SCIENTIFIC ABSTRACT GINZBURG, I. - GINZBURG, I.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R000515120017-9
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: September 26, 2002
• Sequence Number: 17
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

Asymptotic Behavior of the Matrix Elements in the SOV/155-58-2-33/47
. Two-Charge -Meson Theory
There are 6 figurest and 5 references, 4 of which are Soviet,
and I Italian.
ASSOCIATION:Matomaticheakiy institut imoni V.A.Stoklova (Mathematical
Institute imeni V.A.Steklov)
SUBMITTED: March 1, 1958
Card 2/2

GINZBMIGI I.F.; SFMBRYAKOV, V.V.
Electromapetic corrections to weak interactionse Zhur*
okep. i teor. fit. 40 no.6:1738-1745 Je 161. (KIRA 14:8)
1, Institut matematiki 43 Vychislitellnym teentrom
Sibirskogb otdoleniya AN &SSR.
Ta6Ctv%ag"tic theory)
tlear "actions)
St-

~ .1
GINZBU.,iG, I.F.; K;,KCIVA, V.J., red.
11.1 .11 1.. -
(InelastJc, interactiono between hilgh-enert,~v particL-,i lrA
reziormahzinf..,, theorles of strong interaction.,31 N'ouprusyie,
v2aimociei.,tviia chastits vyookikh enorgli v renovmlniei-,~7kh
teoriiakh vzni,-,.ode4'stvH. 111-t 11:.'i-
turiAlki ~4) llj~ 19o". P 1. .

S/05 63/044/002/020/065
BI 02XBi o6
AUT E'021: Ginzbur.-, I. F.
T! T L-'-' ~.nelastic interactions of high-ener.-y particles in
renortualized stront;-interactiori theories
Zhurrial eksperimentallnoy i teoretichesl4oy fiziki, v. 44,
no. 2, 1963, 500-515
T iWl'. A :.~:t~thod i:5 developed for analjzing hit;h-ener6y 3tronc: interactions
in Lhoories. The Diethod is based or, a re:,,resentation of the
commoi. propvrti,s of these theories, such as those given lby N. N'. Boj;olyubov
and D. 7. (Vvedeniye v t,?oriyu kva,-,tovannykh poley - Introduction
into quaxit~,~;:. fuvld thoory, Goste.,,.!;izdat, 1957), an-I an ex ansion cf the
Green functio.-.r, anal the differential crous-sectiona for illo I ast do
procesavu in tt series of the reciprocal enerjy 1/s, taken as the
811jall para MC,. 4, 1. )2 . m2+~,2
(k +p +21, E, a t F~rst the author
0 0 0 0 0
investiaat~~ the kinematics of the inelastic processes considered for
a --~ co; these processes are divided into two cases accordinE; to the type
Card 1/3
r
r

Inelastic interactions of ... BIG2/BI66
of momentum, transfer between the fast and slow (kj particles
characterized by I pi-po ;l i1a 1 p U1~s-l -u > 0 and
- 1 , 8400
(2' im 11) 1! S 0. In the following single case (1) id investi,--ated.
0
0-~00
All graphs of '~hq perturbation theory Lire subjected to a classification
and are dlivided into a finite number of diagrain groups characterized by
certain topiAot,:JeB. It is shown that the contribiitiono of all of
a diven to the Green function are equal in first mpproxii.;z,tion.
2ur a comparison of the importance of 1;ra,)hs of a 6ivt-,n to:oL-)j;y it is
therefore ,-off.icient to compare the 6raphs of this class wh:)Se hi6L-cnergy
parts correspond to the first nonvanishine perturbation-thcoretical
approxii.,at i on. For this the well-known method of generalizad &!raphs is
applied. This Methol, is also used in what follows for comparin8 the
importance of Liraphs of different topologies. It can be shown t"at in
the limiting case a -t oo , graphs of a Certain def initt! topology make the
main contribution to the Green function in the process. This topology
corresponda to the exchange of one or a few particles between the fast
Card 2/3

S/056/63/044/002/02o/o65
Inelastic interactiona of ... B102/BI86
and the slow Groups. The region of applicability is shown to exceed that
for the usual pole theory of periphoral interactions. There are 3 fi,~ures
and I t~,ble.
Assck"I'V21ON: Institut matematiki a vychislitellnyr.-i tsentrom ")ibirakogo
ottle'laniya Alkadenii nauk SSSR (Inatitute of -athematics with
Co,;ipoterine, Center of the Siberian Branch of the ;,cademy of
S,--ionces USSR)
SUBlUTTE-J); !;aW 5, 1962
Card 3/3

GIIIZBURG, I.F.
Inelastic intemetions of high-energy particles in
renormalized strong interaction theories, Zhur. eksp. i teor.
fiz, 44 no.2000-513 F 163, (MIRA 16:7)
1. Institut matematiki. a vychialitellnyn tsentrom Sibirskogo
otdeleniya AN SSM.

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AUTHOR: jtepanov, G.M.; Girizburg, 1.1.
TITLE: Some Methods of ~'tandardizing Electric Power Consumption in
Depth-Pumping Oil Production (0 nekotorykh mptodakh normiro-
vaniya elektropotrebleniya pri glubinnonasosno~ dobyche nefti)
PERIODICAL: Energeticheskiy Byulleten', 1958, Nr 7, pp 1-7 (U65R)
ABSTRACT: The authors discuss K.N. Kulizade's article on methois 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 Kulizade's experimental findings
with the results worked out from hin forinuln (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 offic6s of Orgenergoneft' and O.P. Shishkin's

00-58-7-1/6
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 212 1. Electric power-Consumption 2. Oil industry-Applioations
3. Mactric power-Ztandards

GINZBLRG,-I.I.,.Inzh.
Two wires and pipe svstem for the electric power supply
of an electric bit. Prom. energ. 20 no.11:49-53 N 165.
(MIRA 1811l)

