SCIENTIFIC ABSTRACT MOSEVINA, R. I. - MOSKVITIN, A. I.
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CIA-RDP86-00513R001135410002-4
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S
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100
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December 31, 1967
Content Type:
SCIENTIFIC ABSTRACT
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CHMINNORDIK, P.M.; VISHNNIK, B.Z.; VOLKOTA, A.G.; KOMINA, R.I.;
KUGARO, TU.V.; BAVALISKATA, N.M.
Clinical treatment with proserine of chronic diseases of the ner-
vous system. Nevropat.polkhlat., Moskva 20 no.1:68-70 Jan-Yeb 51.
(CLML 20:6)
1. Of the Nerve Division of the Hospital for Chronic Cases imeni
Karl Marks (in consultation with S.S.Davidenkova, Active Member of
the AcadeV of Medical Sciencos USSR).
l!',---jACHEVl'I:KA7f I'll, "' N. ; AGFYEV, N.V. , red.; ;(.Ya. , red.
(Cons titutloaal diagram of 7.!~t~pilic svs,.ems published
in 1962] Diagra=y sostoianiia metalill-cheskilkh sistem,
opub.likovannye v 1962 godu. Moskva, Frolzvodstvermc-
izdat. kombina VINITI. No.8. 1"Ifu- ~31 F-"
! 1-. -0
ALISOVA., S.P.;KOLES141KOVA, T.P.; MARKOVICH, K.P.; FETROVA, L.A.; ROGACHLV-
SKAYA, Z,M,; AGEYEV, Me. red.; MOSKVINA,. R.Ya.,, red.; MUKHA, S.Ya."
tekhn. red.
(Conatitutionql diagrams of metal systems published in 19581 Diagrammy
sostoianiia metallicheskikh sistem,, opublikovanrqe v 1958 odu. Pad
ized. 11N.Ageyeva. Mosk7ap No.4. 1961. 402 p. 11MA 14:12)
(Phase rule and equilibrium)
ROGACHEVSKAYA, Z.M.; AGEYEV, N.V., red.; !~~S~VINA
,R.Ya., red.;
SAMYLINA, S.I,, tekhn. red.
[Constitutional diagram of metal systems, published in 1960
(no.6)]Diagrammy sostolanita metallicheskikh sistem, opubli-
kovannye v 1960 godu (vypusk 6) (By] Z.M.Rogachevskala. Pod
red. N.V.Ageeva. Moskva, Proizvodstvenno-izdatellskii kombinat
VINITI, 1962. 173 P. (MIRA 16-2)
(Phase rule and equilibrium) (Metallography)
ROGACHEVSKAYA, Z.M.; AGEYEVA, V.V., red.; MOMMA, R.Ya., red.;
STEPANYUK, A.A., tekhn. red.
(Constitutional diagrams of metal systeris published in
1961 (no.7)] DiagrnnW sostoianiia metallicheskikh sistemp
opublikovanrle v 1961 godu (Vypusk 7) [By] Z.F.Ftogachevskaia.
Pod red. II.V.Ageeva. Moskva, Proizvodstvenno-izdatellskii
kombinat VINITI, 1963. 262 p. (MIRA 1?:l)
(Alloys--4letallograpby)
(Phase rule and equilibrium)
EXCERPTA MIDICA See 17 1101 5/3 Publiz Health Var 59
1029. STUDY OF ULTRAVIOLET RADIATION OF THE SUN AND SKY 11%
KAZAN (Russian text) Mos kv ina T.N. - SBORN.NAUCH. RAP. KAZ.
GOS. MED. INST. 1957 1 1 - I I q
A st,idy of 'he dynamics of the intensity of ultraviolet radiation from sun and sky
was carried out by the photochemical method, with use of oxalate techniques in the
modification of A. N. Boiko and Z. N. Kulichkova. It wa a begun in the spring of 1950.
It was found that in spring, summer and autumn, even under unfavourable meteoro -
logical conditions, the amount of ultraviolet radiation is sufficient for coverage of
the Wological requirements of the body. To satisfy the needs of the body (in child-
ren), it is necessary to remain outdoors in the open air (on unshaded dites) for
45-90 min. an a sunny day or for 3-5 hr. when the sky is overcast. In the winter
season, the biologically active radiation is insufficient, Ind in addition to exposure
do
In the open air, children should receive vit. D or ultraviolet ray treatment from
artificial sources. The dispersed radiation from the blue sky constitutes move
than 501. of the total biologically active rays of the total stream derived from sun
and sky. (S)
TOLEDVA. To' R.v WSIVINA. T.N., KELINIKMA, N.A., BEUGOVSKAYA, Z-G-
ProbLw of organizing an effective diet* Toppit. I no;501-83
5-0 958 TKIDU 11:20)
I& Xx kafedry giglyeny pitaniya (sav. - dots. A*N. Tvzmov) laxanakogo
neditsinakago Inotituta;
(DIM 0balanced diet arrangement Mus))
MOSKVINA V. S. Cand Med Sit -- (dies) "The drop method of examimtion of the
humor of camera oculi anterior in cases of the presence of metal fragments in the
eye." Voronezh, 1956. 9 pp (Voronezh State Mad In8t), 200 ool)ies (KL, 3-58, 99)
-52-
.-MCOUINA, V,S,, assistent
zlinicr~l observations on the use of iont9phoresis for the diagnosis
of the natl4re of meta.Uic intravcular splinters. Sbor. tin*. Kursk.
.10
goa. med. inst. no.13:54-56 158.* (MIRA 1423)
l. Iz klinJki gldtnykh bolezney (zav. - profe A.Q.Kroll) Kurskogo
gosudaratvannogo meditainakogo institutao
(ElECTROPHORESIS) (EYE-FOREIGN BODIES)
MOSKVI e.
I kand.ekonom.nauk
Statistics of the turnover of goods and production outprut.
Obahchostv.pit. no.8:40-44 Ag 162. (MHU 16:10)
KOTOM. N.H.; KCSKVINA. Ye.K.
