SCIENTIFIC ABSTRACT ZHUKOV, G.V. - ZHUKOV, I.V.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R002064920012-5
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: September 19, 2001
• Sequence Number: 12
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

BELEVTSEV, Ya.N. - FOWNKO, V.Yu.; NOTAROV, V.D.)- MOLYAVKOp GI.;
HELINIK, Yu.P,; SIROSHTAN, R.I.; DOVGANI, M.N.; CHERNOVSKIY,
M.I.1 SHCHERBAKOVA, K.F.; ZAGORUYKO, L.G.; GORWOHNIKOVO B.I.;
AKIMNKO j N, M, I SMRGMVA I To. A. I XUCHERp V. N. I TAKHTUYEVt 0. V.
XALYAYEV, G.I.; ZAMJBA) VA; NAZAROV, P.P.; MAKSIMOVICH, V.L.;
STRUYEVAq G.M.; KARSHEMBAUM, A.P.j SKARZHIUSKAYA, T.A.;
CBEREDNICHOKO, A.I.; GZRSHOYG, Yu.G.1 PITADE, A.A.; RADUTSKAYA.'
P.D.; ZHILKIN5KIY, KAZO, V.M.; KACHANp V.G.; POLOVKO,N.I.,
red.; LADLUVA, V.D., red.; ZHUKOV G V red.; YEPATKO, Yu.M.,
red.; SLENZAXO.I., red. izd-va,- KULICHENKO, V.G., red.;
RAKHLINA, N.P., takhn. red.; MATVEYCHUK, A.A., tekhn. red.
[Geology of the Krivoy Rog iron ore deposits) Geologiia Krivo-
rozhakikh zhelezorudnykb mestorozhdenii. Kiev, Izd-vo Akad. nauk
USSR. Vol,l,,[Goneral problems of the geology of the Krivoy Rog
Baain. Geology and iron ores of the "Ingulets," R&Wumovskiy,
and Illich ore'deposits) Obshchie voprosy geologii Krivbassa.
Geologicheskoe stroenie i zheleznye rudy mertorozhdenii rudaikov
"Ingulets," Rakhmanov3kogo i im. Illicba. 1962. 479 p.161.2.(Ge-
ology and iron ores of the Dzerzhinskiy, Kirov, Liebknecht, Ootober
Revolution, "Bollshevik, " Frunze, 22d Partslezd, Red Guard, and
Lenin deposits]Geologicheskoe stroenie i zheleznye rudy mestorozhdonii
im. Derzhinskogo, im.Kirova, lm.K.Linkankhta, im.XX parts"ezda, im.
Krasnoi Gvardii i Im Lenina. 1962. 564 P. (Mila 16;5)
(Kriv;y Rog Basin-Iron ores)

BELEVTSEV, U.N.; FOM[EN1(O,.'V.Yu.; NOTARCV, V.D.; MOLYAVK0pG.I.;MEL1NIKp
Yu.P.; SIROSHTANq;R.L;/DOVGAN'., M.N.; CHERNOVSKIY M.I.;
SHCHERBAKOVAP K.F.; ZA0ORUYKO0 LfG.;.GOROSHNIKOV,$.I.;
AKIMENKOt N.M.; SEMETEYEVA~ Ye.A.;..KUCEER, V.N.; TAKHTUYEV,
G.V.; KALYAYEV, G.I.; ZARUBA, VA; NAZAROV, P,P.; MAKSIMOVICH,
V.L.; STRUYEVA) G.M.; KARSHENBAUM, A.P.j SKARZHINSKAYA, T.A.1
CHEREDNICHENKOv A.I.; GERSHOYGI Yu.G.; PITADEO A.A.; RADUTSKAYA,
P.D.; ZHILKINSKIY,'S.-I.; KAZAK, V.M.; KACHAN, V.G.; STRYGIN,
A.I., red.; LADIYEVA, V,,D, red.; ZHUKOV, G.V., red.; YEPATKO,
YU.M., red.; SHCHERBAKOV IAD., red.; 9=W, 0.1., red.izd-va;
RAKHLINAp N.P., tbkhn, red.
(Geology of Krivoy Rog iron-ore-deposits]Geologiia Nrivorozhskikh
zhelezorudnykh mestorozhdenii. Kiev,.Izd-vo Akad. nauk USSR.
VoLL(General problems in the geology of the Krivoy Rog Basin.
Geology and iron ores,of the deposits of the "Ingulets,"
Rakhmanovo, and Illich Mines]Obshchie voprosy geologii Krivbaasa.
Geologicheskoe stroenie i zheleznye rudy mestorozhdenii rwWkov
"Ingtdets," Rakhmanovskogo i im.nficha. 1962. 479 p.
(Krivoy fOg Basin-Mining geolop) (MIRA 16:3)
(Krivby Rog Basin--Iron ores)

71 Grigor4 Vasillyevich; USACHEVAI I.G.p red,; TRUKHMIA, O*Nop
telcbn,red,
[Paratyphoid in young farm animal I Paratif molodniaka, Hoakva)
Goafizd-vo iselikhozolit-up 1961, 135 p. (KMA 3.4 t 6)
(Paratyphoid fe-ver)
(Vatertutry medicine)
... .. .....

