SCIENTIFIC ABSTRACT USELIS, J. - USENKO, S. KH.
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CIA-RDP86-00513R001858110020-5
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RIF
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S
Document Page Count:
100
Document Creation Date:
November 2, 2016
Document Release Date:
March 14, 2001
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Publication Date:
December 31, 1967
Content Type:
SCIENTIFIC ABSTRACT
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DYK, Tadeusz; SOWIN3KA, Janina; USELIS, Jullusz; BORDZILMSKA, Irena
Nteomyelosclerosis. The nature of disease and its clin-Lml
picture. Pol. arch. med. wewn. 33 no.,4:439-446 163.
1. Z III Kli:aiki Chorob Wewnetrznych AMG Klerawnik: prof.
dr med. M. Gmski. KI-iniki Radlologii. i Radioterapii AMG
Kierowniks prof. dr mod. W. Grabowski.
(AMffA, LEUKOERYTHROBLASTIC)
USELIS, Jqnusz; RhYDICKI, Andrzoj, Stwilolaw
Health condition of seanpn examined at the C~tFatfrz~-zs_~
for occupatlenal 11-seasps of the Jru;titute rX ',.Tr_IrJnf- '--.
Gdansk. Bill. In.,A. Mar. Med. Gdansk 15 no.*'.-2I'I_2I8 I ~. '?,
.j ~ ~
1. From the Institute of Marine Medicine in Gdruisk.
DYK, Tadeusz; USELIS, Ju1iusz
Anyloid renal cirrhosis. Renal amyloidosis in ankylosing
spondylitis. Pol. arch. med. wown. 33 no,7:835-839 163-
1. Z III Kliniki Chorob Wownetrznych AM w Gdansku Kie:rownik:
prof. dr mad. M. Gamaki.
SIONDYLITIS, ANKYLOSING) (ANYLOIDOSIS)
DNEY DISEASES) (ARTHRITIS, RHEUMATOID)
M
DYK, Tadeusz; SOWINISKA, Janina; BORDZIIDWSKA, Irena, USELIS, Juliusa
Cases of osteanyeloscleroals. The latent and polyglobulic
period of disease complicated by liver cirrhosis. Pol. arch.
med. wewnet. 3.3 no.11:1283-1287 163.
1. Z III Klini1d Chorob Vewnetrznych AMG (kierowniki p:rof.,dr.
med M.GamBki) '.*z Zakladu Radiologii AMG (kierownikt prof., dr.
med. W.Grabowsm).
it,
TZENBAYEVA . K.
... ...
Approximate method of solving the first boundary value problem
in the mathematical theory of elasticity for a sphere. Izv.
AN Kazakh. SSR Ser. fiz.-mat. nauk 3 no. 3:45-51 S-D 165.
(MIRA 18: 12)
fv x
8h670
17 34
/I. 'SIP 0
AUTHORS:
TITLE:
2,101
PERIODICAL:
S/020/60/13'i/001/023/030
B004/BO56
Xasatochkin, V. I., Zamoluyev, V. K., Kaverov, A. T., and
Usenbayev, K.
The Thermophysical Properties of the Transition Forms of
Carbon I
Doklady Akademii nauk SSSR, 1960, Vol. 135, No. 1,
pp. 121-124
TEXT: The authors give a report on the determination of the specific heat
ep, of the temperature coefficient a of thermal conductivity and of the
thermal conductivity A of the transition forms of carbon, obtained by
heating petroleum coke, channel black, and thermal carbon black to
tempezatures of between 1000 and 30000C in nitrogen- or argon atmosphere.
