SCIENTIFIC ABSTRACT VASILYEV, YU.K. - VASILYEV, YU.M.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R001858920016-1
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: August 31, 2001
• Sequence Number: 16
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

NECHAYFV, G.K., kand.tekhn.nauk; V~I41YEV,__Ku.~., kand.teklin.nauk;
BOGAXENKO, I.N., Inzb.; BEREZYUK, B.S., inzh.; SHER14AFEEVICH,
M.G., inzh.
Devices for temperature control in large d.c. machines.
Vest. elektroprom 33 no.11:31-34 N 162. NIRA 15:11)
iBlectric motors, Direct current)
I.- -- -

VASIL'YEV, YU.K.0 PROKOFIYEVI YU.A.
"Step motors with active rotors."
Report submitted to the Second Intl- Congress of the Intl. Federation
of Automativ Controlp Basel, Switzerland 27 Aug- 4 Sep 1963

--VASIL! YEV-5 I Pi. _K,
32514, PaIlTsev.,A. Gi Pialmo V redul4slyu. (Po,povody stqLt*i,V.,V. Tastchina
*Povyaitl urovent takhnicheakojo proyektirovaniya torfyanykh predpriyatly" v zhurn.
"Torf. omm-st'". 1949, No. 6). Torf. -mrr.-stt, 1-r-49, N.. 10, s. 31-32.
SO: Letopis' Zhurnallrorkh Statey, Vol. 44

1. PALITSEV, A. G.: VASILIEV, Yu. K.
2. USSR (600)
4. Peat Industry
7. Twenty years' activity of the State Planning Institute "State Institute
for the Planning of Peat Industry Plants." Torf. prom., 29 no. 12, 1952
9. Monthly List of Russian Accesslins, Library of Congress, March 1953.
unciassiTI-eff.--

VASILIYNV, Yu.K.
(Preparation of peat fields for extraction] Podgotovka torfianykh mestorozh-
denii k ekspluatataii. Moskva, Gos.energ.izd-vo, 1953. 55 P.
(KIM, 6:7)
(Peat industry)

IMONOV, V.Ya., kand.tekhn.nauk; BEZZLTBOV, N.D., kand.teklm.nouk; BELCKO-
MOT, I.Ye., kand.sellskokhoz.nauk; BLTUMMM, V.V., kand.tekhn.
nauk; BOGDAIJOV, N.N.. kand.tekhn.nauk; BRAGIN, N.A., inzh.; VASILI M,
Tu.K., inzh.; VINOGRADOV, V.A., lnzh.; ROZMIBM, B.I.. inzh.; GOR-
GIDZHANTAN, S.A., kand.tekhn.nauk; ZIZA, A.A., kand.seltakokhoz.nauk;
X&LkB=OV, N.V., agronom-meliorstor; KOLOTUSHKIN, V.I., inzh.; KORCHU-
NOV, B.S., kand.tekhn.nauk; KRYUKOV, M.N., doteent; VAVULO, V.A., inzh.;
RAUMOV, D.K.. kand.tekhn.nauk; OLKNIN, A.S., inzh.; PROVMKIN. A.S.,
insh.; PROKHOROV, N.I., dotsont; RASKIN, G.I., lnzh.-. SAVMO, I.V..
inzh.; SXRGZTZV, B.F., kand.tekhn.nauk; STOYLIK, N.A., iazh.; SUKHA-
NOV, M.A,, inzh.; TOPCLONITSKIT, N.M., kand.tekhn.nauk,- TYURWOV, S.N.,
doktor biol.nauk, prof.; FATCHIKHINA, O.Ye., kand.sellskokhoz.nauk;
TSYMOV, B.I., inzh.; CHUBAROV, N.D., inzh.; KAIMMIBAUM, A.I.. inzh.;
(Continued on next card)

ANTONOV. V.Ta.-(continued) Card 4'.
TA SN, A.K.; SJWSONOV, N.N., inzh., glavnvy red.; BIRSHADSKIT,
L.S., inzh., nauchnyy red.; VARENTSOV, V.S., kand.tekhn.nauk, na-
uchnyy red.; VTSOTSKIT, X.P., kand.takhn.nauk, nauchn7y red.; GO-
RINSHTM, L.L., kand.tekhn.nauk, nauchnyy red.; GORTACHKIN, T.G..
prof., nauchnyy red.; YEFIKOV, P.N., kand.tektm.aauk, nauchnyy red.;
KUZEWAN, G.I., kand.takhn.nauks nauchnyy red.; KULAKOV, H.S., kand.
takhn.nauk, nauchnyy red.; KWAIS, L.J., prof., doktor tekhn.nauk#
nauabny7 red.; HIRKIN, M.A.. inzh.. neuchnyy red.; SZMSKIY, Ye.r.,
kand.takhn.nauk, nauahnyy red.; SOKOLOV, A.A., kand.takhn.nauk,
nauohnyy red.; KHAZANOV, U.N., doteent, iiauohnyy red.; KHALUGO,
A~X~, Inxh., nauchnyy red.; TSUPROY, S.A., dotsent, nauohnyy red.;
SHIAMOK, G*D,, inzh., naucbnyy red.; XCLOTUSUIN, V.I., red.;
GUORTSOV, I.M., takhn.red.
(Reference book on peat] Spravochnik po torfu. Koskva, Gos.energ.
izd-vo, 1954. 728 P. (MIRA 13:7)
1. Chlon-korrespondent AN BSSR (for Goryachkin).
(Peat-Handbooks, manuals, etc.)

13AUSiN, A.F.;~~SOKOLOV, A.A.; AIMONOV, V.Ta.; KUMMMY. S.Y.; BHLIKMVICH,
P.I.; SAYINM, A.T.; KARAKIN, F.F.; SOMPOY, S.G.; THFIHOV, V.S.;
TARIVITSIA, V.I.; WKIN, B.A.; BABARIN, A.F.; MMSIM. L.M.;
FUNI)a)V,S.A.; CHMNENKOV, D.P.; BULAYWSKIT, N.Y.; kandidat tekhni-
chookikh nauk: S11TIMARINK, K.K.: TSUPROV, S.A.; GINZIAJRG, L.N.;
VASTL'TV,V, Tu.K.
Scientific and technical conference on the work of the DoOt Industry
of the Ministry of Electric Power Stations. Torf.prom. 32 no.2:1-20
'55. (MLRA 8:5)
1. Zamestitall ministra alaktrostantaiy (for Bausin). 2. Zamostital'
direktora VNIITP (for Sokolov). 3. Zameatitell direktora MTI (for
Antonov. 4.Zameatitall direktor "Ikrnilmesttopprom"(for Kurdywov).
5. Dirmktor Inatituta torfa AN BSSR(for Bmllkevich). 6. fiachal'aik
Glavexergompehasti MES(for Savimykh). 7. Glavin iazhex"r Ivatovokp
go torfetresta (f*r Xarsk1n). 8. Zamostitell direktora MTI (for Soli
pov) 9. Upravlyayushchiy Shaturskogo torfotresta (for.Tefimov). 10.
GlavW mekhanik Invanosvkogo torfotresta (for Tarovitsin). 11.
Gl&vYWv mekhanik Leningradskogn torfotreata (for Rabkim). 12. Glavvyy
insboner Ozerstoko-HoplyWavokogo torfoprodpriyatiya (for Babariz).
13. Gl"Wy inzhmnAr Gar'lovskogo torfotresta (for Matvayev). 14 Ra-
kovoditell laboratarti VNIITP (for Zinlknv). 15. GlavM7 inzhoner
treat& Lmatorfontroy (for Chernankov).
(Continued an next card)

