SCIENTIFIC ABSTRACT IVANKIN, P. - IVANKINA, N.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R000619010010-3
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: August 10, 2001
• Sequence Number: 10
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT


WO NMAD t

H
j 4
7
1
1
111 11P T,
.

IVANKIN, F.F.; LIOGENIKIT. S.Ta.
Electrical prospecting In the RudvVy Altai. Vest.Aff Kazakh.
SSR 12 no.8:15-24 '56. (MLRA 9:12)
(Altai Mountains--Prospecting--GeopbysicaI motbods)
w

- ------------------------ -- - ----------------- -------------------------------
USSR/Cosmochemistry. Geochemistry. Hydrochemistry. D
Abs Jour Ref Zhur - Khimiya, No. 8, 1957, 26514.
Author iygn~-i~p ~F
Inst Scientific Research Institute of Mining
and Metallurgy of Altai.
Title Questions of Geological Development of
Mining Region of Altai at the Irtysh.
Orig Pub Tr. Altaysk. gorno-metallurg. n.-i. in-ta,
19569 3, 5 - 49o
Abstract No abstract.
Card 1/1

IVAMN P 7 doktor go Iologo-mineralogichankM nauk.
~Y_ I
Geological service of the Ruduyy Altai in the sixth five-year plan.
Vest.AN lazakh.53a 12 no.4,8-13 AP 156. (MMA 9:8)
(Altai mountains--Geology, Economic)
Y
joll :,YJ
;H'll INN

IVAVKIN, P.F.; MITRYNTEVA, N.M.
Process of the development of copper and lead-zlnc mineralization
in the Nikolayevskoye deposits In the Altai. Izv.KN SSSR. Ser.
gaol. 21 no.9:27-43 S 156. (MLRA 9:11)
1. Altayskiy gorno-mefallurgicheakiy nauchno-iseledovateliskiy
institut, g. Uat'-Kamenogorek. Kas. SSR.
(Altai MountainB--Iron ores)

A
IYANKIN, P"rjilippovich; SEMN110VA, M.Y., redAzd-va; KRYNOCHKINA, K.V.,
tekhn.red.
[Geol y and genesis of complex metal depostis in the Xrtysh River
regioln Goologtia i voproBy genezies polimetallicheskikh mestorozhdo-
nii FrUrtyahlia. Hook-va, Gos.nauchno-tekhnJzd-vo lit-ry po geals
i okhrane nedr, 1957. 246 p. (MIRA 11:2)
(Altai Rountains-Ore deposits)

M 41111" . ..... .

SUBJECTs USSR/Geology
AUTHOR; Ivanking P.P., and Purkino A.V,
TITLE- "Structural Metallogenic Zoning of the hudnn Altay Ore Depo-
sits Area as a Basis for Exploration and Prospecting ti. (Struk-
turno-metallogenicheskoye rayonirovaniye Audnogo Altaya kak
oenova vedeniya poiskovykh i razvedochnykh rabot)
PERIODICALt "Izvestiya Akademii Nauk SSSR", Seriya Geologichel3kaya, 1957,
#4# PP 84-97 (USSR).
ABSTRACT: While the system of metallogenic zoning of the south-western
territory of the Altay mountains by V.Po Nekhoroshev and P.P.
Pilipenko had proved to be a valuable aid at prospecting in
the past, these zoning schemes did not meet present requirements.
Presently the question of origin of poly-metallic mineralization
and its location gained great importance. Experience obtained
at numerous large ore fields and deposits of sulfide ore has
shown that a3sumptions of deposits can not be based solely on
studies of respective geologic textures, but have to be based
also on the knowledge of interrelations existing between the
peculiarities of deposits and their geologic texture.
Card 1/4
tq 11 q! jjj~ !I.

.i 7 ':
---7/23
TITLE: "Structural Metallogenic Zoning of the Rudnyy Altay Ore Depo-
sits Area as a Basis for Exploration and Pruspecting". (Struk-
turno-metallogenicheskoye rayonirovaniye rudnogo altaya kak
osnova vedeniya poiskovykh i razvedochnykh rabot)
Lead-zink and copper deposits within the Rudnoy Altay area are
dispersed over a wide territory and overlie different strato-
traphic complexes of the central Paleozoic era. The vertical
extent is also considerable, the stratographic thickness being
6-7 km. It is of importance to note that mineralization took
place on all known intrusions of magmatic rocks. Peculiarities
of sulfide layers are depending largely on the geologic texture
and tectonic development, the metamorphosis of rocks and other
circumstances accompanying the sedimentation of ore. These
peculiarities enable to differentiate the poly-metallic belt
of Rudnoy Altay.
The following characteristics can be used for the classificatIon
of ore bearing geologic layers: the relation of ore fields and
deposits to regional textures and geologic complexes, the inner
texture of ore fields and deposits and the shape of the ore
layers. According to these symptoms, sulfide deposits of the
Rudnoy Altay can be subdivided into 3 basic groups% 1) ore
Card 2/4 fields and deposits located beyond the direct influences of

3. ja -.1[23
TITLEt "Structural Metallogenic Zoning of the Rudnyy Altay Ore Depo-
sits Area as a Basis for Exploration and Prospecting". (Struk-
turno-metallogenicheskoye rayonirovaniye rudnogo altaya kak
oanova vedeniya poiskovykh i razvedochnykh rabot)
regional wharping zones, 2) Ore fields and deposits located
within the regional wharping zones, and 3) Ort fields and de-
posits located at some distance from the regional wharping zones.
The authors give a detailed account of the geologic peculiari-
ties ariaing from the varying degree of deformation during and
after the process of contortion.
The article containG 5 figures. The bibliography lists 10
references, of which 10 are Slavic (Russian)
ASSOCIATIONi Trest "Altaytsvetmetrazvedkall of the Vinistry of Non-Ferrous
Metallurgy of the Kazakh SSR. Altay Mining Metallurgic
Institute of the Academy of Sciences, Kazakh SSR, city of Ustl-
Xamenogorsk.
PRESENTED BY t
SUBMITTEDi At the Session of TEKHSOVIET of the Ministry of Geology and
Conservation of Natural Resources USSR, in conjunction with the
Card 3/4 Ministry of Non-Ferrous Metals and the Academy of Science of

