SCIENTIFIC ABSTRACT KULIKOV, L.A. - KULIKOV, M.V.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R000927420011-5
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: August 23, 2000
• Sequence Number: 11
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

ACC NRt AP7002993 SOURCE CODE:
INVENTORS: Kulik _A.;__ Kita, V. F.; Veselov, M. P.
- --9y
ORO: none
TITLE.- A device for pre-ignition heating of an internal combustion engine. Class 46"
No. 189643 Za-nnounced by Central Design and Construction Bureau MRF RSFSR
(Tsontrallnoye proyektno-konstruktorskoye byuro MRF RSFSR)7
SOURCE: Izobratoniva, promyahleruVye obraztoyp tovarnyye %naki, no. 2h, 1966, 95
1 T~TIC TAGS: internal combustion onginep diesel engine, engine ignition systemj engine
cooling system
ABSTRACT; This Author Certificate presents a device for pre-ignition heating of an
internal combustion engine,, such as a marine dieselp prior to its starting. The
heating is accomplished by admitting hot water from the cooling system of a working
engine to the closed oircuit of the engine to be heated (see Fig. 1). To increase
the reliability and to improve the starting properties, the circuit Is provided with
artificial circulation produced by an ejector placed at the circuit outlet. The
input and the output of the circulating circuit may contain automatically directed
two-seat valves for connecting the engine (after it is started) to the cooling system.,

ACC NRt AP7002993
Fig, 1, 1 -'ejector;
2 two-seat valves
Orig. art. has% I figure,
SUB CODE% 21/ SUBM DATE: O9Nov65
Card 2/2

1,01"o-7. S.I.
Ilu
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TITLE;: of Redil-u'-ro.
;(irovcmd
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mimm"tions h,-~Ve
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(centrill Bourd, of the "'TO for
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A"R

SO'711Y-rl -1P I
Hesults of Reducint; Reaj,~ent Consumption at the NirovLgad
Benoficiation Works
eroup). The authors describe the residts obtui),,~d,
Two types of ore are treated at the vic-,h s: an _'r4,rv..'1n-ed
copper-zinc-pyrite (12-24%S) ard a Lniform sulphide,
(44-46% S) noverinF, the composition r,,.Inje (table 1)
0 84-1.70% Cu, 0.50--5.62q, Zn. The first, , -
type tare
treated by a collective-selective flot_--tion
fl ovis tie et (fig.1) with two stabe the 2e _---ond
by simple copper flotation after Lrindir,~, to 90-921% -
0.074 mm. Laboratory experimonts o.,j tLe effectiveness
of various collectors on the flot4tior. of Kirovbrud
sulphides viere carried out with butyl ,.-nd et-hyl
xanthates and mixtures of them. In Febr-L,,ary 1958
production tests with the two collectori; for the
flotz;~tion of copper, zinc and iron miner~_Is showed that
the optimal condition3 were different for different
minerals. In the second sta,~,e, labort,tory te-sts on
J
xanthate consumptions -L*r- the reoo,7,.I_r.y c" copper (fiL.2)
Card 2/3 zirc (fiL!,-.3) and. Pulphide were follovied bi the adoption
pq -.- -- g
~g
_-P Nt

Resi.,lts of Roduci-nL Reat~erit Constjmption at tLe
Benef iciation Works
of a new practice in Mar-ch 1953. This hus reduced
butyl-xanthate and flotation.-c-il consuinpt-icn.6 by
52-80 and 59-5(y%7 respectively. The auI.L,,zs i.,how thLt
reductions in collector and foaml%-dLent Constimptionz
led to savings in other rearents and Eave better
concentrate-a. There are 4 fij~ureq tird 8 tabiQcl.
1,4
.,SSOCIATION:Kirovgradskiy medeplu'vil'nTy komb-Aint 1. (K-,.rovf,'rt%d
Cojjj,,er-smeltin,r,- Combine)
Card 1/3

~ELEKHOVA, Ye.L.; KULIKOV, L.D.; FOFGV, S.I.; KHOKILLO, N.K.
Comparative testing of "Mekhanobr" and "Sikhali" flotation machines
at the Kirovgrad plant. TSvet. met. 36 no.9tl4-16 S 163.
(MIRA 16:10)

KULIKOV, L.D.; POPOV, S.I.; KHOMULLO, N.K.
Technology of treating impregnated sulfide ores from the Levikha and
Lomovo deposits. TSvet. met. 36 no.12:72-73 D 163. (MIRA 17:2)

- KULIKOV, L.D.; POPOV, S.I.
Increasing the wear reoictance of sand pump parts b7 rubber
coating. Obog. rud 4 no.5:14 159. (141.U 14: 8)
1. Kirovogradskiy medeplavilInyy kombinat.
(Mechanical wear) (Rubber coatings)
~I

XULIKOV L.Dt-a--KHOMULLO, N.K.
- -_
Increasing the completeness and the.complaxitj of ore utilization
at, the Kirovgrad OreDressing Plant. TSvet. met. 35 no.3i
82-84 Mr 162 011RA 1514)
(Kirovgrad (Sverdlovsk Province)-Ore dressing)

KULIKOVI L.D.; BOLKOV, D.A.; POPOVy S-1,; MIOMLO, N.K.
Selecting a flow obsot for the dressing of Gay deposit ores.
TSvet. met. 36 no66JI-2 Jq~' 163. (MIRA, 16 -.7)
(GV Reglon-Nonferro4p metals)
(Ore dressing)

KULIKOV, L.D.; KJIOI,PJLLO, N.K.
---
Testing the "Sikhali" flotation rachine at the Kirovgrad Plant.
TSvot. met. 34 no.1:12-15 Ja 161, (MA 1-7: 3)

KULIKOV, L.N.
P-pendence of the transient renfstanc8s of galvanized palladium
Coatings on the nature of the olectroVto. Zhur.fiz.khim. 38
no.llx2662-2663 N 164, (MIRA 18:2)

USTINOV, V,S,- Ali'JI'VIN017. E.A.- MA.~,ITYIINTKOV, I.P.; 'f3FLIJYKO, I.M.;
I!OLI.SX,',YA, I.Ya.;
TPruriaNA, 'L.V,
Increasirig niamaolium recovery during the remeltir,g of a
conderisau! of' inagneeiim motal and mignesium Chloride.
,rsvet. met. 3-1 N I G". . (MIRA 13:4)
3

ILI INSKIY, Yu.A.; MJLIKOV, L.S.
Immunological reactivity of mental patients following therapy
with aminazine, insulin, and other methods [with summary in French).
Zhur.nevr. i psikh. 59 no.2:156-159 159. (MIRA 12:4)
1. lafedra psMiatrli (zav. - prof. 0-V. Karbikov) II Moskovsko-
go meditsinskogo inatituta im. N.I. Pirogova.
(MEUTAL DISORDERS. immunol.
off. of ther. (Rue))

KULIKOV, L.-S., Cand. Medic. Sol. (disi3) "Immunological Reacti-
vity for Schizophrenia and Effect on It of Modern Methods of Treat-
ment," Moscow, 1961, 16 pp. (Central Inst. improvem. Trng. of
Doctors) 250 copies (KL Supp 12-61, 286).

