SCIENTIFIC ABSTRACT BABAYEV, A. A. - BABAYEV, A. G.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R000102810017-1
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: June 6, 2000
• Sequence Number: 17
• Publication Date: December 31, 1967
• Content Type: SCIENCEAB

3699,;
S/044/62/000/003/037/092
C111/C444
,IUT11ORs Babayov, A. A.
TITLE: On the theory of non-linear singular integral equations
with a Cauchy kernel
PERIODICALj Refortitivnyy zhurnal, Matematika, no- 3, 1962, 70,
abstract 311295- ("Uoh. zap. Azerb. un-t. Fiz.-matem. i
khim. ser.," 1960, no. 2, 23-54) -
TEXT: Let Y,, fs f f be positive nul"k ors; 0~+ if, 0 + S < I . Let
0 Lly L ts k (k - const). The family of the functions u(x)
2
which are given in (a, b) and satisfy the conditions
u (x) ~ ::5 L x - a x b U(X + L X) -
U(X) L x - a + x b + Lx J
2
was considered by A. 1. Guseynov (Izv. AN SSSR, Ser. matem., 1948, 2).
It is proved that the family Hk -L
tx r~ f becomes a complete metric space
by int oducing the metric
Card 1~4

S/044/62/000/003/037/092
On the thoory of non-linear singular ... C111/C444
r
t1 U(X) - V(X)! (x-ft) x-b
'(U, V) sup
x ~ (a,b)
is complete under a convenient choice of
where > 0, and the 11k
also in the sense of the metric of the space Lp(~) (LP(R) is tho opace
J
o
of those functions which are summable in p-th power (P > 1) with weight
P(X) = (X- ).t (g-l)(,6_x)/3 (y-1)).
Theorem, 1: The following conditions be satisfied:
1. The functiona K(X, s) and f(s,_u) are defined for x, s E (a, b)
u E (- 00 00 ). 2. 1 K(x, a) M0 const, IK(x 29 62 K(xl , 91 A,
.1 + A > Gf 3. f (s ~ 0) E Hk 't f(S
X2-xl I j 21 92-81 16' CI 1 (11 cri 2u2
f(s Vul B1 1 s2-s1 id, +B21U2-U, 1 where u4 (3 < d --I and M., A,, A2'
B1, B2 are constants. Then the equation
Card 2/~-

S/044/62/000/003/037/092
On the theory of non-linear sin&ular ... 0111 C444
1
U(X) K(x,s)f Es,u(s)j da
3 - X
for sufficient small k Ix I, for which tin estimation is given, possesses a
unJque solution in H0~ 6 Swhich can be determined by successive approxi-
nation, where as initlai approximation an arbitrary function u 65 H k
1 C41 a I d*
may serve; the successive approximations converge to a solution in the
sense of the metric of LP(SI) In the second part of the paper the
equation
U(t) K (t, T f (T, u (T) ) dr (1)
L t - T
is considered, where L is a closed smooth curve of the complex plane. This
equation is investigated in the class of those functions which are uni-
fcrinly bounded by a constant M, satisfying the Hblder condition. For (1)
a theorem, analogous to theorem 1, is given. One compares the obtained
_r
V
Card 3/4

S104 62/000/003/037/092
On the theory of non-linear singular ... C111YC444
results with several results of A. I. Guseynov, V. F. Kropachov and
Pshevorskaya-Roleviuh. There are miBprints.
-
LAbstracter's note: Complete translation.]
L.
I
\j1
Card 4/4

UUIEV9 A.A,
Method of perturbations for a certain class of nonlinoar
singular integral equations with a Cauchy kernel. 'Trudy
Inst.' mat. i makh. AN Azerb.SSR 1:158-163 161. OMIRA 14:11)
(Integral equations)

L4!.. h, i ! .~, , ; - . I , . ~ , ,. I . . . .p , .- . I .. . . I , q . I...-I-C I Z-,
; I ~ - ~ I-- j "l, - I - . t. - . I -. - i , . , " I I ~ -) (' " ,
'I.- - -
. . ., !!I. 1,~ , , - 1 r . -
I!.,'. !, -,, ~ ;" f; (I , I ~ I '.

BADAYIEV, A.A.; SALAYRV, V-V-
An analog of Memel-PrIvalov's theorem in the case of nonsmooth
curves and its applications. Dokl,, AN SSSR 361 no.21267-269
mr 165. (MIRA 1814)
1. Azerbaydzhanskiy gosudarstvennyy universitet* Submitted
August 31, 1964.

BABLAYEV, A.A*
Surgical anatomy of arteria colica media. Sbor. nauch. trud,,
GIDUV no. 14:21-24 158. (MIRA 13:10)
1. Iz kafedry topogrgifichoskoy anatomii i oper,stivnoy khiru:rgii
(zav. prof. A.P. Vadein) i III khirurgichesoy kafedry (zav.
prof. N.I. Blinov) gosudarstvermogo instituta dlya usovershenstvo-
vaniya vrachey.
(MESENTERIC ARTERIES)

BABATNV, A.A. (Leningrad. Zanevekijr prospekt, 1/82, kv.6o)
Surgery for varicose dilatation of the superficial veins of the
lower extremities in the presence of thrombophlebitle. Test.khir.
83 no.11:54-56 N 159. (MIRA 13:4)
I. Iz 3-y khirurgichookoy kliniki (sav. - prof. N.I. Blinov),
Laningradekogo ordena TAgnina, instituta ueovershonstvovanlya
vrachey im. S.M. Kirova.
(LIO blood supply)
(VARIGOSIC VICINS compl.)
(THROMBOPHLIBITIS compl.)

BABAYKV, A.A., m1adshiy nauchnyy sotrudnik
Some data from a study of the etiological structure of poliomyelitis
in Baku. Azerb. mod. zhur, no.1100-54 N 160, (MIRA 13:12)
1. Iz Azerbaydzhanskogo institute. epidemiologii, mikrobiologii i
gigiyeny.
(UKIJ-POLIOMrELITIS)

BABAYLV, A.A.
Dissemination of the poliomyelitis virus and of other enteric viruses
in the patient's surroundings (as revoaled by material from Baku).
Azerb. med. zhur, no. 4t6EL-71 Ap 161. (MIM 14-4)
1. Iz Azerbaydzhanakago Nauchno-iseledovatellskogo instituta
opidemiologii, mikrobiologii i gigiyeny (direktor - prof. B.F.
Medzhidov).
(BAM-POLIOMYELITIS)

YUSUPOV, A.M.; BABAYEVs A.A.
Significance of the height and orientation in a hot climate,
Zdrave Tadzhe 8 no. 209-45 161. (KERA 14:4)
1. Iz Stalinabadskogo Iwtituta epidemiologii i gigiyeny,
(TAJIKISTAN-LABOR AND LABORING CLASSES-DWELLIMS)
(TAJIKISTAN-BODY TWERATURE)

BABAYEVI -- A.A.; LEV, A.B.
Clinical and virusolog~cal study of pollomyclitalike diseases caused
by Coxackie viruses in Baku. Vop. virus. 7 no.2:2/,2 Ml-Ap 162,
(MIRA 15:5)
1. Institut opidoiniologii, mikrobiologii i gigiyeny i dotakoyo
poliomiyelitnoye otdoleniye ob"yedinennoy bollnitsy llo,2j,,, Baku,
(BAKU--CIIILDREN-DISEASES) (COXSACKIE VIRUSES)

BAUTEV. A.A.
Serological and virological Btudy of peroral immunization of
children with attenuated live monovalent (1, 111, 11)
poliomyelitis vaccine in the city of Baku. Azerb,med.zhure
no.2t6l-66 F 162. (MIRA 16t4)
1. Iz Azerbaydzhanskogo nauchno-iseledoVatel'skogo instituta
epidemiologii mikrobiologii i gigiyeny (direktor - prof.
B.F.Medzhidov5.
(BAKU-POLIOMYELITIS--VACCINATION)

3
BI,BAYEV~ A.A. (Tashkent, Ladozlisk-4y p~reulork, L.,)
Effect of ligation of the arter.~a colica meri,a on blool circulation
in the transverse colon. Vest. khir. ?2 no.r:43-51 xy 161,
(,%171;A 18:1)
1. Iz gospitallnoy khirurgicheskoy kliniki (mv. - prof. S.A. %.-iunov)
lechebnogo fakullie a Tashkentskoro rneditoinokoro inqtltutza.

