113-116 D
161. (MIRA 15:2)
1. Ministerstvo geolcgii i oklira:ay nedr SSSR.
(Goology-Haps)
I
(it, 9spe -tin )
(iklt d,cceall

AYZENSHTADT,, G.Ye. .-A.1 BIREZOVSKAYAS V.L.; IMASHBV,
11.1J,
Proarpects for oil potential in the southern Ibba region
Geolo
neft*i i gaza 6 noo4:17-24 Ap 062. iMM 15:4)
1. V,3esoyumiyy neftyanoy nauchno-Issledovatelloldy
geologorazvedochnyy
instItut i Zapadno-YazakhatarLskoye geologichoskoye
upravleniye.
(EmImL region-Pettroleum geology)

AURNSHTADT,.Airph-m-levelt Aronovichl 'PINCIIUK, Irima
Amb!ianovna;
lh~VEI.ISHTEYN' .veaiiahchty red.i YASHCHURZILINSKAYA,
A.B.,
tekhri,red.
[luzlmaya Raba 2 and Tugarakc)mn 5 key wells)
.111zhno-Embenskaia 2
i Tupmkchanskaia 5 opornye mkvaz~ainy Leningrad,
Gos'nauohno-
tekhriiaheskoe izd-w neft.i gornot3plivnoi Le;Z. otd-nis
1961, 293 ps (Leningrad, Vsi)soiusnyi neftiamd.
nauchno-insledovatelf-
skii geolo oravedochnyi institut. Trudy, no.lta ~, (MUM
15 1 U)
Iftra: Lowland region-Petroleum geology)
(Kura Loi~land region--Gas, Natural-ClIvology)
(Ust-Urt region-Petroleum geology)
(Ust,-Urt region-Gas, Natural-Geololp,)

AYZFNSIITADT Girsh Yesell-A.ronovich; ANTONOI, Karp
Vasillyevich;
i
red,; SAFRONOVA, I.M., tekhn.red.
(Fornation of salt. domes and oil pools in the
southern part of the
~mbaj Formirovanie solianykh kupolov i zRlezhel nefti
IUshnoi
"'mby, Leningrad. Gontoptekhizdat, 196). 315 p.
(Leningrad.
Vsosctiuznyi neftianoi nauchno-issbdovatellskil
geologorazvedoch-
nyi institut. Trudy, no.207). (MIRA 16:8)
(Emba region-Oil fields) (Emba regicn--Salt domes)

AXZENSHTADT, G.Te.; EVENTOV, U.S.; YENIKE)MV, P.N.;
LII?OVETSKIY, I.A.;
NEVOLINP N.V.
More on the problem of drilling extra-deep holes in tj:te
Caspian
Lowland. Razved. i okh. nedr 29 no.9:17-20 S 163. (MM
16:10)
1. Vs-esoy-uznyy neftyanoy nauchno-Iesledovatel'slAy
geologoraivedochnyy
institut (for Aysenshtadt). 2. Vseso),uzny)r
nauchno-issledovatel'skiy
geologorazvedochnyy neftyanoy Institut (for Eventov). -
3. Gogudarstvennyy geologicheskiy ~omitet SSSR (for
Tonikeyev).
4. V&3soyumnyy nauchno-issledovateltskiy institut
geofizicheskikh
metod,)v razvedki (for Lipoiretskiy, Nuvolin).

GERSHTEYN, E. I.
Initial thickness of the Kurgur salt-bearing complex
in the Caspian
Lowland. Dokl. AN SSSR 151. no.5$1156-1158 15.3. (MIRA
16:9)
1. Iraesoyuznyy neftyanoy nauchno-Issledavatellskiy
goologo-
raziredochnyy institut. Fredstavlano akademikom
A.L.Yanshinym.
(Caspian Loqland--Salt domes)

A'YZE'N,6HVdYT, G. Ye.; 1EVOLIE', 11. V..,, EVEIMN, Ya.
S.
it Gcological i;tructure and oi-l depa:-,its of t)-,e
Caal.dan depresr,Lon."
rejort submitted for 22nd Sess, Intl Goolo;,,.icELl
Cong, NE!w Delhi, 14-22
Dec 1964.

ATZEMHTADT1, G,Ye.,-A. ) DKEFROVp V.S.
Evaluating the proepects for,finding oil in the
southwestern
Caspian La,41and and basic trends in prospect-Ing
operations.
Neftegaz. geol. i geofiz. no.70-1,! 164. (MIRA 17t8)
1. Veiesoyuznyy neftyanoy nauchno,' isle dovatell
sUy geologorazve--
dochriyy institut, Leningrad.

ACF NRs AT5028971 SORCE CODE: URtt)ooo/61i/(ioo/c)oo/o~~30/oL~143
Asze jbtadt. G. Ye Et~vpiin ]~Kentov, ra.G
AUTHOR:: N. V!;
ORO: none
TITLE: &1212-1 al structure ud deposits of i;he Caspian depression
nal Geolo
SOURCE:: Internatio I ical CongTess. 22d, New Di~lhi, 196h.
Geologiya nefti.:..
(PetroleuR geolo'). Moscow, T& -vo R&A-a-,"'196
k, 230-243
9y
TOPIC 17AGS: geclogy, earth crust, natural gas, petrolei=, fuel
phy!3ical geology,
seismology, Moharovicic discontinuity
ABSTRACT: In recent years nev data have been obtained on the
G-ological structure
of the Caspian depression--onle of the vety promising new oil and
gas areas. Region-
al seiiimic profiles obtained 'by the ccmbined refracted i3nd
reflected wave methods
gave an idea of the depths of the mantle and erystalline basemen',,
as well as of
the made of occurence of the .1~re-Kungur Taleo,.oic deposits
(subsalt bed) in the near-
flank s:one and central parts of the depr-ession. Sevekc~l ke- and
parametric wells
are betng drilled there, one of them to a deplih of 7000 meters.
This will be one
of the first vells drilled to such a depth in Eurasia. The Caspian
depression is
a de 'eply sunken part (pericr&ton fore-deep) oi! the Russian
platform consisting of
Paleozoic, Mesozoic, and Cenozo:Lc deposi-be from 15 to VT
kilometers thick. The
oldest rocks unCDvered within the central parts of the depression
belong to the