KULIKOVt L.S.
Immunological reactivity in patients with schizopbrenia during
treatment with insulLh and neurqeptic drugs. Zhur.nevr.i psikh.
61,-l'n&.Zs20l-207 161, (MIRA 14:6)
L' Kafedra paikhiatrii (zav. - Prof. O.V.Kerbikov) II Moskovskogo
meditsinskogo instit4ta.
,WCHIZOPPMIA) (INSULIN) , (CHLORPRCMAZINE)
(D*HITY)

BELOV., V.P. (Moskva); KULIKOV, L.S. (Moskva); TRIFONOV, O.A. (Moskva)
Some characteristics of the dynamics of neurotic states originating
in childhood. Zhur. nevr. i ps1kh. 65 no-5:733-736 165.
(MIRA 180)

KULIKOVI L.V.,, Cand Agr ,ci (dis:;) "Certain data on -?m
4-aw-sf covm.lf s; 22 pp (Yor, Order of
Agr Acad im K.A. TiArya,;,cv. Chair of Gattle) 110 co~)J-el,
nj 2b-59, 129)
bb -

IMIKOV, L.V,, aspirant
hilk-ylolding processes In cows. l%v,T-SlChA no-3:173-182 159,
(HIRA 12:10)
(Inctation) (Milking)
!,-, %
~,-V 5

KnIKOVp Lev Vasillyevich; K.OKOSIMO, A.G.,, red.
(Meat productivity of cattle and waya for its increase]
Miasnaia produktivnoott krupnogo rogatogo skota i puti ee
povynheniia. Moskva, Izd-vo VPSh i AOIT, 1962. 63 p.
(MIRA 15:7)
(Beef cattle)

SHVABE, A.K., kand.se1'sko4ozyuyatvennykh nauk; MMIKOV L V., kand.
sellskokhozyaystvennykh nauk =U-Z=
Effect of environmental factors and the period of lactation on
tUp'letting down of milk in cows. Zhivotnovodatvo 23 no.5:79-U
my 161. (MIRA 16t2)
(Milklng)

. . I ~ ! '~ t , :~:~7 %-z'-M 7:.'T"~ -, ' ~ . ~;'~~A , '~-. :- I - ~. o, , ~ - ~ ~ . - . I .
- fR - :
AI&I-3 A, -N-f I -tU- v
P Ye'A'; GOLUB, I-V-; KULIKOV, L.Ta.
Processing the hydration precipitate in preliminary settling tanke. x"1.
-zhir.prom. 18 no.5:24-25 My 153. (XWA 6:5 )
L Saratovokiy Mallozavod Wo.l. (Oils and fate)

XULIKOV, L-Ya.
Reconditioning rollers. Kael.-zhlroprom. 10 no-3:37 154.
OMRA 71Q
1. Saratovskiy maslozavod No.].
(Machinery-4ainten"ce and repair)

KITLIK~~~
K teorii abelevykh grupp proizvollnoy moshchriosti. Yo)tem. SP., 9 (51), (1941),
165-182.
SO: Mathematics in the 'USSR, 1917-1947
Edited by Kurosh, A. G.
Markusevich, A. I.
Rashevskiy, P. K.
Moscow-Leningrad, 1948

0LIKOV, L. Ya.
Mathematical Reviews
MaY 1954
History
Cl)
Kulikov, L. Ya. On direct decompositions of
11
Ukrain. Mat Z6rnal 4,230-275,347-372 (1952). (Rus.,
sian)
Let G be a torsion-free abelian group which is completely
decomposable in tile sense of being a direct sum of groups
of rank one. Is every direct summand of G likewise com.
pletely decomposable? This question'was raised by Baer
[Duke Math. J. 3, 68-122 (1937)] and was answered by film
in the affirmative tinder the extra assumption that the iso-
morphism types of -the components' satisfy a certain de-
scending chain condition. The main new result of the present
paper is to answer the question in the affirmative in case
G is countable. This is the end product of a long investiga-
tion, many aspects of which are of independent interest.
Let G - _rA , it 1, be a direct sum decomposition of a
group G (not necessarily abelian) and let 0 be a set of
endomorphisms of G. The index set I is topologized by
declaring a subset J to be closed in case E& j e J, is
invariant under 0. A critical question is whether I thus
topologized is a Kolmogoroff t,0L,:e- (distinct points have
distinct closures). If it is, we pet a rl~ tural partial ardering
L(1, (1) of I by setting i;Sj when i is !it the closure of J.
In case 0 is tile set of all normal endomordhisms of G (i.e.,
endontorphisms commuting with inner autonlorphisins), tile
Kolmogoroff condition is equivalent to the following: for
no two distinct summands is it the case that each admits a
non-trivial homomorphism into the center of the other.

relic s as follows: Suppose (1) G EA i has
the Kolmogoroff condition relative to the set of all normal
idempotent endornorphisms of G, (2) for each i, any two
decompositions of Aj admit centrally isomorphic refine-
ments, (3) either (a) G is countable or (b) L(1, 0) satisfies
the descending chain condition; then any two direct de-
compositions of G admit centrally isomorphic refinements.
(Two' decompositions are centrally isoniorphic if one is
carried into the other by in automorphisni v-x' such that
x'x-l is always central.)
In the application to a torsion-free completely d(!com-
posable A lian group, one forms G=EAj by i
IV e grOUpirIg
together in one summand ill isomorphic SUminands of
rank one. Conditions (1) and (2) above are then verified;
condition 3(b) coincides with the hypothesis used by Baer.
The paper concludes by extending the result to completely
decomposable abelian groups which are not necessarily
torsion-free. The main fact needed is the author's ealier
theorem [Mat. Sbornik N.S. 16(58), 129-162 (1945); these
Rev. 8, 252] that any subgroup of a direct surn of cyclic
groups is cyclic. 1. Kaplansky (Chicago, Ill.).
/0 - ~/ - SY Z_ /

L. Ys. Generafized primazyMmm- IL Trudy
i-"108koV.-NM.ObV.2,85-167(1953). (Rumianj
[11'art I appeared in sanieTrudy 1, 247-326 (11952); these
Rev. 14, 132.1 Let Obt a generalized primary group (that
oVer Ar,
is, a module or Z, in the notation of the cited re-
7.~,L vie%-.,). We 4kfl'n'e a transfinite series of subgroups G. as
Matfiematica Reviews
Vol. 15 No. follows- (0; a a li ordinal, G. is Oe intersection 6f the'
preceding subgroups and otherwisi G.=(IP-G.-I. The--~
Jan. 1954 N
-Alg9bra subgroups settle down to the maximal divisible subgro'up
of G, and if the latter is 0 we say that G is reduced. The
groups A.-G.IG.-I are called th,' Ulm invariants of G;
they are groups with no elements of infinite height; The
bulk of the paper (1�5-10) is devoted to the proof of
Theorem 10.1, which gives necmqary and sufficient condi-
VV I tions for the existence of a reduced group with prescribed
cardinal number m and Ulm invariarts A.. These conditions
are as follows:
(1) EIA.1 ;Sm;SjjjAj,
a . it -
(2) 1 (P4A.) [P] I ~. I A.+ -PA I
(3) A. -2~- F- A
i~l 6
k
A
,;31, i'Va-
Z tR-