BMYEV, A. B.
M. Azizbekov Azerbaijan Institute of Petr6leum and Chsmistry on
the 40th anniversary of Soviet Azerbaijan. Izv. vys. ucheb.
zav.; neft' i gaz 3 no.4:3-8 160, (MIRA 15:6)
1. Azerbaydzhanakiy institut nefti i khimii imeni M. Azizbekov&.
(Asorbaijan-Petro*m engineering--Study and teaohing)

XAYST&KATA, A.G.; LAPOTI, A.I., atnrn)iiy inzhanar-agromateorolog;
SUMTA, Ts.T., starshiy invhener-klimatolog; YLADIMIROVA,
II.T., inzh.-agrowAteorolog-, KMTXT. M.I.. inzh.-agromsteorolog;
TSZRTSTAD23, Sh.I.; CHIRAKAD23, G.I., dotnent, starshiy nauchnyv
sotrudnik; BABATHT, A.D., otv.red.; USRAKOYA, T.T., red.; TOLKOT,
N.Y., towintrwe-."
(Concise agroclimitio reference book on the Azerbaijan S.S.R.]
Kratkii ngToklim ticho ski i upravochnik po Azerbnidzhnnskoi SM.
Leningrad, Gidromateor.izd-vo, 1959. 67 p. (MIRA 13:2)
1. Azerbayfthanakaya S.S.R. Upravleniye giarometsorologicheskoy
sluzhby. 2. ZAveduyushchiy otdalom agromteorologit Thilieskogo
Nauchno-issladovatellskogo gidrometeorologicheakogo institute
(for T&rtsavadze). 3. Nachal'nik Upravleniya gidrometeorologichaskoy
sluzliby Azarbaydzhanskoy SSR (for Babnvev).
(Azerbaijan--Crops and climata)

GYLIL I ,K.K., prof.; VLASOVA, S.V.j K18114~j I.E.; MTEIMV, A.A.;
Prininali uchaotiye: BABAMI, A.D.; 1:011DRASEOV, V.D.;
'n
PAZU'ABIN, P.11., red.; KHA IT,--LT.-., tekhn. red.
(uivera of tho Daghostan A.S.S.R.Iltoki Dagestnnskoi AFSH.
LBy) X.H.Clull i dr. Makhnchkala, DagoBtanskoo ),,nizhnoe izd-
vo, 1961. 368 p. (PaChestan-Itiveri) (MIRA 15: 10)

BABAYEV, A.D.; VLASOVA, S.V.
Research undertaken by the Administration of the Hydrometeorological
Service of the Azerbaijan S.S.R. in studying the snow cover and gla-
ciers. Trudy Thil.NIGMI M.9:18-22 '61. (MIRA 15:3)
1. Upravleniya gidrometeorologicheskoy 5luzhby Azerbaydzhanskoy SSR.
(Azerbaijan--Glaciological research)

CTI. C
7~

BABAIEV, A.G.; AMURSKIY, G.I.
Ancient cave dwellings in Takhta-Bazar District. Izv.Vsea.CooE.
L',~
ob-va 93 no.5:439-A.41 S-0 161.
(Imu. 14~)O)
(Taljta-Bazar District-Gave dwellings)

D1KENSHTEYN, G.Kh.; KUTUZOVA, V.V.; MASHMOV, K.K.; DABAYEV, A.G.;
FOLISTER, L.A.; YUFMEV, R.F.; SHISPnVA, A.I.; BAREYEV,
R.A.; MAROVA~ L.N.; IMADOV, K., FYAN.OVSKAYA, I.A.;
SEEM, V.N.; SIROTINA, Ye.A.; TURKINA, I.S.; FELIDMAN,
S.L.; KHON, A.V.; KUNITSKAYA, T.N.; GOLENKOVA, N.P.;
HOSHINA, VJI.; FARTUKOV, M.M.; SHCHUTSKAYA, Ye.K.;
ALTAYEVAI N.V.; BYKADOROV, V.A.; KOTOVA, NI.S. ; 514IMICV,
L.1%; IBRAG11,101OV, MI.S.; KIIAVC11121KO, II.F.; Y'ABKOVA, L.P.;
T.R.; UZAKOV, 0.; SLAVRI
ROZYYEVA, 3 P.S.; NIKITINA, Ye.A.;
I-ILOGRADOVA, M.V.; BARTASHEVICII, O.V.; STAROBINETS, I.S.;
KARDIOV, A.K.
[Splicing of the wires of overhead power transmission lines)
Soedinenie provodov vozdushiWkI1 linii clektroperedachi. 1,10-
skvap Energiia, 1964. 69 p. (Bibliotoka elektrumuntera,
no.132) (MIRA 17:9)

TER-GAZAROV, Arshavir Mikhaylovich; BABAYXV, Akhmed Gndzhiyevich;
GULIZADE,M.P., doteent, kand0b~i"tekbnichi6ak-lkh'iifmk, -redaktor;
UDALYY,A.M., tekhnicheskly redaktor. (deceased]
[Manual for the self-propelling drilling unit model AVB.1 Spravoch-
nik po samokhodnym burilInym agregatam tipa AVB. Baku, Azerbaidzhan-
okoe goo. izd-vo neftianoi i nauchno-tekhn. lit-ry, 1955. 200 p.
(MIA 9: 2)
(Petroleum industry-Equipment and supplies) (Boring mnehinery)

BABATEV, A. G..
Solving the problem of compensation of faulting using sedimentary
deposits as an analogy. Izv.AN Arm.=.Ser.MT nauk 9 no.8:31-35
'56. (KLRk 10:2)
1. Inatitut geologichagkikh nauk AN AxmMskoy SM.
(Irsults (Geology))

IRABA , A.G.
-: '. - , ~ ~ . I % ~ 1 1. - -
Paragaitic series amE generations of authigenic mizerals and their
sigaifiewace for studying formation conditions of sedimentary rock-so
lzv. AN k". ISSR. S*r. IM zauk 9 no.10145-53 '56. (nn 1o:4)
1. lantitut goologichookikh *auk 0 Armyanskey SSR.
(Rncks, Sedimentary)

ABRAKYANIH.S.; BABAM, A.G., otvetstvannvy rodaktor; MUNTAN, M.A.,
(Brachlopo" of the Upper Famenlan
Southwestern Amenial Brakhiopody
otlozhonli lUgo-Zapaclnol Armanii.
1957- 141 p.
(Armenia--Brachiopods. Fossil)
and Stro*ungt deposits of
varkhnsfamenakikh i stronakikh
Xrevan. lxd-vo AN Armianskoi SSR,
(KLRA 10:7)

,BABAYEY,,Jh.G'.
Paragenesis and generation of authigenic minerals as r-zemolified
by Cretacenqs sediments In western Uzbekistan. Izv. AN Arm. SSR.
Ser, gaol. i geog. nauk 10 no. 5/6:41-58 157. (MIRA 11:8)
1. Institut geologicheskikh nauk AN Ar!nSSR.
(Urbekistan-Mineralogy)

