SCIENTIFIC ABSTRACT GRIGOROV, N. - GRIGOROV, N.L.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R000516720017-2
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: January 3, 2017
• Document Release Date: July 27, 2000
• Sequence Number: 17
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

-Asymptotic Behavior of Higher Green
SUBMITTED: February 1, 1958
Funotions SOV/155-58-2-32/47
Card 2/2

240)
AUTHOR:
TITLE:
Ginzburg, I.F.
SOV/155-58-2-33/47
Asymptotic Behavior of the Matrix Elements in the Two-Charge
Meson Theory (Asimptoticheakoye pavedeniye matrichnykh elementov
v dvukhzaryadnoy mesonnoy t*orii)
PERIODICALt Nauchnyye doklady vysshey ahkoly. Pisiko-matematicheakiye nauki,
1958, Nr 2, pp 152-157 (USSR)
IBSTUCTi In the present paper the author Inveatigaten the anymptotio
behavior of the matrix elements of the S-matrix during arbitrary
2
processes for "large impulasn"t Ip I P)c I >"V M,in connection with
the paeudoecalar meson theor$. Ii Is assumed that b bosons and
n+1
2f fermions (b+2f - n+1) with the impulses Pl""'Pn+l' P, - 0
have a share in the considered procens. The behavior of the matrix
elements is considered in two canes: 1) p 2) P2 __poc)
'% iPk __*Co % i
At first the behavior in the first non-vanishing approximation of
the theory of perturbation is determined. Then numerous corrections
are introduced. The author thanks D.V.Shirkov and B.V.Medvedev for
t1eirvaluable discussion of the results.
Card 1/2

Asymptotic Behavior o-f the Matrix Elements in the SOV/155-58-2-33/47
I Two-Charge -Meson Theory
There are 6 figures, and 5 references, 4 of which are Soviet,
and 1 Italian.
ASSOCIATIONtMatematicheskiy institut imeni V.A.Steklova (Mathematical
Institute imeni V.A.Stoklov)
SUBMITTED: March 1, 1958
Card 2/2

GINZBURG, I.F.; SEREBRYA.KOV, V.V.
Electromagnetic corrections to weak interactionse Zhuro
ksp. i teor. fi2. 40 no.6:3.738-1745 Je 161. (MIRA 14:8)
:
. Institut matmatiki -s Vychis3-itellnym tsentrom
Sibirskog'O' otdeleniya AIR AMR.
UE'luctromagnetic theory)
(Nuclear'reactions)

GINZBUHG, I.F.; Ki~KOIVA, V.I., red.
(Inelastic interactions between high-energy particles in
renormalizing theories of strong Interactions] Neuprugie
vzaimodeistviia chastits vysokikh enorgil v renormiruemykh
teoriiakh sillrykh waimodeist,vii. Novw;,'Ldr.,;1K, Di-L m;1-
tomatiki. 50 JUI SSSR) 1962. 17 ij. (elli"A 17:"')

S/056/63/044/002/020/065
B102/Bla6
A UT HORL Ginzbur.1,, I. F.
TITLE: Inelastic interactions of high-energy particles in
renormalized strong-interaction theories-
PERIODICAL; Zhurnal eksperimentallnoy i teoreticheskoy 'Liziki, V. 44,
no. 2, 1963, 500-513
TEXT: A method is developed for analyzing high-eneray strong; interactions
in renormallized theories. The method is based on a representation of the
common properties of these theories, such as those given by N. N. Bocolyubov
and D. V. Shirk-ov (Vvedeniye v tiooriyu kvantovannykh poley - Introduction
into quantum field t1heory, Gostekhizdat, 1957), and an ex:)ansion. of the
Green functions and the differential crous-sections for inelastic
procesoes in u power series of the reciprocal enerby 1/s, tak-en as the
small parameter (S - (k +P )2 . m2+11 2+2p E, S>>1ti)- F~rst the author
0 0 0 0 0
investi6fates the kinematics of the inelastic processes donsidered for
a --~ oo ; these p.ro.cesses are divided into two cases according to the type
Card 1/3

8/056/63/044/002/02o/o65
Inelastic interac ,tions of ... BIG2/B166
of momentu transfer between the fast and slow (k,~!particles
m
characterized by -1 - 2:p,-po (1)_~lim 1po lls-1 .'Ju > 0 and
1, . ;m s -~oo
'2) lim)p I - 0. In the following single case
. Is- (1) ~d investi4;ated.
All graphs of Oiq perturbation theory are subjocted to a classification
and are divided into a finite number of diagram groups characterized by
certain topologi6s. It is shown that the contributions of all -ra-,)hj of
a given topoloey to the Green function are equal in fir4t, aPproximation.
For a compari3on of the importance of graphs of a given to:,ology it is
therefore sufficient to compare the graphs of this class whose hi6h-energy
parts correspond'to the first nonvanishing perturbation-theoretical
approximation. For this the well-known method of aeneralized graphs is
applied. This method is also used in what follows for comparing the
importance of graphs of different topologies. It can be shown that in
the limiting case a -+ oo , graphs of a certain definite"topology make the
main contribution to the Green function:in the process." This topology
corresponds to the exchange of one or a'few particles between the fast
Card 2/3

Inelastic interactions of ...
S/056/63/044/002/020/065
B102/Bia6,
and the slow groups. The region of applicability is sho~in to exceed that
for the usual pole theory of peripheral interactions. T4ere ure 3 fii;ures
and 1 table.
ASSOCIATION: Institut mateinatiki a vychialitellnym tse *ntron, Sibirokogo
otdoleniya Ak-aderiii nauk SSSR (Institute of IMathematics with
Coinputerind Center of the Siberian Branoh,of the Academy of
S~;iences USSR)
SUBMITTED: Ma'W 5, 1962
Card 3/3

GII?ZBIJRG, IoFv
Inelastic interactions of high-ener&y particles in
renormalized strong interaction theories. Zhur. e*ksp. i toor,
fiz, " no.2:500-513 P 163. (MIRA 16:7)
1. Institut matematiki s vychislitellnym tsentrom Sibirskogo
otdeleniya AN SSSR.

L 17618.6" EW'd)/EWr(1)/F0G(W)/8DS AFFM /ASD/ESD-,3/IJP((;)/SSD
S/056/63/044/003/020/053 -0
AUTHOR. GINZBURQ. I. F.
TITLEs Nonaymmatric.q1tppytolq~ asymptotic expressions for hiepar
Green's functions of tha ranormali7od ihoory
PERIODICAL: Zhurnal eksDerimentalinoy i telchnicheakoy fiziki, v. 44, no- 3,
.1963, 894-8�8
TEXT; The highor Green's functions of the ranormolized theory were usually
studied in the weak coupling region with a logarithmic accuracy Vhile S. Weinberg
(Ref. 2: Phys. Rev., 118, 838, 1960) investigated such Green's functions with a
power accuracy. The present paper obtains 'doinberg's estimates using a simpler
method, convenient for the analysis of physical processes at high energies.
Nonsymmetric ultraviolet asymptotic expressions for multiparticle Green's functions
in the nonDhysical region (q-'Ooo) are defined by diagrams with exchangn- of a
minimum number of particles. There ar9 3 figures.
Card 1/2

L 1761-9-6,3 8/056/63/044/003/020/053
Nonsymmatrio ultraviolet asymptotic expressions ...
A45001ATIONI Inatitut matematiki a vychislitallnym toontrom Sibirskogo
otdoledya Akedamil. nayk SSSR Qlathematical Institute and the
Comuutar Canter of the Siberian c--a-do"-m-v--of
-.-SaiencAn. MA)
SUBMITTED3 may 5, 1962
Card 2/2

L 2213-6'6* rEWT(d) IJP(c)
ACCESSION HH1 AP5019250 UB/0056/65/049/001/0335/0
AUTHOR: Ginzburg, 1. F.; ShIrkoa
D* Ve
TITIZ: The renormali~~tion Uoup and the ultravi6let &r otic 3A of scatter-
ympt
Ing 4,f" -K
SOURCE: Zhurnal eksperimentallnoy I teoreticheskoy fiziki,, ir, 49, no* 19 1965#
335-344
TOPIC TAGS: scattering amplitudep uv sp*ectrum., Green functiono group theory
ABSTRACT: This paper contains a concise aurvey of the basic points of the
renormalization-group method and a detailed analysis of the possibilities of this
method in problems of ultraviolet asymptortics. The foundations of the
renormalization-group method are briefly outlined;, The general solutions of the
functional equations derived by L. V. Ovoyannikov (DAN SSSR Y. 109j, 1112.. 1956)
are written out and are used as the basis for finding the high energy-asymptotic
behavior of the scattering amplitude (f), If the mass variable drops out at high
energiesp then f Is a function of one argument if the scattering angle is fixed
and a function of two arguments if the momentum transfer is fixed. In the former
case the renormalization-group method gives a better asymptotic than ordinary per-
turbation theory,, but in the letter case it does note The sum of the main loga-
.Card--