Z1fUK0Vj G.V.j Doe Vet Sci - (diss) "Paratyphoid of ibe
~~"e and calves." Loss 1959, 25 pp (All-Union
Inst of Fzcperimental Vet Sci. All-Union Order of Lenin Acad
Of Agr1ci im V.I. Lenin) 140 copies M, 33-59) 120)

Munw, Ta.116 (Bialteyteevo U.N.]; Z=07' O.V. Nhukov, H.VJ
Second scientific conference on problems of geology and the
origin of Iron-silicon formations in the Ukraine, Oeol,xhur,
18 no.4:123-125 158, (HIRA 12:1)
Mwaine-aeO1097)

S;KEIEWO, Rikolay Panteleymonovich; FCLOVXO, Nataliya Ivanovna; GRITSKOV,
Takov Hikhaylovich; MROXHOTOT, Mikhail Nikolayevich;,MAXEBMINA,
An~a Alskeandruna; LADITVA, Vlktorlya Daulloyne;
--Viktorovich; HASTMO ' Andrey Andreyevich; RODIONOT, S.F., otvoredo;
Uft Y.N., red.izd-va; IIOZMITBVBYG, Ye.N., tekhn.red.
(Geology of farroviliceous formations in the Mcraine] Geologiia
sholesisto-L-remnistykh formateii Ukrainy. Kiev, Izd-vo Akadonauk
USSR', 19~96 697 p, (MIRA 12:3)
l..Chlen-korrespondent_AH USSI (for Rodionov).
(Ukraine-7arrosilicon)

-3-461
?O-JA9
tat
01.
Ito -qo% 'JICTS,
0 Lve tail 1:10,
ija*A:, A191
tyle OT 'gol -
A9551
ati.0%, O~ the t,~te-
j.St ~ 555VL t to.
eles viswf. "tomea- ove
aAi. .1186 . O'A 4- 6
~S&e fge OTC~ a Us
vou-'s-l", Of the 101 toss 9 he 131CTS, m, h eT e
50- T oov's 00,j.~All of t C-91C * TOO
CSAIOT-~G te& qjt& the part the vil SqV
evresell is & III T&OTS ieotelte& -V the
'the TtSlte e it, b 0 T e. OT , a09, a ~TL 6.0
ti.t"e 6eve" ~Ov 1010-0 j.Gh a 'V -ItS al
Oaei! I -% -'r "YL The
'060 a ti_oOlerrxo
ho-rost T e %0~ saif Q I %oue ti.O'A jors t e
S, 0 - &~-r c 0
Thel ille T-~ela ioae& t at eT
I s IAOILt I 1. 6-
tal In 1.6jolts-1 eU
OTIS for,% a Mel: of at 0 05 e
they VASiA.4 ev, joeva-do a th
1.1 ,e~, -L the q , n t 6c) ob 0-,e
a . -r-t - V. oll 0, To. I es 'J~
k. OTS
6t
OSV
%ell 0
000% r4
aT )&6
,t a]: 7,01-
~~061
I I t 0 'ph e Ta
ves
PST
T&

On a New Development Area of Perruginmo Siliceouo 2o-119-3-48/65
Formations in the Ukraine
which lies much further in the north. Howeverithese are
not the boundaries of the distribution area of the rocks
mentioneds still farther eastward already in the central
part of the Priazovskiy crystalline massif, single out-
crops of magnetite silicate-hornaton-a are known. Ilready
after 1945 a series of magnetic anomalies was found between
the river Kiltiohiya (left tributary of the Obitoohnaya,
river) and the meridian which passes somewhat in the east
of the town of Zhdano*. In the years 1951-1952 some of
these anomalies were struck. On this occasion hornblende-
magnetite-quartz-hornstones were extracted. Besides amm
phibole also diopside was partly contained. The individual
beds of the ferriferous hornstones show a thickness of 2o m.
They form an alternation of beds with biotite - plagioclase
gneisses and mainly with basic and ultra-basio rocks; am-
phibolites, tremolitites and aerpentinites to which they
are quantitatively subordinated. The ferriferous rocks of
the central Priazov'ye doe not differ at all from the
Card 2/4 analogous rocks of the mentioned districts of the UCM

On a New Development Area of Perrugilams Siliceoua 2o-119-3-48/65
Formations in the Ukrain
according to their structure, texture and mineralogical
composition; like the latter they are well metamorphized
formations of sedimentation from the genetical point of
view. According th the character of the magnetic fields
the struck places do not form an exception. Without any
doubt ferriferous rocks are contained at different
amounts also in other anomalies. Thereforet it can be
assumed'that between the Ziltiohiya river and the town
of Zhdanov a whole area of distribution of this specific
complex of rooks of the ferriferous ailiceous formation
is situated.1t deserved special attention because of its
isolation and also a special names Central Priazovskiy.
From the structural point of view this district forms a
complicated folded zone stretching north-north-west. Its
peoularity consists in the fact that here metabasites
play a leading r*o^le in the ferriferous siliceous formation.
A similarity with the districta Orekhovo-Pavlogradpkiy
ZDWriklyand Verkhovstevskiy in,this respect could not be
Card 3/4 found. A strong difference can be observed with the