GINZBURG, I.
Oct 1947
*rA*":PW*MMO Of the 7104 In the NOW FIT~-TOW
Plan.,* 1. GWburgj, L. hrotekly, 5 pp
"Mrskoy Flot" No 10
Issue of the gools sot for the merchant fleet In the
1946 - 1950 Me-Tear Plan. Present equlpmt Is to
be ame, *=plvt*4 Utilizedp Operations expolted.,
ad now Mlpmt Is to be added to carry out Us
Plan,

GINZBURG, I
lim/Sh4w ~. R"40~ out 107
ONO%
Nap of De4rowing the Cost of Ship Repairs," 1.
Oluburg, A. Syrmsyp 4 pp
Om"kew Floto No 10
OwIdefration Is given to the varims expenditures I&
Ob4 repairUW and the means and possibilities or do-
ftw~*slmg them In order to out the very heavy expense
b*wred in this wak.
b 30T"

?UW3XIT, L.; GINEDURG, I.
--`
TUrty years of saa transportation. Mor.flot 7 no-11:5-10 1 147.
(Shipping) (Ships)

GiNvURG, 1.
Ummerawt noot ".0410 Doo 1947
"The Maritime ?loot on the Inoreaos, 1. Ginzburg,
Q'L. Turetskly, 31 PP
"Morskoy Flot" No 12
Maritime fleet has exceeded norm for first year of
postvar Stalin Five-Year Plan, In 1947, plan had
almost been fulfilled by November, an average of 2rd
Increase over operations for similar period during
1946. sme data, all in percentage figures.
te
i7o6o
17G60

H" 48
shipping
Shiva, cargo,
Tapacity of the Pleat and Reduction Of the Cost
J~Ice of Transportation)" 1. Gintburg and L.
PP
*orskoY Flot' 110 5
Oirat part of series on methods for reducing
t~amsportatlon costs. Discusses effect of
c~P&oltjy of fleet on ictual cargo capacity and
vice per ton mile f4 cargo transported.
lAgm

cost accountine of nopgoing vflp-el
Mo,kve, Mor-Irai transport, 1049. 90 p. (Ile,-"7b55)
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0a 41111104101841 M14 off ita Aj_ 41 a aftusinnuat s i tit I t I
to 00 0 0 0 0 0 0 0 is 0 0 gi 00

T--
17"T I I : 00
Otto U41
L L I
L -00
be
sade III *dj,,0tAFY
. S 'w
801 iptop" INj.UI-
rile"j. '00
7.50 hi, glul Ull I'ApId. Th"e
a fid- IN r
y Slid ge"'i, 'd It tote 4), Al "I so
tr .11 Nell t I.1 4 w
kp it ( It 'j"UtMe. ; " i " 0 0
SRO -It that the,
onted -t that
it is and F, [am the the
'A NI 10 ftorn H
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0 - Po' a
fX1111111
Us
M-i kit a
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: : : : 0 9 06 a a 0
0 0 q o o 0 0 0 0
:

INZBURG I I - BILYARIN D,S., akademik, redaktor; SOLOLOY, G.A., rodaktor.
Mm"=.LL- 0
4
(Geschemistry and geology of the ancient veathering zone in the Urals)
Geokhimiia i geologiia drevnei kery v"etrivaniia na Urals. Moskva,
Iod,ors Akad.naxdc SSSR, 1947. 134 p.(Akademila nauk SSSR. Inatitut geo-
logichookikh nauk. Trudy, no.81). (MLRk 9:7)
(Ural Kountains--Geoehamistry)

j:i
it 1~

GINDURG, I.I.
Ginyburg, I.I. "Protective films on diffused-pulverized silicates and
their posFible technological vignificance in ceramies," in FymDosium:
Syr1yevy,ye resury tonkokeram. prom-stl SSSR J putt ikh Ispollsovantyq,
Moscow-Leningrad, 1948, p. 149-54
SO: U-2888, Letot)ts Zhurnallnykh Statay, No. 1, 1949

GINZIIURG, 1. 1.
A823. 1. 1. O)rrsizovnnio Drr.,inev Eory VyvvtrJvnnJyn lia torij
l7k, Minarnly J lHi "'vopitwi "rudy YuH,(~ynijy LiverIJ, :t,,)jptjjb So
'Dnya it-whoeriiyA -15
M. L., 19h0, F. 201-1r. -- H~ . F, 2 1 h -
SO: Ldtopis' No. 11, 19119