Clpand a were determined according to G. M. Kondratlyev (Ref, 7), A, was
calculated according to the equation A = c pap (P = weight by volume). The
measurement results for op and a are represented in Figs. 1,2, the
Card 1/4
8~670
The Thermophysical Properties of the S/020/60/135/001/023/030
Transition Forms of Carbcn B004/BO56
calculated values of k in Fig. 3 as a function of temperature. Fig. 4
shows A as a function of the duration of heating of the substances
mentioned at 1600 and 25000C, as well as for coke coal (5000C) and coal of
the type 7TC, (PS) (7000C). In Table 1 the degrees of graphitization y are
given. The results obtained are interpreted. 1) Petroleum coket: slight
decrease of cp below 18000C by destruction of the side radicals. As a
result of recombination of the liberated bindings, the spatial network of
bonds, however, remains conserved. At 1600 to 20000C, a considerable drop
of cp takes place by combination of neighboring carbon layers. Abcve
20000C cP decreases becauae of orientation cf the carbon layers from
dmax - 3.42 A to dmin = 3.35 A in graphitized carbon, Ymax = 1- In the case
of thermal carbon black crystallization also sets in at 20000C,
gTaphitization, however, remains incomplete, Ymax ~ 0-77. The uniform
course taken by the crourve and the incomplete graphitization is
explained by the forming cf a spatial network of bonds. which contains
Card 2/4
8h67o
The Thermophysical Properties of the S/020/60/135/001/023/030
Transition Forms of Carbon B004/BO56
thermostable =C=C=C= bonds between the carbon layers up to 30000C.. In
channel black, cP is low -uptoi about 13000C, it has' a maximum at 17000c,
whereas between 2700 and 30000C, cp, a and A fall. Channel black does not
crystall'", Ymax - 0.09. Also in this case the cause is a (dianser)
spatial network of bonds, formed by the splitting off of oxygen-containing
radicals and the forming of allene-carbon chains between the carbon layers.
In fossile coals, a melting of the spatial network of bonds occurs at low
temperatures similar as in the case of organic polymers. The properties of
the carbon materials thus depend on 'he polymeric character of their
structure and on the nature of the s;atial network of bonds. Only f~or
y = I there is no spatial network of bonds. There are 4 figures, 1 table,
and 12 references: 11 Soviet and 1 British.
ASSOCIATION: Institut goryuchikh iskopayemykh Akademii nauk SSSR
(Institute of Mineral Fuels of--the Academy of Sciences,
USSR)
Card 3/4
84670
The Thermophysical Properties of the S/020/60/135/'001/023/030
Transition Porms of Carbort B004/BO56 "X
PRESENTED; June 10, 15,60 by M. M. Dubinin, Academician
SUBMITTED; April 2, 1960
Card 4/4
11, - - 1,
USENBAYEV9 K.t CAND CHEM SC19 1" 01' THE
4~
" 10 ORKSOF CARBON'l~
STRUCTURE AND PROPERTI.18 OF TRANSIT N F a
Q - - - "- ,
moscowt 19610 ON a INST OF MINERAL FUELS). (KL,
2-61t 200).
-32-
2063P
S/0 2 0161113 6,10r-~61011.,102 b
B103/1*03
AUTHORS: Korshakj Ve V., Corresponding Member AS U3~41, Kasatochlkiri, V.I.
Sladkov, A. M., KudrYavtsev, Yu. P., and Usenbayev,
TITLE: Synthesit, and properties of polyacetylone
PERIODICAL: Doklady Akademii nauk SSSR, v. 136, no. 6, 1963., 131!2-13)j1,
TUXT : The authors produced polyacetylene (PA) and studied its chp-ilcal
structure and physical properties. They assumed that PA formed in the
oxidation of bis-acetylene acetylenides of the type HC - C --'(Cq2)n C CF
which are said to be among the polymeric products not yet studied. TheF-
had already suggested a formation mchanisn of PA in Ref - 3. In the present
investigation, they produced the required acetylenide by passing acetylene
through the ammoniacal solution of a salt of bi valent coppf~r. Subsequently,
the acetylenide was oxidized by an aqueous solution of potassiu:q ferri-
cyanide at boiling temperature. The authors assumed that the resultin.
black povider (containing 98% of C) was a mixture of polymer homologs of
polyacetylene. On the basis of the temperature -denerden' veirht losses
Card 1/2
(Fig. 1) and the electron paran-ar!netic resonance, they conclude that this
product is a polymer wth cuwilence rtructure, prolhably H_ (C..C..C.=C) n- 1%
PA shovmd hi~,h heat resistancr., being trannforrPd Into .7rap'nite 1 4
1 on. 1,
23000C- Below 2300 C- the carbon In PA remains i.n the form of poIjac-tylere.
conclude that the PA sample investigated is an n-type semi conductor. The
copper atoms imbedded In the molecular carbon chain with polyallene struc-
ture play the role of the electron donor. This Is confirmed tT the fact
that the of PA sampleo %41-tch w-re produced with the use of strorv_er
copper-free oxidizers (nitrate ion, H202) is equal to zero. The chanfe of
the sign of (near zero at 1300 and 15000C t above 1500 up to 23000C
corresponds to the trannition of the PA sample to a p-ty
, pe seraiconductor.