On a New Development Area of FerrugJnous 2o-119-3-48/65
-Siliceous Formations in the Ukrain:-1
Saksaganskaya series (Krivoy Rog) and with the deposits,
of the West Priazov'ye where no alternation of beds with
the magnetic formations but with schist and para-gneisses
ooours. The mentioned similarity probably indicates the
same age of the corresponding masses.
There are 2 referonces, both of which are Soviet.
ASSOCIATION: Institut geologicheakikh nauk Akademii nauk USSR
(Institute of .eological Sciences AS Ukrainian SSR)
PRESENTEDs November 16t 1957, by N. M. Strakhov, Member; Academy
of Sciences, USSR
SUBMITTED: November 14, 1957
AVAILABLEs Library of Congress
Card 4/4

SEMIMNKO, M.P. CSemenenko, N.P.3; ZIRIKOV. G.V. CZhukov, H.v.]
The Fetrovo graphite-bearing series* Geol, zhur. 17 no-3:48-57
'57. (MIRA 11:2)
(Kirovograd Province--Graphite ores)

ZHUOT, G.V. [Zhukov, H.V.1; HASTRIM0, A.A.
Stratigraph7 of the Iron-ore aeries of the Oulyay-.Pole mangetic
anomaly (with oil y in English]. Dop. All URSR no.1:66-68 158.
(MIRA 11:5)
141notitut goologichnikh nauk AN 1JRSR. Prodstavleno akademikom
AN USSR N.P. Semenenko.
(Gulyay-Pole-Geology, Stratigraphic)
IMIN
Mv

Hu k'OV
YSSWCultivatal Plants - Grains 14-4
Abs Jour Ref Zhur - Blolaj, No 11 1958p No 3,510
Author F*Sv B=toveya, S.V. VO-V-ttoanko, P.V, Zhukov, A.I. Milovzor.)~.
F.A. Mironchenko, D.D. Mishustin..-Ta-m-.-Misirullin
Inst Not Given
Title Experiments with Corn
OrIg Pub 5b, nauchn.-isaled. rabot. Azovo-Chernomor., a.-kh. in--t,
1956s. 14j, 5-18
Abstract In 1955 there was a study of methods of harvesting corn in the
Hostovskaya and Kamenskaya Oblastao Pxeliminary results of
the tests while working the noll according to the ~Wlltsev
method have shown an incraase In the yield of cobs to 15
centners per hectare. The favorable effect of beeding the
prop roots, of VIR-42 corn with solutions of urea (1%( and of
ammonita aultate (1%) (plemt feeding Inprovedp ripening was
comsiderably accelerayed and the y1eld Increased). 1h8 P-rop
root supplemental of feeding Pc (1 : 10) cauBed some scorching
of the corn leaves. Treating the seeds with microelaments ard
concentrations of W04 0-041 ZnS04 0-04% bag easo incr.-iased
Card 1/2

zMOV G v
A now area of forrugineous-siliceous formations in the Ukraine.
Dokl. AN SSSR 119 no.3:563-564 Mr 158, (MIRA llt6)
l,lustitut goologicheakikh nauk AN USSR, Predstavleno akoAamikom
N.K' Strakhovyme
(Ukraine--Iron ores)

ZHTJKOV, GeV* [7,hUkOVo HPV*J
Genesis of the rich magnetite ores of the Koreak-Hogl;a di;poldts
(with summary in English). Dop. AN LM. no.4:380-302 '57.
(HIRA 11:3)
I.Institut geologichnikh nauk AN IURSR. Predstaylano akadomikom AN
'URM N,P. Semenanko.
(Azov Sea region-Magnetite)

AUTHORSt
TITLE:
Zhuk-ov, G V. (H.V. and Nastenko, A. A. 21-1-15/26
Stratigraphy of the Ironstone Series of the Gulyay-Pole Mag-
netic Anomaly (Stratigrafiya zhelezorudnoy serii Gulyay-
Pol'skoy magnitnoy anomalii)
PERIODICAL: Dopovidi Akademii Nauk Ukrainslkoi RSR, 1958, ff 1, pp 66-68
(USSR)
ABSTRACT: As a result of explorations carried out in 1930 by the
Ukrainian Geophysical Trust in the Zaporozhlye region, a
magnetic anomaly was detected near the railroad station
Gulyay-Pole. Prospecting drilling conducted by the Ukrainian
Geologic Administration in 1953-1954, es 'tablished that the
anomaly was caused by ferruginous hornstones overlaid by the
Cenozoic deposits at depths from 90 to 135 m between the
migmatites and genisses of the crystalline foundation. To-
gether with underlying and penetrating rocks, these formations
form a peculiar series which the author proposes to name the
Gulyay-Pole ironstone series.
The Gulyay-Pole series is divided into 3 suites. The
lower suite is compoaed of staurolite-diethene-biotite-
muscovite shists; the middle suite is represented by quartz-
-Card 1/2 magnetite hornstones with streaks of biotite shists, and the