L 2213-66
ACCESSION M: AP5019250
rithmic t" in the symmetric elarged pion thepry to found. A special bypotheals
is formulated,, vhich leads to,,an asyiptotic exprecsion.of the quasi-Regge type for
both the elastic and the ic amplitudes* i "we thank 1. Tp4qm!~- "ONritiag
the Appendix and A, L o=V,
.y?~~Oi prov$ding the initiative i4cW the work, -&i~ of us
(I. Go) also thanks Do Stellm l! ;~ 0 l.figure and 38 fonmlas-
;"rig. art. has i
Zwl:~;
ASSOCIATION: Institut matematikL i iychislitellnyu teentram Sibirskogo otdeleniya
Akademii nauk SSSR (Institute of Mathemstice with CCMM~A lon.Copter
of Sciences
e rty~~A~cM
SUMUTTED: 27Feb65 JWL-. dO SUB CODS: NP
RR REF GOV 015
f
Cor 2/2
d
R-M
M, is V,
FUR
47V20- EMUR",

RAPOPOll', '1 .14.; Gillf&iURG, '..',G.- K1111,ASNIKOV, I.I.A.;
rl;d.
(Engineering, and structural drawring,; a rronun"L for
-in rourse 11 of "Buildini., of lliiridgu~l Elul DIT.-
nels", "Indu:,trlal. and Civilian Cono trixticnll , "Wavir
ply and Sewerage Ilysilem", "Econumik-s and
Cr,n:: true t Lon for Raill-vad Transportn'.iorl"I lrizlhencrn~,-
st.2-oi t,ellnoe, cherc),enle, uc!hf~brioe po,;oblo diln ,ztiiolenLw;
II kursvi. spotsiallnostoi: "Stroitellotvo
"N.-isty i tonnell" (14T), "Prur,;yshlennf-)e i -ru~"Alan.3kce s-ro4tell.-
st~vall (PGS), "Vodospabzhenic i "Ekom-mlka
organizalLsiia st,roitel-Istva na
(ES). t-,Ogkva, vsas. ztioclillyi 111-11, ra"
i963. 69 p

AUTHOR: Stepanov, G.M.; Ginzburg, I.I.
TITLE: Some Methods of 'tandardizing Electric Power Consumption in
Depth-Pumping Oil Production (0 nekotorykh metodakh normiro-
vaniya elektropotrebleniya pri glubinnonasosnoy dobyche nefti)
PERIODICALt Energeticheskiy Byulleten', 1958, Nr 7, pp 1-7 (USSR)
ABSTRACTi The authors discuss K.N. Kulizade's article on methods of
standardizing electric power consumption in depth-pumping oil
production; agree with his formula for calculating the speci-
fic electric power consumption but cannot accept his conception
of k - the factor covering the variable component of the power
consumed by the pump in relation to the size of the useful load.
Kulizade regards this as a constant depending only on the type
of pump, whereas the authors state that k also varies from
field to field depending on the working conditions and can not
be generalized. As an illustration of the errors possible
by this method, they compare Kulizadela experimental. findings
with the results worked out from his formula (Tablon I and 2).
Some inaccuracies in the experimental data are pointed out.
The method of calculating the specific power consumption
Card 1/2 employed in the officbs of Orgenergoneft, and O.P. Shishkin's

910-58-7-1/8
Some Methods of Standardizing Electric Power Consumption in Depth-Pumping
Oil Production
empirical formula, as mentioned by Kulizade, are discussed and
their degree of error compared (Tables 3,6, and 7). Neither of
these two methods are founded on accurate study of a sufficient
number of cases and, in fact, the most accurate calculation
of the specific power consumption can at present be made by
a graph. There are 7 tables, 1 graph and.2 Soviet references.
Card 2/2 1. Electric power-Consumption 2. Oil industry-Applications
3. Electric pover-Standards

GINZBURG, I.I., inzh.
Two wires and pipe system for the electric power supply
of an electric bit. Prom. energ. 20 no.11:49-53 N 165.
(MI RA 18: 11)

GINZBURG, I.
=a/lklpep Oct- 1947
ftipso APIPMt an& ft"lles
one Pwfarmwe of the Pleet in the Now Five-Year
Planp' I. Ginsburg, L. Turstakly., 5 pp
"Morskoy Plot" No 10
Resume of the goals set for the merchant fleet in the
1946 - 1950 Five-Year Plan. Present equipment Is to
be more empliptely utilized., operations expqditedj,
and new qquipiont to to be added to oem7 out the
plan.

PA 3099
GINHURG, I-
Oat l9kT
Shipbuilding
"Ways of Doorewing the Cost of Ship Repairs," I.
Ginsburg, A. Sy=v, 4 pp
"Jimskoy Flotm No 10
ConsIdeTatIon le given to the various expenditures IL
!ship repairing and the means and possibilities of do-
crowing then in order to out the very heavy expense
ine arr ed in this work.
W 3OT"

TURNTSKIY, L.; GINZIRTRG, 1.
4'A-~'e
Thirty years of sea transportation. Kor.flot 7 no.11:5-10 X 047.
(Shipping) (Ships)

GINZFUnG, 1.
usa/kerchwt nest Vo4.o4io Dec 1947
"The Maritime Fleet on the Increase, "I. Ginzburg,
Q~. Turetskiy, 31 PP
"Morskoy Flot" No 12
Maritime fleet has exceeled norm for first year of
postwar Stalin Five-Year Plan. In 1947, plan had
almost been fulfilled by November., an average of 20%
Inorease over.operations for similar period during
1946. Sme data., all in percentage figures.
17G60
1C 17o6o

May 48'
ShippIng
Ships, Cargo
Ocapeolty of the Fle-
et and Heduction of the Cost
Price of Transportation," I. Ginzburg and L.
Turetskly, 4f pr
'Morskoy Flot" No
first part of series on methods for reducing
transportation costs, Discusses effect of
ORP&OIty of fleet on sictual cargo capacity and
frice per ton mile foi cargo transported.
1AW 25

(,Ost accountln~-, of sopgaing vest4el
MO'k've, Morckai trans.port, 1949. 99 p. I
.1le847.G5 (50-27455)

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Exchange adsorption of nickel by different minerals.
1. Git iwrx and A. 1.
R .-S. S.~-SH. 1940. No 2. W) NJ; cf. C. V 34,
-1011P.-IN1,11. 41111a we Iliven Im Ow admwp-
lion of NJ by alxmt U) InInerAl. indUdIllif 001111114 Ill % 111111
f-oug clays. hydfou!o malgivila 111catc, clijurl,", tco,
lites. and hydroxides of tfivairlat IjIrt;Ij.% al,41 cajjq)jIjg_
-IIALtUPGKAL LITIFNAVAI CLAISIFKATIOP
'aw OF -0
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09
400
coo
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400
1000
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XgiaffK"S
- .040
lb"Ca. Tb$"=W-rP"
aiN1bysW1j
I
fol"Wels is expi by hydrab%le. F. pmwtw
goo
zoo

goo
'goo
goo
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L r A -.I L it P F U
v T , V A I L AA 00 Lt. W if
!