The authors Viink that this is coupled w-ith the thermal dissociation and
the separation of copper- and hydrogen atoms from the carbon chain., and
is certainly connected mith the acceptor properties of the terminal C
atoms. There are 3 figLLres, 1 table, and 3 reP?rences: 1 Soviet-bloc
and 1 non-Soviet-bloc.
ASSOCIATION: Institut Coryuchikh iskopayeaVIdi Akademii nauk 5.SSR
(Institute of Mineral Fuels of the Academy of Sciences USISR)
Institut ele,-rientoorganicheskikh soyedineniy Akademit nauk
SSSR (Institute of Elemental-organic Compounds of the
Academy of Sciences USSR)
Card 2/2
. I
f ;' I- - ~'- - r17 '1--- -~ .1 ~ - I-
ZAPLAYNYT,
Potential production caperity increase at the Unt-Tammogorsk
zinc plant. Trudy Alt. GWEI no.2:155-163 155. (MIRA 10:1)
(Ust-lamenoprok-Zinc industry)
137-1958-2-2632
,;r/a~nslation from: Ref ~alvn~y zhurnal, Metallurgiya, 1958, Pir 2, p 61 (USSR)
AUTHORS: Zaplavnyy,A.Ya., Usenbekov,A.P.
TITLE: The Cost of Producing Lead at the Plants in Kazakhstan
(Sebestoimost' svintsa na zavodakh Kazakhstana)
PERIODICAL: Tr. Altaysk. gornometallurg. n.-i. in-ta, 1957, Vol 4,
pp 160-171
ABSMACT: This is an'analysis and break-down of the.net cost of smelting
lead and its associated metals at plants in Kazakhstan. It includes
recommendations for cutting costs and for increa.sing the volume
of treatment of Pb concentrates with the aid of the reserves
exiBting at the Ust'Kamenogorsk plant.
B.Z.
1, 14ad-Production-Cost analysis
Card 1 /1
USENKO, A.; MERKIN, A.
Preventing axial displacements of bottom rolls in the ZM roller
mill. Muk.-el(qv-prom. 24 no.12:21-22 D 158. (MIRA 12:1)
l.Sorochanalmara mallnits, No.16 Vinnitakage upravleniya khleboproduktor
(for Usenko). 2. Upravlenive mukomollnokruwanykh i kombikormovykh
predpriyati.v Hinisterstva khlaboproduktov SSSR (for Markin).
(Milling machinery)
USM09 As, insh,
1; ~ 1',",-
~"
The ~Jaro device for cleaning and chocking spark plW used for
checking armature winding of generators, Avt, transp, 36 caj.,
13 Hr v 58. (kMA 1113)
It Mislyabinskiy politakhnichookly inatitat,
(Aul;omob ile a --Mle o trio equipment-4lesting)
USENKO, Anatoliy Fedorovich
[Auxiliary groups of the party and state control at work]
Gruppy sodeistvila partgcokontroliu za rabotoi. Tula,
Tulfskoa knizhr..oe Izd-vo, 1963. 33 p. (MIRA 17:9)
BOBROVI F.S.,, polkovnik medosluzbby; USE14KO, A.G., kapitan med.sluzhby
DDaimetric control of protection agains X rays b7 means of the
ODKZ' dosimetrio de7lee. Sbor.nauc'h.trud.Kiev,okruzh.voem#gosp,
no#4045-352 ~62,- (HIRA 1635)
(RADIATION-DOSAGE) (Z RAYS)
USHNKOI A.I :.
Surgical treatment of acute cholecystitis in elderly senile
patients. Wravockhraneniye 6 no.2t 24-26 Hr-Apt63.
(MIRA 161l0)
1. Xv kafedry gotipitalinoy khirurgii (zave - prof* PoVo
R,yzhov) Kishinevakogo meditsinskogo institutao
A
TSIULIN, Vladimir Andreyev.lch;POZDIIEYEV, M.L., red.; USENKO, A.L.,
red.izd-va; AKOPOVA, V.M.p tekhn. red.