'17r
Ail'
'j,h ;-'4t
tI, t~
31
MI
'At
j I
Jk~ 11 4"~ ii'd itv

C/V
Korautoo. 111,110 38J0 311,0 1 1 (.11J)hwx food I
" I -r-triwirl, t*,*
kuLavWmj%,,.* npiki I , 4,,
~0,10- INIt'll M. 1...t willh.1 , Yu. t, 441mtop).-
KoPf"J"O' 14 IMP(atital ed The gra"Al $rnebst cal mot"tfis cg
the N hroir-oll"'Ate wife- 1; And k duit'n'tjoith
A I-,it, (it , I ".f.ll ,I "'c"hoof
it " tisic. I.." W.". hislwf
$kll..
11k.11 It I-willf,tink
,Oil -tflwltll[R ; it, - if 7
.11 fivAill 1. Alm slinsim 11, Kor'dift M 1. ilk " Ollso .
litc." is u,101Y prinli-11 114114wrtli in Iloilo
vitill 11-mlik"N 21".41 ~' 111IN'litil-lik... lathinwr.
the OlArd'sils, hilf c0lik.1A PI %titistuse is wrly
tywAl, Willi 4 IAIIIC'r 11141,111"1 bilt-flJOStUlt; IN 411411111
i4tts if, n lu%,r j drimitly I.-or -- 1,411-1.494. jud a
1,11rhmirm-r up It .11kii. '%I., AJ.111wil 1.41tillic 1141-
't 1 "'of ol"ol '"'I
")-MV p-aft1v III-of ,w, I Willi jflw
Switad"Id'sillati'lor 1. .11% It I- I-- f ,.If . ilk 4 O'ch,
N1 C..Illrrll. (141011 l-V1fk,lw%.k , 1 111
th"Ittill 14 U 1. wIllt.41 t" I "I J A
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lhn Ill 1, .0.1 till, Imordlo, 1" Ill 11 Ilk
t-tittru jiv o%- -1,4-
mr-11 lob, 11 1, it I I.Ir I,,- qg d%l,-
I#hr tokism *04ilm, , -,4, I-L. hOll-o -it, , -11 Wit
Rk#ltgltl ilk 1"..
41W s 444 Jf-K# -0l- 11. "-il A11 " " 1. , . ~.h lilt. .A
1(41111. ffl~ 1- -11 A I'll - ;'& 14 0 0 1' -l'
1111. uggir-l- cli'l K"". "I, I I" '.. "'J., 4
I tpoill 11. -11 -h
1. fillvil
A L
torlim-h mAk" 'lm. r'O.W. "till
Niff,11111, 1.1-- if 1'.1.4111"1111, juvivi.
T)w .11~jmrfk-,
firl.
.j " 11111 .1 1 If
avilumml A 11 i'l.
ill.. 14 IIIC I r .1. ol'.j It'
still m tor,ile III 01.4t 4, let 1.111 1. "Moll IllAto
1" -tlwlllI.I. . I"k-, (It, It,
,1111l Nits k I I. L. m If. liv

Lr
C.Yf-
1"bigmi of mininjigoolov in the esploitabom, of mithel
deposits connoct~4 vr w"thatt! aust 1 1
I Z Kolill ( .... RVI US. \,, ", -, [IV 101t ~ ,
't1l"IIII: Ill tilt lvi". I,( \I 111.11 Ini"
I 111-1411 A 01411 4 tit Ill i . 1-1 Ill. . 11, oJI111, f,,l is,
0.. if I"1111,10 %I H.-),

1. n1s"m I T- I.; PUrAVTMWFOVA, 1. A.
2. USSR (600)
4. Mineralogy
7. Minerals of veathering of the ancient emst. 1. 1. Ginzburg, 1. A.
Rukavishnikova. Reviewed by I. D. Sedletskiy. Izv. AN SSSR. Ser. geol.
No. 5, 1952.
9. Monthly ~jst Y Russian Accessions, Library of Congress., April - 1953, Uncl.

The I:cmrdttee an SWU Prizes (of the councU or ministers lisa) In the r1e.,ds Qr
science aad inventImm ammoces that the following scientific works, popular sclen-
tift, books, and textbooks have bow submitted for ca"tition For Stma.in Prizeb for
the yeara 1952 raA 1953. a Kultum. Wbcov, &. 212-4,1,, 20 Feb I Apr 1954)
Umm Title of Work
L C"
J: Iv I.,;
C)f
Wadnated by
I !V;0
Acride.,:,y of
W--R~k~4, July 1-954

GINZBURG. 1.I.; SOKOWV. G.A.
rj,;~)Ot~ LA.11-1 1; 1
In connection with the article of V.N.Poddubnyi on "The problem of the origin
of iron ore.* IsveBt. Akad. Nauk S.S.S.R,, Ser. Geol. '5), Ho.2, l1)-14,
(CA 47 no.Z2:12148 '53) (MIRA 6:4)

T1
14
tic
If!
~47
, t.,
rti;
;:LA
v 'it 1.7
!v, fA
*Wig,
f iN
c!:7
V: 11
41 1
1~4
71 -
i-A
W~ kui-i i i
Wo W ILL a fimli 4,

14~
it 1~
quo
fz
;%M ID'
A:; ROM
Kt'
-iftter ad
tb*
Q:
,j:
f

"Difo,miation on 111yof-r,-one Processes in -the Vlorkr, of A. Y-. F-- , n"
m
4 r. !dneral.orich. mizeya A!! SSISSR, 195'), tic, 5, 19-,1,9
The author briefly erpounds the `-asic ideas of 11%. Ye. Fcr.~~m-m in t1c fic-ld
of' h,
per[-Pncsis and their developnent in the works of Smiet, scieni.i,,
1l(! not,,~,!-, the mA Amportant successess in Ow stmly ol' Ili,) o~ hy-
of t1w !'omal lorl (1,i Id"Icrilt, ar a rc-
perpene w tlisrov(- i-
milt. of !1oil fol-flilf- (woric of 11. Pol.-iov and IdS -,.chool), the
Work of A. P. Vinorradov in -vork on crirt and
oy-idalinn zon-:7 (S. f-7,. Snirnov, 1. 7. 1.
.950
No 31 1 'Q
SO: vl-31-1~17, 6 !~-!ar 55-

-----------
USSR/ Cosmochemistry Geochemi6try, K~dr,-,,--hemistry
Abs Jour ReAperat Zhur aimiyrt, No 2, 1957, 4153
Author 91wWww Vitovska.V(I, I.V.
Inst U-11
Title Sokonite in Weathering .11hell. of Lead-Zinc Deposit$ of
Central Kitzakhstan
Orig Pub Sb: Kora vyvetrivaniya. No 2, M., AN SSSR, 1956, 184-187
Abstract First description in central Kazaltstan of the clLycy
mineral, r, vokonite, formeil in ore skarns and skarnic
limestones. Assoclated minerals: montmorillonite,
baddeleyite and nontronite. Chemical composition of the
sck,c)nite (in %): SiO2 38.16, A1203 6.70, Fe 203 2.381
CaO 1.27, MgO 1,19, K20 + Ns'20 0-981 ZnO 34.88, H20-
8.28, E20 +7.52, total 101-36. Structural formula
Card 1/2 - 142 -

