SCIENTIFIC ABSTRACT GAYNANOV, A. G. - GAYNULLINA, R.KH.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R000514520018-5
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: July 19, 2001
• Sequence Number: 18
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

S/169/62/000/004/010/103
D228/D302
U T 111 0 R Gaynanov, k. G.
-217rtILE: Gravirietric determinations aboard the diesel-elec-
tric vessel "0b"' on the first Anta-rctic voyage
PI7-'R.IODICA.L: Referativnyy zhurnal, Geofizika, no. 4, 1962, 18, ab-
stract 4A138 (V sb. Morsk. gravimetr. issledovaniya,
no. 1, M., Ylosk. un-t, 1961, 23.306).
TEXT: Gravity measurements were made with two triple-pendulum
instruments (Cambridge and "Askania-Werkell) in order to test new
apparatus and clarify the conditions and possibilities of under-
taking marine gravinetric ob_~ervations. Before the beginning of
Ulie voyage the pendulum instiuments were overhauled and fitted
wit,h, gradient and vertical-acceleration recording blocks. Five
marine chronometers and a device ]"or checking the fi,7Y-q (-220h-4)
watch were used as time emitters. The instruments are described.
The I'Askania-';Ierkell pendulum instrument with invar pendulum-s was
was olaced in a Helmholtz coil. The original and the final obser-
vations were carried out in Moscow, the control observations be-
Card 112

S/169/62/000/004/010/103
Graviae-.ric determinations aboard ... D228/D302
ing made in the ports of Leningrad, Capetown, Wellington and Ade-
laide, as well -as at many points with a known gravity value. Data
on the gravity field of the coastal zone of Antarctica's indian
sector were obtained for the first time; the BlIguer anomalies
were defined with a mean square error of from + 6 to + 9 milligals.
The undertaken tests showed that on account of-the str-ong engine V/
vibrations it is only possible to carry out satisfactory pendu-
lum observations on the diesel-electric vessel "Ob"I at stations.
tLD Stracter's note: Complete translation.-7
Card 2/2

S/169/62/000/004/014//103
D228/D302
AUTHORS: Zommer, 1. B. and Gaynanov, A. G.
TIT113: Methods and results of gravity determinations in Ant-
arctica
-PERIODICAL: Referativnyy zhurnal, Geofizika, no. 4, 1962, 19, ab-
stract 4A143 (V sb. Morsk. gravimetr. issledovaniya,
no. 1 , M. , Mo5k. un-11-, 1961, 63-68)
TEXT: Gravity measurements with a four-pendUlUM instrument, of the
G
'.A-ISh) design with bronze pendulums, were carried out along
the coast of Antarctica. The pendulum observation points were used
as the original ones for a survey with PAK-3N(GAK-3M) gravimeter,
Uransported in an AH-Z(AN-2) aircraft and a helicopter. The pen-
dulum gravity determinations are estimated to have a mear. square
error of + 2.0 milligals. The gravity anomalies, defined by gravi-
meter at Eoints located on the pack ice, are estimated to have an
error of + 3.2 milligals; the error at, Doints, situated on the land
ice, is lfl~om + 10 to + 15 milligals. The characteristic peculiari-
Card 1/2

S/169/62/000/004/014/103
Methods and results D228/D301
ties of gravimetric determinations, made with pendulums and gravi-
meters under conditions of large diurnal temperature changes (up t/
to 30 - 400C) and ice-sheet movements of Anta-rctica, are described.--
A table is given for the physical properties (density and coeffi-
ciqn~ of magnetic susce.p-61 4 -
U L U 'ibility) of 10 _Lntarctic rock specimens.
On the grounds o--:' the gravi'Cly -field' s character t*.-.e au-Uhors notle
Uhe considerable deviations of the pliunb-line. They point out -lihat
it is expedient to use the gravimetric method for determining the
thickness of the ice-sheet over the continental bediocks. /-Ab-
stracter's note: Complete -uranslation--7
Card 2/2
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GDra I/W

S/035/62/000/003/046/053
Gravimetric investigations ... A0011A101
voy~ige. Quartz-metallic penduiums (6 main and 3 reserve ones), quartz clock of
the Aerogravimetric laboratory at the Institute of Physics of Earth, AS USSR,
(M-IhAstr, 1960, no. 6, 5766) were used. A suspended magnetometer M-8 was
employed to check the variations of magnetic field. The authors note the stabi-
lity of regulating the optical system of the pendulum instrument, the good
quality of the Cardan joint, stability of quartz clock running, and small
changes in the length of the pendulums. In view of a strong magnetic influence
of the damper in the Accelerometer unit on the periods of quartz-metallic
pendulums (see 3G221), magnetic damping was replaced by the air damping in the
very beginning of the work. The authors describe the dctermination of the
constants of the instrument, the program of initial and marine observations,
methods of processing observations and calculating corrections. The accuracy
of determination of Fay and Bouguer anomalies from pendulum observations is
estimated by errors of + 6 - 7 mgal. The design principle of gravimeter with
strongly damped elastic system proposed by Veselov (RZhAstr, 1957, no. 6, 5172)
is described, as well as the design of the quartz system with horizontal filament
and pendulum in a position near the horizontal one, propoced by Smirnov. The
quartz system is placed into a liquid whose density and viscosity are so selected
that it could serve simultaneously as the thermocompensator of the quavzz system
Card 2/4

03/03V62/000/003/046/053
Gravimetric investigations A0011A101
and a damping medium. Moreover, a thin quartz plate is fastened to the pendulum
for damping, whose movement is restricted by a narrow gap between two fixed
metallic plates. Fundamentals of the motion theory of such a damped pendulum are
expounded for the case of existence of alternate, in sign,- perturbing vertical
accelerations. The design of marine gravimeters with ordinary and double quartz
system is described, as well as methods and results of determ.1ning their con-
stants, methods of measuring and processing photographic records, two methods of
stabilizing horizontal position of gravimeter by means of Cardan joint and
-yz The marine gravimeter
rostabilized platform, and the design of the latter.
6
with ordinary quartz system was mounted in a Cardan joint, and the gravimeter
with the double quartz system - on the gyrostabilized platform. Measurement
results were discordant, both between gravimeters and pendulums. insufficient
damping of oscillations of the pendulum quartz system at large vertical accelera-
tions is supposed to be the main cause of discrepancies. Amplitudes of residual
effect-of vertical accelerations ranged from a few tens to 600 mgal. Mean
amplitude values in adjacent portions of the records differ by 100 - 150 IrGal.
The authors note necessity of a further improvement of the gravimeter, its
adjustment to observational conditions on an above-water ship, studying the
Card 3/4

S/035/62/r,00/003/046/053
Gravimetric investigations ... AOOI1AlOl
functioning of the gyrostabilizing device, development of devices for position
control of the gyrosta~llizing platform relative to the true horizon. x
P. Shokin
[Abstracter's note: Complete translation]
Card 4/4

S/035/WCOG/003/048/053
AO01/AlO1
AUTHORS: Kuzivanov, V. A., Qavnanov, A. G.
- " me-
TITLE; On measuring magnetic field while carnjing out marine pendulum
observations
PERIODICAL: Referativnyy zhurnal, Astronomiya i Geodeziya, no. 3, 1962, 32,
abstract 3G221 (V sb. "Morsk. gravimetr. issledovaniya", no. 1,
Moscow, Mosk. un-t, 1961, 109-111)
TEYTt It was discovered at the starting point of the marine gravicietric
expedition of GAISh (see 3G219) in 1957 that, in observations with a marine
slx-pendulum instrument, the unit of accelerometers with strong magnetic danpers
creates magnetic fields up to 10 oe near the invar heads of the TsNIIGAiK quartz_
metallic pendulums. This led to a change in the oscillation period of s~vcral
TsN!IGAiK quartz-metallic pendulums up to 110 x 10-7 sec (-- 45 mgal). It is
necessary to determine admissible strengths of magnetic field while using these
pendulums, and in the field observations with penduli= instruments to observe
that the magnetic field should not exceed admissible limits. A device widely
used in practice of magnetometric studies is recommended for approximate
Card 1/22

3/035/62/000/003/048/053
On measuring magnetic field ... A001/AlOl
(+ 10 - 15%) determination of components H and Z of the magnetic field. The
d-evice is described which contains compass pointer, conventional compass and
electromagnet, and whose constants are determined by means of a Helmholtz coil.
P. Shokin
[Abstracter's note: Complete translation]
Card 2/2

GAYNANOV, A.G. - S141MIGV$ L.P.
Crustal structure in the transition area from the Asiatic continent
to the Pacific. Sov.geol. 5 no.3:108-218 Mr 162. U-MU 1524)
1. Wskovskiy gosudarstvewW universitet imeni Lomonosova i
Vsesoyuznyy nauchno-issledovateliskiy institut razvedochnoy geofiziki.
(Soviet Far East-Barth-Surface)

