SCIENTIFIC ABSTRACT GRIGORENKO, YA.M. - GRIGORESCU, ST.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R000516720012-7
• Release Decision: RIF
• Original Classification: S
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• Document Creation Date: January 3, 2017
• Document Release Date: July 27, 2000
• Sequence Number: 12
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

15-57-5-6653
Translation from: Referativnyy zhurnal, Geologiya, 1957, Nr 5,
PP 138-139 (USSR)
AUTHOR: Ginzburg, A. I.
TITLE: Kirghiz Hard Coals in Polarized Light VJith Crossed
Nicols (Kamennyye ugli Kirgizii v ~olyarizovannom
svete pri skreshchennykh nikolyakh
PERIODICAL: Materialy Vses. n.-i. geol. in-ta, 1956, Nr 8,
pp, 241-251
ABSTRACT: Clarain, clarain-durain, and durain coals were studied
in normal light and in polarized light with crossed
nicols. Thbn sections parallel to the surface of
stratification were placed at an angle of 450 to the
crossed hairs of the eyepiece in the position which
provided maximum lighting for the coal. All com-
ponents with the exception of the fusain showed aniso-
Card 1/2 tropy anti interference coloration in polarized light

Kirghiz Hard Coals (Cont. )
15- 5'/-5-6653
with crossed nicols. Thec-e phenomena were intensified with a,.-,
increase in the degree of metamorphism. Double refraction of coa'l
substances varies from low (D-PZh quality coal) to average (1,-T
quality coal) to indistinct (PA quality coal). Extinction varies
from slight (D-PS coal) to almost complete and direct (PS-PA). The
most marked changes in properties occur between G arid PZh qualities
and between K and PS qualities. Use of polarized light is recom-
mended for study of coals of PS and T qualities. It provides a more
precise idea of the rreserved plant structural substance in co-al aL
a low degree of metamorphism.
Card 2/2 0. D, FL.

15-57-1-806
Translation from: Referativnyy zhurnal, Geologiya, 1957, Nr 1,
p 127 (USSR)
AUTHOR: Ginzburg, A.
TITLE: The Evolution of Fusain During Metamorphism in the
Coals of Centrhl Asia (K voprosu ob evolyutsii fyuzena
pri metamorfizme v uglyakh Sredney Azii)
PERIODICAL: Materialy Vses. n&-i. geol. in-ta, 1956, Nr 8,
pp 252-258.
ABSTRACT: Fus n, fusain-xylain, and fusain-xylain-durain in the
Central Asian coals undergo changes during metamorphism
similar to those for bright clarain coals, but in a
smaller range'of variation. In brown coals, fusain-
xylain types are distinguished from clarain by the
higher content of carbon, the lower yield of volatiles,
and the lower content of hydrogen. In bituminous coals
of the first type, changes in the content of carbon,
hydrogen, and volatiles, according to increased stage of
Card 1/2 metamorphism, are less than in clarain coals of the

15-57-1-806
The Evolution of Fusain During Metamorphism (Cont. )
1
same series. Similar types of changes in coals of different
I essential compositions are observed for color, luster, densityx and
fracture,
Card 2/2 14. K.

14
Category: USSR D
Abs Jour: RM--r1h) 110 31 1957) '((",5~
Author : Krylova, N. M., Vallts, 1. E., Lyuber, A. A.) and Gi _,buri A.I.
Inst : Coal Geology Laboratory of the Academy of Sciences USSR
Title : Basic Principles in the Materials and Petrographic Classification
and Terminology of Humus Coals
Orig Pub: Tr. Labor. Geol. Uglya. Al SSSR, 1956, ijo 6, 42-53
Abstract: No abstract.
Card : 1/1
SUBJECT: USSR/Geology
AUTHOR% Ginzburg, A.I., and Gorzhevskiy, D.I.
TITLE: On Interconnection of Rare-Metallic Pegmatites and Some Types
of Ore Veins (K vopro8u. o vzaimoevyazi redkometallnykh peg-
matitov i nekotorykh tipov rudnykh zhil)
PERIODICALt Izvestiya Akademii Nauk SSSR, Seriya Geologicheakaya, 1957,
# 6, p 14-29 (USSR)
ABSTRACT: Interconnections of rare-metallic granitic pegmatites of the
pure series and high-temperature pneumatolytic-hydrothermal
formations are analyzed in the article. The authors came to
the following conclusions:
1) Rare-metallic pegmatite fields and ore veins occur
most often in different regions. Sometimes they occur in
the same metallogenic provinces, but also in these cases they
are spatially separated and localized in different sections.
2) The territorial separation of the rare-metallic peg-
matites and ore veins is determined by different geological
conditions of their origination; the connection with differ-
Card 1/5 ent intrusive rocks, different depths of origination and

io-6-2/13
TITLEt On Interconnection of Rare-Metallic Pegmatites and Some Types
of Ore Veins (K voprosu o vzaimoavyazi redkometaltnykh peg-
matitov i nekotorykh tipev rudnykh zhil)
difference in ages.
3) Pegmatites are usually connected with normal micro-
clinic biotite granites, whereas ore veins are often connect-
ed with muscovite and alaakite granites. These varieties of
granites correspond often to different phases of intrusive
complex origination.
4) Rare-metallic pegmatites and ore veins are originated
at different depths: the origination depth of pegmatites
varies from 4 to 8 km and that of ore veins from 2.5 to 4.5 km.
5) Ore veins are essentially younger formations than peg-
matites. Many cases were observed where pegmatites were inter-
sected by ore veins but no case of a reverse situation.
6) Rare-metallic pegmatites and ore veins differ from
each other in chemical composition. Pegmatites are distinguish-
ed by a very high concentration of alkalis Li, fla, K, in part-
Card 2/5 icular Rb and Cs, rare eartba, Y, and also Nb, Ta, Zr, Hf,
4i -

1o_6_21i3
TITLE: On Interconnection of Rare-Metallic Pegmatites and Some Types
of Ore Veins (K voprosu o vzalmoavyazi redkometallnykh peg-
matitov i nekotorykh tipov rudnykh zhil)
and Th. For the ore veins are typical S, W, Mo, Cu and Pb.
Some elements can accumulate both in pegmatites and ore veins,
such as Li, Be, B, Ga, So, Bi, Sn, Go, As and U.
7) According to many of their peculiarities, pegmatites
occupy an intermediate position between igneous magmatic rooks
and ore veins.
8) The available factual data make it probable that the
development of pegmatites and ore veins proceeds along two
parallel independent lines, but this development does not
occur simultaneously. Pneumatolytic-hydrothermal processes
occur later than pegmatite development and are often connected
genetically with the younger intrusive phases. These both
branches of development can be schematically presented as
follows:
Card 3/5

1o-6-2/13
TITLE:
Card 4/5
On Interconnection of Rare-Metallic Pegmatites and Some Types
of Ore Veins (K voprosu o vzaimoavyazi redkometallnykh peg-
matitov i nekotorykh tipov rudnykh zhil)
Normal
Granite pegmatites
(without ores)
Granite pegmatites
rare-metallic
(biotite) granites
Leicocratic and
alaskite granites
I
Pneumatolytic-
hydrothermal form-
ations (ore veins)
The article contains 1 table.
The bibliography lists 19 Slavic references.

lo-6-2/i3
TITLE: On Interconnection of Rare-Metallic Pegmatites and Some Types
of Ore Veins (K voprosu o vzaimoavyazi redkometallnykh peg-
matitov i nekotorykh tipov rudnykh zhil)
INSTITUTIONt Vae-Soyumnyy Institut Minerallnogo Syrya "VIMS" (All-Union
Institute of Mineral Raw Materials) in Moskva and L'vov State
University
PRESENTED BY:
SUBMITTED: On 10 September 1956
AVAILABLEt At the Library of Congress
Card 5/5

GINZBURG, A.I.
-:1-
~wm-
characteristics of lithium. Trudy Min. muz. no.8:29-41
157o (MIRA 1193)
(Lithium)

TiSSR/Physical Chemistry - Cryst&bl.
Abs Jour: Referat. Zhurnal Rhind ; 110 3, 1958, 7014.
Author A_T_
Inst Acade.W of Sciences of USSR, Mineralogical Hiseum.
Title Isamorphous Substitutions in Lithium Mims.
Orig Pub: Tr. Mineralog. muzeys AN S3SRj 1957.s vn, 8j 42-60,
Abstract: Questions connected with all the possible isomorphous substi-
tutions in -lithium micas are discussed in detail based on the
genera.liza-It'lion of the great factorial material in the litera-
ture. The main conclusions and results are as follows: l/ the
,composition of Li micas can be e:qressed -by the formUa (K, Ila,
Rb, Cs) f(Lit, Mg, Fe~' '.ft)n (Al, Fe3+, f(SipAlk,_p)
010 7 (OH, F)2, where k = 0 to 3, n = 0 to 3, m. = 0 "to 2 and
P = 3 to 4; 2/ the most abaracteristic substitutions in Li micas
have been established; 3/ it has been shown that muscovite may
contain Up to 1.8% Of L102 as an isomorphcras admixtare withuat
Card 1/2
_10-
USI~JR~yGicaL Chemistry - CrystAls. B-5
Abs J.'.vir: Referat. Zhurnal "Jinlya, No 35 1958) 7014.
any atructural changes; should the IAO_ content be uP to 3.2%,
Li-muscovites (2-layer lepidolites) wZ~ be fom~d, their d
differs somewhat from -that of muscavIte; 4/ the diependence be-
tween the chemical coiqposition and structure of lepidolites
has been established; -W there is a direct dependence between
the Li and Fe contents In minerals of the ruscovite-lopidolite
gn~up- Question conce:,-ning the connection b,~tween the struc-
ture of Li micas wid the c3nditions of tlv-i-- foz..,Mtion are aloo
disCusoed.
card 2/.2