Aleshkow's thtOFY Of th# otion of dvposits of hydrous '

~;jfwbula. 11-11 .""j. ... I x %
NJ silicates l. - 90
-
4 1941. N". .1. 11'1 S. ( ii.. 00
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4lon
.1. 1. 1111vilc 11
41. 1~ v
I .
Ifloo
1-9 M-WS, ~VIIIPMAIIII% Zu .'ad "I Afss., 54, too
cr-4, N-- 4, 6-11 1 11-421 Wngli-h noundry, Ill. -AW-4
Vol Amuum cut lw fjound In tho, w4ulion as well 64 In Ilar
ui~-Iublv troWur lurnil 4)1 aluluilliff"Mi
Ionic volutiolis form by wrathefing. with III.
Ompmitinvo prolt-redinx its A6i anti Alkaline inediA. SIM
hi. lite highest migration ability with AIr0. and Frill, 'C'
t"11(roving its that (inter. Kaolin Is formed At pit US to
.J1 while in the ba4v media the" ate forturd clAys of th,
tyroe. Sruiral Virdia, Are not
J"
I. vocable to clay formation. 114u0c forutilion i% due
t,, introoduction of altunina a% well A% top leAching t;ut of
%ifica with %ulporquent migration of aluinin.t. &
i!
IS . IS I? Is 0
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00
00
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, - , JW U dl ft 41 n It t Iro
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i
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of lite
'
'
"
r
'c pr
00
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V-21101"
ollml. i
" ,,, and
f
.
o!
etrogfiLl, - hich they 2' age it
w
vl

0
0 he p
it, in
, C4
611'10011~Vlw
~
(1"" NO%& t1w :.
the N1 ms
l, , lAtion 11
! l
.1
Witt l9elle"O I - -veil to the olu - -tin' on
try
site[,
00 It il, pAnted out that .Ulfil,. (sits) - of them

- the ha",
roon
the IF
00
'
ows.
J Si -it Fe fton, tits or , A the ififfe'"t "f
forrilatitill
l
lu"
0

00 the
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GINZBIURG I,I,- BELYANKIII, DeS., akademik, rodaktor; SOMLOV, G.A., roda)-ttor.
(Peachemistry and geolog7 of the ancient weathering zone in the Urals]
Geokhimiia i geologila drevnei kory vyvetrivaniia na Urale. Moskva,
Izdwvo Akad.nauk SSSR, 1947. 134 P.(Akademila nauk SSSR. Institut geo-
logicheakikh nauk. Trudy, no.81). (MLRL 9:7)
(Ural Mountains--Geochemistry)

_U
achgmUtry and ccolocy of a
r
e
the Pudy
1
,
ered cr-%
-
- - - -
Akad Nd:-*
'-
k
N
au
,
Gc,al.
. - t 9 4 A
~-
c
t and 1110iph-
~
d ptirn k
-- (1) d':,IaI
t
,
-
C 'r
n in
~ i cru-tj In the ultrar~-'c
~thcr,
W
i
,
e
tut we
"tLu':i (-
) (lisruidon th'!'Xies Of the 1111c
WII-
l
.
;I
usts, and ' 3) min"algy of the anciLnt W
he conflectioll I'lith the Ni
crod, crusts. .d in p~cutmr I I water
TabIcs of rcek 1,
lsit5
l d
.
cp
Ura
deo,its Of ibe 11TOignout the repert.
ided t
Its "t prov
Cev
awdyi;cq ft, Glmfvs S.

N,

Eli
... - - - - - - - - - - -
R. 731 WIN
11 WrMl; I Immil- - Owl!

GINZBURG, I.I.
Ginzburg, I.I. "Protective films on diffused-pulverized silicates and
their posFible technological-significance in ceramics," in symposium:
Syr'yevy.ve resury tonkokeram. prom-sti SSSR i puti ikh ISDOVZOVaniyA,
Moscow-Leningrad, 1948, p. 149-54
SO: U-2888, Letopis Zhurnallnykb Statay, No. 1, 1949

I. ~
0 .. -1 .
A 823 - 011-17"IfRfl, 1. T. 0)-)razovrjnio T)r,c,-v.,iey K.01,y Vyvotilvanlyn th, Turritor-JA :35~fl,
Ee flinornly i lkh Svoystva ?"rudy Yuhkeymy Sessli, PoF,!rya~;hrh StoletiYI) So
Dnya Rozhoeniya Doluchayeva. Pl. L., 19h9, 'S. 20-1-15. -- Biblio".: S 2lb-15
SO: Ldtopisl No. 33, 1949

~r aremkonavdim gnd ffnvk
"a 141Y saidys" are faclutled. 'it Is cou 1u 0 lano.
te Is not Identiled voith Woysite am4 m be ehmed
with the madtaxaffleafte nor ILM kulfalte Imp.
=
Marie Slclft$L-.

Oil
Kgrofile. 3M40 JSIO J11,0 I I ('.1111hurig and I
Airlills 1 1, twh.
Ott'll. -- 1u.W 111111bil A 70. :U 11,10001.-
t- oriffI.Art-int if% the gen.-ril arn-o c4 Abejm I
itle Nig hydi-illwAir -ric, C. R. I,.tjncuj,h7
h"All, (1) - &-- A tooixhm~
fl... Mir. 1". 1 , .. F.14 . 1118her
I it, 11'. 0 1,, It 1 1.1 ., Omit, .11 riulo.
lltA% :it ;ikl,. .111.1 Ali Tv.11trellm.
April At 910'. %mill.tr two IIJAI of III 4-fAy
.It 44FAill t. Al", ittiflar. tf-Ki,ohlt (it , im hi-fing "almif.
m1c." 1, tiol"lly gwqviil.ll r.d'oed. triti'llorill Its thin
Amitill hAllitle,%~1 5.ij lothiowc.
Ism'. tile w:hA~r,fm1v-Ilkr WWI .11%ultur Is witty
I)TwAl, flit A 141her 111411ird hirchillatme, 0 AIXXII
L~ 13-I.SRS (from 6differrut twcurrcnces). FilmousAgpe.
sites in It have A (felinitcly Wwrr m., 1.40-1.494. And ;t
I'll cil marm-C fill to flIkks. atimixtif lWiAtellite Okirr-
tritiarriec 0.411 2t Is rait-tv ohwivrJ Tile tht,rtntil ,utwv of
It rop'. tll~". tMO)'. wAd
"I-W)* (11W l.tl,t ..I. polly 111,10111"I -fill -III,
11U. 1114d " I. .11h to $.A.. I...- I m I 1 .1211 A If. Kb A
N I`wwilir 'It .lt,li.l I'vilk-st, VA I it rI t.m. ff.
thevinAl curvc 4 111, miml..r I-, tft~o ~
onlo Iml III. wo A it,
va"t At 149.0 IM 1,. 11
thall 1.1 1. Aml 41, jill'im"j. .1. 1" wt.4-ml.. 11, It 11.
'111%. 1, -11 ~0
i&hVlIfAtUwI1 "III%- AIV O%Ine "hd, f.
Ate, -If v., fl t.v I,--- qx .6;,-
I'lit- -.1 I'L. ""'Itc.
1.10.1 it. I 1 .1 -"K I ... -- . I ,,, III
the , a AV dl..Nt Am_ fit .."o, A, 11.1. ."A
K.I..61H. I,
I fit,t It, ovj~ 1111A I'molmok .4
'd Foofft thr lion ml.l. f.
Ill flflcfl
I
Mg:
WhWh MAke, its,- llgll,i(v I- evIlls"ll- with
IllgiOll), lIet-v" flu. Imr-1.
1. 4 it,, ml,
........ ...
Or. I Is, I T .1, told I. till 'h'i'villor
all'i Imigil-lic 1, 01.1f it 1, _I.Villors I IL&IIKCII
1" Wilwallool, . Is ... o Ill, 111v -0..f. It, 1.01A
-mo tille. t it, till, .1 -0. 1 Ile I firm
,0 Ill.." sit,
1 '10

GT
nthur g, and A ilka via h nli:b v a
eft"O:."kor~f 'uvarival,lyd j-
llvtlJwActd,6cj.,st3.S.p.

If
CIVO-
k1fobisms of mWaggeolov In the exploitation of nickel
deposits connected wi wg&thtf&d crust I I (-.j1,1I"Ir-
I'l I Z. Korill (;",Hyl /hot. 123. N'- 5. 7. 119 10.14) - 't
:
11wo-imt 4.1 IIIv Ivj- fd 'ifietim, Ni Ilmor
" .111.44-a1 .11111 L-111-111 %M111111 , .111.1 it;
,,.4 minilix 'N1

1. rnznlmn, T- T.; RUrAVTSWTrFOVA, 1. A.
2. USSR (600)
4. Mineralogy
7. Minerals of weathering of the ancient crust. 1. 1. Ginzburg, 1. A.
Rukavishnikova. Reviewed by I. D. Sedletskiy. Izv. AN SSSR. Ser. geol.
No. 5, 1952.
9. Monthl List of Russian Accessions, Library of Congress, April -1953, Uncl.