L 106?1=~i- EWT(I)/kffi(v
T 015(-ga qW
ACCESSION NR: AR4046166 S/01(19/64/000/008/GOOS/GO05
SOURCE: Ref. zh. Geofirika, Abs. 8G17
AUTHHOR: ynanov A. G.
TITLE: esulte of &tavtuietric Inveatigationii in the Sea of OWhotsk, the
ome r
Kurile-Kainchatka trench and adjacent parts of the Pacific ocean
CITED SOURCE: Sb. Morsk. ~Iravlmet'r- issledovanlya. Vy,,*cp. 2. M., Mosk, un-t, 19-6-3-9
66-n76 -
TOPIC TAGS: -gravimetry, gravimatric, survey, earth crust, island arc, selsmIcIty,
Volcanism, pendulum gravimetW,~qravlmete,r, sea-gravimeter, damped gravimater,
gravity anomaly, Mohorovicic discontinuity, deep seismic sounding, airborne magne-
tometer survoy, geoloqicaljdult'~ tectonics
TRANSIATION; This paper reports on integrated neismic, acromagnetic and gravimetric!
Investigatlons made for the'ourpose-lof clarifying the character of the structure
of the earth's crust in the transition zone from the Asiatic continent to the
Pacific Ocean In the zone of development of a recent geosyncline, Island arcs,
intense seismicity and volcanIsm, The gravimetric measurements were made using
seq.gqndulum qravimeters and sea damped. gravimeters. The accuracy of determination

L 10627-65
ACCESSION NR: AWW166
of gravity anomalies In the Bouguer reduction (a*= 2.67 9/cm3) in sectors with
small gradients was + 6-8 mgal and In sectors with large gradients was+ 15-20
mgal. The data froff~_these investigations were used to compile a schematic map of
the relief of the MohorovIcIc discontinuity. it was found that the accuracy of
determination of the thickness of the earth's crust to the Kohorovicic discontinu-
Ity on the basis of gravimetric data Is Influenced by the variation in Bouquer
anomalies depending on the thickness of sedimentary deposits and their density.
The paper includes an analysis and computation of the change of density of sedi-
mentary rocks with depth. As a result, it was established that at depths of the
order of-lo kmthere Is-no-differ-ence in denfltles between compacted sedimentary-
deposits and granite rocks. The upper 4-lun layer of sedimentary rocks exerts the
maximum Influence on the Bouguer anomaly. The collected data on the Influence
of the sedimentary layer were taken into account in determinations of the thickness
of the earth's crust. The computations of the latter were made by three methods:
standard columns of the earth's crust; the R. M. Demenitskava method; and the
Tsubol-Tomada-Aki method. The basis of all three methods Is described. This made
It possible to compile a schematic map of the relief of the Mohorovicic discon-
t(multyl the (sobath interval Is 3 kn- Thero Is a description of the Influence
of various factors an the accurac of determinaticri of th~., Mohoroylelc discon-
tinuity on the basis of gravimetric date. It has tern establAshed that the princl-
:,-,I'error in the latter is associated with the complexity of the structure of the
Zi3

L 10627-65
ACCESSION NR: AR4046166
studied area of the earth's crust. in the region of the Okhotskiy platform the
thickness of the earth's crust Is 25-30 km. In the southern basin of the Sea of
Okhotsk, In the central parts of the Kurile Island arc and In the little Kurillskly
Ridge the thickness of the earth's crust decrea5es-to 15-18 km, The northern
and southern groups of the Kurile Islands are characterized by an Increase In the
thickness of the earth's crust to 20-27 km, while to the south of Petropavlovsk-
Kamchatskiy the latter Is 30 km. The comparison of gravimetric data with deep
seismic sounding and airborne magnetometer surveys made it possible to detect the
boundaries between the sedimentary and crystalline rocks and between the "granite"
and "basalt" layers and detect zones of faults and the occurrence of thick "-
trusive strata, as well as determine the tectonic patterns for the Kurile Island
arc. S. ZhItnikova
ASSOCIATION; -Moskovskly universitet (Moscow University)
SUB CODE: ES ENCL., '00
Card 3/3

S 1/2-3- 5/WOOO/O()3/OM/002
AUTHOR: Solov'yev, 0. No and Gaynanov A
TiTtEll Features of the deep-seated geological structures of the transitional
zone from the asiatic continent to the pacific ocean in the region of
the kurilv-1mmchatka island an
PERIODICAL: Sovetskaya geologiya., now 3j, March 1963., pages 213-123
;.,.TEXT: The article deals with a complex and intensive geological and geophysical
study of the Xbrile-Kamchatka region in connection with International Geophysical
Year. . Observations were made by seimdo., gravimetric and magmetometrie methods*
Participatir~g agencies were Institut fizild zemli Akademii nauk TJSSR (Institute of
Physics of the Earth,, AS., LOSSR)., Vaesoyuzniy nauchno-issledovateltsk:Ly institut
razvedochnoi geofizild (A-11-Union Scientific Research Institute of Exploratory Geo-
phyBica)., Gosudarstvenniy astronomichealldy institute imeni P. K. Shternberga, (state
Astronomic Insta tit MOU (Geologioal
Itute im, Pe X, Sternberg), Geologicheskly fakull
Famaty of Moscow State University) and others& Overall direotion was by Institute
of Physics of the Earth.
A conal. .-erable bibliography (21 articles) main2,y by researchers of named
Card I of 3

S/215/63/000/003/001/002
Features of the deep-seatedesse
4. organizations is included, One U.S. source is cited since results in similar struc-
tural areas Are compareds Mason., R. B. and Raff, A. D. "Magnet., Survey of the West
.,:.,,Coast of N. America"., Bull. Geol. See* of Amere.ve
'72, No. 8., 19619
Purpose of the study is clarification of characteristics of the earth's crust
.--.in the region. 'By seismic methods., three types of earth crust were determined to ex-
ist in the region: 1. Three layered continental type, consisting of sedimentary.,
granitic and basaltic layers, averaging 20-30 km; near Sakhalin, Kamchatka., Northern
Xuriles and also between southern islands of the are and the deep water basins,
This continental typej characterized chiefly by its granitic layer., is typical of the
northern and central parts of the Sea of Okhotsk* 2. Oceanic type crust$ consisting
of a thin sedimentary- layer (up to 1 km) and bas 'alt (5-12 km)., and having an average
thickness of 10-17 km., including 5 Im of water. This is observed beyond the Kurile-
Kamchatka deep )mtor trough.* in the region of the ocean plateau. 3e, The intermedi-
-ate zone., differing from-'the continental by the absence of a granitic layer, and
from the oceanic by its_~dgnificantly thicker sedimentary layer. Comparing these.
.findings with those obtained by use of magnetometer surveysp discrepaneies were found
to exist& Several theories are postulated-as to reasons for this., and it is conolud-
ed that further research,, based on sei wd o.' gravimetric and magnetometric methods, is
~Card 2 of

0/,.15/63/000/003/0M/002
Features of the deep-seated*.*#
.,,necessary before a unified hypothesis can be developed.
IJ Further surveysj as well as more intensive study of available data are rec-
~ommended in order toclarify the deep structures of the complicated transitional
zone*
ASSOCIATIONt VsesoY'UzrO7 nauchno-Usledovatelakiy institut razvedochnoy -geogizild
(All-Union Scientific Research Institixte of Exploratory Geopbysios)
and Moskovskiy gosudarstvannyy universitet im. M. V. IoDmonosova
(Moscow State Vniveraity im. M, V. Lomonosov)
Caird 3 of3

GAYNANOV), A.G.; SOLOV'YEV, O.N.
Nature of magnetic anomalies In the area of transition from the
Asiatic continent to the Pacific Ocean. Dokl. AN SSSR 151 no.6t
1399-1401 Ag 163. (MIRA 16slo)
1. Predstavleno akademikom D.I.Shcherbakovym.

1. 12'454-65 0T(1)/FCr./F.F.C('&.) Po-4/Pi-4 R t~ E; I GW
-ACCESSION RVR: AP4048356, S/0215/64/000/010/0122/0128
AUTHORi Gaynanov, A. G.
. ".11
.TITLE: The nature of mamietio anomaliekalong transitional zones of the Pacific
Ocean
SOURCE: Sovetskaya geologiyal.nof lot 1964t 122-128
~TOPIC TAGS: geomagnetio fieldi Sgean\~Moho discontinuity
~.ABSTRACT- The author compares the topographic character of continental margins
:about the Pacific*border with variations in magnetic intensity across these zon e8,
.There is practically-no correlation between relief on the ocean floor and magnetic
anomalies. Few data are available onsusceptibilities of rocks on the North
.American side of the ocean floor. Several measuremen)s on the Asiatic side, on
basalto from the bottom, show variations from 200-10-0 to 3600-10-6 cm g,sec.
Relations between magnetic variations an d topography along the Asi&tic coast of the
Pacific are shown in Figs. 1-3 on the Enclosures. Profiles on the Hort-h American
sid
e are shown in Figs. 4 and 5 on the Enclosures. In the Kurile zone the upper
edge of the magnetically disturbed zone lies in the "basaltic" layer or' possiblyf
in the upper mantle. The lower edge also lies in the upper mantle. This means
Card