VASILIYBV, Tu,K,
Winning and utilization of peat In Scotlamd. Torf.prom.33 no.3:
32-33 '56. (MIRA 9: 7)
I.Giprotorf. (Scotland--Psat)

JASILOYEV- 1-6- lnzh., red.; PEVZNFR, A.S., red.izd-va; GUSEVA, S.S.,
t-elam. red.
(Reference book on consolidated cost indices for planning and
research) Spravochnik ukrupnennykh pokazatelei stoimosti pro-
ektnykh i izyskateltakikh rabot. Vvoditsia v deistvie a 1 ianvaria
1938 g. Moskva, Gos.izd-vo lit-ry po Btroit. i arkhit. Pt.11.
(Enterprises of peat industry] Predpriiatiia torfianoi pro-
myshlennosti. 1957. 8 P.- (MIRA 12:8)
Ruo:ia (1923- U.S GosudarBtvannyy komitet po delam
roit Pstva,
(Peat induatry-Costs)

VASILITZV, Tu.K,, inzh.
Develop the winning of peat in the Ural Mmintains and in Western
Siberia. Torf. prom- 35 no.5:21-22 '58. (MIRA 11:10)
I.Gosudaretvenny7 institut po proyektirovaniyu zavodov torfyanoy
promyshlonnosti. (Ural Mountain region--Peat)
(Siberia, Western--Pent)

VASILIYEV, Tu.K.., kand.tokhn.nauk; BOGAYWO., I.N.j, insh.
Stu4y of thermal condtions in the operation of heavy rolling mill
Vestoelektroprom. 33 nool2t32-35 D 162, (MIn 15d2)
Miling

.- VASILIY3?V, Yu.K.
New desiga of supports for bani conveyera. Hashinostroitell no.12:
17 D 160. (Conve7ing machiner7) OCMA 13: 12 )

-- -- I - --
-/ ~l I I - ~ ~ - .. - -- -
1~ . ~ I - - . - -

AUTAHOR: V -a s i 1 ',yc vY uC a-n c i d: t e of T e c I I n --* c a 1 A'J c -' c-.-. c e F,
TITlE: Thermal Tests on Hi h-power Alternat-~.n6 Current Lotlors
under OperatinE Conditions (Teplovyye ispytaniya moshchr."11.
elelctrodvi6ateley peremennoEo tokc v usloviyalech
atsil)
PERICDICAL: Vestnik Mashinostroyeniya, 1953, Vol-2c) .1o.3
pp. 36 - 39 ~USSR)'
ABSTPA'T: The article describes wort;~ carvied out by staff of
Kiyev Pol technical Institute (Kiyevskiy politekhnich,eskily
ir-stitut5l of the Central Asian Polytechnical Institute
(S-redne-Aziatski,y politekhnicheskiy institut) and of factories
under the leadership of ProE T.1.1. Postnikov. Electrical,
thermal, ventilatin_- and a ..,u-(Tiber of special tests were LfC"e
o.a dozens of motors; the article describes sore t1--ermal
tests axid calculations.
The object of the theri-n-lal tests was: to establi~;h ... hether
the motors confar.1ned to the standards for temperature rise;
to reveal power reserves in respect of teraperature rise; to
establish the hi-.-he,~t ;-,,ermissible stator and rotor currents
de~%endin- on the am~bicnt temperature; to determine the
b
heatinC ti-ue constants or different parts of the mach*
dne; to
det.-rmine the teLTperature distribution in the stator; to
Uardl/4

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-12/4

1-7-o' -er
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110-3-?/22
Thermal Tests on High-power Alternatiruc~ Current Motors under Opera-
ting Conditions
should indicate the permissible current at various ambient
temperatures. The diffarence between the mean and
temperatures can be 10 C or iaore. It was often found ';-.hat
hot air leaving the ~aiachine re-entered it; machines should
be designed in such a way that this catnot occur. In ~;o.me
cases, inadequate provision is made for cooling the end
windings. Many motors get very dirty in service and should
be made with a closed ventilation system.
There are 2 figures, 1 table.
ASSOCIATION: KiyevPolytechnical Institute (Kiyevskiy politekh-
nicheskiy institut)
AVAILABLE: Library of Congress
Card 4/4 1. Eleotrio mcytors-Test methods 2a k;lectric motors-Test results
3. Bleotrio motors-Thermal effeotB

VASIL'YEV., Yu.K.J. kand. tekhn. nauk; KARPENKO, B.K., kand. tekhn. nauk;
KRAVTSOV, O.K., inzh.; MURASHY-0, V.A., inzh.; IVAROVA, I.G., inzh.
Direct current motor with printed armature winding.
Energ. i elektrotekh. prom. no.1:25-28 Ja-Mr'64. (MIRA 17:5)

Yll.K., kancl.ti~,~hri.ria!ik; DOGAYFINFO, 1.N., InZh.
Operational test3 of the Oo5liDg of (-:.
Elektrctekhni~,a 35 lAr 164. -u. -~ - ~ Z'~

L 10228-66 EWT(1)
- _AKDOMOB _COOZ:
I XCC NR% sloljA~i
AUTHOR i 'Vasil 1yev, Yu. Ko (Candidate of technical scien"s; Kiev)
ORG: none
TITIE; Thermal calculation of geared stepping motors
SOURCEi Elektrichostvo, no. 10, 1964, 20-23
TOPIC TAGSt electric motor, electric engineering
ABSTRACT: The motor analyzed In this paper Is an encased four-phase motor,,
which contains a reactive toothed rotor and a stator having GQht slots &M.
elGbt toothed pole-plooes. Each slot bas a two-layer lumped control wind"'
Ing. ldhen the motor is runnirg, two phases are always energized. r1wo
.sections of eacb phase are located In oppoQIte slots. A aross-section of
.the motor Is shown in the figure, in which the bold lines Indicate the
windings energized at a given Instant. The motor heats up nonuniformly
when the motor is stopped and the same set of phase windings are drawing
current# With respect to heating, this is the least favorable mode of
operation, and must be.) considered In designing such motors. rMe funda-
mental assumptions jwAo for encased motors are the usual ones with re-
gard to beat dissipation, teoperature distribution, and heat transfer*
'Equivalent circuits are shown for the motor and are used to compute temp-
eratures* To simplify computations the equivalent circuits Is divided
I CG!jd :kL2 UDCs 621.31 e1 .4
y-,

L 10228-66
I ACC NR, Ap6owhN
In%o Me parts In Whiab therml process are identioale ftiststionary
-temperatures are eomputed by treating the motor as a %vwo-jWt IyS%GMI
the casing and mechanical parts as a heat sink and the rout of the. motor
as a heat source& A detailed numerical example of calculations is given mid it is
shown that these results compare wel.1 with the theory. Orig. &A* has: 6 figures,
17 f ormulas 9 Cim-7
SUB COOSt 09 SUBX DAM 09PAy& CRIG REFs 005
'4 ~1~

kand.tekhn.nauk; PROKOFITEV, Yu.A.,ksnd.tekhn.nauk;
RYBAL'CftFNKO, Yu.I., irzh.; LARCHENKO, V.I., inzh.
Stepping reducer motors and semigraphical method for their
design. Elektrotekhnika 36 no.12:11-16 D 165. (MIRA 19:1)

VASILITEV,,,TW,,X.,, kand. takhn. nauk, doteent (Kipv)
Preciso thermal design of a single-row excitation winding. Ilektri-
ahestvo no,609-45 Je 165. (MIRA 180)

