SCIENTIFIC ABSTRACT KHOMENKO, Z. S. - KHOMENYUK, V. V.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R000722220007-9
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: September 17, 2001
• Sequence Number: 7
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

BARBARRIA, T.M.; BUBYRI~ H.F.; BUTT, VEL'SOVSKIY, V.N.;
GORLOV, Yu.P.; GRIBMIOVSKIY, V.G.; DROZDOV, I.Ya.;
YEREI-J111, I.A... ZEN11, V.G.; KEVESH, P.D.; KOGELROV, E.P.;
KOSYREVA, Z.S.; LEVIN, S.N.; MAKIWOVICH, A.T.; MERZLYAK,
A.N.; RODOV, E.S.; ROZHNOV, A.I.; SEREBRYANSKAYA, B.I.;
SUKHAREV, M.F.; USTENKO, A.A.;
~ _A,.�,.j SHKIDT,
L.M.; ETIN, A.O.; YAKHONTOVA, N.Ye.; KITAYTSEV, Vladimir
Andreyevich) prof.2 dokt6r tekhn. nauk, red.; SKRkITAYEV,
B.G., glav. red.; TROKEIMOVSKAYA, I.P., zam. glav. red.;
KRAVCHENKO, I.V., red.; KITAYGORODSKIY, I.I., red.;
KRZHE14DISM , S.A., red.; ROUVARCM, Ye.L., red.;BALATIYEV,P.I.
red.
[Manual on the manufacture of heat insulating and acous-
tical materials) Spravochnik po proizvodstvu teploizo-
liatsionnykh i akusticheskikh materialov. Moskva, Stroi-
izdat, 1964. 524 p. (MIRA 18:1)

KROWK09 Z.--s.-
USSR/Chemistry - Hydrocarbons
Chemistry - Catalysts Feb 49
"Irreversible Catelyals-and- Ca-talytic Dehydro-genation of H.1drocarbons
on Activated Carbon, G. A. Rildakov, N. P. Borisova, 0. A. Temallyanova,
I. G. Yeroshevskiy, N. 1. Komshilov, A. N. Kakarova, N. M. Nerlis,
Z. S. Khomenko. Can Sci Res Inst of Wook-Pulp Chem, 181 PP
02hur PrWad Wa V01 XXII, RD 2
Investigation carried out on pure zterpenes and a naphthene hydrocarbon,
n-methane, showed that activated carbon brings about irreversible catalysis
and dehydrogenation of hydrocarbons. This confirmed conclusions made
long ago by kassian scientists working on pyrolysis of petroleum.
Describes reactions in detail. Submitted 13 Mr 48.
PA 48/49T19

R Chemistry Catalysts
Card 1/1 Pub 151-- 29/38
.Authors. Rudakov, G. -A., and Khomenkol Z. S.
Title The nature of catalysts Iused for isor-orization and pol-3ime-ri7ation of hydro-
carbons. Part l.-.Cause for catalytic activity of titanic acid
Periodical I Zhur. ob. khim. 24/2~,.: 337-343, Feb 1954
Abstract I The catalytic aIctivity oftitanic acid in the isomerization of pinene was com-;
pared with that of aluminum silicate catalysts. The activity of -the titanic
catalystwas found to be,due mainly to its acid properties, The derivation of
active titanic acid through electro-dialysis with soditun salt proves that the
activity of theji~catalyst is caused mostly by the characteriatics of the ti-
tanic acid and not~by tha presence of adsorbed acids or basic salts. The high
catalytic activity and: plainly expreased acidity make titanic acid clo~!elyre-
lated to alumirram. silicates and not toAts clorest analogues - silicic acid
-6urtoen referenc -U'SR; 1-1J,5A and I-English (M91-
and aqueous A1201. r es: 12
.1953). Tables graphs.
Institution Central Scientific Research Forest-Chemical Institute
Submitted July 6, 1953

/VI/
USSR/ Chemistr7 - Catalytic isomarization
Card 1/1 Pub..151 -~-.31/37
Authors Rudakov,,~G. A.; Khomonko., Z.-S.; and Shostayeva, M. M.
Title Mechanism of heterogeneous catalytic hydrocarbon isomerization over
acid catalysts. Part I.-
Periodical -Zhur. ob. khim. 24/3) 549-557,01ar 1954
Abstract The mechanism ofreaction betweer. pinene, camphene and limo Inenevith cat-
alysts'resulting in their isomerization (titanic acid and activated lime)
was investigated. . It-vms observed that all three Irydrocarbons tested
isomerizo.rapid3,y and.two of them racemize when heated Uith titanic arid,.
Camphene and limonene~formed.during catalytic isomerization of pinene over
activated lime (1250) and over titanic acid (135~-1600) will not react With
above mentioned catalysts until the pineno concentration in the reaction
mixture-is reduced to'25-3~%. . ItAms found.that the isomerization reaction
takes place only~ -on 'the surface of the catalyst and does not penetrate into
the volturoo Seventeen references: 9-USSR,- 2-USA; 2-Garman and 4~English
(1891-1953). Tables; graphs.
Institution Central Scientific Research Forest Chemical Institute
Submitted, July 212 1953

Authors Radakov., 0. A., Shesta.evaj M. M., Marchevskiy, A. and Mvnerko, Z so
Title Mechanism Of heterogonecas oatalytio isomerization of hydrocarbons over
acid.catalysts' Part 2.- Formation of terpinolene and terpinenes during,
catalytic iso;~rization of pinene and AMDnene over titanic acid,
Periodical Zhur. ob. khim. 24/8, 1452 -:1457s August 1954
Abotract i The ionic.scheme oUf6rmation of terpinolenes and terpinenesi as result.
of catalytic isomerization of pinene and.limonene over atitanic acid
catalyst is explained, Direct conversion of pinene and limonew -into -
alpha-teerpinene,~without the formation of terpinolene as an intermediate
product, was established. The increase of the alpha-terpinene content, ,
in monocyclic terpenes., after reducing the pinene content in the.86lution
its effect.on the formation of alpha-terpinenes from terpinolenep
are explained, Ten references: 5 USSR; 3.USA; 1 German and 1 English,
(1899 1954). lable; graph.
institution Central Scientific-Research Wood Pdlp Che-mical Institute
Submitted January- 13P 1954

KHOMENKC, Z. S.
KHOMENYO, Z. S. -- "Perfecting the Industrial Technique of Isomerization of
Pinene to Produce Camphene." Min Higher Education USSR. Sverdlovsk, 2955.
(Dissertation for the Degree of Cndidate in Technical Sciences).
So.; Knizhnaya Litopis'. No. 7. 1956.

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exclutfige resills b"Thig 340fuilic. grallp-i (IV); 2% Ivater N~&i
ill Ill, all.1 a highrr dibl, Was pirvelkii-st by lbu
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widis 11w favoi:,14 - coodidooi thc %-;, I'l
and
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voli'liNals will; shiggi-Ak awing ((I Ow gut-'Wt of W;'Ovir
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TT-aF-'Zr~'l:#5V---fte ester% are alutaitted by treating cim-
Olene with an r- of a haglAy cx~!wd OTA. acift ill fll~
presencc of a catalyst imsol. in we re~lctwg quhiuvice~. Al
cata!yst rarz be used cation exchanzr resiris or ~Iulauled
coal, ~Jjtcr t1w CUMPIC63a CA (Im r'~-.miuu u'le exce-.L9 acid
is t1riven OtT. Cf. Cj. 50, 0~1,

KHO14ENKOP Z.B.; OTLIVANCHIK, A.N.; KORCHAGINAO I.A.; MAKAROVAO M.M.
-- z----
Fibrous slabs made of straw, Stroi, mate 7 no.7sl4-15 JI
161. (MIRA 14:7)
(Straw) (Building materials)
0

hMOMMTK0_, y kand. tekhn. nauk; BUKHAREVA, B.V.,, inzh.;
GURVICH~ B.A., red.; ERUSINA, L.N.p tekhn. red.
[Structural fiber slabs of reeds and straw] Stroitellpye
voloknistye plity iz kanWsha i solonT. Moskva, Gosstroi-
izdat, 1963. 51 P. (MIRA 17:2)

KHOIENKO, Z.S-~.P..kand. tekhn. nauk; pROTOPOPOV, JUN.) inzh.; BYWREVA, B.V-.,
inzh.
oards resistant to micro-orgmLsms. Sbor. trua.
Producing fiberb (MJRA 17:11)
VNIINSM no.7.'59-64 163.

fT
fi-b(xbcard:3 from r-,olr al"d IJ 53 -b0-, - JnfO'
Vtilllf,'314 no.14:27-34 'i~ lev-3)

KHOKIKOV, L.
Track Athletics
Path to victory, Mol. kolkh, Noo 3, 1952.
Moithly List of Russian Accessions, Library of Congress, May 1952, Unclassified.