Here the v(,.rt;cql bar5 denott. cardinal number, a and V run
over the ordinals occurring in the given series A., is runs
over the inteVers, and the notation G[p] calls (or taking the
subgroitp of G conski ing of all clements x natisf ying Px - 0.
this result the author in able to sharpen .1 theorem of
~Kurosch LINIat. Sborilik N,S. 5(47), 317-354 (1939); these
Rev. 2, 2] asserling that there are prccisely 2" non-iso-
morphic groups of cardinal number ?n; he proves that there
are already that many abelian grotil),,;, By duality there i% a
corresponding enumeration of compact abeliangroul-A.
The final section gives a generalization of Ulm's theorem.
One assumes that G is a reduced generalized primary group
which satisfies three hypotheses: (1) G is countably genCT-
ated (as a m(witile over Kv or 7,), (2) each Ulm invariarit
is a direct sum of cyclic groups. (3) if E is a finitely generated
subgroup of G, then there Are only a finite number of indices
a suA that En G.;-1 Erl G. ~,. It is immediate that ordinary
primary groups satisfy these hypotheses, so that Ulm's
original theorem is subsumed. Known examples show that
hypotheses (1) and (3) cannot be dropped, but the author
leaves open the possibility of omitting (2).
1. Kaplansky (Chicago,

V

Call Nr: AF 1108825
Transactions of the Third A21-union Mathematical Congress (Cont. )Mozcov,
Jun-Jul '56, Trudy '56, V. 1, Sect. Rpts. , Izdatel'styo AN SSO Moscow, 1956, 237 PP.
Kaluzhnin, L. A. (Kiyev). Generalizations of Basic theorem
of the Galois Theory. 23-24
There are 4 references, 2 of Which are Frehchp and 2 English.
Kemkhadze, Sh. S~ (Batumi). second Pr4fer Theorem for Regular
p-Groups. 24-25
K)ntorovich, P. G. (Sverdlovsk). On the Theory of Semi-
groups in the Group. 25-205
There are three references, 2 of which are USSR and I English
Kostrikin, A. I. (Moscow). Nilpotent Groups and Lie Rings 26
Kulikov, L. Ya. (Moscow). Universal Complete Abelian Groups. 26-28
Lyu-Shao-syue (Moscow). On Splitting of Infinite Algebras. 28
Card 9/80

AUTHOR: Kull kov,.,--L'.Iya.- ('140800w) SOVI42-13-3-38141
TITLEi Decomposition Conditions for a Mixed Abelian Group (Usloviya
raeshcheplyayemosti smeshannoy abelevoy gruppy)
PERIODICAL: Uspekhi matematicheskikh nauk, 1958, Vol 13, Nr 3, p 247 (USSR)
ABSTRACT: Let F(G) be the maximal periodic subgroup of the mixed abelian
group G. Lot H(G) be the intersection of the subgroups nG,
H(G) - n nG, where -R is the set of the natural numbers. Let
n -ITL
B(G) be the subgroup of G generated by F(G) and H(G). Let M(G)
denote the set of all prime numbers p for which pF(G) ~ F(G)
and p7G ~U, where'U - G/F(G).
Theorems Let G be a reduced mixed abelian group, the factor
group G/B(G) of which is countable. Let the set M(G) be finite.
In order that G is decomposable it is necessary and sufficient
that H(G) is periodic and that every finite set of elements
of the factor group d is contained in any Servanz-subgroup
of finite rank of the group G.
Card 1/1

o i 2,,-ur, c. nbJ- I -In GrOUL .:ra 2 2 3 2
-Ap '6-' 17 6

KULDWV, I.I.A. [Kiilykov;) 1u).1 (Yayov)
Use of a conditlopal probabilitie3 mthod for establi-sh~-.g a medit-all
diagnosis. Avtomatyka no.5:1.33-19 '61. (111MLI 14 10)
(Medical electrordes)

'0V 0. j
Yu. A. OLIK M.A. [Kidyk
Statistical proconlin,", of wpurl"norit"Ll ditt'l. lalkl'OU01. 2~lUr.
25 no.2:62--69 163, (NEU 17: 10)
1. Institut raikrobiologrii Ali' UlrrSS;t i InAitut maternatiki AW UkrSSR.

15-1957-7-9003
Translation from: Referativnyy zhurnal, Geologiya, 1957, Nr 7,
;p 23 (USSR)
AUTHOR: Kulikov, M. B.
TITLE: Treatment of Paleontology in the Abstract Journal of the
Academy of Sciences USSR (Oaveshcheniye paleontologii v
"Referativnom zhurnale" Akademii nauk SSSR)
PERIODICAL: Inform. sb. Vses. n.-i. geolog. in-t, 1956, Nr 3,
pp 145-146
ABSTRACT: Bibliographical entry
Card 1/1

VIKTOROVp Z.F.; MIKWLOVp
nauchW red.; VOROBITEV, 0.5,~q red. izd-va; GURDZIiIYEVA,, A.M.0
tekhn, red,
(Navies of the United States and
SShA Velikobritanii. Laningrady
znanii RSFSRp 1961. 61 p.
(qnited States-Navy) (Great
Great Britain] Voenno-morskie floty
Ob-vo po raspr. po3dt I nauchn.
imim V'-.8)
Britain-Navy)

KULIKOV, M.F.
Chemical aDwpositinry and nutritive value of meadowand petsturo forage
In the Gorno-Altai Autonomous Province. Trudy Biol inst. Zap.-Sib.
fil. AN SSSR no.2:109-134 156. (MIRA 13:10)
(Gorno-Altai
Province--Forage
Autonomous
Plants)

KULIKOV, M.G.
Ventilating device for double-pano windows. Biul.tekh.1nf(;rm.j,v,
stroi. 5 no,12:22 '59o (MIRA 13:10
(Windows)
K4,

URP079 V.V., kand.takhmnauk; HUTUS9 M.X.v kand.tokhn.nauk; TSUKERMAN,
N.Ya. , inzh,; BELOLIKOVI V.N. 9 inzh. 9 naucbMy red.;. GRUTS, B.V.
inzh., naucbmyy red.; KULIKOV, M.G., inzh., naucbm;y7 red.;
FEDORTSOV, B.D., in2h.-P ndu-cffia~57 -red.; GRIGGRIYEVA, I.B., red.izd-va;
VORONETSKAYA9 L.V., tekhn.red.
[Roofing and waterproofing operations; reference maTmall Krovellmye
i gidroizoliatsionrWe raboty; spravochnoo posobie. Pod obshchei
red* V.V,Karpova. Leningradq Goa,lzd-vo Ut-ry po stroit., arkhit.
i stroit.materialamy 1961 302 P. (MIRA 14:6)
(Roofing) iWaterproofing)

KnIKOT, M. r.
*Theoretical and Experimental Investigation of Drives of a Cotton XAchIns
With a View to Increasing Its Output.* Sub 28 Jun 51, Moscow Textile Inst
Dissertations presented for science and engineering degrees In Moscow during
1951.
SO: Sum- No- 480. 9 y4W 55

iamIKOV. Y. -1.
Electric Drivine.-
Computing specifications for the electric drive of a viltiplo flat hosiery ma-cnine.
Leg. prom., 12, No. 6, 1952.
Monthly List of Russian Accessio , Library of Congress, October, 1952 1~M Uncl.