TITLE: Structural Metallogenic Zoning of the Rudryy Altay Ore Dopo-
sits Area as a Basis for Exploration and Pruspectling". (Struk-
turno-metallogenicheskoye rayonirovaniye rudnogo altaya kak
osnova vedeniya poiakovykh i razvedochnykh rabot)
the Kazakh SSR, JulY 17, 1954.
AVAILABLEt At the Library of Congress.
Card 4/4
- ---- -----
I W-pu, X1 U M!u Laum!4
77
TIT

IVANKINt P.P.; MITRYAMA, N.M.
iome -results of struatural and paragenetic studiess o:e "Xikolayevi*0700
sulfide deposits in the Altai. Truc~T Alt. GMI AN Xazshh. SSR no.5s
14-33 '57. (MIR& 11'114)
(Altai Territory-Salfides)

iv~<
AUTHOR: I-vankin, P.F. 11-10-21/23
TITLE: About the Book Structural Geology"by G.D. Azhgirey (0 knige
G.D. Azhgireya "Strukturnaya Geologiya")
PERIODICAL: Izvestiya Akademii Nauk SSSR, Seriya Geologicheskaya, 1957,
# 10, p 110-112 (USSR)
ABSTRACT: For a period of 15 years, after the publication of "Structural
Geology" by M.A. Usov, no new books were published on this
subject. Thus the publication of G.D. Azhgirey's book on the
subject, published by Moscow University, 1956, meets a long
felt demand. The book is richly illustrated with geologic
plans, structural charts, various schematic drawings, and
photographs. The author deals in detail with the geologic
structures of the Caucasus, Kazakhstan and the Altay. The book
is well edited and due to its ease of comprehensibility is
suitable for a wide circle of industrial geologists.
SUBMITTED: 26 December 195] (Notei Evidently a typographical error)
AVAILABLE: Library of Congress
Card 1/1

IVANKIN* Pj.. doktor geologo-mineralogichookikh nauki KMEBM, Y.S.,
-----"9MVtftt geologo-mineralogicheskikh nauk.
Methods for petrographic and mineralogical study of are izones
in the Irtysh Valley. Vbst. AN Kazakh. SSR 13 no,6:22-32 JTe
'57. (MLRA 100)
(Irtyah Vallay-Ore deposits)
]T7]T..

or
8 0
ri
lWai
ainuj
SZ;
RON&
toc!
vs gE st
HIP Al -.85o
0.9 E z U19
i *- 4 lo! I IN'T.Is
L'3 a i". a -j
av
0., Mill

IVANKIN, P.F.
Genetic types and stages of the sulfide mineralization of the
Rudnyy Altai. Zakonom. razm. polezn. iskop. 2:351-Ya (159.
MIRA l5t4)
1. Altayskiy gorno-metallurgicheskiy nauchno-issledovatel'skiy
institut AN Kazakhskoy SSR.
(Altai Mountains--Ore deposits) (Sulfides)
F "I

illrRoV, P,Ya.; AYTiJ,JY.-,7, Z~~, A.; AUZOV, M.0,; AXHVYDSA?11J, 1TX,,; BATISHCH37-
TARASO17, n.D.; U7,A110VA, 11.1%; BRISUV, S.B.; BXYMIUMV,
'BJ-XTUROV , A,'B,; BOGATM, V, A.B.; "BOK, 1. 1 .; B0111JU.TYIN, R.R.;
N.L.; BYK&A, 11,S.; ZHILIj'-,SEIY, ZYKOV, D.A., IVAMKIN P.'.-
WAITLI, D.T.-, YAYMV, A.'.~.-, UMMATU , S.K.-, lt~- fi
MIA73N, D.A..; K'USJMV, G.L.; *L.*.'. .', i.'1.; WHAMT, O.Zh.;
rr.TS.; VONICHO V.K.-, MMOTOV, S.: 14115REPOV, G.; 1U12UM'DZ,HA?T1OV, S.M.;
PARSTUIT, A.11.; POFROVSKIY, S.N.; POLOSITKIRITT, A.P.; RUSPKOV, Y.P.;
SEPGIYNV, I.I.G.; SHYPULMIT, S.Sh.-, TAZHI3AY-&V, P.T.; FAM'DIKOV, 7.G.-
,SRLTGI)7. Yo.D.; OCIHI.RRA, G.N.; CHOKIIT, Sh.Gh.; 1.",HOLPi%1rr.-ULOV, T,Ch.
Sixtieth birthday of Academician Yany8h Irnntae7iCh Sabpaev. Vest.
AN Kazach. SS-R 15 no.IL:,58-61 Ap 159 (MIRA 12:7)
(Satpaev, Kanysh Imp-ntae;ich, 1890-)

3(5)
AUTHOR-
TITLE:
-Ivankin P. F.
SOV/20-126-4-41/62
Zonality of the Pyrite Series in the Depositu of the Irtysh
Crumpling Zone in the Altay (Zonallnost' kolchedannogo ryada
mestorozhdeniy Irtyshskoy zony smyatiya na Altaye)
PERIODICAL: Doklady Akademii nauk SSSR, 1959, Vol 126, Nr 4, PP 838 - 840
(USSR)
ABSTRACT: The zone.mentioned in the title - one of the most important
zones in the south-western Altay - contains a large group of
minable sulphide deposits.,They formed in tht Upper Paleozoic
(Ref 2). The aepth of their formation widely varied in differ-
ent parts.of the Irtysh zone, probably from 2-3 to 5-6 km and
more. The deposits are "continuous" (skvoznoy) for all Paleo-
zoic calcareous masses and show no direct genetic relations
with the large intrusions of the Zmeinogorskiy complex. However,.
there exists a close spatial, structural, and chronological re-
lation with the later small intrusions of the plagio-granite-
-porphyrs, albitophyres, and porphyrites (Ref 2). This indicates
a great depth of the deposits of the sulphide-fluorides. As was
shown by the investigations of the author (Ref 2) special struc-
Card 1/3 tural conditions for infiltration metasomatic processes (Ref 2)