GINZBURG, A.I.
Bitylte-litbium-baryllian marpAritf). Trudy Min. muz. no.81128-131
'57. (MIRA 110)
(Margarite)

GINZBUR~~.Ax
- - k4w*--
~ -M
m----44A,4 I
Componition of zinc rockbridgelte. Tmdy, Kin. rviz. no-8:131-134
'57. (KIM 110)
(Rockbridgeito--Analysis)

GINBURG, A.I.
-.1" -,;.
,,,O~Go`netic types of rure element deposits. Razved. I okh. nedr 21 no.6,
1-12 A 157. (MIRA 11:7.)
1. V9oso,,Atznyy natichno-isfiledovatellskiy institut minerallnogo eyrlya.
(Chemical elements) (Mineralogy)

3(5), 15(6) PHASE I BOOK EXPLOXTATION sov/1644
-I. Ye.A. Nechayeva, Yu.B. Lavrenevy and L.K. Posharitakaya
Gi!!b A~
Geologiya. mestorozhdenly redkikh elementov. vyp. 1: RedkcKetallnyye karbonatity
(Geology of Rare Element Deposits. no. 1: Rau,@ Metal Carbonatites) Moscow,
Gosgeoltekhizdat, 1958. 126 P- 5,000 copies printed.
Sponsoring Agency: Vsesoyuza7y nwAchno-iss;edovatellskiy institut minerallnogo syriya
Eds.: A.I. Ginzburg, and S.V. Ovchinnikova; Tech. Ed.: T.A. Averkiyeva; Editorial
Board: Aj. Ginzburg (Chair-man), I.I. Malyshev, G.G. Rodionov, F.P. Fpgatov,
N.t,Ao Krushchov, Yu.'L. Chernbovitov, IN. Shmanenkov, V.V. Shcherbina,, and M.A.Eygeles.
PURPOSE: This booklet is intended primarily for geologists. It may, however, because
of Its non-technical nature be of interest to the general reader.
COVERAGE: The introductory chapters of this booklet give a short history of the explo-
ration and stW~y of carbonatities. Approximately half of the contents are devoted
to a description of the- geological and geochemical properties of same rare minerals,
mainly niobium. These% descriptions am aided by the, use of tables and charts.
The second half of the book gives a physical description and the geographical loca-
tion of sane of the well. known deposits of the world. There are 131 references of
vhich 16 am Soviet.
Card 1/2

Geology of Rare Element Deposits. sov/164
TABLE OF CONTEM:
From the Editor
Foreword
The Geological,. Mineralogical and Geochemical Charactiriatics of Cazbonite Deposits
(L.K. Pozharltsksya, and A.I.. Glpzburg)
A Brief Description,of Non-Bovi*t Carbonatite Dep*its
Carbonatite deposits of Europe
Deposits of Alno Island (Ye.A. Nechayeva)
Deposits of the Yen Region (Yu.B. ~avrenev)
Carbonatite deposits of Africa Povh&rltskV&)
Carbonatite deposits of America (L.K. Parharitskaya)
Basic Characteristics of the Alkaline Group of Minerals (Ye.A. Nechayev'06)
Bibliography (D.B. Yegorov)
AVAILABU: Library of Congress
Card 2/2 MR/hcr
5-Lll-59

AUTHOR3: fi~ Gorzhevokaya, S. A. SOV/7-58-5-10/15
Yerofeyeva, Ye-.A.,Sidorenko, G. A.
TITLE: On the Chemical Composition of the Cubic Titanium-Tantalum
Niobates (0 khiaicheskom sostave kubicheskikh titano-tantalo-
niobatov)
PERIODICAL: Geokhimiya, 1958, Nr 5, PP 486 - 500 (USSR)
ABSTRACT: The specific properties of the so-called mineral group are
described in detail in the beginning; then the division into
the perovskite type (ABX 3) and pyrochlorine type (A 2B2X7)
is discussed. 22 chemical and x-ray analyses (Table 3) are
the basis of thia paper. A number of analyses are plotted in
several diagrams of ternary systems:Nb - Ti - Ta (pig 1);
A - B - X (Pig 5); Nb - Ti, Zr - Ta (Fig 6); Ca - TR - U - Th
(Fig 7). The dependence of the lattice constant on the TiO
2
content in the perovskite group (Fig 2) and in the pyrochlorine
group (Fig 3) is also shown. The result of the paper is a
classification of the mineral groups investigated (Table 2).
Card 1/3 The empiric formulae of minerals greatly differ from the

On the Chemical Composition of the Cubic Titanium- 3011/7-58-5-10/15
Tantalum Niobates
theoretical formulae generally adopted for them. A deficiency
of cations in the group "All was found. In connection herewith
the formula A B X is proposed where x denotes the value
n-x p q
determining the deficiency in the atomic numbers of tho group "A"..
For the pyrochloric type the formula then reads A 2-xB2X7,
and for the perovskite -type A 1-x BX 31 or A2-xB2X6' The atomic
proportion of the cations of the group 11,111 in the cubic titanium-
tantalum niobates ranges from 2,0 to 0,5, a definite do-
pendence between the extent of the cation deficiency in the
group "All and the content of titanium, zirconium, uranium,
thorium and water in minerals having been observed. The usual
minerals with an increased cation deficiency in the group "A"
are metamictic minerals. There are 9 figures, 3 tables, and
23 references, 15 of which ar- Soviet.
ASSOCIATION: Vsesoyuznyy institut minerallnogo syrlya, ',,Ioz;kva (All--Union
Institute for Mineral Raw Materials,lJoscow
SUBMITTED: March 17, 1958
Card 2/3

On the Chemical Composition of the Cubic Titanium- SOV/7-58-5-10/15
Tantalum Niobates
Card 3/3

r-)f
AUTHOR: Ginzbuie, A.I. 11-58-6-7/13
TITLE: On the Classification and Nomenclature of Coal Microcom-
ponents (0 klassifikatsiyakh i nomenklaturakh. mikrokompo-
nentov ugley)
PERIODICAL: Izvestiya Akademii Nauk SSSR, Seriya Geologicheskaya, 195a,
Nr 6, PP 88-94 (USSR)
ABSTRACT.- The author studied various methods of classifying micro-
components of coal. By the old system f-Ref -',, 4_7, all
microcomponents of humic coals were divided intO 4 baaic
groups, three of which represented the products of trans-
formation of vegetable fiber, and the fourth - spores,
cuticules and resinous bodies. Another method was pre-
'. Vallts Z_Ref 2
sented by I.E _7. She introduced a series
of new denominations. This method is described in detail.
The All-Union Petrographic Conference in 1956 established
another nomenclature of petrographic coal components
(Table 1), which calls for five groups of microcomponents.
The author is of the opinion that the old /_ Ref 3, 4-7
method, with adjustments, is the best method. The Vallts
method could be used for brown coal, and the method ac-
Card 1/2 cepted in 1956 - for coal used for coking purposes.

11-58-6-7/13
On the Classification and Nomenclature of Coal Microcomponents
There are 2 tables and 5 Soviet references.
ASSOCIATION: Vsesoyuznyy riauchno-issledovatellskiy geolo6icheskiy in-
stitut Kinisterstva geologii i okhrany nedr SSSR, Leningrad
(All-Union Scientific-Research Geolcgical Institute at the
Ministry of Ceology and Conservation ui Mineral Resources
of USSR, Leningrad)
SUBMITTED: August 24, 1957
AVAILABLE: Library of Congress
Card 2/2 1. Geology 2. Coal-Transformations

PBLII)KAN, L.G.; STATROV, O.D.
I:. I
Trace elements in igneous rocks-, results of the sMosium on the
geochemistry of trace elements in connection vith petrogenevis.
Sov. gaol. 1 no.4-170-178 Ap 158. (MIRA 11:6)
l.Vsesoyuzn" institut minerallnogo syriya.
(Trace elements) (Igneous rocks)

ICAT NOV, A.D.; LIBERMAN, R.K.; G , nauchnyy red.; YMSHOV.
A.D., glavayy red.; NEXRASOVA, N.B., red.izd-va; IVANOVA, A.G.,
tekhn.red.
[Industry's demanda in tho quality of mineral raw materials:
handbook for geologists] Trebovaniia promyshlennosti k kachostvu
minerallnogo syrlia: spravochnik dlia geologov. Moskva, Goa.
nauchno-tokhn.izd-vo lit-ry po geol. i okhrane nedr. No.68.
(Scandiuml Skandii. Izd.2.0 perer. 1959. 17 P. (MIRA 12:8)
1. Moscow. Vaevoyuznyy nauchno-isaledovateliskiy inatitut mine-
rallnogo syr1ya.
(Ores--Sampling and estimation)

0W".I..,-nauohnyy -- d.; NLTJIASOVA, N.B., red.izd-vn;
KOGAN, B.I.; ~LIJV .,a
IVAIIOVA, A.G., takfin.red.
[Quality required by industry in mineral raw materials; handbook
for geologists] Trebovaniia prowyahlonnosti k kachestvu mine-
rallnogo syrlia; spravochnik dlis geologov. Izd.Z., perer.
Moskva, Gos.nauchno-tekhn.izd-vo llt-ry po geologii i okhrane
nedr. No.41. (Lithium] Litii. 1959. 26 p. (HIFLA 12: 11)
1. Moscow. Vsesoyuznyy nauchno-isaledovatellskiy inatitut mine-
rallnogo syrIya.
(Lithium)