AUTHOR BABAYEV JLG. ==3=M 2D~Z4 6/ 67
TITLE -On-_Ye_w Po'im-at-Ibna of Rutile in Cretaceous Deposits of Central
Asia.
(0 novoobrazovaniyakh rutila v melovykh otlozheniyakh Sredney
Azii -Russian)
PERIODICAL Doklady Akademii Nauk SSSR,1957,vol 113,Nr 2,pp 407-410(U.S.S.R.)
Received 6/1957 Reviewed 7/1957
ABSTRACT New mineral formations in sedimentary rocks are important mainT
1y because they permit an explantation of the,geochemical entire
formation background of both the sediment and its single compo-
nents. Thus the new formations belong to the most important ini.
tial criteria for the wh6le task of explaining sediment develop-
ment. For a long time it was maintained that thiskind of new for-
mations was practically only represented by carbonates, sulphates
haloids and iron-hydro-oxides. But their list wns considerably
extended during the last years. Many minerals which are apparent-
ly only connected with magmatic or metamorphic formation(feld-
spar, tourmaline and many others) were considered as sometimes
autogenoaa by a number of authors. Furthermore, some sulphide
minerals, especially of the nonferrous metals, belong to this
group. These two perceptions have been expreS3ed in the present
paper. The author makes a crose-section through the sediments of
the cretaceous, which lie on palaeozoic granite. They are bright
Card 1/3 red, brown and violet kinds of limestone, aleurolites, loams and

On New Formations of Rutile in Cretacsous Deposits W-34 6167
of Central Asia. =MMGPP
conglomerations. The material mineralogical composition of li-
mestone and aleurolite shows a remarkable peculiarity: they are
concentrated with magnetite, hydrohetite, haematite, tourmaline
and rutile. The content of the two latter is greatly increased in
the heavy fraction compared with the higher cretaceous layers of
this cross-section. lt is surprising that the rutile content in-
creases together with the content of tourmaline, whereas ore miner-
als decrease. Together with zircon, tourmaline and rutile probab-
ly are the most frequent components of mineral association of the
heavy fraction of the cretaceous sediments in Central Asia. Apart
from the high content at the respective place of discovery the
extremely peculiar form of the rutile grains (ill.1) surprises.
Here two types must be distinguisheds a) idiomorphic,prismatic,
rounded ones with a crossed hatch typical for rutile, b) grains
of bizarre contours with excrescences of different forms or id-
iomorphic prismatic regenerated individua. The color here is ligh-
ter. Optical properties of both forms are practically analogous,
that is positive. Double rofraction is very intense (0.290). Re-
fraction exponents of the second form are N n2,286, N '2,6oo. The
here described variation of the rutile graIns is eider a comp-
lete new formation or a new formation on grains of the doubtless-
Card 2/3 1y allotigene rutile. Reasons for the assumption that the latter

on New Formations of Rutile in Cretaceous Deposits 20-2-46/0
of Central Asia. 21 , I ~Jjlj
are completely allotigene seem to be lacking.Tt is usually main-
tained that rutile is an example of high temperature minerals.Re-
cently,however,Yarosh described ilmenite-transformation in rutile
among others at relatively low tomperatures(6oo-7000).Probably it
can proceed at even lower temperatures.In arid climate an immense
difference in the water saturation develops between the lower and
the upper layers of the lithosphere.This not rarely caused an in-
tensified ground water supply to the upper layers,and so-called pseu-
dohydrothermal solutions develop.It can be assumed that such 8olu-
tions wash out T102 from deeper layers and then deposit it in upper
horizons as new formations.Thus the development of new formation of
rutile can be connected firstly with the decay of the original ti-
taniferous minerals and secondly with its secretion from sediment
solutions in connection with fast evaporation.Purthermore they can
then serve as attraction centres.
(With 1 illustration, 11 citations ftm Slavic publications).
ASSOCIATION Institute for Geological Science of th e Academy of Science of the
PRLSENTED BY SMKHOV N.M.,Member of the Academy--- USSR'.
SUBMITTED 22-10-1956
AVAILABLE Library of Congress
Card 3/3

,Q THOR -.BABAYEV, 'k.G. 20-1-39/54
T I TUE Terrigenous-Mineralogical ProvinceR of Cretaceous Leposltq In the
South- Western Part of Central A.91a
(Terri gerino-ininer,-ilot_,ichegRiyt.- provintsii melovykh otl(.17,11oniY
-vostochnoy chasti. Sredney Azii. Russian)
Y~tIoljic.~T, Doklady Akademil Mauk SSSR, 1957) Vol 115, Nr 1, PP 145-148(U-S-S-R-)
~iJSIRACT The present paper 6ives the results of 1500 inLner-,Aon analyses
by the author of Cretaceous deposits of that territory. The heavy
fraction is of main importance in the soparation of the associations
of clastic minerals. Thu leading terripenoits componontq of thf- lAght
fraction are constant: quartz and fieldspar, sometimes: bits of' nieta-
morphic and effusive rocks as well as mica. Thu heavy fraction shovis
another picture: the associations of heavy minerals are unequal. in
the individual districts. Mine fundamental types were established:
Type I. is characteristic of the Cretackgous of tho depression around
lashkent. It has a high content of Zirconium, -w-net, apatite, epi-
dote and partly staurolite. The terrigenous components wer4 developed
by the destruction of the Paleozoic deposits of the Kuraiiiin and part-
ly of the Kara-Tau mountain ranges. Type II. charactarize,-, the Cre-
taceous of southern Fergana and has a high content. of maGn%~Ute,
zirconium, turmaline, epirlote, staurolite and biotite. Apatite, to-
Card 113 pas, disthene, rutile and picotite occur in smaller quantities. In

20-1-39/54
Turricenoils-Winer,ailogical Provinr%-r~ oi Gretae~ntu; Jupo~iits in the
:.)ou Lh.i,es tern Part of Gantral Asia
south-eastern and northern Fergana quite an-Aher asrioi,,iati~)rl is fcir.A.
irom the Turkestan and Alai ranges in the south, Crotaceous bits
were sinifted to soutbern Fergana. Typta III. I,-; fOLAnd to exist in tliw
Zurafsi)an vallwy. It emme here from the north aftur (histi'lleLion of,
granitoids of the Palazoin of the Turkestan raneo. Type IV, is chara'--
teristic of the southwestarn branches. of the Hisspr mountain ranve.
Tile clastic particles mainly cazirie form tho norLh, frori the fil.~i;iar
and the Zerafshan ranges. The provinCe-3 is, howQver, complicated by
additional sources, probably those of Pamir and Darvaz. !jpe V. rliq-
covered in the southern parts of the Bukhara depre.--sion. This re-
gion Is set up as the southern subprovince of the bukhara-Karshi
terrigenouq-4nineralogic province. Type VI. coiijbines Oo crois sec.Llo:..
of the morthern parts of the Bukhara depreasion with soine sections
of the Cretaceous of the steppe belt. This is the northern subpro-
vince of tile province described under V. The sourcfs ~-' We clwitic
material lay in the region of the Nura-Tau and the Zirabulak-Ziaet,,li-i
mountains. Type VII. combines tile sections of the Ky--yl-Kum. It is
the Kyzyl-Kum terrigenous-mineralogic province. It has most prob-albly
Card 2.13 to be considered a complex province, since several sotLrees iTjy i)e

js530CD%T1ON
PRLSi;'ITED DI
"UbUITTED
,tVAILABLE
'l.lerrli;eiio)in.-~Aineralogical Provinces of Cretact--ous 11 ~ii !A-~:
South-Western Part of Central Asia
deterinined: the southern periphery of the Ural-3ibirian epil;vru~~n4an
plateau and thf-- archipelago: Bukan-Tau, Taridy-Tlau, Kul Idzhuk-7 1,';;:i,
Type VIII. charactvrizes the cross sections ,Nf the Pitnyak
~':Aca prevails here, and these sections are thuq combined to a miLa
province. Typc IX. was discovered on the periphery of the Sultan-
-Ui-,,-I)ar, antl west of it and set up as a province. (With 1 illliqtraa-
tion, 7 Slavic references).
I-Institute of Geology of the -icademy of Science of the ~Lrmt--nian 6SA
(Institut geologicheskikh nauk Akadeinii nauk iriii1i3m)
STRAKHOV, N.11. , Academician, Ibbruary 6, 1957
6.2-1957
Library of Congress
Card 313