21-1-15/26
Stratigraphy of the Ironstone Series of the Gulyay-Pole Magnetic Anomaly
upper suite is made of quartz-biotite-muscovite shists and
arcooic sandstones. The total thickness of the entire series
equals about 800 m.
In its atratigraphic position, the Gulyay-Pole series is
apparently,an analogue of the Yrivoy Rog series. Its ab-
solute age, determined by the argon method, in 1,720 million
years.
ASSOCIATION: Institute of Geological Sciences (Instytut heolohichnykh nauk AS
UHSR) of the Ukrainian Academy of Sciences
PRESENTEDt By Academician of the Ukrainian Academy of Sciences N.P.
Semenenko (Ukrainian spelling: M.P.)
SUBMITTED: 5 April 1957
AVAILABLEt Library of Congress
Card 2/2 1. Geology 2. Magnetite

V -2-
SSMININKO, Hikolay Panteloymonovich; POLOVKOp Ilatallys Ivanovna;
ZHUXOV. Geo- h; tADITXVA, Viktorlya Danilovaa;
Anna Alaksandrovae; ZAVIRTUXHINA, Y.N.,redaktor
izdatellsiva; RODIOffOT,.-'S.P-.,otvetelVenny~ redaktor; ROZENTSVITG,
Ye.N.,tekhredaktof~
[Pqtrography of ferrosilicate formations of the Ukraine]
Petrograftia zhelazietokremnintykh formateii Ukrainakoi SSR. Kiev,
lzd-vo Akad. nauk USSR, 1956. 535 P. (MLRA 10:4)
1. Chlea-korrespondent AN USSR. (for Rodionov)
(UkraiAe--P6trology)

Carbonaceous rocks and grapbites from the iron or@ system of
the veslvjrn Azov Sea region. Dop. AN URSR no-5-465-466 156,
I.-Inatitut goologichaskikh nauk Akademli usuk URSR.
Pradstavleno akademikom Akademit nauk USSR N.P. Semenanko.
(Azov Sea regiou--Iron ores)

F'J'.
ZHMV,, G.V.
low data on the stratigrapby of the iron ore series of the
western Azov region. Izv.AN SSSR Ser.geol,; 21 no.94.101-104
S 156. (WRA 9:11)
L Institut goologicbeskikh nauk Akademii nauk USSR, Kiyev.
(Azov region--Iron ores)
.~i till
A 1 111 11
mftm
0X4:Mtj3_FIVi;l1M1t.;1 IWI LI fill] I u I It lift NNE11 .0 11~111. il. MHAESM"

,-ZIAUKOV, 6-i-V
AUTHORt Zhukov, H.V. (In Russian G.V.) 22-4-15/24
TITLEt On the Genesis of Rich Magnetite Ores of the Xoreak-gogila
Deposits.(Pro henezys bahatykh mahnetytovykh rud rodovyishcha.
Xorsak-Moh-yly)
PERIODICALt Dopovidi Akadsmii Sauk Ukrainalkoi RBR, 1957t #41 pp 380-382
(USSR)
ABSTRACTt In the western Azov Sea area, the Kormak-Mogila deposits con-
tain rich magnetite ores among hyperstfienic-magnotits quartzi-
tes of Precambrian age,
The quartzites are sedimentary metamorphosed rocks. The rich
ores are skarn formations created in the iron quartzites as a
result of the action of microoline granite intrusion.
Two references are citedg both Slavic.
INSTITUTIONt Institute of Geological Sciences of the Ukrainian Academy of
Sciences.
PRESENTED BYsSemenenkogNsP., Member of the Ukrainian Academy of Sciences.
SUBMITTEDs 20 December 1956
AVAILABLEt At the Library of Congress

ZHUXOV, G.V.; POLOVXD, Me
MOMIMW
Stratigraphic nomenclature and divisions of the metamorphic
complex in the Krivoy Rog,iron ore basin. ftul.MOIP-Otd.geol.
32 no.1:93-97 J&-F 157. (MLRA 10:5)
(Krivoy Rog--Geologr, Stratigraphio)

AYZEM,RG, D.Ye.:, geolog; BALUKIMVSKIY, N.Y., goolog; BARTIOSuffSKIY. T.I.,
goolog; BASS, Yu.B., goolog; VADIWV, H.T., gaolog; GLADKIT, V.Ya.,
geolog; DIDKOVSKIY, V.Ya., goolog; YERSHOV, V.A., geo1og;-Z'M--MOT-j-
,.G.V. goolog; ZAIDRIY, PIK., geolog; IVANTISHIN, M.N., geolog;
KAPTjdM,tW-CHL'R1?OUSOVA, O.K., geolog; KLIM811KO, V.Ya., goolog;
KtU~AIN. V.L. gaolog; KLYUSHNIKOV, M.N., goolog; KRASHOMMAKOVA.
O.V., 9'eolog; KUTSYBA, A.M., geolog; LAPCaIX, Me.. goolog:
LICELkK, I.L., geolog; MAKUF-q1H&, A.A., geolog; HkTVITE11KO, Ta.M.,
goolog; MKIMIA. V.S., geolog; MLYAVKO, G.I., goolog; NkYDIV,
D.P,, gmolog; NOVIK, Ye.O., geolog: POWVKO, I.K., geolog; RODIONOV,
SIP., geolog; SEIAMONKO, NIP., akademik, geolog; SHRGRIW, A.D..
geolog; SIROSHTAN, R.I., geolog; SLAVIN, V.I., gaolog: SUKHARIVICH,
PIP., goolng; TKACHUK, L.G., goolog; USHHKO. I.5., geolog; USTI-
NOVSKIT, Tu.B.; geolo*g; TSAROVSKIT, I.D.. gmolog; SHULIGA. P.L.,
geolog; TURK, Tu.Yu., geolog; TAM11ICHZNXO, I.M., geolog; ANTWPOV,
P.Ta., glavny7 redaktor; FILIPPOVA, B.S., red. izd-va; GUROVA,
O.A., tekht.red.
[Genlogy of the U.S.S.R.] Geologita SSSR. Glav. red. P.IA.Antropov,
761.5.[Ukrainian S.S.R., Moldavian S.S.R.1 ... Ukrainskaia SSR,
Moldavaknia SSR. Red. V.A. grabov, N.P. Semenenko. Pt.l.LGeological
description of the platform area] Goologichenkoo opisania platfor-
mennoi chasti. Ybakva, Gos. nauchno-tmkhn.izd-vo lit-ry po geol. i
okhrane nedr. 1958. 1000 p. Supplonent] Frilozheniia.
-7continued on next card)