VASILOYES, Yu.K., kand. tekhn. nauk (Kiyev)
Thermal desigr. of rF~du-:~ef-tzpe stepping motorn.
no,10;20-23 0 1641. (M:RA 17:12)
I- - - -,

VASILSYEV, YU.K. kand. tekhn. nauk (Kiyev); MEMO, I.N., inz)1.
~(Kiyev~
Experimental study of the beating and ventilation of the
traction motors of main-line electric locomotives. Elektri-
chestvo no.2:32-37 F 164. (MIM 17: 3)
1. . . 1. :". ~~, : Ij .- I -.'
" - - , . . : _ -!~ -Q-1

I
VASILIYEV, Yu.K., kand.tekhn.nauk; PROKCFIYEV, Yu~A., kand.tekhn.nauk;
VAYNBERGER, G.Ya., inzh.
Stepping motors with active rotors. Elektrichestvo no.2:50-56
F 163. (MA 16:5)
1. Institut Artomatiki Gosplana UkrSSR.
(%Wtric motors, Synchronous)

VASILIYEV, Yu.K.,_inzh.
Wooden rollers f?r belt conveyers. StroiA dor.manhinos~.r- 5
no-7:25-27 Jl 60. (MIRA 13:7)
(Conveying machinery)

Do%1,
7 "C 4
A" Cal)

S/56:2/62/000/008/013/013
D405/1501
AUTHOR: Vaaillyev
L_J__Y1X I-L -(Novosibirsk)
TITLE: Close packed non-group codes
SOURCE: Problemy kibernetiki. no. 8, Moscow, 19062, 337-339
TEXT: A method for construction of close-packed (n,3)-codes is
proposed. Unlike similar methods (considered in the references) it
yields not only group codes, but also stronglynon-group codes
(a strongly non-group code is a code which is neither a group code
nor a group-code shift). This means that the question whether
strongly non-group code* exist is answered in the affirmative..'A
lower estimate is given of the ratio of the number of tyyes of
strongly. non-group (n,3)-codes -to the number of all (n,3 -codes.
This eat imate is expressedby the number
2
2
,Card 1/2

S/5E 62/000/008/013/013
Close'packed non-group codes D405%301
The- strongly non-group code is constructed with the help of a the-
orem. Several other estimates are derived. Since each (2p + 193)-
up code is completely determined by its 6:enerating functions,
ro 11
g
whose number does not exceed 2p, it follows that the number of
2
(2p 1,3) -group codes does not exceed C 2P2p 1 25P
2
SUB14ITTED: -November 13,1961~.
Card 2/2

32823
7 Z) c) D S/02o/62/142/002/'001/029
C111 C222
AUTHORs Vasilly
TITLE: Irreducible disjunctive normal forms for certain classes
of trath functions
PERIODIM; Akademiya nauk SSSR. Doklady, v. 142, no. 2, 1962,
263-265
TEXTs The author examines the relationship between the complexity
of an arbitrary irreducible disjunctive normal form (d.n-f)(Ref- 1:
S. V. Yablonskiy, Tr. Matem. inst, im. V. A. Steklova AN SSSR, 51, 5
(1958)) and the minimal d.n.f. of the fun~;tion f, taking into con-
sideration dim f (dim f ---the maximal dimenq'ons of ouch Bubcubes of
the unit-cube, for which fO'g-, Xn)
To estimate to what extent the complexity of an irreducible d,n.f.
is larger than the complexity of the minimal d.n.f. Y(f) = max
[I(T,)/I(T 2)] is introduced, where the maximum. extends over all pairs
of irreducible d.n.f. T,, T2 of the furiction f; I(T), I(T2 ) denote
the number of conjunctives in these d.n,,f.s. One has Y(f)t-- 2dim f
Card 1/3

32823
S102016211421002,10011029
Irreducible disjanctive normal C 1 1/ C 2 2 2
and Y(f) - 2 dim f only for functions w i th d f - 0.
,dim f
The author examines to what extent the estimat~j Y(")N,--- ~ is
sharp. Let D(n) be an integ-ra! func tion, 0 :!S D(n) -::~-n; let V D~n)
denote the class of functiona f( X ) for which dim f ts D n);
n
Y(A D(n)) = max Y(f)
f F- IX D(n)
Theorem; For each integral functJon Z(n), 0 !!f LZ (n) 10 n, a function
D(n) and a class '~'D(n) can be given, so that D(n) -, ZZ (n) and
Y( K(n)) -V 2D(n) . III the proof, th#~ ituthor :.,oi,s:.der8 fir.'t 11super-
positions" of irreducible d.n.f., then powers of so called support-
functions and, on this basis. con3tructs functions f II(xi'..., X n),
for which Y(f n) -42 dim 'n wheAfn --) ju , and diEl f V increases with n,
for instance, dim f n > n - Ln/k] , whore k arid, ju indupendant of n.
Card 2/3

32823
S10201621142100210011029
Irreducible disjunctive normal . . . C',11/IC222
There are 3 Soviet-bloc references.
ASSOCIATIONt Institut matematiki a -7ychislitellnym teentrom Sibirskogo
otdeleniya Akademii nauk SSSR (Inbtitute of Mathematics
with Computing Center of the Siberiftn Department of
the Academy of Scienes USSR)
PRESENTEDs August 12, 1961, by S. L. Soboley, Acudemioiaii
SUBMITTED: August 10, 1961
Card 3/3

-VASILIYEVp Yu.L. (Novosibirsk)
Ungrouped tightly packed codes. Probl.kib. no.8:337-340 162,
(KMA 1614)
(Information theory)

WILI-YLV, Yu. L.
Dissertation defended for the degree of Candidate of Physic,matlieilatical 3ciences
at the Joint Scientific Council on Physicumathematical. and Technical 3ciances;
Siberian Branch
"Comparison of the Complexity of .4inimal. and cul-de-3ac Disjunctive Normal Form.,'
Vestnik Akad. Nauk, No. 4, 1963, pp ~-19-145

VASILIYEV, Yu.L.
Length of a cycle in an n-dimensional unit cube. Dokl.AN SM
148 no.4s753-756 F 163. (KIRA 16:4)
1. Institut matematiki Sibirskogo otdeleniya AN SSSR.
Predstavleno akademi-kom S.L.Sobolevym. Dokl.AN SSSR 148 no.4s
753-756 F f63. (MIRA 1624)
1. Institut matematiki Sibirskogo otdeleniya AN SSSR.
Predstavleno akademikom S.L.Sobolevym.
(Cybernetics)

Acussw NR-. AT4016486 8/2582/63/000/010/0005/0061
AUTHOR: 1L4-6WMY,-XU,-L, (Novosibirsk)
TITLE: A comparison of the complexity of blind and minimal disjunctive normal
forms
SOURCE: Problemy* kibernetiki, no. 10, 1963, 6-61
TOPIC TAGS: cybernetics, automation, control system, automatic control, disjunctive
i normal form, circuit design, localness, equivalence, monotonicity, error correction
ABSTRACT: The author first defines what fig meant by the complexity of the disjunctive
normal form (d. n. f.). The concept of "almost minimal" d. n. f. is then discussed, along
I with the algorithmic difficulties encountered In the synthesis of minimd circuits (the d. n. f.
Is considered as a control sysiem circuit, whose operation is describedby the corresponding
function of the algebra of logic). It Is pointed out that In tho d.n.f. theory many synthesis
algorithms are known, all of which give d. a. f. which might be considered "Bufficiently i
simple", the essential point being that this 11sufficienc I
_V1 of simplicity Is not of a metric
(digital) nature, but of a descriptive nature, connected with a certainnatural, partial
I ordered state of the d. u. f The present paper seeks to derive some estimates in response!
.1/4

