SCIENTIFIC ABSTRACT RODYAKIN, V. V. - ANDREYEV, B.M.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R000101510013-9
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: March 20, 2001
• Sequence Number: 13
• Publication Date: December 31, 1967
• Content Type: SCIENCEAB

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71
ACCESSION HR: AP5019971 UR/01361651000100810064/0068
669.295
AUTHORS- Rodyakin, V. Gamete, V. A.~f Sokolon I I Sandler, R. Ajf~
A nov, E. A.t/Vlagov, V. A~l us Ind;ay v, A. Ye..
V,_ 5
TITIZ: Quality of-the titanium spong obtained by using different types Of 'Lag'
nesim ; 5, 2.1 ) i
SOURM Tsvatnyye ustally, no. So 1965. 64-68
TOPIC TAGSt titanium sponge, raw electrolytic magnesium, refined magnesium,
sponge block, condensate magnesium, titanium tetrachloride, spongy titanium.
uagnasium electrolysis
ARSTRAM The article presents the findings of experimantal-industrial
rison tests of the quality of partA of a block of spongy titanium obtai.Zle,
using raw electrolytic %Isflned magnesiumt and condensate magnesium
the C I asata of the vacuum separation of titanium) Thm
(obtained by remelting
tests vare based an the use of titanium tetrachloride of a fixed composition.
Analysis showed that the bardoess of the refined part of the block, obtained b
usid refined magnesium Is 6-5 units lower than the hardness of the swas parts

L oml -a - 4~ ~.
~FACCESSIOM NRt' AP501997'1 C)
of the sponge block obtained by using condensate magnesium. On the whole the dif'
ference in the quality-of co=ercial metal am6unts to 6-7 units (hardness) in
favor of the titanium sponge obtained on the basis of refined magnesium. There. IL
fore, the use of liquid instead of solid magnesium does not appreciably affect
the quality of spongy titanium. As the motbods of transporting liquid magnesium
are improved, the expediency of conversion to the liquid foim of this ieducin&
agent will increase. Analysis of the quality of the titanium sponge obtained
with the aid of different types of magnesium has confirmed that the impurities'
(Yel Si. C, N$ 0) from the magnesium concentrate chiefly at the bottom of the
sponge block. This leads to a deterioration in the quality of the commercial na-
tal which, In Its turn, causes a decrease in its recovery from TiC14. The de-
terioration in the quality of spongy titanium is chiefly due to the gaseous Im-
purities. With respect to the content of these impurities. raw and refined mag-
nesium are of a much better quality than condensate magnssita%6 Owing, however,
to the still current imperfections in the technology of removal of magnesium
from electrolytic calls,-the use of raw nagnesim often leads to a lower quality
of the bottom and surface layers of blocks of spongy titanium. These operations
must be Imptoo d before the quality and recovery of titanium metal can be im-
2/3

MEM
/171
ACCUSIM IIRs AP5019971
proved. Thus, the reduction Of titanium from its tetvgthlDvids is best accoot- th
plishad with the aid of raw magnesium, but this requires prior improvements 10
Uchnology and equipment for transferring magnesium from slactrolyzers to re-
duction. Orig. art. hass I figure, 3 tables.
ASSOCIATIONs none
SUIRrMDi 00 INCM 00 OUB CODES )21
XO RZY SOV3 OW MMI 000

TJ J
ACC NRt AP6020737 SOURCE CODE; Ult/0136/66/000/0-06 0-0~-6TOO--5-7
AUTHOR: V11charev, A. F.; Andreyev, A. Ye.; RodyRkin, V. V.
ORG: none n
TITLE: Use of titanium tetrachloride vapor in refining niagnesturn C3
SOURCE: Tovetnyye metally, no. 6, 1966t 66-67
TOPIC TAGS: metal purification, magnesium, titanium compound
ABSTRACT: Laboratory and field tests on refining of magnesium by exposure to vaporB of
titanium tetrachloride were carried out In steel or titanium crucibles and employedpetal
containing from 0.027 to 0.032% Fe and 0.002% Si. Results indicate that tlta~iumIdrucibles
redu" Fe to a level of 0. 005 to 0. 007% and St to trace quantitieS at a MagneSiUM COM3-111,-1011
factor of 2 to 3%. Steel crucibles required higher consumpticm (3 to 5%). Observntions of the
change in the quality of magnesium during reduction yielded results which are given In Table 1.
Jorig. art. has- 3 figures and 1 table.
co'd 1/2 UDC: 669.721

L 4U54-66
ACC NRe APS020787
Table 1. Change in the composition of inagnestum. in tho initial
stage of reduction, %
Specimens during reduc-
Initial tion with a magnesium
Specimen consumption coefficient
P" S1
Fe S1 Fe S1
I ..'
0.027 0 00210:014 trac] o:oos traces
0
03 0:002 0 017 [G. 0 006
0:032 0.00 0.019 0,007
SUB CODE: 11,13/ SUBM DATE: 00/ ORM REP: 001/ OTH REFi 004
2/2 hs