USSA/Cosmoc hemistry. Geochemf3try. Hydrochemistry. D
Abs Jour : lief Zhur - Fhimjya9 No. 8t 1957t 2651f2.
Author : Ginburg, I.I., Nikiti
-
-
_
'
' na A A.P.
Inst : Ac
a
of Sc
ience3 of
do
my USSR.
Title i Weathering Products of Some Chlorites
from Mcrainian SSR.
Orig Pub In synposium Kora vyvetrivaniya. Vyp. 21
M., AN SSSR) 1956, 193 - 215.
Abstract The process of alteration of amphlbolized
pyroxenites and pyroxene veins in the complex
of fundamental rocks of the pre-Kembrian
crystalline foundation was studied. The chemi-
cal, roentgenographic, thermal, chromatograDMC,
microscopic and electron-microscopic methods
were used. The process of weathering proceeds
according to scheme: l/ actinolite -4 chlorite
(1)(-nnhi.lte) -)-jefferisite (1); 2/ monoclinic
Card 1/4

USSR/Cosmochpm i stry. Geochemistry. Hydrocho!mistry. D
Abs Jour Ref Zhur - Khimiya, No. 8) 1957, 2)6!1~2.
Ca 0.081 0.03 M92-551 2.67 NiO.04, 0.01,/ (OH 6)
(tO.40H20). Debye crystallograms of I and
Il are also somewhat different. The flormula
of III is 1 3.59 Al 0.41 0 10 [A-1 1.0 FC 1. 0 21
Z/1 7 1 =1
OF.) 0.887 (0H)61-011120
gl.7,Ni The
formula of IV is Si4olo 'Al Fe3-'- 7 (0H)2
L 2.35 0.65/
9 Ni 6. 24S i '). 21" F
o.67 0.02~(OH)6 02+ ) F e203
The formula of V is IS 13.96 Al 0.04~ 010 rAl
z -
(OH) 2 ~11-75 Mg 0.09 Ni 0.005) (01-1)6 t- 0. 99112
The chemical composition of VI is (in I',):
C; ar d 3 /*1+

GINZBURG, I.I.; VITUVSrAU. LV.
Broolon of quartz In hydrous micaosous-montmorillonite clays.
lora vyvetr. no.2:23~-238 156. (mm 918)
(clay) (*art$)

'01 ER,,&JO, VITOVMYA, I.V.
Weathering of garnet, azinitic, and tremolitic rocka in arid
regions of central Kazakhatan. Kors, vyvetr. no.2:299-316 '56.
(KLU 9: 8)
(FAzakhstan--Tremolits)(lazakhmtan--Garnot)(Kazakhatan--Axinits)

15-57-1-579
Translation from: Referativnyy zhurnal, Geologiya, 1957, Nr 1,
p 92 (USSR)
AUTHORS: Ginzburg, 1. 1., Rakavishnikova, I. A.
TITLE: The Age of the Weathering Crust in Central Kazakhstan
(K voprosu o vozraste kory vyvetrivaniya v Tsentrallnom
Kazakhstane)
PER10DICAL4 V sb: Kora vyvetrivaniya, Nr 2, Moscow, AN 333R,
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. Ks

15-1957-3-3174
Translation from: Referativn zhurnal, Osologiya, 1957, Nr 3s
P 106 (USS7H
ALITHOR: Ginzburg, I.I.
TITLE: The Aggrepsiop of Water in Relation to Its Movement
Through Book [Tr. note: 6qresBive water is aoid,,
limestone-attaoking water] (Agressiya vody v svyazi
a yeye dvizheniyem v kamne)
PERIODICAL: V ob: Kora vyvetrivaniya. Nr 2,, Moscow,, AN SSSRj,
1956o 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
f rom the Shiryayevskiy and other kar I yery (quarries) es the Zhigull
0ountaine, near Kuybyshev. It was noted that the most
highly dolomdtized samples are diitinguished by variable
composition, attended by rluotuation in the tranniasi-
bility coefficient, porosityo size of pores, and so
forth. Chemical, thermal, and petrographic studies in-
Card 1/3

lb -1957-13 -3174
The Appression of Water i n Relution to Its Movement Through Rock
dicate that the doloadte content in the samples ranges from a
truce to 96.0111f.. The chemical analysis is as follows: insoluble
residues 0.05 to 0.38%; S102 0.01 to 0.09%; Fe '0 0.02 to 0. 13%;
A120q 0.02 to 0.09%; CaO 33.43 to 55.80%; Mgo 6.i9 to 19.63%,;
C08 ~3.75 to 47 00,~
_;A;qO-,+O V t,0,0.20~6; S a truce; Cl 0.01 to
.r,
0 M O~N to 0. 12~,: 31. formed 27.87 to
6%; Y,: a t ac
BK95~6 0 the insoluble residues. Prom experiments on the
.seepage of H20, Ca304, and Ca(OH) ' it Was ascert6inid that the
coeffic, ent of transmIssibility ranges from>l ,~ 10- 0 to
1 x 10-~ for dolomitesA*rMl 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 tiie 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 grhins
forming the pores; the gradient; the chemical Band mineralogical
composition of the pore walls; the thickness of the walls in
thin-welled pores; and the temperature, Viscosity, and composi-
Card 2/3

15- 1957 -13 -3174
The Aggression of Water In Relation to Its 14ovement Through Rock
tion of fluids migrating through the rock. The factors of tima
and pressure also Influenee the c oofficient of' transmissibility.
It was calculated that water will pass through approximately
100 m of rock, even if dense, in 3,300 years. With water pas-
sing through it, dolomite loses 0.00A~ of its weight in a year;
limestone loses up to 0.27,v. 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 pares, and because imperme4ble layers, if
present, prevent free drainage. _Thus 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.; MUAMY. K.M.
1. ~
-11 1. FbI,JI in and Cu, distribution in various classes und fractions
of the DIluvIum In the region of two deposits in Central
Kasakhatan [with Inglish sumary in insert]. Gookhimlia no.4:
50-57 156. (KLBA 9tll)
1. Institut geologil rudvykh nestorothdaniy, petrografii,
mineralogii I gookbiali Akademii nauk SSGR. Moskva.
(Kazakbotan-Geochemistry)