AYZEMRG, D.Y~.---(contInumd) Card 2.
3 fold.maps' (in portfolio) 04IRA 12:1)
1. Russia (1923- U.S.S.R.) Glavnoye upravleniye geologii i
okhrany nedr. 2. Ukrainskoye genlogichatikoys, upravlentya'
MinIsterstva geologii i okhrany near SSSR i Inatitut geologicbeakikh
nauk Akademii nauk USSR (for all except Antropov, Filippova, Gurova).
3.Glavnyy geolog Ukrainskogo geologichaskovo upravlaniya (for Tershov).
4. AN Ukrainekoy SSR (for Semenenko).
(Ukraine--Geology) (*ldavta--Geology)

M Viii
EWT(
W(t
I ACC NA, AP6013070 SOURCE Cam. UR/0048/66/030/004/0637/(1643
AUTHOR: Bundel',A.A.; V10hnyskQV&A.V fiAA_a1q _Ianov -S-A. ; q~Lr_eLt#_k_M_aR- I Zhukov,Q-
Namenskaya,S.A.; Kreytoor,X.A.; OranovsksiyaT.Y.; ChashchinN.A.
OPJG'. None
TITLE: On the effect of the preparation conditions on the formation of traps in ZnS
and ZnO base phosphors and the inflUetwo of rludooomposition phenomena in nolid soolu-
tioms ot cuso in ZnS on their lumint /Report, Fourteonth Conference on Lmlaoa-
conce lt~irx Riga,16-23 September 19657
SOUROH: AN SSSR. Izvestiya. Seriya fizicheskaya, v. 30, no. 4, 1966, 637-643
TOPIC TAGS: luminescence, crystal phosphor, zinc sulf Ide, current carrier, "O~'O'
ABSTRACT: Introduction of new experimental methods has increased rather than =Iuced
Vulf We':
the disagreement among different investigators regarding the structure of_Aig~,k
luminaphors. On the basis of previous Investigations of glow curves and the poliarlty
of the photocurrent carriers the authorn showed that for the most part the discrapan-
cies are due to inadequate control of the synthesis conditions , i.e. , that the phoo-
phors studied by different groups differed as regards structuro owing to uninten.-
tional variations of the proparatlon conditions. Experiments iihow, for example, that
truly self-activated ZnS exhibits only one glow curve ponk, but that if the conpound

-NRi 1:-AP6013070
is exposed to rxygen, even at low pressure, during heating a second glow-curve peak
appears and this 18 accompanied by change in the polarity of the photacurrent carriers,
(from n to p). Various experiments were carried out with pure, self-activated ami
impurity-activated ZnS aiA ZnO (including surface oxidized apecizens) and several
series of glow curves are reproduced. Da-ta on the polarity of the current carriers in
photoconductivity are also adduced. The ourves and data demonstrate the effects of
the synthesis conditions. A series of phosphors was prepared by heating differ-out
S without flux at 10009c, f-.11oed by reheating with quartz
mixtures of ZnS with Cu
2
ipowder (to prevent CakIng) In sealed tubes at 10500. These ZnS:Cu phosphors were
stiAied immediately alter preparation, after various heat treatments and after storage '.
for some months at 200. Their attributes differed considerably. again indicating the I
iimportance of synthesis and other conditions. It is pointed out that understanding of .
the peculiarities of the complicated chemical system constituted by copper-aotivated
zimc sulfide luminophors requires further thorough investigation of the ZnS-%S-Cu
system. Orig. art. has: 1 formula and 6 figures.
SUB CODE: 20/ SUBAI DATE: 00/ ORIG REP: 008/ OTH FW-. 008

Crd 2/2 OU

AMMTSW7, A.M.; Z!~gOVG.Y..,--DRIGORYEV, B.F.,- MAKSIMOV, I.S., red.;
GERASIMOVA, Ye.S., tekbn. red.
[Standardizing the consumption of materials in production and
construction] Normirovanie raskhoda materialov v proizvodstve i
otroitellotwe Moskva., lzd-vo ekon. lit-ry., 1961. 99 p.
(MW 14,10)
(Materials)
i mil f in i7l! Ill, -,T It 11T
MOM ti~ Ij
z I 111

