SCIENTIFIC ABSTRACT BALAURE, F. - BALAYAN, M. S.

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• Collection: Scientific Abstracts
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• Document Creation Date: January 3, 2017
• Document Release Date: July 27, 2000
• Sequence Number: 15
• Publication Date: December 31, 1967
• Content Type: SCIENCEAB

BALAURE, Fl.; WOOREScut C.
Carrying out the polioy of the Rumanian Workers Party in the liquida-
tion of the kulaks as a class. Problem soon 34 no,70-15 Jl 161.
BAuum, n.
Completion of collectivization,, the triumph of Leninist policy in
the kttmanian villages. Problems soon 15 no.1200-106 D 162.
6AI A.,rr,'r ~ 1 -1.
So- I
, IM ('O',131,10rFktA(-,nJ Or~ t~O 'flOtIrY .3f sw!alrr,. Problew
mnc,n IF no.1.17-V J& 165.
FENTEA, N'., Ing.; BALAUTA, M., Ing.
An Installntior "-r Insiming the firtit grade consumern with
electric power from the IndustrIal Complex, fira.'Aa. Cel
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( ~lf I v- '~ . 1, '70. ":, I'll"'.0, "'.. 5
ARUILIk, M.S.; . BAJAVAM..A. ...,
Density of rooks at lakhetia. Trudy Inst.geofisAN Oru&.SU Ili
111-135 '49. (Mw 9:8)
(Xkkhotla...-Prospooting--GeophysteaI wAthoas)
---- -I,- -BALAVADZEV D4--K-# - -- --- - - --- - ---- - --- - ----
2. USSR (600)
4o Varioneter
7. Temperature cycle in the field themo chamber of a gravitation vari(~wter.
Soob. AN Grua. SSR 11 No.. 6, 1950.
9. Monthl List of Russian Accessions, Library of Congress, April. -1953, Uncl.
BALAUDZE, B.K.,- SHENALAYA, G.Sh.
XxImrimental determination of the vertical gradient of gravIty.
Dokl.AN SSSR 93 no.1:69-71 Mr 154. (KLRA 7:3)
1. Institut geofIzIkI Akademil nauk Grusinskoy SSR. (Gravity)
:3 -i
Un-I&RIGec hysies '7-
- Akm_vlty gradient
cam 1/1 Pub. 45-5/12
Author Balavadzej, B. K.
Title Procedure for the determination of the vertical gradient ef gravity
Periodical UY. AN SSSHj Ser. geotiz., 45-56, Jan-Feb 1955
Abstract The author expounds the results of a field determination of the anomaly
of vertical gradient of gravity by means of the quartz gravimeter. He
indicates the possibility of the utilization of these results for the
purposes of geophysical prospecting. In order to reduce the force-of
gravity to the level of reference or to study the distribution of plu-
tonic anomalous masses it is necesoary~to use the regional part of the
anomaly In the gradient, vh1ch part can easily be computed in accordance
with a smoothed map of gravity differences (gravity increrents or dec-
rements,, Ag). Fifteen references; e.g. YU. D. Bulanthe, "Tables for
treating of observations with quartz grayineters,*4 Moscow, 1952; A. K.
Manlovichko# "Study on the analytic extensions of gravitational anoma-
liesp" Trudy Novosib. In-ta inzh. geodetil, serofotoo"yemki I karto-
grafii, Vol. IV, 1951.
Institution : Institute of Geophysics, Academy of Sciences Georgian SSR
Submitted : December 26, 1953
U,W/G,6,-)physics--- G--r-a-v-i-t-y--g---r-a-d-i--e- nt_ ID--270-9 - -----
Ca rd 1/2 Pub. 45 - 3/13
Author : Balavadze, B. K.

Title : Problem of calculating the vertical gradient of gravity
Periodical : Izv. AN SSSR, Ser. geofiz., Sep-Oct 1955, 425-434
Abstract : The author Investigates the problem of the accuracy calcu-
lating the anomaly of the vertical gradient of gravity
according to the gravimetric map. He concludes that the
accuracy of calculating the full value of the vertical
gradient of gravity by mans of the computational formulas
of A. K. Malovichko ("Study by analytic continuation of
gravitational anomalies," Trudy Novosibirskogo in-ta inzhen-
ernoy geodeiii, aeroslyemki I kartografii, IV, 1951) and
W. Hoffmann ("Ueber Anwendungen einer Formel zur Berechnung
des Vertikalgradienten der Schvere," Geofisica purs, e appli-
cata., 14, No 3-4, 145-161, 1946) depends directly on the
depth of the anomalous masses if the influence of the cen-
tral zone is not consideredo and that the full value of the
vertical gradient can be obtained by the indicated method if
the anomalous masses are sufficiently deep under the point
of observation; the errors In the computation of the verti-
cal gradient increase sharply with the approach of anomalous
FD-2169
Card 2/2
Abstract manes to the point of dbeervation. The result of the cal-
culation of the vertical gradient according to a map of the
anomaly of gravitationj especially for a smoothed map, corres-
ponds to the regional part of this gradient, vhich is of con-
siderable Interest particularly in the reduction. of gravity.
Eight references.
Institution: i Institute of Geophysics, Academy of Sciences Georgian SSR
Submitted : July 1, 1954
TkAI-AVADZZ, B.N.
-&
Hatoactivity of some hot springs of Tkyarcholl. Soob.AX Orus.
6M 16 no.10:781-784 155. (" 915)
1. Akademiya mauk Orusinskay SU, Institut gooftsiki, Tbilisi.
Prodstayleno deystyltell We chlenom Akadeall A.A. Tvalchrelidse.
(ftvarchall-Springs)
DIUVADZIC. D.K.-
IN lb~-
Use of-gravitation vi%ricesters In underground surveying Cla Georgian
with. summary In Russian]. Tmdr Inst.coof Is.AN Orus.&U, 15129-34
056. ~ (NLU 10: 7)
(Kagnetlo varloseter)
I Li IV ! i T_% -T
X10) PHASN I BOOK ETWITATI011 sov/1663
Akademiya, nauk SM. Kmitet po goodezil I geoftsikee
Tezisy dokladov n& X1 Generalluoy ussableye Xezhdwt&rodnogo geode4icheskogo
I geofizicheskogo soyuzae Methdunarodn" assotsiatsiya saysmologii I
fitiki nedr zemli (Abstracts of Reports Submitted to the XI General
Assembly of the International Union of Geodesy and Geophysics. The
International Association of Seismology and Physics of the Earth's
Interior) Moscow, 1957. 102 Vs /P&r*uei torts in Russian &n& English/
1,500 copies printed.
No additional contributors mentioned
PURPOSE: This booklet Is Intended for geophysicists, especially those special-
Izing in seismology.
COYMMIt, This collection of articles deals with the structure and composition
of the Earth and phencmena related thereto. The majority of the articles con-
cern studies of e&rthquakes and, seisaia waves - Other articles cover the struc-
ture of the Earth's crust and. mountain roots; the elastic properties of rocks
at high pressures; the piezoelectric effect of rocks and the method of
Card l/ 5
Abstracts of Reports (Cont.) 80V/1663
modelling In tectonophysics. The collection also contains articles on the
Birth's thermal history, the microseismic method of tracing storms%and others.
No references am given.