BABAY IV)
I I I.------ - -
Hypcrgono.d~; C I : (-,(Ii; ontary rocl~o.
va no.1:131-llil Y'%). (~LA IJ,:10)
(Rocks, Sedimentary)

PALER3KAYA, L.N,,, LOBOVA, Ye.V.; LAVROV, A.P.; RABOCHEV, I.S.; BADAYEV, A.G.;
TRAPE71;IKOV, F.P.; KOSTYUC)ILNKO, V.P.; NOSOV, A.K.
Gr'Lgor.l.'. 1,.lic-h Dolenk,;, a88(-14964; an obituary. Pochvoveden.Ie
Mly 165. (MIRA 18:5)

AKRARKHODMYEV. A.M.; BABAYXV, A.G.; ABDUZJAYEV, Kh.M., daystvitallnvy chlen.
Materials on the lithostratigraphy of cretaceous deposits of northern For-
gana. Dokl.Aff Uz.SSR no.4:9-12 149. (KLRA 6:5)
1. Institut geologii AN U&.SSR (for Akramkhodzhayev, Babayev). 2. Akade-
miya Nauk Uzbekskoy SSR (for Abdullayev). (Fergana--Geology, Stratigra-
phic)

r)
1 7 1
eralma of clog oui Bull') of up-per cretitteolls
Fergan JU.S.S.R.).
Oidd. Viesoyin. Afinmlq. Obihchestra
4ty'.-Syraneoiji Imite of Fcrgan Li
cbayacttrlzcd by the prf'.5ulve of oullilgenit, (dolomite. gyp-
stim" glati"Irlile) and clastik, (q1taTtE, mchochst, t0bite).
inincrak. In addn. flie folloMit'g ne pre-itt: visagnetitc.
i1mcult'." limunite, tourinallsie, gatnrt, amphitw4e, bi
Oduritc pcnninite, clim0lort, apmite, staurolite,
and Tuttle. A. 1'. Kutlohy.-Ar\

I
v
i
lw~-r
,I(,
~~ N

B,TAYF,V, A. G.
ffethod, for studying sedimontary forruitionn and rocks in connection
with 2onality and pariodirity In andiment formations. Tnidy InBt.
gool.AN Uz. SRR no.9:91-108 '53. (MIRA 12:1)
(Rocka, Sedimontary)

DABAYEV, A. G.
"Certain Peculiarities of the Real Compo-Ation of the Cretaceous Deposits of tile
Lo~4er Beaches of the Amu-Darlya" (Sedimentary Foriratiun anI Lithology, Regional
Litholo6y) Dvkl. AN Uzb . SOR No 12, 1953, Pr 13-17 (Uzbekistun resume)
ft~-
1-~31146, 1 Feb 55

PIkIIAi'r;, A. G.
ItTourinaline in the Chalky DeFoo-its of the Lowlands of WeAern Uzbeldstanll
Dokl. M Uz)). SSR, " 19 p1) 25 28 (Uzbek remime)
NO 1 5113
I
The author divides the chalky deposits of Western Uzbekistan into nine
basic types of tourmaline, according to form, size, color, character and
intensity of pleochroism. Each type is described briefly. (RZbGeol, No
1951.)
SO: W-31187, 8 Mar 55

USSRIGeology - Minerals
CArd 1/1 1Vb- 46 - 7/19
Authors vBabayev. A. G., and Akramkhodzhayev. A. M.
Title iCarbonacews rock3 of the Cretaceous period in the Ferg.ansk depression
Periodical IIzvo AN SS.5R. Ser. geol. 3, 109 - 119, May - Jun 1954
Abstraot IThe changes in chemical aM petrographic'composition of carbonaceo-as rocks
of the Crataceous period, discovered at the Forganak depression,are
analyzed. The conditions of furmation of these rocks End their facial
paragenesis are exj,lained. Twelve USSR reference.% (1933 - 1951). Tableal
diagrams.
Institution: .....
Submittedi July 10, 19-53

0
ri Ps Ot 0- V1
i2jr of r. o,~-..-trit2on of 0-,o v-'norrloric: 1 c, o!- t Ion of
oli:n
.5 Ito, of oi&- of I
t.nin vith tjie th-P, :11i--:~otic
tions -nvient sedii-entry atrutiz of thit; rpi-ion, the :tit',.,Dr vrrivev
at the conclusion that meteribl of thp. crc-.1-~ce-,ue de,,ot~its of thz~,
-'~ a]. t,,wai, d- t- 11,11ountFdn R;.ni-(: wi.oz frrmHk~ no'. 1.t:ci 'as o 3f I ic.~n
of --,vr1&r lvyori-, but ~,:its, bicught there 'Iroim otber Dari a ~7
the Ort~tac,wir, eD-Ich the ~'-ultnnuizd"~A- '.:ountin 'jRwnO-,, under ~-ev
1955)
1,3. 681, 7 Oct

BABAYF-V, A.G.
Strntigraphy nnd faclas of Cretacimaus dononitm of the Karshi Step-
pan. Gsol.ebor.(Lvovj no.1:91-107 154. (KLRA 10:1)
1. Tashkent, Inntitut geologii Akademii nauk Uzbekskoy SSR.
(Karshi Steppes-4reolopy, Stratigraphic)

7 fIr-1AYEV 1 .11
Certain Red Colored (Krasnotsvetnyy) Horizons of the Cretaceous in Kyzyl-
kurrV
On the basis of a study of the cretaceous red-colored (Krasnotsvetrlyy)
rocks of KyzylkunV the author concludes the presence among them of deposits
possessing a mirine origin. (RZhOeol, No. 6, 1955) DQkI. AN Uz SSR. No. 7.,
1954, 29-32 (Uzbekistani reswe)
SO: Sum, No. 744, 8 Doc 55 - Supplementary Survey of Soviet Scientific
Abstracts (17)

- -------------- ----------------------- - --
ut I-eriL
a Upper cretaccioas qos ts a
,j-, Tmdy Inji. Aka4. Nowl,
No. 10, ~,-144(1954).,L-]7txl)~tl)itive discuWoll.
U14PI i.tvv- t rogroplik-41 d 1~ tit 10",rchrolcm M.Hol"V

BABAYXV,A.G.
Lithology of Cretaceous deposits Of the Yakkabag region
(Southwestern spurs of the Glesar Range). Trudy Inst.
geol.AN Uz.SSR no.11-64-79 154. (KIRA 8:9)
(Gisear Range-Petrology)

15-1957-3-2629
Translation from: Referativnyy zhurnal, Geologiya, 1957, Nr 3,
p 12 (USSR)
AUTHORS: Vyalov, 0. S., Babayev, A. G.
TITLE: Some Data on the ~taceous and Tertiary Rocks of the
Zeravshan Valley (Nekotoryyo dannyye 0 melovykh i
tretichnykh otlozhoniyakh Zeravshanskoy doliny)
PERIODICAL: Zap. Uzbekist. otd. Vses. milneralog. o-va, 1956, vol 9,
pp 63-75
ABSTRACT* The paper describes sections of Upper Cretaceous rocks
in the Zeravshan River valley at khshikat (TadzhSSR),
near the Stalinabad--Ura-Tyube railroad, and of Upper
Cretaceous-Paleogene rocks at Vishist (middle course of
the Zerayshan River). The Upper Cretaceous rocks con-
sist of marine and lagoonal deposits. In lithology and
environment of deposition they are similar to the-Upper
Cretaceous rocks of Fergana. The Lipper Paleogene rocks
Card 1/2 are chiefly marls and clays, but some limestones and