BULGARM / General Problems of Pathology. Tw-,iors. U-7
I s in 1!11111rms.
Ccmparatfve OncologY. Imior
Abs Jour: Ref /.hur-Blol., 111o 151 1'-)5(31 70,366.
Author Ikono'nov I! .. jIndreyev
Inst Not given.
Title A Rare Case of a Neurofibroma of' the Shin.
Orig Pub: Khirurgiya (Belgrade) 1956, 9, i,~o 6, 537-541.
Abs'~ract: No Abstract.
Card 1/1
53

WSR/Biology - Ornithology
Card 1/1 Pub. 86 - 35/37
Authors I Gagina., T. N..,
Title Birds of central Vilyuy
Pericuma, o Priroda. 44/4.0 124 i25P Apr 1955
Abstraot A review is made of the book, "Birds,of Central Vilyuy". by
B,, Andre 1W auspices of the.Institate for Training of Teachers.
Oy~~HKMTP Autonorms'.-Soviet Sooialiat Republio Yakutsk,
1953s 127 pages. One handred afid fiTty-nine 'species of birds
are presented in the book, Extraote of.Yak-ut folklore are also
includedin the book,, whichis given;a high ratUg.
Institution-s
Submitted

ANDUYEV. B., master
W . . ''
Using platform-mounted crane in assembling. Stroitall no-5:23 Mv '58.
(Cranes, derricks, etc.) (MIRA 11:6)

M111=9 B., master
Installing gates in indr O-rial buildings. Stroitell no.3:15
Mr 159. (mim 12:6)
(Gates)

ANDRETIV, B., insh.
Me.chanized application of bituminous waterproof coatings.
Stroltall no.12:13 D 159. (MM 130)
(Waterproofing)

ANDRITSV, B., rasluzhennyy maBter sporta, SSSR.
Taking aim and pulling the tripgor. Voen. znan. 34 no.1'1:31-32 IN "~.
(MIRA 12:1)
(Shooting)

ANDREYEV, B. (Volgograd)
Thpy throw a monkey wrench into the machinery. Sov. profsoiuzi
18 no.5:27-29 Mr 162. (MIaA 15:3)
1. Spetsiallnfy korrespondent zhurnala "Sovetskije profsoyUzy".
(Volgograd--Steel industry) (Volgograd-Works councils)

ANDIEYEVY 13., p.ropodnvzatoll
OcclusJ or, in a lxX. uz,azlld. al". 'l lic ."f- J, 1, ,
0
1. 1--)tnoy~, lic hi -1

V,-Z
____ANDREYF _jAndreeu, B.)
Don't leave your work unfinishek Rnb.i sial. 38 no.4:7-8 Ap
,62. (MIRA 15:4)
1. Kolk..oz imeni XXII s"yesda Kommunisticheskoy partii Sovetskogo
Soyuza, Ushataki., rayon.
(Ushachi District--Dairying)

ANDRFM, B.
Span bridges across gulfs. Sov,,profaoiuzy 19 no.2:4-5 A 163.
(MMA l6t2)
1. SpetBiallnyy korrespondent zhurnals, "Sovetskiye profsoyuzy.wl
(Construction ind t -Technological innovations)
(Socialist compatiutionj (Trade unions)

ANDREYEVS B. A. Cand. Tech. Sci.
"Design of Converters of Sma2l Bessemer Process," Stall, No.6, 1948
Magnitogorsk Mining Metallurgical Inst.

Tem 11 --It converter lintng 11
Whedul of a
A. Stitt 8, T~1-709W liv ti,itq a w- ,f
thermocouples. the cmim- of thr trinp. %4, outlit-A it
otany poiniq an the hell and liniog ,I ., t-oevrirr lurvig
the hCAtitig-in Mid MH (11 * ",ovemr. After 4-.,, It ruts ,f
the converter trimpaign. the Cluingei (rso'mll' %Ligging-111.
dism, etc.) in the converter lininS wtir t ii.mid I lie rc.
tults Lif theite olneri-2tions lretywded graphi(Al'.. I ""1r
io dritgning 4 (11"Vatcr 11.4%-goit " it'.. rr-' -Aplo
N1. 11-01

AMMYICV, B.A., inshener (Odessa); VATAY, M. B.. inzhener (Odessa).
Modernization of offset plate graning machines. Poligr.proisr.
no.3:21-22 My-Je 154. 0(LRk ?.- 8)
(Printing machinery and supplies)

R 0 J) 1~ i~ ~ E;,J, ~~- h -
--A;4 ~ ~ I ..- ~A. -
- '' - -.1., ;Ial-lit'n.,
Anire-v. 7'. A. iiC,,l thu, C~-nstrlict..'-:T" ;-,f hcgc:-,~~ :~ ~ 1; ... , '- - 1 -, - 'I, - I
I, I c,,. i li I rc' c,~. , I'c ~-ow,-Lenin~r a ri , ", , I , - :
- - 1. 1 - I -- " I., . I ~ -, ., -) I I - --./- ., .