Zonality of the Pyrite Series in the Deposits of the SOV/20-126-4-41/62
Irtysh Crumpling Zone in the Altay
existed in the Irtysh zone owing to a combination of perfect
tectonio anisotropies (a plane parallel and a linear one).
Under these conditions the mineralizing solutions flowing up-
wards formed compact rays which entered the zone of schists
in a linear direction. For this reason enormously long (3-4
km) ore deposits of a band type are forined which are also In-
cluded in narrow but very long (7-8 km and more) zones of
rocks changed by the ore contact. The totality of the ore
zon6s may be represented as a column. Transition formations
(Refs 1,30) are found between the most extreme members: cop-
per pyrrhotite and the polymetallic type. Independent of their
position in-the column the sulphide deposits formed in 2 main
stages:. a) in the pre-ore stage a strong metasomatic change
of the containing rocks took place in the range of the band-
-shaped structures. b) in the second stage, the ore stage
proper the solutions, varying in their composition, (2-3
8-tages~ deposited ores of non-ferrous metals and relatively
small amounts of vein minerals. They fill pores, gaps etc.
and form inclusions in ores by crystallizing mainly from the
Card 2/3 solution. The solutions of the pre-ore stage were first gase-
11 IMF i I P ii ~ i~ I

Zonality of the Pyrite Series in the Deposits of the SOV/20-126-4-41/62
Irtysh Crumpling Zone in the Altay
OU8 and diluted-hydrothermal. Sometimes they were strongly
concentrated and sometimes they were capable of injection or
of stripping of rooks. 3 main zones were separated: (from top
to below): 1) the upper zone - with a strong predominance of
the phenomena of deposition over the leaching of bases at low
temperatures; 2) the intermediate zone of acidic leaching at
mainly medium temperatures; 3) the lower zone of the high-
-temperature substitution of lateral rocks by magnesium. There
are 4 Soviet references.
ASSOCIATION: Gorno-metallurgicheskiy nauchno-issledovatellskiy institut
Akademii nauk SSSR g. Ust'-Kamenogorsk (11ining-Metallurgical
Scientific Research Institute of the Academy of Sciences, USSR9
Ust'-Kamenogorsk)
PRESENTED: December 22, 1958, by D. S. Korzhinskiy, Academician
SUBMITTED: December 20, 1958
Card 3/3

IVANKIN, P.F.
Position of the Rudnyy Altai in the system of tectonic zones
of the southwestern Altai, based on geological and geophyei-
cal data. Trudy Alt. GMNII AN Kazakh.SSR 8:10-31 160.
(HIRA 13:7)
(Altai Mountains-Geology, Structural)
-1 flT

ITANKIN, P.F.; VEDERNIKOV, P.G.
Systematics and petrochemistry of igneous complexes in the
southifeste= Altai. Trudy Alt.GMNII AN Kazakh.SSR 8:44-69
16o. (MIRL 13:?)
(Altai Mountains-Rocks, Igneous)

IVAIIKIN, F.F.; TIISHIN, P.V.
Metallogenetic stages and genetic types of the endogenoue
mineralizatJon in the Hud*7 Altai. Trudy Alt.GMII AN
Kazakh.SSR 8:70-83 10- (MIR& 13:7)
(Altai Mountains-Gre deposits)
J

IVANKIN, F.F.; KUZEBM, V.S.; INSHIN, F.Y.
Contact changes as indications in ore prospecting as exempli-
fied by the exploratory work in the Irtyah Valley portion
of the Altai ore region. Trudy Alt.GMNII AN kazakh.SSR 8:
84-93 '60- (MIRA 1317)
(Irtysh Valley--Ore deposits)
(Prospecting)

511 1 1~ I I;I I; 1:
VOROBITEV, Tu.Tu.; IVANKIN, P.L; KUMONYY, V.S.; LIKHODED, R.Ya.
Relationship between the hydrothermal metamorphism and
sulfide mineralization in the Berezovski7-Belousovskly ore
region. Trudy Alt.GMNII AN Kazakb.SSR 8:126-145 160.
OUBA 13:7)
(Altai Mountains-Sulfides)
(Metamorphism(Geology))
,11! -:z i
1TH 11i;;q;! 1 7,~
'IJ

' 1 1 ; 1. 1 . I ~ I ~ I.: I r, 11 ~ I :A.; ; 17 -11 i!:H:- I I, I F [I , , , , , 'i I I I I : I r f , I I I I - ; I
IYANKIN, P.F.; MITRYAYEVA, N.M.; FMINA, Z.A.
T~7pes of ores and stages in the ore formation in the
Novoberezovskoye deposit. Trudy Alt.GMNII-KN Kazakh.SSR
8:146-169 160. (MIJRA 13.' 7)
(Altai Mountains-Sulfides)
ifli tiP
F
i fln F

IVANKINA.P.F.; KUZEBNrY, V.S.
Upper age limit and depth of formation of ore in the Ilikolayevsk
deposit in the Altai. Vest.AN Kazakh.SSR 16 no.1:36-43 Ja
16o. Ow 13-5)
(Altai Mountains-Ore deposits)

GORZHEVSKIY. D.I.; IVANKIN, P.F.
Geotectonio position of the Rudzy7 Altai and Kalba Range based on
geological and geophysical data. Izv. All SSSR. Ser. geol. 25 no,4:
26-40 Ap 160. (MIRA 1311l)
1. LivovBkiy gosudarstvennyy universitet, Gorno-metallurgicheakiy
institut AN KazSSR, g. Ustl-lamenogorsk.
(Altai Mountains--Geology, Structural)

I NI
IVANXIN, P.P.; LIOGENIKIY, S.Ya.
Characteristics of the regional magnetic field in tho RudmyyAltai
and problems relative to mapping it. Geole rud* westOrO2h* no.5:72-
81 S-0 160. (MMA 13110)
1. Veesoyuznyy geologicheaki3r nauchno-issleodvatellsldy institut,
Leningrad.
(Altai Mountains--Ha~etism, Terrestrial--Wps)

IVANKIN., P.F.
Genetic types and stages of sulfide mineralization in Rudny
Altai. Trudy Alt% WII AN Kazakh. SSR. 9:29-49 160.
(MIRA :14: 6)
1. Altayskiy gornometallurgicheakiy nauchno-issledovatel'tskiy
institut All Kazakhskoy SSR.
(Altai Mountains-Sixlfides)
!I]

IVANKIYI, Petr~~~ich, doktor geologo-minor. naukj INSHIN, Pavel
-VIR-torovich; 4UZEBM, Valentin Stepanovicb--POGOZHEV, A.S.P
red.; ALFEROVA, F.F., tekhn. red.
[Ore formations of the Rudnyy Altai] Rudnye formatsii Rudnogo
Altaia. Alma-Atax Izd-vo Akad.nauk Kazakhskoi SSR, 1961. 285 p.,
(MIRA 15:2)
(Altai Mountains-Ore deposits)