TABLE Or CONT
Belousov, V.Vt Types and Origin of Folding 5
Belousovp V-V- Development of Geosynclinee 11
Balavadgeo, BOK*jand G*K. Tvaltvadze. Structure of the Earth's Crust
in Georgia Determined ?r= Geophysical Data 13
Bunes, V.I. 33cparience in Using Energy Characteristics in the Study of
Tadzhikistan Seismicity 20
Vved*uskV&l AeV,.p4md LA., BKIWdna* Sme PecUlarities of a Displace.
ment Fleld of P - and 8: Ways Propagation in the Earth I s Mantle 23
Volarovich,.M.P., Z.1. Stakhovskaysand D.B. Balitshoy. Investigation
of Elastic Properties 6f Rocks at High Pressures in Connection
With Geophysical Problma 25
Card 2/5
Abstracts of Reports (cont.) sov,/1663
Volarovich., M.P. and I.I. Parkhmanko. Pieozoelectric Effect of Rocks 29
Ve7tsman, P.S.,I. P. KosmInsk"a" mind Tu. V. Ritnichenko. Now Evidence
on the Structure of the larth's Crust and Mountain Roots in Central
Asia From Selesic Depth Bounding Data 31
Ozovskiy,, M,V. Method of Modelling in Tectonophysics 37
Gorshkoy, G.P. Seismic Intensity Rqgions of Asia 42
Davydov, B.Z. Physie&l Prorrties of Soild Bodies at High Pressures 43
Ke7lis-B~rok, V.I. Investigation of Earthquake Mechanism 46
Keylls-Brok, Volo Dinamic Methods of Investigating the Earth's Crust
and Internal Structure (Theor7, Electronic Camputationa and
Practical Tests) 51
Kam,, Ye.V* Absorption of Elastic Waves in Rocks 55
Card 3/5
Abstracts of Reports (Cont.) SOV11663
Kondorskaya, NeVs Travel Times and Scme Dynamic Characteristics of
Seismic Waves 58
Wimova, Ye.A. 1114e Swrth's Tbemal: History and Its Geophysical
Consequences 63,
Madvedev, S.V.,and B.A. Petrushevbkiy. Yethods and Experience in
Zoning*UM Territory According to Seismic Intensity 66
Magaitskii,-V.A. Properties of the Earth's Mantle and the Physical
Nature of the Intemediate L&yer (L4yer C ) 70
Monakhov, F61. Develoluent. of the Microssismic Method of Tracing
Stoz= at 'sea 74
Rykunov, LoNs Study of the Character of Decrease of P-Wave Amplitudes in
the Shadow Zone on a Model 78
SoloTlyev, S.L. The Energy and Intensity of Earthquakes 81
Savarenskiyo T96F, Results of Seismic Studies in the UNR 84
Federov, YeeP,- ResearchAn Nutation in Connection With Some Problems
of the EartIL's Constitution 90
Card 4/5
Abstracts of Reports (Cont.) sov/1663
Sbaidt, O.Yu. (deceased)$ and BoUs Levine Origin and Campoeltion of
the Earth
Shebalin. N*V* Correlation Between Magnitude and Intensity of
Earthquakes and Asthanosphere
AVAILABLE: Library of Congress (Q3 5~4,0)
Card 5/5
5-if-'59
9D
97
professor; doktor fisiko-ustaimaticheskikh-nauk; HOL4MMKIT,
m $0, otystetweaW r*dsktorl TTAIRVADZI. 0.1.. kandidat fisilro-
,;; tomatiaheskikh nauko otystetvenW radaktor-, UKRADZIp D,S,.$
redaktor.- UMCHKOV. S.R., tokhmitchesidy redaktor
[Gravitational field and struoture of the earth's omet In Georgial
Gravitattionnoe pole I, stroante seanot kory v OruziL. Tbilisi$
1zd-To Akadensuk Orusinskot SU, 1957. 120 p. (Kw, 1017)
1. Ch1sa-korrespondent Almdomil nauk SSSR (for Molodenskiy)
(Orsylty) (Sarth-Surface)
UUTADZA, D.K.
Tarloutria ablOrlStiftf It the GoUthVeStorn ooloble and r~#Ulto
of their Interpretation* trudy Inst, g*ofis. AN Grus, Sn 16t22
230 '57- (Colchis-Oravity) (XMA 1116~
(Colohle-Geolo,S7, Stratigraphlo)
BALAVADZN. D.X.
Classification of gravitational snomall** In a geosynallual rogion.
Boob. AN Orus.BMt 18 50o2:155-157 7 '57. (KW 10:7)
1, Akademlys, nauk Orusluskoy SSR, Institut gooftsiki, Tbilisi,
Pr*astavleno skadoulkom G.B.Dsoteenidus.
(Gravity)
RAIAVADZE, R.K.
Xffect of topographic masses on the vertical gradient of grolvity.
Soob.AN Grus.SSI 19 no.lr29-32 JI 157. (XIRA 10:12)
1. AN Grd%SSR, Inatitiat geotiatki, Tbilisi. Predstavlano chlenou-
korrespondentou Akademil, V.1.9azaaakhlisovyu.
(Gravity)
AUiHORS: Balavadze, B.K. and Tvaltvadze, G.K. SOV/49-58-9-2/14
T.ITLB-. 6onsti`uc ~arthls Crust of Georgia as Determined
by Geophysical Data (Stroyeniye Zemnoy kory v Pruzil, po
geofizicheskim da W m)
PERIOD10AL: Izvestiya Akademii Nauk SSSR, Seriya geofizicheskaya,
1958, Br 9, PP 1025 - 1084 (USSR>
ABSTRAM As a result of the seismic survey earried out in 1941-1945
in Georg*n SSR,# it was possible to determine three layers
of the Eartia's cruet: the first, 3.5 - 4 km deep in
which the longitudinal and transverse waves travelled with
the velocities V ip - 4.4 km/sec. and V is - 2.6 km/see
respectively; the second layers, 20 km deep with
v2p - 5-6 km/sec and V28 - 3.2 km/sec and the third
layer having V 3P ' 6.5 km/see and V 3B - 4.0 km/see
It was estimated that the NdkhorWUbdrA- 1"erls situated
at the depth of 48 km. Similar results were obtained from
an experimental deep-detonatioa in 1954 in the Tkibuli
area (Figure 1). The three layers were estimated to be
composed of sedimentations, granite and bazalt,
(;ardl/4 respectively.
SOV/49-58-9-2/14
vonstruction of Xarthle Crust of Georgia as Letermined by
Ueophysical Data
The sedimentary layer was investigated in various regions.
In the *Akhraaskaya dalina (v&Uey). its 'thlek4ess
varied from several meters (Dzirul) to 4 km (Karellskiy rayon).
Wave velocities differed very much but it could. be
established that. the thin layers Drmed during the post-
Tertiary era were characterised by velocities ranging from
1 400 to 2 500 m/sec, while the upper parts of the
Tertiary layers were having velocities of 4 200 - 4 400
m/sec. In West Georgia, the thickness of the sedimentary
layer was found to be not so great to the isast and almost
10 km thick near the coast of the Black Sea kFigures 2 and
3). The whole area showed the wave boundarl velocity
to be 5 500 - 6 400, m/sec but 9-10 km1sec in the Dzirula
which shows shallow foundations in this region.