MOMINKOVA, I.G., Inzhetier.
Using the method of statistical control for evaluati3g shoo quAlity.
Standartizateiin no.4*42-45 Je-Ag 157. (KLRA 10:9)
(Shoe industry) (Sampling (Ststistias))

KMKBNMVA, I.Ge, inzh,; GORSHKOV. S.I., Imnd.biol. nauk.
- - -----
Physiological considerations for manufacturing more flexible shoes.
Nauch.-imal. trudy MIKP no.28:131-13 '57. (min 11: 10-).
I (Boots and shoesT -

P-AffiO'XY'Othylbls(a -61aroothy0arniplys-
K. K. Khomen-
kova and
Ru--slan).-(CICH,CTl,).N beated with ROH
tc- 2 the fcatc-ming Ro(cll~)~N(Cll.cll,cl)- (R and m p
!of HCI sA given): Ht, 134'; isk)-Pr, 15:1'; Bts, IN';
!rtNfccflc,lT,, 12"V; CJi". 115,: CJI"ClIhIc, ll,~.5*;
Ctl,:CIICII,, 121.ry'; cycl.lwxyl, 150': NMI, 112-130;
(phcffo(clflMIN(ClJ,,WJi 77-8'. Tim compts. inay be
USeful la the treatmmt of malignut neoplwims.
j rj-Bas,,P--qco~t
I Ukrainskiy nauChno-iseledovatellskiy sanitarno-khtmichealcly-.-
i;stltut.

XORMT, I.A. . KNOMMOVA. I.I.
Synthesis of some chloroalkylminas of the pyriaidine series.
Zhur.prikl.khln,, 33 n0,7:347-350 A 060.
. (KM 13:7)
1. Ukrainskiy rauchno-Iseledovatellskiy sanitarno-kbimichonkly
InstItut.
(Amines) (Pyrialdlw)

ADROVA, N,A.;_~LONEMOVAl- K.& ----
Synthasis of some derivatives of p-virtylbenzoic acid. Zhur.obkhim.
32 no.7:2267-2268 JI 162. (MM 15:7)
1. Institut vyookomolakulyarnykh sovadineniy AN SSSR.
(Benzoic aeMY
-,;,- ..
7"*. -

ADROVA~ N.A.; KHOIENKOVA,,--K.,K.; DUBNOVA, A.M.
Synthesis of new derivatives of p-vinylbenzoic acid. Zhur.
ob. khim. 34 no. 5tl545-1546 My 164. (KRA 17:7)
1. Institut vyBokomolekulyarnykh soyedineniy AN 3.13SR.

ACCESSION NR: AT4020708 S/0000/63/000/000/0195/0197
AUTHOR: Koton, M. M.; Adrova, N. A.; Khomenkova, K. K.
TITLE: Polymerization of some derivatives of p-vinylbenzoic acid
SOURCE: Karbotsepny*ye vy*sokomolekulyarn)dcye soyedineniya (Carbon-chain macro-
molecular compounds); sbornik statey. Moscow, lzd-vo AN SSSR, 1963, 195-197
TOPIC TAGS: polymerization, vin~lbenzoic*acid, vinylbenzoate, vinylbenzamide,
polymer physical property, polyvinylbenzoate, dilatometry, azodiisobutyronitrile,
butyl peroxide, block polymerization
ABSTRACT: Using a dilatometric method, the a uthors compared the block and liquid-
phase polymerization rates of p-vinylbenzolc acid, its methyl and amyl esters,
p-vinylbenzamide and its N-methyl, N,N-dimethyl and N-amyl derivatives, using
i 0.2 mol.% tert.-butyl peroxide or azodlisobutyronitrile as the initiators, respec-
tively, at 120-180C. Some of the physical properties (thermal stability, solu-
'bility, weight loss during heating) of the polymers obtained were also studied.
The polymerization rate'of e derivatives of p-vi6ylbenzoic acid decreased in
the following order: acid amides esters. It was found that the polymerized
amides of p-vinylbenzoic acid have ~h`igher softening point and a higher thermal
sbab'ljty than the corresponding polymerized esters. Orig. art. has: I figure
Cor

ACCESSION NR; AT4020708
and I table.
ASSOCIATION: Institut vy*sok(xnolekulyarny*kh soyedineniy AN'SSSR (institute
of Macromolecu)ar Compounds, AN SSSR)
.SUBMITTED: 18Jun62 DATE ACQ: 20Mar64 ENCL: 00'
SUB CODE; OC NO REF SOV: 002 OTHER: 004
Card 2/2

7 __7 ------
L 19760-6 PC
RPI,
WW/WMK
ACCESSION'Mt-.TI41H 000/64/000/000/0257/0259
5/0
ATIT1101t: Adrova, 94 K~ 2tloh~"If* Khome K. K.
TITIX: Reaction of pUl -ii-VIDIMenzovi chloridellmith alcohols and amince
$01MCF.. 1(himichook,lye svoyetva -1. modtfikatslyn polimerov (Chemical properUe s-And the
mmlif lentlowof polymcTs);'abornI,k stateys Moscow. lzd-vo Nauka, 1964,
TOPIC TAGS: vinylix'"zole acid,- poljMnylWnxoyl chloride, polyac.0 chloride,
vnterl f i cation# nivildation, polymer thermostability
ABSTRACT.- Under refluxInOctrahydroruran solution, poly-p-vinylbenzoyl chloride, pro-
pared by polynierizing the monomv at IOOC with 0. 2 mol. % azodisobutyronitrile, gave
polymeric 0 -viny-11MIlzoateAvith d -N-n- lbenztunide
T thyl p_ - ry- methanol. and Ir- amyl-p-viny
-.with, n-anvylamine.: nothermal7tability of the polyam Ide -was- improved by-partial
Ir
dCILMInation.~ `-Yfolds 0M.- I PO Y-p- fivIlreni6y! chloride and 5 ml amylamine or 10 ml
methanol Woke -0. 7 g of thebenzarntdo or 0. 8 9 of the methyl ester, respectively. Trt-
uthylamIne was added-in both readtlons to neutralize liberated HCI. Poly-N-n-amyl-p-:
vinylbenzamide was also prepared by a seeond route by polymerizing the monomer at 900
with axodisobutyronitrile in d(methyi(ormanide solution, yielding -after approximately 19%
deamination by 2 hro., of heating at 280-300C In argon under 8-10 mm. Hg pressure, a -
C.rd 1/2

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L IA73-66 Ewvm) AWOV
ACC NR: AP5025346 SOURCS GODEs UR/0366/65/001/010/1742/1743
AUTHORs Chovnikp L. L; Pazenkop Z, N,; Kornevp K. A~;~,1hggWjU-,
A ORG: Institute of Chemistry of Hie-Moleculdr-ftight Compounds. Academy of
�ciet rcea, Ukrallaian SSR kinstitut khimii vysokomolekulyarnykh soyedineniy Akademii
nauk Ukrainskoy SSR)
TITLEs Synthesis of 5-milw~1-123-di!IIZlisoovanurates
SOURCEt Zhurnal organichaskoy khimii,, ve 1, no* lop 1965, 1742-1743
TOPIG TAM copolymerizationy copolymer,, polymer, heat resistance, chemical
I reaction, heterocyclic base,compound
LBSTRAM-The title compounds W are heavy liquids of a characteristic odor;
,C interest as potential grafting agents for the production or imat_-_
they are
resistantj~~polymers. 'The syntheses were carried out by the reaction of an alJwl
bromide witfi~ii-Na 6ailt of a diallyllsocyanurate in HCCNMq 9. 41.8
diallylisocyanurate (see Franaier T.C. at al., J, Org. 25 1944, 1990) was
Card 1/2 UDC 1--- -547-491*3.

t 16173-66
ACC NR: 025346
mixed with 130 ml waterj-8 gNaOH were added; and the mixture was heated, filteredpt
and evaporated. The residue was dried at 900 to yield 45 g 1,3-diallylisocya-
and the hot soluti
nurate Na salt. This (56 g) was dissolvel In HCCNH32 on treated
d the
with 35 g PrBr. After 3-5 minutes of hsatingp NaBr was filtered aff, an
!filtrate evaporated under reduced pressure to give 56 9 5-propyl-1,3-diallyligo-
1cy,5nur 00 Similarly were synthesized the following I (alkyl %.Yialdp b.P.C/mm,
I nD given)s methyl, -9 3.24/29 1.5145, 1.1956; ethyl, 94: 113/0-5, 1-5145j
1,1956; propyl, 90# 136/2p 1.5000, LlW; butyl,72, 140/2, 1.4970, 1.1248;
isobutyl, 67,, 139/1 (m.p. 26),-, -; amyl, 82, 136/1 (m.p. 16), 1.49620-,- hevlp 790
156/2, 1.4940P 1.0909; heptvlj, 890 14/11 1.4919; 1.0720; octy1p 969
~1-4900) 1.0560; nonylp 167/2p 1*4890j, 1.0466; decylp 58.. 172/2,, 1.4879p 1.0305,
All the compounds synthesized were capable of copolymerization*// Orig.'~jt. has:
1 table.
Lf ~j
SUB CODE: SUBM DATEs 09Sep64/-, ORIG ~AF: OM/ OTH REF: 003
6,d

1-Ha:-"-Y0V4, 1111- '-
J.
Shoe Industry
Efficient utilization of cheeks and faces of hides, Lea. prom., 12, No. 6, 1952.
Monthly List of Russian Accessions, Library of Congress, October 1952. Unclassified.