L 12'454-6~3
ACGESSIO14 Wq: AP4048356
;that the anomaly in the,oceanic segment is due to inhomogeneities in the upper
mantle. Depths to the upper edge have been computed to be 1-4 kmq to the lower
,edge 6-9 kn. The author considers the anomalies to be due to volcanic rocks of
.different thicknesses and ages. Computations for the Aleutian zone indicate the
,upper edge to be 14-24 kmq the lower edge 48-60 km in the deepwater basin, 4-14 km
,and 17-26 km along the island ridge, and 3-9 km and 15-25 km in the Bering Sea.
Basalts from drill holes at Guadalupe Island have susceptibilities ranging from
6 6
40- 10:_ to 1170- 1C cm g see. The direction of the remanent field is reverse. The
,author concludes that the cause of the ma6netic anomalies in the transitional zones'
.of -the Pacific Ocean is chiefly thermoremanent magrietiam of bodies, produced during,
in the earth's field. The variations in field may be due to variations in
position of the Mohorovicia discontinuity in passing from the continents to the
.ocean basin. Magnetic anomalies in the ocean basin may be due to sources in the
"basaltic" layer'or even in the "peridotitic" layer. Orig. art6 hast 5 figures.
~ASSOCIATION: Moskovskiy gosudarstvenr4r*y universitet im. M. V. Lcmonosova (Moscow
State UniveE2jty)
smmns ENCL: 05,
so CODE: ES NO REF SOVs 013 OTHERi 010~
Card 2/

L 1JE&66 EWT(~), GW__ __ ~ - - ____ 1 1- - - - - -
ACC NR*. AR6000807 SOUkE CODE: UR/0169/65/000/009/G004/005
.SOURCE: Ref. zh. Geofirika, Abs. 9G27
~AUTHOR: Gaynanov., A. G.'~
~TITLE: Some peculiarities in the structure of the earth's crust in transition zones
!of the Pacific Ocean a ording to ophysical data
9e
;CITED SOURCE: Sb. Geofiz.. issledovaniya. No. 1. M., Mosk. un-t, 1964, 228-241
TOPIC TAGS: geophysics, magnetic anomaly, gravitational field
TRANSLATION: 'A brief general survey of the results of Soviet and foreign geophysi-
~cal studies made In the Pacific Ocean. A general conclusion is drawn that the boun-
.dary regions of the ocean, which are transitional zones to the continental regions,
are characterized by-anomalous geophysical fields (gravitational, magnetic) associ-
-ated with the structure not only of the earth's crust, but also of the upper-mantle.
.This is shown by gravitational anomalies as the difference between the actual values
band those theoretically calculated for deep seismic sounding profiles assuming a
I
iconstant,density wiihin the layers of the earth's crust and the subcrustal layers.
!Card UDC: 550.311,551.14

'L 1'184&44
ACC MR: AR6000807
.According to ihe author, these anomalies indicate a discompaction of the material in
the upper mantle beneath ths-- Kuril and Aleutian Archipelagoes. ''Lower edgesiv (and.j
sometimes "upper. edges") of,magn6tic,disturbin.g masses'are also.frequently.associ-
ated with the upper mantle
SUB COEE.- 08

L 24823-6 EwT(l) AFnR aw
ACCESSION NR: AP4046375 S/0020/64/158/003/0594/0597
AUTHOR: Gaynanov, A, G.;'QE;bakov. S. A.
TITLE: Isostasy and plutonic structure of the zone of the transition of the Asiatic'
Continent toward the Pacific Ocean in the region of the Chishima- Kamchatka.
Depression
SOURCE: AN SSSR. Doklady*, v. 158, no. 3, 1964, 694-597
TOPIC TAGS: qjrL1j_c_rust, isostatic deflection, Chishima Kamchatka depression,
geology
i ABSTRACT: Recent investigations have disclosed that the earth crust hab a consi-
derable plasticity M A.'Heiskanen and F. A, Vening - Meinst, The Earth and its
Gravity Field, N. Y. 19518). The present paper investigates the isostatic state of
a given region by the method 'suggested by Lyustikh, Tr. Geofiz. inst. 38, 2 (19g6
in which the pressure P -WiHi = const. .' where d'i is the density of the !-layer,
H is the depth of the compensating surface, n-number of layers. This, expression
is valid for HA100 km. The method was applied to the study of the isostatic state
of the transition: Asiatic continent- Pacific Ocean, in the region of the Chishima-
tzrd 1/2

21427-66 EllV1)/FQQ/E'.'1A(h) G11
ACC NN AT6010298 SOURCE CODE: UR/3l95/65/OOO/oo6/oo6o/oo65
AUTHOR: Gaynanov, A.- G.; Tulina, Yu. V.; Kosminskaya, I. P.; Zverev, S. M.;
Solov'yev, 0. N.
ORG: none
TITLE: Comprehensive interpretation of data from geophysical observations in the
Sea of Okhotsk and the Kurile-Kamchatka zone of the Pacific Ocean
SOURCE: -All SSSR. MezhduveAomstvennyy geofizicheskiy komitet. Seysmicheskiye
issledovaniya, no. 6, 1965, 6o-65
TOPIC TAGS: seismology, gravimetry, geomagnetism, deep seismic sounding, geophysical
anomaly, transition zone
ABSTRACT: Data on the earth's crus- cquired during the IGY from geological and
geophysical studies (by magnetic, gravimetric, and seismic methods in ~he transi-
'Y I
tional zone between Asia and the Pacific Ocean were used to invest'ga two problems:
1) qualitative comparison of special features of anomalous gravitational and magnetic
fields with structures of the earth's crust determined by seismic data (deep seismic
sounding); and 2) some results from a quantitative ccmparison of gravitational and
magnetic anomalies -with deep selsmic-sounding data. A map of magnetic anomalies
shows moderate isometric anomalies in the Sea of Okhotsk and pronounced anomalies
in narrow belts in the Sea of Okhotsk, along the Kurile-Kamchatka ridge and adjacent

L ~, 1,127-66
ACC NR: AT6olO298
parts of the Pacific, and near the )Comandcrddye Islands. The sources of magnetic
anomalies in the North Okhotsk and Sakhalin depressions seem to be confined to the
uppermost or lowermost portions of the "granitic" layer and the upper part of the
."basaltic" layer. In areas in the Pacific off the Kurile Islands, the anomalies-are
in the uppermost part of the mantle, and east of the deep offshore trench, they are
in the upper mantle and the "basaltic" layer. It can be assumed that these magnetic
anomalies are caused by processes associated with the formation of discontinuities
and lava intrusions from the upper mantle onto the ocean floor. Comparisons of the
anomalous gravitational field with deep seismic-sounding data showed that the prin-
cipal features of the field coincide with the structures in the crust indicated by
the sounding data thus making it possible to identify regions of anomalous density.
Orig. art. has: 4 figures. [EO1
SUB CODE: 08/. SUBM DATE: none/ ATD PR.EBS,:
Card o/o k1\,%

L 7977-66
ACG NR: AP5026536 SOURCE CODE: UR/0286/65/000/019/OCY79/0080
AUTHORS: Veselov.-N, Je.;.Gmanov A G. Luginets, A. P.; Smirnov, L. P.;
Shelkovnikov
ORG: none
TITLEi Gravimeter for measuring the force of avi in motion. 'Class 42, No.
,-175257 Zannounced by All-Union Scientific Research Institute of Geophysical Recon-
naissance Methods Me-aoYuzYwY nauchno-issladovateltakiv institut aeofizicheakikh
metodov raZVedk:L)jq,55
SOURCE: Byulleten' izobreteniy i tovarnyk -80
vi znakov, no. 19, 1965j.79
TOPIC TAGS: gr t
gravitation
.!!vime er 1ELvime try,
A13STRACT: This Author Certificate presents a gravimeter for measuring the force
of gravity while in motion. The gravimeter is provided with an automatic com-
pensating system to-
'(see Fig. 1). It includes an elastic sensitive system, pho
electric converter of angular displacements, filter, amplifier, electric motor,
reducer, and measuring*potentiometer. To increase the accuracy of continuous
measurements of the gravity force, the quartz sensitive system of the gravimeter
Card 1/2 UDC: 550.831

L--7977-66--
!ACG NR: AP5026536
P11
Fig, 1, 1- pendulumj 2- damping plate; 3- spiral compensating spring
is provided with a damping plate rigidly connected to a pendulum. The plate is
located in the-opening b6tween the auxiliary immovable plates and a spiral com-
pen.sating spring. The auxiliary plates and the spring are submerged in a viscous
liquid. Orig. art. has: 1 figure.
SYB~CODE: IE/ SUBM DAIE: ~18Sep63
Card 2/2