KULIKOV, M.1.1 FEDOTOV? O-V-
Studying the electric driving of the P-105 make pneumatic
loom. Izv. vys. ucheb. zav.; tekh. tekst. prom. no-4:122-125
163. (MIRA 16:11)
1. Moskovskiy teketil'W institut.

-- -- - -- - - - ---- - ---- - ~ m -.I- -- - - - -- - - -- - - -- - --- -- - ---- ---- - - - - - --
Kr,,YL()V, G.V. ; RULIKOV, kl.- . ; ljt~r~ .,
RQVit-'W3 tXr,i bit,111011-rW11-Y. li.~,-!. "), .".
n-auk no.21:115 165. 1 18,9)

karri. ~ekhn.
trx,
C - v,-, r fD r
ri- r~.

KULIKOV,K.M., inzhener
Change the accounting and wage system for road construction work.
Avt.dor.17 no-3:23 N-D'54. (MIRA 8:10)
(Road construction--Costs) (Wages)

KULIKOV, M.M.
Work of mixed crews in la7inf asphalt concrete pavements.
Avt. dor. 22 n0-5:18-19 MY 59- (MIRA 12:8)
(Pavements, Asphalt)
(Road construction workers)

,--KUIKCYV, M.M., inzh.; PZMOV, V.A-, inzh.
The DBI-20 pXavel separator, Tranap. stroi. 10 no-10:32-33 0 160.
(MIRA 13:10)
(Sand and gravel plants--Rluipment and supplies)

ACC NRt AR6o1625l
SOME CODE:
AUTHOR: Kulikovp M. N.;,Stal'makhov, V. S.
TITLE: c~aiculation of the interaction between an electron eam of -finite
thickness and a traveling-wave field in beam'devices with crossed fields
SOURCE: Ref. zh.-Fizika, Abe. llZh180
REP SOURCE: Sb. Vopr. elektron. sverkhvysok. chastat. Vyp. I. Saratavl-ka-ra-tovs-
M=t4 1964, 81-94
TOPIC TAN : electron beam, traveling wave interaction,, electromagnetic fieldp ways
propagation, adiabatic approximation, electron motion, space charge
ABSTRACT: Resulta are presented of a calculation of the propagation constants (PC)
for an electron beam of finite thickness In devices with crossed fields, with allowanef
for the distance from the cold cathode to the slow-wave system. Certain results are
aslo given of an analysis of the influence of the beam position in the interaction
space on PC of the waves in the system. The problem is solved In the adiabatic approx-
imation. It in assumed that the electron trejectories are straight lines, and that
the space-charge density is small and Is homogeneous over the section of the beam. An
equation is obtained for the PC; the results of its numerical solution are given for
the case of small signals, together vith the corresponding plate. An analysis of cer-
tain particular cases'shows that &.1lowance for the geometry of the interaction space
and for the position.9f,the electron beam in it can greatly change the PC of the waves[

L 33573-66
ACC NRs AR6016251 6
in the system. The character of variation of the PC is closely connected with the
variation of the PC of space-charge waves. If the modulation waves at the upper and
lower limits turn out to be uncoupled to each other for a given thickness of the elec-
tron beam and for a given beam position in interaction spacep.then the modulation wave
at the lower limit turns out to be practically uncoupled with the slow-wave system,
too, so that only two waves are excited in the system in lieu of three. Certain ways
of simplifying this general solution are indicated. A. Rosh&l'. -[Translation of
abstract]
S,UB.CODE: 20"
?
imi"20 M . . . . .

FWT(l).___ JY1
ACC NRs AR6015868 SOURCE CODE:
AUTHOR: Kulikov, M. N.; Stallmakhov, V. S. X110
TITLE: On calculation of the Interaction of an electron flux of finite thickness with a
traveling-wave field In radial beam devices with crossed fields
SOURCE: Ref. zh. Elektronika I yeye primeneniye, Abe. 12A160
REP SOURCE: Sb. Vopr. elektron. 3verkhvysok. chastot. Vyp. 1. Saratov, Saratovsk. un-t,
1964, 81-94
TOPIC TAGS: radial beam tube, traveling wave, electron flux, wave propagation
ABSTRACT: Calculation of propagation constants (PC) Is performed by the field method in an
adiabatic approximation for an electron flux (EF) of finite thickness with rectilinear electron
trajectories and a low homogeneous density of the space charge (SC), with a consideration of
the distance from the "cold cathode" to the moderating system. For determination of the PC,
eqtLatlons are written for the variable components of electron motion and the longitudinal elec-
field in an EF, standardized conductivities of the boundaries of the regions are determined,
a common dispersion equation Is found, satistring the boundary conditions. In the disper-
slon equation it Is considered that the characteristic s of the SC depend upon the thickness of the
UDC: 621.385.6
P

L 04-211--b7
- ------
ACC NR- AR6015868
0
EF and upon the geometry of the reaction space, including the position of the EF between the
conducting planes. For certain particular cases, PC of SC waves In EF and PC of waves In a
moderating system are analyzed. [Translation of abstract) Bibliography of 6 titles. D. Ya.
SUB CODE: 20
'I~ard 2,2
Tj

xk.(:C AP6007638 SOURCE CODE: U!,t/0 M 1 /66/009/010 110 1,16/0 154
AU'1110P: Gurr-o' V~ V.; 1"'kfli1fQV, t1C N.; V. 5,
OTRG: Sarat State Unive aratovskiy gosudarstvenny-i universitlet)
.LsLty
TITJ, [-.": Inventigation of tho instability (of diocotron impti(icat"011) of thill OCCtroll
1)ealrv; moving in crcnsed fic1da
P~OURCE: IVUZ. Radiofizi1,a,,,v. 9, no. 1, 1966, 146-15.1
;TOPIC TAGS. electron tube,,cross field tub,/
IA13STRACT:
i The results are roporti-A of aii experiii-icrital inw--stigation of (br.,
linst--'~hilitv c)( Olin et(-'ch.(jn bf,-arnn moving in crotisctl fi4.0dn iii a r(tgicm frci, from
le-xLerrizil t--Af ficids. Unlike other works (L. A. HaTri s, Proc. IRTE, B- 105, Suppl.
1645, 1958) -,where gain per unit current or
lbi--arn length was reported, tWis article gives 5
,ain in th ion, Ir -
jh~i tat.0 c drift rep An IM-type
cc figure) wat3 ufw (51
It"CLvoll-wave amplifiel
The. (Alocotron gain (over
db) watj deterinincd an,the difference
!'In and that of the m;%tching r I r nt~ nd --it ~irnpljfic-r for 4iocotrtm
Vain rneasurernentci
Card I

L 20a
ACC NRt
7638
devices. The experimental amplifier comprised: 1 - electron gun, 2 - electron
beam, 3 - first coupling element, 4 - second coupling element, 5 - third coupling
element, 6 - base (negative electrode), 7 - collector, 8 - absorber, 9 - drift. A gai
of 15-18 db war, obtained when an r-f signal was applied to tlie f1r:,t Lind takenfromt!
third coupling element. It was found that: (1) broa(Riand operation of the diocotran
amplifier is possible, even with dispersing coupling elements, if the latter are short
enough; an amplification band of 8116 was achieved in the experiments; (2) practical
application of such an amplifier is limited by its low efficiency and high internal nois
level. Orig, art. has: 9 figures and 6 formulas.
SUB -CODE: 09 / SUBM DATE: 08Jul65 / O1UG REF: 002 OTH REF: 005
ATD PRESS:q It