15-1957-3-2629
Some Data on the Cretaceous and Tertiary Rocks of the Zeravshan
Valley (Cont.)
dolomites are Present Similar rocks occur in the Tadzhil,
depression, especiall; on the northern and northwestern bordei.
Card 2/2 A. V. Go

15-57-12-16790
Translation from: Referativnyy zhurnal, Geologiya, 1957, Nr 12,
pp 13-14 (USSR)
AUTHORS; Babayev, A. G., Suleymanov, I. S.
TITLE: The Upper Cretaceous De osits in the Northern Part of
the Bukhara Depression Nerkhnemelov ye otlozheniya
severnoy chasti Bukharskoy depressiiT
PERIODICAL: Zap. uzbekist. otd. Vses. mineralog. o-va, 1956, Nr 10,
pp 221-239
ABSTRACT: The author investigates the Upper Cretaceous rocks of
the western part of the Bukhar depression, which have
previously been but partially studied. The boundary
between the Upper and Lower Cretaceous series is one
of the most obscure points in the stratigraphy of the
region. The age of the variegated series lying con-
formably between fossiliferous Albian and Cenomanian
Card 1/6 beds has been variously treated. From regional

15-57-12-16790
The Upper Cretaceous Deposits (Cont.)
considerations the author believes that it most likely belongs to
the Cenomanian. A study of the Cenomanian rocks permits them to be
subdivided into zones characterized by different facies environments.
The first of these zones adjoins the Zirabulak-Ziaetdinskiy Mountains;
in this locality the Cenomanian is composed of rocks of the Karaiz
facies, consisting predominantly of poorly sorted conglomerates,
with lenticular structure and sharply varying thickness (from O-5m
to 15 m). Individual horizons of littoral-marine horizons finger
into this unit from the south. One may assume that these zones
represent piedmont alluvial fans, deposited from uplifts bordering
the 8ukhar depression on the north. The Karaiz. facies gives way to
the south to a zone of littoral-marine deposits, in which horizons
with marine fossils are frequently encountered. Still farther south,
the marine formations form a continuous sequence. On the north, the
Cenomanian deposits range in thickness from 0 to 100 m; on the south
they attain a thickness of 350 in. The author divides the Turonian
into two zones on the basis of foraminiferal groups; a zone with
Card 2/6

15-57-12-16790
The Upper Cretaceous Deposits (Cont.)
Gaudryina asiatica belongs to the lower Turonian, a zone with
'ffa-p-dryinella pseudoasiatica to the upper. Marine fossils were
found in rocks of the first zone in all parts of the investigated
region. The lithology of this unit is very constant (gray and green
clays below, clays with layers of sandstone upward); the sandy ma-
terial becomes somewhat more abundant near the Zirabulak-Ziaetdin-
skiy Mountains and consists of shallow-water formations; this zone
gives way gradually northward and southward to the second, composed
of deeper-water deposits. The rocks of the lower Turonian are
characterized by good sorting and by variable mineral content,
though the constitution of the unit is uniform over the entire
i:egion. The upper Turonian rocks are found in the northern part of
the depression and are as widespread as the lower Turonian. They
are sands, sandstones, clays, and rare layers of pebble conglomerr
ates. Coarsely fragmental and red rocks in the foothills of the
Zirabulak-Ziaetdinskiy Mountains are clearly more abundant than
marine deposits, although the facies zonal arrangement is much more
Card 3/6

15-57-12-1679o
The Upper Cretaceous Deposits (Cont.)
weakly expressed in these sediments than in the Cenomanian and lower
Turonian. Tortoise and crocodile bones and plant detritus are found
with marine fossils in rocks of the upper Turonian. Of the fora-
minifers, Gaudryinella pseudoasiatica N. Byk. is the most character-
istic, and, up till now, has been considered a guide fossil to the
Senonian. However, the discovery of this form in association with
upper Turonian pelecypods in Kassan-Tau and other places permits
one to consider that the zone with Gaudryinella pseudoasiatica N.
Byk. includes upper Turonian beds (-aTt-hough it may correspond in
part to the lower Senonian). Mineralogically the deposits are simi-
lar, on the whole, to the rocks of the lower Turonian. They are
characterized by variability along the strike and by a predominance
of fine- and medium-grained well-sorted sands and sandstones.
During upper Turonian time continental and marine conditions of
sedimentation alternated in the northern part of the Bukhar de-
pression. Sands and sandstones are the dominant kinds of rocks
among the Turonian deposits. A study of grain size, chemistry, and
Card 4/6

15-57-12-16790
The Upper Cretaceous Deposits (Cont.)
mineralogy indicates relatively uniform facies in these rocks. This
circumstance, in addition to the wide distribution of various marine
fossils in the razrez (section), points to the deposition of most of
the sediments in a single, broad marine vodoyem (basin). The Tu-
ronian sea was considerably broader than the Cenomanian sea. In the
upper Turonian the sea grew shallow and lagoons developed, but by
the end of the epoch marine conditions had again been re-established.
The greater part of the Cretaceous rocks that are exposed in the
northern part of the Bukhar depression is composed of Senonian
strata, which have not been subdivided into individual formations
because of incomplete study. In the Senonian deposits one should
note the persistance and uniformity in the razrezi'(sections) (the
presence of limestone slabs with rudistids in the upper part,
greenish-gray and green rocks, and the predominance of sand and
sandstones). It is interesting that small clay mudballs occur at
the base of individual horizons and that an increase in glauconite
content is noted in the strata overlying these horizons. This
Card .5/6

The Upper Cretaceous Deposits (Cont.)
15-57-12-16790
relationship points to repeated local erosion. The author furnishes
lists of the species identified in the Senonian rocks. The mineral
content is also described. The Senonian deposits in the northern
part of the Bukhar depression are shallow water littoral-marine
formations. Danian deposits are not pres;nt. iccording to general
considerations, Danian gypsum beds underlie the Bukharaseries in the
steppe zone of the Bukharadepression. The distribution of the
gypsum indicates a regressive sea and the formation of isolated
lagoons. All the formations of the Upper Cretaceous are charac-
terized by an increase in thickness from north to south (except for
the belts along the foothills of the Zirabulak-Ziaetdifiskiye
Mountains).
Card 6/6 V. A. Levitskaya

15-1957-3-3087
Translation fromt Referativnyy zhurnal, Geologiya, 1957, Nr 30
pp 94-95 (USSR)
AUTHOR: '.Zlkkay- em,
TITLE: The Mineral Composition of the Upper Cretaceous
Rocks of Southern Fergana (Mineralogicheskiy
sostav verkhnemelovykh otlozhaniy Yuzhnoy
Fergany)
PERIODICAL: Tr. In-ta geol. An UzSSR, 1956, Nr 12, pp 47-63
ABSTRACT,, The Upper Cretaceous rocks of Fergana were studied
for their mineral content. Syngenetic minara13
found in the light fraction are opal, calcite,
dolomite, glauconite, collophane, and gypsum;
elastic minerals found are quartz, potash feldspar,
plagioclasey muscovite, biotite; and epigenetic
minerals are sericite, chlorite-group minerals,
Card 1A serpentine, kaolinite, and mintmorillonite. In

15-1957-3-3087
The Mineral Composition of the Upper Cretaceous Rocks of
Southern Fergana
the heavy-mineral fraction syngenetic mi'nerals were also
found--pyrite, fluorite, siderite's aragonites barite#
calestite, and anhydrite; elastic minerals--gold, corundumy
hematite, ilmenite$ spinel, picotite, magnetite, rutile,
anatase, brookite, hypersthene, diopside, augite, tremolite,
actinolite, hornblende, glaucophane, garnet-group minerals,
&ndalusite, chiastolite, sillimanite, diathene-1 zol3itep
clinozoisite, epiodta, tourmaline, staurolite, muscovite,
sericitep biotite, sphene, and apatite; and epigenetic
minerals--limonite, leucoxene, malachite, and chlorite-
group minerals. The most noticeable Tluctuation in content
In the different fractions was observed in the ore minerals,
but also in tourmaline, disthene, rutile, epidote, topaz,
garnets several resistant minerals# quartz, and feldspars,
It was discovered that the greatest quantity of the ora
minerals--diathene, rutile, epidote, topaz, feldspars, and
Card 2/3