The gravimetric measurements were carried out in.all
regions and plotted. The charts showed the anomalies such
as the areas of minimum and maximum of the vertical
gradients reaching 35 mgl. Large gravitational minimum
fields were found in the region of Great Caucasus and Dzha-
uard2/4 Ydkhetskiy vangb. Maximum fields were found in the
SOV/49-58-9-2/14
Construction of Narth's Grust of Georgia as Uetermined. by
U;''eophysical i~ata
crystallic regions of Dzirula, and Lok.
In order to determine the character of the anomalies of
gravitational force a comparison was made between the
gravimetric, geological and densometric charts. As a
result, a z ationship between the structure of the "rth's
crust and the anomalies was defined. Figure 4 shows a
general character of this relationship (I - direct,
II - inverse relations, a, v, e, z - positive,
b, S, d, zh - negative anomalies; 1 - sediments,
2 - granite, 3 - basalt, 4 -foundation). The actual
cross-seotions are shown in Figures 5 - 7. These represent
the most characteristic profiles, marked 1, 111 and IV
in Figure 3.
It should be noted that the gravitational method of
determination of the geological structure requires further
investigation before it can be generally applied, especially
in the regions of less developed seismic observations.
t;ard3/4
r SOV/49-58-9-2/14
. Constructioh of Earth's Crustof Georgia as Determined by
Geopusical Data
There are 7 figures and 18 references, 13 of which are
goviet, 4 English and 1 Dutch.
ASSOCIATIONt Akademiya, nauk Gruzinskoy SSR,Inatitut Seofiziki
(Ac.Soo Georgian SSR,Inatitute of Geophysics)
SUBMITTED: June 12, 1957
Card 4/4
BAIAVADtl,-B-K.; SMIGNUU, O-Sh.
Density determination of rock Iskyers br un4arground gravity
measurements. Trudy Instageofis.AN Orus,SSR 17047-433 '58-
I (KIPIA l3t4)
L Institut geofts1kt AN OrusSSR Thillel.
(Caucasus-Rocks--Density) tGravity)
TVANTADIN, GK*j BTUS, Tej., asslushounyy daystall nauklo otyeredo;
_YADZ".K.. prof., doktor f1s.-satau.nauk, otv.red.1
AULIAMI, VA.. red.Isd-va: TOWA, A.R.. takhred.
(Crustal structure In Georgia based on seismic date and the
plotting of systems of theoretical hodographal Stroanle samol
kory v Orusil po, sainalohaskis dannym I postrosale slates tooreti-
Ohesklkh godogrefove ThIllal. Izd-vo Akad.nank Grusinskol. SM.
1960. 142 p. (KIRA 13t11)
(Osorgla-larth-Sarfoos) (Bodograph)
S/63Y6O/OOO/OO2/OO6/OO6
D055 D114
AUTHOM Balavadze, B.K.; Tvaltvadze, G.K.
TITLE-j The structure of the Earth's crust of the Transcaucasian-Caspian
Depression according to geophysical data
SOURCEs International Geological Congress, 21st.Copenhagen, 1960. Doklady
sovetakikh geologov, problems. 2t Geologicheskiye resulltaty
prikladnoy gookhimii i goofisiki. Razdel ID Goofizika.Glubinnoye
stroyeniye zemli po geofizicheskim dannym, 82-90
TEXT% The Institut fiziki Zemli AN 38SR (Institute of Physics of the Earth
AS USSR)t Institut goofiziki AN Gruzinskoy $BE (Institute of Geophysics AS
Gruzinekaya SSR) and geophysical organizations of the Ministerstvo geologii
i okhrany nedr SSSR (Ministry of Geology and Conservation of Mineral Re-
sources USSR) and the Ministerstvo. neftyanoy promyshlennosti Azerbayd-
zhanskoy SSR (Ministry of the Oil Industry Azerbaydzhanakaya SSR) have for
several years been studying the structure of the Earth's crust in the
Caucasus and the seas around it. From the material available on the sub-
ject, the authors have selected that part which deals with the Transcau-
Card 1/4
9/63 60/000/002/006/006
The structure of the Earth's ..... D055YD114
casian-Caspian Depression. In particular, the profile of a narrow belt
along a line through Anakliya - the Suramakiy Range - Min ech U
t Sul : rt
Byandovan - Caspian Sea - Karshi (Krasnovodekiy Pon n 41 w a udied for
the structure of the crust. The results of gravimetric measurements are
described; the geological interpretation of anomalies in the force of grav-
ity in parts of the Transcaucasian Plain has been given in several published
works, e.g. V.V. Fedynekiy (Ref. 161 Gravimetricheeka a kha akteristika
predgornykh i mezhgornykh vpadin v geosinklinalyakh ~Gravimretric Character-
istics of Depressions Close To and Between Mountains n Geosynclineel . Sb.
pamynti akad. A.D, Arkhangellskogo, AN SSSR, 1951). Seismic studies of the
crust in the inter-mountain depression of Georgia were carried out under
Academician G.A. Gamburtsev. B.S. Khachaturyan and B. D. Trebukova of the
Azerbaydzhanskaya kontora morskoy geofizicheskoy razvedki (Azerbaydzhan
Office for Geophysical Sea Surveying) made deep seismic soundings of the
crust in 1957 in Southeast Aserbaydzhan. The same method was adopted for
the Caspian Sea by the Institute of Earth Physics in 1956. Isodepth charts
were compiled for the crystalline base, basalt and Yohorovicic surfaces in
the central area of the Caspian, and a seismic section of the crust was
made along a line from Lenkoran' to Kraenovodskiy Peninsula. Recordings of
Card 2/4
S163016010CO100210061006
The structure of the Earth's .... D055/Dll4
elastic waves derived from explosions in mining and construction work were
used by Ye.A. Koridalin and G.K. Tvaltvadze to study the crust in the region
of Mingechaur. The average propagation rates of longitudinal seismic waves
for the a/- areas of Transcaucasia- and Caspian Basin were close to one
ai,other f...,- the same formations for the sedimentary complex - 3-6-4.8 km/soe;
the granite layer - 5.6-6.0, the basalt layer - 6.3.-6.7 and the sub-crustal
material - 7.9-8.1 km/sec. Recordings of local earth tremors were also used
in the study of the crust: there are more than ton well-ecpipped seismic
stations in Transcaucasia. Waves from these tremors show considerable diver--
sity in their apparent velocities in different directions from the epicenter:
this phenomenon is associated with the varying depths of interfaces in the
crust. The authors refer to geological data taken fromi V.V. Bolousova
(Ref. 21 Osnovnyye voprosy geotektoniki [Basic Questions of Geotectionicil.
Gosf;coltekh1zdat, 1954), P.D. Gamkrelidze (Ref. 4: Stroyeniye Adzharo-
Trialetzkoy kladchatoy sintemy LStructuro of the Adzhuro-Trialetakava
Folded Systi,'.' I'lonografiya no. 2. Tr. In-ta geol. i :ainer. All Gruz. SSR.