KULIKOV, M.N.
Crossings handled by switchman. Put' I put. khoz. no.6:24
Je 159. (MIRA 12:10)
l.Starshiy inshener sluzhby puti, LIvov.
(Railroads--Crossings) (Railroads--Employees)

ACCESSION NR: AP4017595
-AUTHOR: Kulikov, M. N.; Stallmakhov, V. S.
TITLE: Calculating an electron-wave M-type amplifier with a thin beam
SOURCE: Radiotakhnika i clektronika, v. 9, no. Z, 1964, 252-261
TOPIC TAGS: M type tube, M type amplifier, electron wave amplifier,
diocotron amplifier, thin beam M type amplifier
ABSTRACT: Based on R. W. Could's theory of a thin beam (J. Appl. Phys.,
1957, Z8, 5. 599),. formulas are developed for a few particular caacs of
calculating the overall gain of a crossed-field M-type (diocotron) amplifier. The
design procedure developed involves not only parameters of the electron beam and
the drift space but also parameters of matching devices employed with the
M-tube. The problem of gain determination is solved in these three steps:
(1) Determining wave -propagation constants in the matching and drift regionc
S/0109/64/009/002/0252/0261
Card 1/Z

ACCESSION NR: AP4017S95
(2) Determining boundary conditions in the input and output matching devices and
in the drift region., (3) Determining initial amplitudes of partial waves in the
matching devices and in the drift region. It is claimed that a numerical case
computed by the new formulas was In good agreement with experimental results
obtained by P. Gue'nard, et al. (AAn. radioa'lectr. , 195Z. 7. 30. ZSZ). Orig. art..j
has: 4 figures and 30 for=-'-a.
ASSOCIATION: none
SUBMITTED: 19J&n63 DATE ACQ: ISMar64 ENCL: 00
SUB CODE: GE
Card Z/2
NO REF SOV: 00 1 OTHER: 005

Lat i-n:
WALLilm,
t
o-f th: La.or Pa.-.mr ~iiffler Tec.~rdcal ~,ciool 4-,:.eni
Vecheryava Mo3lKva

AUTHOR:
TITLEi
PERIODICAL:
ABSTRACT:
Sherstyuk, V.N., Engineer
SOV-135-58-11-17/21
Card 112
A Welding Conference of Pacific Coast Plnnts (Konforentsiya
po sverke predpriyatiy Tikhookeanskogo basseyna)
Svarochnoye proizvodstvo, 1958, Nr 11, p 39 (USSR)
A welding conference of the Pacific coast plants convened
at Vladivostok by the Scientific Technical Section of Water
Transports. The following reports were delivered: Engineer
V.N. Sherstyuk on "Further Development of Welding Practice
in Far-East Plants"; Dotsent, Can~idate of Technical Sciences
M.S. Kulikov on the repair welding of crankshafts; Dotsent,
-C
aMn~ te of Technical Sciences, H.V. Barabanov on a rational
design of welded ship hulls; Engineer S.N. Agranomov on the
use of the latest methods in jemi-nutomatic and automatic
welding processesi Alekseyev, Gubskiy, Yung, Mallopuro,
Tsirkullnikov, Kagner and other plant workers made various
valuable suggestions on the further development of the weld-
ing process in Far-East plants. The Conference decided to

I i
A .'elding ('onference of Pacif-Lc Connt 11ants S~V-135-58-11-17/21
establish a welding laboratory on the Pscific coast, and
resolved to take various measures to improve welding
practice in this re~-ion.
1. Welding-USSR
Card V2

PALIADIN.. A.V., akademik; FEDORCHENKO, I.M., akademik; GULYY,, M.F.,
akademik; BJIKULIN .D.I.; IELINIKOV, N.P., kand.tekhn.nauk;
OKERBLO14) 11.01) P~f., doVtor tekhn.nauk; LYUBAUKIY., K.V.,, prof.
doktor tekhn.nauk, laureat Stalinskikh premiy; PORTNOY, N.D., I"
kand.tokhn.nauk; TSYBANI.. N.G.; KULIKOV M.S dotsent; AGRONOMOV,
S.N.,I inzh.,- FOLYAKOV, V.A., iniK-.; Sit~ARYU , V.N.J. inzh.
Congratulations on the publication of the issue no.100 of
the "Avtomaticheskaia Svarka" journal. Avtom.svar. 14 no.7:
3-8 J1 161. (i.aRA 14:7)
1. Prezidont AN USSR (for Palladin). 2. A14 LB4. glavnyy uchenyy
sakretart AN USSR (for Fedorchenko). 3. AN T6SR, prodsedatell re-
daktsionno-izdateliskogo soveta All USSR (for Culy.10'. 4. Uchenyy_sekretar?
AV USSR (for Bakulin). 5. Direktor instituta "Proyektstallkonstrukts3-,ya"'
(for Ibllnikov). 6. Predsedatel sektsii svarochnogo proizvodstva
Tekhniko-ekonomicheskogo soveta Loningradskogo sovnarkhoza (for
Okerblom). 7, Glavnyy svar;shchik Liralvagonzavoda (for Portnoy).
8. Glavnyy inzh. zavoda im-. Noseako (for TSyban,'). 9. Dallnevostoohnyy
politekhnicheakiy institut im. V.V.Kuybyshove. (for Kulikov).
10. DalIzavod (for ALronomov, Polyakov). 11. Dallnevostochnyy
nauchno-issledovateliskiy institut po,stroitellstvu (for Sherstyuk).
(Electric weldinU-PerlodivAls)

IOMILOV~ A.P.,, VARSITAVSKIY, S.L.; KTJLIKOVI M.T.; SHIRSOVO Yu.D.
Electrochemical mynthesis of hexamethylendiamine and amino
capronitrile. Xhim. prom. 41 no.5:329-333 My 165. (MM l8t6)

KULIKOVP M.V.
Turret equipment for lathes. Paiihinostroitell no.2124 F 164.
(MIRA 17:3)

hmiwv, ~i.v.
1111evT Data on BrachippoCies of the Terrogenic Phase of the Kungurski Belt on the
Western Slope of the Urals," Dok. All, 56, No. 6, 1947

- - kMI]Mlrg M, To - - - - - - -- - - - - - --- - - - - - - - - - - - -
-F~4'AV:.
1
Fauml Occwrsncss In ffylva. reefs, ft. TMBI Ob. ser. no.8s83-M
1489 (MIM MO
NVIT& valloy--Paleoutology) (Beef 8),

USSR/Geology Jul 48
Petrology
-Age of the Bylven Shelf," M. V. Kullkov, All-
Union Sol Res Geol Insto 11 pp
"Dok Ak Nauk SM" Vol LXI,.No 1
Some authors oonsider the Sylven reefs around
Mw2gur belong to the Ehngur layer of the Permian
system. Study of fauna led Willkor to conclude
that reefs are Upper Artinsklan. Submitted
6 may 1948.
______81_49T78

M. V.
USSR/000aw Der, ~.8
Stratification
"Most Becent ledges in the Urals,* M. 7, r-i.11kov,
4 pp
"Dok Ak Nauk SSSB" Vol LMI, No 4
Lists characteristics which distinguish more recent
ledges from ancient ones: a smaller range of qx-
tensign, closer location to one another, and differ-
ent types of fauna. Submitted by Acad D. V.
Nalivkin, 7 Oct 48.
45/49T52

-~ , 1,
1. h-IlLfKOV, M. V-
2. USSR (600)
4. Paleontoloa
7. State of Soviet paleontology. Izv. AN SSSR. Ser. biol. 11o. 5, 1952
9. Monthly List of Russian Accessians, Library of Congress, Janum,- 1953. Unclassified.