L 52441-& ._EWP(1).,
ACC NR: AP5021211 SOURCE CODE: UR/0213/65/005/004/0684/0691
AUTHOR- Stroyev_, P.A.; Gaynanov, A.G.
ORG: Moscow State University im. M1. V. Lomonosov (Moskoveldy gosudarstvennyy
universitet)
TITLE: The structure of the Earth's crust In the Indian Ocean from geophysical inve'sti-
gation data
SOURCE: Okeanologiya, v. 5, no. 4, 1965, 684-691
TOPIC TAGS: ocean floor topography, oceanographic expedition, gravimetric analysis,
earth crust/Indian Ocean
ABSTRACT: The structuj~e of the Earth's crust under the Indian Ocean is not well knoww
The present article: 1) gives,a comprehensive survey, with 29 references, of geophysical
research carried out in the Indian Ocean from the first studies of Vening-Meiness in 1923.
to the present; 2) presents a comprehensive discussion of the newest results obtained -
during the IGY by British, US, and Soviet expeditions; 3) establishes, on the basis of
these recent data, the Capetown-Queen Maud Land and Ceylon-Shackelton Ice Shelf pro-
y_i~n~ Bouguer anomalies as function of
files; and__j)__p*Lents the graphs showingj4e 1~
C
j~ aier _--W2 7-- UDC: 550.311

1 5244a-~
ACC INR: AP5021211
the Indian Ocean depths. Orig. art. has: 2 formulas and 2 figures.
SUB CODE: ES SUBM DATE: 19Jun64 ORIG REP: 021 OTHER REP: 008
Card 2/2

L 08532-67 L14T (1) OW
ACC NR1 AP6
035596 SOURCE CODE: UR /038T/66/000/010/003~/~cl.-,--~-
AUTHOR: Gaynanov. A. 0.
ORG: Geology Department, q_qscov State University (Geologicheskly
fakulltet Moskovskly gosudarstyennyy univeraltet)
TITLE: Density inhomogeneity of the upper mantle
SOURCE: AN SSSR* Izvestlya, FIzIka Zemliq no, 10, 30-39
TOPIC TAGS: upper mantle, selemic.modeling, earth crust, gravity
anomaly, earth density measurement
ABSTRACT: Investigations of the correlation dependence of grfflo~ity
anomalies on the thickness of the Earth's crust,,carried out on various
models of a single-layer and doubfe--'lay_e_r' -c"rust' have shown that com-
putations of the density difference between layers of the Earth's crust
and the upper mantle using the formula for attraction of an infinitely
plane-parallel layer considerably underestimate the true difference
in density. Comparison of correlations between crustal thicknesseag as
determined from seismic data, and gravity anomalies for different
regions with correlations computed for models of the Earth's crust re-
veal the density Inhomogenelty of the upper mantle. This Inhomogenelty
is most evident In the transition zones from continents to oceans* To
Card 1/2 UDC: 550.312

L 08532-67
_kck' AP6035596
compute the effect of gravity, a model of the Earth's crust 120 km in
radius with an uplift of 15 km for cases with apexes located at depths
of 15, 30, 45, and 60 km was selected. Computations were made on the
"Strela" computer programmed by 0. K. Lityinenko and V. R. Melekhova of
Moscow State University for 18 different models of the Earth's crust
For the first three groups of models, the Earth's crust to assumed to
be a single layer or a double layer with the following density differ-
ences in subcrustal and crustal matter: 1) 3.4-2. 0.T g/cm39
2) 3.3-2.8 - 0.5 g/cm3, and 3) 3.2-2.9,- 0.3 g/cm1._ mmenfied
that in future Investigations gravity and seismic data be combined with
data obtained by 'iirtificial satellites so as to provide an even better
pictare of the horizontal density inhomogeneity of the'upper mantlee
Orig. art. bast 4 figures an4 3 formulase
SUi CODE: 08/ BUSH DAM 25Kar66/ ORIG REIN 018/ OTIN RZVt- 0091
ATD *PRESS: 5103
Card

ACC NR, AP6035896 131
INVENTOR: Gavninov A. r.; Dmitriyev, V. A,; Luginet A.-P.: Mikhavlova, K. K..;
Pantelelev. V. L.. Smirnov, L.P.
ORG: none
TITLE: Gravimeter for measurement of Rr~Li~ttv during motion. q~rlass 42. No. 187337
(announced by the All-Union Scientific Resea~ch Institute o0_ Geophysical
I - _r_0 - .1 -
Methods (Vsesoyuzi~yy nauchno-issledovWtel s 1~y institut geof'izicheskikh metodov
razvedki)]
SOURCE: Izobreteniya, promyshlennyye obraztsy, tovarnyye znaki, no. 20, 1966. 131
TOPIC TAGS: gravimetry, gravimeter, geodetic instrument, surveyi instrument"
ABSTRACT. An Author Certificate has been isstied for a irravimete7for the measure-
ment of gravity during,motion. The device consists of a gravimeter with double
optical-mechanical damping and two flexible quartz sensitive systems on a single
armature immersed in a damping fluid. To Increase measurement accuracy and work
productivity, the flexible sensitive systems have equal products of time constants
for each system on the scale division.
SUB CODE: 081 SUBM DATE: 23Apr65/ ATD PRESS: 5106
qrn a"ii

ACC INR: VI!6028018 SOURCE CODE: Uii/000O/63/O0O/ooo/oo66/oot6
AUVOR: Gaynanov. A.
ORG: none
TITIZ; Several results of gravimetric investigations in the Sea of Okhotsk, the
Kurile -nKa:nchutka depression, and in adjacent parts of the Pacific
SOURCE: Moscow. Universitet. Astronomicheskiy institut. Geologicheskiy fakul'tet.
~brskiye gravimetricheskiyd issledovaniya; sbornik statey, no. 2, 1963, 66-76
TOPIC TAGS: gravity measurement, marine pendulum, damped gravimeter, accelometer,
gravity anomaly, Bouguer reduction, anomaly gradient, Mohorovicic Discoju'rit4wil ,
6*94ver)7e7le-l ) -,9RrH !;re1i7-1d7a4PNq , 0CfN0,1C6,09Aq1Q -EJYPC017-1od le"Orim SE,4
ABSTRACT: Gravity measurements were made with a Soviet marine pendulum apparatus
and marine damped gravimeters. Second-order corrections for sea swells were
determined by accelerometers. A quartz clock was used for time measurements. The
low accuracy of the determination of the ship's position and sea depth caused a mean
lerror in Bouguer anomaly reductions of t6-8 mgt in regions with small gradients
and 115-20 mgi in regions with steep gradients. The northern part of the Sea of
Okhotsk and Sakhalin are characterized by weak positive and negative Bouguer
anomalies. The southern basin of the Sea of Okhotsk has intense positive Bouguer
anomalies. The arc formed by the Kurile Islands and the Kurile-Kamchatka deep
idepression have anomalies with great gradients located along the ridge beneath the
Card 1

ACC N1. AT6028018
water. In the northwest part of the Pacific, great positive Bouguer anomalies are
predominant. A schematic map of the Mohorovicic discontinunity was compiled on the
i basis of gravity anomalies and deep seismic soundings. The accuracy of the thickness
of -t~he earth's crust to the ~bhorovicic discontinunity depends upon the sediments
and 'their influence on the Bouguer anomalies. The maxiolm quantity or sediments was
I A'-'ound to the south of Sakhalin and the southern basin of the Sea of Okhotsk. The
density of the sediment matter was determined by an exponential formala. Table 1
shows the dependence of the gravity anomaly upon the Mass sediments. Bouguer
Table 1.
,.Thickness of sediments' 1 2 3 4 5 6 7 10
in km . . . . .
V ariations of Anomiay
-
-
1
1

3.n mg..-
--U
1 601
-8
. 1 1 -95 .-104 -11.21 -119 -k28

ACC MR: ATW28018
zinomalics woro corrected for sedie=t influence, and thickness of the cartUil:; cru:;t
*w,-w determiriod. A standard column for the whole thickness was chosen with a [.-(,-an
density consistinG of sediment, granite, and basalt layers. The thickness of the
colurm was determined from Bouguer anomalies allowing the depth of the Mohorovicic
surface to be computed. A preliminary map of depths was compiled for the Sea of
O'xdio'"k and the Pacific depression. Orig. art. has: 2 tables, 3 figures, and
12 formulas.
SUB CODE: 08/ 6UBM DATE: 22Nov63/ ORIG REF: 014/ OTH REF: 003
LCOrd 3/3

--AT7000193- OURCE-CODE.--M/ 0000/ 64-/000/000/0228/ 0241-7-1
ACC NR, S
AUTHOR: Gaynanov, A. G.
ORG: none
TITLE: Some characteristics of the structure of the earth's crust in the transition
zones of the Pacific Ocean
SOURCE: Moscow. * Universitet. Kafedra geofizicheskikh metodov iseledovanlya
zemnoy kory. Geofizicheskiye issledovaniya (Geophysical research), rso. 1. Moscow,
Izd-vo Xosk. univ., 1964, 228-241
0- 5--
TOPIC TAGS: e tMust, seismic profiling, gravity-survey, upper mantle, continents,
shelf, geophysic survey, earth structure/Pacific Ocean
ABSTRACT: A short general survey is presented of the results of Soviet and non-
Soviet geophysical investigations conducted in the Pacific Ocean. The general con-
clusion is drawn that the marginal zones of the ocean, those marking the transition
to the continents, possess features of anomalous geophysical fields (gravity and
magnetic) related to the structure not only of the earth's crust but of the upper
mantle as well. This is proven by the presence of remanent gravity anomalies obtaine
as the difference between their actual values and the values computed theoretically
for deep seismic profiling on the assumption of a constant density within the layers
of the earth's crust and subcrustal layer. These anomalies suggest a decrease in the
density of the upper mantle under the Kurile and Aleutian Island chains. Lower
Card 1/2