USSR/Commochamistry Geochemistry. Hydrochemistryp D
Abet Journalt Referat Zhur - Khimiyaj No 1, 1957P 743
Authort linsburg,_~. 1.
Institutions Academy of Sciences USSR
Title: Geochemical Methods in Ore Prospecting
Original
Periodical: Vestn. AN SIBSR, 1956, no 61 58-64
AbBtractt 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. Semiqxwtitative
spectroscopic analysis is of great importance in this respect.
Purther progress in geochemical prospecting must be achieved by the
utilization of one sample for the determination of 6-10 and more
elements. Geochemical, bydrochanical, biochemical, and geobotanical
prospecting methods are -finding wide application. For complex in-
vestigationa the creation of integrated prospecting tews and field
laboratories is nemseary. For the preliminary survey of large
Card 1/2

PHASE I BOOK MLOITATION 646
Gjazburg, n1ya Isaakovich
Qpyt razrabotki teoretichesXM onnoy geokhimicheakikh metodov poiskov rud
tsvetuykh I redkikh metallov (Experience in the Development of Theoretical
Principles for Geochemical Methods of Prospecting for Nonferrous and Rare
Metals) Moscow, Gosgeoltekhtzdat, 1957. 10,000 copies printed.
Ed.: Smirnov, V. L Ed. of Publishing House: Godovikov, L. A. Tech.
Ed.: Gurov., 0. A.
PURPOU: The book is intended for practical and theoretical exploration
geophysicists specializing in geochemistry.
COVFJL4GE: The book covers the entire field of geochemical exploration and reviews
both the recent methods of chemical analysis of rock (or soil) and the peculiari-
ties of geology of Individual mineral deposits, essential for practical prospecting
vork. Rach 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 frcm the reports of leading Soviet geochemical
,ers and from the records of the All-Union Congress of Geochemists (1956).
C,ATq

&periance 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. Aw Rukavishnikova, I. V. Vitovskaya, V. V. Borodin,
Yu. Yu. Bagel'skiy K. X. Mukanov, L. D. German, A. 1. Pokrovskaya (an
analytical chemists, and L P. Sechina, (a spectral analyst); furthermore,
the following scientsits have contributed their material to the author:
S. D. Miller, I. P. Benivalenakiy, G. 1. Boosman, and A. G. Betekhtin; in
addition, the following scientists have revieved the book: 0. D. lAvitskiy,
F. I. Vullfson, 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. Following the
decree by the MInistr7 of Geology in 1955, the geochemical element has beccme
an integrated part of every geophysical and geological prospecting scheme. Each
chapter is acccepanied by an extensive bibliography, consisting almost entirely
of Soviet contributions. There are 328 references, 317 of them Soviet,
8 Ehglish, 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 saaWle 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 "bypergene" includes all relevant ore-fornation
processes.
Card 2/16

Ibmerlence in the Development (cont.)
TAMX OF COMMM:
646
[11ote: There is a certain discrepancy between headings in the Table of Contents and
those in the text. Information in brackets is added to clarify the text]
Forevord
Introduction
3
5
KistM of geoche2dcal exploration in USSR 5
Ceochezdcal prospecting outside of USSR 7
Slime analysis in geochemical prospecting 8
Development of prospecting methods - physical, physiochemical,
chemical, biochemical, etc.
Connection between geocluntical prPopecting and geological surveying;
integrated (combined) character of operations 10
Contributions of geochanistry to prospecting 11
Card 3/ 16

Experience in the Development (Cont.)
646
Ch. 1. Yethods of Analytical Geochemical Prospecting 13
Spectroscopic method 13
QuaUtative chemical spot test and powder method 15
Colorimetric method; comparison between chemical and colorimetric
methods 15
Pbase analysis (Analysis bued on differences in solubility) 20
Electrodialynio 21
Water analysis; other methods P-1
Selection of proper method of aualysis 22
Ch. TI. 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
Geochemical, correlation of elements (paragenesis) 34
Fax-tore on which geochemical indication is based 37
card 4/16

Experience in the Development (Cont.) 646
Ch. IIL Metal Concentrations in Eruptive and Metamorphic Rocks 38
Geochem:4-cal basis of concentration and dissemination (dispersion) of
chemical elements in rock 38
Ability cE ebwU to disseminate and concentrate 39
Permeability of rocks and metal concentration in them 41
Con-.ept of dissemination halos 44
Conneetion between the contour of dissemination halos and the
structure of deposits 45
Features cf meta 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
Tm~.e elements in thu crystal lattice of minerals 52
Xoseminated mi-neralization 54
SyngeLeti,2 and epigenetic dissemination 55
Enriched metallic mineralization 58
Xner&Lization of balos. Indices of mineraLization 6o
Forms of mineralized areas, their size and extension 60
Card 5h6

kxperience in the Development (Cont.) 646
Ch. IV. Concentrations of Vatal In Sedimentary Rock 69
Conditions inducing concentration 69
Transportation of sedimentary materials 70
Conditlow of deposition and transportation of metal-bearing sediments 72
Stageo of sedimentary ore formation 77
Penetration of solutions into the rock strata and its influence
on uxaniua content 78
Yetal content in sedimentary rocks 79
Stratification of metal ore concentrations in sedimentary rocks 80
Deposits formed by sedimentation 81
Vietals in coal ashes 83
Correlation of individual elements 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
biportance of metal-inpregneble 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 bypergenic zones and in original rocks
Dissemination of high-mobility elements and their compounds
in original rock 98
Gec.zhemiaal prospecting for sedimentary rocks 101
card 6/ 16