ACCESSION NR: AT4016486
to the question: what is the difference between the complexity of "sufficiently simple"
and minimal d.n.f.? For a clearer exposition of the problem, the author reviews the
basic Information with respect to d.n.f., drawing heavily on the work of S. V. Yablonskly.!
The terms I'localness", "equivalence" and I'monotonicity" are discussed and defined. A
d. n. f. T Is called "blind" (a term introduced by Yablonsidy) if the cancellation of any
disjunctive term or any factor In any disjunctive term transforms T Into d. n. f. T*, non-
-equivalent to T. A minimal d. n. f. to blind, but a blind d. n. f. may or may not be
minimal. In practice, as a "wdfictently simple" d.n.f., one takes an arbitrary blind
d.n.f. for a given function f. It to pointed out that the construction of any one blind d.n f
for a given function f . It Is pointed out that the construction of any one blind d. n. f. for
function Is a relatively uncomplex matter. The author usea the term "spread" for an ar-
bitrary function f and the nomenclature R(f) for the ratio of the complexity of the ation f,
maximal d. n. f . of function f to the complexity of Its minimal d. a. f. (for any func
the multiplicity of all its blind d. n. f. is finite; the blind d. n. f. having the greatest
complexity Is called the maximal d.n.f. of function f). Ile purpose of this work Is to
obtain estimates for R(n) = max R(f), where the maximum is taken for all f of n variables,,
aswell as estimatea of R(f) for Individual functions f . Iluo, the paper seeks to investigate
-2/4
Card- -

ACCESSION NR: AT4016486
the difficultles encountered at different Individual stages In the synthesis of minimal d. n. f.
and to give metric (digital) estimates. Ile methods developed in this article have been
found to be applicable to certain other problems as well, relating to the construction of
functions, In which one or another of the metric propertlea are extremal and which, at
first glance, have little in common with the comparison of the complexity of blind and
minimal d.n.f. In this way, on the one hand, certain new facts and estimations have been
derived In the theory of errpr- correcting codes and, on the other, there has been co
st~vcted in an n-dimensiondl unit cube a cycle in which the length equals Zn for n - 2
n
m 3, 4. and not less thip a n) 2 1 for arbitrary n, n ># 3, e -P 0 when n
n
n
All the basic results were obtained in the study of amther digital characteristic of the
functions - the eccentricity Y(f) - rather than directly of R(Q. The transition to esUma-
tions for R Is made only toward lltfke~end of the paper. The author makes the point that
whatever synthesis algorithm is obtained as "sufficiently simple". It Is not excluded that it
may be found to be not only not the minimal, but even the maximal d. n. f . of the function f.
7bus, comparison of the complexity of these d. M. bears cc a wide class of synthesis algor-
ithms of "sufficiently simple" d.n..f. The work is devided late 10 sections: 1 - introduction;.
W4
C',
r4

ACCESSION NR: AT4016486
2- general part; 3 -theorem concerning the "superposition" of blind d.n.f.; 4-estimate
of Y(n); 5 - theorem of splitting; 6 - relation between eccentricity and uniformity of
functions (first step); 7 - relation between eccentricity and uniformity of functions (second
step); 8 - constructidn of reference sequence; 9 - estimates for R; 10 - some other appli-
cations of the theorem of Bpllttings. Each section Is provided with a brief introductory
statement. A diagram illustrating the Interrelation of the individual sections 18 also pro-
vided in the section entitled "Introduction!'. Orig. art. has: 3 tables, numerous equations 1
and 6 figures.
ASSOCIATION: none
SUBMITTED: 31JulG2 ENCL: 00
SUB CODE: IE, MA NO REF SOV,. 016 OTHER: 008
4/4
Card

VASILIYEV, Yu.L. (Novosibirsk)
1%
Comparison of the complexity of dead-end and mlni:~--_l d"-s.unctive
normal forms. Probl. kib. no.10:5-6 163.
(MIRA 38:1.)

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" S up c r,,. .~ i,, 1. '1--' - on l' -i E-, ,~ i Y'.-I , i -; ~, !'I" ri ') rra 1f 11 -
- I I - - I .:; .; , ", ( .
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VASILITEV, Yu,.M.
Stratigraphy of the upper Cretaceous on the BU2achi Peninsula
based on Foraminifera. lzv.vyo.ucheb.zav.; geolA razv. 2
no.4:57-67 Ap 159. (MIR& 12:12)
1. Moskovskiy institut neftakhimichookoy I gazovoy promV-
shlennosti im. akademiks I.M.Gubkina.
(Busachl Penizwula-GeologV, Stratigraphic)
(Foraminifera, Fossil)

15-1957-12-17005
Translation from: Referativnyy zhurnal, Geologiya, 1957, Nr 12,
p 44 (USSR)
AUTHOR: Vasillyev, Yu. M.
TIME: YoungTe~ctoni"cMov-ements in Northern -Caspian
Region' (14olodyye tektonicheskiye dvizheniya v Severnom
Prikaspii)
PERIODICAL: Tr. Mosk. nef t. in-ta, 1955, Nr 14, pp 3-11
ABSTRACT: Bibliographical entry
Card 1/1

CHARTGIN, M.M.; VASILIYZV, Yu.M.
Oil prospezting in the Zmba. region, based on facies and thicknesses
of Mesozoic sediments. Geol.nefti 2 no.9:37-144 S '58. (MIRA 11:10)
l.Moskovski7 ordena Trudovogo Kraenogo Znameni neftyanoy institut
im. akademika I.M. Gubkina.
(Xazakhatan--Petroleum gpolog7)

VASILOYEV, Yu.M.; KAZAKOV, M.P,; CHARYGIIT, M.M.
Gas and oil potentials of the northern Caspian Sea region.
Izvovyseuchebezave; neft' i gaz. no-7:3-9 '58'-' (MMA 11:11)
1. Koskovskiy neftyancy institut im. akad. I,M,Gubkina.
(Caspian Son regiov--Petroleum geology)
(Caspian Sea region--Gas, Natural--Geology)

A U 1' 0 7 " S' C 1 T
2 Y u 2 2
TITLE: 'low Data Sl-rrr,,ti )hy of t -,c,. Pal e
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of Penins!liu (Nov.-.yc d un.~ y y epo

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IT ew D--' a Con cer.:L~ t'.-e S-, e r,
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v a r i e s ;_ ae en 0 an d 3 5 r, - "L st r- -.p h i c
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ou L - _.: - -;ere of t'he BU~Lachi perl-
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PetrrZleum institate imeW. I. M. Gubkin
S7'- ':7 '-'T:LD
Card 31 4