6
15-1957-3-3087
. The Mineral Composition of the Upper Cretaceous Rocks of
Southern Fergana '*
several resistant minerals--was concentrated in the silt
fraction, whereas garnet, tourmaline, and staurolite were
more abundant in the sand fraction.
G.A.G.
Card 3/3

AUTHOR: BabaLev, A.G.
TITLE% Facies and Geologic History of Western Uzbekistan Durint, the
Cretaceous Period (Fatsii i geologicheskaya istoriya zapad-
ncgo Uzbekistana v melovoy period)
PERIODICAL: Byulleten' Moskovskogo Obshchestva Ispytateley Prirody, Otdel
Geologicheskiy, 1957, No 3, pp 3-31 (USSR)
ABSTRACTt The author considers the history of paleographic changes whic.)l
occurred during the Cretaceous period in the south-eastern
part of Central Asia. Starting from the data of detailed
lithological investigations, the author describes the zon-
ation in distribution of various facies types, shifts of coast
lines, and sequence of changes in direction and scale of oscil-
lational. movements. Three large phases, sufficiently and
distinctly separated from each other, can be singled out in
the history of paleographic changes in Western Uzbekistan
during the Cretaceous period. The first of these phases in-
cludes the Valanginian, Goteriv, Barremian, and partially
Aptian stages. This phase is characterized by the beginning
sagging of the southern regions and the filling-in of de-
pressions, first with continental red-colored facies and then,
Card 112 with lagoon sediments, marine clustic, organogenous sediments

- FABATZV, A.G.
Association of heav7 sedimentar7 minerals and terrigenous mineralogical
provinces of Cretaceous sediments in Uzbekistan. Uzb. gaol* zhure no.4:
55-66 '58. (NIRA 13:2)
l.Institut geologil, AN Usbekskoy SSR.
(Uzbekistan--Mineralog7)

BABATEV, A.G.
series in the profile of Mesozoic deposits
of western Uzbekistan. Dokl. AN Uz. SSR no.8-.9-12 158.
(MIRA 11:9)
I.Institut geologii AN UzSSR. Predstavlano chlenom-korrespondentom
All TJzSSR G.A. Mavlvanovym.
(Uzbekistan-Petroleum geology)

BABAYEV, A.G.
Mesozoic formations in eastern Uzbekistan. Dokl. AN Uz. SSR
no.4:19-23 158. (MIRA 11:6)
I*Institut geologil AN UzSSR. Predstavleno chlenom-korrespondentom
AN UzSSP G.A. Mav2,ranov7m.
Mbokistan-Geology, Stratigraphic)

BL13
!i~
~
Oil and gas yotentials in the plains of western Uzbekistan. Geol.
nefti 2 noe*7:18-25 J1 158. (mm 11:8)
1. Institut geologitUAS USSM
ibakistan-Patroleum geology)
(Uzbekistan-Gas, Natural-Geology)

RTMOY, Oleg Alskanndrovich; BABATEV, A.G., doktor goologo-mineralog.
nauk, otv.red.; CHHRi_TA"M?X71.B'*, red.izd-va; GORIKOVATA,
r, Z,P,, tokhn.red.
Dectonice of Cretaceous and Cenozoic sediments in the Fergana
Valley] Tektonika malovykh i kainozoiskikh otlozhenii For-
ganskoi depregaii. Tashkent, Izd-vo Akad.nauk Uzbekokoi M.
1959. 199 P. (MIRA 13:5)
(Fergana--Geology. Structural)

BABAYZV, A.G.; GABRILIYAN. A.M., prof., doktor heologo-mineral.nauk,
otv.red.; TUHASHVSKATAP B.S., red.lzd-va; GORIKOYATA, Z.F.,
takhn.red.
[Lithology, paleontology, and oil and gas Rotentials of
Gretaceous sediments in western Uzbekistanj Litologiia,
paloogeografiia i neftegazonounost' melovykh otlozhenii
Zapadnogo Uzbekistana. Tashkent, Izd-vo Akad.nauk Us-
bekskoi SSR. 1959. 340 p. (MIRA 1):2)
(Uzbekiatan-Patroleum geology)
(Uzbekistan--Gas, Natural-Geology)

BABAYKV, A.G.; SULEYMANOV, I.S.
Campan sadiments in certain regions of western Uzbekistan. Uzb.
geol. shur. no.1:5(-61 159. (MIRA 12:7)
1.Institut geologii AN UzSSR.
(Uzbekistan--Geology, Stratigraphic)

BABATEV, A.G.: IMIN, Te.V.
Studying the tectonics of western Uzbekistan in connection
with its oil and gas potentials. Uzb.geol.zhur. n0-3:40-43
159. (KIPA 12t12)
1. Institut goologli AN U%SSR.
(Usbekintan--Petroleum geology)
(Uzbekistan--Gas, Natural--Geology)

GABRILOYAN, A.M.; BABAYIV, A.G.
Xvaluating oil and gas potentials of Uzbekistan. Geol. nefti J
gaza 3 n0-9:13-19 S '59. (MIRA 13:1)
I.Inetitut geologii i rasrabotki. goryuchikh iskopayemykh AN SSSR
i Institut geologii AN UzbSSR.
(Uzbekistan--Petroleum geology)
Ozbekistan--Us, Natural--Geology)

BABAV-XV, A.G.
Mesozoic source bads in western Uzbekistan. Geol.nefti i gaza
no..5.-29-33 147 159. (MIRA 1217)
1. Inatitut geologii AN UzbSSR.
(Uxboldstan-Petroleum Mology)
(Uzbeki6tan--Gas, Natural--Geolonr)

AKRAMODZWEV9 Abid M=atovich,-,BA-BAYEV, A.G., doktor geol.-min.nauk,
otv, red,; RUSINOVAg G,I.p rerJ-*-j;--GCrIT'KOVAYAp Z.F., tekhn. 10
red.
[Lithology of oil- and gas-bearing Cretaceous sediments of the
Fergana Valley] Litologiia neftegazonoorifth ralovykh otlozbonii
Ferganskoi depresaii. Tasbkontp Izd-vo Akad. nauk Uzbekskoi SSRp
1960. 430 p. (MIRA 108)
(Fergana--Petroleum geoloF) (Fergana-Gas, Natural-Geology)
Petrology)

BABATBEV, A.G.; PEDOTOV, Yu.A.
Tectonic pattern of the Kara-Kalpak A.S.S.R., as an indicator of
oil arA gas occurrences* Uzb* geolo o-hur. no&5:12-21 16o.
(MIR& 13:11)
1. Institut geologil L razrabotki neft7any1di i gazovykh mesto-
rozhdeniy AN UzSSR.
(Kara-Zalpok-Petroleum geology)
(Kara-Wpak-Gas, Natural-Geology)

IBRAGIMOV, Zarif Sabirovich;,_ _A_.,_G.,_Aqktor geologo-mineral.
naUK, otv.red,; MANSUROV, A.R., red.; GORIKOVATA. Z.P..
takhn.red.
[Physical parameters of Cretaceous and Paleogene oil- and
gas-bearing horizons in Fergana] Fizicheskie parametry nefte-
gazonesnykh gorizontov mela i paloogena Fergany. Tashkent,
Izd-vo Akad.nauk Uzbekskoi SSR, 1960. 130 P.
. (HIRA 13:12)
(Fergana--Petroleum geology)
(Fergsna--Gaa, Natural--Geology)