Tbilisi, 195 , A.I. Dzhaneli ze (Sef. 5: K probleme Gruzinskoy glyby [The
Problem of the Georgian Block]. Soo'bshch. AN'Gruz. SSR, t. III, no. 1-2,
"1'bilisi.1942) and V.P. Rengarten(Ref. 11: Geologiya SSSR [Geology of the
Card 3/4
S/630/60/000/002/006/006
The structure of the Earth's... D055/Dll4
USSR] , t. X, 1937). The thickness of the sedimentary complex along the
graVimetric profile is 8 km near Anakliya and falls to nil in the region of
the Dzirul'skiy Massif. Further to the east itincreases, reaching over 20 km
in the center of the Caspian Sea, whence it falls abruptly to 3 km and re-
nains thus until Karshi. The thickness of the granite layer varies consider-
ably - from 5 to 25 km, while that of the basalt layer remains more or loso
uniform at 25 km, though its depth from the surface varies from 12 to 25 km.
The 'Mohorovicic surface follows the ba:3alt layer fairly closely. There Is
1 czkotch map, I profile fieure and 20 Soviet references.
Card 4/4
,,BALAVADZEO D.K.; SIIENGELAYAl G.Sho
Densities of rocks on the territory of the Greater Caucasus.
Trudy Inst. geofiz.AN Gruz.SSR 221153-170 164.
(MIRA 18: 12)
s/16q/62/ooo/oo8/oi5/oqo
E202/E192
AUTHORS: Balavadze, B.K.o
-Mn-sliT ~z,
Mindeli, P.Sh.
Gabuniyal V*P*j Shengelaya, G.Sh&j
Kartvelishvili, K.M., and
TITLEi Studies oC gravitational field df the Bol'shoy Kavkaz
PERIODICAL; Heferativnyy zhurnal, Geofizikaj-no.81 1962, 2o,
abstract 8 A 134. (Geofizikis institutix shromebi.
Sakartvalos SSR %jetsniyerebita Akademia, Tr. In-ta
goofiz. AN GruzSSR, v.19, 196o, 199-216).
TEXT: Results of the studies of the Kavkazkaya gravimetri-
cheskaya ekspeditslya (Caucosian Gravimetric Expedition)*of the
Institut genfiziki AN-,Gruz.SSR (Institute 'of Geophysics of the
AS Gruz. SsR) carried out between 1955 and 1958, in the region.of
the Boltshoy Kavkazl are described. The measurements were carried
out on Norgard gravimeters. Two simultaneous observations were
taken which secured good control. Prior to the field work, the
apparatu-9 was studied and particularly careful determination of
temperature coefficients, calibration in field conditions and
determination of the stability of the rate of division, was made.
Card 1/3
Studies of gravitational field ... s/169/62/000/008/015/090
E202/E192
The survey was based on 41 supporting points which are linked
through the initial Tbilisi point with the Potsdam grid. The
results of survey (1902 points) were completed by 57 pendultim
points and 1393 points collocted by industrial organisations.
Method of survey in difficult and inaccessible mountainous regions
is described. The errors in the determination of the anomalieb are
described. It is shown that in order to increase the accuracy or
the gravity force reduction in mountainous regions, it is of greater
importance to determine more accurately the density than the
elevation or the point. The tA29 (Iluge) anomalies are istrongly
deformed by the effect or the topography and hence for all the
34oo points the effect of the topography was taken into considern-
tion within a radius of 200 km. Brunco and Zhongolovich
(iongolowicz) corrections were incorporated in the observation.-..
A brief description of the gravitational field of Caucabus in the
"free air" (Faya) reduction b1g, and local topographic "2g
(Buse) reduction is given. Simultaneously with the survey, studies
of rock densities were carried out which showed that the belt of
density changes (Increases with the Increasing age of the rock--~, and
Card 2/3
j s/169/62/000/008/015/090
studies of gravitational field ... E202/E192
the average density values tend asymptotically to a limit.
[Abstractor's notei Complete translation-I
Card 3/3
- - ---- -- -- -.-
, -- , - --- r.,- -- -,,-.-- . - -
ALUSIDZE, ~I.A.; KMELAVA, D.A.j, red.; BALAVANE, B.K., rti.
(Roductlon of the force of gravity) Reduktsila sily tia-
. zhenti. Tbilisip Metaniereba, 1965. 253 P.
WIRA 18t7)
-----T)ALAVADZ8, O.K.; HINDELI, P.Sh.
Earth's crust structure of the Black Son Basin from geophysical
evidence. Studla geophys 9 no,lt75-80 165,
. j
1. Institute of Geophysics of the Georgian Soyiet Socialist
Republic, Tbilisi, Zoji Ruchadze 1. Submitted October 19, 1963.
-"/ -~ll~J/LA.JV/UUZ/UU7~,/1Y)7Q
4
.6 20837-66
ACCEWION JNRt AP5026877 Cz1bO23165A09,10011OW510080
AUTHOR: Balalradze B. X.1 Hindells-P, Sh,
TITIXI Structure of the Urthts cruet in the Black Se/lbxaaint from geophysical
evidence
SOURGE: Studia geophysics, st geodaetierv v. 9, no, 1, 1965, 75-80
TOPIC TAGSs tectonicat geomorphology, seiwologyt earthquake
.Abstract (English articleo "thorel Russian aunu4ry]: 'The structure of the
;'Earth's cruet of the Black Sea anod the mainland surrounding it is investi-
Gated, on the basis of a quantitative interpretation or the gravity wuxulies
In the Dourguer reduction. Use is made of deep seismic soundings, geologicall
data, ani of the data cbtained from analyses of the earthT.~akae in this re-
gion as recorded by the seismic stations in the Caucasus and the Krimea, It
:is inferred from the investigation that the structure of the FArth I a crxwt
I , hfts 1 figti" and
under the Mack Sea is of the. intermediate type.! Orig. airt
3 graphe
Acad, Sci. QroKaftan SSRjk Thili8l
ASSOCLATIONI G"
SUBMITTEN l9Oct63 ENCLI 00 SUB 0ODE1 ES
NO RU SOVI 017 OTHERI 004
vmb
Card 1A
BALAVADZE, H.K.; MINDELIP P,Sh,
Crustal strueture of the Black Sea basin based or. geophysical
data. Salem. Isal. no.6166-76 165. (MA 1819)
L Z16W EWT(1) GW
-C6DEj-Wj0Mj65j000 017, OM
ACC NNI Alujoh-321
AUTHOM 00 Sh, 41
ORO# Institute of Geophysics AN GrueSSR (Institut goofisiki AN Gru&SSR)
TITIEs Gravimtrioxvin"etigation of the struaturo'of the earth's crust along the
profile LWiiikkifiki-Aizur-Stspnoy (Caucasus)
SOURCKt Sovetskaya geologiya, no, 12, 1965, 93-99
TOPIC TAGSt Earth crust. Earth gravity. oeiomlogy, petrology
APSTRAM We paper gives the results of a quantitative interpretation d"
gravimetric data obtained along a seismic profile in the Caucasus; the
work was done by the InAitute of Geophysics of the Goorgio Acada
,--,.Sciences. Fig. I is a croon seat, an of cruotal structure in the invest-4
ig"ai-o'd -area. Full information is given on seismic and gravimotric in-
voutigationo And geological studies made in this area,, as well &a an
interpretation of gravity anomalies. Tho depth of the eurface of the
,"basalt'$ layer along the profile varies from 25 to 35 W. 'Dlie surface
--l-a-at a great depth under the Akhalkalakokoys Plateau and the Greater,
Caucasus-and is -most uplifted under the Kura depression and loe&14-
elesAoroo Th* liurAce -of Ahe suboruots.1 eubstrate for the most par.