Tv I
VA~iL ~E_V
" (4) 1?K4M I BOOK F.19WITATION SOV/1492
Moscow. Neftyanoy institut
Voprosy geologii i dobychJ. nefti (Problems in Geology and Oil Production)
Moscow, Gostoptekhizdat, 1958. 282 p. (Series: Its: Trudy, vyp. 22)
1,300 copies printed.
Exec. Ed.: G.F. Morgunova; Tbch. Ed.: A.S. Polosina; Editorial Board: K.F.
Zhigach, Professor (Fe.-sp. Ed. ); I.M. Mux-avlyev, Professor; A.A. Tikhomirov,
Candidate of Economical Sciences; V.I. Yegorov, Cand1date of Economical
Sciences; M.M. CharygLa, Professor; F.F. Danayev, Professor; N.I. Chernozhukov,
Professor; Ye.M. Kuzm3.k, Professor; I.A. Charnyy, Professor; G.M. Panchenkov,
Professor; V.N. Dakhnov, Professor; N.S. Nametkin, Doctor of Chemical Sciences;
N.A. Almazov, Docent; V.N. Vinogradov, Candidate of 7.1echnical Sciences; V.I.
Biryukov, Candidate of 13echnical Sciences; E.I. Tagiyev, Professor; V.M.
Gurevich.
PLWOSR: This book is Intended for technical personnel in the oil and gas in-
dustries, as well as for instructors and advanced students in petroleum
Card 1/ -5

Problems in Geology end Oil Products SOV/1492
engineering institutes.
COVERAGE: This collection of articles, written by members of the teaching staff
of the Moscow Petroleum Institute imeni I.M. Gubkina, is devoted to a discus-
sion of the geology and prod-action of petroleum, particularly as it applies
to the Stalingradskoye Povr)lzhlye., the Fredlavkazlye, and the. Southeastern
part of the Rassian Platform. The articles include reports on studies in
hydrogeology and geophysics, a discussion of problem3 in directional drilling,
and a review of the methodology of oil displacement. (dislodging ) in porous
media through water drive. The articles are accompaaied by diagrams, graphs,
tables, and bibliographic references.
TAMZ OF CONTKUS:
Florenskiy, V.P. (Deceased), T.A. lapinakaya, and V.S. "zev. Petrography of
the Stalingradskoe Povolzhlye Crystalline Basement 3
Kazakov, M.P., Y~i.M. Vasil'yev and V.L. Shirokov. Developmnt of the Frin-
ciplea of 11!~_C' zlye and the Southern Periphery of the Rm-
sian Platform 29
Bykov, R.I. Certain Characteristics in the Development of the Southeastern
Card 2/'5

Problems in Geology ard Oil Products SOV1492
Part of the Russian Flatfzzm in. Sakmarsko-Arti--akoye Times (Imwer
Perrd"I 63
Yedrenkin, S.S. Oil and Gas-bearing Potential of -the Stavropol' Area 78
Kartsev, A.A. Classification of Rydrogeological L-Aices in Evaluating
012 and Gas Potential 91
Baskov., Ye.A., and V.P. Shutgrin. Comparison of the Analyses of Dissolved
Gases Extracted by Different Methods 98
Zhdanov, M.A., and G.T. Yadin. Factors in the Ratio of Gas Recovery From
Gas or Oi.1-Gas Deposits
Vendel'shteyn, B. Yu.- Relation Betwesea the Parameters of A Double Faectri-
oal lAyer on the Sarface of Rock Particles and the Diffusion-adsorbtion
Blectrowtive Force 115
Card 3/5

Problems in Geology and Oil Prod-mets BOV1492
Dobrwin, v.m.. Elements in the Mwory of a Potential Field for Induced
Polarization in Boreholes 1;26
Nosheleva.. I.M., and M.M. Muakov. Yethodology of the Study of Oil Disp3ace-
=nt by Water in a Porous Wdium. 142
Koebeleva, X.M., M. N. M%sakav. Displacement of Matually Soluble
Vjd,rocarbons in a Purous &dium 158
Masakov, M.M., and I.M. Moshelava. Effect of Capillary Forces on Rydro-
wbon Liquid Displacewnt in a Rydrophilic Fbivas Medium by Water 170
Misakov, M.M., and I.M. Kosheleva. Displacement of Oil by Water in a Hydro-
phobic Porous Medium 181
Masakov, M.M., and Sh. K. Gimatxkiinov. Capillary Displacement of Oil by
Water From Natural Cores 19B
card 4/5

Problems in Geology and Oil I'l-,Aucts SOV/1492
Gimatudinov ** Sh.K., and M.M. Khmkov. Effect of the Velocity of Displacement
of Oil by Water in Natuxal, Cores on Oil Recovery 207
Govorova, G.L., and M.A. Gusayn-Zade. Simplified Formulas for Computing
the Well Output 217
Uhrikhin, I.D. Effect of the Free Volumes of a Borehole on Pressure
Ih3J 1 d -up Curve s 231
Rw Shang-ping. Computing the ant-pe. of a Well With a Fractuxe Close to
the Productive Horizon 245
Belorussov, V.0. Directional Well-drilling by Well Bottom Variable Three-
Dimensional Coordinates 254
Simonov, V. V. A StuAy of the Yiow of Solutions Th=4~h Flushing Channels
of Hock Bits 270
AVAIIABIZ: Iibrary of Congress
Card 5/5
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5-8-59

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arid TuTpper 1~~_Iazar beds. I:1_ all staL;os are
Card 215 about 15-13 m t1dek. Tl_-,~ follo-AnL; -eolo-istc

2he ~Uatcrral:~-,' Dop),-;i t o c)
0-ion.
are
Yc--V- Ohant~;,:!r V.I.
la-ev,
G D c,
V.P. -,oc V.
I. -17vi 4L
lftcyova,
31-d.yl ai-.1 E. P.
are
1,CfererLoer'.
A 32 0 1 -'l T 10 ! 7
S3SR (2ho C-ocjoL;j3
Stitute of t-
"le
,lj!,-ust 2o 19 r-,-
"lard 313

A UTHOR Vasiliyev, Yu.11% '10V/11-58-12-11/1=
TITLE: On the Appearance of Trpces of Permafrost Processes in the
Ct'uaternnry Deposits in the Northern Part of the Cnopinn Sea
Region (0 sledakh proyavleniya merzlotnykh protsessov v chei-
vertichnykh otlozheniyakh Severnogo Prikaspiya)
PERIODICAL: Izvestiya Akademii nauk S-SH, Seriya geologicheskayn, 1958,
Nr 12, pp 110-111 (USSR)
ABSTRACT: The author describes the traces of cryoturbation in "he Yiddle-
and Upper-Quaternary layers near Chdrnyy Yar village on
the banks of the Volga river, in the northern part of the
Caspian Sea region. Repeated findings of wedge-like cryolites
embedded in successive layers of that period show that there
were four interglncinl otages In the .-,unternnry period.. Simi.
lar findings were made in other parts of the Russian Plateau
There are 2 Soviet references.
AS30CIATTON: Geologicheakiy inatitut Al'i 335~iR, tt,,oskvn (The Geological Tristi -
tute of the Af; US'51?, Moacow)
SUBMITTED: April 22, 1957
Card 1/1

r1 0 n
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t'n I P,
V n d ma s i
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Oi Petrolom
by
Ca rd

VASIL'TEV, Yu. K. , Cand Tcch '~-Jci -- "Rollui- I'voil, wool,~
of contour Di-essing (DP-K) in cast and in lift-transpol-t
Voronezh, 16,60. 1" pp; Of l--iir7l;l.;r arid C- c j:-
Education RSF'~,R, Voronezh ~ore,--,ry Eiv. ri r J. n..~
1 -.1 Ce lriz;t); L50 c o I, I
riot given; (K.L, 24-60, 132)