. i
; ; .~ ~,; , 1, .
t, 1~;i. /II.I.Iv Y,I,,I
XHCHMOVA:,N.G., inzhener
WWWW&O"a";
Factors influencing the flexibility of welt shoes. leg.vrom.
15 no.8:30-31 Ag '55. (MLRA 8:10)
(Shoe industry)

b Ki 1-' K C K"
AUTHORs Khomenkoval N.G., Engineer, 28-4-11/35
TITLEs Application of Statistical Inspection Methods in the Evaluation
of Footwear quality (Primeneniye metodov statisticheekogo
kontrolys pri otsenke kaohestva obuvi)
PBRIODICALs Standartizatsiya, 1957t # 4, PP 42-45 (USSR)
ABSTRACTi The present-standards for footwear contain only technological
norms and descriptions of material and finished product. Para-
meters for determination of flexibility (Ref. 2 and 3) have
now been developed. The article contains a detailed desorip-
tion of a now device for testing this flexibility of shoes
(Fig. 2).
An investigation proved that stiff shoes require more energy
in walking and wear out faster than flexible shoes. The
measuring device indicates the effort required to bend a shoo
to a 250 angle. This method was applied in a mass 2-3 week
test on 0.5% of the total output of welted or rand-soled
men's shoes at the factories "Skorokhod", "Parizhskaya Kommunall
and imeni Kspranov. Altogether, 378 half-pairs of leather-
soled shoes at "Skorokhod" and 11Pa3Jzhskaya Kommunall and 312
half-pairs of foam rubber soled shoes at "Parizhakaya Kommunall
Card 1/2 and the factory imeni Kapranov were tested. All had approxi-

KHOMOVA, N. G.: Master Tech Sci (dise) -- "Investigation of the strength
of welt shoes an& its effect on the wearing of leather soles". Moscow, 1958.
10 pp (Min Higher Educ USSR., Moscow Technological Inst of TAght Industry),
130 copies (m, ?io 4, 1959p 128)

KOM EIVKOVA~
AUTHORSi
TITLEt
PZRIODICALs
X I Irl
28-5e-1-9/34
Zakatoya, N.D., :and Gubarev7, A.S9 I Candidates of Technical
Sciences, and Khomenkova, N.G., Engineer
A New System of Sampling Chrome Leather (Novaya ekhema ot-
bora prob khromovykh kozh)
StandartizatsiYa, 1958P # 1, PP 29-30 (USSR)
ABSTRACTs The article describes a new system of sampling chrome
loathert developed by the Tsentrallayy nauchno-iosladovatelf-
ekiy institut khozhevenno-obuvnoy promyshlennosti (Central
Scientific Research Institute of the Leather-and-Shoe In-
dustry). The now system consists in using a slightly smal-
ler size of samples# as shown in the illustration (Figure 1).
Testa at 6 different plants showed, that this system re-
duces waste and gives a more correct evaluation of smaller
hides. The article includes a chart showing test resultm.
A corresponding amendment is suggested for the "GOST 938-45"-
standard.
Card 1/2 There are 2 figures and I chart,

SERGEUVP M.o prof.; KROMENKOVAt N.v inzh,j
Hardness is an important indicator of the quality of shoes,
Sov. torg. 34 no. 1:44-46 A 161. (MIRA 14:1)
(Boots and shoes-Specifications)
*, 4

HaMOK, V-P-9 kand.med.naukp podpolkovnik med.oluzhby
Mechaniom of the excoriation of the wo gins of a bullet vound
caused by a point-blank shot from a Kalashnikov automatic gun;
according to data of a high-speed motion picture. Sbor.nauche
trudeXievookrushevoenegoope no-41353-356 t62. (MM& 1685)
(MMSIIOT 'WOUNDS)

KHOI-1310K, V.P. (Kiyev)
I
Mothod of study of the vessels of the heart and kidneys by
means of liquid rubber injectlon and sulx~equent use of
corros-1hre preparations. &-kh. pat. no.1.2-.78-82 162
(MIPIk 18:1)

--KHOME14TAUSUSp T. [Homentauskasp T.1
Mo re products for people. ~TO 3 no. 101 A 161. (MM 14:2)
1. Ucherqy m9kretar' ayaso-solochnoy sektoii Litovskogo
reepublWwko promphlemosti.,
(Lithuania-Dairy p-oducts)

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KHOM M OVSKIY, A.S.
Khomentovskiy, A.S. "The carbonaceous deposits of the Chkalovsk oblast, their
geography and mining prospects," Izvestiya Chkal. otd. (Geogr. o-v* SSSR), Istue 1,
1948, p. 25-38 - Bibliog: 6 items
SO: U-2888, Letople Zhurnallnykh Statey, So. 1, 1949

KHOMENTOVSKIY, A.S.
Khomentovskiy, A.S. "The Gavrilovsk mineral deposit," Izvestiya Chkalov.
otd. (Geog. o-ve SSR), Issue 1. 1948, P. 51-60
SO: U-2888. Letople Zhurnalinykh Statey, No. 1, 1949

KHOMIiNTOVSKIY, ;'. -
.i 3.
42126 KHO~!ENTOVS)KIY, A. 13. 7 rredgornyye vpadiny i twh-mosnost.1 (5 primech. red) Trudy
Geol.-issled. -Pyuro (Mvo ugolinoy prom-sti Z~p. r-nov SISR, Geol.-razvedoch. upr.),
Vyp. 4, 1946, c,17-26. - Bibliogr: r, MAN. 1;,I .
walk - --tl ,,,/ /,I,I. If ~ Ac-, , ? " 1,1~
- ;, ~. f'~, ~-*I.-;J~~ ~, C I," i, ~., ."', :!~ b- _-i, " ~.Jafljl
~ ~- 1;- I . .
SO: LetopistZhurnallnykh Statey, Vol. 4?, 1948

1. KIMMIRITOVSKIYt A. S.
2. USSR (600)
4. Geology and Geography
7. Orenburg Steppes In the Works cf P. L Rychkov, E. A. Eversman, S. S. Neustruyev.
By F. N. Milkov (Doctor of Geographical Scienees; editor, ccrotentator and
author of introduction). (Moscow, Geography Press, 1949). Reviewed by A. S.
Khomentovskiy. Sov. Kniga, No. 5x 1950.
9.4M Report U-3081, 16 Jan. 1953. Unclassified.

6.3, ig5o p
.79
Description of origin of.'the thick strata of the Cambrian platfom In 15
northern foothills of Eastern Sayan and in the dcrwnstreams of the Tumar.shet and
Tagul Riven3 in EaBtern Siberia., which platform is covered with a noncc,nforndng angle
by the -D6Vo-jjJU-*- an accumulation od~'4amb-L-lian-4epos-lts,.----
in a mobile depression arising-at. the end of the Proterozoic and PM-Cembrian
folding zonI3, which,paIss,ed*al6n he-sIouthwestern pasrt of the Siberiali.-platf6rm.,
States that fomqtion of Eastern Sayan is made up of two folded bel ts northeast
Pre-CambrLan and southwest - Caledonian,
253T104
40
!I ;t-7
K14t)W"Ir, IT07MY -A- S'.

KHOMENTOVSKIY, A.S.
Most recent movements of the earth's crust within the limits of certain
saline structures of the southern Ural foothills. Biul.NOIP. Otd.geol.
28 no.4:$-20 053. (NUU 6:9)
(Ural Hountains--gubsidences (Ikrth movements) (Subsidences (Zarth
movements)--Ural Mountains)

K1T(MT-'NT0V.cK1Y, A, S.
Dissertation: -- "The Regularity of Arrangement of the Lignite Deposits of the '
Southern Ural Coal Fields In Relation to Its Structure and Tectonic Development."
Dr Geol-Min Scip Inst of Geological Sciencesj Acad Sci USSRp 17 Jun 54. (Vechernyaya
Moskva, Moscow, 8 Jun 54)
SO: Sum 318, 23 Dec. 10.54