Synthesis and polymerization of nucleo-substituted iodoetyrols. Zhur.
prikl.khim. 26 no.6:660-662 Je 153. (IG-RA 6:7)
1. Leningradekly fiziko-tekhnichookiy institut Akademii Sauk SWR.
(Styrene derivatives) (Polymers and polymerization)
BELIM, F.P.; NDSMNA, Ye.M.
Comparative study of lacticacid bacteria in the oral cavity of
healthy persons and in that of patients with dental caries. Stomato-
10911a, 38 no.4:3-7 J1-Ag 159. (MIRA 12:12)
1. Iz Imfedry mikrobiologii (zav. - prof. P.P. Belikov) *skovskogo
zed,tsinekogo atomtologichookogo instituta (dir. - dotsent G.N.
BeletskI7).
(LACTIC ACID BACTARIA) (TEMR-DISFASSS) (NDUTH--BACTARIOLOGT)
BELIKOV, P.F.; MOSKVINA, Ye.H.
Significance of the quantitative determination of lactic acid
bacteria in the saliva for the characteristics of awles formation
in, Wth. Stomatologiia 40 no.2:3-*5 Ya-,Ap 161. (MMA, .14:5)
1. Iz kafedry mikrobiologii (zav. - prof.P,F&Belikov) Moskov~kogo
xeditainskogo stamatologicheskogo instituta (direktor - dotqent G.N.
Beletakiy), (TEETH-DISEA-SP11) (LACTIC ACID BACTERIA)
ADROVA, N.A.; KOTON, M.H.; HOSKVINA,le.m,
Synth4in and ploymerAzation-af amw new derivatived'at biphanyl.
Izv, SSSR.Otd.kbim.nauk Ab'A011804-1807 0 162. (KIM 15:10)
lo Institut vyaokomolekulyarmykh soyedineniy AN SSSR.
(Butadiene) (Polymer~xation)
MOSKVINA, Ye.M.; BUBYAKINA, M.S.
Effect of parotin on the quantity of lactic acid bacteria in the
saliva of white rats. Toor. i prak.stom. no.6t64-67 163.
(141 RA 18 3)
1. Iz kafedry mikrobiologii (zav. - dotrent L.N.Rebreyeva) i kafedry
patologicheskoy fiziologii (zav. - prof. II.A.Fedorov) Moskovskogo
meditsinskogo stomatologicheskogo instituta.
A D ROV A, -'1.A.; KO',"Or:,
CyTit,he ri !, of !~-w aromri r~ m*. based on
3,3:4t41 d phenyltetracarboxy, ii act'-~ Dot-,
AN if"'Sft 265 no.5:2069-1010 D 165. (IM, 1 ~i A
1. Lnstitlut vysokomolf-Li '~.7~.r!!ykh soyedironly AN
2. ChIt,n--j:nr;,es-,,o-idcy-,t A?,I Ic.. ~R (for Koton). Sibmi'~,,Pd
April 14, 1~465.
MOSKVINA9 YE. -10
MBr., Leningrad Pbysico-Technical Inst., Dept Pbysico-Math Scl., Acmd. Aci.,
-cl949-c5O-.
"Reactions of Met&Uo-orgainc C=puunds with Phenols, " Zhur. Obahch. Xhim., 19, No. 91,
1949; "Reactions -of Organio-Metallic CompauDds with Thipphevols," ibid., 20, No. 1-1, 1950.
YE. T- . YA 17CT-217
-- --ri< %4*b=m
I)A .111 1- I
~ 11 i*ftd- 4. ' We 0 PC." .1 -j
7 '-117
-deficud" od tMeAU401"k campomads W(m UL*Ikquqlo
U. M. Raton., H. P lifoahvilm and F. 8, FuWmAl;
J. G.. Ckw. t5M* i.-t'W*lVWXHugI. trmdA-
\' time).-lim C-A - 43. r4sk. It L. %I
ft"Im" M g, Rw and A a. Fe, Failkewed ler 3 hm &I
his I(l+4% thb ON MI I dow by Im"NOW.
MA 3W-W fA 110 ter Im Md by Immucte -
bab 3!w" wkb ail i. iR1fzCwIz.,
d m Ed. prom 4 misid - , Am"
0
two (34 a.) bessud 3
a. ca" sod 0 4woorm with Ollow disco.
bi 3111-M,.,280 1 AM.
11,13*4 1-trapIM72 =&ad. b, 67. v
3.-7 4E
#461wa-~. be V 's
L Sw&*. t"=" J1A* After-
00 a- #4 loss an a woo bath 6 Imn.
mL bwftOli and IN) ml. told, MOCIIWA im
WHO wilb dim". of ittemevct) CA%T 7.3 5% q4tevi,
aseffykakoW. b. 144 3% VirldfUs an JfZy=fAtkPn 4%fl
_00. IA. 1412'. 4111' 1 -MA111 I'tw
AIA 47.3% P-SfvmvtUfY
had "vw M #46pmmapew, it. Vm'. b. ICU 4'.
d:* 1=11. (am #*Sxw~smoim 6(4, 0. Z12 14* WKI
Omg [(Wt g, V%%'II S4 he* with 2M S. Av~O said 1110 g
MCI,. PUMFIGS 114(0 644 19,41, MQUIUS'N With AMA14.
filtecing. whug (for 1*4. 1 1w. Willi C"Ka. HO. mutrA14.
ing. steltm4fift. the midad amt eatz the gvoi&w
With Htc) gave 16 a. mt, IM W (fimn
110). wbkh. diasodswidim 110)6 andavitten -4-% a mist
of Vj. ki&w. and pmd. Ca in RIO Vic 48% d-
75%
M. 3W-W. Which an
i K112be In the pmew of it ve 40%
p4akay"w. own. 440-V MOM G. M. K
((Acad. Sd. V.S.S.R:-.V~
k". Chem.) to. ING-WHA51).-
the k&kjgc"4tr4 slygetwo tworgm" (*we IAVWIY limit
tynve il~cw, witts the 0-knocis p(Ayttmid"s
hm the p4saastn, FoOver ta.pts. =1=11-11
t
he I jr: jv-P 97-104' all M-40' P-0 123-M..