16(1)
AUTHOR: Vasillyev,Yu.L. SOV/20-127-2-2/70
TITLE: Minimum Contact Circuits for Boole's Functions of Four Variables
PERIODICAL: Doklady Akademii nauk SSSR, 1959,vol 127,Nr 2,pp 242-245 (USSR)
ABSTRACT: The present paper is a further development of the author's
certificate, on the most essential results of which in 1957 S.V-
Yablonskiy has reported on the All-Union Congress on All-Relay
Systems. The author starts from a catalogue of circuits for
functions of four variables (synopsis of the catalogues of
'Ref 72 and ~-Ref 82). Then it is proved that all circuits of
L
the catalogue are minimal. The idea of the proof is as follows:
for the number of contacts in all possible realizations of the
given function by circuits, a good estimation from below is
determined so that this estimation is reached by at least one
circuit. Five theorems are given <ogether. The author mentions
A.A.Markov, and G.N.Povarov.
There are 2 tables, 2 figures, and. 11 references, 6 of which are
Soviet, 3 American, and 2 French.
ASSOCIATION:Moskovakiy gosudarstvennyy univervitet imeni M.Y.Lomonosova
(Moscow State University imeni M.11.Lomonosov)
PRESENTED: April 2, 1959, by M.V.Keldysh, Academician
SUBMITTED: March 31, 1959
Card 1/1

VASIL"YU, Yu.N., Whener.
--I
Sme problems in the route planning for the Moscow city transporta-
tion. Gor.khos.Mosk-30 no.12:16-18 1) '56. (NW 10:2)
(Moscow-Traffic engineering)

VASILIYXV, Tu.M., insh.; OKMIMMO, R.K.
...
Now rollers on pneumatic tires. Avt.dor. 23 no.7:10-11
J1 160. (MIRA 13:7)
(Rollers (larthwork))

VASIL'YEV, Tu,H,, inzh.
geehanization of the surface treatment. Avt.dor. 23 no.1:22
Mr '60. (MIRA 11:6)
(Baltic States--Road machinery)

VASILITEV, Yu. M.
Ability of various normal tissues to stimulate the growth of
tumor cells. Vop. onk. 8 no.4:62-67 '62. (MIRA 15:4)
1. Iz otdela kantserogennykh agentov (zav. - cbl.-korr. AMN SSSR,
prof. L. M. Shabad) Instituta eksperimentalinoy i klinicheskoy
onkoloaii AMN SSSR (dir. - deystv. chl. AMII SSSR, prof. 11. 11.
Blokhi~). Adres avtora.' Moskva, T-1.10, I-ya Meshchanskaya, d.
61/2, korp. 2, Institut ekaperimentallnoy i klinicheskoy onko-
logii.

CHUMAKOVA, M.Ya.; VA$ILIYL?V _Yu.M.; SAVDIOV, A.P.; AGOL, V.I.;
TSMIN, L. B.
Strain of malignant cells obtained through the prolonged culti-
vation in vitro of normal kidney tissue from mice of the A/811
line. Vbpoonk. 8 no.8:51-57 162. (MIRA 15-.9)
1. Iz Instituta po izueheniyu poliomeliti i viraorqkh entsefalitov
(dir. - deystv. cbl. AMN SSSR.. prof. M.P. Chumakov) i Instituta
eksperimentalln-di.i klinicheskoy onkologii (dir. - deystv. chl.
MT SSSR, prof* Blok.hin) Akademii meditsinskikh nauk SSSR.
(CAFCER) *--,(TISSUE CULTURE) (KIDETYS)

VASILIYEV, Yu.M., kand.tekhn.nauk; KHAPMiUTA, N.Ya., kand.tekhn.nauk
Rollers on pneumatic tires. Stroi. i dor. mash. 7
no.8:11-32 Ag 162, (Rollers (Earthwork)) (MIRA .15:9)

VASILIM, Yu.M.j* OBLISHTLMI,, M.
Receprocal relations of precancerous chWes and reactive proli-
feration. Veat.AMN SSSR 17 no.6:7-16 162. (MBA 15:8)
1. Institut eksperimentallnoy i klinicheakoy onkologii AMN SSSR.
(CARCINOGEMIS)

VASILIYEV, Yu. M.; KAZAKOV, M. P.; CHARYGIN, M. M.
Prospects of extra-deep drilling in the Caspian Lowland. Razved.
i okh. nedr 28 no.5t4-6 my 162. (MIRA -15:10)
1. Moskovskiy institut neftekhimicbeskoy i gazovoy promyshlennosti
im. akademiks, Gubkina.
(Caspian Lowland-Boring)

PROSHLYAKOV, B.K.; VASILIXEV, YU.M.
Reef formations in the southern Emba region.
no.38j144-US 162.
(Emba region-Reefo
1519)

ARAMMIlly M.S.; VklK'YLV,, Yil.K,.~ IIILINTCHUI~P V.S.
SelsmJc errors in the central Pnd zeetern regions of the
Caspian lowland. 17,7. u:heb. zav.; aef-,' ' gaz 4
no.llg3~-7 162. (Y.TPA l7iO
Moakovakiy insLitut I ,:v.zr)yr.y prOMY3'llennosti
imen! akedentka I.M. liu~klrm.

I-MILRYGIN, M. M. ; VASIL'YEN, Yu. 114. ; K;,Jt'JTARCV, V.
I
"Sow recld Iar--, ties of ri-I gas ;Iistrib-ition, -r, salt J Mes Sf ---
- - - I - - -~D -
world. if
report submitted for 22nd Sess, Intl Geological Cong, New Delhi, 14-22 Dec
1964.

VASILIYEV, Yu.-M
Geology - Caspian Depression. Folds (Geology).
On the existence of the buried Hercynian folding in the northern part of the
Caspian Depression., Dokl. AN SSSR, 81, No. 5, 1951.
Saratovskiy Goaudarstvennyy Universitat im. N. G. Chernyshevskogo.
2
SO: Month List of Russian Accessions, Library of Congress, - May 195Y, Uncl.
Red. 5 July 1951. -

VASILIYNV,Yu.H.
Young tectonic movements In the northern Caspian Sea region. Trudy
MEI no-14:3-11 155. (KLRA 8:11)
(Caspian Depression-Geology)

VASILITIV, Yu.M.
Tectonic structure of the Buzachi peninsula. Dokl. AN
SSSR 110 no.6:1053-1056 0 156. (W2A 1W)
1. Moskovskly neftyanoy Institut imeni I.M. (hibkina.
Predstavleno akademikOL S.I. Mironovym.
(Buzachi Peninsula--Geology, Structural)

Uning aerophotographic methods for geologleal surveying in the Ural-
VAa oil-bearing area. 7ridF KKI no.19:1.11-173 157. (KIRA 11:1)
(Caspian Dapreasion-Geology)
(Photography, Aerial)

TASILITXT, Tu.M.
Characteristics of the Nungar facies in the Caspian Sea region as
compared to certain features of the cauthwestern parts of the Russian
Platform. Dokl.AN SM 112 no.1:109-112 A 157. (MLPA 10:2)
1. Moskovskiy neftyanoy institut imeni I.M.Gubkina. Predstavleno
skademikom S.I.Wlronovy -
(Caspian Be& region-Geology, 3tratigraphic)

AUTHORS: Vasillyev, Yu..M. amd 20-5-32/54
Proshlyakov, B.
TITLE* The Petrographic Pecularities of the Carboniferous
of the South Emba Upheaval (Petrograficheskiye
osobennosti. karbona, Yuzhno-h'mbenskogo podnyatiya).
PERIODICAL: Doklady Akademii Nauk SSSR, 1957, Vol. 115, Nr 5,
pp. 968-970 (USSR)
ABSTRACT: Recf,ntly the question of the character and the origin
of the carboniferous deposits which were discovered
by bore-holes in the said elevation, were discus-ied,,
Sone experts were of opinion that these sediments re-
present typical formations of plateaus which, according
to their composition, are very much related to those
belonging to the "syneklisis" of Moscow. The petro-
graphical investieations of the rocks by the authors
supplied additional material wich permits a critical
consideration of the above conclusion. The super-
carboniferous lime-stones are conspicuous even in case
of z. superficial macroscopic observation by their
CARD 1/5 extremely intensive condition of recrystallization and