RAKOYl B.N.9 km~d.tckl~~.n"9%L,'A~~(SHW, B.G., profs, doktor tekhaasuk;
ANKOWF. 1. r., doktor geol.-min.umuk; AWRIYWSKIT, V.De, insbsi
AMMAM# Atle, Inshol AFARASIM, BeLet Inshol BMGKAN# Ye.T.,
lashq IMM, To.Ye.. insh.; BOGACKMA, U.N., insh,j DMIMITIT.A.,
kind stekba onmuk I VASIL'YHV, ?.V., doktor gool.-min.mmuk; VINWRADOT.
3,Go# Inshol OCUMN, 84., inahs-, OORDIYIKC, P.D,, inshol GUSNj N*A.g
kandstekbusnaukl 11CHM1110 I.V.g kandejecl. -win sumuk I KAINTIOV0 G*1.0
inshal SAIATOCHKIN, V.I., doktor khts.muk; KCIROLIT, I.T., inuh.;
XONS&MBUp A*As, Insh.1 ]D?ATXOVBXIY, LJ.0 tnsh4; DAIHIMINIECT, G*P,,,
prota',Uktor jeolo-min,nauk; MIKUMOV, L.A., insh.; LMVIT, D.Ye.0 insh.1
101212"1 1*099 kand.tokhn.nauk; LUSHNIKOV, V.A., Who; MATMEY, A.99s,
dotes@ kondegeols-minonsuk; MIMIBHVILI, Moms tanhol KUM=$ I.Tog
lumbel MOLONANOV, I.I., irnh,l SUMOVA. SoNe, stershiy nawhqy satradulk;
XKZPZW, T.Ye.~ insh.. PAYWY, F.F., doktor takhususukl FAN=QT, Poles
daktor goals-minensuki POPOV, V.S., insh.; PYATLIN, N.Peg kendetektas
nsukj UBHXMKIY, Yo.B., inshel RMANOV, V*A*, profs, doktor teftne
mak J1TWW9 FeAes prof., doktor tekhmenauk; BILTATITNICIY# O,Aeg imsh,11
=
MlYo N*A* Inshol TMMiT#Ylffo Y*oT*g inshol TIM9 M.gdaktor
khtviownukl OM&, I,P,, insho %20YANIKIYe B-T-0 prefti doMer goals-
C4 e:0,1300WO B.D., dote@, kondstekhasumuklUDORCY. T.N., task,
So 1143 011MMUM, A.Boo prof to daktor Cool*-%tn#vAukl TROTAM-
WTI Me TW ZOOM o A.Mej reds; UZVJNQTo TivAs,
rod )I zi& WF# I.As, red.; MIRONCY, X.Tv, rods; AVUSHIS& 8*0*g redo;
Sm8wv,X.P,o rod.1 VAUILOYLYl P.V,, redol MOICHANOT, Isle, redal
RYZHDT, P.A99 redel BAIAMIN, V.V., inshes redo; DIM, I.M., kand.
toNagouko redel SUIRINSKIYg V,At, kandetelchusuruki redel TOLKOT, 16*-Yu.,
insh.g Pedal YMMIYEV, A.Ao, inshso reds; ZVOMM, I.A#,-Vrds doktor
tekbnansuk.-rede 1C^M-.4vn%aA nvk ~&" mmwAl

ABRAMOV, (continued) Card 2.
ZDANOVICH, Y.G., prof.,doktor tekhn.naukired.; IYANOV, G.A.. doictor
geol.-min.nauk, red.; KARAVAYEV, N.M., red.; KOROTKOV, G.Y.9 kandegoole-
min.nauk. red.; KOROTKOV, M.V., kand.tekhn.nauk. red.; HAHATEM. A.A..
doktor geol.-min.nauk, red.; OMELICRUKO. A.11..kand.tekhn.nauk,rsd.;
SENDERZON, H.M.,kand.geol.-min.nauk. red.; USHAKOV, LK., dote., kand.
tekhn.nauk, red.; YABLOKOV. V.S.. ka nd.geol.-min rouk, red.; KOROLWA.
T.I.. redizd-va; KAGHALKINA, V.I., red.izd-va; FROZOROVSKAYA, F.L.,
tekhn.red.; NADHINSKAYA, A.A., tekhn.red.
[Mining; an encyclopedia handbook] Gornoe delo; entsiklopedicheskii
apravochnik. Glav. red. A.M.Terpigorev. Moskva, Goo.nauchno-tekhn.
izd-vo lit-ry po ugollnoi prou7shl. Vol.2. [Geology of coal deposits
and aurvey'lngl Geologiia ugolinykh mostor'ozhdonii i marksheiderskoe
delo. Rodkolegila tomm S.Y.Troianskiy, 1957. &6 p. (MIRA 11:5)
1. Chlen-korrem ondent AN SSSR (for raravaiev)
Mal geology-Dictionaries

K1101,1114INTOVSKIY, A.S., nauchn. red.; SHPAKOVSKAYA, L.I., red.
(Geology and conditions governing sedimertation in the
Suchan coal basin] Geologicheskoe stroenie I. usloviia
osadkonakopleniia na territorii Suchanskogo kwrennougoll-
nogo basseina. Novosibirsk, Red.-izd. otdel Sibirskogo
otd-tiiia AN, SSSR, 1964. 231 P. (11,111HA 18:1)
1. Akademiya nauk SSSR. Sibirskoye otdolenlye. 2. Chlen-
korrespondent AIII SSSR (for Kliomentovskiy).

KHOMENTOVSKIY, A.S., otv. red.
(Geology and paleogeographic conditions governing the forma-
tion of Mesozoic and Cenozoic continental depressions in the
Bouthern part of the Far East] Geologiia i paieogeografiche-
skis usloviia formirovaniia mezo-kainozoiskikb vpadin iuzluioi
chasti Dallnego Vostoka. Moskva, Nauka, 1965 105 P.
iMIRA 16!4)
1. Akademiya nauk SSSR. Dallnevostocbr*ry filialp Vladivostok.
Geologicheskiy institut. 2. Chlen-korrespondent AN SS9 .
Rli

1-7 Tv
XMIZY, A.J.; KELLIMI, B.X., translator,# XOLGHMOVA, T.Y., translator;
RAAREN, M.Ts., tramnlator; wrnvQvTv -40A., translator; SRATSKIT,
N.S.. ak-cademik, radaktor; BVIT. U.K., redaktor; IMNILOV, B.I.,
tekhnichaskiy redaktor
[Structural geology of Worth America. Translated from the Inglish by
B.M.11eller wA others] Strukturnais, geologila Severnoi Amertki.
Perevod a angliiskago B.K.Irellers I dr. Pod red. i a predlelovism
N.S.Shatakogoo Kooky&, Izd-vo inostrAnnoi lit-ry, 1954. 665 P.
(Wortb Asierici-Geology. Structural) (MMA 8:3)

REPINA, L.N.; UXIKHATOV, X.A.;
Stratigraphy of Cambrian doposito In the womtern regiou of lant-
ern ftyan. Dokl.AN SM 110 no-1:133-136 S-0 156. (KM 9til)
1. Institut geologicheskikh nauk Akademit nauk SM. Predstayleno
akadealkom N.S.Shatskin.
(Sayan Mountains--Geology, Stratigraphic)

SEMIKffATOV, N. A.
Stratigraph7 of pro-Cambrian deposits of the western part of
the Flastern Sayan. Dokl. AN SSSR 110 no.2:273-275 S 156.
(MLEA 9:12)
1. Inatitut geologichaskikh nauk kkademli nauk SSSR. Prodstavlono
akademikom N.S. Shatakim.
(Sayan Mount at ns--4geo logy, Stratigraphic)

7 e,' i/_s A~'
AUTHOR: Khomentovskiy# V.V.
11-7-1/23
TITLE: "On Tectonics of East Sayan" (K tektonike Vostochnogo 8%yana)
I
PERIODICAL: "Izvestiya Akademil Nauk SSR11 Seriya geologicheskaya, 1957,
No. 7, PP- 3-26, (USSR) I
ABSTRACT. The western section of the East Sayan presents a classic ex-
ample of ancient layerep the formation of which can be studied
due to their accessiblity, simplicity of structure, undis-
turbed strata, well recognizable horizons levels and abund-
ance of Cambrian faunal fossiles. The Geologic Institute of
the Academy of Sciences of the USSR assigned a group of geo-
logists in 1953-55 to study the various stratographic com-
plexes in order to clarify the existing contradictory views.
Scant data are available on the Pre-Cambrian development of
the explored sections of East Sayan. Although many geologic
problems have yet to be solved, it can be stated that this
area was subjected to great changes during the Archean and
Lower Proterozoic ns well as between the Lower and Upper Pro-
terozoic eras. Moro definite data on geological structures
of the East Sayan are available of the beginning of the Lower
Cambrian period. When analyzing the facies,of the Caabrian
Card 1/4 period'it must be concluded that the anticlinorium. formed a

"On Tectonics of East Sayan"
11-7-1/23
dry rigde dividing 2 sea basins during the entire Lower Cam-
brian period. Although concrete data on the continuation of
the East Sayan geosyncline beyond the surveyed territory are
not available at present, based on recently conducted studies,
it can be assumed that Proterozoic layers -xtend several
hundred km in south easterly direction from the boundaries
of East Sayan. Judging by Cambrian deposits, it must be
assumed that the entire area of the East Sayan anticlinorium
was geoanticline during the Cambrian period. In contract to
this, the Sisim synclinorium, experienced an intense depression
during the Cambrian period, and does not differ structurally
in any way from the extensive Sayan-Altay geosyncline terri-
tory. The compositions of the Bellykak White Mountains
area's Lower Cambrian deposits differ essentially from the
Sisim synclinorium, since they are almost void of effusions
and consist predominantly of limestone formations. The avail-
able data indicate the originality of the geologic structure
of the Mans, aynclinorium. The texture of the Cambrian de-
posits of which it is composed, have been influenced to some
extent by Pre-Caabrian rock formations. In fact, the very
simple texture of the Solbin syncline supports the assumption
Card 2/4 that it extends as a consolidated strata underneath the Arch-