6. IA .
01,
-:ornill, 7, D-nir,,nid--

ANDREYEV, B. A., ZAKASHANSMY, M. S., SAMON, N. N., and FOTIADI, E. E.
(Course in Gravity Prospecting). Gesgeolizdat (1941).

ANDREYEV, B. A.
"Calculations of the Spatial Distribution of Potential Fields and Their
Utilization in Geophysical Prospecting. I," Iz. Ak. Nauk SSSR, Ser. Geograf.
Geofiz.,, 1l,, No.l., 1947
Part II, ibid., 13, No-3, 1949

1. AND=, D. A.
2. ussn (6oo)
"Problems of Prospecting Geophysics Connected
with the Diricblet Problem.-Waterials of the
All-Union, Geolopical Research Institute."
Goeftsika, Collection 13., 194e (57-71).
9. Yeteorologiya i Giarologiya, No. 3t 190.
-W Renort U-2551.30 Oct 52

ANDMEM, B. A.
Andr�yey, B. A. "On the problem of explaining results of gravelcKploration work
durin& research on layers of the type," Razvedk-a nedr, 1948, No. 6, p. 32-35 -
Bibliog: 6 items
SO: U-3264p 10 April 1953, (Letopis 'Zhurnal Inykh Statey) no~ 30 1949)

ANDREYEV, B. A.
It Calculations of the Spatial Distribution
Utilization in Exploration Geophyuics. II"
Iz. Ak. Nauk. SSSR, Ser. Geogr. i. Geofiz.
of Potential Fields and Their
3, No. 3, pp. 256-267, 1949.
TTonalation 563976

USSRAW=mla May/Jan 49
Prospecting
Geophysics
COalculations of the Spatial Distribution of
Potential Fields and Their Utilization in Geo -
physical Prosp6cting, Part II," B. A. Andreyev, 11 pp
"IZ Ak Nauk SSSR, Ser Geog I Geofiz" Vol XIII, No 3
Describes method for computing potential fields in the
lower semispaces vhich encompass the source of the
potential. FormuJA most frequently used for this
'purpose uses values vhich are computed consecutively In
their Insagpl-twn. Mentions methods, for using compu-
tations to evaluate results of geopbysic4l surreys,
USS/Minerals ~Contd) May$Y= 49
particularly vhen computing the depth of the
UR)er Surface Of theLeXCiting mass and when com7-
paring results of aerial andgrouA iagnetic
Surreys. Part I of this series appeared in "1z
Ak Nauk SSSR, Ser Geog i Geofiz" Vol XI, No 1, 194T.
Submitted 1 Jul 4T.
63/4W103

Andreev, B. A. Calculations of the spatial distributions of
potential fields and their application to prospecting geo-
physics. 111. Izvestiya Akad. Nauk SSSR. Ser. Geofir.

1952, no. 2, 22-30 (1952).
(Russian)

The author considers a so-called "two-dimensional" case 4 t P4
4
when the geophysical anomaly is generated by a cylindrical
structure extending to infinity in one direction, lying parallel

to the horizontal surface of the ground and whose cross- A
section is the same evervivilere. In such a case the potential
U(X, i" at a depth z (z > 0) is related to the observed profile
U(x, 0) on the ground r=O by tile equation
wU(x,O)=Zf [(x-u)'+z;_-lU(u,z)du.

Using this equation as Avell as the Laplace equation, tile
author studies a practical method for the computation of
U(x, z) from the observed values of U(x, 0), based on the
successive approximations. [For parts I and 11 see --tine
'
4
journal 11, 79-92 (1947); 13, 256-267 (1949); these Rev~ 1
0
E. Kogbelliantz. >

-~' /7 -
/1/~/p /f Ai~J~3~~ ~SK IVY/, M. rY'e. ;' 11 ; GOLORB, Y.B.; SAMSONOV, N.N.;
PAVLUTSYAIA, f j # tor; POPOV, N.D., tekhnicheskiy
redaktor.
(Course in the gravitational method of prospecting for technical
schools of geological surveying] Kurs gravirazvedki dlia geologo-
rasvedochnykb takhnikumov. Moskva. Goo. nauchno-tekhn. izd-vo
lit-ry po geologii i okhrane nedr, 1954, 357 P. [Microfilm]
(P"specting-Geophysir,al methods) (MIJRL 7:11)

US6R/Geophysics"I Prospecting geophysics
Card 1/1
7ff
Author ; Andreyev, B. A.
Title : Calculations of the spatial distribution of potential fields and their
utilization in prospecting geophysics. IV
Periodical : Izv. AN SSSR, Ser. geofiz. 1, 49-64, Jan/Feb 1954
Abstract : Treats the problem concerning the application of the calculations of the
spatial distribution of potential fields to the geological interpretation
of magnetic or gravitational anomalies. Describes in detail one of the
methods of interpretation and its application to determining the depth at
which the crystalline fundamental rocks of the platform lie. Eighteen
references, all Soviet.
Institution : Leningrad Mining Institute
Submitted : December 27, 1952