ACC NRt AT7000193
"fringes" and sometimes upper "fringes" of magnetically disturbed masses are often
associated vith the upper sentle. Orig. art. has: 3 figures.
SUB CODE: 08/ SUBM DMB: O5Kav64/ ORIG REF: 016/ OrH REF: 018/

ssil
lm;~, and 3. .1. SOA~vn~-), f I
Nery4IA. Naut S.S.S.R.
of cul- ilt
C-allod ILI:
"a thet~akjtl~
Lwa do-L by rvaiintcl!
'I, IS"i4d). FO r d~glcz; 'If v-C
I witit the cakw.- jf U-0 T
4 00 otual. allol IV ovrt 160

LYAMUTSKAYA', Ye.1 nauchnyy sotrudnik; GAYNANOVA? S', aspiratitka,
R1,O)VASHKITE, 0. (Puimakyte, O.b aup'lrantka
Garden posts reeding on leaves. Zashch. rast. ot vred. i bol.
10 no.12:261-27 165. (KIRA 19: 1)
1. Odesskaya sellskokhozya)stvennaya opy-tnaya stantsiya (for
1,yalyutskaya). 2. Saratovskly sel'skokhozyaystvennyy institut
(for Gaynanwa). 3. Litovskaya sellskokhozyaystvennaya akademiya
(for Puavashklte).

11-58-5-6/16
AUTHORS: Ivanov, B.V.; Mole'va, V.A.; Gaynanova, Ye.l.
TITLE: On the Alteration of Crystalline Scblvt During Heating (Ob
izmenenii kristallicheskogo slantsd pri nagrevanii)
PERIODICAL: Izvestiya Akademii Nauk SSSR, Seriya Geologicheskaya, 1958,
Nr 5, pp 60-77 (USSR)
ABSTRACT: The authors studied the alteration of the crystalline shist
in a block taken out of the lining of the furnace used
for the lime-calcination. This block was cut out of the
albito-actinolitic shist and the results of its roentgeno-
graphic study are given (Table 1). This block underwent
a long process of furnace heating and was composed of three
different colored parts: grey, brown, and dark-brown
(shokoladno korichnevaya). The microscopic study of the
grey part showed that its mineralogic composition remained
unchanged, and only the crystals of the actinolite were
gradually transformed into separate filaments. The results
of the roentgenographic study of this part (Table 4) show-
ed that it was composed of albinite, diopside, and hema-
tite. The last two products could be called the pseudo-
Card 1/4 morphic actinolite. The roentgenographic study also showed

11-58-5-6/16
On the Alteration of Cryatalline Scb1stDuring Heating
oxidation of the magnetite and its transformation into
hematite. The albite remained absolutely unchanged. The
brown part of the block, sharply differs from the grey
part in its structure and mineral composition. The lineal-
parallel texture disappears and the glass-like phase ap-
pears in a small quantity, indicating the beginning of the
melting of the rock. The transformation of the albite is
also observed. Its larger grains had started to melt and
its smaller grains were transformed into a mass of fine-
grained plagioclase. The labradorite was found in the
glass-like phase. The results of the roentgenographic
study are shown in Table 5. The dark-brown, porous part
of the block had a very dense caked structure and was
characterized by the presence of large and small pores.
Caverns were found in spots on the surface, filled by a
light-grey fine-grained mass. The albite disappeared
completely, it had melted and formed a part of the glass-
like mass. The quantity of the labradorite increased,
and a new product appeared in the glass - colorless cryB-
tals of pyroxene. The ferric oxides were also found in
Card 2/4 the glass-like substance, containing small cubic crystals

11-58-5-6/16
On the Alteration of Crystalline Schist. 3uring Heating
of secondary magnetite. Results of the roentgenographic
study of this part of the block are given in Table 6. The
caverns on the surface of the block were filled with a
powder, caked into a solid mass. Between this mass and
the dark-brown surface, small seams of characteristic mi-
nerals were formed. According to the authors, these seams
represent a miniature skarn. The roentgenographic study
of the powder showed that it was composed of calcite. The
seams were formed as a result of interaction of the lime
and the components of the block. The composition of these
seams were: well formed crystal of melilite; yellow-
green pyroxene and colorless pyroxene. The comparison of
the chemical analysis of the original minerals and of two
heated parts showed the identity of their composition,
which proved the supposition that in the zones of the
blocks of rocks, reactions in a hard state occur by the
redistribution of the oxides of the composing products
of the rock without addition of any now material.
There are 8 tables, 2 figures, 9 photos and 14 Soviet re-
Card 3/4 ferences.

11-58-5-6/16
On the Alteration of Crystalline sddot During Heating
ASSOCIATION: Institut geologii rudnykh mestorozhdeniy, petrografii,
mineralogii i geokhimii AN SSSR, Moscow ( Geological
Institubeof Ore Deposits, Petrography, Mineralogy and Geo-
chemistry of the AS USSR, Moscow)
SUBIAITTEDz 12 July 1957-
AVAILABLEt Library of Congress
Card 4/4 1. Rocks-Cryatal-Heating-Physical effects

IVAROV, B.V.; CATMHOVA,-X~,,1-i-(Hainanova, 0.1.1
Iron cordierite, Fe.~14S'5 0, from the bottom of an electric
furnace used for smelting calcium carbide [with summary in
Inglish]. Dop.AN UM no.12:1328-1331 '58. (MIRA 12.-1)
1. Institut geologii rudnykh mestorozhdaniy. petrografit.
mineralogil I geokhimil AN USSR. Predstavil akademik AN USSR
P.P.Budaikov (P.P.Buinykov].
(Cordierite)
I N

15(2)
AUTHORS: Tatarokayal T,D,j Gaynanovej Yea L. SOV/131-59-11-5/13
TITLE: Peculiarity of the-Destruotion of the Fireproof Casing of a
Molybdenum furnace With Hydrogen Filling
PLIZODIoAL: Ogneuporyt 1959, Nr 11t PP 507-510 (USSR)
433TRACT! In the work under review the authors carried out physico-
chemical as well an petrographio investigationa'af
high-aluminiferous oh&motte and magneelte for their use in
hydrogen medium. i1th respect to "he chamotte with high oontent
of aluminap 3amples were investigated from vault and bottom
of a molybdenum furnace with-hydrogen filling after uninter-
rupted work in tha.oourse of,12 days at a working temperature
of 15000 and were compared with a muffle sample before its use.
The sample from the furnace vault exhibits a Strong Chan90 in
its external appearance after use.-The furnace bottom changed
but little in its chemioal oomposition,(soo Table). The
petrographic investigation agrees basically with the ohemical
analysisp as may be seen from the miorostruotur*e in figures
I and 2. Magnesite sample@ of the casing of a molybdenum
,furnace with hydrogen filliAg were investigated after their
Card 1/3 use during 30 days at a working tempoiature of 16000. Their

Veoullarity of the Dentruation of the Fireproof SOV/131-59-11-5/13
Vasing of a Molybdenum Furnaos With. Hydrogen Filling
microotructuroo are shown in figures 3 and 4. It is atated in
conclusion that the refractories with a high content of alumina
change markudly after their use in the vault of a furnade with
hydrogen fillingp namely in their aoloring, density and
mineralogical structure. The porosity of the furnace bottom
dropped from 23.8 to 1.8~. Data,frcm publications are confirmedt
according to whioh.refraotories with an.SiO content are not
suited for use in hydrogen madiumt Under t9eae oonditione, at
tomperatures of from.1000 to 1600 0 compact oorundum.produots
are advisable. When used In hydrogen mediumt magnesite.&IaL-
changes markedlyt namely in coloring and.orystallization, which
ist however, not accompanied by a change in porosity, in
volumetrio weightp and in shrinkage. The use of ordinary
magnesits tiles in, hydrog8n medium can be rsoommended,only at
temperatures of 1400-1600 . There are 4 figures, 1 table, and
6 references. 3 of which;aro Soviet.
ASSOCIATIONt TeNIICh=ZT a Teentrallnyy nauahno-Iseledovatel'skiy institut
ohernoy metallurgiib (Central Scientific Research -Insti tut e of
Card 2/3 ferrous Metallurgy) Institut geologii rudnykh mostorozhdaniy,

Peculiurity of the Destruction of the Fireproof SOV/131-59-11-5/13
Casing of a Molybdenum nrnace With Hydrogen Filling
petrografii, mineralogii i geokhimii MI SSSR (Institute of
Gtology of Ore Deposits, Petrography, Mineralogy and
Geochemistry of the Academy of Sciences, USSR)
Card

GAYNANSMINA, A.M.; HAMAN, I.G.j
Efficiency in using production wells drilled in layer D, of
the Bavly oil fteld. Nefteprom.dalo nc.10;3-5 165.
(MIFtA 1,)I1)
1. Neftepromyslovoye upravieniye "Bavlyneft" i TaLarskly
neftyanny nauchno-isslpdovatellskiy institut.