ZIV, Ye.F.; VAYS-IMBERG, A.I.; STEPANOV, I.S., nauchnyy red.; YERSHOV. A.D..
glavnyy red.; GINZBURG Aj., red.; ZVEREV, L.V., red.; MYTER, V.K.,
~4;46;54 -
red.; KOKROU A., reG; SOLOVIYEV, D.V., red.; KHRUSHCHOV. N.A.,
red.; CHMIOSVITOV, Yu.L.. red.; SHMAII-AITKOV, I.V., red.; NLUUSOVA.
N.B., red.izd-va; IVANOVA, A.G., tekhn.red.
[Industry's requirements 08 to the quality of mineral raw material; hand-
book for geol ogistal Trebovaniia promyshlonnosti k knchoatvu minerallnogo
syr'ia; a ravochnik dlia goologov Monkva, Goa. rvinchnQ-tekhn.izd-vo lit-ry
~o geol. ~ okhrane nedr. No.49. (Niobium and tantalumJ Niobit i tantal.
zd.2., perer. 1959. 49 P. (MIRA 12:12)
1. Moscow. Vneaoyuznvv nauchno-inuladovatellnkiy inatitut*minerallnogo
syrIya. (Ni6bium) (Tantalum)

MILOVANOV, G.B.; CHBIUIOSVITOY. Yu.L.;_XgZB J., nguchnyy red.;
'riMSHOV, A.D., glavnyy red.;-ZVEREV, L.V., red.; ZUBARHY, U.N., red.;
OSYTIM, V.K., red.; MOKROUSOV, V.A., red.; SOLOVIYEV, D.V., red.;
MUSHCHOV, N.A., red.; SIKAHMOV, I.V., red.; IZRAIMVA, G.A.,
red.izd-va; IVANOVA, A.G., tekhn.red.
(Industry's requirements as to the quality of mineral raw material;
handbook for geologists] Trebovnniia promyshlennosti k kachestvu
minerallnogo syrlia; spravochnik dlia geologov. Moskva, Gos.na,~chno-
tekhn.izd-vo lit-ry po geol. i okhrane nedr. Wo.51. [Rare earth
elements] Rodkozemelinye elementy. Izd.2., perer. 1959. 58 p.
(MIRA 12:12)
1. Moscow. Veesoyuznyy nauchno-iseleaovateliskiy institut mineral'-
nogo syroya,
(Rare earths)

CHONOSVITOY, Tu.L.; KONSTANTINOV, K.K., rwuchnyy red.; TARSHOV, A.D.,
glavnyy red.; SHKAHICIMOV, I.V., zam.glavnogo red.; GINZBURG,
A.I., red.; ZViOW, L.V., red.; KRLTM, V.K., red.-; -ROEROUSOV.
v.j., red.- SOLOVITNV, D.Y., red.; KOUSHCHOV, N.A., red.; NE'W-
P
SOVA, N.B., red.izd--va; IVANOVA, A.G., takhn.red.
[Industrial re irenents for tile quality of raw minerals; handbook
for geologister Trobovaniia promyshlonnouti k kachestvu mineral'-
nogo syrlia; spravochnik dlia geologov. Moskva Goa.naiphno-tekhn.
izd-vo lit-ry po gaol. i okhrane nedr. No.67. (UraniumJ Uran. Nauchn.
red.K.K.Kon5tantino,r. Izd.2., parer. 1959. 65 P. (KIRA 13:1)
1. Moscow. Veasoyuznyy nauchno-iasledovatellskiy inatitut minerallnogo
syrlya. (Uranium)
U..
5

3(8) SOV/7-59-2-5/14
AUTHORS: Vaynshteyn, E. Ye., Ginzburg, A. I., Shevaleyevskiy, I. D.
TITLE: On the Ratio of Hafnium and Zirconium in the Zircons of
Granite Pegmatites (0 sootnoshenii gafniya i tairkoniya v
tsirkonakh grs.nitnykh pagmatitov)
PERIODICAL: Gookhimiya, 1959, Nr 2, pp 124-129 (USSR)
ABSTRACT: 25 samples of the zircon group were investigated by the X-ray
spectrographic method. The samples were: 1) zircons from
medium- and coarse-grained plagioclase-mireocline-biotite
pegmatites (Table 1
Analyses 1-7); O-7-1-4%HfO
1 Zr0
/HfO
2
2
2
between 46 and 89. Cirtolites from uranium - rare earths
;)
pegmatites (Table 1, Analyses 8-15); 2-7-6 ' V,4 HfO , ZrO 111f0
9-21. 3) Cirtolite from a beryl - muscovite pegmaiite (Kble2j,
Analysis 14); Hf02 3.3%, ZrO 2/Iffo 2 17-3. 4) Cirtolites from
strongly albitized pegmatites (Table 1, Analyses 15-18);
5.3-7.4 % Hf02, Zr 02 /HfO 2 8 - 11.5- 5) Late cirtoMes from
replacement pegmatites bearing rare metals (Table 19 Analyses
19 - 24); 6.6 - 13-8% Hf02' the Zr 02 /11fo2ratio varies be-
Card 1/2 tween 3-7 and 9.1. Table 2 is a summary of table 1. This in-

SOV/7-59-2-5/14
On the Ratio of Hafnium and Zirconium in the Zircons of Granite Pegmatite6
vestigation shows that hafnium is enriched in the course of
the pegmatite process while the zirconium-hafnium ratio de-
creases; early formed zircons correspond completely to the
zircons contained in granites. In pegmatites descended from
alkali syenites or granosyenites zircons habe a strikingly
high zirconium-hafnium ratio. This may be used in determining
genetic relationships. Zircons of metasomatic origin have a
ZrO2/11fo2ratio of between 3 and 20, while the ratio to be
found in zircons from pneumatolytic - hydrothermal ore veins
ranges from 25 to 45. Zircons of the last stages of the peg-
matitic process contain up to 14% Hf02 1 they may be regarded
as hafnium minerals proper. There are 2 tables and 9 Soviet.
references.
ASSOCIATION: Institut -eokhJ.mii i analatichaskoy khimii im. V. I. Vernadskogo
AN SSSR (Institute of Geochemistry and Analytical Chemistry
imeni V. I. Vernadakiy AS USSR). Vsesoyuznyy institut mineralL
nogo syrlya.Moskva (All-Union Institute of Mineral Raw Material~,
Moscow)
SUBMITTED: November 13, 1958
Card 2/2

GINZBMG, A.I.
New ty-Pee of rare metal deposits. Gaol. rud. mestorozh. no-3:34-47
M7-Je '59. (MIRA 12:10)
l.Vsesoyuznvy inatitut mineral'nogo syriya. Moskva.
Ore deposits)

GINZBURGj.,A.!.) ZHURAVLEVA, L.N.
Genetic types of deposits of rare earth elements. Geol.
meot. red. elem. no.3:59-103 159. (MIRA 14t7)
(Rare earth metals)

GINZBURGJ, A.I.
Conclusion. Geol.. mest. red. elem. no.3:104-109 159.
(Pare earth metals) (MIRA .14:7)

S/081/62/000/CO8/015/057
B160'/B1O1
AUTHOR: Ginzburg, A. 1.
TITLE: Aspects of Cermanium geochemistry and prospectin6 indicators
of rich germanium ores
PERIODICAL: Referativnyy zhurnal. Khimiya, no. 6, 1~62, 94, abstrL~ct
BG7 (Geol. mest.o,-,ozhd. redk. elementov. MI., Goo,--Ieoltekhizdat,
11c. 5, 1959, 86-91)
TEXT: Pub!--"shed data on the Eeochemistry of t-,7er.-,a-1iuM are examined and
consolidated from the point of view of cr~stal-chemical features and the
redox potential of the medium. Conclusions are drawn concerninE, the
conditions under which deposz-ts of Ge minerals and prospecting indicators
lacilitating the discovery of rich Ge ores are formed. rAbstracter's
note: Complete translation.]
Card 1/1

GINZBURG, A.I.
Relation between nnclosing rocks and granite-boaring pegmatiten
of the soda-lithium type. Trudy Min.muz. no.9:53--58 '59.
(MIRA 12:6)
(Mineralogy)

30)

AUTHOR:
--- "-() il'20-124-4-51167
Ginzburg' A. 1.
-------
-
TITLE: ------------------
Sulfide Conoretionary FormuLion in the Coul jeums of the An6ren-
skoye Deposit (Sullf-idnyye, konkretsionnyye obrazovaniya v ugoll-
ny!Lh plastakh Angrenskogo mestorozlideriiya)
PERIODICAL: Doklady Akademii nauk SSSR, 1959, Vol 124, Nr 4, PP 907-910 (USSR)
ABSTRACT: There are only a few data on Lot.- above mentioned formations avail-
able in publications though concretions are important to the
genesis of coals. They are briefly described -in the present paper,
The deposit mentioned in the title belongs to the Middlp Jurassic
and is divided into two parts (lower coal seam, 30-50 m thick,
simple structure- upper part - complex alternation of coal seams
'k
he coal is described in detail. The above mention-
with the rock),
ed concretions occur more frequently in the coal aeams than in the
rock; in the latter case, however, they are to be found only at
the contact point with the c3al seam (Fig 1). In the lowe--, seam the
concretions are irregularly distributed throughout the coal ma8s and
are bound to their individual horizon8. They are often accumulated
(Fig 2). In the North there are much more concretions than 2 km
south in the same part of the seam. In the South lenticular forma-
Card 1/4 tions predominate while in the contral part and in the North there