EVerien.-e in the Development (Cont.)
646
Ch. V1. Prospecting for Blind Deposits (Underground Prospecting) 103
Beax-.h for ore in sedimentary rock under alluvial blanket 103
Seaz~h 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 320
Symptums of possible mineralization; tests 111
Interpretation of results of geochemical prospecting 118
Conclusions 119
Ch. VII. Metal Concentrations in Loose Rocks Covering the Halos of
Mineral Dissemination 122
Halos of dissemination 122
Factors 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/ TW

Experience in the Development (Cont.)
k-_,umilation of minerals depending on the Interplay of soil and
646
climatic conditions 134
Metal content in dissemination halos 135
Metall below the vater-table stratum 135
Importance of the composition of ground air 135
AnAent erosion 136
Abs~)rption of solutions by roots 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 gases 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 lover oxides of metals) 148
leached and weathered zones 154
Mineral composition of oxidation zones; ferroginous outcrops (gossans) _1~5
card 8/ 16

Experience in the Devel%wnt (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 waos
Shapes of dissemination halos in blanket deposit
7mterpretation and evaluation of dissemination halos
Ch. VIL Surface Prospecting in Blanket Deposits
Depth of the test pit
Size of rock swaples according to type
The veight of rock sample tested
Slim and spectroscopic analyses
Selection of proper method of test pit
Casez of "pseudocontamination" of rock
minerals in rock samples)
Search for lead
of rock
analysis
(incidental occurrence of
157
158
159
164
165
168
169
171
174
174
175
176
177
177
178
178
Card 9/16

&perience in the Development (Cont.)
Search for zinc and cadndum
Sean-b. for silver
Search for copper
Search for molybdenum
Search for tungsten
Search for tin
Search for gold
Searzh for nickel, cobalt and chromium
Search for fluorspar
Search for heavy spar (barite)
Search for lithium
Some practical advice; conclusions
Un. IX. Metal Idgration in Water
Hydrogenic elements
VIneral. solubility and hydrogen-ion concentration
Forms of metal occurrence in water
Metal content in water of different origin
Factors influencing metal content in viter; the importance of the
pH fa.:tor
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 I o/ 16

Experience in the Develolment (Cont.) 646
Features of sulfide distribution in sulfide-bearing rock 204
ClIziatic conditions (and their input on metal concentrations);
impact of water-bearing rocks (aquifers) 205
Concept of mig3mtion coefficients 206
Migration of metals in water 206
Metals in swaups 208
Degrees of dissemination of metals in water 209
Behavior of Individual metals in water and soce other chemical elements
or their coWounds 210
Lead 211
Zinc 212
Silver 213
Cadmium 214
Bixmth 215
Tin 215
1-blybdenum 216
Vanadium 217
Chrmdum 218
Card III, e

Experience in the Develcyment, (Cont.)
Nickel
Cobalt
Arsenic
Yercury
Uranium
Antimony, selenium, tellurium, phosphorus
Germanium, gallium
Beryllium
Titanium
Scandium
Barium and strontium
Ions of sulfuric acid and of chlorine
Fluorine
Boron
Analysis of water extracted from rock
Determination of the pH of water
646
219
219
220
220
220
221
221
221
221
221
221
222
223
224
225
225
Card 1246

A
Experience In the Development (cont.) 646
Ch. X. Hydrogeochemical Prospecting for Metals and Characteristics of Water
for Various T~pes of Deposits 227
Determination of features of dissemination 227
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 multlmetalllc (caVlex nonferrous) deposits 237
Water in deposits of rare metals 238
HydrochemIcal nethods in permafrost areas 238
Determination of total Isotopic composition of water and its importance 238
Gas analysis as a method of prospecting; other methods 239
Ch. IL Biogeochenical 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 (Cont.) 646
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. XIL Gedbotanic Prospecting Method 253
Theoretical principles 253
Types of indicator plants (graving on soil rich in particular metals) 254
Teratological factors (indicating structural peculiarities);
metallophillic flora 255
Factors indicating the presence of copper, uranium, and selenium; exazoples 256
Vegetation blanket as an indicator of lithological cwVosition of rock,
hydrogeological conditions and tetonic rock structures 259
Aerial geobotanic prospecting 26o
Card 14A6

Experience in the Development (Cont.) 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
Geochenical 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 swanpy regions 267
Importance of au~dliary methods: hydrochemical, biochemical, botanic, etc. 267
Drilling for map-naking 268
Types of metallometric survey 268
Selection of proper method and interpretation of geochemical
prospecting data 269
card 15/16

~Exparience in the Development (Cont.)
646
Distortion in position (site); forms of bounds marking the halos of
mineralization. Application of geochemical exploration methods in extreme
North-But. Selection of proper scale in mapping a deposit. General
conclusions 270
Appendix
SIM11fied method of assaying lead,, copper, wolfram,, mblybdenum, and
silver in the field 275
Reagents 275
Determination of wolfram 276
Determination of molybdenium
Determination of silver
Setermination of L.Vper 279
Determination of zinc 280
DeUrmination of lead 281
Bibliography 282
AVAUAMM: Library of Congress
Card 16116 *Vbmd
10-14-58

AUTHORt Ginx')urg, I.I. li-12-5/13
TITLEj Basic: Results of Study of Ancient Cores of Weathering in
the USSR (08novnyye rezultaty izuct)enlya drt~vnikh kor vyvetri-
vanlya v SSSR)
PERIODICAL: Izvestiya Akademii Nauk SSSR, Seriya ~eologicheskaya, 1957,
# 12, pp 61-88 (USSR)
ABSTRACT: Studies of disintegration of* mountain rccks -were taken up
more than 20 yeare ago by B.B. Pulynov and other reulogista,
and they were continued in 1956 by D.T. Ullyanov, G.S. Gritoayen-
ko and other USSR scientists. Examinaticns of the effects of
disintegration of the earth's crust were brou6ht about by
prospecting for nickel, aluminum, iron, marigan, kaolin, heat-
resisting clays, zirconium, titanium, diamonds, optical quartz,
rare earths and other minerals depcy~sits aosociated 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 ever the entire terri-
tory of the USSR. Ancient rinds of disintegration proved to
be of such importance that it seemed ~ustilfied to establish a
new branch of geology, specializing on t~ie pecu -larities of
Card 1/3 these geologic formations and the methods of research. At the