GE""""'
The Cc=ittec on Stalin Prizes I.Of the COuncil of Xinisters UE'"R) Ln Ute CiCds of
science and inventions announces that the following scientific works, VAVular scien-
tific books, and twftbooks have been submItted for competition for Stalin Prizes for
the ye&ra 1952 and 1953- (Govet!~Uo- KUtw-a. Hoe,7ov, Ro. 20 Feb Apr 1954)
Title of 'dark
Ginzbtirg, I. I. Antiont, Crust OC .,'.ro-
Korin, !.Z. sion on !-he Ultra
'Z it
.mkavis'llni~ov, I. A. Rocks of the Urals
Gf Lho An(At--rit
Cruo, of D'o. "NO,
slorl oc
Urals"
rkminated by
Institute of Geolo'-'-.Cnl
Sciences Acade:iiy of
11
'Xiences 'J,3-~'H
SO- W-3o6o4, 7 july 1954

GINZBURG, I.I.; SOKOWV. G.A.
In connection with the article of V.N.Poddubnyt on "The problem of the origin
of iron or@.* Izvest. Akad. Mauk S.S.S.R., Ser. Geol. 153, No.2, 113-14.
(CA 47 no.22:12148 153) (MLRA 6:4)

13
VY'rogrusive weatlicritig of micall and ~Jij()ritc 1. 1
G, pip7l4g., Voproty T`440g~ Akdfl. 'VaL7.77:
%tensive t;l1lillatiml alld (fit- i
u s s R p "11H.6,11-urc giv,on of jll~ M~Jlml[L---sl foriffilla, f,-t lipfromica,
(1), ';vvatlwrv,l Iii,,titc-i, :llj,l ejjj..rjtc% ill
diff(mit of malfirrifig, I itichi(irm hydrmaicv,
vvv:l I 111scil ill itci"
all )r -wilich sitim tit,: limri,isive repLicenictif )f JK4 bv
(11,0)1. Till- great, critiftinim , the lit-fliciviat'lle 'n ill ,
, if , is
fidd 6 callsed by tilk. li-w-wi"'kal rharacLer of 111"'It (if tix
hydrilillican Hild hydniclAmitet'. The ll,~fillitiolln Miicll G.
fcccmlnlulfl.,~ for nil impf.,vid 11"llifild-, tim, ;,re tit'! 1"Umv-
ing: (A) jl)llrobi, , tiIrj are blotilus alld phlogripio.:: fluml
whichalko lit-. lia ve bevii 011- h1.1
bOVI h1tri)(11KC(l. Alg" ill lite wtalwdral laym in cluinged
only it (B) Wrillicillitc.5 lift: ltitjtifu~ :ill([ phloj,')pilc:l
rrma wisici, tile am;oi itm, itave iitot enfird), or tit ~trly vit-
tircly mplaNA by Oil - Mg' I b;.i lwi:iz -votwwhat 1~:.whvd
li(-cli Cf;itnl:'-,l ii,tk, I"c
'of Mg (A,,itit 1/1 tti tile ~ rt)cntiilc coltilmimtt'. Tit-. ]ale)
Stitgvs are (D) hyfirtwIllorites %%itil l.,w Wid hig.wr
Al mitenti. , lie diffuuntW-Owrtiml ctirv,:~ (it
puttluctil fire Andlar I,) thia of ":mfillift , wbilo till. (-)4l-
therinic ortitochluritic OTict tit 820-8-14' i~,
(E) flydrommirovitei ari: the fir,,, sia~,i:-, of vliangc-i of
muscovitk in which no c-m-mi:11 chwiges t,( 1!w .-ptica! otid
thermal jmqwtfiv~ are bi,-rvvfl. %Vi,,-,i Ld,!, tit.,
talk- ImOwd awav, hm,r hi If mg, Ill - i. ld-(~.A, .'I'l k1
typivill endollivi-mic oTcri, -A Md.ii- j
lklica" The I u 1 1, 1 , 't-
ing flj~ It, I ml
I IVIlf "I tit,- 1; ":1 flill'11131 Jai, ;it it,

Strilettlip ah R mixed pfiwtv with parveh o1 Wite and Illunt-
i I Im j tv. Anot1wr imliortwot proh!'-m i4 that (if the
11iml to Ow It v'va.
is ~t Ilydirottlit:.l I ;l , high '1' (7(":",) -' K ' wpLwed
It, Ito, m-,--1ht:rlui1v oi tfi-~ 1:1:11 1e.~;. fr"1:1 Dili-
V%'Vlk m of Inollo-
Ihonlift. i-o" 1-lol;llile k hulifMcd by :.. im"W".1ve Wlrlrv~~-
ill thl: -mill 1 ('111 ~' 1- (11,0) " from al),alf 2 .5 to :'bout 4.0;
it I., fhw~f'qv I"'f. a, a harrogmeows wixt. Lf
hvilrot1mv;Ls wifli kw)Iii6f(: anil qwtrt,~, and 1he 0-dPin-
Illiailp.lylbic C.'1111171. ooll~lul~ Illin hocro"oleily. N"Ollo-
thirrmite is chancluized It%, the ;jc watcr ad~orbcd
-is flw m
,I., Iomdcd ill (010- and ill (11tO)" wherino
Ing of ftl(kpars io si,ricif(~, hydiontica-i. inivi-irudi-ac inimxcd
pluse", "id ka.liirtit~. triuc L" a scqu-ce if
philub! mi'wrat' t" CIA,tritc, j~ffwfi-~;(C' Ivy'tolehloriw'4'
4wllltfljwi1J~mitc (rare), IwIlow,ite, and Paolio;ll. Th"
flivir ctid virw"llcts llr't id, oli'- I. lk~ftni-
t :,J venniculite am dill't-reat Ili thuir
d (ficrert,re should not br dassifivd to;wthcr,
w .
4y,

T
"Infomation on llyper;7ene Processes in the Works, of 1,. Ye. Fenm;anll
Tr. Mine ralo f!ich. muzeya AN SSSR, 1953., r-To 51 19-29
The aut1hor briefly expounds the 1-asic ideas of A. Ye. Fert;man in the field
of hyporgenesis and their development in the works of Soviet scientis f,..
Ile notes the most imipoftant successes in t-he studir oJ* the --.cochenistry of hy-
perpene proccf7scs; e. r. 2 t1in diocoVC17 of t1w foinal,ion 0'1* minerals "ts a
cult of ,-,oil forminr process (work of B. B. Pol-iniov and Iiis ::;chool), the
work of A. P. Vinorradov in biorcochemisti-f, work on rucathcrin,- cruot and
oxidal.ion zonos (S. S. Smirnov, F. U. C"u'Khrov, !. I. Gin,,'.)urf-). (1,,,'hGeol,
IT
io 3, 1954)
SO: VI-31 1 ~7, 8 Mar 55

USSR/ Cosmochemistry - Geochemistry. Hydrochemistry D.
Abs Jour Rct'erat Zhur - Khimiya, No 2, 1957, 4153
Author Vitovskaya, I.V,
9juQuWa ,
Inst Ac6icldizy of Sciences USSR
Title Sokonite in Weathering Shell of Lead-Zinc Deposits of
Central Kazakhstan
Orig Pub Sb: Kora vyvetrivaniya, No 2, M., AN SSSR, 1956, 184-187
Abstract First description in central Kazalchstan of the clayey
mineral s sokonitc, formccl. in ore skarns and skarnic-
limestones. Associated minerals: montmorillonite,
baddeleyi-be and nontronite. Chemical composition of the
sokonite (in %): SiO2 38.16, A1203 6.70, Fe203 2-38,
CaO 1.27, MgO 1.19, K20-+-Na2o 0-98, ZnO 34,88, H20-
8.28, H20 +7.52, total 101-36. Structural formula
Card 1/2 - 42 -
USSR/Cosmochemistry - Geochemistry. Hydrochemistry D.
Abs JOUV Referat Zhur - Khimiya, 110 2, 1957, 4153
Si 3.49 Al 0.5,24 010 Czn2.41mgo .17 Fe 0.17 A10.1177
(OH)2-+-0.10(ZnO + Cao). Spectral anallIsis revealed
in addition: Pb, Cu, Cd, Cr, V, Ba, Sr, Ti) Sc and Y.
Secured were a thermogram, roentgenop:am and electron
microphotoaaph of the mineral; simplest physical and
optical properties vere determined,
Card 2/2 43 -

GINZBURG, I.I.; VITOVSKAYA, I.Y.
-.-FMMWVW-
Erosion of quartz in hydrous micaceous-montmorillonite clays.
lora vyvetr. no.2:235-238 '56. (Nia 9:8)
(clay) (Q4mrts)

01 ja& VITOVSKAYA, I.V.
,LAJ,,;
Weathering of garnet, axinitic, and tramolitic rocks in arid
regions of central Kazakhstan. Kora vyvetr. no-2:299-316 156.
(MLHA 9:8)
(LLzakhatan--Tremolite)(lazakhstan--Garnet)(Kazakhatan--Axinite)