SOV/20-124-4-51//67
Sulfide Concretionary. Formation in the Coal Seams of the Angrenskoye Deposit
is a somewhat larger amount of ball-shaped and bump-like inclu3ions.
Thus, it-could not be observed teat the concretions are rigidly
bound to certain seams and horizons.. The concretionary forms are
shown in figure 32 1,2 and are described in details. In a macro-
scopic sense, almost all of them are yellow with various shades,
The crystalline structure is not always dientinctly marked.. Their
specific weight is high,, Under the microocope (Linder the soiaist3nre
of B., B. Rozina) iron disulfide (primarily pyriteo, les's inarcaqite
with a small amount of melnicovite) wai detected. The spectroscopi,;
analysis (Table 1) shovied the oi~cuirence of molybdenum, copper,
lead, zinc, and germanium, as well as a considerable amount of ar-
senic. Provided the respective con,~retionv are contained directly
in the coal, there aze splinters of plant tissues in good condi 'tion
to be seen under the microscope; whic:h are mineralized by the Sul-
fides, with the only exception of a cake-shaped pyriti,:: concretion
(Sample 239) on the base of the r1oal eeam., A large amount of plant
residues is mineralized by inarcasite here. Only interstices are
filled with pyrite which probably was formed a little later (Fig
There are also some concreti,)naxy format.-;-ons representing pseudo-
morphs of wood splinters., Herp it can be clearly observed that the
Card 214 channels in the wood are filled with sulfurous iron solutions,

SOV/20-124-4-51/67
Sulfide Concretionary Formation in the Coal Seam3 of tne Angrenskoye Deposit
The organic substance of tile concretions is represented primarily
by plant tissues (wood). In individual cases, annual rings and
also tracheids are visible. The plant group cannot be determined.
From the observations the following assumptions may be made: the
concretions were formed in situ. Apparently, iron in the form of
oxide as well as sulfur were present in the swamp water; sulfur
waa produced by the reductive medium. The apecific medium caused
the reduction of trivalent to bivalent iron which represents a
constituent of iron disulfide. It may be supposed that iron disul-
fide had been deposited first as melnicovite which afterwards
crystallized to pyrite and marcasite, according to conditions,, The
plant tissues which are in good condition (e.g. compressed trunks)
indicate that concretionary formation began in the early period of
peat accumulation. In the peatbog all processes of transformation
and the solidification of tile plant material were not yet finished.
Consequently, the concretions were formed before the diagenesis of
the entire peat deposit.- There are 3 figures and 1 table,
Card 3/4

30'VI20-124-4-5!167
Sulfide Concretionary Formation in the Coal Seams of the Angrenskoye Deposit
ASSOCIATION: Vaesoyuznyy nauchno-iseledovatellskiy geologicheskiy institut
(All-Union Scientific Research Institute of aeology)
PRESEVTED: June 20, 1958, by N,3 M, Str8khov, Acudemician
. SUB14ITTED: June 3, 1958
Card 4/4

PATROVSKAYA, N.V.; JMIMMKO, N.G:; nauchnyy red.;
MOMOT, A.D., glevnyy red.; CHMHOSVITOV, Yu.L., zam. glavnogo
red.; SHKOMMOV, I.V.o zam.glavnogo red.; ZYNHEY, L.V., red.;
ZUBAIU,'V, N.H., red.; MYTER, VA.,, red.; KOKR(XJSOV, V.A.. red.;
SOLOV113Y, D.V., red.; KHRUSHCHOV.,N.A., red.; SI!OMOV. A.G.,
red.izd-va; IVANOVA, A.G., tekhn.r4d.
[Industrial requirement for the quality of mineral raw materials;
handbook for geologintel Treboveniia promyshlennosti k kachestvu
mineralinogo syrlia; spravochnik dlia geologov. Izd.2., parer.
Moskva. Gos.nauchno-tekhn.izd-vo lit-ry po geol. i okhrane nedr.
No.71. [Selenium and tellurium] Selen i tellur. Nauchn.red. A.I.
Ginzburg. 1960. 45 p. (MIU 14:1)
1. Moscow. VeesOYU2]lyy nauchno-issledovatel'skly inatitut mine-
rallnogo syrtya.
(Selenium ores) (Tellurium ores)

SHCHERBINA. 7.T.; GINZBU-RG,, 4.1-,.__red. vypusim; KALYSHEY, I.I.. red.;
POLTAKOV. P.A., red.; RODIONOV. G.G., red.; STEPANOT, I.S., red.;
TROXWHEV, P.A., red.; FAGUTOT. V.P.. red.; KHRUSHCHOV. N.A.,
red.; CHMOSVITOV. Yu.L.. red.; SHMANINKOV, I.V., red.
ETGEUS, N.A., red.; ROZHKOVA, L.G., red. izd-va; IYERUSALIKSKATA,
Ye.S., tekhn. red.
(Geology of rare metal deposits] Geologila mestorozhdenti
redkikh elementov. No. 8 [Geochemical characterietics of scandium
and types.of its deposite.] Osobennosti geokhimii skandiia i
tipy ego mostorozhdenti. Moskva. Gos.nauch.-tekhnAzd-vo lit-ry
po geol. i okhr. nedr, 1960. 56p. (Geologiia mestorozhdenii
redkikh elementov, no. 8). (NEU 13:11)
(Scandium)

ZHMCHtJZHUIXOT, Turiy Appolonovich; G~#Pt4~(!,--Anna--Il'inichna;
POGRIBITSKIT, Te.O., otv.red.; GODOVIKOVA, L.A., red.izd-va;
BRUZGULI, T.V., takhn.red.
[Principles of coal petrology) Oanovy petrologii w,,lei. Moskva,
Izd-vo Akad.nauk SSSR. 1960. 399 p. (mrRA 13:2)
(Coal geology)

GINZBURG. A. I.; GOILMIEVSLAYA, S.A.; YNROYMVA, Ye.A.; SIWIaNKO. G.J..
Chemical composition of tetragonal titanium-tantalum-
.t' niobaten. Geokhimiia no-1:11-30 160. (MM 13:6)
(Fergusonite)

GINZBURG, A.I., RODIONOV, G.G.
Subsurface formations of granititc pegmatitites. Geol. rad. mesto-
rozh. no.1:45-54 J.&-F 160. (MIRA 13;7)
1. Viesoyuznyy institut minerallnogo ayrlya, MOBkva.
(Pegmatites)

S/081/62/000/010/028/085
B177/B144
AUTHORSt Gorzhevskaya, S. A.
TITLE: Characteristics of titanium-tantalum-niobates
PERIODICAL: Referativnyy zhurnal. Xhimiya, no. 10, 19,~2, 108 - 109, ab-
strict IQG61(~;b. "Geol. mestorozhd. rodk. ele*qntov" . no. 10,
Mi., GoageolLekhizdat, 1960, 5 - 10) r
TEXTj The composition of titanium-tantalum-niobates is-i...onventionally
represented by the formula A MBpXq , where A and B combine'*r-ations of
closely similar dimensions. lit many of them, the group A cations are lesq-
strongly bound with oxygen than group B cations. Gro-up A includes cation~,',
with large R s Cat Nat Y, TR, Th, U, and to a lesser extent Kp Pb, Bat
Sr, Lin and others. Group B includes cations having relatively small R iI
Ti, Nb, Ta, W and also Al, 'Sip P and others. For several titanium-
tantalum-niobates, group A may usefully be subdivided into two sub-groups,
1 - 2 1 2' 2+
A ana A , whemof A includep Cat Nat U, Th, TR whilst A .includes Fe
Card 1/2

Characteristics of...
S/081/62/000/010/028/085
B177/B144
Mn, 11g. In many cases a deficiency of cations exists in group A. In the i,
minerals described, both isovalent and heterovalent substitutions are
widely developed. It is observed that, as the ratio betw6en atomic
quantities of cations in group A and the atomic quantities of oxygen in-
creases, the syngony of titariium-tantalum-niobatea decreases. The variable
composition of many minerals is governed by the different p-roces8ea that
change them, which mostly take place under hydrothermal conditions.
Probably the processes of change are connected with the extraction of water
and with.the partial leaching ofoatione in group A besides others. LAb -
stracter.'s notes Complete translation]
Card 2/2

510811621-000101010321085
B177/B144
AUTHORSS Ginzburg, A. I., Gorzhevakaya, S. A.
TITLEt Cubic titanium-tantalum niobates. The co osition of the
rare-earth elements tTl
PERIODICkLi Referativnyy zhurnal. Khimiya, no. 10, 1962, 109, abstract
lOG66 (Sb. "Geol.' westorozhd. redk. ellementov", no. 10, Y,.,
Gosgeoltekhizdat, 196o, 84 - 89)
TEXT. The minerals of the perovskite type related to ultrabasic alkaline
intrusive complexes, are highly selective Ce minerals,.though they also
contain La, N'd, and some Sm. Pyrochlores from carbona-tites, alkaline
beds and their pegmatites possess a constant TR conjosition. There is a
marked predominance in them of elements in the Ce group, with slight
quantities of Gd and Dy. In pyrochlores from albitites~'related to sub-
alkaline granitoids, TR of the Y sub-group occur in slight q~iantities.
In pyrochlore-type minerals encountered in granitic pegmatites, the TR
content is very variable. A typical feature of them is the higher content
of the middle members of the series TR - Sm, Gd, Dy, and sometimes Ce.
r
;Abstracter's notei Complete translation-3
dard 1/1