GLYNASHIN, I.G.
Useful initiative. Bezop. truda v prom. 3 no.11:37 H '59.
(MIRA 13:3)
l.NefteproVolovoye upravleniye Bavlyneft'.
(Bavly--Oll fields--Safety measures)

ZINATULLINA, A.M.; DANILIN, R.A.; IWIKOV, R.A.
Stimulating the recovery of oil in the Bavly field by using
surfactants. Nefteprom. delo no.2124-26 164. (MIRA 17:4)
1. Neftepromyslovoye upravleniye "Bavlyneft'".

20921
S/057/61/031/003/005/019
B125/B202
AUTHORS: Zagorodnov, 0. G., agRberg, Yegorov, A. M., and
Bolotin, L. I.
TITLE: Multiplication of the frequency by means of plasmallslamming"
PERIODICAL: Zhurnal tekhnicheskoy fiziki, v. 31, no. 3, 1961, 297-300
TEXT: The present paper deals with the experimental study of the problem
of frequency multiplication-by slamming.. As.is knqwn,.,a Doppler effect
occurs when electromagnetic waves are reflected froik a moved surface. In
this case. frequency-'and amplitude of the incident. wave are changed. The
effect concerned.can-be considerably increased in,the case of multiple
reflection. This is attainel, e.g.., by concentrating the electromagnetic
energy in a volume completely or partially filled with the plasma. This
volume is then rapidly reduced by slamming the plasma. In this case not
only density but also the total electromagnetic energy are increased.
In the case concerned the energy of the photons that are multiply reflected
from the plasma is increased. This effects the reversal of the Fermi
Card 1/4

20921
S/057/61/031/003/005/019
Multiplication of the frequency... B125/B202
acceleration effect. In the case of multiple reflection frequency and
amplitude strofigly increase even in the case V 0))C(V4CC). This effect was
experimentally checked for an H Oil wave in the 10-cm region. The electro-
magnetic field was compressed in a resonator having the shape of a metallic
rectangular resonator. The plasma piston entered the resonator by a
grating consisting of three metal bands. The second front face of this
waveguide gradually passed into a waveguide with the critical wavelength
)LC r -4.6 Cm. This waveguide serves as filter for the harmonic frequencies.
The plasma piston was produced by a two-electrode discharge with special
ignitor and with additional electrodynamic acceleration. Fig. 1 shows the
general block diagram of the experimental arrangement. The beginning of
discharge can be regulated such that the plasma compression occurs two to
three microseconds after the beginning of the high-frequency pulse in the
waveguide. On slamming also the frequency of the electromagnetic field
increases as a result of multiple reflection from the moved plasma until
the frequency of the field exceeds the critical frequency of the waveguide
filter. Fig. 3 illustrates the oscillograms of the high-frequency signals
with the "multiplied" frequency at different instants of time of the
Card 2/4

20921
3/057/61/031/003/005/019
Multiplication of the frequency... B125/B202
plasma slamming. In this case the maximum pulse.height of the high-
frequency signal with the multiplied frequency-corresponds to the
shortest duration of slamming. These outputs are separated from the
high-frequ9noy pulse which-is interrupted by the moving piston by the
time interval T.. This time.interval corresponds.to the "slamming time",
i.e., the time required for.the.multiplication.of the frequency cf the
initial value (in this case 2840 m g
,e:gacycles) to, a..value slightly exceedir
the critical frequency of the wa uide (6530 megacycles). Thus, the
frequency was increased-by little more than 2..3 times. The spectrum of
the oscillations,produced-by the.magnetron..contained harmonic.osaillations
of small amplitudes which penetrate.into the..waveguide. Their amplitudes
reproduce the form of.the magnstron pulse. During slamming dissipation of
the field ener.gy. caused by losses.in the cavity.and in the plasma com-
pression occurs besides the frequency multiplication and the intensifica- V4
tion of the field amplitude. To obtain a sufficiently large amplitude
of the signal at the output the "slamming time" must be of the same order
of magnitude as the attenuation time To - q/6). In the experiments
described slamming takes -0.4 microseconds, which corresponds to a
Card 3/4

20921
S/057/61/031/003/005/019
Multiplication of the frequency... B125/B202
velocity of motion of 2-107 cm/sec of the plasma compression. Thus, it
was shown that by slamming a sufficiently strong frequency multiplication
can be attained. There are 3 figures and 8 referencest 6 Soviet-bloc and
2 non-Soviet-bloo. The 2 references to English language publications read
as follows: E. L. Ginston, Science, 127, 3303, 1858; A. C. Kolb, Phys.
Rev., 107t 345t 1957.
ASSOCIATION: Fiziko-tekhnioheskiy institut AN USSR Khartkov (Institute
of Physiosand Engineering of the AS UkrSSR Kharlkov)
SUBMITTED: May 20, 1960
Card 4/4

GAYNETDINOV. M.. kandekonomicheskikh nauk
Possibi-litiii~,itt~'-'i,owering costs on state fattening farms.
Mias. ind.-tSk'ji"40'.404-35 160. (MIRA 14:7)
1. Ityazanil4,'6&likokhozyaystvennyy inatitut.
(CAtle-Feeding and feeds)

GAYNETDINOVY M.
Beef cattle should be fattened in specialized enterprises. Kiss.
ind. SSSR 34 no.304-35 '63. (MIRA 16:7)
1. Ryazanskiy sel'skokhozyaystvennyy institut.

i /Z;, Z
GAYNNTDINGY, H'. kand. ekon. nauk.
,---~Capacity of livestock fattening farm. Klan. ind. SSSR 28 no.5:41 157.
(Bashkiria-Clattle-Fleeding and feeding stuffs) (MIR& lltl)

GITNNTDINOV. N.7.
-' -, _-_- - " ~ - - , "
Using attl1age an antmel feed. Spirt. prom. 24 no. 4:19-20 158.
(MIRA 11:7)
(Distilling Industries--By-products)
(Feeding and feeding stuffs)

f~-
GAUETIIIIIJOV, 14., dots.
. . ~ ~ - f - .. --- , i-,-
Fattening swine on distillers' food. Nau)m i porod.op.v soll-
khoz. 9 no.8:17-18 Ag '59. (MIRA 12:12)
1. Sverdlovskly sellakokhozvaystvannyy institut.
(Swine-Iondinc and foods)
(Distilling Industries-By-products)

&YNjW- iff, M.F.
Fattening of cattle with the by-products of the alcohol-industry.
Spirt.prom. 26 no-7:25-26 160. -.1 -;-.V .. -- (KRA 13:10)
.(Distilling induotrieo-*--'prOdU~C-6)' (Cattle-Feeding and foods)

GAYINETDINOV, M.F.
Wastes of distilleries as an important source for increasing
feed production. Spirt. prom. 29 no.7:35-37 163. (MIRA 16t12)
1. Rya7,anakiy sellskokhozynyutvannyy inatitut.

GAYNETDINOIJ, M.F.
Use of distMery wastes for cattle fattening. F6rm. i spirt
ixom. 30 no.6-.15,17 164. (" 171U)
1. I)razanBkiy sel IskokhozyaystvenVy inotitut.

GAYTIETDINOV, ",11.
Transportation or food industry by~pr~-Aucts used as feedo. Avt.
transp. 42 no.10:39-41 0 164, (NIIP]t 17: 11)
1. Ryazanskiy sellskokhozyny-.tvennyj institut.

WlllXEV,.,5.S.j-dota.; KIRILLOVA, A.A., doto., glav. red.;
BLAGOVESIMMISKAYA, N.N., dots., red.; SlITYAGINA, N.P.,
St. prepod.) red.
[Vertebrates of Ullyanovsk Province) Pozvonochnye zhivotriye
Ullianovskoi oblasti. Ullianovsk, Gos. podaeog. in-t, 1959.
74 p. (Ullyanovsk Province-Vertebrates) (MIRA 16:10)

GAYNOT, A.?.
q- - 1.
Identical correlatiou for binary Lie's rings. Usp.set.nauk 12
no.3:141-146 NY-Jo 057. (MIRA 10:10)
(Rings (Mathematics))

GAYNOVI A. T.
Cand Phys-Math Sci - (diss) "Several problems of the theory of
non-associative rings." Novosibirsk, 10,61. 9 pp; (Academy of
Sciences USSR, Siberian Division, Joint Academic Council for
Physics-Matbematics and Technical Sciences); 160 copies; free;
bibliography at end of text (11 entries); (KL, 7-61 sup, 218)