15-57-1-579
Translation from. Referativnyy zhurnal, Geologiya, 1957, Nr 1,
p 92 (USSR)
AUTHORS: Ginzburg, I. I., Rakavishnikova, I. A.
TITLE, The Age of the Weathering Crust in Central Kazakhstan
(K voprosu o vozraste kory vyvetrivaniya v Tsentrallnom
Kazakhstane)
PERIODICAL: V sb: Kora vyvetrivaniya, Nr 2, Moscow, AN SSSR,
1956, pp 321-322.
ABSTRACT: From a study of a brontotherium jawbone (containing
teeth), found in red clays, the authors have concluded
that the weathered layer in central Kazakhstan was
formed no later than the Oligocene, and possibly
earlier. The latest age of nontronite and opal develop-
Card 1/1 ment is no later than Oligocene. Ye. S. K.
Q~_ MAM

15-1957-3-3174
Translation from: Referativn zhurnal, 4~plogiya, 1957, Nr 3.
p 106 NssyR~
AUTHOR: Ginzburgo
TITLE: The Aggrepsio of Water in Relation to Its Movement
Through Rook FTr. note: aggressive water is acid,
limestone-attacking water] (Agressiya vody v svyazi
a yeye dvizheniyem v kamne)
PERIODICAL: V 5b: Kora vyvetrivaniya.' Nr 2. Moscow, AN SSSRv
1956p pp 355-387
ABSTRACT: In order to study the chemical aggressiveness of solu-
tions while they are seeping through rock, experiments
were conducted on 16,samples of limestones and.dolomites
from the Shiryayevskiy and other karlyery (quarries) 9s, the zhiguli
fountains, near Kuybyshev. It was noted that the most
Ughly dolomitized samples are diitingui5hed by variable
composition, attended by fluctuation in the transmissi-
bility coefficient, porosity, size of pores, and so
forth. Chemical, thermal, and petrographic studies in-
Card 1/3

15-1957-3-3174
0
'rho Aggression of Water in Rolution to Its Movement Through Rock
dicate that the dolomite content in the 3amples ranges from a
trace to 96.0%. The chemical analysis is as follows: insoluble
residues 0.05 to 0.38C%O; S102 0.01 to 0.09%; Fe Oj 0.02 to 0.13%;
A12N 0.02 to 0.09%; CaO 33.43 to 55.801/~Q; MgO 8. 9 to 19.63%,;
C08 43.75 to 47.00~L P"3tpo..0.20%; S a truce; 01 0.01 to
0 6%; P~O~ a trace; ~0+*up o d.12~: Si formed 27.87 to
,~A
8;-.95% o he insoluble residues. From experiments on the
seepage of H20, CaS04, and Ca(OH) I It Was ascertainyd that the
coefficient of transmissibility rEges from>l x 10- 0 to
1 x 10-6 for dolomitesAranl x 10-5 to 1 x 10-7 for limestones.
The value of this coefficient depends on the total porosity;
the total specific surface of tqe pores; the size of the pores
themselves; the connection of pores of different sizes with each
-other; the volume of airtight pores; the shupe of the grains
forming the pores; the gradient; the chemical and mineralogical
composition of the pore walls; the thickness of the walls in
thin-walled pores; and the temperature, viscosity, and composi-
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15-1957 -3-3174
The Aggression of Water In Relation to Its Movement Through Rock
tion of fluids migruting through the rock. The factors of time
and pressure also Ini ''luence the c oefficient of transmissibility.
It was calculated that water will pass through approximately
100 m of rock, even if dense, in 13,300 years. With water pas-
sing through. it, dolomite loses 0.0054% of its weight in a year;
limestone loses up to 0.27;~. In 3,300 years, 18% Ca and Mg
would be removed from dolomite; but porous limestone would be
dissolved entirely in 400 years. However, the processes of
solution generally proceed much more slowly because of the pre-
cipitation of sediment from the solution and the consequent
stopping up of the pores, and because impermeable layers, if
present, prevent free drainage. jhus external conditions deter-
mine the results of the struggle between the two opposing proc-
esses of leaching and cementation.
Card 3/3 V. A. V.

GINZBURG, I.I.; MUKANOV, K.M.
~
Fb. Zu and Cu distribution in various classes and fractions
of the Diluvium in the region of two deposits in Central
Kazakhstan [with Inglish summary in insert]. Geokhimiia no.4:
50-57 '56. (MLRA 9:11)
1. Institut geologli rudrWkh mostoroshdaniy, petrografti,
mineralogii i gookhimii Akadenii nauk SSSR. Moskva.
(Kazak~stan--Geochsmistry)

USSR/Cosmochemistry Geochemistry. Hydrochemistry, D
Abst Journal: Referat Zhur - Khimiya, No 1., 1957, 743
Authors Ginsburg, L I.
Institutions Academy of Sciences USSR
Titles Geochemical Methods in Ore Prospecting
Original
Periodicals Vestn. AN SSSR~ 1956, No 61 58-64
Abstract: Geochemical prospecting methods based on the analysis of a large num-
ber of small samples containing trace amounts of the elEments of in-
terest require a quick and accurate methodology. Semiquantitative
spectroscopic analysis is of great importance in this respect.
Further progress in geochemical prospecting must be achieved by the
utilization ofone sample for the determination of 6-10 and wre
elements. Geochemical, bydrochemical,, biochemical, and geobotanical
prospecting methods are -finding wide application. For complex in-
vestigations the creation of integrated prospecting teams and field
laboratories is necessary. For the preliminary survey of large
Card 1/2

PHASE I BOOK EXPLOITATION 646
Ginzburg, n,ya Isaakovich
Opyt razrabotki teoreticheaktkh oanov geokhimicheskikh metodov poiskov rud
tsvetnykh I redkikh metallov (Experience In the Development of Theoretical
Principles for Geochemical Methods of Prospecting for Nonferrous and Rare
Wtals) Moscow, Gosgeoltekhizdat, 1957. 10,000 copies printed.
Ed.: Smirnov,, V. 1. Ed. of Publishing House: Godovikov, L. A. Tech.
Ed.: Gurov., 0. A.
PURPOSE: The book is intended for practical and theoretical exploration
geophysicists specializing in geochemistry.
COVERAGE: The book covers the entire field of geochemical exploration and reviews
both the recent methods of chemical analysis of rock (or Boil) and the peculiari-
ties of geology of individual mineral deposits, essential for practical prospecting
work. Each method is described in its teleological aspect. The material for
conclusions as to the methodology was partially supplied by the author himself
and partially extracted from the reports of leading Soviet geochemical
eXplo rs and from the records of the All-Union Congress of Geochemists (1956).
Card Vige

Experience in the Development (Cont.)
646
Acknowledgment Is extended to the following Soviet scientists (from the
geochemical laboratory staff of the Academy of Sciences, USSR) for their
contributions: I. A. Rukavishnikova, L V. Vitovskaya, V. V. Borodin,
Yu. Yu. Bugellskiy K. M. Mukanov, L. D. German, A. 1. Pokrovskaya (an
anAlytical chemists, and N. P. Sechins. (a spectral analyst); furthermore,
-the following scientsits have contributed their material to the author:
S. D. Miller, 1. P. Benivalenekly, G. L Rossman, and A. G. Betekhtin; in
addition, the following scientists have reviewed the book: 0. D. levitskly,
F. L Vullfaon, and V. M. Kreyter. In the introduction to the book, the
author recapitulates the main achievements of Soviet geochemistry in the
field of petroleum and metal prospecting by geochemical methods. Folloving the
decree by the Ministry of Geology in 1955, the geochemical element has beccime
an integrated part of every geophysical and geological prospecting scheme. Each
chapter Is accompanied by an extensive bibliography, consisting almost entirely
of Soviet contributions. There are 328 references, 317 of them Soviet,
8 English, and 3 German; and 72 figures (mostly diagrams) and 28 tables. The
appendix, written by A. I. Pokrovskaya, contaIns a summary of practical
geochemical methods used in sample analysis for determining the presence of
metal in rock. In the conclusion it must be mentioned that the term "hypergene"
(supergene) has a broader meaning than one given to it in the American scientific
literature. In this book the term "hypergene" includes all relevant ore-formation
processes.
Card 2/16

lb,Terience in the Development (cont.)
TA13LE OF COMENTS:
646
(Rote: There is a ceitain discrepancy betveen headings in the Table of Contents and
those in the text. Information in brackets is added to clarify the text]
Fore,iord
Introduction
3
5
History of geochemical exploration in tJSSR 5
Geochemical prospecting outside of USSR 7
Slime analysis in geochenical prospecting 8
Development of prospecting methods - physical, physiochemical,
chemical, biochemical, etc. 8
Connection betveen geochendcal prqspecting and geological surveying;
integrated (combined) character of operations 10
Contributions of geochemistry to prospecting 11
Card 3/16