M P-fiv IW634. t44& I-,O-fv;- rM Adiva-
lion tuctsy of pudytarcUAtion of the p-ITr daiv. L,,
13,W Cal-Imak. lust of Ow P-Woo d"iv. 6 14.fw Cal
mok- (d. styfvae. 23.700 caf.lavk). G. M Koqof;ikmA
UMM/Citemistry - Chlorostyrenes Nay 52'
"Paymerization or styrene Derivatives with salogen
Substituents in the Nucleus. II, Polymerization of
Dichlorostyrenes,!". M. M. Kbton,~'-Te. P. Maskvina,
F. S. FlorinskiyAeningrad Physicotech Inst, Acad
Sci USSR
Zbur Obshch Khim, Vol 22, No 5, PP 789-792
The process of polymerization of 2,5-., 2,4-p and
3s4-dichlorostyrene at 75, 100, and 1250 vithout
catalyst was investigated. Introduction of 2 C1
atms into the benzene ring of styrene considerably
25ft16
Increases the rate of polymerization. The highest
r#te of polymerization was observed vith 2,5-di-
chlorostyrenev the.lovest'vith 3;4-dichlokostyriene.
Introduction of C1 aUns-into.1he benzene ring
lowert the energy of activation of the p.3lymerization
process.
K v 1 16
T%j.29LZMIdA&jj=Gf dSeg ti at I'& .falrabild-
T
tull'a IV , "
'3~ na, and F. S,
ChF..,rIcal Abst. L(Lenl', rat ns CROW
. 2 ~ ' #
V .6 tran. a Intl). See CA. 47'
/43 No- 5 ~.nj_j
3253e. If. L
10, 1954
llaullatry
USSR/Chesistry - Polywrization Jun 53
"Synthesis and Polymerization of Ring-Substituted
-,Iodostyrenes," M. M. Koton and-Ife. X-.PMoskvina,
,.,-J,eningrad Physicotech Inst, Acad Sci USSR
Zhur Prik Khim, vol 26, No 6, pp 66o-662
The polymrization rate of iodostyrenes is of the
following order: ortho, > , meta > , pam From
viscosity detns, it was found that the polymrs in-
crease in mol wt as follows: meta > , ortho > ,
PeLra
257T43
AGLINTSEVP K.Ke; MOSKVINA, Ye.P.; RUSINOVA, S.A.
Measuring the activity of beta emitters by means of an
ionization chamber. Trudy inst. Kom. stand., mer i izm. prib.
no.69:42-55 '62. MRA 17:8)
1. Vaesoyuznyy nauchno-isoledovateliskiy institut metrologii
im. Mendeleyeva.
MOSVINJPi, MWLOVAq A. F.
"Some Methods Included in the Agrotechnics of Flax Fiber Under Conditions of Ch1(alov-
ski,v Rayon in Gortkovskaya Oblast." Cand Agr Sci, Gorlkiy Agricultural Inst, !-dn Jfi;~!her
E;ducation US3R, Gorlkiy, 1955. (KL, 110 17, Apr 55)
SO: Sum. No. 704, 2 Nov 55 - Survey of Scientific and Technical Dissertations Defended
at USSR Higher Educational Institutions (16).
MOSKVIKOVq V.I. (Sokolp Vologedsk"a obUst')
I--
On the motorship. Zdoravle 5 no.8:20 Ag 1599 (MIRA 13:8)
ir %
(VOLGA RIVER--TRAVEL/
MOSKVINOV, T.N.
Mlr'A%Uf4QMtWl.
A doctor's heroic deed. Worov's 2 no.4:27 Ap 056. ()MA 9:7)
(MROVO. MARION IVANOVICH)
KOSKVIKOV, V.H.
Cre9tive longevity. Zdorov's h no.4:9 Ap 158. (MIRA 11:4)
(BAISHERV. TASILII NINDLARTICH, 1862-)
14DSKyntov, V.S.
...... .--- ".,-
P.P. Leogaft in the chair. Zdorovle 5 no.12:6 D 159.
(MIRA 13:4)
(LISGAFT, PWR FRANTUVICH, 1837-1909)
U'
l7dan ('-00:
DiS3-rtation
Tn~st- r,
- MOSUITINPL. A.I.
Traces left by permsfrost wA the need for recognizing them.
Herzlotovedenie 2 no,1:3-22 04?. (MIRA n: 4)
(Frozen ground) (Glacial epoch)
- --l" , I .
11, A.
Kal ~ 11 ", 1, T rc--,v ~ ixe - Ge I ~"-Iy
I!
Vol)ga-Sheksna irfterglacia2 lakc. inEt. ,,1 ~, - I, -
r . , .. . ? ~~
11 . I.. .
Monthly List of Russian Accessi,ns -:4-C, -
, Library of Congress , SePte:~er 1"52. . '' J., r 1, .l.
- "~
Vr', (I',,' r Tr T'!
-1-1-If
.I
11 , .1,
Geology - OB Val-ley
Origin of the relief of the ObI Valley Stepnes, Izv. AN SSSR. Ser. geol. No. 2, 1952.
Monthl ruist of Russian Accessions, Library of Congress, July 1952. Unclassified.
YOSYMIN, A. 1.
Geology, Structural - Zhiguli Ilountains
Geological history of the Zhiguli Mountains, Priroda, 41, No. ?, 1957--
S Russia Accession , Ubrary of Congress, November 1952. UNCLA53IFIED.
Month L"s o
KCSKVITM, A.I.
On the possibility of using a uniform atratigraphic scale for
diagraming (biatenary deposits In western Siberia. Biul.iram.
chetv.per. no.19:7n-73 '53. (IMRA 7:11)
(Siberia. Westein-Oeology, Stratigraphic) (Geology,
Stratigraphic-Siberia, Western)
KOSXVITIN. A.I.