, -' 1, ' ~ -" j f;7;. .' - ,
I .' ".
ANDP"IEV.B.A.
Determining the surface depth of crystalline bedroi:- of platform
regions by means of magnetic anomalies. Prikl.geofiz.no.13:80-
98 '55. (MIRA 8:10)
(Rocks, Crystalline and metamorphic) (Magnetism, Terrestial)

/. *) 1~ ).~) i~ "', \/ Y k" I I*,-, - 0,
SHAYMIOVSKIY, Ilarion ilarionovich; TATARINOV, P.M., red.; GORSKIY, I.I.,
red.; ALMOV, B.A., prof., red.; AIDRZYXV,B.A., prof., red.:
GRIGORIYEV, D.P., prof., red.; 71TY-An-R~.. ~_,~_rof., red.; TOLSTI-
XHIIJs II.I., prof.red,; IEVEIMRG, N.V., red.: YODOLAGIIIA, S.I.,
tekhn.red.
[Mineral crystals] Kristally mineralov Cleningrad] Izd-vo
univ. Pt.l. (Plane-face formal Ploskogrannye fornV. 1957.
(MIRA
1. Chlon-korrespondent All SSSR (for Tatarinov, Gorskiy)
(Crystallography)

leningr.
220
11-2~9

J~
ANDREYEV, B.A.
Computation of
no.17:170-177
11/~
the vertical gradient of gravity. PrIkI. geofiz.
157. (MIRA 11:2)
(Gravit.r)

ANDRVEV, B.A.
'.' - .. .Relation of platform structures to the horizontal zoning of physical
properties of seclimentary rocks. Sov. gaol. no.61:112-120 '57.
(MM& 11:4)
1. Laningradskiy gorzV7 Inatitut.
(Rock, Sedimentary)

ARMEYEV, B.A.
Use of oxygen in small converters. Lit. proizv. no.3:4-7 Mr 158.
(MIRA 11:4)
(Oxygen-Industrial applications)
(Converters)

?AUTHORt Andreyev, B. A. 20-1181-4 -4 5/61
TITLEt On the Problem of the Southern Boundary and the Dimensions
of the Vyborgskiy Massif of Rapakivi Granites (K voprosu o
yuzhnoy t e i razmerakh Vyborgskogo massiva granitov
rapakivi
PERIODICALt Doklady Akademii Nauk SSSR, 1956, Vol. 118, Nr 4, pp. 789-791
(USSR)
ABSTRACTt The structural position, petrology, and origin of the Rapakivi
granite intrusions at the southern boundary of the Baltiyskiy
shield have been discussed for years in geological publicat-
ions. The course of the southern boundary and the real dimen-
sions of the greatest Vyborgskiy massif have hitherto not been
clear enough, since its southern part is covered by the Finskiy
gulf. This boundary has hitherto been drawn rather approxi-
mat,ely between the northern and southern coast of the gulf
(references 1-4). The dimensions of the massif are estimated
at 18 000 - 20 000 km2 (reference 4). The minima of gravity in
the region of the Rapakivi massif have been detected already
since&long time (references 5-7). The latter have a relative
Card 1/3 density of 2,6 9/cm3 compared to the containing gneisses and

On the Problem of the Southern Boundary and the Dimensions 20-118-4 -4 5/61
of the Vyborgskiy Massif of Rapakivi Granites
migmatites for which this value amounts to 2,7 - 2,8 C/CIO
At present the position of the southern boundary and the di-
mensions of the Vyborgskiy massif can be determined with great-
er aocur'acy. The results of the measurements carried out by
means of the gas gravimeter of Khaallk (Haalak) in the Finskiy
gulf by this author (reference 8) are of great importance.
These results have never been geologically interpreted in the
publications as far as the author knows. The results showed
among other thirgs that the apparatus is apt for measurements
on a ship at sea and that the aocuracy of the measurements
amounted to +5 M91- Figures 1 and 2 show that the Vyborgskiy
massif exter~d_s below the bottom of the Finskiy gulf towards
the south and reaches the northern boundary of the Estonskaya
SSR. This agrees with the discovery of rocks of the Rapakivi
type in the borehole,s ir the district of the city of Tallin.
Simultaneously the results of the pendulum survey exclude a
greater distribution of Hapakivi-like rocks in the region of
the Estonskaya SSR except the region at the southern coast of
the Finskiy gulf. Thus the range of the massif is extended to
40 - 45 000 km2, i.e, double the value that has hitherto
Card 2/3 been assumed. It was detected (reference 9) that the region
Libr&rY of congre5o
AVAILABLE'
card 3/3

INDRF,YKV, B.A.
G~rnvltAtlonnl PnomalleB and the thicknenn of the Earth's crust
in continental regions. Dokl. AN SSSR 119 no.2:2~5-256 Mr 158.
(MIRA 11:5)
1. Leningradnkly gornvy Inatitut im. G.V. Plekhnnovn. Predetnvlano
nlradamikom D.V. Hnlivkin7m.
(GooT)hyn ic a )(Gravity)