"On Tectonics of East Sayan"
11-7-1/23
ean. The Zherzhul syncline is distinguished from the Solbin
syncline not only by its more complicated structure, but also
by its composition and the magnitude of Cambrian deposits.
Thus, the vast Archean strip, extending over a vast distance
in a north-westerly direction parallel to the East Sayan anti-
clinorium, covers a distance of almost 1 meridian. The meri-
dian virgation of the East Sayan anticlinorium, superposed by
unconformable Cambrian layers of the Mans. synclinorium, are
extended into the Yenisey ridge. Consequently, the Man& syn-
clinorium represents a depression overlaying a very complex
and heteregeneous Pre-Cambrian formation, The great magnitude
of Cambrian deposits, intense deformation and great number of
intrusions indicate the geosyncline structure of this depress-
ion. Cambrian layers, found on the northern slopes of the
East Sayan resemble very much as to their magnitude, litbo-
logic composition and stratographic sequence, deposits of the
Lower Cambrian of the Mans, synclinorium. When comparing
various sections of the Angara-Kan depression, it will be
noticed that the typical geosyncline characteristics diminish
with increasing distance from the Mans, synclinorium in the
direction of the Siberian plateau. It follows that the An-
Card 3/4 gara-Kan depression was formed at a time of intense sagging

"On Tectonics of East Sayan"
11-7-1/23
of the 6ayan-Altay geosyncline area, preceded by heavy tec-
tonic movement and erosion. The author lists the following
subdivisions of geologic formations and periods:
1. Mans, synclinoriumt Ust'-Mana, Zherzhul Solbin syncline;
Izyak and Beretsk antioline.
2. Lower Protezoic era: Kozhelak, Derbino and Zhayminsk
layers.
3. Upper Proterozoic eras Kuvaysk, Pavlovsk and Urmansk
layers.
4. Mana synclinorium: Angul, Anastassinsk and Zherzhul
layers.
5. Sisim synclinorium: Xameshkovsk, Balakhtisonsk and
Kizirsk layers.
6. Cambrian-Ordovicium: Badzheysk and Narvsk layers.
The article contains 7 maps, 1 figure, 1 diagram and 1 table.
The bibliography lists 33 references, 30 of which are Slavic
(Russian).
ASSOCIATION: Geologic Institute of the Academy of Sciences USSR (Geo-
logicheskiy institut AN SSSR) Moskva.
SUBMITTED; February 12, 1957
AVAILABLE; Library of Congress
Card 4/4

PHASE I BOOK EXPLOITATION 1199
Khomentovskly, Vsevolod Vladimirovich
Geologicheskoye stroyenlye i istorlya razvItiya Vostoohno-Urallskogo
antiklinoriya na Srednem Urale (Geological Structure and History
of the Development of the East Ural Anticlinorium in the Central
Ural Region) Moscow, Izd-vo AN SSSRO 1958. 68 P. (series:
kkademiya nauk SSSR. Geologicheskiy institut, Trudy, vYP. 7)
1,600 copies printed,
Chief Ed.: Shatskiy, N.S., Academician; Re5p. Ed.; Shtreys,, N.A.; Ed.
of Publishing House: Kotlyarevskaya, P.S.; Tech. Ed.: Rylina, YU.V.
PURPOSE: This monograph is intended for professional geologists, pe~
trographers, and students of the structural geology of the principal
metallogenetic provinces in thd.USSR. .
COVERAGE: Referring to numerous earlier studies of the Urals, the
author reports on recent mapping achievements, the stratigraphic,
structural, and petrographic studies compiled on extrusive rock
massifs in the heart of the industrial Urals, and their distribution
Card 1/3
Geological Structure (Cont.)
1199
and configuration. The effects Of vOleanism and the Hercynian re-
gional trend bearing on the regional structural pattern of the area
is also discussed. The following are mentioned as having contribut-
ed to the study of this area: Borodayevskaya, M.B. - dike formations
and small intrusions; Nalivkin, D.V. - stratigraphy of the Ural5;
Librovich, L.S., Gorskly., I.I., Kuznetsov, Ye.A., Romanov, M.B. and
Matveyev, V.I. - the geological structure of the eastern slope of
the Urals; Shteynberg, D.S. and Borodayevskiy, N-I. - surveys of the
environs of Berezovsk for large scale Mapping; Sh4L-Ireys, N.A. - strat-
igraphy of greenstone series of the Central Urals; Sergiyevskiy, V,M.-
VOlcanism in the Urals; Sobolev, IoD.9 Aladinskiy, P.I., Burdinp. 0V.,
Dianova, T.Vo, Kudrina., N.I., Nenakhov, Ye.M., Nechayeva, A.P., '
Nechayevp P.N. and Spasskiy, N.A. - cross-sections of the Central Ura3s;
Ste'panenko, A.F. and Khalilbeyli, Ch. Ao - petrographic studies; Pav-
lova, T.G., Zavodehikov, S.G., Zakhvatkin, V.A. and Sidorenko, N.F. -
field studies o.'~' Central Urals; and Kashin, S.A., Keller, B.M., Men-
ner, V.V. and &ieraskov, N.P. - editorial advisora. The text Is ac-
colnpanied by 6 diagrams and 38 Soviet references,
TABLE OF CONTENTS:
Card 2/3

AUTHOIC: Keller, B.M. and
TITLE: The Differentiation of the Rifey Group (0 reschlenenii ri-
feyskoy gruppy)
PFRIODICALt Byulleten' Moukovskogo obshchestva ispytnt,eley prirody,
Otdel geologicheski-y, 1958, Nr 4, PP 148-140, (USSR)
ABSTRACT: This is a summary of a report given by the authors at a con-
ference of the Moscow Society of Naturalists on 29 April 1958-
The study of profiles of the European part of the USSR and
Siberia shows that two distinctly different complexes can
be distinguished in the composition of the Rifey group (as
established by N.S. Shatskiy for the late Pre-Cambrian
period): 1) the Lower or Sinian complex and 2) the Upper or
T11manfty complex. The authors describe these two groups in
detail.
1. Geology
Card 1/11

AUTHORS: Repina, L.N. Khomentovskiy, V.V. SOV/5-58-4-2-1/43
TITLE: Basic Stratigrap~hica ~ro Tems of the Lower Cambrian Stage
(Osnovnyye voprosy stratigrafii nizhnego kembriya)
PE2IODICAL: Byulleten' Moskovskogo obshchestva ispytateley prirody,
Otdel geologicheskiy, 1958, Nr 4, PP 149-150 (USSR)
ABSTRACT: This is a summary of a report given by the authors at a con-
ference of the Mosccw Society of Naturalists 6n 29 April 10,58.
The authors consider and explain new data on the stratigraphy
of the Lower Cambrian Stage in Siberia and America, and
come to the conclusion that according to its importance, the
Lower Cambrian Stage should be regarded as a separate system
in future geological studies.
1. Geology 2. Geological time--Determination
Card 1/1
xxm W

3(0) SOV/20-123-6-37/50
'AUTHORS: Zhuravleva, I. T., Repina, L. N., Khomentovbkiy,-Y,-Y-----,
0 -
TITLE: Now Data Concerning the Stratigraphy of Lower Camtrian of the
Mariinakeya Tayga (Novyye dannyye po stratigr'afiiL nizhnego
kembriya Mariinskoy taygi)
PERIODICAL: Doklady Akademii nauk SSSR, 1958, Vol 123, Ir 6, pp 1092-1095
(USSR)'
ABSTRACT: By interpreting the profile at the middle part of the Kiya
river,'on which 'all the stratigraphic constructions of the
Lower Cambrian of the northern Kuznetskiy Alatau are bdaed,
o7ccur still several not 'fully solved problems: 1) The age of
the limestones containirig' Archaeocyathen is very,contradictory
determinedi 2)'There is no agkeement about the existence and
the stratig3~aphical poaition of the limeatone maast which Is
characterize'd by alga of the Newlandia type (Refs 192).' The
gool6gibal-structure of the above mentione'd.,distriqt is il-
lustrated''by figure 1. Here one can separat6 four natural
sediinent-complexe.s.'The.Arohaeod~athen fimestones, which are
widie"pread'her'e, a.r.e. mas-sive and gii6 hardly essential facts
Card 1/3 for the deter~ination'of the inner structure. Therefore, the'

SOV/20-123-6-37/50
New Data Concerning the Stratigraphy of Lower Cambrian of the Mariinskaya
Tayga
paleontological method becomes very important in this area.
An idea of the full stratigraphical extent of these limestones
could be gained by the construction of two actual profiles at
the Kiya river. The authors separate five layers in these
Archaeooyathen limestones (total thickness 2300 respectively
1300 m). These limestones comply with the Bazaikhakiy horizon
of the Lena stage, according to the results. The upper part
of the mentioned limestones belongs to the higher lying
Sanashtykgol'skiy horizon, while the lowermost part and the
platelike limestones belong to the Kameshkovskiy horizon. This
fact complies (Ref 3) with the upper part of the Aldanskiy
stage as well as with the Sinskiy, Tolbochanskiy, and one part
of the Olekminskiy horizon of the Lena stage in the plateau.
The under-lying black limestones and schiSt3 (at least 2000 m
thick) are connected to the Archaeocyathen limestones by grad-
ual transitions. Therefore, they can only be compared with the
Aldanskiy stage of the Lower Cambrian. The finding of alga of
the type Newlandia (determination by P. S. Krasnopeyeva) cannot
Card 2/3 prove the pre-Cambrian age of the rocks containing them. The