(Womorpholo&7 and recent earth movownts in the siddle Volga region (aathor's
sumary). Blul.NOIP. Otd.gsol. 28 no.l*.94-95 '53. (KLRA 6:11)
(Volga valley-Geology. Structural) - (Geology, Struct-wal-Volga valley)
KOSIVITIN. A.1.
Stratigraphy of Quaternary deposits end the history of stave of
the Pleistocene period in the Shwopean part of the U.S.S.R. Biul.
KOIP. Otd.pol. 29 no.2:43-56 Nr-Ap 054. (KM 7:7)
(Geology, Gtratlgraphic) (Glaclal epoch)
KOSKVITIS. A.1,
Relation between geomorphology and the present movement of the
earthle crust in the central Volga Valley. Doki.AN SSSR 95 no.
4;869-872 AP '54. MRA 7:3)
(Volga Valley--Physical geography)
(P~Ysical geography--Volga Valley)
ZUOTAW, N.A.; PIDOPLICHM, I.C.; FEDOROV, P.7,; VASILITET, T.N.; IVAROVA.
I.K.; GROKOV. 7.1.; SONDIOV. D.S.; ZHIRMUNSKIT. A.M.; PARKMIN, Tu.P.;
PLYUSNIN, I.L. XATS. Y.T&,; GRICHUX, V.P.; YXFFJWV, Yu.X.; WSXVITIN
A&Iow- LRBZ13V, V.D.; TIODOROVICH, G.I.; ZVORMN. X.V.;
V.P.; GALITSKIT, T.T.; MAKIM, P.S.; NIXIFOROVA, X.T.; GORIEYNT, D.I.;
TANSHIN, A.L.; DUMITRA , N.Y.; SHARTMM, Te.T.;
PITATCHEM, N.I.; YL3WV, X.I.; PIDOPLICM, I.G., doktor biologiche-
skikh nauk., professor.
Papers presented at the conference on the history of Qaaternary flora
and fauna In relation ro the development of Qjiateraary glaciation.
Trudy Kom.chetv.per. 12:129-189 155. (141RA 9: 4)
LGidrometaosluzhba, (for Zel*tarev)*2.Zoel9g1cheskiy institut AM USSR
(for Pideplichko).3.In3titut skeanologli AN SSSR (for Fedorov).4.3ota,-
nicheskiy institut AN SSSR (for Vasillyev).5.Komissiya pe izuchaaiyu
chatyartichnege perioda, AN SSSR (for Ivaneva).6.Inatitut geologichs-
94M nauk AN SSSR (for Gromov, Tanshin, Nikiforova. ~26~ ~.7.Kos-
kovokly goolego-rasyedochnyy institut Iment Ordzhonikidze (for Sokolov).
8.Akademiya nauk Belorusakoy SSR (for ZhIrmunskiy).9.Moskovskiy insti-
tut Inshanerov vadnogo khozyaystva (for Plyusnin).10.Geografichaskiy
fakul'tat Moskovskogo gosudarstvennogo universiteta (for Tefremov,
Parmizin).U.Moskovskiy gosudaretvannyy universitet (for Lebedev, Zvo-
rykin).12.1natitut nefti AN SSSR (for Toodoravich).13.Transproektkarlyer
Miniaterstva putay soobahchaniya (for Mikhnovich).14.VsesoyuznYy aero-
geologichaskly treat (for Galltskly)-15-Sovet Po izuchenlyu proizvo-
dital'afth ail AN SSSR (for Kakeyev). -
(Continued an next card)
ZOLOTARU, H.A. --(continued) Card 2.
16,Laboratoriya gidro-geologicheskikh problem AN SSSR (for Gorde780-
17.Institut geografii All SSSR (for Damitrashko, Grichuk).
(Palsontolog7) (Falsobotany) (Glacial epoch)
YOSMUZOV. A.T.. MIZINOT, I.T.. KOSKVITIN. A.Z., CHGOUTIVA. A.A.
Climatic conditism of Ow akchagyl stage based om now litholo-
gic&l and uterepalsobetanical Investigations In the southern
trans-Volga region. Dokl. AN SM 105 ne.1.144-146 N '55-
(am 9-- 3)
1. InstItut goologichookikh muk Akadeali nauk WS. Prodsts;v-
lea* akmAsmilcom N.M. Strakho"u.
(Volga Valley-Faloobotamy) (Palsoclimtology)
KOSUITIN, A.I.
-
The lower boundary of Pleistocene according to now data. Blul.
KOIP.Otd.gool. 31 no.2:21-36' Nr-Ap '56. (KLHA 9:8)
(Geology. Staratigraphic)
BIL I KIND, Lev Davidovich: GRUDINSKIY, Petr Grigorlyevich- KOSKY1,711-
ANT11, I.T.. redaktor: VOROMIN, K.P.,
zoHnnicnialff"Twati-tor.
Klavdli Ippolitovich Shenfor. Moskvn, Goe.energ.izd-vo, 1957.
75 P. (Detatell energeticheakoi tekhniki. Biograficheeksia
seriia, no.20) (MIRA 10:11)
(Shenfer, Klavdii Ippolitovich, 1885-194-6)
FAMOT9 Pavel Vasillyevich; Kos"TaimmAO&W Otv~t$tvamW redaktor; MOSOT.
G.11~. redaktor Isdate-17s-tva: PPBMOTA, T.A., takhmichegkiy redak-
tor.
cstratigrILAY of the qmternary deposits and the history of the
development of the Caspian Sea] Stratigraflia chetvartichnyft
otloshanil I Istorlia razvitila Kaspliskogo moria.-Mmakwa. Izd-vo
Akad. nauk SSSR. 1957. 295 P. (Akademita nauk SSSR. Geologichaskil
Lnetitut. Trudy. no.10). (KM lots)
(Camplan Sea region-Geology, Stratigraphicy
Uc,5R / Soil 3cience~ Soil Genesis and GeoGraphy.
kbs Jour: Ref Zhur-3iol., No 2, 1959, 6029.