AUTHOR: Andreyev, B.A.
TITLE: Metallogenic Zones and
(struktiarno-metallogenicheakiye zDny
PERIODICAL: Doklady Akedemii nauk SSSR, 1958,
(USSR)
SOV/20-121-6-"2/45
Gravitation Anomalies
i grovitatsionnyye anomalii)
Vol 121, Nr 6, pp 1063 - 1064
ABSTRACT: In 1946 S.S. Smirnov (Ref 1) described the Pacific ore belt where
he separated two structural metallogenic zones: 1) an external
continental; it is characterized by an acid magmatic complex and
by a tin tungsten mineralization and 2) an internal, oceenio zone.
In this case a more alkaline mei-matic complex is characteristic
as well as a copper mineralization. Smirnov brought into relation
the differences between these zones and a considerable reduction
of the thickness of the upper sibl strata of the earth crust at
the trrnsition from msihland to ocean. This Dhenomenon causes a
strong change of the character of the gravitational field: Over
the mainland the anomalies according-, to Buge are equal to zero or
negative whereps above the ocean they are highly positive (hun-
dreds of milligals). The enslysis of the gravitation results shows
Card 1/3 that 9 number of metallogenic zones with a mineralization of the

Structural Metallogenic Zones and Gravitation SOV120-121-6-32145
Anomalies
limesocratia"'type are characterized by intensively positive Buge
anomalies: 1. The internal and external geosynclinal of the
Japanese main* islands ~' id=Ufied by Schneiderhbhn (Shneydergen),
Ref 3). They bre-charBeterized by Cold, sili4er and copper mineral-
ization. 2. Java Island (Indonesia) with copper, Cold and mercury
deposits' (Ref 5) shows also positive Buge anomalies. 17. Cuba Island
(West Indies) with chromite rend copper deposits (Ref 7) and 4. the
Island of C 'vprus (mediterreneous geosynclinal) with its abundant
copper deposits (Ref 7) is in an area of forspread Buge anomalies.
On the other hand also a number of metallogenic zones of the
"leucocratic" type are connected with zones of relatively low Buge
anomalies which are close to zero or necative; 1~ The middle zone
of the Ceosynclinal of the Japanese main islands, 2) South Kiangsi
and South Hunan (Ref 10), 3) enormo-as tin deposits in Bolivia,
4) molybdenum ores (C11x=, USA) and tungsten ores (Bo04m?,USA)
There are 13 references, 6 of which are Soviet.
Card 2/3

Structural Metallogenic Zones end Gravitation SOV20-121-6-32/45
Anomalies
A-SSOCIATION: -Leningradskiy gornyy institut im. G.V. Plekhenove (Leningrad,
Mining Institute imeni G.V. Plekhanov )
PRESENTED: April 23, 1958, by D.I. Shcherbakov, Member, Academy of Sciences,
USSR
SUBMITTED: January 17, 1958
Card 3/3

ANDREYEV, B.A.
Prospects for the development of structural geophysics. Sov 801.
2 no.6:3-12 Je '59. (MA 12:;25
I.Leningradekiy gornyy inatitut im. G.V. Plekhanova.
(Geology, Structural) (Geophysics)

3(5)
A1;'2j i 0:': Andreyev, B. it.
TITLE: A Relation Between the Structural -Pelie~ and ti:,-, Anw.in.*liec of
Gravity in the Cano of 'Soveral F)Op,1rLt ion Boundaries of' -Density
(Sootnoshuniyo mozlidu strUkturiiym rel 'yo."oi-i i anoimr-.1iyami oily
tyazhosti v sluchr~,-e ~,r-anitc ---azdela Tplotnosti)
PEY.'IODICAL: Dokl ndy Akadenii nauk SSS:~., 195", Vol ',21,, Nr 2, r, P 311-313

ABST:IACT: The present paner investiCatos the case in which the anomalous
'i,
ravitational i aid is due to several density separation
j,
boundaries. These separation boundaries are of equal shape and
are at equal vertical distances from one another. Thus, a
stratified medium is concerned. In the case of a separation
boundary the known approximation relation
At-'(X2) - AU (x 1 ) rv 2 kfL-6 (h 1- 112) holds,
Here k denotes the gravitation constant; - the excess
density, i.e. the difference between the densities of the
upper and lower layers; Ill and 110 - the ValUC3 of depths up to
Card 1/3 the separation boundary at the points x = x 1 and x = x2