11-12-5/10
Basic Results of Study of Ancibnt'Coreg of Weathering 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 'I 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, leachinC, filtration, re-
Card 2/3 deposition, transformation, washing-out and the development of

11-12-5110
Basic Results of Study of Insievt-1wee of Weathertng in 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 whicb is overlaying or which is
covored 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, I British, and I American
references.
AVAILABLE: Library of Congress
Card 3/3

GINZBURG, 1. 1.
"Types of Old Crusts of Weathering in USSR."
paper distributed at the International Clay Mineralogy Congress in Brussels, Belgium,
1 - 5 Jul 58.
Comment: B-3,116,85?.

AUTHOR: Ginsburg, 1.1.
TI'"LE: Conferonce on the Research and the Use of Cays 'Soveshcha-
niye po issledovaniyu i ispollzovaniyu glin)
PERIODICAL: IzYestiya Akademii Nauk SSSR, Seriya Geologicheskaya, 1958,
# 1, pp 110-111 (USSR)
ABSTRACT: The first conference on research and u3e 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. 5.
Engineering-geological properties of clays and minerals. 4.
Study of clays and soils of different districts. 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 112 lysis, mineral composition, technological properties, genesis,

Conference on the Re.,iearch and the Use of Clays 11-1-23129 1
classification and other characteristics of c-lays.
AVAILABLE: Library of Congress
Card 2/2

Cal Zll

GINZBURG, I.I.
Comaittes of the Academy of Sciences of the U-S.S.R. on the
study of clays. Gool.rud.mostorosh. no.1:127-128 Ja-F '59.
(MIRL 1215)
(clay)

I GINZBURG.
Hickeliferous magnetite in stlicate-nickel deposits. Kora
vyyetr. no. 3:33-38 160. (MIRA 13:12)
1, Ingtitut geologil radnykh meetorothdenly, petrografii,
mineralogil i gaokhimit AN SSSR.
(magnetite)

GINZBURG, I.I.
"Ifickelmelane" and mcobaltmelandg. lora vyvetr. no. 3:56-66
'6o. (XIU 13:12)
1. Institut geologit rudnykh mestirozbdeniy, petrografii,
mineralogit i gookhim! i M SSR.
(Poilomelana)

XABOOVA, Too$.
Silica content in natural waters and forms of its occurence.
lora, vyvstr. no. 31313-342 160. (MIR& 13:12)
(Silica) (Water--Composition)

GI117,BU11Q,_J.j,; 01,1311ARSKIYj Ya.l. [deneaeod); BELYAT3UY, V.V.;
Prinimali uchast~ye-. 1.1JUDENOVSKAYA, T.S., laborant;
RO&ABSTUNSKAYA, Z.B., laborant; KOZHINA, V.M., laborant;
F.EODOTIYEVt K.M., otv.rod.; SHIAZOV, V., redAzd-va; UUT,
V.G., toklin.red.
40ftaisivot experimental and technical petrography and mineralogy]
isslodovaniia po ek.9 rimentallnoi i t--khnielieskoi petrografii i
mineralogii. No .4: tudius on oxidation of sulfi os 'As~,eri-
rs d I - p
niont,Ulln310 issledovaniia po okisleniiu sullfidov. Moskva,
Izd-vo Akad.nauk SSSR. 1961. 130 p. (Akademiia nauk 019R.
Institut geologii rudynkh nestorozhdonii, petrografii, mineral-
o6li i gookhimii. Trudy, no.59) (MIRA 1J,:7)
(Sulftdoo)

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 '61. (MIRA 14:9)
1. Institut geologii rudnykh nestorozhdeniy, petrografil,
mineralogii i gookhimii AN SSSR, Moskva.
(WeatherinF) (Minerals) (Prospecting)

ALITGAIMN, H.N.; MRZBURG, I.I.; DUBOVSKAYA, M.V.; VMHOV, A.D.;
wimvp V-.g.-;06 lKINt N.-J.; RMHEOVA 0 Ye,V.; SMAKHOV j N.M.
MUSHGBOV# N.A.1 SHMANEGHKOVj I.V.; SlIGIMWOV, D.I.;
UMHIN, A,L.; AMIRASUNOVp A.A.j GOTHU, Ya.D.; ZUEMV, I.N.;
KOOVYAXOV) I.A.; ORLOVA, F.V.; PASOVA, F.G.; SAAKYAN, P.S.;
TUMIYKVA, K.F.; SHANOBSKIY, L.M.; CHMOSVITOV, Yu.L.;
SHOBERBIIU) V.V.
IUrii Konstantinovich Goretskii; obituary. Sov.geol. 4 no.12:
153-155 D 161. (MIRA 15:2)
(Goretskiip Iurii Konstantinovich, 1912-1961)

NIKITIN, Konstantin XanstantJ.novich; GINZRMb,-j.J_., otv.red.; ASTROVI
A.V.,, red.iod.-va; WHINA, P.S., tekM.red.
(Ancient weathering surface of ultisbasic rocks in the Buryktal
Massif) Dr"ala kora vyvetrivaidia Buryktal'skogo massiva
ul'traosnovnykh porod. Moskva, Izd-vo Akad.nauk SSSR, 1962.
189 P. (Akademiia nauk SSSR. Institut geotogii rudnykh mestorozh-
denii, petrografii, mineralogii i geokhimli. Trudy, no.69)o
(Ural Mountain region-Weathering)
(Ural Mountain region--Ultrabasite)