SOV/20-123-6-37/50
New Data Concerning the Stratigraphy of Lower Cambrian of the Mariinskaya
Tayga
tuffogenic suite covers the uppermost strata of the
Archaeooyathen limestones without an apparent discordance.
Their age can be determined as the upper part of the Lena stage,
although a part of it is possibly already encroaching on Middle
Cam',rian. Their age is not greater than Middle Cambrian.
L. V. Alabin collected and delivered the Archaeocyathen. There
are I figure and 6 Soviet references.
PRESENTED: April 29, 1958, by N. S. Shatskiy, Academician
SUBMITTED: April 24, 1958
Card 3/3

Kll%l8NT0VSKjy, V. V.: ~Jaster Geolog-Mineralog Sci (diss) -- "rhe Proterozoic
and Cambrian deposits of the western portion of the eastern Sayan". Moscow,
1959. 20 pp (Acad Sci USSR, Geol Inst), 150 copies (KL, No 12, 1959, 127)

PXPINA, L.N.; KMMENTOVSKIY, T.V-
-
Stratigrapby of the lower Cambrian. Jzv.vys*ucheb*zav*;
geolst razy. 2 no-10:3-19 0 '59- (KIRA 13:6)
1. Inatitut goologichoskikh nauk AN SSSR.
(Geoloar. stratigraphic)

3(5) SOV/11-59-10-4/16
AUTHOR: Khoment
TITLE: Structural-Facial Lowor Cambrian and Riphean Zones of the South-
Western Framing of the Siberian Plateau
PERIODICAL: Izvestiya Akademii nauk SSSRp Seriya geologicheskaya, 1959,
No- 10, PP 42-49 (USSR)
ABSTRACT: The above zone is described by the author who studied it to-
gether with I.T. Zhuravleva and L.N. Repina. Other parts of
the Sayan-Alatay-folded zone have already been studied and de-
scribed by V. A. Kuznetsov, S.V. Obruchev, A.S. Khomentovskiy,
V.M. Yaroshevich and Yu. G. Shcherbakov. A large miogeosyn-
cline borders the Siberian Plateau from the southwest (figure
1). It is composed of Lower-Cambrian strata similar to those
of the Siberian Plateau, only less thick. In both cases, the
Cambrian strata non-conformingly overlie the Riphean forma-
tions. The Plateau and the miogeosyncline are delimited by a
long bending flexure. 0n'_ihd'YeAim~skiy)e.T mountain ridge, the
structure of those Riphean formations on both sides of the
Card 1/4 flexure are different. In the eastr carbonaceous strata are

SOV/11-59-10-4/16
Structural-Facial Lower Cambrian and Riphean Zones of the Southwestern
of the Siberian Plateau
Fr"in
predominant, and in the west - mainly terrigenous and effusive
strata. Farther to the southwest, the miogeosynclinal cross-
section type of the Lower-Cambrian strata is replaced by one of
a eugeosynclinal type characterized by large effusive strata
often intensively metamorphized and faulted by numerous intru-
sions. The East-Sayan anticlinorium forms a border between the
mio- and eugeosynclines. In the eugeosynclinal part of-the
Sayan-Altay folded zone, two different cross-sections of the
Lower-Cambrian and UpperL-Paleozoic strata were found, one -
essentially carbonaceous, and the other - essentially effusive.
The author gives a detailed description of the region from
which it appears that the internal part of the Sayan-Altay
folding zone was filled with carbonaceous facies of Upper-
Riphean and Lower-Cambrian formations forming a huge triangle
bordered on each side by a narrow stretch of effusive forma-
tions of the same age. These facial zones are at the same time
structural zones, as the effusive formations are thicker than
Card 2/4 the carbonaceous formations, the regions of theiVdevelopment

SOV/11-59-10-4/16
Structural-Facial Lower Cambrian and Riphean Zones of the Southwestern
Framing of the Siberian Plateau
form depressions or troughs, and a linear folding is observed
in these depressions filled with effusive rocks. The regions
where the carbonaceous facies are developed were characterized
by large brachy and box-folds of various form and orientations.
The structure of facial zones especially stands out when spe-
cific belts associated with the central parts are examined.
These belts are characterized by their association with the
widely metamorphized and deformed strata of the Paleozoic
era. These belts were presumably formed in places of plutonic
rupturesq which explains their expansion (up to 700 km).
Their connection with magmatic hearths explains the degree of
metamorphosis of strata formincr these belts. Sharply defined
limits of metamorphouis in these belts proves, says the
author, that they were formed along the plutonic rupturbs
which explains their "longevity". The geosynclinal troughs,
originated in places of plutonic ruptures, have existed at
least since Upper-Paleozoic times. Thus, the peculiarity of
Card 3/4 these ruptures was that they formed highly penetrable belts

KELLER, B.M.;,KHOMENTOVSKIY, V.V.
Abstract of Carl Dunbar and John Rodgers' book 'Principles of
stratigraphy," Blul. MOIP. Otd. geol. 34 h0-5:150 S-0 159.
~i (MIRA 1416)
0 (Geology., Stratigraphic) *
(Dunbar Carl)
(Rodge,
rd, John)

KHOMINTOVSKIT. JaavoloA VladimirqKiqh;__~SZMIMTOV, Mikhail Aleksandrovich;
RVINA. Lada NIkolayevna; SELAMIT, N.S., akademik, glavWy reds;
KUM, V.V., samostitell glavnogo red.; KNJM, B.M., red,tow;
TMTAX, G.B., red.isd-va; KASHINA, F.S.. takhn.red.
(Areal geology of the U.S.S.R.] Regionalinals stratigrafile 30R,
Glay.red.N.B.Shatskil. Koskva. Vol.4. [Pro-Cambrian stratigrapby
and lower Paloosolo sediments of the western part of the lastpm
Sayan Mountains] Stratigraflis d6kembritakikh i nishne soiskikh
otloshenil sapadnol chasti Tostoohnogo Solana. [Lower and middle
Cambrian trilobite complexes in the western part of the Sayan
Mountains] Komplakey trilobitoy n1zhnego I arednego kembrile me-
pednoi chasti Vostochnogo, Smians. 1960. 235 p. (MIRA 1314)
1. Akedemlya nank SM. Geologichaskly institut.
(Sayan Mountains-Geology. Stratigraphic)
(Sayon Mountains-Trilobites)

ZaMTMA., I.T.; RVIRL, L.N.; XHDIWNMVSKIro T.T.
Continuous carbonate section of the Lem stage of the lower Cam-
brian in the Altai-Sayan mountain country and Its paleontological
characteristics. Dokl.AN SSSR 132 no.5slI60-1162 Je 160.
(XIBA 13: 6)
1. Geologicheskly InstItut Akademil nank SSSRe Predstavleno
Madeudkom N.S. 8hatakim.
(Altai Mountains-41ocks, Carbonate)
(&Wan Mountains-41ocks, carbonate)
(PaloontoloCr, Stratigmphic)

REFINA, L.N.; KHOMENTOVSKIY, V.V.
Subdivision of the lower Cambrian. Izv. AN SSSR. Ser.geol. 26
no.8:83-87 Ag 161. (MIRA 14:9)
1. Geologicheskiy institut AN 55SR, Moskva.
(Siberian platform--Geology, Stratigraphic)

KHOMENTOVSKIY, V,V.
Formation Of structural and facies zones in southwestern Siberia
and minerals associated -4ith them. Zakon.raw polesn.ink-op.
31747 160. 0 imm 14:31)
L Geologicheokiy Institut AN SSSR.
(Siberiap Western-41inerals)

KHONENTOVSUL-S,V,,, ZHURAVLEVA, I.T.; REPINAp L.N.; ROZANOV, A.Yu.
------ ~ I -
Lower Cambrian In the Gornyy Altai. lov.AN SSSR.Ser.geo. 27
no.3.-55-71 Mr 161. (MRA 15:2)
1. Geologicheskiy iwtitut AN SSSR,, 14Dskya.
(Altai Nbuntains--Geology, Stratigraphic)

ZHURAVLEVA, I.T.; REPINA, L.N.; KHOMENTOVSKIY, V.V.
Plan for dividing Lower Cambrian sediments in the Sayan-Altai
folded region. Geol.i geofiz. no.1:21-41 162. (MIRA 15 %4)
1. Inetitut geologii i geofiziki Sibirskogo otdeleaiya AN SSSR,
Novosibirsk.
(Sayan Mountains.-Geology, Stratigraphic)
(Altai Mountains-Geology, Stratigraphic)
(Folds (Geology))

SEMIRUMV9 Mikhail Aleksandrovich; JMOMUMV-qXII,-VY" otv.red.;
SHEYMMAN, V.Z., red.lzd-va; NOVICHWA, N.D., tekhn.red.
[Riphean and Lower-Ca~brian in the Yenisey Ridge] Rifei i
nizhnii kembrJA Eniseiskogo krIAzha. Moskva, Izd-vo Akad.
nauk SSSR. 1962. 239 p. 18 plates. (Akademiia nauk SSSR.
Geologibheskii institut. Tj no.68). (KMk 16s2)
(Yenisely dge-XIeology)

REPINA, L.N;;,KHOMENTOVSKIY, V.V.; ZHURAVLEVA, I.T.; ROZANOV, A.Yu.;
S XOLOV,'--B'."S'.-,-'o-~ VANIN, V.S., red.izd-va;
IL'INA2 N.S.j red.izd-va; DOROKHINAp I.N., tekhn.red.
[Lower Cambrian biostratigrapby of the Sayan-Altai fold
area) Biostratigrafiia nizhnego kembriia Saiano-Altaiskoi
skiadi-.Mtet. blasti.[By] L.N.Repina i dr. Moskva, Izd-vo
IINauka,,I 1964. 363 p. (MIRA-17:3)
-g --g -----