KULIKOV, M.Y.
Academician T.D. Lysenkole ONew aepecta of the biological Emecies* and
biostratigraphy. Zot.zhur. 38 no.):389-400 153. (KLaA 6:6)
1. VaesorivVy Oeologicheskty inatitut.Leningrad,
(Species, Origin of) (Paleontology)

KULIKOV, M.V.
",--
Licharewin or RugulAtin. Gsol.sbor.[Lvovj no-1:172-176 154.
(MIRA 1011)
(BrAchiapocirt, 'Possil)

Tx i-I _IXvF I

15-57-12-16783
Translation from: Referativn y zhurnal, Geologiyaj 1957, Nr 12,
p 12 (USSRT
AUTHOR: Kulikov, M. V.
TITLE: The Biostratigraphic Subdivision of the Permian Rocks
of the Kharaulakhskiye Mountains (Bio5tratigraficlie-
skoye raschleneniye permskikh otlozheniy Kharaulakh-
skikh gor)
PERIODICAL: Inform. sb. Vses. n.-i. geol. in-ta, 1955, Nr 4,
pp 20-27
ABSTRACT:
Card 1/3
As a result of the geological investigations of A. A.
Mezhvilk and of his determination of fossils collected
by the author, it has been possible to distinguish
Upper and Lower Permian rocks in the northern Kharau-
lakh region. The lowermost TiksinskEiya group (Sakmara
series) contains brAchiopods. It is overlain uncon-
formably by the widespread, richly fossiliferous

The Biostratigraphic Subdivision (Cont.) 15-57-12-16783
Verkhoyanskdya group, 270 m to 1400 m thick, which is especially rich
in Productus verchovanicus Frdcks, Rhynchopora labjaensis Tolm., and
Chonets brama Fred. In addition, Pseudorthoneras khoxense McChesney
and indi-vi-N-a-1 pelecypods and gastropods have also been found. By
comparing the fossils of this group with the Lower Permian forms
known in the Urals, it is possible to correlate the Verkhoyanskiy
group with the Arti and Kungurskiy series of the Urals. On the other
h~and, many species are present in the Verkhoyanskiy roup that have
been described from the Kolyma reka (River) basseyn fbasin), and -.
als6 from the Lower Permian of the trans-Baykal region. The presence
of local forms indicates that the fauna was developed not only by
migration, but also in local foci of specific evolution. The wide-
spread overlying Upper Permian Kharaulakh group is 150 m to 1100 m
thick, composed of sandstones, siltstones, and, to a lesser degree,
shales. Pelecypods and brachiopods are present. Of the brachiopods,
six species of the genus Kolymia have been found. Of speclal inter-
est are the absence of Prod'uctus verchoyanicus and the presence of
Strophalosia. This entire fauna is directly associated with the
Card 21 j

The Biostratigraphic Subdivision (Cont.)
15-57-12-16783
fauna of the Upper Permian Kolyma basseyn (basin) and has little in
common with the fauna of the Kazanskiy deposits of the Russian
platform. It is especially interesting that representatives of
Licharewia are completely absent, though they are widespread on the
platform, as well as in Novaya Zemlya, Taymyr, the Verkhoyanskiy
Range, and in the basseyn (basin) of the Kolyma reka (River). The
extensive development of Kolymia in the Kharaulakh region makes this
genus an important guide fossil for the Upper Permian.
Card 313 1 B. K. Likharev

KULIKOV, M.V.
Znhoritance of acquired characteristics by organisms. Mat.VSEGXI no.9:
222-228 155. (KIRA 9:9)
(Paleontology) (Heredity)

USSR/ Gf-, n !a U
Card 1/11 Pub. 22 - 34A7
Authors t Kulikov, M. V.
Title I data- on' bioqtratjgrarhic dissectJcn c.,r !-,e ia~n de;~os-
in north-
ern Verkhoym
Periodical s Dok. All SSER 101/6, 1101 - 1103, Apr. 2-1, 1955
Abstract I New geological data am precented regarding the biostratigraphic dissection
and the fauna of the Permian deposits discovered along the northern ~~--rts
of the Verkhoyan mountain range. Five USSR references (1931-1048).
Instit-Litirm : All-Union Sc. Res. Geol. inst., Leningrad
Px-eson!,,nd by: Academician N. M. Strakhov, December 23, 1954

KULIKOV. M.Y.
Interprotgtinn Of palsontolog7 In the *Referativnyi shurnalsof the
Academy of Sciences of the U.S.S.R. laform.sbor.VS1CdlI no.3:145-
146 '56. (PoLle onto logy-Torminolog7) (MLRA 10;1)

15-1957-7-8964
Translation from: Referativnyy zhurnal, Geologiya, 1957, Nr 7,
p 13 (USSR)
AUTHOR: Kulikov, M. V.
TITLE: New Data on the Uppdr Permian-Deposits of the Vayen'ga
River Basin (Novyye dannyye o verkhnepermskikh otlo-
zheniyakh basseyna r. Vayen'gi)
PERIODICAL: Inform. sb. Vses. n.-i. geol. in-t, 1956, Nr 4,
pp 3-5
ABSTRACT: A section is presented of the Upper Permian deposits
on the Vayen'ga River, a right-hand tributary of the
Northern Dvina, Ya. T. Bogachev (Byull. Moak. o-va
ispytateley prirody, Otd. geol., 1936, 14) considered
that the red layer A (Nizhneustlinskiy beries) lies
on an erosion surfacg in the carbonate layer A , and
g
eds is
that the marine facies of the Upper Kazanskiy
absent. As a matter of fac:t, the conglomerate indi-
Card 1/2 cated by Bogachev at the base of the red layer, cor-

15-1957-7-8964
New Data on the Upper Peruinn Deposits of the VayenIga River Basin
I(Cont.)
responding to the Nizhneustlinskiy series of the Tatar stage,
does not existq although the erosion surface at its base is
present. The underlying deposit-s (dolomitized limestones)
are to be referred to the Upper Kazanskiy substage, inasmuch
as Lower Kazanskiy rocks with Licharewin and Permospirifer
are not exposed here.
Card 2/2 B. K. Likharev

KULIKOV, N.Y.
~ -~ -
Biontratigraphle correlation of Permian deposits in the Xbaraulakh
R&nV. Inform. abor. VSZG3I no.4:20-27 156. (KM 10:4)
(Zharaulakh Range-Paleontology, Stratigraphic)