(Reference book :)n internal combustion engines for a mechanic
in lumber floating] Posobie po dvigateliam vnutrennego j3gora-
niia mekhaniku lesosplava. Moskva, Goslesbumizdat, 196%
160 p. (MIRA 17 1 1'.))
MOMTS 0 P. V. j USENKO,, A. N.
First coat of paint baBed on magnesiumo Mashinostroitell no.7:40 JI
162. (MIRA 15:7)
(Painting,* Industrial)
FILIPPOVA, Ye.S.; YASOV, V.G.; MMIYENKO, I.A.; ARTSIMOVICH, G.V.,-
EPSHTEYN, YeJ., prof., doktor tekhn','--naukj UZMO A.P .
1 9
SIRIK, V.P.; SMIRNOV, L.V., otv. red.; KOSTONIYAN, A,YA.0
rdd. izd-va,- HAKSDIDVA, V.V., tekhn. red.
(Combinition drilling of holes with hydraulic drills] Udamo-
Vmshchatellnoe burenie skvazhin gidroudamikami, Moskva
Gosgortekhizdat, 1963. 83 p. (Boring) (MIRA 16:5~
YASOV, V.G.; USENKO, A.P.; BESSONOV, Yu.D.; SIRIKI V.F.
L, Ll-
Influence of certain parameters on the characteristics of direct
action Jet bit,, Izvo vys, uchobo zav.; noft' i gaz 6 ni).10:19-23
163. (MIRA 17:3)
1, Dnepropetrovskiy gornyy institut,
SOLNTFIFV, A.M., inzh.; USENKO, A.S., inzh.
Rapid vertical shaft sinking in the Kuznetsk Basin. Shakht.stroi.
7 no-5:17-19 ItT 163. (KRA 17:4)
1. KuzNlIshakhtO;3troy (for Solntsev). 2. Stroitellnoye
shakhtoprokhodchf)skoye upravleniye No.1 tresta Prokoplyeiskshakhtostroy
(for Usenko).
USENKO, D,N., dotsent; KRYUKOV, B.I., inzh.
Basic principles in desigining systems of resonance acreens
with nonlinear vibration absorbprs. Izv. vys. ucheb. zav.
gor. zhur. no. 4:98-105 161. (MIRA 14:6)
1. Dnepropetrovskiy ordena Trudwogo Krasnogo Znameni gornyy
institut imeni Artema. Rekomendovana kafedroy stroitellnoy
i teoreticheskay mekhaniki Dnepropetrovskogo ordena Trudovogo
Krasnogo Znamnni gornogo institilta.
(ScrTp~ (Fining))
KRYUKOVJ, B.I.; LYAKHOVITSKIY, S.I., kand.takhn.nauk; USENKO, D.N.,_krAnd.-
tekhn.nauk
Designing resonance conveyers. Vop. rud. tzrancp. no.6tl36-141
162. (MIRA 15:8)
1. Dnepropetrcivskiy gornyy institut.
(Conveying machinery)
STOVASI M'V-;-Y=KQ346XI-
Briefly about the forces of gravity and inertia of our
planet. Izv. AN SSSR. Ser.geoll 27 no.11:101-102 N 162.
(MIRA 15:12)
1. Dnepropetrovskiy gornyy institut.
(Gravitation)
Works rf t,?-.e Ccntrc~ rc--l. cl, ",.E, REr'",
3. orl,
Volume 9, 1939, 91 pages.
"The Drying, Collecticn and Storage of Peat Stable litter." by
F, Usenk , A. P. Glukhareva, A. 14. Mitorfanova.
SO: Botanicheskiy Zhurnal, Vol XXXV, No 1, po 100-110,
Jan-Feb 1950, Russian birno ner, Moscow/Leningrad (U-5511,
12 Feb 1954)
USEINKO, F. I.
Isenkov F. I. "Mechanization of the extraction of peat for fertilzer, "
In symposluri: Torf v nar. khoz-ve Belorus, SSR, Yinsk, 1948,
p. 219--22
So: U-3566, 15 March 53, (Lotopis 'Zhurnal Inykh Statey, No. 13, 1949)
USSERK01 G.
Alfalfa.
Summer sowing of grasses and: legumes. Kolk.proiz. 12 no. 5, 1952.