5/G81/62/GCO/010/035/C85
B177/Bl-44
AUTHORS& Ginzburg, A. I., Gorzhevskaya, S. A.
TITLEt Tetragonal tantalum-niobates. Composition of rare-earth
elements
P*--iIODICALt lleferativnyy zhurnal. Khimiya, no. 10, 1962, 110, abstract
lOG73 (Sb. "Geol. mestorozhd. redk. elementov". no. 10, W.,
Gosgeoltekhizdat, 1960, 144 - 152)
TEXT& Fergusonites are distinguished from other titanium-tantalum-
niobates by their content of Y and TR Y sub-groups. The content of Y
fluctuates from 40 to M.' of the entire TR content.' Different genetic
types of fergusonites are characterized by a specific TR composition. In
some types of deposit, fergusonite is a substant 'ially ytterbium-bearing
-mineral (unsubstituted granitic pegmatites); in others, dysprosium-
ytterbiam-bearing (accessory in granites); substantially dysprosium-
bearing quartz albitites conylected with granosienites); cerium-dysprosium-
bearing ~alkaline pegmatites); neodymium-dysprosium-:Dearing (albitised
alkaline beds and albitised granitic pegmatites). The ratios in
Card 1/2

Tetragonal tantalum-niobates...
ler,wusonites,TY s'~Ce,
1. L~
enabling one to Judge
beds and to different
Complete translation.1
S/061/62/000/O1o/o5a/o85
B177/B144
Yb i Dy, and Ce t Nd may be regarded as indic,~tive,
the relation of fergusonitesto various intrusive
genetic types of deposits. I-Abstracter's.notet
Card 2/2

GIRZBURG, A.I.-.-DOP-ZHEVSKAYA, S.A.; YEROFELEVA, Ye.A.; SIDOIQX0, G.A.;
-----VLYSIU,;V, I.I., red.; POLYAKOV, I.I.V., red.; RODIOFCV, G.G., red.;
STITAPOV, I.S., red.; TliOrvl!ACIIBV, P.A., red.; FAGUTOV, V.P., rod.;
KIUWSIICIIOV, N.A., red.; CIMPTOSVITOV, Yu.L., red.; SIRVIFE11YOV, I.V.,
red.; SHCHERBUIA, V.V., red.; EYGELES, M.A., red.; VERZ"OVA, G.F.,
red.izd-va; BYKOVA, VoV., teldm.reda
(Titanates, ttntalates, and niobettes) Titano-tantalo-niobaty.
146skva. Gos. nauchno-tc'xhr.!!,,rl-vo IJA-i7, po f,-,eol.i ol-lirene nedr.
Part 1. 1960. 166 p. (Goologiia mostorozhdenii redklikh elonentov,
no.10). (IaTU, 14:6)
(Titanates) ~%Tantalates) (Viobates)

PYATVOVY VJ.; BIBIKOVA, V.I.; DARVOYD, T,T,~ IVANOVA., R.N.) KASATKINA,
N.A.1 GINOURG, A.I., nauch.Vy red.) NEMANOVA, G.F,, red. izd-7a;
BYKOVJG-- T.-V';-,Te1ffiff-4- -red 0
[Industry's requirements as to quality of mineral raw materials]
Trebo-vaniia pronyahlennosti k kachest-vu minerallnogo syrlia; spravoch-
n1k dlia geolcgo-v. Izd.2., perero Moskva, Gos. nau,-,'nno-.tekhn. izd-vo
lit-ry po geol. i okhrane nedr. No.53. (Thalliun, indium, gallium]
Tal-Iii,, indil, gal-1,11. By V,I.Piatnov i dr. Waachn. red. A.I.Ginzburg.
1961. 53 P. (AURA .1-4. 11)
1. Mos--ow. Vsesoyuznyy nauc!2Lno,--is!)Iedovafoilskiy institut mineral'-
nogo s r1ya.
Nballium) Undium) (Gallium)

GINZBURG, A.I.; VOLZHENKOVAj A.Ya.; POLKUNOV, V.F.
Characteristics of spodumene pegmatites in carbonate rocks. Geol.
rud. mestorozh. no.3.:52-60 Ja-F 761. (MIRA 14:4)
1. Vaesoyuznyy instItut minerallnogo syrlya, Moskva.
(Spodumene)

S '007
16110001'00210041004
B107/B202
AUTHORS: Ginzburg, A. I., Stavrov, 0. D.
TITLE: Content of rare elements in cordierites
PERIODICAL:~ Geokhimiya, no. 2, 1961, 183-185
TEXT: Until recently only little attention has been paid to the composition
of cordierites, above all, to their content of rare elements, although
cordierite ds an especially interesting mineral from this point of view.
Hollow channels were observed in its ring structure which is analogous to
that of beryllium. !jike in beryllium and milarite, the occurrence of large
ions, such as calcium and sodium, potassium,rubddium, and cesium ions which
are isomorphous to it, is expected in these channels, Furthermore, the au-
thors point to the fact that the composition of cordierite is interesting
also from another point of view. As was observed in recent years (A. I.
Ginzburg, G. G. Rodionovj Ref. I)$ rare-metal pegmatites are formed only at
certain depths, and therefore they are found in most cases within metamor-
phic sediments at this depth. Andalusite and cordierite are typical minerals
Card 1/7

Content of rare ...
5/007/61/000/002/004/004
B107/B202
of these rocks. For this reauon, cordierite is frequently found in rocks
surrounding rare-metal pegmatites, and occurs in exocontacts of pegmatite
dikes and in pegmatite dikes as a typical "xenolithic" mineral. Usually,
lithium is transported from lithium pegmatite into the surrounding rocks
where it is fixed in magnesium-containing minerals - biotite and amphibole
which, in turn, are transformed Into protolithionite or lithionite, and into
holmquistite. In this connection, the problem arises whether lithium partic-
ipates in the formation of cordierite, and whether lithium cordierite occurs
in nature. To answer these questions, 0. D. Stravrov analyzed cordierite
samples from various regions of the world for rare alkalies. He obtained
the following results:
Card 2/7

S/007/61/000/002/004/004
B107/B2O2
Content of rare
Origin of sample region Li2 0
from metamorphic sediments Switzerland 0.11
without occurrence of
lithium pegmatites
from metamorphio sediments in Norway 0.02
regions with alkali maasives
from metamorphic sediments in Bavaria 0.02
regions with occu=ence of Madagaskar 0.043
pegmatites Northern
without lithium minerals Pribaykal'ye 0.043
From endo contact zones of Ural,
pegmatites without lithium Murzinka 0.19
minerals
from endo contact zones of Turkestan-
beryllium-muscovite pegmatiteS skiy Range 0.43
containing triphyline
Tables I and 2
Rb 2 0 C.92 0 BeO
not found M04
n.f. n.f. 0.004
n.f. n.f. 0.04
n.f. n.f. 0.005
n.f. n.f. n.f.
0.005 0.023 0.16
n.f. n.f. 0.0052
Card 3/7

Content of rare ...
Origin of sample region
from metamorphic sediments at Eastern
certain distances Siberia
from spodum-,ne pegmatites
from metamorphic sediments Eastern
near OLMAILMOtIV P(,LJ,'IIIatite8 Siberia
S/007/61/000/002/004/004
B107/B202
Tables 1 and 2
Li2 0 Rb20 Cs20 BeO
0.24 n.f, n.f, 0.004
0.64 0.05 0.2
Pure cordierites were analyzed, some of which had been collected by the au-
thors, while others had been made available by L. G. Fel'dman and I. N.
Timofeyev from the collections of the Mineralogicheskiy muzey AN SSSR im.
akad. A. Ye. Fersman (Mineralogical Museum AS USSR imeni Academician A. Ye.
Fersman). Lithium analyses were made by flame photometry. Rubidium and
cesium were analyzed directly by spectrum analysis (A. K. Rusanov, V. G.
Khitrov, N. T. Batova, Ref- 3), The following conclusions can be drawn fran
the data mentioned: (1) The maximum amount of lithium is contained in
cordierites from areas with lithium pegmatites. A lower amount is contained
in cordierites from beryllium pegmatites which contain only sinall amounts of
lithium. (2) Cordierite also contains Cs, in some cases even up to tenth
Card 4/7

S/007/61/000/002/004/004
Content of rare ... B107/B202
Apparently, Cs occupies the same place in cordierite as in beryllium. Like
in beryllium, the amount of Cs is much larger than that of Rb. Since
cordierite is a magnesium mineral, lithium contained therein apparently re-
places magnesium, much like in mica, tourmaline and amphibole. This replace-
ment may take place in two wayst (A. I. Ginzburg, Ref. 4). (a) Two magnesium
ions can be replaced by lithium and aluminum 1 2 Mg 2+ (-- Li++ A13+. With
the cordierite composition (Mg, Fe )2 Al3[si 5Alo 1.1, the lithium analog of
cordierite will have the following composition in the case of the mentioned
replacements LiAl 4 Si5A10 113; (b) the magnesium ion can be replaced by
lithium; valency is compensated such that aluminum is replaced by silicon
having a coordination number of four, i. e., Mg2+ Al + (--Li +
(VI)_'_ ~Iv) (VI), si~+
IV)-
In this case lithium cordierite will have the following composition:
(Mg, Fe)LiAl 31S'601 ]or (Mg, Fe)LiAIA12 [Si 601]which is close to the beryl-
lium composition: Be 3Al 213'60181' The lithium-containing cordierite of the
composition (Mg, Pe)LiAlAl2 r"601.1 differs from beryllium in that it contains
Card 5/7