ABDULLAYEV, Kh.M.; ALYAVDIN, V.F.; AMIRASLANOV, A.A.; ANIKEYLT, H.F.;
ARAPOV. Yu.A.; BARSANOV, G.P.; BFIUYEVSKIY, N.A.; BOKIY, G.P.;
BORODARVSKAYA, M.B.; GOVOROV, I.N.; GODLEVSK17, M.N.; SHGHEGLOV, A.D.;
SHAKHOV, F.N.; SHILO, N*A,; YA&IOLYUK, V.A.; DRABXIN, I.Ye.;
YEROFEMS B.N.; YERSHOV, A.D.;-,jZAgINL P.JA,; ITSIKSON, M.I,;
KARPOVAY Ye.D.- ; KASHIN, S.A.; KASHKAY,, M.A.1 KORZIIINSKIY., D.S.;
KOSOV't B.M.; KOTLYARy V.N.. XMTER, V.M.; KUZXETSOV, V.A.; LUGOV,
S.F.; MAGAKIYAN, I.G.; MAARIKOV, M.P.; OMRrSOV, 14.14.; FAVLOV, Ye.S.;
SATPAYEV, K.I.; SMIRNOV, V.I.; SOBOLEV, V.S.; SOKOLOV, G.A.; STRAKHOV,
N.M.; TATARINOV, IsMa; KHRUSHCHOV, N.A.; TSAREGRADSKIY, V.A.;
CHUKHROV,F.V.
In memory of Oleg Dmitrievich Levitskii; obiturary. Sov.geols 4
ho*5:156-158 My 161o MU 14:6)
(14vitakii) Oleg Dmi-trievich, 1909-1961)

IVANKIN P. F.
The problem of small intrusion clusters and hydrotherma streams in
pyrite-polymetallic ore fields of the FIudnyy Altai. Dokl.AN SSSR 138
no.4:897-" je 161. (MIRA 140)
1, Altayakiy gorno-metallurgicheakiy institut, AN KazSSR. Predstavleno
akademikom D.S.Korzhinakime
(Altai Mountains-ore deppaits) '(Mataaomatism)

C()mplex me tal deposits -in tho Arl,run Vcillr-y. Trn tl,, Zab,111I no.],.~2-126
162. (MI RA .1812)
fit i2 I!
:TH

IVANKIN. P.F.
Magmatic activity and regularities in the spacial distribution of
copper and complex ore deposits in the RudW Altai. Zakonom. ra=,
Volezn. iskop- 5:190-206 162. (IMIA 15:12)
1. Altayakiy gorno-metallurgichookiy institut AN Kazakhakoy SSR.
(Altai Mountains-Ore depositB)

VOLKOV, V.~L,-VOROB'Wl) yU,y%j~ IVANKIN, P*Fa; STUCHEV-SKIYP N-1-
Experience and methods of large-scale prediction in the BerezovO-
Belousovka ore deposit. Trudy Alt.GMNII AN Kazakh.SSR 12:37-48
t62. (Ajt.ai ~buntains-ore deposits) (IG:RA 15:8)

IVANKRI, F.F.; 14ALYGIN, A.A.
1-bthod of interpretation and systematics of magnetic anomalies
as rervealed by the studies in the Leainogorsk region. Trudy Alt.
GIOUI AN Kazakh.SSR 12:49-55 162. 0-MU 15:8)
(Leninogorsk region (Altai MDuntains)-thgnetic anomalies)

-JIUalU,-~LYUBITSKOY, V.N.
Block structure of the complex metal belt in the southwestern
Altai. So - ~. 5 no.6:77-93 Je 162. (MIRA 15: 11)
1. Vostochno-Kazakhstanskoye geologicheskoye upravleniye.
(Altai Hountains-Ore deposits)

VEDEMIIKOV., P.G.; IVANKIN, P.F.,, doktor geologo-mineralogicheskikh naak;
SHNAYD* i, I'Lb.
Recent data on small intrusions and sulfide mineralization in the
upper Paleozoic coal-bearing stratum of the Rudnyy Altai. V6st.All
Kazakh.SSR 18 no*3:35-42 Mr 162. OUPA 15:3)
(Altai Ibuntains-Ore deposits)

IVA14KRI I P. F.
Origin of miaeralized breecias in some pyrite-type deposits of
the Altai and tne Urals. Dokl. AN SSSR 142 no.2:422-424 Ja
162. (14IRA 15:2)
1. Altayski- jorno-metallurgicheskiy institut AN Kaz.SSR.
Predstavleno akademikom D.S.Korzhinakim.
(Altai Territory-Breccia)
(Ural Mountains-Dreccia)

.VOFQBIYEV,, Yu.Yu.; IVAN&U4_LJF_,, otv. red.; KROTOVA, I.Ye.,
red.izd-va; IYERUSALIMKAYA, Ye., takhn. red,.
(Geologic and genetic-characteristics and zoning Qf the
Irbysh complex metal deposit in the Altai) Geologo-
geneticheskie i zonallnost' irtyshskogo polimetallicheakogo
mestorozhdenita na Altas. Moskva, Gosgeoltekhizdat, 1963.
125 p. (MIRA 16:5)
(Altai Mountains-Ore deposits)

IVANKIN, P.F.
Morphological types of clusters of small intrusives and hydrothermal
jets. Dokl. AN SSSR 149 no-43925-9Z7 Ap 163. (MIRA 16:3)
1. Gorno-metallurgicheskiy nauchno-issled4atellskiy institut AN
KazSSR. Predstavleno akademikom D.S.Korzhinakim.
(Mining geology)

IVANKINY P.F.; INSHIN, P.V.; KUZEBNYY, V.S.
Geneti-c types of quartzites in the Rudnyy Altai.. Trudy Alt.GMNII
All Kazakh.SSR 16-.46-56 163.
(MIRA 17:10)

tl~l:~ III -If! I, I ;
IVOKIN, P.F.; KUZEBIM, V.S.; VEDFJUTIKOV, P.G.
Skarn deposits in the northwestern part of the Fiudnyr Altai.
Trudy Alt.GMNII 91 Kazakh.SSR 16-:81-92 163. (MIRA 17:10)

PANKINY P.F.
Closed explosions accompanying hypabyssal j-ntru,3ions and
their role in the formation of ore deposits. Geol. J
geofiz. no.10:23-33 165. ( MA 18:12)
1. Sibirskiy nauchno-issledovatellskV Institut geologii,
geofiziki i minerallnogo syrIya, Novosibirsk. Submitted
January 7, 1965.