86369
8/020/60/13
C 111/ 0 333
AUTHORQ A. T.
TITLEt Free Commutative and Free Anticommutative Products of Algebras
PERIODICALs Doklady Akademii nalak- SSSR, 1960, Vol. 133, No. 6,
pp. 1275-1278
TEXT: Let the polylineal and homogo3neous polynomials p,(x I ---,x
(i = 1,2i ... ) of degree > 1 be elements of a free nonas~..iathe
algebra over a field JI with eburacteristic 0. If Ax oc E S are
algebras over dL , then - IF
F1 A
0,65
is said to be the nonassociat4ve free produot of the A which is
construsted under a certain self-ctijn of the bases L of the Ax
Let I be the set of all elements from G of the kind
o4 b. b b
.1 2 ... kPi 1
where C-A , b, Oj , c with ind!cea are regular words Qf the
6 in the sense of Kurosh (Ref.1), whero; If all the words
Card 1/5

86369
S/020/60/133/00,6/018/0~1ix
C !11/ C 333
Free Commutative and Free Anticommutative Products ol Alzebras
CLIP ... (J4 n have the length 11, than at least two of them lie in
different . Parentheaea are arbitrarily distributed in the
product b b b p -In't'on'
2" k i O'V- an.~) '11 '2 " 01' Det
The factor al-ebra G 6/1 is called the reduced free product of the
0
algebras AO(. i oC & S, which ij given by the identity relatione
(P) pi(x,,.., x .) - 0 or in shorti P-free product
n,&
of the algebras A,,
, and is denote with
G Tr " AC - A 17 A V.... . The author gi-es a se,:,ond equivalent
a4 1 2
definition, He enumerates nine propertlea of the P.-freo products,
e.g. I. A V B - B V A V. If G = A v B, and A is the bilateral
ideal which is generated by A in G, then It Is G/1 Q- B. Every
algebra, for the arbitrary elements x,, X,,P--., x . of which all
n4
the equations (P) are satisfied, is n6lle -algetra.
The reduced free products defined by the systems (K)(Xy - yx - 0
or (AK) xy + yx - 0 are denoted no free commutative K*free) or
free antioommutative (AK-A.ree) prod-tit~'-s of algebras.
Card 2/ 5

86369
S/020/60/133/006/0'18/031XX-
C i-1/ C 333
Free Commutative and Free Azitico=utative Products of Algebras
In the following P-free is understood as K-free or AK-free.
Theorem ls Let G - 77 A 7 F
OLk S
be the P-free product of arbitrary algebras AjK and of the free
P-algebra Fj let H be a P-algebra which is assumed to be a sub-
algebra of G. Then it is
H - 7 " BQ 7 V, where JT 7 is the same P-free
*Lr. S
product,
B a4 ~~ H /\ A rA and V a certain free P-algebra. V<
Theorem 2: Let G be a P-algebra with finitely many generators
(2) g-'Y g2w gn
and let G - Al A9 V ... Ak be a P-free product. By
elementary transformations (see (Ref-5)) the system (2) can be
Card 3/5

8636 9
S/020/60/133/006/Old/031XX
0 11V C 333
Free Commutative and Free Anticommutative Producto of Algebras
brought to a form such that all generators (2) lie in the factors
AV-! A k, wheret if gl, g? ... gI are all generators from (2)
which lie for instance in AV, then they generate A I'
The author Introduces the notion of the isomorphism of two P-froe
deoompositions of an algebra anti states that decompositions wit
irreducible fa-,tors are isomorphic.
A. G. Kuroah is mentioned. The auth-or thanks A. J. Malltsev and
A. J. Shirshov.
There are 5 Sovilet references.
EA.bstracter~a notes (Ref.1) concerns a paper of A. G. Kurosh in
Matematichesk.1y sbornik, 1947, Vol. 20, No. 2, p. 239; (Ref- 5)
concerns a paper of A. 0. Kurosh in Matematicheskly sbornik, 1955,
Vol- 37, No. 2, p. 251-1
Card 4/5

86 36 9
Si'0201601133100610181031XX
C 111/ C 333
Free Commutative and Free Anticommutative Products cf Algebras
ASSOCIATIONs Institut matematiki Sibirskogo otdeleniya Akademii
nauk SSSR (Institute of Mathematics of the Siberian
Department of the Academy of Sciences USSR)
PRESENTEDi April 14, 1960, by A. J. Malltsev, Academician
SUBMITTED: April 6, 1960
Card 5/5

GAYNOV, A.T.
Commutative and antico=ltative free products of algebras.
Sib.mat.zhur. 3 no.6.805-833 11--D 162. (MIRA 15:11)
(Algebra, Abstract)

GAYNOV, A.T.
Binary Lie algebras of the lower ranks. Alv. 1 1,-- " --. I-
21-40 163. . - I -, ~ - %,
Alternative algebras of ranks 3 and 4. lbid.:41-46
(MIRA 17:8)

KOZLOIISKI-Y, M.T.; GLUYSHEII, V.P.; ~AnRIKFS, K. Ya.; TI-1-IB-,T,, G.A.
i
Separation of bismuth from lead and some other metals by the
amalgam method in perchloric acid electrolytes. Zhur. prikl.
khim. 37 no.11:2402-Q-407 N 16), (MIRA 18:1)
Kazakhskiy gosudtrstvennyy urtiversitet.

AUTHOR: Gayntsevv A. F., Senior Engineer
SOV/92-58-1-5/22
T Drilling the Loose Devonian Argillaceous Rocks (Burenlye v
osypayushchikhsya argillitakh devona)
PERIODICAL: Neftyanik., 1958 3Nr lp pr, 7-8 (USM)
VA
ABSTRACT: The author states that serious difficultles are encountered in
drilling Devonian sedimentary rocks in the Stalingrad petroli-
ferous area. These difficulties are mostly caused by stalled
tools,, sudden puanp pressure increases, and even by the loss of
circulation. All these troubles begin vhen loose Devonian
argillaceoue rocks, 800-1#000 meters thick, are reached. Of
the total mulber of oil vells drilled during the last five
-years only two were drilled there to the depth of 288p--2936
meters, although it was plan d to reach the depth of 3000
meters. Various drilling fluids and reagents vere tested
during this period of time. Among other reagents the alkall
Card 1/3

Drilling the Loose Devonian Argillac6aus Rocks
SOV/92-58-1-5/22
carbonate solution (USbCbR) was used in various combinations with liquid
glass and soda ash. The successful drilling of the I-To. 205 cd]. well
proved that the UShChR content may be raised to 35-40 percent without
increasing the looseness of the formation drilled. The foUawing speci-
ficationn of the drilling mud may be recommended as a result of numerous
tests: viscosity at least 50 seconds.. shear stress., after one rirmtee.,
not less than 70-100 milligrams per cu.centimeter.-specific gra-vity no'.
less than 1.30., and water filtration at the borehole bottom 66 cu. centi-
meters. The problem of cleaning boreholes under exasting condItiona
should also be taken into consideretion because the pollution of the
drilling fluid increases -vith the deepening of pe-rforation. When 71sccas
solutions with UShChR are used., it is necessaxy to their
adhesiveness and to increase their fluidity in order to preve-nt clogging
in the formation. Oil-emulsions with an admixture of petroleum in Vie
amount of 10-12 percent and lime-starch solutions mixed with petrolt"=
may serve the purpose. These recommendations are based on observatiloms
made in the course of operations when drill tools were lover-ai 8--&
without difficulty., turbo-drills worked satisfactorily and op.~ratjl.~_,
pressure wan normal. Properly treated drilling fluids having the
Card 2/3

Drilling the Loose Devonian Argillacdous Rocks SOV/92-0-1-5/22
required rties may be useful for dtilling Devonian sedlLmentary rocks
in the Stalingrad region or in any other region where similar drilling
conditions prevail.
ASi*L4TX(X: ToWL tresta, Stalingradneftegazrazvedft -(TOM of the Stalingrad-
neftegazrazvedka Trust)
1. Petroleum industry 2. Drilling machines-Operation
3. Drilling fluids-Performance I+. Drilling fluids-Properties
Card 3/3

mi.j.; CAYIWISEV, A.F.; DUMCN, P.1-u.; ANAWYEV. A.N.
LIMES .
h
Industrial tests of chlorolignin a new viscosityreducing
reagent for drilling muds. Trudy MING no.2:20-26 163.
(MIRA 17:5)

GAMTSEV, F.M.
Possible main source of diamonds in the Southern Chunya Basin. Mat. po
geol. i pol.iskop.Kras.kraia no.3:237-239 162. (MIRA 17:2)

Electric '.'otors
lnoreasinr- the stabilily of mi electric notor wh(m vmrkinf- in tao pha-,es. -,rom. encrr..,
9, ro.'?, 19-~2.
N'onthly List of PuEsian Accession
s, Library of Conrresc-, October 'RMILP,~"IFM

N C
"VIIII3.37, 671 n1r,
'.;j. !~170MATIC rXCrrATlON W~GTJLATOTA FO: ';~,T A I L
i P F. ~'[) A L T~l 11,
, i y q JY.!Z;k i Qv-
--,:
(Mk-cow), 1956, No, 8, 7-9. ;'1 Vovi":Ian.

i, (.,r mnd Win,m-A rmall 100- $00 hVA high- spot! J:~ I!- ni., i~

V(;It 1~!, 1:~~

ar, r,)qulrvi :t "i

[1!i unif, coxilant lu U.017 Sin. chitractevistio, of -i i eplbtou

. GAYNTSLI
-2LIJ-~
Diaphysial fracturea of the bones of the forearm and their
treatment. Ortop.., travm.,i protez. no.ltl5-23 163.
(MIRA 16tlo)
1. Iz khirurgicheskogo otdola boltnitay cUya gornorabochikh
(glavnyy vrach - d6ktor meditsiny G.Gayntall) r Eysleibenev
Germanskaya Demokraticheskaya, Respublika.