S/007/61/000/002/004/004
Content of rare ... B107/B202
one magnesium, lithium, and aluminum ion instead of the three beryllium ions.
In this connection it should be added that N. V. Belov (Ref. 5) regards the
replacement of beryllim by lithium as possible since he assumes that lithium
may have a coordination number of six four. Also the replacement of beryl-
lium by aluminum is regarded as possible. R. E. Folinsbee (Ref. 6) assumes
that the replacement of beryllium by magnesium is possible without essential
structural changes. Since beryllium and cordierite have the same structure
it can be assumed that beryllium may enter the cordierite structure (A. I.
Ginzburg, Ref. 7). For this reason R. D. Pavlova made quantitative analyses
of beryllium oxide in various cordierites in the spectral laboratory of the
authors' institute. As may be seen therefrom no large amounts of BeO are
found in the cordierites. The largest amounts - between 0.15 and 0.20.% -
are found in cordierites from some pegmatite deposits. Cordierites from
metamorphic sediments contain almost no beryllium oxide. The following
conclusions can be drawn: (1) owing to their ring structure cordierites
may contain - similar to beryllium - considerable amounts of alkali, Na, Li,
Cs. (2) Cordierites may be enriched with Cs. (5) Cordierite may serve as
characteristic mineral indicator of the occurrence of lithium pegmatites.
(4) Natural occurrence of a Li cordierite of the composition LiMgA'3[Si6Ol8]
Card 6/7

Content of rare ...
S/00 61/000/002/004/004
B107YB202
is possible. [Abstracter's note: Complete translation]. There are 2
tables and 7 references: 6 Soviet-bloc.
ASSOCIATIONt Vaesoyuznyy nauchno-isaledovatel'skiy institut mineral'ziogo
syr'ya, Moskva (All-Union Scientific Research Institute of
Mineral Raw Materials, Moscow).
SUBMITTED: March 18, 1960
Card 7/7

8/0131/62/030/010/024/085
B1 30101
A L" i'H J R Ginzbur~-:, A.
T IT LE :TOW data on the :lLneralogy of deposits of rare elements
PERIODICAL; Haforativnyy zhiirzial- Mii~no.10, 1962, 102, abstract IOG12
(6b. 111;eol. uieawr*ozhl. redk. elementov". rl'oi. 9,
Gos,-Poltokhizd%t, 1~,61, 3 - 27)
TEYT: This is a review of tho most important new data obtained fr_)m 1956
to 1~59 as a. rosult of mineralaGical investigations covering different
types of rare metal depositsi 1) granite ranges enriched by accessory
rare metal mineraLs, .tnd plac,~r deposits connected aith them; 2) Granite
peF,aatites; 3) pneumatolithic hydrothermal formations connected with
granites; 4) the pegimatites of alkaline mab-mas; 5) pneumatolithic hydro-
thermal formations connected aith alkaline rock (albitito's); '6) carbon-
atites; 7) hydrothermal deposits of rare earth formatioPs. [Abstracter's
note: Complete translation.]
Card I/I

GINZBUK,--~- NAZAROVA, A.S.; SUKEOPIAZOVA, L.L.
Nigerite from Siberian permatites. Geol-mest.red.elem. no.9:
61-67 '61. (MIRA 14:9)
(Siberia--Nigerite) (Siberia--Pegmatites)

GIMLBURG, A.I.; YAKOVLEVA, M.Ye.
Some phenomena of the redeposition of spodumene in pegmatites.
Trudy Min. nuz. no.11:3-12 161. (I-aRA 16:7)
(Pegmatites) (spodumene)

ORLOV, YU.L.; GISZBURG, A.I.; PINEVICH, N.G.
Paragenetic relationiships between beryl minerals in certain veins
of pegmatites. Trudy Min. nme. no,11:103-113 161.
(KIRA 16:7)
(Beryl) (Peginatites)

KUM~TCJVA, V.A.; GINZBURG, A.1,
Hydroxyl-herderite froin pegmatites of Transbaikalia. Trudy
Kin. muz. no.11.175-180 761. (MRA 16:7)
(Transbaikalia-.-Elerderite)
(Transbaikalia-Pegmtites)

-_~~N~~URG; A. I.
Some regularities in the distribution of rare metal pegmatite
fields. Trudy IGE14 no.41:37-47 161. (IMU 14:8)
(Pegmatitoo)

a~~BURG,_A.Lj RODIONOV,, G.G.
Criteria for prospecting for and evaluating rare-metal pegmatites
as propoodd by K. Le Vlasov. Sov. geol. 4 no.3:127-132 Mr '61.
(MIRA 14:5)
1. Voesoyuznyy nauchno-issledovatel'skiy Institut minerallnogo
syr,ya.
(Pegamites)
(Setals, Rare and minor)

, GINZBURG., A.I.p doktor geol.--mineral.nauk
I - I --I------- - - - -.-- -
"Handbook on minerals." Vol. 1. Reviewed by A.I.Ginzbur Vest,.
- -10)
MIRA 14,
AN SSSR 31 no.9:144,146 5 961.
(Minerals-Handbooks, *muals, etc.)

.~ZBTJR,G A.I. ,
ABDIJLIAYEV, Kh.M.; RI
Claosification of granite pe&rmatites. Sov-geol. 5 no.1:71-81
ja 162. (MIRA 15:2)
1. Vaesoyuznyy nail hn -issladovatellskiy institut minerallnogo
syrlya.
(Pegmatites--Classification)

TERENT'YEVA, K.F.; pIjtZLURG, AtI-, vlavnyv ro-d.; 1"AlYCHEV, I.L., red.;
RODIONOV, G.G., red.; I,Sjj red.; TI(Al"ACHE71, T red.,
FACUTOV, V.P., red.; i-Taljncl!~N' red.; CHERNICS11ITOV, Yu.L.'
red. -,',ISFMANEfIKOV, IN., red.; Lif'OHERBINA, V.V., red.; EYGEU'S, M.A.,
red.; ROMKOVA, L.G., redAzd-va; GUROVA, O.A., t(Ahn.rpd.
[Hare elements in bauxites] Redkie
Gos.nauchn-tekbn. izd-vo lit-ry po
(Geolopiia mestorwhdenil redkikh
(Metals, Rare and minor)
elementy v boksitakh. Foskva,
geolA okhr.nedr, 1959 47 1).
elementov no.6). (Mil'('~ 13--12)
(13auxiteY
I-

SHEYNHANN, Yu.M.j AFELITSIN, F.R.; NBCHAYE;VA, Ye.A.; GINZBURG A.I. red.;
NALYSM, I.I., red.; POLYAKOV, M.V., red.; !16i~ G.10 red.;
S~EPANOVt I.S., red.; TROKHACHEV, P.A.,, red.; FAGUTOV, V.P., red.;
KHRUSHCHOV, N.A... red.; CHUMOSVITOV, Yu.L., red.; SHMANENKOV, I.V.,
red.; SHCHERBINA, V.V., red.; BYGELES, M.A., red.; ROZHKOVA, L.G.,
red.izd-va; BYKOVA, M., tekhn.red.
[Alkaline intrusions their distribution, and the mineralization
associated with theml Shchelochnys intrazii, ikh razmeshchenie i
sviazannaia a nimi mizieralizataiia. 14oskva, Gos.nauchno-tekhn.
izd-vo lit-ry po geol.i okhrane nedr, 1961. 176 p. (Geologiia
mestorozhdenii redkikh elementov, no.12/13). (MIRA 15:8)
(Rocks,, Igneous) (Ore deposits)

ZABOLOTNAYA, N.P.; NOVIKOVA, 14.1.; SHATSKAYA, V.T.; GINZBURG A.I.,,
glavnyy red.; POLYAKOV, M.V., zam. glavnogo od..-
F.R., red.; GRIGORIYEV, VA, red.; RODIONOV, G.G., red.;
TROKHACHEV, P.A., red.; FAGUTOV, V.P., red.; KBRUSHCHOV, N.A.,
red.f CHERNOBVITOV, Yu.L., red.; SHMANENKOV, I.V., red.;
SHCHERBINA, V.V., red.; EYGELES, M.A., red.; KOLOSHINA, T.V.,
red. izd-va; BYKOVA, V.V., tekhn. red.
(Tungeten-molybdonum--tin-beryllium deposits and their formation].
Vollfram-molibden-olovo-berillievye mestorozhdoniia i usloviia
ikh obrazovaniia. Moskva, Gosgeoltekhizdat, 1962. 94 P. (Geo-
logiia mestorozhdanii rodkikh elementov, no 18).
?MIRA 16:4)
(Metals, Rare and minor)