L 27609-166
A E-C-N R,
duplicates the config4ratio~ ~f th6 surface' of t~he "basalt" layer andl
its depth varies from 45 to 55 km. Its mdmum depth is below the
'Greater Caucasus and the Akhalkalakokoye Plateau and the increase of
!the thlokness of the earth's crust in these areas is accou4to-for
'primarily by an increase of the "granitell.LVere Origs art* hast 2 figures,
S68 CWSt 08 SUBM DAM Pone ORIO REFs 024
N' R T_ 6
-3165/0001006/0066100-7
com uR1J10
AUTHORS -AAIAV&414 K,j Hinds.1i, Ps Sho
ORCt none
TITLEs Structure of the earth's crust'in the Black Sea basin accordin
to geophysical data
SOURCE: AN SSSR. Hathduvedomstvennyy geofizichookiy komitat. Saysmi
cheskiya iseledovaniyal no. 60 1965, 66-76
TOPIC TACSt structural geology, earth crust, ____V
seismology, deep seismic sounding. oceanic crustal structure,----'---
**eveadqk, Hoho,,,discontinuity
K4,
ABSTRACT: The structure of the earth's crust in the Black Sea and the
Sea of Azov basins is analyzed on the basis of: a) quantitative inter-I
pretAtion of the regional gravity field (Bouguer reduction) and mag-
netic anontallexib) records of the Caucasian anti Crimean seismic sta-
tions on the propagation of the first arrivals of LR anti R,,short-
period surface waves traversing tits bne1n; and c) records first
arrivals of P and S vaves from near earthqunkcs durina the period
1955-1960. In addition, those deep _a- ei-amic' -a'oundinal"data which are
available for tits northern half of the Goa as well an geological
LC;prd3
ACC NR! A76010299
evidence and density data for the adjacent areas to the north and south
are utilized. The Black Sea Basin gravity anomaly Is positivel over
the doop-vater portion it is a latitu4inally-elongated, large regional
maximum, which rather regularly decre4sea toward the const; in the
littoral zone it becomes negative, with larRer negative values in the
Caucasuso Mountainous Crime& and the northern port of the coastline
Are exceptions, showing high positive values which decrease toward the
north# Records of elastic waves Renerated by earthquakes recorded at
the Tbilisi, Sochi, Simferopol', and Yalta Stations were utilized to
determine, from the S-P travel-time curves, the structure of the
earth's crust at eight points around the Black Sea and one point in
the sea. The crustal thickness under the continent varied from 43 to
49 km, with the sedimentaryo granitic, and basaltic layers amounting
to 8, 18, and 23 km, respectively. Under the sea southwest of
Sevastopol the crustal thickness reached 33 km. The granitic layer
In the Black Sea Basin, determined from L, :nd R. short-period wave
records, has been found to thin out towar he central part of the
sea and to either absent in the deep-sea portion (h ;, 200 km) or in too
thin to be detected by this method# The depth of the Mohorovicic
discontinuity in this region varies from 22 to 23 km In the central
part of the sea and from 35 to 43 ke in the coastal areas. The
presence of a thick layer of sediments In the crust under the basin
Card 2 / 3
010299
appears to support the thesis that ito structure to continental, but
the lack of a granitic layer suggesto t1int it in of the oceanic typete
The authors think that the structure to intermediate, and chnrac-
teristic of inland and marginal seas. Orig. art. lines 3 figure.$,,,)
SUB COM 08/ SUBM DATE: none/ oRic Rut 0251 OTH REN 004
3/3 b I
A','o 0" j 21
Ut)()/~- 0j~,/000/0U17/0A
ACC N:%L 1661 :MURG)", c0i,A..
AU7 HOR 11. Sli.
ORG: none
T ITLE: Mlain results of geophysical inveatigations of the structure OC
the Earth's crust in the Black Sea basin
SOURCL; Ali SSSR. %,',ezhduvodomstvannyy goofizichoakiy komitet,
Stroyaniya Charnomorskoy vpadiny (Structure of the Black Sea depres-
auka, 1966 1T-21
sion); abornik utatcy. Moscow,, Izd-vo N
TOPIC TAGS: carth crust, Mohorovic'A.0
d.,',.scont Inta i t y J
~ABSTRACT: A short Gummary is preoented of the main rdsults of
I
igravir.atrIc investigations of the Earth's crust under the Black Sea
band -he Saa, of Azov as well an adjacent area* along tan profiles, It
~was ~etcrmined that the results of a quantitative interpretaition of
30." cono
1'..4,4-XvIty anornalie:; aro in ar,.
z;eiamaic zoundinp; which indicate that Ll'-.o 't;nlcicnuz;!; of tiit;
cover increases from 5-3 ku, in the coautal regionz; to. 13-15 '4.1
:toward the deep part of the Black Sea basin, 'A"he 10-11-kr. Uiick
/ 2'
LCRrd
~_ACC' NRt j%-. 6034361
sodimantary complex in the southern part, of the Sea of Azov decreases
gradually toward the north, pinchinr, out at the northoen shore. 'A.'h a
granitic layer has a thickness of 10-2.5 km in the coastal areas of
!the black Sea, but decreases evenly, finally pinching out near the
ideep-watc.- part of the basin. The 20-23-kn thick basaltic layer in
.the coastal regions or the Black Soa decreasea to a thickness of
17-9 km at the center of the western part of the sea and to a thicXnesal
lof 10-14 km at the center of the eastern part. Under.'the Sea oA^ Azov, If
ithe surface of the basaltic layer is approximately parzillel to the Moho
f
idiscontinuity. interpretation of the Ar, curvea indicate3 that the
Earth's crust is 22-25-kn, thick in the central part of the sea and
35-115-1m, thick at the shores, 'A"he geophysical data indicate that the
n-
,Earth's crust under the Black Sea is intermediate between the co
itinental and oceanic crustal typea, while the cru3t under the Sea of i
~Azov is of the continental type. Two oil' the three figure3 in the
lartic1c Ghow the depth of the M.OhO discontinuity in the Black Sea
,rc(;ion, as determined by two different methods. OriG.*.art. has: 3
figures.
SUB CODE: 08/ SUBM DATE: 044,,,ay66/ ORIG RLF: 013/
ACC NRt AT6034511 SOURCE CODE: UR/0000/66/000/000/0125/0134
AUTHOR: Bulavadze, B. K.
ORG: none
i TITLE: Geophysical investigation of the structure of the Earth's crust in the Black
It Sea basin
SOURCE: AN SSSR. Otdeleniye nauk o Zemle. Nauchnyy sovet po komplekanym
issledovaniyam zemnoy kory I verkhney mantii. Glubinnoye stroyeniye Kavkaza
(Abyssal structure of the Caucasus). Moscow, Izd-vo Nauka, 1966, 125-134
TOPIC TAGS., Hohorovicic discontinuity, earth crustf gpqItic layer, basaltic layer
sedimentary complex# earth gravity / Z7100AV ~,~ ~q
ABSTRACT: The thickness of the Earth's crust and granitic and basaltic layers in
the Black Sea basin were determined from the Bouguer gravity anomaly, seismic data#
rock densities, and geologic data. The thickness of the sedimentary complex Is
shown to increase from 7-8 km along the coast of the Black Sea to.15 km in the
deep-vater region. The thickness of the granitic and basaltic layers in the
coastal and deep-water are" 45-20 and 20-23 ka, respectively) decreases toward
the deeper part of the sea. The granitic layer wedges out at the 2000 mm isobath.