Experience in the Development (Cont.)
646
Ch. 1. Methods of Analytical Geochemical Prospecting 13
Spectroscopic method 13
Qualitative chemical spot test and powder method 15
Colorimetric method; comparison between chemical and colorimetric
methods 15
Phase analysis (Analysis based on differences in solubilityl 20
Electrodialysis 21
Water analysis; other methods 21
Selection of proper method of analysis 22
Ch- II. Geochemical Indicators (of the type of deposit] 24
Chemical elements in the role of Indicators 24
Trace elements In the crystal lattice serving as indicators 28
Minerals in the role of goechemical indicators 29
Selection of proper indicators 33
Geochpmical correlation of elements (paragenesis) 34
Factors on which geochemical indication is based 3T
Card 4/16

Experience in the Development (Cont.) 646
Ch. III. Metal Concentrations in Eruptive and Metemorphic Rocks 38
Geochemical bazis of concentration and dissemination (dispersion) of
chemical elements in rock 38
Ability oV ekmnats to disseral nate and concentrate 39
Permeability of rocks and metal concentration in them 41
Concept of dissemination halos 44
Connection between the contour of dissemination halos and the
strueture of deposits 45
Features of metal distribution in original rock; metal distribution in
contact rock enclosing the halo 46
Mineralization of metal ore 48
Mineralization of "sterile" metal ore (nonconcentrated ore] 49
Trace elements in the, crystal lattice of minerals 52
IYI.Pseminsted mineralization 54
Syngenetic and epigenetic dissemination 55
Enriched metallic mineralization 58
Kneralization of halos. Indices of mineralization 6o
Forms of mineralized areas, their size and extension 60
Card 5A.6

*eeience in the Development (Cont.) 646
Ch. IV. Concentrations of Metal in Sedimentary Rock 69
Cond-ttions inducing concentration 69
Transportation of sedimentary materials 70
Cond-itiow. of deposition and transportation of metal-bearing sediments 72
Stages of sedimentary ore formation 77
Penetration of solutions into the rock strata and its influence
on urar-lum content 78
Metal content in sedimentary rocks 79
Stratification of metal ore concentrations in sedimentary rocks 80
Deposits formed by sed-Lwntation 81
Metals in coal ashes 83
Correlation of individual e2ements and types of their occurrence 83
Ch. V. Prospecting in Bedrock 86
Effect of "hypergenic" ore-forming processes on the changes in metal
content in bedrock 86
Importance of metal-impregnable rocks 87
Hypergenic migration of metals into metal-impregnable rocks 87
Conditions effecting the stage in development of areas of mineralization 87
Correlation problem in hypergenic zones and in original rocks rjL
DILasemination of high-mobility elements and their ccapoun&
in original rock 98
Gec-chemical prospecting for sedimentary rocks 101
card 6/ 16

Experienne in the Development (Cont.) 646
Ch. VI. Prospecting for Blind Deposits (Underground Prospecting) 103
Search for ore in sedimentary rock under alluvial blanket 103
Search for blind ore in original rock 104
Rock structure as indicator of deposits 104
Zonal arrangement of ore and stages (steps) of hydrothermal processes 105
Behavior of metals embedded in or in contact with ore body and the
extent of their dissemination 1o6
Importance of eroded surface in searching for blind ore bodies 3-10
Symptmw of possible mineralization; tests in
Interpretation of results of geochemical prospecting 118
Conclusions 119
Ch. VII. Yetal Concentrations in Loose Rocks Covering the Halos of
Mineral Dis~emination 122
Halos of dissemination 122
Fa.:tors and processes effecting the formation of dissemination halos 123
Present-day erosion and soil formation 124
Behavior of individual elements in soil (copper, lead, zinc, cadmium,
molybdenum, tin, arsenic, selenium, antimony, tellurium, gold, silver,
nickel cobalt, barium., strontium,, boron, fluorine, other elements) 125
Card 7/ ~7'

Experience in the Development (Cont.)
Ao-cumulation of ininerals depending on the interplay of soil and
646
climatic conditions 134
Metal content in dissemination halos 135
Metal belaw the water-table stratum 135
Importance of the composition of ground air 135
Ancient erosion 136
Absorption of solutions by roorts of plants 138
Mineralization of decayed vegetation 139
Capillary extraction of underground water and its natural
evaporation (by sun) 140
The role of capillary extraction in and regions 141
Impact of irrigation on concentration of metals 143
Problems of the uptake of deep-seated water-soluble salts 144
Diffusion of gazes by heat 144
Ionic diffusion 144
Importance of electric currents [in dissociation processes] 144
Ascending (Pressure) waters and their role 145
Oxidation (of sulfides and of lower oxides of metals) 148
Leached and weathered zones 154
Ydneral composition of oxidation zones; ferroginous outcrops (gossans) 1-55
Card 8/ 16

Experience In the Development (Cont.)
646
Erosion of soil crust and of oxidation zones
Porcesses of mechanical transportation
Formation of zones and streams of dissemination (of rock fragments);
bottom sediments; eluvial processes; pseudo-halos of dissemination
Search in eluvial and alluvial formations
Coagulation, sedimentation and absorption
Genetic types of dissemination halos
Shapes of dissemination halos in blanket deposit
Interpretation and evaluation of dissemination halos
Ch. VU. Surface Prospecting in Blanket
Depth of the test pit
Size of rock samples according to type
The weight of rock sample tested
Slime and spectroscopic analyses
Selection of proper method of test pit
Cases of "pseudocontamination" of rock
minerals in rock samples)
Search for lead
Card 9116
Deposits
of rock
analysis
[incidental occurrence of
157
158
159
164
165
168
169
171
174
174
175
176
177
177
178
178

kgerience in the Development (Cont.)
Search for zinc and cadmium
Search for silver
Search for copper
Seaxch for molybdenum
Search for tungsten
Search for tin
Search for gold
Search for nickel, cobalt and chromium
Search for fluorspar
Search for heavy spar (barite)
Search for lithium
Some practical advice; conclusions
Ch. IX. Metal Migration in Water
Hydrogenic elements
Mineral solubility and hydrogen-ion concentration
Forms of metal occurrence in water
Metal content in water of different origin
Factors influencing metal content in water; the importance of the
pH factor
Degree of sulfide oxidation and its importance
Water exchange processes
646
179
181
181
186
187
189
190
191
193
193
194
194
197
197
197
198
199
202
202
204
card ao/16

Experience in the Development (cont.)
646
Features of sulfide distribution in sulfide-bearing rock 204
Climatic conditions (and their impact on metal concentrations);
impact of water-bearing rocks (aquifers) 205
Concept of migration coefficients 206
Migration of metals In water 206
Metals in swamps 208
Degrees of dissemination of metals in water 209
Behavior of Udividual metals in water and some other chemical elements
or their ccepounds P-10
Lead 211
Zinc 212
Silver 213
Cadmiun 214
Bixmuth 215
Tin 215
Molybdenum 216
Vanadium 217
chromium 218
Card 11/16

Experience in the Development (Cont.)
Nickel
Cobalt
Arsenic
Mercury
Uranium
Antimony, selenium, tellurium, phosphonm
Germanium, gallium
Beryllium
Titanium
Scandium
Barium and strontium
Ions of sulfuric acid and of cblorine
Fluorine
Boron
Analysis of water extracted from rock
Determination of the pH of water
646
219
219
220
2W
220
221
221
221
221
221
221
222
223
224
225
225
Card 12A6

A
Experience in the Development (cont.)
646
Ch. X. Hydrogeochemical Prospecting for Metals and Characteristics of Water
for Various Types of Deposits 227
Determination of features of dissemination 2ZT
Prospecting in closed and open areas 227
Consideration of factors causing an increase in metal content of water;
classification of waters in mineralized zones of West-Siberian mountains 229
Water In copper deposits and Its features 232
Water in pyrite deposits 235
Water in multimetellic (complex nonferrous) deposits 237
Water in deposits of rare metals 238
Hydrochemical methods in permafrost areas 238
Determination of total isotopic composition of water and its importance 238
Gas analysis as a method of prospecting; orther methods 239
Ch. IX. Biogeochemical Prospecting Method 241
Theoretical foundations and practical application of biogeochemical methods 241
Metal content in vegetation ashes 242
Absorption of metals by different plants 244
Card 13/ 16

Experience in the Development (cant.) 6V
Search for sulfides of copper and iron 245
Search for nickel, cobalt and chromium 245
Search for copper 247
Search for zinc and lead 248
Search for molybdenum 249
Search for uranium 250
Search for other elements 251
Practical advice on methods; conclusions 251
Ch. XII. Geobotanic Prospecting Method 253
Theoretical principles 253
Types of indicator plants (growing on soil rich in particular metalsi 254
Teratological factors (indicating structural peculiarities);
metallophillic flora 255
Factors indicating the presence of copper, uranium, and selenium; examples 256
Vegetation blanket as an indicator of lithological composition of rockY
hydrogeological conditions and tetonic rock structures 259
Aerial geobotanic prospecting 26o
Card 14A6