, A.I., glavnyy red.; POLYAKOV, M.V.1
SHVEY, Igor' Vladimirovich; CaSZDaRG
zamestitell glavnogo red.; APELITSIN, F.R., red.; GRIGORIYEV, V.M.,
red.; RODIONOV, G.G., red.; SrEPANOV, I.S., red.; TROKHACHEV, P.A.,
rqd.; FAGUTOV, V.P., red.; KHRUSHCHOV, N.A., red.; CHERNOSVITOV,
N.L., red.; SHMARNKOV, I.V., red.; SHCHERBINA, V.V., red.;
EYGELES, M.A., red.; ENTIN, M.L., red.izd-va; BYKOVA, V.V., tekhn.red.
(Basic geochemical problems of rare earth elements and yttrium in
andogenic processes] Oanovnye voprosy geokhimii redkozemellnykh
elementov i ittriia v endogennykh protsessakh. Moskva, Gos. nauchn.-
takhn. iad-vo lit-ry, po geologii i okhrane nedr, 1962. 105 p.
(Geologiia mestorozh(lenii rodkikh elementov, no.15)9 (KRA 15:11)
(Rare earth metals) (Yttrium)

EPSHTEYN, Ye.M.
Conclusion; main problems in studying the massifs of ultrab"Ic
alkali rocks and carbonatites. Geol. mest. red. elem. no.17:
142-147 062. (KERA 16:10)
(Ultrabasi te) (Carbonatites)

GINZBURG, A. I.
Petrographic characteristics of sapropelites a rd saprohmoliths.
Sov.geol- 5 n'o.81-62-78 Ag 162. (MIRA 15:9)
1. Vaesoyuznyy naucho-issledovatellskiy ge~logicheskiy inkR,itut.
(Sapropelites)

GRABOVSKAYA, Lidiya Ivanovna; ASTRAKHAN, Yevgeniy Davidovich;,,GINZBURG, A.
I., glavnyy red.; POLYAKOV, M.V., zam.glavnogo red.; K6LOSfftNA*., T.
V-., red.izd-va; DYKOVA, V.V., tekhn.red.
(Biochemical and geobotanical studies in prospecting for rare-
metal deposits.] biogeokhimicheakie i geobotanicheskie issledo-
vaniia pri poiskakh redkometalInykh mestorozhdenii. Moskva, Gos-
geoltekhizdat 1963. 62 p. (Geologiia mestorozhdenii redkikh ele-
mentov, no.iq~. (MIRA 17.-2)

STAVROV, 0 . D. 1.4 Z BURG,'A.I., glavnyy red.; POLyAKOV, M.V., zam. glav-
nogo red..,
~-APEVISWT.R., red.; GRIGORIYEV, V.M., red.; RODIO-
NOV, G.G.J. red.; STEPANOV, I.S., red.; TROKHACHEV, P.A., red.;
FAGUTOV, V.P., red.; KHRUSHCHOV, N.A., red.; CHERNOSVITOV, Yu.L.,
red.; SHMANENKOV, I.V., red.; SHCHERBINA, V.V., red.; EYGELES,
M.A., red.; FEDOTOVA, A.I., red.izd-va; IYERUSALIMSKAYA, Ye., tekhn.
red.
[Basic characteriotics of lithium, rubldium, sesium in the process
of the formation granite Intrusives and the pegmatites connected
with them.] Osnovnye cherty geokhimii litiia, rubidiiat tseziia v
protsesse stanovleniia granitnykh intruzivov i sviazannykh s nimi.
pegmatitov. Moskva, Gosgeoltekhizdat 1963. 140 p. (Geologiia Ses-
torozhdenii redkikh elementov, no.21~- (MIRA 17:2)

EGELI, Lev Yevenlyevich; YERSHOV, A.D., glavnyy red.; ZUBREV, I.N., zam.
glavno red GUDALIN, G.G., red.; KHASNIKOV, V,I., red. [de-
ceaseT.KORE~LKOV, B.Ya., red.; MOMDZHI, G.S., red.; POZHARITSKIY,
K.L., red.; SMIRNOV, V.I., red.; POLOVOV, A.P., red.; TROYANOV, A.
T., red.; FILIPPOVSKAYA, T.B., red.; KHRUSHCHOV, N.A., red.; CHER-
NOSVITOV, Yu.L., red.-..GINZBURG, A.I.. red.vypuska; PROKOFIYEV, A.
P., red.vypuska-, SOKO eY , red.izd-va; BYKOVA, V.V.,
tekhn.red.
(Rare-earth metals.] Redkozemellnye metally. Mook-va, Gostoptekhiz-
dittv 1963. 332 p. (Otsonka mentorozlidenil pri polakukh I razvadkAkh,
no.21). (MIRA 17:2)

A. I. GINSBURG (USSR)
"The peculaties of rare-elements concentration in endogenic processes."
Report presented at the Conference on Chemistry of' the Earth's Crust,
Moscow, 14-19 Mar 63.

r,
I I k: rlw. Mi~ f';

GINZBURG9 A.!., BEREZRO, SHARM1119 NU.
I
Surface studies of' iierJul anomalipej o,' 5,-,,mf4
types of rare mo-tal deposits. Gool.-Iym4. r&'I. elmn. no.20,,
84-115 163. (M-1 PA 17 4 5,
M,P ~.. .

UNKSOV, V.A.; BOROVIKOV, P.P.; RUNDKVISTY D.V., -'AVLOVA, I.G.;
ALYAVDIN, V.F.; VOLOSTIIYKH, G.T.- ROZINOr, M.I.,Y SHCHEGLOV, A.D.;
9
IVANOVA, A.A.; KORMILITSYN, V.S.; SHCHEG-,OV, A.D.; ARTEMOV, V.R.;
RYTSK, Yu.Ye.; GINZBURCs. A ,_;. DORTMAN, I.B.; TOPORETS, S.A.;
-- ~ --T
TRUNINA, V.Ya., YAK0VLF:V, I..K.; BOGDANOVA, L.A., SARBEYEVA, L.M.
Problems of the geologir and characteristLes of the distribution
of mineral deposits. [Trudy] VSEGEI 92i53-89 163. (MIRA 17%4)

GInBluna, P-1,
Genetic classification of humic coals. Izv. M SSSR Ser. geol.
29 rio.7:94-98 Jl 164 (MIRA 3.9.-l)
1. Ilsesoyuznyy nauchno-isfiledovatellskiy geologicheskiy institut,
Lanlngrad.

G1112BURG, A. 1.
Flxa~,ant 8-tat-us Of 5tudles of ptgmat.i ee and probllea..3 frr
~nrvestigalllon. Geol. mat. red. el6m. no.2234-11'~/-
!I-upvt llo)
Eff-2,-,t- of exterT;---! Ci on T,111,;~ of '.ho 1)~_gmaitit
pro.-.-e3g. lb 11 d . ;7 4-8 'IL"

GLTLZBII~~.--. ~UTSKAYA, V.T.
Some data on the migration of in the supe-1-9pne zone of
a fluorite-berryllium deposit. Dakl. AN SSSR 159 nc.5-.WD-1-105~1
D 164 (MIRA 18-.1)
1. Predgtarleno akademkom D.S. Xrvshl~gum.

GORZHEVSKAYA, Susanna Aleksaildrovna; SIDORENKO, Galina Aleksandrovna;
GINZBURG, A.I., glavnyy red.; FOLYAKOVI M.V., zamestitell glavnogo
FO',; APELITSIN, F.R., red.; GRIGORIYEV., V.M.p red.; RODIONOV, G.G.,
red.; STEPANOV, I.S., red.; TROKHACHEV, P.A., red.; FAGUTOV, V.P.,
red.; CHERNOSVITOV, Yu.L., red.; SIDIAUENKOV, I.V., red.; SHCHERBINA,
V.V., red.; EYGELES, H.A., red.
[Titano-tantalo-niobates. Part 2.) litano-tantalo-niobaty.
Moskvap Nedra. Pt.2. 1964. 115P. (Geologiia me3torozhdenii
redkikh elementovo no.23) (MIRA 18:1)

VIASOV, K.A.; BELOV, N.V.; VOLIFSON, F.I.; GENKIN, A.D.; GI-NIZ-BURG, A.I.;
LUKIN, L.I.; KORZHINSKIY, D.S.; SALTYKOVA, V.S.; SAUKOV, A.A.;
SOKOLOV, G.A.; SHCHERBAKOV, D.I.; SHADLUN, T.H.
Konstantin Avtonomovich Nenadkevich, 1830-1963; obituary. Geol.
rud. mestorozh. 6 no.1:123-125 Ja-F 164.
(MIRA 17:11)

BLOKH, A.M.; KOCHENOV, A.V.; GINZBURG, A.I., glavnyy red*; APELITSINP F.R., red.;
GRIGORIYEV, V.M., red--P~ DiAKOV, M.V., red.; RODIONGV, G.G., red.;
; 0
STEPANOV., I.S., red.; TROWCHEV, P.A., red.; FAGUTOVI V.P.J. red.;
CHERNOSVITOVJ, Yu.L., red.; SDJANENKOV, J.V., red.; SHCHERBINA, V.V.,
red.; EYGELES, M.A., red.
(Impurity elements in bone phosphate of fossil fishes.] Elementy-
primesi v kostnom fosfate iskopaemykh ryb. Moskva, Nedra, 1964.
106 p. (Geologiia mestorozhdenii redkikh elementov, no.24).
(V~ 19-. 1)