TITOT"VAIA . I r' !/],A,]! if;!! -,vna; . GI%BUh3f L I.. dor tll,. rinuk,-
A,, r(A , izd-vil; 3U'jHE-Vn, , rpc,.
--I on and of Iz.1 -e 311par-
giclif! zxrja of A-o~uag.,,l and Ktzyl-FFpAj I-Iline-al nyl sostrav i povedenif
Tpik.,c.el,~mertov v --one i Kjzyl-.i,:spp. Moskva,,
-7, 'OSR,
1A ir,
-Jrr, depoilts) E-loments)

GINZBURG, I.I.. NADZHAKOVA, 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.
(KRA 15:9)
1. Institut. geologii rudnykh mestorozhdeniy, petrografii,
mineralo, il i gookhimii AN SSSR.
lBrazil--Weathering) (Brazil--Basalt)
(Russian Platform--Weathering) (Russian Platform-Basalt)

-.UNZBURG, I.I.; PI!FMSKIY, CO.
Z~.
Weathering surfftce of rocks of the greenstone formation in
the Uchaly pyritic copper deposit. Kora vyvetr. no.W47-
177 162. (KRA 15-09)
1. Institut, geologii rudnykh mstorozhdeniy, petrografii,
mineralogii i gookhimil AN SSSR i TsNIGRI.
(Ural Mountain region--Weathering)
(Ural Mountain region--Greenstone)

VOLIFSON? rj~a G3MRG J.1,; SAPOZBNITOV, D,G*; SOKOLDV, G.A.;
I , ~411UIIII
T"I
Eightieth birthday of B%P. Krotov, Geol.rud.mestoroshe no,51117-
'KrRA 1502)
118 8-0 162, (Itrotovp BDrim Petrovich# 1882-) %

6JNJ
Th.*-Conference.on applied karatology
PERIODICALi Izvestlya Akademll nauk SSSR, Berlya giologicheskaya, no. 1, 1963,
124 - 126 (antl=*1 Oftzdetskly, 1. A., and ChikUbelr, A. 0.)
TEXTt The Conference van hold in Moscow on Apr?l 23 - 25, 1962, and was
attended by 35 representatives from 16 sciantifloti and Industrial organizations.
The Conference was opened by N. A. Ovotdotakly wh,j reported on the activities of
the Geographical section of the Moscow Society of Natural scientists. The folloV
In& reports were dellvera4t A. 0. Lykonhln on the investigation of karats for
hydro-engineering construction by geological ang!,neeraj V. S. Polevoy o
of geophysical methods to study karstB in areas of hydrological engineering atruo-
tures; 1. A. Savarenskly on problems considering karats In Industrial and urban
cons region; N. A. Ovasdotskiy on "Karat in the region
of Caucasian Mineral Water Souroes"I I . 0
on mineral resources onnected
with karat prooesseal 0 kl; on tauxite an: phosphorite karat depoeltal
Ys, T -DIbroy on *Karat bauxites of the Yanisay ridge and the adjacent region of
the Siberian platform"; 44-~I~ailts ~& an "Karat bauxites In the Xaz&kh fold1w
and the Turgay depression ; B N 'Iyanov and V. N. Dubl an
lyM!kIy on "The Importance
of the CrImea karst In natlon:d :Oonomy ; A, V-Chl "-1hev on "The importance of
the Central Ural karat In national economy I I. K. Kudryashov on the influence.of
karat an agriculture In some Bashkirlan regloiiil The-reports delivered were dIs-
cussed by D. S. Sokolov&, V. A. Varmanoflyeva, N. A. Krasll'nikovs, S. A. 3144-
kopevUeva, V. S. Polevoy and others, The Conference approved the methods of
karat Investigation, Including geophysical means, electrical asismio and ultra_
sonio prospecting. It was deoided to Investigate in detail the development and
expansions of karstj to study the origination of karat bauxites, to control the
purity of mineral water sources and to oantinue resoarah in the agricultural re- I
glonn of BasWr1a.

ILA6"ft
Reaction energy of weathering processeo of some aluminoollicatee.
Kora vyvetr. no-5:87-119 163. (MIRA 16:7)
1. Institut geologli rudnykh mestorosbdenly, petrografii,
mineralogii i gookhiail AN SSSR.
(Aluninosilicatoo) (Weathering)

CT!;-BURC ' , !J.
(tri,.- .-, ! f i - , -. .~,i gi)ur, i~ . -
I t -i ~ ~ q 11 , : , , ~, ~,i . i ng I ,,, 1, - ~ ,. - , ~ ". - :; 1 1 -;
i r, t r. r.- io;i - i ti: n Ur o .-, , I!-. i. ., ,a - I , -A f-k 1 , I -. A. o " I .Nz'i. o . ulot
( ~' . 1
rv~ . 3 -. - -'- ~~ I t . . : f , P: , ,

SAUKOVI A.A.1 GINZBURG,:jjq; PEMIMAN, A.I.; AYDINIYAN, N.Kh.;
SHMOVI "Mv.' , -
Vladimir Ivanovieb Krannikov; obituary~ Gool. rud. mestorozb.
5 no.21-1/a.-3.42 Mr-Ap 163. (MIRA 16:6)
(Erasnikov, Vladimir Ivanovich, 1907-1962)

BEMIN, $.I.; VITOVSWA, I.V,; GINZBURG, lol.
Montmorillonite containing advdxtures of ballOYSite fz-Om the
oxidation zone in the fysyl-E" deposit. Kora vyvetr. no.5:
7-16 163. (MM 16:7)
1. Institut geologii radnykh mestorozhdaniyj petrografiip
mineralogii i geokhimii AN SSSR.
(Nasakhotan-Montmoril-lonite)
(Kazakhotan-Halloysite)

eathenng surf'11ces, forms cf their
T e ariclenL w I
occurrence and clasonfication. Yorti vy'vetr. no.6&71-101 163.1
(MIRA 17:9)
Y" f i
i) rudnYQ; mw- l,nrnnhdvniy, I-IlroF 1. 1,