BASALAYEVj, A.A., polkovnik meditainskoy sluzhby; PRIKHODIKO, G.F.,
podpolkovnik meditsinakoy sluzhbyj IVANKIN, P.K., podpolkovnik
meditsinskoy aluzhby
Cases of tonsillitis of adenoviral etiology. Voen.-mod, zhur.
no.2g48-49 165. (KIRA 18:11)

USSR/Electronics Television Receivers MAY 52
Measuring Instruments
"An Oscillaior-Indicator for Tuning Televinion Re-
ceivers," V. Ivankin
"Radio" ko 5s'p 50
The oscillator-indicator described is designed for
tuning the video and sound channels of straight am-
plification TV receivers and also the input circuits
and i-f stages of superhets. The oscillator has a
range of 40-75 Mc and the scale is calibrated in
0.1-Mc steps.
238T84
238T84

. I
I W11 : - - , '. I ! ! , I i
IVANKIN, V.I.. inzhoner.
Phaae motor. Inerpetik 1 no.3:19-20 Ag NUA 6:8) 1
(1lectric moters)

11 HIP
it 43 11 111 q W, 11'1~
Ibb, If
e;*- %-WWA 4, 141~
0 0 0 0 0 111 a 0 a 0 4 a
0 0 0 * 0 0 0 0 0 0 0 0 0 0 00 4 4-0Z
l
s0$& 1 0 110111211 It Ad At It It N III a 4?
I 1111 "IS M11410 fall it
I V I& ' Q 4) 0a

A
T A "T V i v 1. J-1 AA a CC 0 94A.-I -I --f-I
V

00
0

1-90
00 lly"Ois Pcoducts of far
f-w ARLWIS
WV
At. 1
1l
likkov
d V
.
am
.-ALt
y
smeAl (I'. S
) 4 dm
S
R

00 8 .
.
.
(gellinq It"
ShOeth wood suM,
fl; bLd Is lt=Vh "WI
-00
At III,,
title Of 4OU I. ftuy
I ti-mikh CM14isd n; dipstilik- pr(j.
f
i
r
n, conwftcd 11 neg. N Wawt into a po,. one
will

9d .
,
anim
at, a P-W buy rullcm. R. C. A.

oo

00

Nee

At, it A WALLL-P(KAt 1.11flATM CLA$jIIICATIr%

oo
it
ILI t 3 La n1 114

T it N alt it q
V
IS a
L
4
OI 0 0 0 0 0 0 4
0 0
OO
6
000
4 00 0
9

IVANKIN, V. K.
IVAHKIN, V. K.
PYATrMf,[IY PLAN KOLKHOZA RISKRAII NA 1951-1955,
KOLKHOZ "ISKRA" MR 10,51 TO 1955, BY-) P. A. KALIM, 11.
MOSKVA, SELIKHOZGIZ, 1052. 221 P. ILLUS., DIAGRS.,
GODY (THE FIVE-YEAR PLAN OF THE
F. PAZENKOV, V. T. IVANKIN (IDR.)
TABLES.
11/5
783.3
.K1

Name: 1VANKIN, Vasiliy Kirillovich
Dissertation: Metabolism and energy in geese and
basis of the methddof evaluating the
general nutritiousness of fodder for
fowl
Degree: Doe Agr Sci
Affiliation: Zn-ot indicateg7
Defense Date, Place: 19 Jun 56, Council of Leningrad Agr
Inst
Certification Date: 6 Jul
Source: BMVO 18/57

Ydrilloljich,
KARNAUKEOV, Ivan Prokof"yevich, dot--,;,jYAUJ4"t;,.
prof.; VERESOV, Konstantir~ Nikolayevieh, do
Nikolay Vasillyevich, dots.; NIKISHIN, Konstantirt
Goorgiyevich, dots.; LANGE, K.P., kand. nauk, dots.
retsenzent; NFAMULOV, M.P., kand. :5ellkhozz. riziuk, dot1j.,
retsenzent; NOVIKOV, A.A.., kand. sellkhcz. nauk, dots.,
retsen--eTit- "OSULIKO, I.1%, st. prepod., retsenment; SAMONIOVA,
O-G., st. prepod., retsenzent; YEFIMOV, A.L., red.
[Fundamentals of agriculture] Osnody sellskogo khozialstva.
3. perar. izd. Mloskvaj Prosveshchenie, 1965. 6,46 -;.
(MIRA 1~:3)
1. Kuybyshevskiy pedagogicheskiy iii-stitut (for Lange, Merkulov).
2. Orlovskiy pedagogicheskiy institut (for Elovdkov, Nosullko,
Safronova).

I,VgKIN-, _V--.Pp-
Study of holes by the neutron gamma method. Uch.zap. SGU 74:t
311-317 160. (MRA 15:7)
(Oil well logging, Ridiation)

IVANKIN, V.P.
Nonlinear apparattis for radiation logging. Razved.i prom. geofiz.
no.45:3.18-122 162. (III-RA 151l1)
(Oil well logging, Radiation--Equipment and supplies)

IYAMIN, V.-'.
er-Lr, nung ~ha v.---l-ame -0 a w", 'h
prom. geofiz. no.49:13C-i*313 6"') (KrRA 17,-,)

~YANY,11-,, V.P.; t--OL-fGflEVcJKlY, YU.M.
Detemining the nonlinearity of radioactive loggin-g apparatt"n.
Razved. i prom. geofiz. no.50:119-120 163.
(M I RA 38:3)
P. IT
"IF I V

IVANKIII, V.P.
Some problems of the rethuds of the radiometrIc study of wells.
Trudy NVNIIGG rio.1:145-163 164. (MIRA 18:6)

IVANKIN, Ya. I.; K07ALEVSKIT, F.P.; BIDULYA, V.I.; TSUKUR, I.D.
improving the control of apparatus for industrial gammaray
flaw detection. Zav.lab. 23 no.9tll27-1128 '57. (MIRA 10:12)
l.Dnepropetrovski3r zavod metallurgicheakogo oborudovanlya.
(Materials-Testing)