KUDRINO V.S.; KUDRINA,, M.A.j SHURIGAO T.N.1 q1.) -vnyy red4;
gAURGO,A.1.0,gla
AFELlTSIN,.F,R,,-zaxriistitel' glaynago redaktora; CifERIIYSHKVA,,
I.*V.,, red.; BEUS, A.A,,,red.; GREKVLOVA,, L.A6t red.;
GRIGORIYEV, V.Mo,,,red.; ZABOLOTKAYA9 N.P., red.; MATIASp V.V.p
red.; POKALOV,, V.T., red.; RODIONOV, G.G., red.; STEPANOV, I.S.,
red.; CHERNOSVITOV, Yu.L., red.; SIKANENKOV, I.V., red.
Dlare-metal me tasC'CLa'tic' formations assoaiated ~With subalkaline
granitoi&,] Redkometallnye metasomaticheskie obrazovaniia,
sviazannys s subahcholochnymi granitoidami. Moskva, Nedra,
1965. 145 P. (Geologiia mestorozliderLii redkikh elemei-.4-ov,
no.25) (MIRA 1818)

L-28020-66 EWT.(I)/EWA(
ACC NRi -AP6005300 SOURCE CODE: UR/0413/66/000/001/0038/0030
INVENTOR: Ginzburg, A'. I.; Lemekhov, V. N.; Chernyak, I. N.
ORG: none
TITLE: A rectified voltage regulator. Class 21, No. 177470
SOURCE: Izobreteniya, promyshlennyye obraztsy, tovarnyye znaki, no. 1, 1966, 38
TOPIC TAGS: voltage regulator, electronic feedback, electronic rectifier
ABSTRACT, This Author's-Certificite introduces a rectified voltage regulator which
contains power and analog rectifiers connected to the output of an ac voltage regulat-
or. The device also contains a unit which compares the analog rectifier voltage with
a standard. This comparator acts on the control circuit of the ac regulator. Stabi-
lity under varying load conditions is improved by using current feedback from the pow-
er rectifier load to control a vaviable resistor connected in parallel with the com-
parator.
UDCt 621.316 722.1 621.314.632
1/2

28020-66
ACC NRs AP6005300
5
5
1--power rectifier; 2--analog rectifier;
3--ac voltage regulator; 4--voltage comparat
or; 5--ac regulator control unit; 6--vari-
able resistor; 7--feedback circuit

GINZBURG, A.H
Comparative studies on blood picture in mice of various strains.
Trudy,#.KN SSSR 21 no.4:198-206 '52. (KLRA 10:8)
1. Iz laboratorii onkolDgil (zav. - chlen-korrespondent ANN SSSR
prof. L.K.Shabad) Instituta normallnoy i patologicheskoy morfologii
AM14 SSSR (dir. - akademik A.I.Abrikosov) i kafedry laboratornoi
diagnostiki )zav. - prof. Te.A.Kost) TSentrallnogo institute
usovershenstvovanlya vrachey (dir. V.P.Iobedava)
(BIA)W'O'-
picture. in mice. comparison in various stamina)
(MICE,
blood picture in various strains, comparison)

SAYDAKOVSKIY, AiG., kand.meditsinskikh nauk; GINZBURG,_A.M., ordinator
Nevus flammeus and glaucoma. Oft. zhur. 15 no.5t292-294 160.
(MIRA 130)
1. Iz gla=ogo otdeleniya (zav. - A.G. Saydakovskiy) 1-Y gorodskoy
klinicheskoy bollnitB7 Fecherakogo rayona, Kiyav.
(MOLE (DEPJLkTOLOGY)) (GLAUCOMA)

t.,
GIL, ) Irk 0. .
Opti ,cLtl jeoignation of orxillograro. Ilriborostroorio I-,o.11:26
17 161. (',:IIIA 14: 10)
(Oscillon-ra-h-'r)
u

GINZBURG, A.M., vrach
- --- ------I
Symptom of the digital supradental pressure in the cl-i4ical
aspects of acute odontogenic inflammatory processes. Vope
obshchei stom. 17:64-67 164-
(MIRA 18:11)
1. Dorozhnaya boltnitsa No.2 Yugo-Zapadnoy zheleznoy dorogi.

GINZBURG. A.M.,_jnzh.
--l-l-
Automation of given gradients in the operation of excavating ma-
chines. Makh. stroi. 19 no.6:28-29 Jo 162. (MIRA 17s2)

ZELIGHMOK) G.G.; GRIMM, A.R.,, red.
[Automation of machinery and production processes in road
construction] Avtomatizatsiia mashin i proizvodstvennykh
protsessov v dorozhnom stroitellstve. In.p.) Hosvuzizdat,
1963. 111 p. (MIRA 17-6)

ACC NR, AT7004921 SOURCE CODE: UR/0000/66/000/000/0013/0019
AUTHOR: Vittikh, V. A. (Novosibirsk); Ginzburg, A. N. (Novosibirsk);
Drobyshev, Yu. P. (Novosibirsk)
ORG: none
TITLE: Methods of measurement signals compression Classification and review
SOURCE: Vses. konf. po avtomatich. kontrol i metodarn elektrich. izmereniy, 6th,
'1964. Avtomatich. kontrol' i metody'elektrich. izmereniy; tr. konf. , t. 1: Teoriya
izmerit. info. sistem (Automatic control and electrical measuring techniques;
transactions of the conference, v. 1: Theory of measuring information systems).
~Novosibirsk, Izd-vo Nauka, 1966, 13-19
i
XOPIC TAGS: measurement, inf ation processing, data processing, 4afermetiow
_Xn
C,9njppe0SjQff- A&A
ABSTRACT: Based on ten 1955-66 Soviet sources and one 1962 U.S. source, a
'Classification diagram (see figure) is presented,and modern information -compression
.methods are reviewed. Compression of information by measuring signal statistics
(H. Blasbalg et al. , IRE Trans. , no. 3. Sep 1962) in explained. Another group of
,methods istatiatical coding) usinjIf signal statistics converts a sequence of message$ a
Card 1/3

'A~C NR, AT7004921'
Measurement-information compression:methods
Statistical Generalized Measurement and
coding discratization transmission of
statistical
I characteristics
Adaptive According to
averaged
characteristics
With with
extrapolation interpolation
Effective Qua~i_
effective
:the input into output binary signals. Unlike the preceding method, these methods
preserve the sequence of events '. In the predictive coding method, statistical redun-
dancy is eliminated; only the difference signal (real value minus predicted value) is
transmitted; the well-known delta --modulation method belongs with this group. The
,methods of general discretization are subdivided into two large groups: (1) Averaged-
LCard_ 2.13

ACC NR: AT'100,1921
characteristic group in which the quantization interval is either f3clected from the
maximum frequency of nignal spectrum (Kotel'nikov'n theorem) or in net under the
correlation interval (continuous quasi -stationary signals with unlimited spectrum); in
both cauen, the quantization interval is constant; (Z) Adaptive methods in which the
quantization interval is variable; it depends on the prcscnt signal characteristic (e.g.
its present derivative). The choice of compression method depends or, the demands
of the information recipient, ~,iz. , on-the proximity criteria, complexity of
materialization, permissible signal delay, etc. Methods of compression of signal
,connected with the reduction of its entropy seem promising; of these, most efficient
I
iare the methods of generalized adaptive discretization with extrapolation or interpola.
Pon of signals. Orig. art. has: 2 figures and 11 foirnulas.
PUB CODE: 09 SUBM DATE: none ORIG REF: 010 GTH REF: 001
'i-card -.3-/3

ACC NRt AT7004922 SOURCE; CODE: UR/0000/66/060/000/OOZO/0023
AUTHOR: Vittikh, V. A. (Novosibirsk); Ginzburg,,_.A..'N. (Novosibirsk);
Drobyohev, Yu. P. (Novosibirsk)
ORG: none
TITLE: Method of discretization of measurement signals
SOURCE; Vaes. konf. po avtomatich. kontrol i metodam elektrich. izmereniy, 6th,
,1964. Avtomatich. kontrol' i metody 161ektrich. izmeireniy; tr. konf. , t. 1: Teorlya
,izmerit. info. distem (Automatic control and electrical measuring techniques;
transactions of the conference, v. 1: Theory of measuring information systems).
Novosibirsk, Izd-vo Nauka, 1966', 20-Z3.
TOPIC TAGS: measurement, information processing, data processing, ialoxxuaUen
==Pra=ion- c
Id
ABSTRACT: Assuming that a certain delay in measurand transmission and a certain
error are.permissible, the following method of quantization and compression of
,measurement signals is suggested: The signal f(t) is expanded into an orthogonal-
'function series within interval a 4 t r. b, and only expansion coefficients are trans-
mitted over the communication channel. Calculation of the first n +I coefficients co
Cap cn Is reduced to multiplying the vector 2M*.(V(-'?(b),
LCO-rd

ACC NR- AT70049Z2
cc Here, A remains constart~
(b). 0 ...to i
Cl and j depends on f(t);
by the matrix A 01 Mo 01 Mt 0 a r d-A hence. it is sufficient to
transmit components of
J 5. (*b)', b (b) Ca I
d which are the results
of successive integrationo
of f(t) or a modified function f(t). The latter is applied to a pulse element (see
figure) which generates regular pulses corresponding to the function values and sends
them to multiplying
617 Pulse 01K) unit x which multiplies
It x
element of, Vw.N them by the integration
4~ interval h. A series of
f f 4W f to-OW summators prepares
final signals. The
system can be further simplified in the cases where multiplying -by-h operations can
~be performed at the receiving end. The method in offered for telemetry systems,
particularly for the cases where the automatic processing at the transmitting end
~must be simple. Orig. art. has: 2 figures and 13 formulas.
ISUB CODE: 09 SUBM DATE: tione ORID REFt 006
Card 2 / Z