A Relation Between the Structural Relief and the SOV/20-124-2-19/71
Anomalies of Gravity in the Case of Several Separation 2oundaries of Density
of the x-axis (line of observation). This line of observation
is vertical to the ntrike of the layers. The above mentioned
relation is in practice quite often used in the case of the
existence of several separation boundaries of similar position.
Here 6 = (5 1 + 62 + .... is assumed, where 6 1' 62 denote
the density differencess on the respective boundaries. However,
such a calculation is liable to lead to grave errors because
the gravitation effect of each boundary actually depends not
only on its relief and on *difforence in pressure, but also on
the average depth of its porition. The present paper endeavors
to clear up this circiunstance. The author begrins by dealing
with the case with one separation boundary. Next, an expression
is derived for the case aith several separation boundaries
between variation of the anomalies and the variation of the
depths. These formulas make --Lt possible to make estimates and
to draw conclusions which are not trivial and are significant
from the geophysical and -Ieolo,~ical point of view. As an
example, the author exanines tho influence exercised by the
depth structure of the terre-.trial shell upon the jravitational
Card 2/3 field. The typical positive and negative regional anomalies

A Relation 'etween 411c th~ S07j"IC 1 "7 1
-
Anomalies o-' ravity i1i thr
()f Sep,,-ration Doundarics of Dcrinit,,,-
in the ,rofiles 'u() tlioir ntrike cPn be
b., approximalion a.-, a coi-bination of h-.r:.ionicc
period of 200 - 400 ~--r- :,re 6 7 o." -,.-hich
arc Soviet.
ASSO-CIATIO17: Lcnin:,rads!-.iy ,,orniy inst-ituL im. G. V. Plekhanova
(Leningrad ...inin,-, Institute imoni G. V. 1'1(,khanov)
PRESEI~T;,"D: October 6, 1/0589 by V. I. Smirnov, Academician
SUBMITTED: October 2, 1953
Card 3/3

PHASE I BOOK EXPIDITATION SOV/4618
Geofiznefteuglerazvedka, trest. Upravleniye geofizicheskikh rabot
Geofizicheakaya razvedka, vyp. 2 (Geophysical Survey No. 2) Moscow, Gostoptekhizdat,
1960. 126'p. (Series: Obmen proizvodstvennym OPY-tcm) 3,000 copies printed.
Sponsoring Agencies: Glavnoye upravleniye geologii i okhrany nedr pri Sovete
Ministrav RSFSR; Upravleniye geofizicheskikh rabot trest Geofiznefte-
uglerazvedka.
Ed.; O.K. Glotov; Executive Ed.: S.M. Yungans; Tech. Ed.: L.V. Ganina.
PURPOSE: This book is intended for engineers and technicians working in geology
and geophysics.
COVERAGE: This is a collection of 11 articles on geophysical methods and tech-
niques of surveying mineral deposits. The authors discuss problems in process-
ing and interpreting the results of surface and underground gravimetric surveys
and-4s;pislffic logging. New types of geophysical instruments and equipment, the
AFI-2 and AFI-U amplitude-phase meters, the small portable OP-55 ultrasonic
Card 1/3

Geophysical Survey No. 2
SOV/4618
seiInjoscope, two-dimensional perforated sheet material. for modeling seismic
wavts, a pantogreph, and a modified ISh-4 inclincmeter are described in detail.
No personalities are mentioned. References acccopany individual articles.
TABLE OF CONTENTS:
Khramoy, A.I. Method of Processing Seismic Logging Observatioriq 3
Yurchenko. B.I. Correlation of Reflections in the Washout and Pinching
Zone 11
Andre ev. B.A. De-velopment and Use of Methods of Processing and Interpreting
tli-e--Resulta of Gravimetric Surveys 16
Mudretsova, Ye. A. Underground Gravimetric Surveys at Copper Pyrite Deposits
in the Middle Urals 31
Tyapkin, K.F. Graphic Computation Of vx md vzz on the Basis of A g
Measurements for Cases of Finite in, Strrke TAnear Anomalies 60
Card 2/3

ANDRIYEV.,-Z.A.-grinimall uchastiye: SUBBOTIN, S.I.; KARATEV, N.A.
KHABAKOV, A.V., nauchnyy red.; SVIGHYRYA, N.A., red.izd-va;
GUROVA, O.A., takhn.red.
[Geophysical methods in areal structural geology] Geofizi-
cheskie metody v regionallnoi strukturnoi geologii. RoBkva, Gos.
nauchno-takhn.izd-vo lit-ry po geologii i okhrane nedr, 1960.
258 p. (MIRA 1-3.11)
1. Chlen-korrespondent AN USSR (for Subbotin). 2. VoeBoyuznyy
geologichaskiy nauchno-isoledovateltakiy institut (for Khabakov).
(Prospacting-Goophysical methods)

ANDRMV, B. A.
DevelopiM and introducing methods of processing and interpreting
grwity prospecting data. Geofiz. razved. no.2:16-.30 160.
(MIRA 13:12)
(Gravity prospecting)