Experience in the Development (Cant.) 646
Ch. XIII. General Conclusions on Geochemical Prospecting 261
Geochemical map-making and types of maps 261
Topomineralogical maps 261
Geochemical maps proper 262
Geochemical prospecting in bedrock 263
Objectives of prospecting 263
Types of geochemical map of bedrock 265
Geochemical prospecting in blanket sediments 265
Prospecting in an open area 265
Prospecting in closed slightly broken areas 267
Prospecting in closed deeply-broken areas 267
Prospecting in wooded and swampy regions 267
Importance of auxi3tary methods: hydrochemical, biochemical, bartanic, etc. 267
Drilling for map-making 268
Types of metallcmetric survey 268
Selection of proper method and interpretation of geochelmical
prospecting data 269
Card 15/ 16

Experience in the Development (Cont.)
646
Distortion in position (site); forms of bmwds; marking the halos of
mineralization. Application of geochemical exploration methods in extreme
North-East. Selection of proper scale in mapping a deposit. General
conclusions 270
Appendix
Simplified method of assaying lead, copper, wolfram, mblybdenum, and
silver in the field 275
Reagents 275
Determination of wolfram 276
Determination of molybdenium 2T7
Determination of silver 277
Setermination of copper 279
Determination of zinc 280
Determination of lead 281
Bibliography 282
AVAILABLE: Library of Co S8
Card 16116 MM./bmd
10-34-58

AUTHOR: Ginx'iurg, I.I.
TITLEt Basic Results of Study, of-Ancient Cores of Weathering in
the USSR (Oanovnyye rezultaty izuchenilya drevnikh kor vyvetri-
vaniya v SSSR)
PERIODICAL: Izvestiya Akademii Nauk SSSR, Seriya Geologicheskaya, 1957,
# 12, pp 61-88 (USSR)
ABSTRACT: Studies of disintegration of mountain rocks were taken up
more than 20 years ago by B.B. Polynov and other geologists,
and they were continued in 1938 by D.T. Ullyanov, G.S. Gritsayen-
ko and other USSR scientists. Examinations of the effects of
disintegration of the earth's crust were brought about by
prospecting for nickel, aluminum, iron, mangan, kaolin, heat-
resisting clays, zirconium, titanium, diamonds, optical quartz,
rare earths and other minerals depcrsits associated with rinds
of disintegration. It was found that the occurrance of these
rinds was not restricted to regions of the southern Urals and
Ukraine, but that they were distributed over the entire terri-
tory of the USSR. Ancient rinds of disintegration proved to
be of such importance that it seemed justified to establish a
new branch of geology, specializing on the pecularities of
Card 1/3 these geologic formations and the methods of research. At the

11-12-5/10
Basic Results of Study of Anoibnt'Cotes of Weath6ring in the USSR
present time ancient rinds of disintegration are regarded as
a special continental formation, which has been formed under
the influences of solar energy, atmospheric and biogenic
agents acting upon basic rocks of different composition. As
a result, new layers with different structural, and chemical
properties were formed containing mineral deposits typical for
disintegrated rinds. Following extensive studies of rinds
of disintegration, the following 7 types of rinds were estab-
lished: 1. Residual rinds of decomposition; 2. Residual
rinds of leaching; 3. Rinds of filtration; 4. Rinds which
were transformed by new processes of disintegration, deposit-
ed on the initial rinds; 5. Re-deposition or shifting of the
rinds; 6. Washed-out rinds; 7. Metamorphosed rinds. Each
of these types can be subdivided, depending on the properties
of the disintegrated rocks as well on the form of deposition,
into the following groups: open and covered rinds; plain and
complex rinds; rinds covering square areas and those covering
strips; widely dispersed rinds and those of local distribution.
The author published 7 tables, on which are given the character-
istic features of disintegration, leachin6, filtration, re-
Card 2/3 deposition, transformation, washing-out and the development of

11-12-5/10
Basic Results of Audy of Aneivat-Veres of Weathating :Ln the USSR
profiles of rinds. The method of determining the age of rinds
has not yeat been settled. 'It is a rather simple matter to
determine the age of a rind which is overlaying or which is
covered by a known formation. The author cites numerous
rinds of disintegration deposited in various geologic strata
of the USSR. He examined furthermore the correlation existing
between ancient rinds of disintegration and sedimentary de-
posits found in depressions, as well as the influence of
climatic conditions prevailing at the time of formation.
There are 8 tables, 68 Russian, 1 British, and I American
references.
AVAILABLE: Library of Congress
Card 3/3

GIITZBURG, I. I.
"Types of Old Crusts of Weathering in USSR."
paper distributed at the International Clay Mineralogy Congress in Brussels, Belgium,
I - 5 Jul 58.
Comment: B-3,116,859.

AUTHOR: Ginsburg, 1.1. 11-1-23/29
TITLE: Conference on the Research and the Use of Clays (Soveshcha-
niye po issledovaniyu i ispollzovaniyu glin)
PERIODICALi Izvestiya Akademii Nauk SSSR, Seriya Geologicheskaya, 1958,
# 1, pp 110-111 (USSR)
ABSTRACT: The first conference on research and use of clays was held
in Llvov from May 26 to June 1, 1957. This conference was
called by the Llvov State University imeni Franko, by six
institutes of the Academy of Sciences and other scientific
organizations. It was attended by 250 scientists. The
following problems were discussed with more than 100 lectures:
1. General questions on the mineralogy of clays. 2. Methods
of mineral research and special properties of clays. 3.
Engineering-geological properties of clays and minerals. 4.
Study of clays and soils of different districts. 5. Techno-
logy of clays. 6. Results of studies of bentonites, bauxites,
loess and erosion of the earth's crust. The lectures dealt
with problems pertaining to the nomenclature of mineralogy,
heating and dehydration curves, thermic effects, X-ray ana-
Card 1/2 lysis, mineral composition, technological properties, genesis,

Conference on the Research and the Use of Clays 11-1-23/29 j
classification and other characteristics of clays.
AVAILABLE: Library of Congress
Card 2/2

e 0 lo i-~ Cal Ln ncralo ~CLI
-lz'I;Or-at'or' 0: 1':eoret,'Cid Laje., oi*
by Q, of
'kilo.

GINZBURG, I.1
Committee of the AcademV of Sciences of the U.S.S.R. on the
study of clays. Geol.rud.nestorozh. no.1:127-128 Ja-F 159.
(NIRA 1215)
(Clay)

GINZBURG, LI
Hickeliferous magnetite In silicate-nick6l depogits. Kora,
vyvetr. no. 3:33-38 160. (MIR& 13:12)
1. Institut geologii rudnykh meotorozbdeniy, petrografii.
mineralogii I geokhimli AN SSSR.
(magnetite)

GINZBURG, I.I.
"Nickelmelane" and mcobaltmeland". Kora vy-vetr. no. 3:56-66
l6o. (MIRA 13:12)
1. InBtitut geologii rudnykh mostirozhdeniy. petrografii,
mineralogii i geokhim!i AN SSSR.
(Pailomelans)

,QjHZBU3G,--I--L-,-A, KUANOVA, Te.S.
Silica content in natural waters and forms of tts occurence.
Kora vvvetr. no. 3:313-342 16o. (MIRA 13:12)
(Silica) (Water--Compoeition)

GI11ZDURGj_L,,T; OLISHANSMY, Ya.I. [decoanod]; BZI,YATSK-TY ) V.V.;
Prinimali uchastiye: 11MUDENOVSKAYA, T.S., laborant;
ROUDESTWENSKAYAl Z.S. , laborant; KOZHINA, V.M., laborant;
Y
FEODOTIYEV, K.M., otv.red.; SHLEPOV, V., red,izd-va; LAUT,
V.G., tekhn.red.
43ftaiem.of experimental and technical petrography and mineralogy]
issledovaniia po eks erimentallnoi i tekhnicheskoi petrografii i
tudios on oxidation of sulfidos] 'Asor-,ri-
iaineralogii. No 4: fS 1,
montallr,w isoledovaniia po okisleniiu sullfidov. Maskva,
Izd-vo Akad.nauk SSSR. 1961. 130 p. (Akademiia nauk SSR.
Institut geologii rudynkh nestorozhdonii, petrografii, mineral-
ogii i gookhimii. Trudy, no.59) (MIRA 11,:7)
(Sulfides)