B.""DAISIX , i"'~ . G , ; -i, - '~ 711' , Y c . V .
Gcolog-'eal :-o.,-ionalization of ~':esozoic oil-and ras-bez-ring-
sedimonts in western Uzbchi~~ti-n. Sov. 9001. 3 no. 12:52-64
1) 16C.. 14;2)
1. Institut Goologii 1.1.* I-,,7L3K.
(t.zbekistLr,-retro1em fcolc-y)
(Uzbckisttn-C,,s, I'atvral-Geology)

GAIRILIYAN, A.M.; BABAYEV, A.G.
Principal geological indications of the Fwasence of petroleum
and gas deposite in Usbekistan. Izv- All SSSR. Ser. geol. 25
no.9:52-60 S 160. (MIRA 13:9)
1. Institut geologii i rasrabotki goryuchikh iskopaye--Wkh
AN BSSR, Moskva.
(Uzbekistan-Petroleum geology)
(Wookistan-Gas, Natural-Geology)

.1. BAUM, A.Q
.
Studying oil and gas potentWs of western Uzbekistan in con-
nection with N.A. Kudriavtsev and N.P. Tuaev's thesis. Uzb.geol.
Alur. no. 1: 79-84-161.
-0 # . (Osbakistan - Petroleum geology)
(Uzbekistan - Gaa, Natural -- Geology)
t 0;~

BABA MUKOVSKIYs L~G.; LEBZIN, Ye.V.; KAYESHv Yu.V.
Types of oil and gas accumulations in regions of western and
southern Uzlekit3tan. Geol. nofti i gaza 5 no. 1t18-25 A 161.
1. Institut geologii i razrabotki neftyanykh i gazovykh
mestorozhdaniy AN UzSSRp i Treat Uzbekneftegazrazvedka.
(Uzbokistan-Petroleum geology)
(Uzbekistan--Gas, Natural--Geology)

BABAYEV, A.G.
More on some -fundamental problems of the genesis of petroleum
and gas and conditions governing the formation of their pools
in Mesozoic sediments of Uzbekistan. Uzb.gool.zhur. 6 no.3:64-72
t62. (MDIA 15:6)
1. Institut geologii i razrabotki neftyanykh i gazovyk-h
meatorozlideniy Art UzSSR~
Nzbekistan- Petroleum geology)
(Uzbekistan,-Gas~ liatural-Geology)

BABATEV, A.G., PARFENOVA, M,S,
Now claosification of limestones. Uzb,.geol.zhur, 6 lio.3:72-77
162. (MIRA 15:6)
1. Institut geologii i razrabotki neftyanykh i gazcvykh
mestoroz)~deniy A17 UzSSR.
(Limestone. -Classif icaticn)

AKRAMKHODZHAYEV, A.M.; FEDOTOV, Yu.A.; MINAKOVA, N.Ye.; IBRAGIMV, Z.S.;
ZHUKOVAv Ye.A.; JXRA)jY,-AG., doktor geol.-miner. nauk, otv.
red.; NURATDINOVA, M.R., red.; HDSHCHENKO, Z.V., red.;
GORIKOVAYA, Z.P.9 tekhn. red.
[Geology and some problem of oil and gas potentials in the Kara-
Kalpak A.S.S.R.]Geologiia i nekotorys voprosy neftegazonosnosti
Karakalpakii. Tashkent., Izd-vo Akad. nauk Uzbekskoi SSR, 1962.
162* pq (MIRA 16:1)
1. Akademiya nauk Uzbekskoy SSR, Tashkent. Institut, geologii i
razrabotki neftyanykh i gazovykh mestorozhdaniy.
(Kara-Kalpak A.S.S.R.-Petroleum geology)
(Kara-Kalpak A.S.S.R.-Gas, Natural-Geology)

BABAYEV, A.G.; STAhOBINETS, I.S.
Conditions governing the formation of oil and natural gas pools
in western Uzbekistan. Sov.geol. 5 no.9:102-112 S 162.
(MIRA 15:11)
1. Institut geologii i razrabotki neftyanykh i gazovykh
mestorozhden4.y AN Uzbekskoy SSR.
(Uzbekistan--Petroleum geology)
(Uzbekistan-Gas, Natural--Geology)

FV
A.KRAKKHODZHAYEV, A.M.; AKIUz',DZIiANOV, M.A.; BF-V A,~-,; BA~AYEV, K.L.;
4L _
'V, N.P.; BAYMUKIW'" V, Kh.fl.; K IN,
BATALOV, A.B.; BASHAYE YMUK ~U~~
K.A.; BORISOV, O,M.; GABRIL'Y,'-X, A.Sh.; GA.RIKWETS, V.G.;
GORIKOVOY, O.P.; GRIGORYANTS, S.V.; IBADULLAYEV, S.I.; ISMAILOV,
M.I.; ISAMUKHAWDOV, I.M.; KAUKHAROV, A.; KENESARIN, N.A.;
KRYLOV, M.M.; KUCHUKOVA. M.S.; LORDKIPANIDZE, L.N.; HAVLYANOV,
G.A.; MOTSOKINA, T.M.; MALAKHOV, A.A.; MIRBABAYEV, M.Yu.;
MIiY.11UDZllIYEV, I.M.; MUSIN, R.A.; NABIYEV, K.A.; PETROV, N.P.;
POPOV) V.I.; PLATONOVA, N.A.; RYZHKOV, O.A.; SAYDALIYEVA, M.S.;
SERGUNIKOVA, 0.1.; SLYADNEV, A.F.; TULYAGANOV, Kh.T.; UKLONSKIY,
A.S.; KHAMRABAYEV, I.Kh.; KHQDZHIBAYEV, N.N.; CHUMAKOV, I.D.;
SHAVLO, S.G.
Khabib Makharnedovich Abdullaev; obituary. Uzb.geol.zhur. 6
no.4:7-9 162. (MIRA 15:9)
(Abdullnev, Khabib Mukhamedovich, 1912-1962)

AKRAMKHODZHAYEV, A.M... red.; UA.P~V ~A.G., doktor geol.-mat. nauk,
red.; RYZHKOV, O.A., doktor geol.-mat. nauk, red.; TULYAGANOV,
Kh.T., red.; ZIIUKOVSKIY, L.G., red.; WASH, O.A., red.;
NURATDINOVA, M., red.1 KARAFAYEVA, Kh.U.9 tekkhn. red.
[Problems of geology, and oil and gas potentials of western
Uzbekistan and the Kara-Kalpak A.S.S.R.]Voprosy geologii i neff-
togazonoanosti Zapadnogo Usbakistana i Karakalpakii; trucV vyead-
noi sesii otdeleniia geologicheskikh nauk AN UzSSR v g. Bukhare.
Tashkent, Izd-vo Akad. nauk Uzbekskoi SSR, 1962. 167 p.
(MIRA 16:4)
1. AkAdemiya nauk Uzbekskoy SSR. Tashkent. Institut geologii. i
razrabotki neftVanykh i gazovykh mestorozhdoniy, 2. Chlen-
korrespondent Akademii nauk Uzbekskoy SSR (for Akrankhodzhayev).
(Uzbeki3tan-Petroleum geology)
(Uzbekistan-Gas, Natural-Geology)

AKRAMKHODZRAYEV, A.M.; BABAMV, A.G.
Twenty-five years of studying oil and gas geology in the Academy
of Sciences of the Uzbek S.S.R. Uzb. gool. zhur. 6 no.6:52-56
162 * (MIRA 16:2)
(Uzbekistan-Petro'leum geology)
(Uzbekietan--Gas, Natural--,Geology)

.BABAYF.V, A-G.- LEBZIN, Ye.V.; SIMONENKO, A. N.; KUSHNIIjov, I.V.;
NUGMANOV, A.Kh., kand. geol.-miner. nauk, otv. red.;
KNNASH, O.A., red.; KARASAYEVA. Kh.U., tekhn. red,
[Bukhara-Khiva oil and gas area; geology, types of oil and
gas occurrences, their distribution and formation] BLikharo-
Khivinskaia neftegazonosnaia oblast'; geologicheskoe stro-
enie, tipy skoplenii nefti i za, zakonomernosti ikh ran-
meshchenlia i formirovaniia. r4] A.G.Babsev i dr. Tashkent,
Izd-vo Akad. nauk UzSSR, 1963. 130 p. (MIRA 16:7)
(Uzbekistan-Petroleum geology)
k'Uzbekistan--Gas, Natural-Geology)