XULIKOV, M.V.
Abnormal situation in regard to abstracting of paleontological vorks i12
the"Journal of abstracts of the Acadeny of Sciences of the U,S.S.R.0
Izv.AN SSSR.Ser.gool.21 no.3:116-117 Mr 156. (MM 9;7)
l.Vaesoyuznyy goologicheskiy inatitut, Leningrad.
(ftleontology-Abstracting and indexing)

KULIKOV, M.V.
N.N. IAkovlev# the outstanding Soviet paleontologist, as a teacher,
public figure, and pedagogue; on his 85th birthda7. Geol. abor. LImovJ
no.4:375-379 '57. OURA 13:2)
l.Vaeso7uzny7 geologicheski7 nauchno-issledovatellskI7 InstItut*
(lAkovleT, Hikolai Nikolaevich, 1870-)

AUTHORS: Kozubova, L. A., Kulikov, M. V. SOV/2o-121-4-38/54
TITLE: New Data on the P Deposits of West Transbaikalia
(Novyye dannyye o permakikh otlozheniyakh Zapadnogo Zabaykallya)
PERIODICAL- Doklady.Lkademii nauk SSSR, 1958, Vol. 121, Nr 4,
PP- 712 - 715 (USSR)
ABSTRACT: In the survey of publications given by the authors (Refs 1,5)
the position of the paleontologically characterized wediments
of the area mentioned in the title is not clear. D. F.
Maslennikov used his monography of brachiopodes and mollusks
as a basis and classified them among the Lower Permian (1952).
Referring to findings made by A.D.Shcheglov (1955), M.V.
Kulikov claimed that these strata were furmed in the Upper
Permian. Yu.P.Denlgin (1956) separated Permian deposits
for the first time. In order to b.) able to prove this deposit
of Upper Permian in this area the first author carried out
a detailed geological investigation in the lower course of
the river Mergen'* The position of the Permian sediments
on a washed out granite surface was determined by means of
Card 1/3 an average cross-section on a geological map (Fig 1); the

New Data on the Permian Deposits of West Transbaikalia S07/2o-1,21-4-38/:~'
_j "
fauna was stratawise collected. Its investigation made
possible the separation between Lower and Upper Permian.
Lower Permian : Total heiglit 100 m. Upper Permian has a
height of 100 m . The sediments characteristic Of the
lower part of the Lower Permian are apparently lacking.
An exact lithologIcal description of the above mentioned
strata is given and the fossils found are mentioned. The
origin of the Permian fauna of this area is interesting
in connection with its geographical position. According
to reference 3 the encroachment of the Permian Sea came from
the Indo-Pacific area (Indo-Tikhookeanakaya ProvintrLya ).
The sea penetrated into Transbaikalia, in the Dzhungariya
and further until the Ural. These assumptions proved to be
wrong. The authors proved that the composition of the Trans-
baikalian fauna is not related rith the Permian faiLna of the
Northeast of the USSR. It is Most probable that the migration
of the fauna to Transbaikalia in'the' Permian started in the
North, the Mongol o-Okhot 3 kaya geosynaline (Mongolo-0khots-
kaya geosinklinall) where it had developed and lead to a
number of local species which are closely related to the
Card 2/3 species formed in the Permian of the Vortheaut.

4-78/54
New Data on the Permian Deposits of West Transb--ikalia SOV/2o-121- , ,
There are 1 figure and 5 references, 5 of which are Soviet.
ASSOCIATION: Vsesoyuznyy nauchno-isaledovatellskiy geologicheakiy institut
(All-Union Scientific Research Institute of Geology)
PRESENTED; April 3, 1958, by S.I.Mironov, Mei;iber, Academy of Scie,.ices, USSR
SUBMITTED: April 3, 1958
Card 3/3

30) SOV/20-123-6-39/50
AUTHORS; Kulikov, M. V., Tulokhonov, M. I.
TITLE: Permian Deposits of the Chironskoye Field (East Transbuykal)
(Permskiye otlozheniya Chironskogo polya (Vostochnoye Zabaykallye))
PERIODICAL: Doklady Akademii nauk 35SR0 1956, Vol 123, Nr 6, PP 1100-1103
(USSR)
ABSTRACT: Marine sediments are known in the above mentioned area at two
places ("fields" in geological literature): a) Chironskoye and
b) Borzinskoye. According to a litera,ture review since 1928
(Yu. M. Sheynman, S. A. Muzylev, G. S. Kryazhev, I. V. Luchitskiy,
S. P. Smelovskiy, D. F. Maalennikov, the last one by Ref 1)
about the exploration of the Chironskaye field, the authors
report about the results of geological fieldwork and mapping
during 1955-1957 by M. I. Tulokhonov. The pale ontological
material was studied by M. - V. Kulikov. The new data given by
him cau-s~d'essential corrections of the lithological character-
istics of the rocks, of the thickness as well as of the strati-
graphical position of the suites, which are known in this area.
L o w e r P e r m i a n . Two uuites belong to the Lower
Card 1/3 Permiant a) Chironskaya with a thickness of 400 - 900 m and

SOV/20-123-6-39/50
Permian Deposita of the Chironskoye Field (East Transbaykal)
b) Ungadyyokaya with a thickness of 370 - 400 m. They are
covering metamorphic schists of the Ononskaya suite with a
sharp angiflar-discordance. U p p e r P e r m i a n is repre-
sented by the Bereinskaya suite only (450 - 500 m thick). All
-the mentioned suites were described lithologically and paleonto-
logically. According to the above mentioned new reports the
Permian sediments have a much greater thickness than
D. F. Maslennikov thought. They are paleontologically classi-
fied everywhere. One part of the sediments, which Maslennikov
put into Trias conditionally, was put in the Upper Permian
after determination of the fauna. The two fields are very
similar to each other, lithologically speaking. But thty differ
from each other by the effusives of the Borzinskoye fieldg to
which the volcanogenic tuffs in the Chironskoye field correspond.
The fauna of the Chironskoye field shows relations to the fauna
of the north-eaet of the USSR. The conclusione of Maslennikov
about the boreal character of the fauna of Transbaykal were
thereby proved. This fauna migrated along the Morgolo-Okhotskaya
geosynclinal zone. The same fauna complex is found in the
Card 2/3 Formian of the northern part of the Mongol'skaya Naro3naya

SOV120-123-6-39150
Permian Deposits of the Chironskoye Field (EaDt-TreAmbsykab)
Respublika (Mongolian People's Republic). The int(rpretation,
that a transgression of the Permian sea surrounded the whole
Mongolia from the south, is quite unfounded. As the fauna in the
southern Mongolia differs essentially from that of the northern
Mongolia, the authors followed the above mentioned ideas of
Maulennikov (Ref 1). According to that the Permian sea penetrat-
ed into Mongolia through Tr&n"aykal. There are 3 Soviet ref-
erences.
ASSOCIATIONt Vseooyuznyy nauchno-iouledovatellskiy geologicheakiy inutitut
(All-Union Scientific Goological Research-Institute)
Chitinskoye geologicheskoye upravleniye (Chita Geological
Administration)
PRESENTED: July 16, 1958, by S. I. Mironov, Academician
SUBMITTED: June 16, 1958
Card 3/3