GINZBURG I.I.
Basic problems relative to the study of the formation of weathered
surfaces and their importance for mineral prospecting. Geol.rud,
mestorozh. no-5:21-36 S-0 161. (MIRA 14:9)
1. Institut geologii rudnykh mestorozbdeniy, petrografti,
mineralogii i geokhimii AN SSSR, Moskva.
(Weathering) (Minerals) (Prospecting)
I
ALITGAUMN) M.N.; GINZBURG I.I. - DUBOVSKAYA, M.V.; URSHOV) A.D.;
MKOV, ROZHKOVA, Ye.V.; STIRAEBOV, N.M.;
KHRUSHCHOV, N.A.; SHMANECHKOV, I.V.; SHCHERBAKOV, D.I.;
YANSHIN, A.L.; AILIRASLANOV, A.A.; GOTMAN, Ya.D.; ZUEMV, I.N.;
KOROVYAKOV) I.A.; ORLOVA, P.V.; PASOVA, F.G.; SAAKYAN, P.S.;
TFMNT'IEVA, K.F.j SHANOBSKIY) L.M.; CHERROSVITOV, Yu.L.;
SHCHERBINA, V.V.
IUrii Konstantinovich Goretskii; obituary. Sov.geol. 4 no.12:
153-155 D 161. (MIRA 15:2)
(Goretakii, Iurii Konstantinovich, 1912-1961)

NIKITIN, Nonstantin Xonstantinovich; otv.red.; ASTROVI
A.V., red.izd-va; KASHINA, P.S., tekhn.red.
[Ancient weathering surface of ul*abasic rocks in the Buryktal
Massif] DrITiaia kora vyvetrivaniia Buryktal'skogo massiva
ulltraosnovnykh porod. Moskva, Izd-vo Akad.nauk SSSR, 1962.
189 p. (Akademiia nauk SSSR. Institut geotogii rudnykh mestorozh-
denii, petrografii, mineralogii i geokhimii. Trudy, no.69).
(Ural Mountain region-Weathering)
(Ural Mountain region--Ultrabasite)

Vladimir,-wria; GIN',- a
l0bulij,'I'L , ,
DROD'~K-T.(, S), A. rind, izil-vil; SUSHO., L,A, , 6'~-nn. 'red.
(Mineral and beh,17ior of ir, -7,,e mlper-
gene zone of Pkpbau-.rl i.And K~fzy!-Espfl Mineralinyi sostav i povedeni6
mLki-celementov v zone gipergeneza Akciiagyla i Kfzyl--Espf-. Moskva,
Alad.n3ul, SSSR, 1962. 121)
:-ud-
ziykh mestoroz~.denil., p~-trografii, :,;inerilot;i i
i tferAhimij- Trudy, (MIRA lr;6)
(KaLaklistan-Ure deposlLs) (Kaviklist-m-Tracp elements)

GINZBURG, I I - NADZHAYOVA, G.E.; NIKITINA, A.P.
Recent and ancient laterite weathering of basalts in Brazil
and the Russian Platform. Kora vyvetr. no.4;3-95 162.
(MIRA 15:9)
1. Institut geologii rudUkh mestorozhdeniy, petrografii,
mineralo, i.1 i geokhimii AN SSSR.
lBrazil--Weathering) (Brazil--Basalt)
(Russian Platform--Weathering) (Russian Platform-Basalt)

--UNZBURG. I.I.; PISEMSKIY, G.V.
L_~.
Weathering surface of rocks of the greenntone formation in
the Uchaly pyritic copper deposit. Kora vyvetr. no.4:147-
177 162. (MIRA 15:9)
1. Institut, geologii rudnykh mestorozhdeniy, petrografii,
mineralogii i geokhimii AN SSSR i TOIGRI.
(Ural Mountain region--Weathering)
(Ural Mountain region--Greenstone)

VOLIFSON, F.I.- GINZBURGI I.I.; SAPOZHNIYOV, D.G.; SOKOLOV, G.A.;
YANI A. L-.
Eightieth birthday of B.P. Krotov. Geol.rud.mestorozh. no-59117-
3-18 S-0 162.
'141RA 15:12)
(Wrotovp BDria Petrovich, 1882-)

The Ccnference on applied karatology
PERroDrCAL, rzvestiya Akademil nauk SSSR, Sarlya giologIchaskayA, no, 1, 1963,
124 - 126 (Wthorml- Gvozdotak:Ll V. A., =4 Cb1kisbay, A. G.)
TEXT- The Conference was hold in Moscow on 1pr-ft 23 - 25, 1962, and was
attended by 35 representatives from 16 acientifictl and industrial organizations.
The Conforence was opened by N. A. Ovozdatakly who reported on the actlvltlea of
the Geographical section of the Moscow Society of Natural scientists. The follo%(7
Ing reports were dellveredi A. 0. LykoshIn on the investigation of karats for
hydro-engineering construction by geological eng!,neeral V. S. Polevoy on the use
of geophysical methods to study karate in areas .if hydrological engineering struo-
turea; I. A. Savarenakly on problems considering karate In industrial and urban
_
_
_
_
_
-
constru
a
t
io
n
fn
thoDzerzhinak region; N. A. Ovozdetakiy on "Karat in the region
of Caucasian Mineral Water Sources"; I z Ap on mineral resources connected
-
tf
b
ii and phosphorite karat depositaj
hinek y on bauxite
with karat processeal 9,
1. Rua ry n
-
Y_eT_ _Bobrov_on "Karat bauxites of the Yoniney ridgi and the adjacent region of
the Siberian platform"; 4N A Lisit
1~ I 3Zna on "Karat bauxites in the Kazakh foldings
and the Turgay depression
B. N.'Ivanov and V. N. Dublz2paski an "The importanc4
of the Crimea karat In national edonomy-; on "The importance of
the Central Ural karat In national economy"j I. K. Kudrya8hov on the Influence of
karat on agriculture In some Baahkirian regio6ei The-reports delivered were dis- i
cussed by D. S. Sokolova, V. A. Varsanof'yeva, N. A. Kraall'nikova, S. A. Slad-
kopevtseva, V. S. Polevoy and others. The Conference approved the methods of
karat investigation, including geophysical means, electrical seismic and ultra-
sonic prospecting. It was decided to Investigate In detail the development am
expansions of karat; to study the origination of karat bauxites, to control the
purity of mineral water sources and to continue research in the agricultural re.
gions of Bashkiria.

GIIiZBURG,-Ial,.--
Reaction energy of weatbering processes of some aluminosilicates.
Kora vyvetr. no-5:87-119 163. (MIRA 16:7)
1. Institut geologli rudnykh mestorozhdonlyp petrografti,
mineralogii i geokhimii AN SSSR.
(Aluminosilicates) (Weathering)

GIUBURG, 1. 1 .
Orf-m~7-t,,kjr, of' geoch~,vii(,-al for I,y:-Ifi~-,
in the ';oiahorn Ur 4a.,3. 0.0, -:-. gool. -1 pcl~ iskop. IlIzh,
no. 1-2~~-36 1(j,, (m, I I f, r - 7 1,

SAUKOV, A.A.; GINZBURG., ;J,; PERELIMAN, A.I.; AYDINIYAN, N.Kh.;
,"' TIC ~
SHARKOV ,Vo -'
Vladimir Ivanovich Krasnikav; obituax7. Geol. rud. mestarozh.
5 no.2q.141-142 Mr-Ap '63. (MIRA 16:6)
(Krasnikov, Vladimir Ivanovich, 19(Y7-1962)

BERKHIN, S.I.; VITOVSKAYA, I-V.; GINZBURG, I.I.
Montmorillonite contairring admixtures of halloysite, from the
oxidation zone in the Mysyl-Espe deposit. Kora vyvetr. no.5:
7-16 163. (MIRA 16:7)
1. Institut geologii rudnykh mostorozhdeniy, petrografii,
mineralogii i geokhimii AN SSSR.
(Kazakhstan-Montmorillonite)
(Uzakhatan-Ralloysite)

i. F.
v I NZ BURG y
anclent weathering surfaces, forms of their
Ty-pes
occurrence and classification. Kora vyve+.-r. no.6a7l-101 163.
(MIRA 17:9)
ykh montnronhdonty, potrogrrifil,
1. ',nsi.Utit goologii rudn,
mjneraj+ogj.j .1 genk",orpli, AN Mntikvyi.

R.S - GDZBURG Lie
YASHINAV of - Is method
Checking on the use of O.P. Mehrat and M.L. Jackson
of the removal of iron OridOB from soils and clays for
mineralogical purposes. Kora vyvetr. no.5:398-403 163.
(MIRA 16-7)
1. Institut geologii rudnykh mestorozhdaniy, petrografii,
mineralogii i geokhImii AN SSSR.
(Mineralogical chemistry)