VAlly", t4li r i
AUTHOR: Ivankin, 1a.I., Kovalevskiy, P.P., Bidulyet, V.I-, 32-9-29/4-3
Tsukur, I.D.
TITLEt Perfectioning of the Control of Apparatus for Industzial Gems,
Defectoscopy (Usovershenstnvan.1ye uprav2enlya apparatov d3ya
prcc;yzh2enr_oy ga=a-defektoakop1l)
PMIODICAL: Zavodskaya Laboratoriya, 1957, Vol.23, Nr 9, PP-1127-1i28 (USSR)
ABSTRACT: The aoamtus GUP-CO-5-1 and GUP-Co-50-1, which are being produoea
by the "Moarentgan" plant, have an important 3isadvantage in that
the switchboard for the radioactive source is mounted inmediately
on the unaerstructure of the device near the protective shield of
the preparation. Here a new constraction, in whida the switchboa%rd
is fitted on a separate table, is described. By making use of a
cable of 21 m length, which connects the apparatus with the opera-
tor stand, and of an operating stand of 7 m length, the person
operating controls Is able to work at a dit;tanoe of 28 m from the
source from an open stand, so that full safety is warmnied. There
is I figure
ASSOCIATION: Dnepropetro;sk Plant for Metallurgical Equipment (Daepropetrovskiy
zavod metallurgicheskogo oborudovaniya)
AVAILABLE: Library of Congress
Card 1/1
"~-S --F"Y3

POLUKHIN) P.I.j BERKOVSKIY, V.S.; OSADCHIY, A.N~; STETSMIKO, N,V.~
KIRUNIN, P.M
Oval and edged oval system of roll passes on tandem light
aection mills for rolling high alloy steel. Stall 25
no.4:337-341 Ap 165. (YIRA 18,11)
1. Moskovskiy Institut stali i splavov i Zavod "Dneprospetsstp-11".

17ANKINA, A.T.; MOROZOYA, A.A.
Plotting a detailed frequency section from neutron-gauma log
diagrams. Razved. i prom. geofiz. no. 34:22-28 16o.
(HERA 13:12)
(Saratov Province-oil well'logging,,Radioacti*e)
f
17,17-lug"
7

IVANKIINA, A.T.
Structure of media close to seismic boundaries in the Volga
Valley portion of Saratov Province. Trudy IFIMIGG no.1:120'-129
164.
Determination of the velocity of the distribution of elastic
waves froin the curves of noutron gamma logging. Ibid.:129-131
(MIRA 18:6)

ACC N.R.
AR6033759 SOURCE CODE: 1JR/0081/66/000/018/P014/P014
ATWITHOR: Chesnokov, A. A.; Ivankina, E. B., Brend.!s, V. P.
TITLE: Influence of naphthenes on the deparaffination process of residual
i raffinates
SOURCE: Ref. zh. Khimiya, Part II, Abs. 18P97
REF SOURCE: Tr. Kuybyshevsk. n. -i. in-t neft. prom-sti, vyp. 32, 1965, 86-96
TOPIC TAGS.; hydrocarbon, mineral oil, deparaffination, petroleum product
ABSTRACT: The influence of naphthene hydrocarbons on the deparaffination process
was studied. Residual raffinate (RA) of industrial manufacture (RA density,
0. 883; viscosity, 18. 69 centistoke at 100C) was used as raw material. Naphthene
hydrocarbons (density, 0. 8678-0. 8775; viscosity, 15, 18, 17, 38 centistoke at
100C; viscosity index 110-100) were separated from the RA by adsorption and then
added to the initial RA in the amount of 1 to 207o. The mixtures then deparaffinized.
It is shown that even an insignificant increase in the naphthene content in RA,
increases filtration rate 1. 5 times, while an increase to 10-207o raises the filtra-
Card 112

ACC NR' AR6033759
tion rate 2-2. 5 times. The yield of deparaffinated oil from the potential content in
RA increases by 2%. A clearly visible crystal formation of solid hydrocarbons is
observed during the deparaffination process. The performance indices improve
through the reduction of the concentration of solid hydrocarbons and tars. The
problem of RA deparaffination with the recirculation of deparaffinated oil is then
examined. After the addition of 5 and 7'/'o of oil, the RA filtration rate during
d eparaffi nation increased by 40 and 6316, respectively, The oil yield remained
unchanged. M. Rozhkov. [Translation of abstract] [GC]
SUB CODE: 11/
U fitc

ACC NR% AR6033759 SOURCE CODE: UR/0081/66/000/018/PO14/PO14
AUTHOR:^ Chesnokov, A. A., MiyvA, E B. ; Brendes, V. P.
TITLE: Influence of naphthenes on the deparaffination process of residual
raffinates
SOURCE: Ref. zh. Khimiya, Part II, Abs. JOP97
-9
REF SOURCE: Tr. Kuybyshevsk. n. -i. in-t neft. prom-sti, vyp. 32, 1965, 86 6
TOPIC TAGS.: hydrocarbon, mineral oil, deparaffination, petroleum product
ABSTRACT: The influence of naphthene hydrocarbons on the deparaffination procesi
was studied. Residual raffinate (RA) of industrial manufacture (RA density,
0. 883; viscosity, 18. 69 centistake at 100C) was used as raw material. Naphthene
hydrocarbons (density, 0. 8678-0. 8775; viscosity, 15, 18, 17. 38 centistoke at
100C; viscosity index 110-100) were separated from the RA by adsorption and then
added to the initial RA in the amount of I to 2016. The mixtures then deparaffinized.
It is shown that even an insignificant increase in the naphthene content in RA,
increases filtration rate 1. 5 times, while an increase to 10-20016 raises the filtra-
Card 112

ACC NR:
AR6033759
tion rate 2-2. 5 times. The yield of deparaffinated oil from the potential content in
RA increases by 2%. A clearly visible crystal formation of solid hydrocarbons is
observed during the deparaffination Process. The performance indices improve
through the reduction of the concentration of solid hydrocarbons and tars. The
problem of 'RA deparaffination with the recirculation of deparaffinated oil is then
examined. After the addition of 5 and 70/6 of oil, the RA filtration rate during
deparaffination increased by 40 and 6316, respectively, The oil yield remained
unchanged. M. Rozhkov. (Translation of abstract] (GC]
SUB CODE! 11/
-ICord-2/2-
!;p-

S,.ahilitv of tra-rofDr-m-~,r oil in relation to the nature of Lba crude
111, 19CA, 15-11
7 0 C A,-,.q tran.,,forynier oil. -I'uv-,nazv* ncttroleurn. hydrogenated p0m] curn. Mukhmnavr