X6
NP- AT50289Ti
PermiEui system. Those are hy1rochemical sedbientD, wetly rock valt,
anhydriteo# and
gypsum of Kungur age occuring in coren of sali; plugs. rhey were
drilled to the
maximLui depths of 2000-4000 meters in wells on the Dossor, Kulsary,
Inder, Chernaya
Rechka,, and other domes. Acooraing to the U,;a of seismic
prospecting the thickness
of salt in some cores reaches seven to nine hilometers'. In the light
of new
geolog!Lcal and geophysical dats. the main featiires of the deep
geological structure
of the Caspian depression appear to bra. as folLows: Seismic
observations by the
combined method of refracted vwires revealed f-Yur seismic surfaceFi
characterized by
abrupt (saltatory) changes in the velocities -)f elastic
flijctuations within the
Caspian depression in the crystalline rock ma-,s of the earth cruc;t.
Judging by
the va:Lues of the top velocities (8.0--8.1 km1sec), the lolgest
si:Lrface (M) corre-
sponds to the surface of the -upper mantle of "he earth (Moborovicie
discontinuity)..
It extends a3xioet horizontally at a depth of 38-h2 kilometers. The
third and
second surfaces are discernible only In the c~~-.ntral part of the
Canpian depression
(in the area of the Mhobdinsk gravity maximum). The third surface
there is at a
depth of 24 kilcmeters. Its -top velocity is S.6 km/sec. The toj
velocity of the
first i3eismic si;Lrface is from 6.0 to 6-5 km/sec. In Khobdinsk
region it occurs
at a depth of lh, kilometers and then rises st,!plike towarda north
and south. The
Pre-Kwigur Palecizoic rocks descent stepvise from the flanks of tbe
depression
towardi3 its center, where their surface is seismically detected at
depths from
7 to 11) kilometers. hi Paleozoic deposits local upliftE: and
doummarps, as well
as lar,~e faults can be developed. The Caspiaa depression is,
cbaracterized by
extensive develcipment of more than 10CIO salt lome structures. WitUn
the south-
Card 2/3

N'
eastern part of the depression.and In its east-trn and
soifteastern framing there
are oil fields with Upper Permian, Triass1c, Jlirassic, ani
1,Dwer Cretaceous
productive deposits; in central parts of -the d,~pression
Intense gas shows are
observed in Mesozoic and Plicene formations. rhe supposed oil
and. gas reserves
are associated with Paleozoic '[Devonian, 1" arbo.3iferous,
Lower Permian) deposits
primarily in the near-flank zoneis of the depre3sion where they
occur at depths
up to five kilometers, and with Upper Permian and Mesozoic
rDcks, throughout the
entire ares. of tbe depression; in some parts of the depression
coixmercial accumula-
tions oj, ' oil and gas can also 'be found in PaleDgene and
Neogene rocks. Orig.
art. hail: 5 figures. (Based on author's abstract.]
SUB CODH: 08/ EUBM DATE: oB)ct65/ ORIG REFt 0191
-Card

AYZENSHTADTO G.Ye,,A.
-111-,- .1-1. . . .1 .. .
Twiards a history of the develorment of the oJ.1 industry
in the Emba
region. Geol. nefti. i gaza 8 no.9356-59 S 164.. (MIRA
17:11)
1. Vsesoyuznyy neftyanoy nauchnc-issledovatel.'skiy
geologorazVedochnyy
Institut, Leningrad.

AYZFJISMIJ;T~t I..~o._A; DIJBININ, A.Z.; YRNMEYMI,
P.N.; MAYSIMOV. 5.P.;
-TOV,
'OVA. YP.A. ; SOKOL 14, Eri.G. ; IWEN YEL.S..;
FZDII:iN, M.B.,
Outlooks of a new oil and gas pmdu~Jng center in tho
Caspian
Lowland and adjacent m-gions. Gcol. neftui i gE~za 9
no.10-8
J11 1 "15. OCRA 18:3)
1. 3osudarstvenriyy geologicheskI3 komitet SSSR;
Vsesc)yuzrivy
neftyanoy nauchno-icsledovatells~Ay
geologoraz"vedochn.'ry instil~ut,
Leningrad; Vsesoyuznyy
viaiichno-J~slc-(Iovtitellskaya gecilcgorazve-
dochnyy neftyanoy instlMit, Mosk-ia;
Nauchno-Isgledow,tellskayn
laboratoriya geologicheskJkh kirlariyev otsenk!
persPektiv
neftegazonosnosti 1 Nizhnevclzhsliy
nauchno-issledovF-tellskiy
institut goologiJ J geOfi2dki.

AY,"lBNSUADT,__I.A.; VOLIPSON, N.B.; 1401SQY, S.A.;
MUSIN, R.A.
Gencitic connection between copper, %mo lybd enum oro
formition in
the Almalyk region and intruitione, and its itq)ortunce
for
copper aro prospecting, Uzb.j;eol.:shur.no.3:7--17 160.
(MIRA 13:11)
1. G-lavgeologiya UzSSR i Institut geologil AR UuSSR.
(Llmalyk region--Copper ores)~,Almalyk
regiau--M~rbdenum ores)

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