Author :11o
Inst :Institute of Geological 3ciences, "cademy of
Sciences Ukrainian 39R.
Title :The Loess horizons and Causes of Interglacial
Soil 3urial.
Orig Pub: Tr. In-ta geol. nauk AN' U33R. 1jer. georraofol. i
chetvertichn. a,eol., 1957, vyp. 1, 125-130.
Abstract: The stratigraphic formation of buried soils in
the upper Bug, aiddle Dnepr, and lower Sula--River
districts were investigated. The causes of the
burial of' interglacial soils appeared to be the
movement of the bottom and the deoosition of
loess de;?osits in the periods of i,laciation and
Card 1/2
USSR / 3oil Science. :.,oil Grenesis and Geoprra,-)I-,y. i
Abs "Jour: Ref Zhur-Biol., No 2, 1959, 6029-
Abstract: and freezing periods. The burie,. soils divide
all basic and suppleL.-ientary strata of loess and
are eluvial earth formations. F. I. -jhcherbak.
Card ?./2
4
A;/-e- S/rv -T 7-:/:7 /V
SUBJECT: USSR/Geology
AUTHORj Moskvitin, A.I.
5-2-1/35
TITLEi Probable Age of the First Glaciation of the Russian Plain
(VeroyatnYY vozrast pervogo oledeneniya Rueskoy ravniny)
PFRIODICALs Byulleten' Moskovskogo Obahchestva Ispytateley Prirody, Otdol
Geologicheskiy 1957, # 2, PP 3-13 (USSR)
ABSTRACT% The author re-investigated the problem of the age of the firat
glaciation of the Russian Plain.
Pollen and seeds of coniferous forests were discovered in the
samples of Akchagyl clays taken from the regions along the
Volga River and the Caspian Sea.
The author found a piece of mammoth (Elephas primigenius B1.)
tooth in the Akch*gyl conglomerate near Ullyanovsk.
A moraine of the first glaciation was discovered by the author
at Solikamsk, and typical signs of sternal frost were found by
Pryakhin in the Akohagyl layers along the Belaya, River in the
Card 1/2 Tartarian ASSR.
5-2-1/35
TITLE: Probable Ige of the First Glaciation of the Russian Plain
(Veroyatnyy vozrast pervogo oledeneniya Russkoy ravniny)
The great Akchagyl transgression was accompanied by glaciation
which left specific flora, northern fauna and lithological
signs. Lithological peculiarities indicating & glaciation
consist in the following factsi traces of the crumpling of
sediments by the block ice, eternal frost, banded sediments,
layers of moraines, ate.
The age of the first Akchagyl glaciation corresponds to the
Calabrian agog and it is propoped to consider the Akchag7l
layers as pertaining to the Pl4istocene age.
The spread of this glac---ation was only slightly less than that
of the maximum Dnieper glaciation.
The article contains 2 diagrams and 1 photo.
The bibliography lists 48 Slavic references.
ASSOCIATIONt Not indicated
PRESENTED BYi '
SUBMITTEDi Report delivered on 14 May 1954 to the Moskva Conference on the
Stratigraphy of the Quaternary Period.
AVAILABLE: At the Library of Congress.
Card 2/2
SUBJECTt EUROPE/Geology
AUTHOR: Moskvitin, A.I.
TITLE: "About the Lower Boundary of Plejt3-t-:::--ar. Deposits In Europe"
(0 nizhney granitse pley3totsena v fevrope)
PERIODICAL: "Izvestiya kkademii Nauk SSSR", Seriya Geologicheskaya. 1957,
#4, pp 3-22, (USSR)
ABSTRACTs Present methods of studying glacial deposits based on pollen
of plants, seeds, micro fauna and lithologic indications enabled
to establish the traces left by glacial climates, formerly as-
sumed to belong to the Upper Pliocene period, The author is in
favor of the recommendations of the 18th Session of the Inter-
national Congress of Geology, (1948) about placing tho lower
boundary of the Pleistocene period under the mentioned deposits,
and presents a new stratographic table of the Pleisto:ene period,
which include the geologic occurances in England, the Alps, the
European part of the USSR and the USA.
Successfully conducted micro-faunal and micro-botanical analysis
yielded deposits in formerly mute glacial formations which were
earlier classified as belonging to the Tertiary period, Several
Card 1/4 reports on thin buoject, dealing with British, Dutch and Italian
TITLE t About the Lower Boundary of 7eposits in Europe
(0 nizhney granites pleystotsens vYdwrope)
territories were submitted, and regarded by the Congress as
being convincing. As a consequence, the Congress accepted the
recommendation to transfer the lower boundary of the Pleistocene
period under the deposits, which contained any characteristics
of glaciation. The Cromerian forest strata, according to old
assumptions, topping the Pliocene of eastern England, proved
to be wholly of the Quarternarypariod, with a large variety of
mammals, now extinct.
Directly above the Cromerian forest strata are located the
deposits of the Leds, myalis of the North Sea glaciation, which
is, according to C.R. Chetwin and others the first of 4 glacia-
tion periods which covered eastern and central England, The
different strata of the central, sections of England were
studied in detail by F.W. Shotton. Geologic formations in
Holland were examined by Pannekoek and van Voorthuysein, who
placed the lower layer of the Pleistocene with "cool" foraminife-
ras underneath the Amatel strata at a depth of 395 m. The
basis of the Ancient Quarternary strata in the western part of
Holland is located 400 m underneath the level of the sea.
J. Virst described the discovery of a large variety of mammals
Card 2/4 in south-eastern France near the hamlet Saint Vallier, 230 m
ix-161-1/23
TITLE: About the Lower Boundary of Plaistjceae leposits in Europe
(0 nixhney granitse pleystotsena vTG7rops)
above the Rhone river in Guenz moraines, which had perished by
sudden cold. Italy presented itself during the Calabrian epoch
an a mountatnous island, wherbby a large bay covered the Lombard
lowlands. The deposits of the mountain lakes supplied the Ita-
lian explorers with material, on the basis of which the Villa-
frank epoch was incorporated in the Pleistocene period. Cala-
b,~Ian Sea deposits near the town of Lodi (south-east of Kilano)
contained theppllen of the alder, pine and chestnut trees-
plants of a cooler climate than the pzesent, while during the
Pliocene period prevailed a climate warmer than at present.