Card 1/2
all
l! 7fil
ACCESSIOIN \R: A24),'398,31)
a nd tpo. ,mi-q Chibrikova and '11A.S. Buggro,vu.'ruiya tc-ok pni La 1.1-40
e xpq r i m en tal wo 0 r ig. art.. has: I tabLe.
ASSOtIATIONt KNMf-D-. NovokuyW-shervskly mod. q!o-vol~uylly.
SUBINUTTED: 00 E NI- L: GO SUB COVE: FP
NO REF SOV: 006 OTHIM- 000

cur4
W
M
o.
rp, .
M

F
V
IR

BADYSHTOVA, K.M.; CIIESNOKUT, A.A.; IVANKINA, E.B.j ZFADANOVSXIY, N.B.;
KONYUKHOVA, M.V. Prinimalt-uc-has-tiy-e:"XMOVAIOVO B.S. lnzh.;
NAUMOVA, A.P.,, inzh.; PYATILETOVA, N.I., inzh.; SMIRqOVA, S.14.p
inzh.; CHIBRIKOVA, L.I., laborant; BUGROVSKAIA DI.S., laborant.
Effect of the nature of raw stock on the stability of transformer
oil. Nefteper. i neftakhim. no*lltl5-17 164 (MIRk 18%2)
1. Gbsudarstvennyy nauchno-issledovateliskiy institut neftyanoy
promyshlemosti , Kuybyshev i Novokuyby-shevskiy zavoda
7

L 22483-66 ZiTW/T DJ
A-CC _NRs AP6007929 SOURCE CODE:
AUTHOR: Chesnokov, A. A.; Badyshtova, K. M.; Konyukhova, V.-;Vrafikina
ZhadanovsWIT N
ORG: 0IINP; Novokuybyshev Ar i (N0voXUYby61ievB1dy, nettekhimicheaU,
kombfn_atT_
TITLE: Antioxidative 21ghLIi -.ydrofined transformer oil
of I
SOURCE: Khimiya i tekhnologiya topliv i masel, no. 3, 1966)* 30-32
TOPIC TAGS: transformer oil, petroleum product, petroleum~refiriing, oxidative degra,-,
dation, oxidation
ABSTRACT: The oxidative stability of hydrofined paraffin-f-ree 'transformer. oil bras in-
vestigated using a sample with the following characte'.ristics: kinematic viscosity (in
cSt) at 20OC--24.45, at 50OC--8.01; 0.14 percent precipita ke after oxidation t-"!atment;
flash point in!a: I S
acid number after oxidation (in mg KOH/g)--0.81, c a ed crucible--
1500c; ur point-- -43OC; transparent at +50C; density at'20OC-~-0.88110; refractive
index J103 --1.4980; sulfur content--0.18%. The oil was thromato r . hically 6apaiated
ap
into 6 narrow cuts. Several blends were prepared and thei r characteristic 'indices
were compared with those of the starting transformer oil. , It was found that reduction
in the content of the high molecular weight aromatics results i1i lower antioxidative
UDC: 665.521.54
Card 1/2

Mil;mi Hirledi ift 'mPimmu.&Mmil
17777!12-1 "HOPMR-mv
4nXly-ja of tile

F
F
h
d 45tsidin XUA
fli
V
l
,
ti.
.
!
y 2ix
a
ii.
and L. L. lirjoikinfl
- T7Vr-Y---

T-
r -
-
MMM
~ . C1,1141
-N 1.

P
A
Zh

ki
-
J)
So ~i
, _7
F ur.,
fern 1.
J
v6curilty, 4urface tcmiimi, and s wal: ituditft ~Vr
the sty~au- it fllir,-11,11. 'rite. (i. (at jo and 50") Lv3dialivi
wcre curN'C,, b,-ut tuA-ard die ccAnpu. &xis witich fi-dic4itmi,
roptaw (iiIA&Ln
runtri;ctiuain tht syst,!m. Dcviaflaa of kbe
r1
from additive itrAlibi tilw-. W-L., Calcd. ;as %ve Hit (Ict,imlims
uf the surfaec,tviiiion curvcs froin thz Stakhon-tif adiflOve
curvg. In itil ca-w, it tviiaspondt-d to it compa. (if 75 triull, %
IMI. Thud, nit voissitimmicin jr itfimpe of d., v1woAty, 1jus-
. it i
volicilidt"I tivit: tilt: vinj
ml
r
1l
k
d
.
s
imil.
"
o
um lvn~wn, an
l
Iq (C.1.11cd

SOY/ 112-58-2- 1854
T r a n ~,i I orn: RefferativIzIly zhIzx:r;II, Elektrntekhn~Ra, 1958, tT:r 2, p 9 (USSR)
AUTH0P.-,.-1.v,3.--hi,;, IA- Gorodetskiy, A. F.
TITLE: Electri.C, Strezgth of NaCl-KCI System Solid Soli-AiDns
,'EjI.e!kt.,,_ichesIr.aya procYmicstl tyerdykh. lastwirov sistermy NaCl-KCI)
PERIOMCAL: T7,-v-. Tomskago politek!%a. i~,_,.-ta, 1956, Yol 91, pp 159-164
A.BSTRAC,-: Electric strength and -microl-a-rd-ness of P-;-.r,,gle czy-Btals cf NaCI-KC1
)17-*141,wi~s Live been. measured. Effect of compo iti r on electric strength
is represer-fted by a curve that has a rrumiT.111-Mm. and effect on the microhardness
-:.. Cm:-.:rve t~-_at has a ma,)dTn,= in t'he regi,-n. of equal co:!.te:,As of the compa-
E_Iectzic etreagth valtues are co~ pa7,ad with the vkl,!.es of formation
e -J ~, TX_T
si:z!ace emergy. Ar.. InfeZence is th-at electric strength do-
c7 eaAe~~: -vi 11-e decrease -*n system durabidity. Bib'13g:tap'~-; 12 ite ms.
pr__",_,tek_I~_n.:_,h. ia-t (Tomsk Polytec~.:i;c Tarnsk.
A. A. V.
Ca ~~! 1 1
.7
11'
7

ILVANIONA) M.S.
Ivankina, M.S. (Tomskiy politueklinichesUy institut (Toinsk, Polytechnical
institute)] Measuring the 11pat of Foruntion in KCI-KBr- a-,,.d KC.L-1'14`.1C1 Solid
Solution3
(1%-~ Ptlys I c a ~--f
of -~A
,--,Cea