AL12-1,.Szr111[A) P.Ye.; BETa-71THA, O.A.; 1jOZZH~:j3t'T!'07j'.-., T.F.; GILI-TSI T.
DUBATOLOV, Mi.; LIM, Ye.A.; Z,d'HA,'tGV, V.A.; A.B.;
SIDYACIIII-10, A.I.; KULIKOV, Y.P.; NYAGKOVA, Ye.I.; OWT., A.Y.;
SAIIIS V.,'A.,- TESXr:OV, Yu.I.; FU:15:-I,'YO, A.V.; VHM.':2-.,TOVSKIY V.V -
Yul-'-L-1-1, O.V.
Corresponding I.'ember of the Academy of Sciences of the U.S.S.R.
Boris Sergeevich Sokolov; 1914 on his 50th birthday. Geol.
i geo-fiz. no.8:140-14.7 t64 ("IRA 18:2)

SEMIKHAMV,' M.A.; KHOMENTOVSKIYy V.V..
Geological prerequisites of the bauxite potential of sediments
of the Wendish complex of the Manskoye aynclinorium (Eastern
Sayan). Biul. MDIP. Otd. geol. 39 no.3t4l-56 Yq-Je 10,
(MA l7tl2)

SEMIFHArtOV, Ill.A.; FIR)MENTOVSKlY, V.V.
Stratigraphy- of the Upper Cambrian in the western part of the Eastern
Sayan Mountains* Geolo i geofL,. ao.7:97-102 164- (MIRA 18:8)
lo Institut geologii i geofiziki Sibirskogo otdoleniya AN SSSR)
Novosibirsk.

26462
S/lAc)/61/000/003/008/009
CiliA333
AUTRORt Khomen?Q4,-V. V.
TITLEs on sys"tems of ordinary differential equations with
generalized-homogeneous right sides
PERIODICALs Izvestiya vysshikh uchabnykh zavedeniy. Matematika,
no. 3, 1961, 157-164
TEXTs The author gives necessary and sufficient conditions for the
asymptotic stability of the homogeneous solution of the system
dx i
T7
where the right sides are generalized-homogeneous.
The matrix
A(xlp-"9 xn' C) aij(Xlt ... 9 Xn9c)II 4~j
where a E ( - oo, aD) is a parameter, a ij are holomorphil; functions
Card 11-40

26462
S/14 61/000/003/008/009
On systems of ordinary differential ... C111YC333
of x1' ... 1 Xn (S En, Ena linear space and A - E for c - 1, where
E -- unit matrix, is assumed to define the system of differential
equations
dzi
a do .Pi(zi Zn) (i = 1'...,n) (1.2)
where
- C n (Xip..."Xn c)
(Pi(zl'--" zn) 7, do
J-1
The x. are determined from
n
z I aij (xj'...' Xn'o) Xi (i=l,..-,n) (1.4)
j-1
Card 2140

26462
S/14 61/000/003/008/009
On systems of ordinary differential ... G111YC333
as functions of the z19 ... P zn-
The matrices A(Xif ... 9 xnc) are considered such that magnitudes (1.3)
do not explicitly contain o. Moreover, let
1.) The / 0, it is nec',essary and ;,ificient
11-1 xn9
that it satisfies the linear partial differential eauation
n
f
7_CFi(xj,..., x (S'f (X, ... oe,
n Tx,'- n,
Definition. 2: Continuous functions f 1(x1?'-'p. xd' ... fn(Xl xn).
given on E n are called generalized-homogeneous funct;Lons of ..the class
A(x17 .... x C) of the order 6 ~,O if~
n
Car d V40

26462
B/140/61/000/003/008/009
On systems of ordinary differential ... C11I/C333
C, bil (XI, All C) b (x .. .... .V.) 0~1~,--.n),
is satisfied for everk c co oo where
av, X,
OAJ U, j~ 1
OXJ
The author considers the system
dx
Tt X (xl"'.' xn) 11 ... pn) (2.1)
Card 6/
40

26462
B/140/61/000/003/008/009
on systems of ordinary differential ... C111/C333
where the Xi are given in En, are holomorphic in xi,"', x n and be-
long to the class A(xlt..., xn,c) in the sense of definition ~, where
61>10 is rational, fr 2, q is odd. Let Xi(O,._.. 0) = 0 (i = 1,...,n).
q
Through every point
x0 x
0 , 1
x of the En there goes an integral curve X=X(t,XO),,,
0 in
n
of (2.1) such that X(t,X*) - Xo for t = 0.
Theorem 2: If the vector function X(t,Xo) is an integral curve of (2.1),
then the vector function
Y(t) - A(X(x 9t,xo), a) X(C8't'X 0) (2.2)
is a family of integral curves of (2.1) such that
Card 7/40 Y(t) - A(Xo,c) Xo for t = 0.

26h62
S/140/61/ooo/oo3/ooe/ooq
7
On systems of ordinary differential ... C111/03_~
Therefore
Y(t) - x(t,A(xo,o)xo) (2-3)
Theorem 3s I-) The zero solution of (2.1) can be asymptotically stable
for arbitrary complex perturbations only for 6 = 0.~
2.) For real perturbations the zero solution of (2.1) can be asympto-
tically stable only for 6- 2k > Of q -- integer and odd.
q
Theorem 41 a.) Assume that the zero solution of (2.1) is asymptotically
stable and that positive numbers oLand (I exist such that
IX(t,Xo) 14 0 t -'for t >,, T(aL ), I Xo - -1 - (3-1)
Then there exist two continuous functions V and W defined in E with
the propertiest . n
1.) V(xl,..., x n) is positive definite, W(xl,.,i., xn) is negative
Card 8/40

26462
S/14 61/000/003/008/009
on systems of ordinary differential ...C111%333
definite, V(0,0..,O) M W(O'...1 0) - 0.
2.) V and W are generalized-homogeneous, belong each to the class
A(xl,..., x c) and have the orders m - 6 and m.
3-) V(xl,---, xn) is continuously differentiable along the integral
dV
curves of (2.1), where Tt- = W.
b.) If there exist functions V and W which satisfy the conditions
1-) - 3.), then the zero solution of (2.1) is asymptotically stable.
Theorem 5s In order that the zero solution of (2.1) be asymptotically
stable, it is necessary and sufficient that the domain of the
asymptotic stability of the zero solution of
dyi f (3.16
_dT i(Y19 ... 9 Yn"r - Xi Y11 ... I Yn)
is bounded. The functions f,(yl,.-.y ynj1V ) are determined from the
following system of linear algebraic equations
Card 9/110

26462
S114 61/000/003/008/009
On systems of ordinary differential... C111YC333
B(Y,e'~) F(Y,t (A (Y, e-r Y) , (3-17)
where
Y yl F f1
;n fn n
The author thanks V. J. Zubov for subject and guidance of the paper.
There are 3 Soviet-bloc references.
SUBMITTEDt February 10, 1959
Card 10/10

261-37
S/0110,/61/025/004/016/021
D274/D306
AUTHORS: Stepanov, K.N. and Khomenyuk, V.V. (Kharlkov)
TITLE: Notes on thdenergy principle in tziagnetohydrodynamics
PERIODIC.,Uj: 1'rikladnaya matematika i melchanika, v. 25, no. 4,
1961, 760-763
TEXT: Thearems tire proved on the stability of equilibrium states
of an ideal conducting fluid, by means of Lyapunov functions. The
uid
equations of motion of an ideal, non-viscous, conducting fl
with small. dis lacements 4(r,t) from the equilibrium position,
are P
~i = Fi(~) (i = 1,2,3)
where F denotes a linear self-conjugated operator
'V(~ Vp) + 7KAp Div.) + 1 (rot rot (C,-'X H) Y, H) + 1- rot H X
41t T;i
x rot H)
It is assumed that the fluid occupies a finite volume V, bounded by
Card 1/3

S/040/61/025/004/016/021
Notes on the energy... D274/D306
S. and that the density P and the displacements vanish on S. Lq.
(1) has the energy integral E = T + U const (2)
where f -
T 3 p~2dr, U [~j 1
2 F(~) dr (3)
V V
Let ~ and be solutions of Eq. (1), satisfying the initial con-
ditions 9. (r), S - ' (r) for t a 0
50 C50
Further, stability. asymptotic stability, and instability are de-
fined. Thereupon, theorem 1, (the necessary condition for stability)
is formulated: In order that the equilibrium state ~ .0' i j 2 0
be stable, it is necessary that 0. The theorem is proved
by reductio ad absurdum. It follows from the theorem that if there
are k's for which U(~ (r)) < 0, then the considered equilibrium is
unstable. It can be readily shown that the equilibrium state of an
ideal non-viscous conducting fluid cannot be asymptotically stable.
Further, the erfect of viscosity on stability is iliveotigated.
Card 2/3