Of interest is to note the development of the flora in northern
Italy during the Upper Pliocene period, consisting of ragweed,
cinnamon, sequoia, cypress, European plane, magnolia and nut
trees. During the following warming-up "interstage" period
developed the Pliocene forest with Greek nut trees and a large
variety of mammals. The age of the ancient Russian glaciation
period can not be established by the paleatropic method, but
the state of "petrification" of moraines indicate the primeval
age of these deposits. Judging by the burried soils, these
deposits of moraines of a maximum glaciation were interrupted
Card 3/4 by a prolonged period, consistingaE at least two interglacial
'AUTHOR: Dobrovdllskiy, V.V. 1112-12-10/12
TITLE& All-Union Interdepartmental Conference on the Study of the
Qmter,aary Period.(Vseeoyuznoye mezhduvedomatyennoyei soveshcha-
niye po izucheniyu chetvertiohnogo perioda)
PERIODICAL: Razvedka I okhrana nedr, 1957, # 12# p 58-59 (USSR)
ABSTRACTi Initiated by the Ministry of Geology and Conservation of Natural
Resources (Department of Geologo.,Oeographio Sciences of the
Academy of Sciences USSR, Committee for the Study of the q0t.
ernary Period, the Institute of Geology and "the Institute of
Geography of the Academy of Sciences USSR) a conference on the
study of the qlatorary Period was hold in Moskva In 1957-
200 lectures were held during the conference which was attended
by 500 scientists from the USSR, the Chinese Peoples' Republic,
the German Democy-atic Republic, Czechoslovakia, Hungary, Roumania,
Poland, Bulgarip. The main problems among numerous othbts'dealt
with during thc conference weres
1. Denomipation of the QLaterary Period and its lower bound-
ary.
2. 3tratiiTraphic subdivision of the rbAterary Period.
The conference was opened with lectures of V.I. Gromov, B.P.
Card 1/3 Grichuk, A.I. goskvitin, E.V. Khanteer and others which dealt
132-.12-10/12
All-Union Interdepartmental Conference on the Study of the Quaternary Period
with point 1, whereby the use of the term "anthropogen" was
favored by the majority of participants beside the old term
" Qwtervary Period". The second point was discussed in numerous
plenary and aub-committee sessions. 1.I. Krasnov (VSEGEI) claim-
ed that the present state of stuftes enabled the issue of an
outline map on deposits of the QuateraAry Period of the scale
115,000,000. Special charts of the Quaternary layars of the
aoftles 1:500,000 and 1:200pOOO and larger were developed during
the past years. Coordination of surveying work was recommended
as well as complex prospecting for the purpose to discover
specific churabtertatios of different formation@. B.A. Fedoro-
vich and others lectured on Qmternary - deposits of northern
Kazakhstan, which are of great general Importance for geomorpho-
logic mapping. E.E. Kilanovskiy lectured on volcanic ashes
f ound in layers of the Quaternary Period in southern plains of
the USSR, which are important inasmuch they are connected with
Pliocene and anthropogen voloanization of the Caucasus. N.A.
Belyayevskiy, member of the board of the Ministry of Geology
and Conservation of Natural Resources USSR pointed out gross
Card 213 omissions of former work, because basic geologic questions of
132-12-IC/12
All-Union Interdepartmental Conference on the Study of the Qmterwry Period
deposits of the Qmtermry Period were viewed by the conference
from different angles. Great interest was devoted to the study
of different angles., The lectures of S.S. Morozov and the Aca-
demiciian I.I. Gerasimov on the subject of geochemistry of Qmt-
ernary deposits were of special Interest for the national soono-
my. It was decided to hold the next regional conference for
Kazakhstan and Central Asia in 1958, for the Ural and western
Siberia in 1959, and for eastern Siberia and the Far East in
1960. The next All-Union conference on the study of the Qmt-
ernary Period will be held in 1960.
ASSOCIATIONt VIMS
AVAILABLEs Library of Congress
Card 3/3
SOV/5-58-6-6/13
AUTHOR: MoSkvitin, A.I.
TITLE: To the Question of the Age and Origin of the
Yergeni Stratum (K voprosu o vozrast,.-~ i
proiskhozhdenii Yergeninskoy tolshch!.'j.
PERIODICAL: Byulleten' MoskovskoCo obshchestva ispyta-
teley prirody, Otdel geologicheskiy, 19581
Nr 6, p 89-9? (U3SR)
ABSTRACT: The Yergeni suite is composed mainl ~ of sand-
ston.-,s 20 to 50 m thick. The suite covers
a considerable part of the Vol6a-Don water
divide and farther south is found over the
entire Yergeni plateau. The opinicns of nu-
merous geologists on th.-- age and origin of
these sandstones differ, but the author, after
comparing existing material finds -1-hat these
sandstones are coastal de--osits of the Plio-
Card 1/3 cene sea or, more precisely, of the Akchagyl
SOV/5-58-.6-6/13
To the Question of the Age and Origin of the Yer-eni Stratum
suite of the Pliocene eDoch. His findings are
confirmed by discoveries of flora and fauna of
this era and by the fact that some of the Akchagy!
layers still bear traces of cryoturbation.
The great glaciation of the Russian Pl~ateau,
according to the author, coincided in time
with the formation of the Akchagyl suite.
The following scientists are mentioned. by tile
author: I.V. Yushketov, Ye.V. Dlilanovskiy,
M.M. Zhukov, N.A. Sokolov, A.N. Mazarovich,
V.M. Kamenskiy, Yu. A. Petrokovich, D.M.