ZHIMOV, G.V. [Zhukov, H,V.j
Forthcoming All,-Union Joint SeBsion.on tho Distribution of Mineral
Resources* Geol. zhur. 20 nc.2:1124,125 160. (HM 14:5)
(Mines and mineral resources)

min WHORT A
I ful
l I EffIRPTHIP "IH
1;

ZHUIKOVO G.V. [Zhukov., H.V.1; NASTENKO, A.A.
Geology and ore potential of the Orekhov-Pavlograd band of magnetic
anomalies. Geol. zhur. 20 no.,3:62-68 160. (MIRA 14W
(Orekhav-Pavlograd region-Ore cLposits)
7-1
RVA"T �R

ZHUKOVp G.V.[Zhukov, H.V.]
Carbonate Metas~matjsm In rooks of-, the Orekho~d"_~"phvlogi~d belt of
magnetic anomalies. Dop.AjI UESR no.3:368-370 161, WAA 14:3)
1. Institut geologicheskikh nauk USSR, Predstavleno ~kadeaikom
P11 USSR NoPoSemenonko[Semenonkop M*P*j*
(Metasomatiom) (Carbonatites)
(Zaporozhlye Province-magnetic anomalies)
IM
OHM.

ZHUMOV, G.V.
Genesis of iron ores in the vestern Azov region. Sov. geol. no.2:
e7_96 7 l6o. (MIRA 13:11)
1. Institut goologichaskikh nauk Almdemii nauk USSR.
(Azov region-Iron ores)

S/006/60/020/003/001/003
B016/.B067
AUTHORSt zhukov-,__G._ V. , NastenVo, A. A.
TITLE: Geological structure and ore content of the Orekhov-Pavlograd
zone of magnetic anomalies
PERIODICAM Geologichnyy zhurnal, ir~'20, no'.03,nd96% 62-68
TEXT: The authors describe the band-type zone of the Orekhov-Pavlogral
magneticanomaly running from North to South. Only its central part
whose geological structure is well known lies in the Ukrainian crystal-
line shield. This.2one siretches southward to Melitopoll over more than
250 km. It is -15'~-45 km wide. The authors discuss the results of
borings in a group of anomalies around the town of Orekhov: 1) Novo-
Andrifvolka, 2) Vasynivs1ka, 3) Teroyanstkat 4) Novo-Danylivalka, and
5) Yelizaveto-Troftalka. A rock complex consisting of magnesite-quartzite,
various gneisses, schists, and metabasites (amphibolites, pyroxenites,
periodites) was found. The magnetite.quartzites of this region do not
essentially differ from rocks of other anomalies of the Ukrainian shield.
Their primarily sedimentary origin is definite. The authors found that in
Card 1/3

Geological structure and ore content... 3/008/60/020/003/001/003
3016/B067
certain anomalies, genetically similar iron-containing silicate formations
occur; the composition of the complexes is, however, different. Accord-
ing to the authors, this indicates different conditions of accumulation.
They suspect the occurrence of two iron-containing silicate formations of
two typess 1) beds with basic volcanogenio rocks; 2) beds with mainly
normal sedimentary formations (gneieL;, schist, iron-containing quartzite).
The age interrelations cannot be definitely established. This is partly
due to insufficient exploration of these areas, partly to the transforma-
tion of the sedimentary layers into migmatite by granite intrusions. On
the basis of comparisons by M. P. Semenenko (Ref. 2), the authors regard
the identification of the formations (complexes) I and II with two sue-
cessive series as possible. In this case, the volcanogenic series was
formed first, while the gneiss-schist series is of more recent origin. The
latter is bedded in the core of the anomaly which constitutes a synclinori-
um, whereas the former is bedded at the wings. Rich oxide ores are prao-
tically not found in this area since the weathered crust in the central
part of the zone is not thick enough. The iron-containing quartzites which
occur as magnetite varieties and contain 30-33% iron, are low-grade ores.
The authors discuss the individual boring sites 1-5 mentioned at the be-
Card 2/3

Ge'ological structure and Pre content... S/008/60/020/003/001/003
B016/B067
ginning, they give the depths at which the ores are bedded, and also their
approximate quantities. On the basia of these data, the authors conclude
that the quartzites do not form largo ore bodies, and that the individual
deposits do not contain more than 35 million tone. It is, however, ox-
pected that individual deposits lying in close vicinity will warrant the
efficient operation of a mining combine. Zones 4 and 5 are most promising.
The northern part of the Orekhov-Paylograd zone is assumed to contain
silicate nickel ores, and iron oxides in q possibly covered weathered
crest. The lower voloanogenio series perhaps contains sulfide nickel or
cobalt ores., Also the southern part of the zone will be explored. The
authors mention Ukra7inelkyy heofizichnyy treat (Ukrainian Geophysical
Trust) and Ukra1ns1ke heolohichne upravlinnya (Ukrainian Geological
Administration). There are 5,figures and 2 Soviet-bloc references.
Card 3/3