MIKHEYEV, Viktor Ivanovich, prof. (1912-1956]; MOBERG, Me, otv. red,;
TATARINOV,'P.M., red.; ALFEROV, B.A., prof., red.;..ANDfMEV B A.
prof.j red.; GRIGORIYEV, D.P;, prof., red.; FOGRZ-BITSKIY, Ye.0 , pFof.,
red.; TOISTIMIN, N.I., prof., red.; SHAPMOVSKIY, I.I., prof:, na-
uchnyy red.;'MIKHEYEVA, IN., dots., iiauchiqy red.; DAYEV, G.A., ve-
dushchiy red.; ZABRODINA) A.Aj tekhn. red.; GENNADIYEVA, I.M., tekhn.
red.
(Homology of crystals! Gomologiia kristallov. Laningrado Gos.'
nauchno-tekhn. izd-vo neft. i gorno-toplivnoi lit-ry, 1961. 206 p,
(MIRA 1010)
1. Chlen-korrespondent AN SSSR (for Tatarinov).
(Crystallograpby)

ANDREYEV, B. A.; BORONIN, V. P.; KRYLOV, S. V,
Geophysical peculiarities of oil-bearing structures in the Volga-
Ural region. Sov.geol. 4 no.-It95-106 J1 161. (MIRA W-10)
1. Leningradskiy gornyy institut imeni G. V. Plekhanova i
Kazanskiy gosudarstvennyy universitet imeni V. I. UlIvanova--
Lenina.
(Prospecting-Geophysical methods)
(Volga-Ural region-Oil fields)

ANDRE)aw. B,A-.-
ii~ree-air anomaly and isostasy. bok3.. .411 SS' R 139 no.1:91-93
il 161. (MIRA 14:7)
1. Leningradakiy gornry institut im. G.V. Plekhanova.
Predstavleno akademikom V.V. Shuleykinym.
(G;-avity)

ApMUV,_B~!rL Aleksandrovl.S~l, KLUSHIN, Igor' Gonnndlyevicb;
A.S.,
retsenzerit~, MIRON,-I, V,S., retsenzent.;
SEMENOV,
DEMENITSKAYA, R.M.,doktor immik, retsenzem.;
MlKHAYlDVP N.N., nauckui)y red.; TOKAlj-"VA, T.A., wid. red.;
SAFRONOVA, I.M., tekhn. red.
[Geological interpretation of gravity ariomalles)Geoloflche-
,Aoc istulkovanie gravitatsionnykh anomlil. Leningrad
Gostoptekhizdat, 1962. 495 p. Ml U 16-~'35
(Gravity anomalies)

AMRSYEV,__~.A.-
On E.H. Liustikh's notes referring to my article "Free-air
anomalies and isostasy.11 Izv-. AN SSSR. Ser. geofIz. no-3;
392-393 Mr 162. (Gravity) (Isostasy) (YM, 15:2)
(Liustikh, E.N.)

THOR Andr S049/63/OW/002/PO67bW,'
,u
A
W63/0307
On 14 temlyev's.c6 on~"Approxiiiat
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atio~--!~ 6"*~tq ~`of the Antarotioll
soot
Akademijai,"ndiUk" S'SSR. Izvestiya.
Seriya
f4idho0aya' zo 2 1963y: 347
geo 1 -348.-
~"MX 6, bonolusi h -~toiiched by Artemlyev x~egarding'the`
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atisfactory assdssment:of .

, -~from%t~ :'.."values of
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-

'xi

C
d
ar 2/21

ANDREYEV, B.A.; RIVUSE, L.A.
Increasing the geological effectiveness of aeremagnotic surveying.
Sov.pel. 6 no.8:11.6-118 Ag 103. WIRA 16:9)
1. Vsesoyuznyy geologicheskiy institut I Zapadnn, geofizicheskiy
trest.
(Aeronautics In Surveying)

ANDREYEV, B.A.
Geophysical and geological features of the zone of deep-focus
earthquakes in the northwestern Pacific Ocean. Dokl. AN SSSR 150
no.1:140-142 My 163. (MIRA 16:6)
1. Vsesoyuznyy nauchno-issledovatellskiy goologicheskiy institut.
Predstavleno akademikom D.V.Nalivkiny-m.
(Pacific Ocean-Seismology)

ANDREYEV, B.A.
-.91
Geologiaal and geophysical characteristica of t-tie arch uplift
regions. Trudy VSEGEI 85~101-LOB 163. (MIRA 16,11)

ANDREYEV, Boris Aleksandrovich; KHABAXOV, A.V., red.
(Geopbysical methods In areal otructural geology] Geofi-
zicheskie metody v regionallnoi strukturnoi geologii. Mo-
skva, Pedra, 1965. 323 p. WIM 16-18)