Konenkov, M.N. Grishchenko, F.P. Panteleyev,
B.P. Zhizhchenko, P.A. Nikitin, Ye. I.
Syrova, G.I. Popov, O.V. Matveyeva, L.A. Skiba,
V.P. Kolesnikov, Ye. N. Ananova, S.A. 'Takovlev,
Card 2/3 M.S. Shvetsov, N.I. Nilolayev, A.I. Pryakhin,
SOV/5-58-6-6/13
To the Question of the Age and Origin of the Yergr~:ni St:-atum
C~ - C~
V.I. Grcmov, K.V. Nikiforova Yu.M. Vas:~-l'yev,
L.I. Alekseyeva, N.A. Sigayci, A.F. Yakushev,
G.N. Rodzyanko and G.I. Goretskiy. There
are 37 Soviet references.
Card 3/3
MOSVITIK'A.
Remark on the pro-Tart& Interetadial deposits at Brzozovice
near Bedzin. In Russian. Bul Ac Pol chin 6 no.1li737-738 158.
(=Ai 9:6)
1. Prodstavleno V. Shafer.
(Polan&-- Fbyelcal geography)
tVSMTIN, A.I.
Modern concepts of the stratigraphic divIsion and duration of tfte
Pleistocene. Blul.Kom*ehetv.per. no.23-.3-16 '59. (KIRA 1'1:4)
(Geology, Stratigraphic)
_ -KOSMT11i,- A. I - --.-
Age &~A origin of Torgirl wands. Blul, NIP. Otd. 9802- 33 no.6:89-98
4%~D 159. (MU 12:A
(Russia, Southeru-Band)
MOSKVITIN, A.I.
Climatic data determining the lower stratIgraphic boundar7 of
the Pleistocene. Biul. MOIP. Otd. geol, 34 no-5tl53-154
S-0 t59. (Geolog7q Stratigraphic) (KIRA 14:6)
30~5) SOV/20- 127 -4 - 36,11,r,
AUTHOR: Moskvitin, A. I.
TITLE: Recent Data on the Most Ancient Glaciation of the Russian Plain
(Novyye svidetel'stva drevneyshego oledeneniya Russkoy ravnfny)
PERIODICAL: Doklady Akademii nauk SSSR, 1959, Vol 12"1, Nr 4, pp 852-85~,
(USSR)
ABSTRACT: The authorts assertions that In the Akchagy-1 age during the
Pliocene the climate of the Sr-3dnyeye Frovolzhlye (middle Volga
Region) (Ref 3) became cooler was considered not correct and
was objected to. Late:r on, however, -.hey -were proved over and
over again (Refs 1,4-6) on account of the lithologic investi-
gation of the sediments and the po4len contained by them
(Ref 1). This ought to be sufficient but som,; of the se--entis-5
seem not yet convinced by the evidences mentioned although T.heae
evidences are constantly proved anew by western European scur_;?,~
(Refs 7,8,10,11). The combination of palinologic and cryologic
data is the most convincing one. Although there are continial
attempts (Ye. V. Shantser) to explain the traceE if ground
movement, still to be seen on top of eternally frozen soils
Card 1/3 after thawing, by "landslides", rt-sc, tiie author wants -1o
OV' - 1. 2 7 - 4 - A '. '60
S
/2 0 0/
Recent Data on the Most Ancient- Glaciation of the Russian Plain
mention some especially striking examples of the ab~Dve pnen~,ie-
na. The attempts at the explanation mentioned are digpre7ed by
him at some other place. Figure ! shovs a disclos-1re 7 km wc-3-
of the suburbs of Rostc-,,-na.-Dcnu. The sand disclosares ment,-cn-
ed and those of the Yergeni mass al,,~ng -.he lower !bourse of
river Sal were obser-,red ther(i by a large group of experte ~:f
the Quaternary: L. 1. Aiekseyeva, Y-,;. 9. Vas"ilyev, V. T. (',--r,
mov, N. A. Lebedeva, A. 1. Musk-,rit'-n (the author', K. V. N-'x--*-
forova, N. V. Rengarien, eta "47J thq Instit-te ME,nt.o:.ed "h,
A3sociation)3 N. A. Sigayev, A. F. Yakuaheva (Mo!ikovskiy
veraitet (Most-ow TJniversity)); G. 1. Popo--ir and G., N. R,,-dzyar-'-.--
(Azov sko -Chernomorsk oye geolugicheskoye uprarleri..ye ~'Azl- ,V
Black Sea Administration)). The two place3 marti~n,-,d are
high above sea level so that traces ~f -ontlnuous grGund fio3t
may be considered proofs of simultaneous -axtPnai,,e glaciaticn
of the Russian Platform and the Caucasian Mn--in-.ains. The -;)m-
parisons indicating ground froat in the parts of Germany and
Hulland near the river Rhine during the Akcha-gy" period may
seem too bold and arbitrary (Refs 7;8) buz the existeno-e of a
glacial olimate has continuously been pro-,red by sediments wh-.-n
Card 2/3 had previously been considered Plio-cere. There are 3 figUrtli
SOV/20-1271-4-516/60
Recent Data on the Most Ancient Glaciation of the Russian Plain
and 10 references, 6 of which are Soviet.
ASSOCIATION: Geologicheskiy institut Akademii nauk SSSR (Geological In-
stitute of the Academy of Sciences, USSR)
PRESENTED: Idarch 24, 1959, by N. M. Strakhov, Academician
SUBMITTED: March 24, 1959
Card 3/3
MOSIVITIN, A.I.
Third terrace averithe floadlands of the central Volga WALLey.
Isv. vys. ucheb. zai.; geol. i razv. 3 no-7:135-136 ii 060.
1. Institut geologi~hesktkh nauk AW SSSR.
(Volga Valley-Gooloa, Structural)
MOSKVITIN, A.I.; RASSULOV, A.M.
Use of models In the experimental study of direct hydrogen cooling
of turbogenerator rotor windings. Elektrosila no.19:19-25 '60.