9. Monthly List of Russian Accessions, Library of Congress, November -19A Unclassified.
USENKOV G.
Grasses.
Summer sowing of grasses and legumes. Kolkh. proiz., 12, no. 5, 1952.
9. Monthly List of Russian Accessions, Library of Congress, November -195:Y.2 Unclassified.
1. USENKO, G.
2. ussa (6oo)
4. Wheat
7. 200 poods of winter wheat per hectare. Kolkh.proiz. 12 no. 12, 1952
9. Monthly List of Russian Accessions, Library of Congress, Mar~-h 1953, Unclassified.
LIVCHAK, I.F., doktor tEkhn. nauk; Inzh.; BEI-Iialfll, M.D.;
inzh#;YMEYKV, B.S., Inzh.; ILIYUSHIN, L.M., inzh.
Using water heating systems with plinth convectors without
casing. Vod. i -,an. tekh. no.3:18-21 164 (MIRA 18:2)
-USENKO, I.K.; ZIIIKHAREVA, K.D,,; RODOVA, F.Z.
Polymethine dyes containing ferrocene residues. Part ):
Synthesis of farTocenylbenzothiazoles and preparation of
thiacyanines. lhurob.khim. 33 no.3:798404 Mr 163. (MIRA 16:3)
1. Kiyevskiy filial Donetskogo instituta sovetskoy torgovll
i Institut orga:rLicheskoy khimli AN Ukrainskoy SSR.
(Ferroccne) (Benzothiazole)
(Dyes and dyeing)
USZWKO, I.M.; VORDBITEV, V.G.
-------
Experience in StUdYing fundamentals of industrial production.
Politekh.obuch. no-12:24-Z7 D '58. (MIRA 11:12)
1. Sreduyaya sh1cola No.45, st.Kavkazakaya Severo-Kavkazakoy
shelesnoy dorog-i.
(Technical education) (Field work (Educational metbod))
Date of crystafto rocks of Smvluk River.
Nd k
S;O MI-W(IL119).-Conspn.
and 'Us. analYersofamphibolit". granites. aplites pegniA.
likes . migmatiles, arul diabase ol this region are *
XFVl mf~h
. . , - , '. , 1. W.. I " "
1 -
0
. . a., SW&CHWO, 1. V'.
Petrology - Donets Basin.
Traces of Jurassic volcanlan In the northwestern part of the Donato Basin.
Dokl. AN SSSR 85, no. 2, 1952.
9. Monthl List of Russian Accessions, Library of Congress, November -1951? Uncl.
1. USrNKOj 1. 3.
2. USSR (600)
4. Azov Sea Region - Geology, Structural
7. Formation of the crystallic foundation of western Azov Sea region.
Dokl.M SSR 87 no. 5, 19,112
9. Monthly List of Russian Accessions, Library of Congress, March 1953, Unclassified.
U$IffQ.A _I.S.; RODIONOV, S.P., redaktor; MUSNrK, N.I., redal-tor; SIVACHOWO,
rg , tekhredaktor
[Precambrian metabasites and U-Itrabasites of the Ukrainian
Crystalline Kessif] Arkheiskie metabasity t ulitrabasity Ukrainskogo
kristallicheakogo massiva. Kiev, Izd-vo Akad. nauk Ukr.S!M. 1953.
100 P. (MLPA 8t2)
1. Chlon-korrespandent AN USSR (for Rodionov)
(Ukraine-Rocks. Crystalline and metamorphlo)
1, "ISETIKO.-T.S.
2- U-;S'.R (600)
4. Ukraine-Geology, Structwal
7. Age relations of 4ike-efNsive rocks of the Ukrainian crystalline massive.
DokI. AN SSSR 88 no.3. 7.953.
9. Monthly List of Russian Accessions, Library of Congress, April - 1953, Uncl.
USMO, I.S.
..............
larly stages of thil Ukrainian crystalline massive forwtion. Dokl.AN
635R 95 no.5:1067-:1070 AP 154. (MIRA 7:4)
1. Institut geologAcheskikh nauk Akadoxii nauk U38R,
Predstavleno akadenikost D,S,Korzhlusklz*
(Ukraine-Rodko, Orystallins and votanorphio)
(Rooks, Orysta)llne and metamorphio-Ukraim)
'U S-ENICO, I. S.