.........
7-7 _77N
E"7
~L'25661-46 EWT(11 GW -
~Ac NRt
C, A1002868T
indivyey,~ Boris ALekeandwov:Lcli
~Geqphyslcal,bethods in-regional stru6tural.po (Ge
LCW_ dizicheskiye ody. v
Moscow, lzd-vo _."fiidia"
,~Aa*aa& V:nbyl~ iuktui6py- geologil). -'_gd'edo.0 enu
iA." 65j:.~ 032). Jnus~o i ti~li6" iude6i :2 -printed.
,000.coyieo,
tectonic
ics poloE op seismology., survey, earth magneti c
X'Atrat,= L
physical geology
PURPOSE AND COMME: This book gives basic principles red major results'using
~geophysical methods In the study of the Earth and the Earth's core and In regional
geological investigations. Also given are recent trends in the development and
results of regional structural geophysicso This book can be useful as a text for
students of geoloeibal survey in the in the umftersities and as a mawua for'geo-
physical engineers and geologists.
TAM OF COMMMS (abridged):
Preface -3
Introduction
Cho Io Study of the inner zones of the Earth -11
Cho IL Study of the structure of the Earth's core -62
Ch. 111. Physical-geological prerequisites for -the use of geophynical methods
ard 1/2 UDC: 550.83

r

'.ACC NR, AT6028374----- 9- /0103 7
SOURCE CODE: URIOO0016510001000100 3
ATMHOR: Andreyev, B. A.
ORG: none
TITLE:. Gravimetry and regional geology
SOURCE: International Geolo cal Congress. 22d, New Delhi 1964. qeolqgi~heskiie
rezulltaty prikladnoy geofizlqi Geological results of applied geophysics ; dok ady
sovetskikh geologov, problems. 2. Mscow, Izd-vo Nedra, 1965, 93-103
T
IOPIC TAGS: Bouguer anomaly, earth crust, gravity,
gravimetry , tectonics., stratigraphy
ABSTRACT: The present article describes the application of gravimetric solutions
to problems of regional geology. Incrdertomake gravimetric studies of the Earth's
crust, man valu,!s of Bouguer anomalies B (mgl) for continents are related to crustal
thickness D (km) by an approximate correlation relationship D = m - nff, where
m = 30 to 35 km, and n = 0.06 to 0.10 km/mgl. In young folded areas (Miesozoic,
Cenozoic) the distribution and character of.regional gravity anomalies agree with
the structural relief of the preinversion stage of development. In the areas of
island arcs this relationship does not obtain, indicating that the geosynclinal stagc
of development is still taking place. Areas with predominant metallizing mesc;--ratiq
i.e. , chromium, nickel, copper, gold, silver, lead, and zinc in mixtures, are
characteristized'by zones of high positive Bouguer anomalies while areas of
leucocratic metallizating lead and zinc veins, molybdenum, tungaten, and tin, are
Card 1/2

ACC NR, AT6028374
represented by zones of negative, almst-zero, Bouguer anomalies, In relatively
mobile platform regions, major structural features are generally directly expressed
in regional gravity anomalies. In stable regions this agreement is not clearly
shown or it may be masked by the effects of the structures from within the basement.
Me gravitational field marks fault zones, intrusions, folded structures, and iron-
ore basins - in the'basement, as well as oil-, gas-, and coal-bearing basins and arche
-with oil domes am associated in.sedimentary strata. Orig. art. has: 6 formulas
and 2 figures.
SUB CODE. 08/'SUBM DATE! o6jan65/ ORIO.REF: OZ~/ MH REF: 008
1; Car*d

L 47 5~ ~.66
ACC NR: AP6032283 SOURCE CODE: UR/002o/66/17O/0O2/o4O2/o405
B. A.
!AUTHOR: Andreyev,
ORG: All-Union Scientific Research-Geological Institute (vsesoyuznyy nauchnon
issledovatel'skiy geologicheskiy institut)
TITLE: Major atructural elements of the basement of the eastern USSR
SOURCE: AN SSSR. Doklady, v. 170, no. 2, 1966, 402-405
TOPIC TAGS: geologic basement, tectonic structure, geologic map, Katarcherin geoblock,
magnetic anomaly
ABSTRACT: On the basis of extensive Le_2~2[,'ical and geophysical (chiefly, jp~fq~ti -c'
anoma.ly) investigations, n new sketch map has bef~n compi-led depicting the major
structural elements of the basement of' the eastern regions (-,)f the USSR. 1n general,
iintensely disturbed fields correspond to tile anclent Katarchean blocks of the base-
ment, while weakly disturbed Err fields (whereNis the mftf,,netic anoinal.~) Correspond
to the more recent (Upper Archean Proterozoic, Paleozoic) formations, The intense
1Fr anomrLlies of the Katarchean blocks are attributed to the high content of iron
ore. Fig. 1 shows clearly the block structure of the eartli's crust. It is seen
that the strikes of the subcrustal faults along the boundaries of the ancient
geoblocks are mostly sublatitudinal (WNW-ESE) or submerldional (NNW-SSE). The dis-
Cord 1/3 1JDC: __55_1.2jj:55j_t*L 47�a-
- tL _~l ) - -

L ~~5_6_6 .... .
A-CC NR: AP6032283
~ A, ~ ) 1% , \ ..."
....... ....
d
Card 2/3
Fig. I . Major i3tructairal elements of
the basement of the eastern regions of
the USSH
1 - Intensive maxima (AT > + 100y);
2 - intensive minima (AT < - 100y);
3 - normal fie T