IV 6 AIX I Of) I P/', , 5 -
AUTHOR: Kuchin, V. D., Candidate of Technical 30 V11 a 5- 56- 7-25/32
Sciences
TITLE: Conference on Solid Dielectrics and Semiconductors (Konforentsiya
po tverdym dielektrikain i poluprovodnikam)
PERIODICAL: Elektrichestvo, 1958, Nr 7,, PP- 85 - 86 (USSR)
ABSTRACT: The conference took place from February 3rd to Pebruary ath
~, in the Tomsk Polytechnical Institute-(Tdh~6ki
-jJ5 :Ly politekhni-
cheskiy institut), Section of Properties of Dielectrics.
Professor A.A.Voroblyev (TPI) reported on the great number of
investi-pa-tions in the theory of ionic dielectriesq of cystalli-
zation, of the mechanical and electric properties of dielectrics
and practical insulation. He shovied that the properties of the
binary compounds --re divided into two jE~roups: the one group of
properties increases with increasing lattice energy, the other
is roduced~ Docent 11,3.11.letsik, Irkutsk University (Irkutskiy
universitet) developed a theory according to which tho cleavage-
-work in mica crystals is composed of the worh P-6~~inst the dipole
forces and the work for the separation o--:' the double layer and
in the last ota~,-e results in an electrostatic mosaic. Docent N.I.
Voroblyev (TH) rc~)oAed on tho roakilto of the invectigation of
Card 1/4 ki

Conference on Solid Dielectrics and Senicor:dzictors 3011/105-5Z-7-25/32
dielectric constant, of the losses, the electric ntrength, and the
specific volume resistarce under temperature influence, moisture,
tropical conditions, in the corona products "fluoroplast-,l.",
"fluoroplast-Y', polyethylene, polymonochlorostyrone, "product-loll,
thernoreactive compounds, arid urethane, (TPI)
measured the factor of linear expancion and the heat produced
in the formation of solid solutions of the KC).- RbC1, M - KBr -
-arid NaCl - ITaBr system in dependence on the com-po3ition in the
ran!,e of from 25 to 1000 C. A. 11 Kislina (TPI) found that the
simple relations between the physical and chemical propertien
of the monocryotals of alkali-halide salts and their electrical
strenZth (as described previously in the papers of A.A.Voroblyev)l
are not always established in the case of solid solutions. Docent
P.A.Savintsev and others (TPI) found that the stren,-,th of alkali-
-haliTe solutions ~etcriained according, to the method of boring
and mutual grinding increases Yfith increasing molecular concentra-
tion its change accordina to its composition following a curve
with a minLitim. Docent V.V.Puelik-ovikilr,Cli(~lyal)insk Institute
of Mec"Anization and Ble ctri:Eicat ion of Agriculture (Clelyabinskiy
inatitut mekhanizatsii i elektrifikat3ii sell.sko,,I-o khozyaystva)
Card 2/4 by meano of experiziento found th,it the dependence of the maximum

Ccnforence on Solid Dielectrics and Semiconductors SOl,'105-58-7-25/32
overheating temperature in the center of the small plate on the
temperature of the surrounding air has maxima in the case of a
change of this temperature of from 2o - looo C.
Section of Ceramics: V.M.Belousov (TPI) 1;,-~Lye it calculation of the
ceramic structure. Docent'V.A.Presnov and other3 (SFTI) reported
on investi.-ations of the vacuum-tight ceramic structure and the
nature of the ceramic-metal boundary.
Section of Crystallization:Professor A.U. Kuztmin and assistants
(TPI) dealt with geological problems. S.A_.Stroitelev (TPI) cave
a method for the selection of effective admixtures. A.P.Iz-ergin
developed a method and an equipment for the purification of li-
quids from small admixture quantities.
In the joint session of the sections concerned with the break-
down of solid dielectrics, ceramics, polarization, losses, and
conductivity Professor N.I.Shishkin spoke about the "Electric
Conductivity of Solidified GI-asses". The final general meeting
was opened by Ye.G.Papush (Dnie-propetrovsk Inntitute of Railway
Traffic Engineers) *~Wh-o reported on the "Foundations of 'ilia Theory
of Polarons".I. Ye.Balygin and A.P.Rumyantsev reported on the
card 3/4 investigation of ~he diusuaion proceii&s of the silver isotope
Z Z:, .,4f - J! :; :

Conference on Solid Dielectrics and Semiconductors jOV/105-56-7-25/32
4.
Ag 110 in amorphous and crystalline quartz, and in agglomerated
oxides as Al2031 ZrO2 and TiO 2*
ISSOCIATION: Tomskiy politekhnicheskiy inatitut (Tomsk Polytechnical Institute)
1. Dielectrics--USSR 2. Semiconductors--USSR 3. Conferences
Card 4/4
114

IVANKINA, H.S.
Crystalline lattice structure of alkali metal halides in solid
solutions. Izv. vys. ucheb,zav.; Fiz. no.1:101-105 158. (MIRA 11:6)
1,Tomskiy politekhnichaskiy institut imeni S.M. Kirova.
(Alkali halide crystals) (Solutions, Solid)

IVAUKRIA, M.S.
Effect of the composition on hoat of formation of alkali halide
solid solutions. Izv. vys. ucheb. zav.; fit. no-3:165-107 158.
(MrRA 11:9)
1. Tomskiy politakhnicheakly institut Imeni S.M. Kirova.
(Alkali halide crystals) (Solutions, Solid) (Heallu- of formation)

AUTHOR: Dranldna, L.S.
TITLL,;: Dependence of -Ehe Idnear E.-qp-ars-,-,n Cceffi-.-~ieot 01'
Solid Solutions of Alkali and Hal-id4.- SaItS, [)'I Unelr
Compositiou 'Zair.S4rGS-1-1 lfeaffitsiyoxita ':LN-,j-r-oi30
rasshireniya tvei:oJJyv1mch ras-~,,.rorov
soley ot sostk-.a,ia)
PERIODICAL: Iz-.,restiya Vysshikh, Ticliebuyk-h Za-7edervi.--, Pizika,
17._ 5-- 9
1958, lir G~ Pp -51, 5
ABSTRACT; The paper was presented. at tha Gonferer.-,e cf
Educational Bstabl---;~3iiments on axid Si.:.,,Mj..-
conductors, held Ln Tomsk an Februa.-cy 1958~ Depandezace
of the iinear ex-pansion c,Doffi-,i,~nt- c.'L 1-1he solit,i
- KCI-KEr and