The basaltic layer is 7-9-ka thick in the west-central part of the sea; it is
10-14-km thick In the east-central part of the sea. The thickness of the crust
v&rIes.from 22-25 km at the center of the sea to 35-43 km in the neighboring aress.
AT6034511
II.Giavimetric data indicate the possibility of a systm of subcrustal faults
Orig,
hast 6 figures and I table, IWA-794)
SUB COM 08/ SUBM DAM 26Feb66/ ORIG REF3 016/ OTH Rat 004/
25(7) BOV/117-59-7-18/28
AUTHORS: Balatz, D.S,,,,,_Grebennik, I.I., Kuzomkin, V.I.
TITLE: A Machine for Bending Cramps
PERIODICAL: Mashinostroitell, 1959, Nr 7, p 34 (USSR)
ABS"I.IRACT: At the Rutkhonkovskiy mashinostroitellnyy zavod gorno-
shakhtnogi) oborudovaniya (Rutchankovo Machine Build-
ing Plant tor Mining Equipment) the bending of rect-
angular and trapeziform cramps was conducted in dies
on frictional presses. The maximum output of one
press was 3,000 to 3,200 cramps per shift. On the
suggestion of inventor V.I. Kuzemkin, a machine was
designed and built for the bending of rectangular
and trapeziform cramps out of blanks, 16, 20 and
24 mm in diameter. It consists of a cam disk with
eight grooves on its 6ircumference, a gear reducer
and drive, a bending-calibrating device, a store-
box for blanks, an inclined tray and a discharging
shoot. This bending machine has been in service for
over a year and produces 30,000 cramps por shift.
Card 1/1 There is I photograph.
r.
A"TA
SOV/124-57-5-6091
Translation from: Referativnyy zhurnal. Mekhanika, 1957, Nr 5. p 152 (USSR)
AUTHOR: Balavadze, V. K.
TITLE: Aspects of Crack Formation in Light-weight Reinforced Concretes
(Nekotoryye voprosy treshchinoobrarovaniya v legkom zhelezo-
betone)
PERIODICAL: Soobshch. AN GruzSSR, 1956, Vol 17, Nr 4, pp 30-336
ABSTRACT- The author has worked out curves for the strain distributions (up to
failure) in light-weight reinforced concretes in axial tension and
bending, curves which indicate that considerable localized yielding
flow occurs in the vicinity of cracks. Strain gages were used to
determine the exact dimensions of the yielding-flow zone, and it was
found that the distribution of the purely plastic relative tensile
deformations v yaried along the length of the yielding-flow zone
according to a &near law. The author has ascertained a relationship
between the critical maximum cp value (encountered at the moment of
cracking at the places where cracking occurs) and the mean value
therefor computed for the entire length of the yieldin8-flow zone. In
Card I/Z the case of tensile -stressed reinforced tuffcrete girders a formula is
SOV/124-57-5-6091
Aspects of Crack Formation in Light-wei8ht Reinforced Concretes
Riven for calculating (for different reinforcement-concrete area ratios) the force
that acts at the moment of cracking upon the place where w`crack is developing.
Results are described of bending tests made on these 8irders, and formulas arc
given for calculating the crack-producing bending moments. Yu.I.Likhachev
Card Z/2
SOV,1- 124- 57-7-8393
Trtkiy3lation from: Referativnyy zhurnal. Mekhanika, 1957, Nr 7. p 142 (USSR)
AUTHOR: Balitvadzc, V. K.
TITLE: On Calculating the Bearing Capacity of Light-weight, Reinforced-con-
cretc Structures With Respect to the Development of Cracks (K vop-
rosu o nesushchey sposobnosti legkozhelezobetonnykh kcnstruktsiy po
trdshchinoobrazovaniyu)
PERIODICAL: Soobshch. AN GruzSSR, 1956. Vol 17, Nr 8, pp 717 744
ABSTRACT: In the author's opinion, it is possible to e-.-ol%c a fairly reliable
method for calculating reinforced- concrete structural members with
respect to crack formation by ia~ing !nto account file ultimate tensile
elongation 4- ult. jells. of the concrete, On the basis of experiments
conducted with a light-weight re'r1orced concrete the following empir-
ical formula is proposed:
ult. tells. - 1. 25 Rkl 1 5 w )10-5
wherein w -- d/ I is the rati-o of the diameter of the reintorcing rods
to the length of the clearance distance separating them and R is the
grade number of the concrete. The author recommends the manuiac,
Card I/Z lure of re info rced- concrete members of a two-layer sandwich type. a
S011/124 - 57 - 7-839 3
On Calculating the Bearit% Capacity of Light-wcight Reinforced-concrete (cont.)
heavy concrete to be used in that layer or portion expected to bear the compression
loads, a light concrete in the portion to be sub.)ccted to tensile stresses. In calcu-
lating such met"bers alto%vance must be made for tile limiting state of brath tile rein-
forcements and the concrete used in the tensile-stress as well as the compression-
stress zones. Bibliollraphy: 4 references.
N. 1. Bezukhov
Card 2/2
features of lightweight reinforced conorsto, loob, AX Orus.
SIR 18 no.5077-584 IV 157. (KUU 100)
1. Thilisekly nauchao-lasledovatel'skir Inst1tut sooruxXenir I gidro-
onerptiki NInisterstva slektrostantely SOMs Pft4stayloko ahleps
korrespondenton AwAsull O.D. Onlashvill.
(Reinforced aosorsts)
UUTAME, V.I.
Determining meadump tensility and the strength yield In the tension
of reinforced concrete by 7arat's method. Boob. AN Orus. SOR 19
no6'31313-320 3 'R, (MM USS)
11 ThIlleekly navahno-Iseledovatel'skiy Institut soorusheniy I
Cidroanargettki Waisterstva elaktrostantoiy SSR. Predstavlano
chlenom korrespondentom Akadeali OeNs Nukhadze,,
(Reinforced concrete) (Strouth of materials)
SOV/98-58-11-12/15
AUTHORSs Toulukidzop P.P,j Candidate of Technical Scionoes and Bala-
vadsor V*Kst Engineer
"MOWWW"MWWW"
TITLF.s On the Problem of Strength and Expansibility of Old Con-
crete Parts of Operating Hydroelectric Power Plants (K vo-
proau o prochnosti i rastyashimosti starykh botonov dey-
atvuyushchikh soorutheniy go#)
PERIODICALs Gidrotekhnichookoydetroitelletvog 1958, fir 11, PP 57-60 (USSR)
ABSTRACT% Experiments made by the authors at TIMEI hay* shown that
the strength and maximum expansibility of old concrete
from the working parts of a hydroolootrioal power plant
increase with the age of this conorete (Table on page 58).
The expansibility of the oonorete Increases in conformanos
with the following logarithnical laws
r= t , 0,69E 26 lgt
p P
Card 1/2
SOV'/98-58-11-12/15
On the Problem of Strength and Expansibility of Old Concrete Parts of'
Operating Hydroelectric Powar Planto
where t. ia the age of the concrete in days andlEp - repre-
ents a sum of 2 componentat limiting elastico-plastio
:
tretch deformation and limiting purely plastic expansibi-
lity. There are 2 tablear 2 diagrams, 2 graphs and 0 re-
ferenoes, 7 of which are Soviet and 1 American.