Card 1/1
Author t Bomadukaya.. L,, Go; Lapehikp F. E,, and Usenco, 1. So
Title t Effusers of Chernigoy region (Dneper - Don depression)
Periodical : Dokl. AN SSSR~ 95p 6,, 1279 - 1282; 21 Apr 54
Abstract : The article tolls about a lately discovered effusive stratum of soil
under Dneper-Dcn river basin. The strat= rests on the pro-Cambrian
crystallic base; its effusive thickness lieG 1587-2751 meters deep*
Petrographic and petrochemical analyses show the strattm to have
great similarity with an Upper-Devonian stratum of the river Mokray*
Volnoyakhap, This indicates that both strata formed abtsut the Sam
time.
Institution i
Submitted t 164#;eb 54
- ------------
'VAMphlbOlO AbbsItOf front XdTOl Rog. Ya',N,Bdeyts~yl
L. 0. Vernadskaju, und 1. S. Usenko. Dokldy Akad:l
Nauk S.S.S.R. IM a cumming-i
Mill',febeekite fit on of I to 2 tntr. length we O)wYlItntly:
dtvdoW in the atuphibole-inagn:t1te rocks of the KjlvoT!
Rox Fe ore depodw. Itcal asbesics 19 lo"Ily otserved in'
veltdots with fibefg-A 6-15numardy up to 23 or even 50min.1
ltngtb. The rulneral is of itilver-gray or sninewhut yellowish'
color, sporadically interspeml with blac rieb"kite. The
fibrous rggregatef; show apparcutly linear eAtinction.
Puartx 13 often itr,trgrown parallel to The fibes. am also.
it,
tiomorphic crystals of magnetite are typical. V. of thf~
4ftipl6bole is 3.34; -Y - IRA to 1,702; a - 1.674 to 1.078;;
Thranuty.56corms-'UmIdsto
the crystali(XIIC-.111. farinula
i.e. of an Fe-rich cutp",
saingtonite. Tlic:owcontciitinalk2:iei(ordyO,28%)isirw
contrast tq,the With conteuts ia riebeckite, a typical Na
FO" a1upbibele. The spectrochern. mamoi. established rml
accessory and trace e efeinents: Cu. Zo, Nii Ga, So. The;
x-ray analysis of piwder dhLgriuns of the tumrningtonit~ as. j
bestos Is different I ram that for other cummingtonites from;
Krivol %)s and fiom Uttersvik. The difiezeatial-tbennal'
analysis wvei show exothermic, effects at 6220 and 910'.1
TUe latter effect is evidoutly caused by an Intemw oxidation
oftheFcOintlici-ilicate. The trietasontatic-bydroihzmali
5tResfs of the asbwtos of Krivol Rog is evilt-1-t6la4.
U,5F-A~ K C~
%.Aaq Sid Of th=kdO!raDniUAdx of the Ukrainim
V t4 1
shield. 1. S. xdy A kad. Na mill S.STR. 104,
viasplex rutarr of Ott UkraiaLw Shield
is chan 'curizeil by the vcry (Ad formati.-a of cryst. jchi~,ts
and thit muds yuuniter fiAnustiiin of highly mcunuxlthic
3JILAS. It 6 conflihied with Amultiplu. wtooic f(Mlag and
ault;ng of grAuitolds, XnL63ca, and migmatites. la the
latter Izoup die koliments wid cffu~ivcs arc witlely dc-
velopcd in ortho und lx&rt gneisses with cordicrite, Oil-
mitnitei aud graphite und with dolumitic liniestouts for mug-*
nesites with sill"tu.; und ulutahausilicaus. Oil the other.
haud there ure amphi1xilites, pYruxcuc-I)Liglocluw lpxeissc-j~
actinuilte-tremolite roks, t;&-chlorilc *chlzits. und tatc-
c4rliomde rocks, :ihnil,sr to l6tviolitc-4, ull derived frunt
ti~trabailu. Grimillwirm of the liyl)rltls to finuiltijids is
jpucral:y observed, e~pccially lit the triLit,ition,% between
the gra-lited (if Derdichev uld the illigulatitt:3. 111C.-K trall-
shions,tre Iltustritud by clonn. analyies of av. rmk groups,
sh,)winjt thecoincidence ef thciv. licruicliev graoitewit:i die
'unip.- of it V. of= llyb~ld -W. froin 15 ff..L--.