BABMV, AeG.1 LEMINP Ye.V.; SDOMKOO A.H.; KMHMZOV, I.V.
Some geologica.1 am&-tedrodynamic O~Rrftbteiiqti6s- of the fmda-
tion and distributibh of oil and gas fields in vestern
Usbekistan. Geol. nef'V t gaza 7 no,59lo-cl My163.
(MMA 16:6)
1. Institut geologii i razmbotki neftyawkh i gazoVkh mesto-
rozhdaniy AN Usbakskoy SSR.
Uzbekis$an-Petrolem geology)
~Gaa, Natural-Geolog7)

BABAYEV, A.G.; KUSHNIROV, I.V.; LEBZIN, Ye.V.; SIMONENKO, A.N.
Types of oil and gas fields in the Bukhara-Khiva area. Haftegaz.
gaol. o geofiz. no.8:5-11 163. (MIRA 170)
1. Institut geologii i razrabotki neftyanykh i gazovykh
mestorozhdaniy AN Uzbekskoy SSR.

- BABAYEV, A.G.
Current problems in Investipations in the field of petroleum
and natural gas geolon,- in Uzbekistan. Uzb.geol.zhur. 8
rio.3:5-11 164. (','!IRA 18:2-9)

i V A . 6,
Ci=ulative Sands on the Ancient Delta LovInn,'s
4, 1953, 28-36
The formation of smd accinulatiors in the riven reri.-~n occurs ~,r st-Iliniferous
soils (solonchak) vith Lrroiu,.d unters lyinzt- shn-113vly I clov !aId is n-ccomp9nied ty
sandy weathered places taid : crenrial ~ nlophytea th-t hold flic? The ~iuthor
gives the charf i c teri sties of thrcc, types of cu,idiAlve stir(Is bird rott.o their p:)or
ndaptiilllity to I'-,rL,3tr, in comicquonce -)f the atr.)m- o-11nit- of !h, :I,-)AIr,.
SO: 1' 31228, 11 Jan 55

BABAYEVv A.
"In the Turkmenian Geographical Society," Izv. AN Turkm SSR, No 2, 97-98~
1954
A report on the general election of members to the Turkmenian Gleo-
praphieal Society, which took plaoe~bn 2 April 1954. Participants heard
the report of A*P. Lavrov, "Origin of the Clayey Tummeki (Mouncls) of
Southwestern Tu:~kemenla." Discusses problems of organization. (RZhOeoll
No It 1955)
SOs Sum. No. 536, 10 Jun 55

14-57-7-14540
Translation from: Referativn y zhurnal, Geografiya, 1957, Nr 7,
P 39 (USSR~
AUTHOR: Babayev, A.G.
. - --.1'._ -------------
TITLE: Strengthening and Forest Planting of Spnds Along the
Course of the Kara-Kum CRnal (Voprosy zakrepleni a I
obleseniya peskov po trasse Kara-Kumskogo KanaM
PERIODICAL: Ylmy yazg lar. Turkm. univ. Uch. zap. Turkm. un-ta,
1956, Nr ~, pp 221-231
ABSTRACT: The Kara-Kutn canal runs westward for 1000 km from the
Amu-Darya River near the village of BasBaga to the
Archman station. The construction of the canal is
divided into three units. The first unit, which the
author examined in April 1955, runs for 400 km along
the dry bed of the Kelifskiy uzb~oy from the Amu Darya
to the Murgab Oasis, The sandy soils disturbed by this
unit began to fill the canal while it was still under
construction. In the period of strong winds, as much
Card 1/3

14-57-7-14510
Strengthening and Forest Planting of Sands (Cont.)
as 15 percent of the sand which had been removed blew back again
into the bed of the canal. In the course of 400 km the canal passes
throqgh fqur.physical districts: 1) A flat, undulating plain from
the Bajdag~~-K6-jikf c'a*n*'a1" to Chaskakshor Lake . In this
section there*is pracricaiiy no loose sand, due to the fact that the
ground is sufficiently moist to permit the quick growth of a vegeta-
ble cover. 2) the Obruchevkaya Steppe . This is a flat undu-
lating plain covered with small ridges and hillocks of sand and
takyr zones, stretching fromLake Chaskakshor to the area around the
Kara-Tepe kolodets (Well). The ground ismaiftly argillaceous; the
sands are very firm. 3) The-next unit runs from the Well area to
the Zakhmet railroad station, over a distance of approximately 170
km. Here the canal must pass through enormous masses of sand ridges
and hillocks reaching a relative height of 20 m to 25 m. 4) The
final unit runs from the Zakhmet railroad station to the irrigated
lands of the Sakarchaginskiy rayon (District). The canal cuts
through the ancient and modern Murgab River delta. The sands are
Card 2/3

14-57-7-14510
Strengthening and Forest Planting of Sands (Cont.)
quickly covered with vegetation in this area. The author makes the
following recommendations for strengthening and forest planting of
the sands along the canal: 1) natural vegetation should be pre-
served over a belt 2 km to 5 km; 2) sands should be stabilized by
covering them with an asphalt coating; 3) dry grasses and bushes
should be used as mechanical barriers; 4) sand stabilizing vegetaticn
should be sown and planted (this vegetation should be of various
kinds and should consist of trees and bushes of the oasis type and
of halophyte psammophytes, depending upon local conditions).
Card 313 N. G. R.

FA BAY F-V, A . , -- .
.ol
4121.121
.B2
ASHKFABAD OCII',,RK) (Ga,RGRAfiJC OF A.'~!TJIABAD, BY)
A. BABAYEIT (1) 41. FIIF",fKIN, ASHITABAD, TIM1,114SKOYE Gw. in-vo, 1957.
104 P. ILLUS., MAPS9 PLANS, TAUM-S.
FR:-:YKIN, -,:AYdiAR GRIGORIYEVICH JT. AUTH.

BABATEV, A.G..
Mikhail Platonovich Petrov; on his fiftieth birthday. Izv.Voes.
geog.ob-va 89 no.3:264-265 My-Je '57. (MIRA 10:11)
(Petrov, Aleksandr Plntonovich, 1906-

BABA YEV 2. _~..G 6
Conference on the control of soil erosion. Izv. Ali T*&-. SSR. Ser.
biol. nauk no.1;86-87 161. (S(L"WLf (MIRA 14:8)
elk A S', C
1. Institut pochvovadaniya i osvoyeniya peskov AN Turkmenskoy SSR#
(SOIL CONSERUTION)

.1-/I
BABAYLT, A.C.
I M.V.Lomonosov and geographical science. Izv. AN Turk.,SSR. Ser. biol.
nauk no.60-6 161. (~IIRA 15:1)
1 Institut pochvovedeniya i osvoyeniya peekov A14 Turkmenskoy SSR.
?L*ONOSOV; MKHAIL VASILIEVI'jilp 1711-1765) (GEOGRAPHY)

BAHAYEV, A.G.; NOVIKOV, G.S.
International,Oonforence on the Methods of Research in Afforestation.
Izv. AN Turk. SSR. Ser. biol. nauk no.6:98 161. (MIRA 15:1)
1. Institut pochvovedeniya i os 0 ni 9kov AN Tur~--enskoy SSR,
I y! ya pe'
(AFFORISTATION-CONGRESSES)

BABAYEV, A.G.
Physicogeographical zoning in southeastern Turkmenia. Izv. AN
Turk. SSR.Ser. biol. nauk no.2s36-43 162. (MIRA 17:4)
1. Institut pustyn' AN Turkmenskoy SSR.