I. Concrete--Mechanical properties
Card 2/2
V--A------I)r-o-f.,-dokt6-r-t,-,ki~n--.n-auk, GROD
B;,NhDZFj VA., lnzh.
Mpsh-roinforced concrete AW its advantares over ordinary rein-
forced concrete. WA. i rhel.-bet. no-91389-391 S '61s
(MIRA 1010)
1. Chlen-korrespondent Akademil stroitpl'3tva I arkhitpktury S:;SR.
(Reinforced concrete)
DAIAVArjZB,,_Y J6-.-
Role of the compressed zone in the work of banding reinforced
concrete elements* Soob,,AN GruzBSR 28 no.1.65-72 Ja 162.
(IaRk 15s4)
1. Tbilisakiy nauchno.-issledsvatellakiy institut sooruzheniy i
gidroonergetiki imeni A.Minterat Tbilisi. Prodatavleno
chlonoo-korrompondentom Akademli OsDoOniashvili.
(Heinforc-ed cone re to---To stint)
BAIAVADZE, V.K.,
Experimental study of the effect of reinforcement on the properties
or tensile concrete. Soob. AN Gruz. SSR 30 no.4:447-452 Ap 163.
(MIRA 17:9)
1. Thillsokiy nauchno-iseledovatellakly institut cooruzheniy i
gidroenergetiki imeni Vintera, Predstavleno akademl.kom O.D.
Oniashvili,
- DAIAVMKAYAt T, TO
Balavenska", T. F. "Preparation of (notlakhokoy) tile from the Kudinovskly and
Pavlovo-Pasadakiy- deposit,ft Sbornik rabot po most. stroit. materialam (Upr.
I
prom-sti stroymaterialov i stroydetaley Mosgortapolkomap "Auch.-icaled. I eksporLu.
stantstya), Issue 1, 1948, p. 22-30
SOI U-32(Ao 10 APril 53 (Letopis 'Zhurnal Irykh Statey, No. 4, 1949).
P.-UAV~'l;SKAYA) T. F.
PALAWTSKAYA, T. F. "Incre.-virif, the production of dryinr, shods for dryinr, liles". 1~:Cst.
stroif. ntprialy, 1~hb, Issile 6, 1). 32-33.
50, U-30h2p 11 ti mh 1 13, (Letopis 'Flittimal ,tatey 'riykh, No. 7 1~,)M.
.-W -
---BALAVBN-,')',KAYAy T4-F.
26406 Cavoyeniye proiabodetva cherepitay na kudinovskom kirpichnom zabode.
Svornik rabot po most. Str,it. Haterialam (Upr. prom-sti stroit. F4terialov
I stroit. Detaley pri mosgoriepolkome, nauch-isaled. I zkoperim. Stantsiya)l
vyp. 2-3, 1949P a-31-46.
SOt !MOPISI NO. 35o 1949
~ - ~-- y - - - I
Hashiny Dlia Proievodstva Tonkoi Kermiki (Machinery for Fine Ceranica Production),
195 P., Moscow, 1950-
ABALTAN, No; ASATURTAN, Vol DAIATAIIo $.; OVCHrYAI;, V.
A map of corrosiveness and its use in planning protective
measures for underground metal conotrOU6nme ft-om.Arm*
4 noo,10856-99 0:161* (MRA 24111)
1. hunUld"-- &
( orrosion and anti-eorrosiveo)
FINTIR. M.: UWAI Amdow"N
wwmm~-
Studies of Cozs&Wde virus Infections In HW&ry. 1. Isolation
and Indentifteation of Coxsackie virus strains, Act& microb. hunge
2 uo.1-2ti6l-W 1954.
1. Institute of Microbiology, University Medical School# Szeged#
(COISACKIR VIRUSES
Isolation & identification of various strains)
SOV/27-58-11-19/29
AUTHOR: Physical Training Instruetor
Balayanp S.
-
TITLEt Gymnastics During Practical Training (Proizvodetvonnaya gim-
nastika)
PERIDDICALt Professionallno - tekhnichaskoys obrasovanlye, 1958, Nr llv
p 23 (USSR)
ABSTRAM In recent years, physical training of students at the Tsch~-
nical School Nr 8 In Rostov-Don has become one of the means
of turning out healthy, educated, all-round developed, young
workmen. In reviewing the students physical training for
the past year, the Pedagogical Council found it necessary
to start daily introductory gymnastics and physical train-
ing breaks when the students are In practical training. The
author describes the preparations made for these activities,
how radio communication facilities were established to carry
out gymnastics in all workshops at the saaa time and how a
team of students was formed and trained to supervise the
gymnastics in the various workshops. Representatives of
the Oblastnoye upravleniye trudovykh rezervoy (Oblast' Ad-
ministration of Labor Reserves). Oblastnoy sovet D30 "Tru-
Card 1/2 dovyye rezervy" (Oblast' Council DSO "Labor Reserves") and
Gymnastics During Practical Trainin,& SOV/27-58-11-19/29
workers, of the Methodological Section of Labor Reserves
have visited the school to become acquainted with the now
system.
ASSOCIATIONo Tekhnicheskoye uchili8hehe Nr 8 , Rostov-na--Donu "(Roatzov--aa-
Doau) Ttachnic&j School Nr 8)
1. Industrial training 2. PtWalcal fitness
Card 2/2
U14,YAN' A.M.
Forlta s otlozhenien solei pri dobyche
nefti (Preventing deposition of salts iurlng petroleum
extraction). Bakuj Aznefteizdat, 1953- 96 p.
SO: FlonthlZ Liat of i~4isaian Accessions, Vul. 7, No. 5, Augu.5t 1~!-L
-WWAv- ---- -- - - - ---
, A . .
"Combating SAlf Nposition in Pipes in the Oilfields." Min. HJFher Education VSSR,
Aterbeydthrm Order of lAbor Red Bannor Industrial Inst trAni M. AT.Stbakov, Baku,
1955. (Distertation for thig Dafre6 of Candidate In Chemical Sciences)
SO: No. 22, 1955, pp 93-105
Invvstigating lyinir rinrlincV!rzi ori ths, reithodic protectlon of
St-3 carbon strel. in ack-tilc ),(,Jd. Izv. AN Am. SSR. Ser. tekh.
nauk 18 no.3t5g-63 165. (YIRA 18r8)
1. Kirovitkannkly I proyektnyy !nst!ttit
M!m.li Sivetit khozytip3tva ArrWansl,ov
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"Fomation of sulfidin- rcslstint pzi,~~umoncoc7l,' Zhu. 1947.
L ~
Central 1nst., Epide.-,jol. & jjcj-oi)jol. .,Qscc),,:,
UJ-,.,'AWjcjw - 7n-Loonit.0 T?*rary MAIN a
lialladne - jarmdunlast wxl 3ul-far'llarjae Derivutivas
ImLinuon O:r %Umwe4w for Tftatim pbraw" in culdren wd a 2~-tlvm
Answe of Its A*Uonp* R, I* Owburgl, E. M. Kravotas, L. n. haayw4 wd 4". Lo
Froyd# last of redistrlco# Aomd Mod &A US"-'!At 3 pp
speastrips go 4
vssm4bse trtatmnt or oo chiwen vith ouiranaw4w. Diewsma Ito effsouvemes.