S10081601020100210011001
13103/B202
AUTHORs Zhukovp G. V.
TITLE: The forthcoming ~All-Union joint session on the rules governIng
the distribution of useful minerals
PERIODICALs Geologichnyy zhurnal, v. 20, no. 21 1960, 124-125
TEXTt The author announces the second ordinary All-Union joint session on
problems of the rules governing the distribution of useful minerals and on
the compilation of prospecting charts. The session will be convened. by the
Akademiya nauk SSSR (Academy of Sciences USSR), Akademiya nauk USSR (Academy
of Sciences UkrB3R)j Ministerstvo geologii i okhrany nedr SSSR (Ministry of
GeoIlogy and Conservation of Mineral Resources USSR)q and Holovne geologichne
upravlinnya USSR (Geological Main Administration UkrSSR) in Kiyev in May
19~60. This session 'is intended to -.oordinate the studies on the rules
governing the formation of deposits, their prognosis and the compilation of
prospecting maps on a large scale. The following problems will be dealt
withs 1) Metallogeny of Precambrian shields and old mobile zones. 2) Rules
Card 1/3

S/006160/020/002/001/001
Theforthcoming All-Union joint... B103JB202
governingthe distribution of sedimentary and secondary depositat 3) Methods
of compiling metallogeny and prosp!~cting aharts. The session will be
attended by leading scientists and pepresentatives of scientifio and
industrial geological organizations of the USSR as well as by professors and
teachers. About 50 lectures will be delivered which will be published prior
to the session. Sections will be held simultaneously dealing with subjects
1 and 2, whereas subject 3 will be discussed at the plenary meeting.
P.,Ya. Antropov, Kiniater of Geology and Conservation of Mineral Resources
USSR, M. P. Semenenko, Member of the Academy of Sciences U`krSSR,
Yu.-G. Staritslkiy, Doctor of Geological and Mineralogical Sciences (VSMEI,".
Kh. M. Abdullayev, Member of the Academy of Sciences Uzbekskaya SSR, and
other scientists will also deliver lectures at this meeting. The work done
by the session will be published in three compendia. Two excursions will
be made after the end of the session, one to the Azovs'ke more (Sea of Azo7)
and to the Kryvyy Rih. 1) The participants will get acquainted with the
geological structure of the southern part of the Ukrainelkiy krystalichnyy
shchyt (Ukrainian Crystalline Shield) as well as with the Donetalkyy baseyn
(Donets Basin). 2) The central parts of this shield as well as the most
Card 2/3

8/008/60/020/002/001/001
The forthcoming All-Union joint... B103/B202
important iron and manganese deposits and other deposits of useful minerals
will be inspected.

MUKQV d.; CEMOVICH, N.Ta., red.izd-va; GMTAROVA, V.Te.
~_J__G~eyop 0tvOre
---T-Sidiarova, M1.1 tekhn.red.
[Characteristics of the distribution of deposits in platform
covers; reports] Zakonomernosti razmeahchenile mestor02hdanil
v platformannykh chekhlakht doklady. Kiev. lad-vo Akad.nauk
USSR& Ptez, 1960. 191 -p. (Knu 13:10)
I# VaesoMnaya oblyedinennsys sesoiya po sakonomernoutyam rat-
meshoheniya polexnykh Iskopayemykh i prognoznym kartam. 2d.
Kiyev, 1960.
(Geology, Aconomic)

in
14 (1
Vw 0;:
am
03 c. pro we
'" '. - " E 0
gf-wig. H,
50
-%. 40 96-.4
W an ft
4 p z
L ci
A~O
t.9
A E
u I
IN I NIL;
till .--a i 0
3
CC

ZWK0 otv.red.; CHEKHOVICH, N.Ye., red.izd-ve; ZLTAROVA,
V,Ye., tokhnered.
(Metallogany of Pro-Cambrian shields and shift zonos3 Notallo-
geniia dokembriiskikh shchitov i drevnikh podvishnykh zon;
doklady. Kiev, Ixd-vo Akad.nauk USSR. Pt.l. 1960. 261 p.
(KIRA 13:12)
1. Voesoyuzuaya obffyodinennaya sousiya po xakonomernostyam
razmashchaniya polesnykh iskopayeaWkh i prognoanym kartam. 2d, riev, 1960.
2. Institut geologichookikh nauk IN USSR (for Zhakov).
(Ore deposits)

ZMOV. G.T., otv.red.; OTCHAROVA, Z.G., red,izd-ve; LISOMS, A.M.,
--tekhn.red.
EKethods of making metallopnot,16c and prognostic maps] Voprosy
metodiki sostavleniia mtallogeniohookikh L prognoznykh kart;
doklady, Xiev. lod-vo Aked.usuk UWR. Pt.3. 1960. 126 p.
(KIRA l3tl2)
1. Veesoyusneya obOyodineanaya sessiya po, iskonomernostyan
rasmashchaniya polesnykh iskopayezvkh i prognoznys karteme Zdj
Kiyev, 1960. (Ore deposits-Kaps)

1. ZWOV, 1.
2, USSR (600)
4. Poultry
7. Development of communal poultry raising on collective farms. Kolkh. proiz. 12
no, 12, 1952.
9. Monthly List of Russian Accessions, Library of Congress, Yarch 1953. Unclassifled.
oil