GLYNUDINOVA P.M.- MWGWVAV le.K.
.--.
Copper and its forms in irrigated Fergana Valley soils. Uzb.
khim.sbur, 6 no.6123-27 162. (KM 1652)
1. Inotitut poohwovedmiya AV UsM
(1%rgdpa--%%il chemistry) (Copper-Anallsis)

GA'LNUIJN, G.A. (Leningrad)
Heating of 'the sewing machine neodlo during sewing. Shvien.
prom. no.6:14,15 11--D '61. (KER& 14:12)
(Sewing machines)

GAYNULINP G.A. (Imningrad)
Effect of the speed rate of the sewing machine operation on
the heating of the needle. Shvein. prom. no.3:16-19 YT-Je 163.
(MIRA 16:8)

GAYNULIN, G.A., inzh.
Study of the beating of a sewing machine needle depending on
its shape. Izv. vys. ucheb. zav.; tekh. leg* prom, no.42
140-l" 163. (MIRA 16:10)
1. Leningradskiy tekstilInyy institut imeni S.M. Kirova.
Rekomendovana kafedroy tekhnologii shveynogo proizvodstra.

ACCESSION NR: Ai4033371 8/2260/83/000/002/0007/0112
AUTHOR: Kondratyev. X. Ya.; Dirpva, M. P.;_qo Alin., L r.; Totmans, 0. r.
.--yw
TITLE: Infrared spectrum of absorption by water Vapor
SOURCE: Leningrad. UhiversiteL Problemy* fi&W atmodery*, - no. 2, 1963, 87-112
TOPIC TAGS: meteorology. atmospheric physics. Infrared absorption spectrum,
atmospheric liquid water content, water vapor absorption spectrum
ABSTRACT: In numerous studies of the spectra of liquid water the principal attention
has been given to the absorption bands, their. structure, position'in the frequency W418
and influence of impurities; little Is known conoefting the spectral absorption coefficients
in intermediary regions between the bands mad in certain cases data are contradictcry.
The authors therefore decided to determine the values of absorption by liquid water in a
broad spectral range. UM-14 and MS-12 Infrared spectrometers were used. Figures 1-7
of the Enclosure represent experimental results of the authors, constituting the principal
contribution of the ; a 10-page table In the or4onal gives the averaged values of the
coefficients. "The authors thank Isboratory specialist R. L Swirnova who did much work
in connection with We pmjed. OrI& art. has: 16 figur" and 6 tobles.
Gard

ACCESSION NR.- AT4033371.
ASSOCL4,TlON-. An wl"wdtd (ladngnLd Univusity)
SUMMED: 00 DATZ ACQ: 23APC64
SUB CODE: ES NO RzF 80v: 013
ENCL- 07
OTHER: 014

OATMIN, T. R. ~ -
Materials on epizootiology of paratuberculous enteritis of enttle in the
Bashkir ASSR. Veterinaril&, 29, No 6, 1952.

GAYSULLIN. TR,. kwAidat vateriumnykh nauk.
Treatment of cattle in paratuberculaus enteritle. Yeterinarila
32 no.11:27-29 N 155. (MMA 6; 12)
1.V&&WdrobW& usuchno-Iseledevatellmkaya veterinarnaye, opytnays,
stantelya.
WOMMIS DISMU)

USSR/Diseases of Farm Animals - Diseases Caused by Bacteria and
Fungi
Abs Jour : Ref zhur Biol., No. 6, 1950, 26299
Author : Ownullin, T.R.
Z
Inst : Kazan' Scientific Research Veterinary Institute.
Title : Hidden Bacillus Transmission in Paratuberculosis of
Large Homed Cattle Ze Author's Own Report).
R.
OriG Pub : Byul. nauchno-telchn. inform. Kazansk. n.-i. vet. ing-ta,
1957, Wo 1j. 20-21
Abstract : Microscopic examination of bacteria in biopsy specimens
of intestinal mucosa of the rectum of four clinically
healthy heads of cattle from farms where paratuberculo-
sis vas present, uncovered paratuborcullur bacteria.
When allergen was applied these animals showc-1- a
Card 1/2

GAmIN, T. R.
C*,j - v J
"Therapy by means of sulfanilamide praparations in the case of
p aratuberculosis.11
Veterinariya, Vol- 37, No. 8., 1960,.p. 27
~ C;_ /&. V~,_t - Al./ tv) z Kk, "L-4 +ij ~

GAYNULLINJ, T.R., kand.veterinarnvkh nauk
Sulfanilamide therapy in paratuberculosis. Veterinariia 37
no.8:27-30 Ag 160. (MIU 15-4)
1. Nauchuo-Issledovatellskays. veterinarno-bakteriologicheskaya
laboratoriya Ministerstva sellskogo khozyaystva Bashkirskoy ASSR.
(Johaels disease) (Sulfanilamide)

GAYNULLINp T.R.., kand.veterinamykh nauk
Complement fixation reaction in the diagnosis of paratuberculosis.
Veterinariia 39 no.1:30 A 162. (MIRA 15:2)
L, Bashkirskaya nauchno-issledovatellskaya veterinarno-
baktariologichaskaya-laboratoriya.
(Johne's disease)
(Complement fixation)

GAYMULLIN,, T.R.,.kand. vaterin. nauk
Ralaing healtby calves from cove Infected with -par&6&w~osim.
vaterinarlia-41-no.4839 Ap 164. (KIRJL 17:8)
1. Bashkirskaya naucbno.-proizvodBtvsnnaya veterinarnaya
liLboratoriyao

GAYMUINA, A. YA.
20023 GAY-IMIINA A. YA. Pazvitiye angorskogo kozoudstva. Sel. khoz-vo
tadzhikistana, 19~9, No. 3, S. 54-55.
T)VIGHTS01, V. Mekhani atsiya i organizatsiya truda v kolkhoznom
kormoproizvodstue. - sm. 2w.
SO: LEMPIS ZHUMU STATEY, Vol. 27, Moskva, 1949.

GAYNULLINA, Xh.G., veterinarnvy vrach.
Modified method of diagnosing rabies. Vaterinariia 31 no.2:32
F 154. (HLRA 7:2)
1. Bashkirskaya reepublilmnskara vaterinarnaya baktariologicho-
okaya, laboratorlya.
(Veterinary "dicine-Diagnosis) (Hydrophobia)

GU99ROVA, M.Kh.; ARISTOVA, T.T.; GILIKAMOVA, R.G.; LIVOT, F.Y.; BUKCHAWAYNA.
M.S.: HUXILIMICTSIUMA. N.A.; KHRAMOVA, M.P.;
KORRANOTA, I.M.. red.; LABUDII. N.T., red.; IBROGIMOVA. Z.A.,
tekhn.red.
[Forty years of the Tatar A.S.S.R.; statistical collection]
Tatarsksla ASSH z9 40 let.- statisticheakii abornik. Kazaul,
Tatarskoe knizhnoe Izd-vo, 1960. 171 p. (Km 14:3)
1. Tatar A.S.S.R. Statistichaskoye upravlaniye. 2. Nachallnik
Statiaticheakogo upravleniya Tatarskoy ASSR (for lobranove).
(Tatar A.S.S.R.-Statistics)

KHLBIBULLIN, Sh.T,.-; GA7NU
Analysis of visual and photographic star counts in the direction of
,the nebula"North America*. Uch.sap.Kas.un. 116 no.5:63-68 '56.
(MLRA 10:4)
1. lafedra astronomil.
(Stars--Distribution)

88938
S/035/61/000/001/014/019
9/4/0 AOO1/AOO1
Translation froms Roforativn7y zhurnal, Astronomlya IGeodazlya, 1961, No. 1,
P. 58, # 1A413
AUTHOR: __~a~yn~. ~..-
TITLEt Spectrophotometry of Red Portion of the Spectrum of Low-Latitude
Aurora of September 29-30, 195T
PERIODICAL: -"Ixv.Astrof1x.in-t& AN MaSSWO 1959, Vol.8, pp-79-81 (Engl.aummaxy)
TEXT: The author presents-resulte of determining intensity of rod lines
63oo and 6364 (oi) during the aurora of September 29-30, 1957, on the Kamensk
plateau near Alma-Ata-Vith a (0-48;(9P-48) speatrogroph. The absolute values of
intensities were obtained by. oamparlngwith the Suh. "The Intensities of lines ?L
6300 and 6364 turn*d,ouj to b*.10 0--7 and 41xlo-3 erg/am sea sterad respectively
at 17h52m UT and 38,40--7 and IWO!ilerg/cm2sec st*rad at 21h551n UT. There are 7
references.
N. D.
Translator's note:. This In-the full translation of the original Russian abstract.
Card 1/1