PA 23/4,9170
,"I
waiclM Resistawe to Sulfa XW/AVr 51
Drugs
tion by Pneumococci of Acquired Resistance to
Drugs,- L. B. Balayan, Dept of Prophylaxis Of
en's Diseases, inst zpidemiol &n& Hierobiol
x. F. Gum I eya, Acad Ned Se i USSR
No 2, p 66
Str&4_ns of pna=ococci adapted to sulfapyridine
sodium (I) remained resistant to it during 2 yr of
reTeated. passages through nice, cultivation in ritrOP
azA storage in refrigerator. Such strains vere
amevb&t less resistant to methyl-sulfathiLzole
1
Medicine Resista=e to Sulfa Xar/Ayr 51,
Drugs (Contd)
sodium (31),and sulfadiazine sodium (III), vhich
~beve stronger bacteriostatic effect than I. n and.
mcan conseqrweently be used for treating Infecticne
~: with strains adapted, to 1.
--Arm
PATLOT, P. DAUTAN. L.
Result of InRunization against diphtheria and scarlet favor with
an associated preparation. Zhur.ulkroblol.aqU. i ionun. m.9t
10-14 S 155. (KLRA 8: 11)
1. Is Institute,,opidentologii I nikrobiologit lueni N*Y.Gmalei,
A14M SSSR (dir.prof. G.T.Tygodchikov)
(VACCINE AND VACCINATION,
diphtheria-scarlet vaccines, results)
(DIPHTMtk., prevention mA control,
Taco, diphtheria-scarlet favor tozolds, results)
(SCARLM Ri", prevention and control,
vace.,diphtberim.-ocarlet fever toxolds,results)
HASATAN. L.B.
Producing scarlet favor toxin in cellophane hags. Zhur.
mikroblol. opId. I Immun. no.llt83-86 N 155. (KIRA 9:1)
1 1. Is Instituta spidesiologii I mikrobiologit imoni N.P.
Y.r. Gamalen AMN SSSR (dir.-prof. O.V.Vygodchikov)
(STRE-MCOCCUS,
scarlatina". toxin, presery. In cellophane bags)
MIAMI -L.- B.
"Kxperimental Production of Scarlet Fever Toxins in Cellophane Bags."
Proceedings of Inst. Epidem and Microbiol im. Gamsleys 1954-56.
List of Works Sponsored by the Institute (Authors are not identified
with any specific division, laboratory, or other organizational component
of the institute.) Inst. Epidem and Microbiol Im.. Gamaleys AM USSR.
SO-. Sum 1186, 11 Jon 57.
BAIAYAN L. B.
Production of xnatural high-qua3Aty serum against diphtheria*
Zhur.mikrobiol, spid, i Jamme 32 no.023-28 Ap 161. (MIRA 14:6)
1. Is Institute 9 idemiologil i mikrobiologil Imeni Gamalei AMN SSSH,
(DIPUTM) (SERUM)
HOROZOVV H.A.I_BALATANp L.D.; KULIKOVA, M.F.
Stability of dry omllpox yaccillos treat"d with penidllln,
Zhur. mikrobiol., spid. i i-in. 40 no.6;105-108 Je 163,
(MIRA VtO
1. It Institute epidemiologii-imikroblologil Impni Gmmlei
AMN SSSR.
BALAYAN L.B.- AKAITU A K
I ---, -1-1 4--'. 1 p . .
Phagotyping of staphylococcl Jsolatc..-(l Jn prvtlftArjc. In!"titutions.
.L
Zhur. mikrnblol., upid. i innun. 42 no.6t86-91 165.
OXTKA Igs9)
1. 1rizititut epidomiologil I mikrobloloi-,11 Imeril ').F.
PIN 5,l,.SR .
AID P - 1341
Subject USSR/Chemistry
Card 1/1 Pub. 78 - 4/3o
Author Balayan, L. 1.
Title t Dehydration of clay solutions treated by
chemical reagents
Periodical : Neft. khoz., V. 32, #12, 13-14, D 1954
Abstract The dehydration of clay solutions as a factor
affecting the soaked state and swelling of clay
and consequently the collapse of the walls of the
well Is studied. Various reagents are recommended
for control of dehydration.
Institution% None
Submitted ; No date
-- - --- -- - -- - -- -- - ---- - - -- - -- -- - - --- - -
ZAGARMISTRO O.S.-, . a
I
Yield tests of the *PLO sulfurised phenol as a viscosity reducer
of heavy drilling fluids. Aserb.neft.khos. 35 no-5:18-2D My 136.
(MLRA 9:10)
(Oil well drilling fluids) (Phenol*)
FRIDMAN, I.D.; BAIATAN, L.I.; SHCHrrKIRA, Te.D.
..........
Production and use of humdo povdars. Aserb. nefte khos, 38 no*8:
18-21 Ag .159 MRA 13t2)
Chemical tests and reagent@)
iOil well drilling fluids)
RUSWI[VILI, I.L. (Tolavi)l GOGUADZE, M.N. (Telavi); 1UIMALADZE, L.71.
(Telayi); DERYABIN, V.I., nauchnyy sotrudnik;
nauchny,y sotrudnik
Testing preparations against the spider mite* Zaahch.raot.ot
vredsi bole 7 no*506 Hy 1629 (MIU 15:11)
1. "arnarkandakaya sel'skokboxyaystvennaya opytnaya at&ntaiya (for
Deryabin, Balayan).
(Red spider--Extermination)
GOLOVANOVA, E.N., k"d.blolog.smuk; DANILOV, %1.; FITERSKAYA, A.M.1
M'RTA]31,Nl V#I,, nnuchnvy motrvadnl(k; BALAYAN, L,N., naue.-hW sotrudnik;
BURDA, Yu.N., nauchnyy sotrudnik
Controlling sparrows. Zashch, rRst. ot vred. i bol. 8 no.9s
19-20 S 163, - (MIRA 16tio)
1. Samarkandskaya oblnatnaya sallskokhozyaystvennaya opytnaya
stantsiya (for DeryabIn, Balayan, Burda).
Use of the precipitation reaction in poliomyelitis. Report No,2s
Study of the serum of immAzed laboratory animals in the precipita-
tion, neutralization and complement fixation reactions Vop.virus,
6 no.4t435-"O J1-Ag 161. jHIRA 14oll)
1, Laboratoriya Wwnologii Instituta po isuchenlyu pollomyelita
MIN SSSR, Moskva. (POLIONYLLITIS) (SERMO
N..-M.S.t BELULVAp A.P.1 SEIBIL, V.B.
Use of the procipitin test in the diagnosis of infootions caWpd by
ECHO and Ccxaackie viruses. Aotavirol. 7 no.3t241-249 My 16).
1. Institute of Poltomyslitio and Viral Encephalitidoe, U.S.S.R.
Aoademyof Modio&1 Solenoes, Mosoov.
(ECHO VIRUSES) (EHTFMVIRUS INFECTIONS) (DIAGNOSIS)
. (COXSACM VIRUS INFECTIONS) (PAECIPITIN TESTS)