I ainpliflialite, and I or 21 clitartzites, ur representatives
of t lies -dintent-clTusiw: o,nildwc. KjOwusevidwstlyiotn-
ducLd atu the byhrid by thc graoitizatioo sjins. 17he
petroclitin. rclatious Intwce" the large grunituid massives
ofWroichey Kiruvogr;sd, und zilitfq] lit arg well Ove.3 frotil a
pri~,Vt '"ll 47 lit; Z,4V.,;itAkd itamiltwi, Oldy Out- jr.ww
dlolltvii and U(V WivolApI64 by 1114,11
114;14ct ilmleut* lit Cito alld b-Cr tN"ItCIM lit KO); 1116 fact
I+ expUncd by the wjimilat-,in ul nitcL-rctius matcrLd bi
hiffier tevi:6. TIM grAnitoid, of Kim-grad alld Zhito.
nor am higher In KO that% WA 4 lk-rdic-o:Y. 11ey art.
howgre", consunguilde its 6 sten from the icry unifuran type
of Aicll- prituary zircons. W. Elled-
~N 4. Z-k-i ~A r-L 0
U E
15-57-4-4482
Yranslation from: Referativnyy zhurnj,11, Geologiya, 19-:77, Nr
p 57-68 (USSR)
AUTHOR: Usenko, I. S.
TITLE: Amphibolites in the Basin of the Gornyy Tikich and
Gniloy Mich Rivers (Amfibolity basseyna rek Gornogo
Tikicha I Gnilogo Tikicha)
PERIODICAL: Nauk zap, Kiyivslk. un-t, 1956, Vol 15, Nr 2, up 67-86
ABSTRACT: The amph~bolites were formed in the first (Archean)
stage of developwnt of the Ukrainian crystalline
shield. They are metemorphosod basic magmatic rocks,
predominantly volcanic. This opinion is attested by
the petrochemical features of the rocks and by the
correspondence between the mineral paragenesis of the
amphibolites, and the paragenesis of the basic rocks:
pyroxene (hornblende in the amphlbolites), basic
plagioclase, magnetite, ilmenite, pyrrhotite, the
Card 1/2 presence of diabase and gabbro-diabase relict structures
Amphibolites in the Easin of the Gornyy Mich (Cont.)
15-57-4 -44 82
and the presence of Ga, Ni, Cr, Cu, and other elements in the
amp hiboli tes .A paragenetic study of the metabasites reveals t~;eir
relationship to three rwt-,amorphic stages: 1) the highest temperature
staze with unstuble mineral associat-Lon--pyroxene, horriblende,
plagioclase; 2) a somawhat lower temperature stage with a stable
association--hornblen(le, plagioclase; and 3) a low-temperature stage
with hornblende and a'bite-epidote minerals. The rocks may be
divided into gabbro-aniphibolites (hypersthene, diopside, and
hypers the ne-diops ide) and amphibolites (plegioalt-se-hornblende,
biotitized, epidotitized, and albitized). The amphibolites belong
to the same group as the amphibolites on the Yuzhnyy Bug River,
those in the western laov region, and those in neighboring areas.
The author supplies data on the chemical composition of the
hypersthene-diopside Emphibolites, amphibolites, biotitized arnpUbo-
lites., and foliated arnphlbolites.
Card 2/2 S. P. P1.
-44 G -o' tel d
M. 4 t i-.-f ni-i~
~j7
all v
Tu
-B--c
777--
USEIMO, Ivan,Stepanovich; LICHAK, I.L.. otv.red.; MELINIK, A.F., red.izd-va.;
BOGDAMV, S.M-., tekhn.red.
[Basic and ultrabasic
ulltraoonovnye gornye
Akad. nauk USSR, 1956.
geologichaskikh nauk.
Trudy, no.5)
rocks in the southern Bug Basin] 09novmys i
porody basseins. lUzhnogo Bug&. Kiev, izd-vo
142 p. (AWemiia nauk URSR, Kiev. Instytut
Seriia petrografil, mineralogii i gookhimii.
(MIRA 11:7)
(Bouther.nBug Valley-Rocka, Siliceous)
U~suw