Tiv., Petrographic Pecularities of the Carboniferous of the 20-5-32/54
Soutti Emba Upheaval
by their maximum solidification. They are transparent.
at fine fissures and may be classified among the
marble-like lime-stones. The loamu occuring in this
area are similarly converted, so that they almoat
entirely lo3t their aptitude for plastic deformation.
The material from the microscopical HLudie8, in
comparison to the similar formations of the batij,~ of
Moscow, is still of greater interest. Theru are no
pores determinable in the Emba lime-stones, not even in
case of 160 X. Substantial differences are also noticed
in the structure of both species of lime-stone: The Bmba
lime stones show a mosaic structure and may be considered
as middle crystalline, according to their Crainsize
(0,08-0,25 mm) Fauna residues are found in the lime
stones of both areas. A great number of coral skel.~toj-,!3,
"formaniferous" shells, splinters of "Echinoderm" shields,
"03trakode" shells, etc exist in the "Podol" liiae~; -of
Moscow. They are well conserved and easily determinable.
CARD 2/5

The Petroeraphic Fecularitie3 Of the Carboniferous of the 20-5-32/54
SOUth Elflib~i Ufh(JUViLl
Incomparably sriall(.-r quantitiet; of thene residuk~a are
found in the Einbu-l'.me. 'Due to an intensive recrystal-
lization their structure has been largelj distorteA and
deformed, which renders the determination ot" their belong-
ing to a specific specien considerably difficult, if it
does not prevent it entirely. Maybe, there once ha5 been
a greater number of these residues which have, however,
become unrecognizable by recrystallization. It hence
follows that the limes of Moscow have nct suffered any
substantial conversions. On the other hand, there are,
moreover, still traces of an arraneement of the initially
accidental orientation of particles, as well as -f
solidification and contraction shrinkaj;e. This proves
a stranee metamorphization (even if it has not been
fully developed) of the carboniferous sediments of the
South Emba elevation. In this context, the increased
pressure may be considered a leading factor. Presumably,
the following paleotectonical conditions of thu two
areas have also been substantially different from each
CARD 3/5 other. Those of Moscow are typical plateau dt;po3ita.

The Petrographic Pecularitles of the Carboniferous of thr; 20-5-32/54
So,ttii Emba Uph(.-av4I
The Embq formations of the aame a6e 3how devi,~.tia~; anci
divergent. featuren. The li3ted petroEraphical pucularititiz-,-
besides the occurence of terrigenous layers of severftj
hundred meters of thickne3a - do not permit the Embft
limes to be conaidered as typical platedu formations.,
These formations - on the contrary - were much more
closely related to the formation of folds ard. tl,F-- 2one
of "Herzynides" embedded nearly than with the processes
which occured at that time in the interior of the
Russian platean. Therefore it would be more correct
to consider the South Emba elevation riot aB L, typical
plateau formation, but as a pecialiar tectonic element
which occurs within the range of boundary flexion. A
practically important conclusion may be drawn from this:
As far as the carboniferous masses occur in thi:i area
in solidified and recrystallized condition, their porosity
and "collector" properties can soarculj be favorable for
the discovery of exploitable petroleum deposits. Waybe
there is an analogy with the area of the Akt7ubinsk-Ural
CARD 4/5 where all efforts to find exploitable i~etroleum have

The Petrographic Pecularitieo of the Carboniferous of' the 26-5-32/54
South Emba Upheaval
failed up to the present. Perhaps it would bv more
advisable to con3ider the "terrigeneous carboniferous
Ma33es more carefully. There are 3 fikures (5 micro-
photographs) and 7 Slavic references.
ASSOCIATION: Moscoit-Inntitute for Putroleum Rosourch imeni I. M.
Gubkin (Moskovskiy neftyanoy institut Im. I. M.
Gubkina).
PRESENTED: By D. I. Shcherbakov, Academician, Fie-bruary 28, 1957
SUBMITTED: February 27, 1957
AVAILABLE: Library of Congress
CARD 5/5

(paak rairco-'I 'h' ORU.MIN, KfI&M!'Vdkh&rlavI*hg-AIKOT, Rink
121.1
ISM, Air-,
,PUXKMIYO Vladlidr
Tywheslavoviii.. 'SIM *-XULTMOT, Rasfev BedirovIch; POIDSIU,
A*S., tekhn. red.
[Tectonics and history of the development of the Oaspian Depression
and adjacent regions in connection with questions of the presence
of gas and Petroleum] Tektonicheskoe stroenie istoriia mzyitiia
Prikaopftskoi *pAdiny i emozhnykh oblastei v eviazi a voprosami
ueftegazonoonosti. Pod red. 14. P. Mazakovs, t - kX*'Chirygina', Hookya,
Goa. nauchno-tekhn. izd-vo neft. i gorno-toplivnoi lit-ry, 1958.
402 p. (NM lio-9)
(Caspian Depression-Geology, Stractural)

VASILIM, Yu.M.
~andgae-bearing prospeots on the Buzachi Peniumila in the
light of new data, Izv. qs, ucheb, zav.; geol. i razv. no,2:
94-98 7 158. (MIRA 11r6)
1. Mosknvokiy neftyanoy institutim akademika I.M. Gdbkina~
(Bazachi Peuinsulap-Petroleum gs6log7)
(Buzachi P6ninsula-Gas, &tural--Zeology)

KAZAKOV, M.P.; VASIL'YEV.-Yu.M.; SHIROKOV, V.Ya.
Development of concepts on the tectonics of Ciscaucasia and the
southern boundaz7 of the Russian Platform. Trudy MKI no.22:29-62
'58- (MIRA 12:4)
(Russian Platform-Geology, Structural)
(Caucasus, Iforthern-Geolog7, Structural)

VASILIYEV, Yu..M.
T
ces o permaf
ra-- .- --i- "-'- root phenowna in Qaaternar7 sedgiamen,7230%oth.12:
northern Caspian 3sa region* Izv# AN SSSR. Ser. (MIRA 12:3)
110-111 D 158.
l.Geolsgicheski7 institut AN SSSR, Hoskva.
(Caspian Sea region-Geolo97, Stratigraphic)
(Frozen ground)
V

AUTHOR: Tasiltyev' Yu. M. 20-119--4--36/60
TITLEs Inherited Folding Between South Ural and Uangyshlak
(Unasledovannaya skladchatoatt mezhdu Tuzziym Uralom
i Mangyahlakom)
PERIODIC.&Lx Doklay Akademii Nauk SSSR, 1958, Volt. 119, Nr 4,
PPL 759-762 (USSR)
ABSTRACTs There is scarcely a problem in geological literature
which to such an extent has attracted the attention
of'geologists as that of thesjoutlk, east framing of the
Rusak.rz Plateau. The discus oz!Pwhether the lold system
of tne Ural is continued underground~ where this
continuation lies, and with which known formations
it is conjugated has now lasted for 40 years.
The numerous published hypotheses could, however,
not solve this problem in consequence of the lacking
fan~ts. The last century furnished such material.
H-encA a structural scheme according to the roof of
IJPDer Cretaceous could be made (figure 1). This acbene might
Card 1/4 be v-sed -t!,j invewltigate several more
-7