Notes on the theory...
1%
26137
S/040/61/025/004/016/021
D274/D306
Theorem 2. If there us such a t; (r) so that U(~(r)) < 0, then the
equilibrium is unstable even in the presence of viscous forces.
Again, the theorem is proved by an assumption leading to a contra-
dictica. Theorem 2 is analogous to Kelvin's theorem on the affect
of dis'sipation on stability of a system of material points. The
functionals involved in the proof of both theorems are analogous to
the Lyapunov functions used by N.G. Chetayev in his proof of stabi-
lity theorems (Ref. 5: Ustoychivost' dvizheniya (Stability of'No-
tion) Gostekhteorizdat, M., 1955). There are 11 references: 6
Soviet-bloc and 5 non-Soviet-bloc. The references to the English-
language publications read as follows: S. Lundquist, On the Stab-
ility of Magneto -hydrodynamics. Ark. Fys. 1952, v. 5, no. 15; ,
I.B. Bernstein, E.A. Friedman, M.D. Kruskal, R.M. Ku1srud, An eneru,~
principle for hydromagnetic stability problems. Proc. Roy. Sac.,
1958, v. A244, no. 1236; A. Hare, The effect of viscosity on the
stability of incompressible magnetohydrodynamic systems. Phil. Mag.,
1959, v. 4, no. 48.
SUBMITTED: January 28, 1961
Card 3/3

38085
S/040/62/026/003/008/020
Y/0 D407/D301
AUTHORS: Stepanovp K.N.p and Khomenyuko V.V. (Kharlkov)
TITLE: On stability conditions for magnetohydrodynamic equi-
librium configurations
PERIODICAL: Prikladnaya matematika i melchanika, v. 260 no. 3.
1962t 466 - 470
TEXT: Stability of an ideally conducting fluid is defined, the de-
finition differing from that given by the authors in an earlier work
Necessary and sufficient stability criteria are established, which
are related to the well-knom energy principle. Vith small displace-
Ments S(r, t)j of the fluid, the equations of motion are
P~j + (i = 1, 2.'3-
F(J) =V(jVp)+TV(pdivt~_
where 1 -(1.2)
xrotrot(jxH) +~-rotHxrot(jxH)
(OV, + LVL 2 'IV,)] + V, (1-3)
T (k
Card Q~3 1 574

S/04 62/026/003/608/020
On stability conditions for ... D407YI)301
p, p and H being the equilibrium values of the density, pressure
and magnetic field, y - the adiabatic index, q and ~ - viscosity co-
efficients. The solutions of Bq. (1.1), satis:~ying the boundary - - '
and initial conditions, are denoted by t~ Ex ressions are obtained
for the kinetic- (T) and potential energ (U5. The notations
3
P10(r))=~4-dr+ay,~(")2dr. PA(r)) 2 d,
ark ~Pi (2.1)
are introduced.' By definition, the equilibrium is stablet if for any
positVie 6" itis-possible to find positive 6, so that if
(-2.2)
<
P, 00 W) < bl,
then -or all 0
_p, < ex. (2-3)
io P2 d (tir, J0 (r), j. (r))) < e2
Instability is also defined, as well as the positive-definite func-
tio.nals V and T. Theorem 3.1: (The necessary stpability-condition):
in rjrder than an ideally conducting inviscid fluid be stable, it is
ne~:~.zZ~zy that U(S).'~,> 0 for all allowed r,-(r). Theorem 3-2: (The suf-
S-Lability:cond-ition): If U(~)'is'a positive-definite func-
Card 2/3

S/040/62/026/003/0081/020
On stability conditions for ... D407/D301
tional in the metric pj(~:), then the equilibrium of the fluid is
stable. The theorem is uroved. It is analogous to Lagrange's well-
known theorem, whose generalization was proposed by A.A. Movchan
(in the references) in stability investigations of elastic systems
and continua. Purther, the stability of viscous ideally conducting
fluids is considered. Two theorems and a corollary give the stabili-
ty (respectively instability-) conditions. The theorems are analo-
gous to Kelvin's well-known theorems on the effect of dissipative
forces on the equilibrium of material systems. The most important
English-language reference reads as follows: A. Hare, The effect of
viscosity on the stability of incompressible magnetohydrodynamic
systems. Phil. 11ag., 1959, V. 4P no. 48.
SUBMITTED: December 2, 1961
Card 3/3

DEM'YANOV I V-1"- (Leningrad);
Solution of 11 linear
24 n0-911174-1177
KHOWMM.__V V.
__F
_ (Leningrad)
problem on
S 163. Optimum control. Avtom. i teleza.
(AutorA&tic control) (MIRA 16,9)

IMST-11- i i , ~ , ~
',-7M7771~~

Z;
_n!7-- - - " 1 -.1,
ACC NRi AP6010277 SOURCE CODE: UR/0103/66/000/003/006-5/-00-1-7--~
AUTHOR: Khomenyuk, V. V. (Leningrad)
ORG: none
TITLE: Synthesis of programmed control in a linear system based on a single coordi-
nate
SOURCE: Avtomatika i telemekhanika, no. 3, 1966, 5-17
TOPIC TAGS: linear automatic control, automatic control design, automatic control R
and D
ABSTRACT: Based on the proof of several control theorems, the author analyzes condi-:
tions and restraints for the synthesis of a control in a linear system based on a sin-
Ele coordinateo Such a system can be described by a system of ordinary differential
. .4 ......r
equations
d X(t)='1j(j)X(j)+ YJ Bj (j) jjj (t) F (i),
Tt
and initial conditions X(O) = X0, where AM is a square n x n-matrix, PM and B j W
are n-dimensional vectors. The elements in these matrices are essentially
pieceviise continuous and given for (0,T] function; u(t) is also essentially piecowise
continuous, Wown for [0,T] and satisfies uj(t) < 1 U=1,...,r). T > 0 is the fixed
UDC: 62-503.52
Card 1/3.

Aff_4R _tA__P 6 0-10 2-7 7-
control time. Let X(t,u) z (Xj(tpU)j---,Xr(t,U)) be the solution of the system (1) fol,
given initial conditions for the selected control u(t) = (uj(t),...,u r(0), UT.
The control 'function u(t) has to be selected such that starting from the initial con-
ditions the object will assume the state xl(T,u) = xf during T > 0, where Xf is Oven.
Let also Ql(xo.T) be the plurality of values of xj(P,u) for all possible UM"
&~UT-
Then: Theorem I: The solution to the problem exists if and only if
E=- (2)
Theorem 2: Assuming (2) is true, then u(t) which provides the solution to the problem
is in the form
u cou(i),
where
CE if iF y-L X,
X
and ais an arbitrary number from the interval (0,13, if X-=;. The third theorem deals
with the conditions which xf must satisfy to make the solution of the problem possible
and the fourth-theorem provides the expressions for u jM which provide the solution.
Theorem 5 postulates that u(t) cannot be determined by the principle of maximum and
the sixth theorem deals with the fast system response. The author also investigates
Card 2/3

1, U,--453-67
'kCC-Nk,- -AP6010277
the conditions of oontr'Ollability and other limitation. fct, U(t).
fOmulas, 3 figules. Or aft has: 73
9
SUB CODE: 12,13/ SUBM DATE.- 120ct6S/ ORM REF-1, 002
Card 3/3

L 16123-M 'EM(k)-21EWP(k)IEWT(d)IEWP.(h)~EWP(1)IEWP(v) BG
ACC, M AP5025115 SOURCE CODES UlV0208/65/005/005/0894/0902
i AUTHORt Baranovj A. Yus (Leningrad); Kazarinovt Yu. F. (Leningrad) Khomenyuk,
I Vj_.L_(1en1ngrad)
ORG: none
TITLE: Gradient methods forsolving problems of terminal guidance in
linear systems of automatic control
q
SOURCE: Zhurnal vychlelitellnoymato ',iki.i matematichaskoy fisiki, V* 5.* no, 5#
1965# 894-902
TOPIC TAGS-.. linear automatic control system, terminal guidance, vector functlon,:~,
ordinary differential equation, function theory
iABSTRACT: The authors consider the problem of minimizing the strongly Convex
'functional of.the terminal stage of an object whose motion is described by a linear'~
1 System of ordinary differential equations
dX (1) B) (t) 11)(0 + A*
dt
!with initial conditions X(O)= X0 where X, Bj 0 f are n-dimensional
Ivectors with respective coordinates xlt'* Nn b1jYo*oRbnj fil"01fn, std
UDGs 516:51:62-50
1/2

L 26113.66
ACC NR: AP5025113
A (sit) is an n by n matrix. It is assumed that bij (t), fi (t) anij aik (t)
are real-valued and continuous for t 9 (0,T) where T-7 0 is the given period
guidances The authors determine the r-dimensional vector-function
.(t), jui(t) satisfying the condition 1u (t)l :Slp (j
U3
(
~1,(%Tl' Which. minimizes- the, functional g(X(T.,u)). R the latter- g(z) is a
-V iil,-Valued, t 0 ".'afferentlable and strougly,convex fun~Won Such' ,
0
02g(x)
Xish M Zia,
h-i
where m> Oisa cons ui,-U)
tant and a the solution of the systen uncler con-
Sideration corresponding tothe solution u.. The use of the gradient method for
the solution of the problem is also studied. The authors thank V. I. Zubov for
advice. (X-ig. art. hast 1 figureL and 37 formulas*
J
A 7
W
V!,
. . . . . . . . . . . . .
A
4