T.,
Subject
Card 1/1
Authors
Title
Periodical
Abstract
USSR/Electricity
Pub. 27 9/25
Institutions:
Submitted
A ID P 9401
Akopyan, A. A., Kand. of Tech. Sci., Gurvich, N. G., Kand.
of Med. Sci., Zhukov, I. A., Eng., Negovskiy, V. A., Doe.
of Med. Soi.
Possibility of cardiac resuscitation by means of impulses
during ventricular fibrillation
Blektrichestvo, 10., 43-49, 0 1954
Experiments with de-fibrillation of dogs' hearts are
described and optimal impulse characteristics were
determined. Posnibilities of application to the human
organism are dii3cussed.. A description of the de-
fibrillator, generating electric impulses is(given.
Ten photographs and drawings, 23 references Russian;
1899-1954).
All-Union Institute of Electrical E*ngineering im. Lenin;
Laboratory of Experimental Physiology for the Revival of
Organisms of the Academy of Medical Sciences
J1 10, 1954

ZIIUKOV. 1.A kand,med.nauk
Characteristics of under water avimming and otorhinclaryngologic4l
solo-ztion of frogmen. 'lout. otarin. 25 no.50-10 S-0 163.
(MIRA ViO
1. lz kafedry boloznoy ukhao nona i gorla (naahalinlk - zasluzhefinyy
diayatall nauki prof. K.L.Khilov) Vornno-meditisinakay ordena
Lanina akademil imeni Klrova, Leningrad.

GURVICHt N.L., doktor med.nauk; AKOPYAN, A.A., Prof.;.ZHUKOV, I.A., inzh.
Constant magnitude ofan injurious electric current. Vop.elektropat.
I elektrotrav. 1915-41161. (MIRA 15:10)
1. Iz laboratorii eksperimentallnoy fiziologii po ozhivleniyu
organizma (zav. - prof. V.A.Negovskly) AMN SSSR i laboratoriya
perenapryazheniy (zav. - prof.A.A.Akopyan) Vsesovuznogo
elektrotekbnicheskogo instituta im. V.I.Lenina.
(ELECTRICITY, INJURIES FROM)

ZHUXOV, I.A.
The GPS-2M tractor crawler dump trailer. Biul. takh.-ekon. inform.
no.16:73-74, '59. (MDU 13:3)
(Dnv trucks)

ZHUXCIV I. A -HypnopsychotheraV of Patients with Skin Diseases together with
T
erap;jtic Factors from the bochi-Matsesta, Spa," Kharlkov.. 1955. (Disser-
h
tation for the Degree of Candidate in Yedical Sciences).
So: Knizhnaya letopis', No 8,, 1956j pp 97-103
NO-

ZH[JKO *A.
Decimeter wave generator. Tlz, v sbkole 16 no.6:62-64
KrD #56. (MLRA 9012)
1. Pedago icheskiy institut, Smolensk.
101'scillators, Blectron-tubs)

FOIATMZCV#, P#Pos km34. tj%jkomtem,, nalk, zliMoVs. 1,&,
of:aodlm olm tba dinti-lbution of cabollo- emm. Vent,
k'T,Kazakh* SIMR 21 V4.12164meA D '165. (Imuk 133u)

I.I., inzh.
Properties of spondil cia*y'andthnir effect '. upon underground
emeavations. Transp stroi. 8 no, 7:21-22 J1 159. (HIRA 11:7)
iclay-Inalysts)
(Soil machanice)

ZHUKOV, I.F.
Construction of a deep sulyway station from precast rein-
forced conorelk-le, 1rans. atroi. 13 nQ.8-32-,-35 Ag 163.
(NIRA 17:2)
1. Glavnyy inzh. Kiye=etroproyekta.

~f J;~O V, I
TSYGMKOT, A,S.,inzho,- ZHUXOV) IsFelinth,
Xvaporating units used on the Antarctic whaler 'Blqvm." Sudostroenie
24 no.4:1&20 Ap 158. (MIRA 11:4)
(whalers) (3vaporating appliances)
jTjj-7
-1 All "If -r--ff
m; miiTi, "'mot, IN' mff mwff%l "391"TIMMITIMMIN

"273-66 WT(m)/ZPAW-2/WAW-2 rip(c) rs
ACCESSION MRs ATS007942 UR /0000/6V000/a00/060010603
AUTHOR- Alekqe
yev A. G.; Rasargj!j~LY!!. G., LavMjjt'=,
Litunovskiy, R. N. iiiT"hev, I. F. , Upvro,%,?I. P.; Stepanov, A. V. 7uzov, V,
TITLE: a"ic characteristics of the isochTsciilator -)as i -,nne(t InTl 4~*t, "le -Zen)-
r.ance S"~,s ~em A connecting r-)~j is us-d, 0,
rT i ~-a I 4ne hori zxin?, a. a~-.,~; Vi i I -i - ir i v( .
-namrer -onsists -)f twr r- I A 114flif -A - I
lni
~aus!, ilong wi-~ !he risorant .1ine,
Card 2 / 3

L 2273-66
ACCESSION MR: ATS007942
installed in the electrowgnet poles. Remetely controlled measuring probes and
targets for operating with the internal beam am installed i_n th(a c-hamber. Place-
nw--nt of -,.')e ion source is airto lone r-eynote v a pwi- w i 'i c u T
(.f tne mcuum, 'I- 5~14t ,)e :a I! ~ -J.? in