3(5)
AUTHOR: Kulikov, M. V. SOV/20-125-5-35/61
TITLE: A Stratigraphic Diagram of the Permian Deposits of Transbai-
kalia (Stratigrafichookaya akhema permskikh otlozheniy Zabay-
kallya)
PERIODICAL: Doklady Akademii nauk SSSR, 1959, Vol 125, Nr 5, PP 1081-1004
(USS11)
ABSTRACT: Marine Permian sediments are known in Zabaykallye (Transbai-
kalia) as small, isolated outcrops. Their stratigraphic posi-
tion has remained unclear until recently (Refs 1,2,6-8). This
was chiefly due to the lack of a detailed study of the fauna.
The first monographic description of this fauna originated
from D. F. Maolennikov (according to Ref 3). He has contrasted
this fauna to the analogous fauna of other regions. In his
opinion the Permian fauna of Transbaikalia is, very similar
to that in the northeastern USSR. Detailed works were recently
undertaken in the Permian area in western an eastern Trans-
baikalia (Yu. P. Den'gin, L. A. Kozubova, M. I. Tulokhonov)
and fauna were stratigraphically collected. Their analysis
has shown that both Lower and Upper Permian occur here. The
Card 1/3 diagram cited reflects the marine Permian sediments (Tablel).

A'Stratigraphic Diagram of the Permian Deposits SOV/20-125-5-35/61
of Transbaikalia
East Transbaikalia 'Vest Trans-i
Age
Chironskoye Field Borzinakoye Fiei~ baikalia
Upper Bereinsk4ya Suite Borzinakaya Suite
Permian, 450-500 M thick 8160-m thick Gutays-
100-150 m
thick Fel4duyskaya
!.Suite 580 M thick kaya
Lower
Permian, Ungadyyslcaya buAe Kharanorskaya Suite
thickness 370-400 11 thick
suite 600 m thick
at least
100-150 m IChironskaya Suitel Kundoyskaya Suite-I
-900 M thick 5-m thick
140-0
Especially interesting is the discovery (by V. A. Amontov) of
Upper Paleozoic fusulinide in a limestone lense of the
Ust'Borzinskaya suite. The determinations originate from
L. P. Grozdilova. They are characteristic from the upper part
Card 2/3 of the Upper Carboniferous to the lower part of the

A Stratigraphic Diagram of the Permian Deposits SOV/20-125-5-35/61
of Transbaikalia
Sakmarskiy Stage. There are I table anki 8 Soviet references.
ASSOCIATION: Vsesoyuznyy nauchno-issledovatellskiy geologioheskiy institut
(All-Union Scientific Geologic Reaeai-ch Institute)
PRESENTED: December 29, 1958, by N. 11. Strakhov, Academician
SUBMITTED: October 6, 1958
Card 313

3 W~ 17 (4)
AUTHOR: Kul sov,/20-127-6-39/51

TITLE: On the Zoogeographic Regional Subdivision of the Northern Part
of the Kazan' Sea
PERIODICAL: Doklady Akademii nauk SSSR, 1959, Vol 127, Nr 6, pp 1283 - 1285
(USSR)
ABSTRACT: The epicontinental Kazan' Sea once covered an extensive area
on the Russian Platform. Only in the north it was connected by
~ narrow channel with the open Boreal Sea. Small water depths,
~ coastline with deep bays, and a warm moderate climate, great-
ly influenced the chemical composition of the sea water, and.
consequently the character of maritime sediments. The surroland-
ings again influenced the composition of the fauna and its
distribution over this specific water. According to A. V~
Ifechayev (Ref 1), and on the basis of his own investigations
of several years, the author subdivided the area mentioned in
the title. The area dealt with reaches from the western slope
of the southern Pritamanlye in the east to the drainage area
of the Severnaya (North) Dvina in the west, to the Sukhonskiy
Wall in the south, and to the continental part of the Russian
Card 1/3 Platform (except for the Kanin Peninsula) in the north. Or, the

On the Zoogeo--raphic Regional Subdivision of the SOV/20-127-6-39/51
Northern Part of the Kazan'.Sea
basis of abundant faunistic material, the author separates
4 zoogeographic regions: 1) V y m I a k i y in the drainage
area of the river Vymf. DurinE the Kazan' period, this section
of the sea bottom underwent several uplifts and depressions.
It had a coast-near character. The fauna was specific:
Pelecypoda prevailed. They were numerous and attained con-
siderable shell sizes. 2) P i n e z h s k i y R e g, i,o n in
the drainage area of the rivers: Pinega, Kuloy, and on the
middle course of the Vayentga. Probably this was the narrow
connecting channel mentioned. Small reefs with faunistic
settlements grow here. The fauna had a brachiopodous character.
Reticular and branched Bryozoa were manifold. Molluscs were
subordinate. The principal part among them was played by
Pelecypoda. The principal mass of Nautiloidea was described
by M. V. Kruglov on the basis of these finds. This rayon was
most favorable to the fauna, and therefore it was most abun-
dant here. Migration took plaoe here in both directions.
3) The V a z h a k i y R e~gi olay comprises the area west of
the northern Dvina including the drainage area cf the river
Card 2/3 Vaga. Pelecypoda prevailed here. Brachiopoda weie rare and

On the Zoogeographic Regional Subdivision of the SOV/20-127-6-39/51
Northern Part of the Kazan' Sea
poor in species. Bryozoa did not attain large dimensiona. Ac-
cording to K. V. Miklukho-Maklay, the foraminifers, had a dif.-
ferent character. In spite of the carbonate rocks, the shellv
of the fauna were not thick, 4) The S u k h o n a k i y
R e g i o ncomprises the so-called Sukhonskiy 'Nall, as well as
the drainage area of the river Toyma. Here, the Kazan' sedi-
ments do not appear on the surface. They are covered by a layer
of sediments of the Upper Permian and the Lower Mesozoic peri-
ods. The fauna is very poor here: 2 species of Brachiopoda,
rare Pelecypoda, and Bryozoa with a very thin skeleton. Appa-
rently, this was a lagoon area of the Kazan' Sea. Living condi-
tions for the fauna were most unfavorable here. There are 2
Soviet references.
ASSOCIATION: Vsesoyuznyy nauchno-issledovatWskiy geologicheakiy institut
(All-Union Scientific Geological Research Institute)
PRESENTED: May 28, 1959, by N. M. Strakhov, Academician
SUBMITTED: May 27, 1959
Card 3/3
YF,

XULROV, M. V.
Concerning V.T. Lipatovals article "Now data on the Kazan stage
In the Aktyubinsk area of the Ural Mountain regiom" 1xv. AN SM.
Ser. geol. 25 no-12:107-108 D 160. WU 13:11)
(Aktyubynak Province--Geology, Stratigraphic) '
(Lipatoya,, VsVo).
4,

KULIKOV, M.V.
Alekfiandra Vasillevna Nemilova; obituary. Sov.geol. 1+ no.12:
152-153 D 161. (11M 15:2)
1. Vaesoyuznqu geologichaskaya biblioteka.
(Hemilovaj, Aleksandra Vasillevna, 1892-196.1.)

KULIKOV, M.V.
Index to articles of the second series of the "Zapiski~ of the All-
Union Mineralogical Society, 1912-1957* Reviewed by 14.V.Kulikov.
Zap.Vses.min.ob-va 90 no.3:355-356 161. (MIRA 14:10)
(Mineralogy-Societies)