Inherited Folding Between South Ural and Mangyahlak 20-119-4-3616o
4mPortant ifema of the problem. The newest investfgatioCs
showed that 1) The Ural fold mystem ceaaes neither at
the southern and of Mugodzhax , nor in the Cbushka-Kull-
-zone., It turne to south west,-ainks gradually, and can
be observ-ed up to the Aul (vIllage) of Ak-Tumsuk and then
up to the northern boundaries of Ustt-Urt. Moreover,
the 3y!5tem is indicated even in the regiun of the northern
Ustl-brt. To this continuation correspoz;d the dislocations
of the Ghushka-Kul, as well as the an~iclinals-
7. ' P p
Wumsuk and KurgaAcoo` zes ond to this continuation in the
sedimentary cover . 2) Two systems of inherited
structures occur in the region of the peninsula of Buzachi.
They do not differ from the dislocations of the Chushka-
-Ku"& -zone and other- Inherited dislocations of the Ural-
Si1-__ r1an 1~-plhercynian plateau. They reflect obviously
the structural main elements of the buried Hercynian
fundament which are analogous to those expressed in the
ChuRhka-Kull-zone of elevationae 3) A now fold system is
found at the east coast of Mertvyy Kultuk which is
analogous to the above mentioned. These folds are
Card 2/4 inherited, too, and the last mentioned reflection of

Inherited Folding BL%tween South Ural and Mangyahlak 20-119-4-36/60
a folded fundament, apparently also Hercynian, takes
also place here. Thus an uninterrupted fold syste-m
lies between the south Ural and the Buzachi peninsula
(figure 2). The folds are completely analogous in all
intermediate zones. Hence can be concluded that these
zones are parts of a now buried qlr-+nm of Hercynian
folding which.,in the. shape of a smooth curve, frames the Russi;m
Plateau, from the southeast . Between this system and the
margin of the plateau lies a thrust-out downwarping
in the region of which no continuous, but an interrupted
folding is distributed. it is not inherited, or 'to a
very small extent so. The masocenozoi(r dislocations
in the district of the south khba elevation nrP of this
kind. (figure 2). There are 2 figures# none of which are
Soviet.
ASSOCIATION: Moskovski- --ftvanoy inRtitut im. I. 1G Gubkina
(Moscov. I'V--trole,= Institute imeni I. M. Gubkin)
Card 3/4

Inherited Folding Between South Ural and Mangyshlak 20-119-4-36/60
PRESENTEDt B-ovember 12, 1957t by D. I. Shcherbakov, Member, Academy
of Sciences,USSR
SUBMITTED: November 10, 1957
Gard 4/4

.VASIL'Tlff, Yu.M.;,KAZAKOV, M.P.; CHARYGIN, N.M.
[Tectonics, oil and gas potentials, and basic trends in geo-
physical Investigations of the northern Caspian Sea region]
Taktonika, perapektivy gazoneftenoonosti I oanovnye napravlenils
goologo-geofizicheakikh issledovanii v Severnom Prikaspii.
Moskva, Vees.nauchno-issl.in-t prirodnykh gazov, 1959. 49 p.
(MIRA 13:9)
(Caspian Sea region--Petroleum geology)
(Caspian Sea region-Gas, Natural--Geology)

VASIL' TFV,--Yu.M,_
Comparing 1~uaternary se-iinentation in the Caspian Sea region with
the glaciation of the Zast European Plain. Biul.Koo.chetv.per.
no.23:91-96 159. (MIRA 13:4)
(zaet European Plain-Glaclal epoch)

3 (5)
AUTHOR: Vasillyev, Yu. M. SOV/20-126-5-38/69
TITLE: On the Structure and Age of the Syrt Deposits in the South
Tranavolga Area (0 stroyenii i vozraste syrtovykh otlozheniy
yuzhnogo Zavolzhtya)
PERIODICA.L: Doklady Akademii nauk S5SRf 10,599 Vol 126, 11r 5v PP 1051 - 1054
(USSR)
A3STRACT: In 1951-56, the author had an opportunity of investigating the
Syrt deposits (mainly on the basis of material from borings)
in the Bouth of the Syrt Plain in the area between the rivers
Volga and Ural (uouth of the Saratov-Urallsk railroad). He was
able to ascertain that the Syrt deposits are little different,
by character and age, from analogous manses of the cover form&-
tion8 in the central and southern areas of the European part
of the USSR. The opinions of different investigators on their
structure are rather contradictory (Refs 3,50,10-12). The data
obtained by the author complete the scheme suggested by F. P.
Savarenskiy (Refs 11,12). The upper part of the mass consists
of 2 horizons I and II with an intermediate layer of buried
soil (P ). The central part of the Syrt mass (horizon III) is
Card 113 mainly trown-colored. The underlying horizon (IV) haep similar

On the Structure and Age of the Syrt Deposits in the SOV120-126-5-38169
South Tranevolga Area
to I and III fossil soil (P 3). Often there is still horizon
(V), consisting of sandy clay, lying under (IV). 1s to the age,
the author Joins those investigators who classify the Syrt mass
to the Quaternary period (Refs 2,40,901,13). By comparing the
horizons of the Syrt deposits with the Kaspiyakiye, it can be
observed that the lower horizon of the former (IV) almost lies
on the same level with the Astrakhanakiye (Bakin:kiye) conti-
nental layereg and is made up of the same clays te. (in agree-
ment with references 2,4,11,14,15). The middle horizon (III)
is put into correlation by the author with the lower Khaurskiye
layers of the"Prikaspiy"(m-m mew Gaspian BeQ.Horizon (II) is
compared with the'iteliskiye layers, while the top horizon M
can be easily compared with the lower Khvalynakiy horizon of
the Frikaspiy. If the above data are correct, the question may
be raised whether the principal mass of the Syrt deposits has
formed in the aeolian ways There is no reason why the Syrt mass
should be considered an old peculiar geological body unique in
its kind. It stands in one line with the other cover formations
Card 2/3 of the Russkaya ravnina (Russian Plain).

On the Structure and Age of the Syrt Deposits in the SOV/20-126-5-718/69
South Tranavolga Ares,
There are 16 Soviet references.
ASSOCIATION: Geologicheskiy institut Akademii nauk SSSR (Geological Insti-
tute of the Academy of Sciences, USSR)
PRESENTED: February 9, 1959, by A. L. Yanshin, Academician
SUBMITTED: February 9, 1959
Card 3/3

B(GACHEVA., Yu.H.; PRWHLYAKOV, B.K.; CHARYGIN, M.M.;
SHLEYFIER, A.G.
Unique Triassic cross oeotion in the AmIsorsk oxtra-deop
borehole (Caspian Lowland). DokI. AN SSSR 165 no.3:629-632
N 165. (M-IRA 18;11)
1. Moskavskiy Institut neftekhImIcheskoy i gazovay promp-h-len-
nosti im. I,M. GubkInu. SubmItted May 27# 1965.

MARADZU, M.S. VAST L'YEV, N,M.; Nif,''IMFIR, V~S-
Using mathematical st-l."StIcl Jr, geolou. Iz-,r. vYs.
-cheb. zav.; neftl i gaz 8 no.4:3-8 1~5,
1. Moskovskiy instff,i~'ne!'tekilimicheskoy i grazovoy promyshiennosti
ira. akademika 1.14,Gubkina.