(MIRA 15:2)
(Turbogenerators--Cooling)
KOSLVIT A 1.
- u - -
-- ---;, -, Mf~ -. !~. -
Representing quaternary sedizents of Western Siberia on ageneral
stratlgraphic scale. Trudy GIN no.26:11-36 960e (MIHA 13:12)
Sxoaria, Western--4eolog7, Stratigraphic)
KOSUITIM, A. I.
Data on climatic factors determInIng the lower stratigraphJc
boundary of the Plelstocenoo izv. AN SSSR. Bar* goal. 23 no.2:39~-
55 1 060e (MIRA 13..10)
1. Geologicheekly Institut AN SSSR, Ifoakwa.
(Geology, Stratigraphic)
MATVEMA, O.V.; IS
Age and conditions of the formation of the first upper flood
terrace of the Tana River near Taltunovo in Rya-zan Province.
Mule Kwo chetva pore noe24:56-65 16o, (MIRA 16:7)
(Tana Valley~Terraces (Geology))
GOW2391Y.G.I., otv.red.; ITAXOTA, I.K., otv. red.;,_M~OSUIT~TINA~_I..
otv. red.; EUMITRASHKO. N.Y.. red.; ZUBKOTICH. H.Ys.. red.;
XAF41111A, T.Yu.. red. izd-va; LAUT, Y.G., tekhn.red.
[Materials from the All-Union Interdepartmental Conference on
tha Study of the quaternary Period] Katerialy Tsesolusnogo
mexhdavedostatwennogo moveshchaniia po tanchaniiu chetvertich-
nego periods. Moskva, Izd-vo And. nauk SSSR. Tol.2 Ubin-
ternary sediments in the 1hropean part of the U.S.S.R.] Chat-
vartiohnys otlozhenlia Xvropeiskoi chasti SSSR. 1961. 502 p.
(HIM 14:5)
1. Tsesoyusnoye mexhduvedometvannoye soveshchaniya po ituche-
n1yu cbetvartichnago periods. Moscow, 1957. 2. Geologicheakiy
Institut AN SSSR ( for 14oak7itin). 3. Institut geografii AN
SM ( for Damitrashko)
(Geology. Stratigraphic)
Poll V.I.; 'ZA,aWlIll, A.G.,; RMOVICH, I.M.; TOLSTOV, Yu.G.;
GUF(UVIC"ll B.A.; iTtACH11V KIY, NIX.; LEBEDEV,
-wDUIAYLOV) IOSY
V.I.; DENISOV, V.I.; At Vl~~
E.A.; TELMH1,Vp
LAPITSKIY, V.I.; KlILYSUZIR, I.R.
Veniamit Isaakovich Wits; obituary. Elektrichectvc) -0-4:
91-92 Ap 16.1 14:
jVeits, Veniamin Tsaakovich, 1905-1961)
FOPKOV, V.I.; TOISTOV, Yu.G.; STEKOLINIKOV, I.S.; METEROVIGH, E.A.;i
klOSKVITIlT A.T - TAFTY V~A.; GORUSHKIN, V.I.; SOVAWV, S.A.j
LYE ~ I A.S.
Si:xtietlh birthday of I.M. Markovich. Elektrichestvo no.5:
87 My t61. (MD.P 14: G/)
(Markovich, Isaak Moiseevich, 1901-)
HOSKVITIN'. A.I.
Review of the comparative stratigraphy Pleistocene cross sections of
the European part of the U.S.S.R.., Poland,, and Czechoslovakia,,
containi traces of the presence of Paleolith man. Biul.MOIP.Otd.
geol. 36 no.6&95 N-D 961. WMA 15:7)
(stone age) (Geology, Stratigraphic)
MOSPITIM A
t-!!#
Relations4p of flood-plain temoLcas of the Volg%. War and
anoient transgressions on the Caspian with glaciations. DokI..
AN SSSR 136 no.3--689-692 Ja 161. (MIRA 14.-2)
4 Predstavleno akademi am V.N.Sukachowym.
(Volga Valley-Terraces (Geology))
(Glacial epoch)
M SV-UZW, Aleksa*Ir Ivanovich; VEFSTAKS G.V.J. red.1zd-va; MKOGONOVA,, I.A.,
- -------------------
(Pleiatoceas of the lower Volga Valley] Plaistotsen Uizbnego iu-olzb'1mq
Moskva,, 10-vo Akad. nauk SSSR, 1962. 262 p. (Akademiia imuA SSSRO
-poologicheakii institu~* Trudy, no.64) (14IM '.6 $3)
(Volga Valley~Geology, Stratigraphic)
140SNVITIN A, I'
of the bror boundary Of
Volum, subdivIlliOnOt and pooition the Russian
the PlOistMOGUG 'a "m cmter glacial SO" of 162.
Kam. chetv. per. 209161-164
platform. Trudy (MIRA 26: 1)
(?4wsian PlatfOrm-Geologro Str&tjgrapb3-c)
MOSKVITIN A.I.
Editor's mail box. Biul.Nom.ohetv.per. no.27#162 162.
(MIRA 16:4)
(Glacial epoch)
MOSKVITIN, A.I.
Wurm subdivisions arid the position in them of Middlo and Upper
Faleolith levols in Lurope. Izv. AN SSSR, Ser.geol. 27 no.7-.35--41.
J]. 162. (MIRA 15: 6,
1. Geologicheskiy institut AN SSSR, Mosk-va.
(Europe-Goology, Stratigraphic)
KOSKVITIN,-A.1,
Structure of covering formations of the anc-'ent terraces of the
Dniester. Biul. Kom.chetv.per. no, 28:33-55 163. (MIRA -17:5)
xj~.00CAM-V61:0- mient of- powet rict-vo 'Nauka 1964j, 5:549
j _;V.
ture,-. ana.,Ai
and byriirl
je
nA
0i an
KR I GER p NiRolay IvarioN~ch; MOSPITIN, A,I,, otv. red.
[Loess, its properties aria rel.-itiorl to i" I c a!
emironment;fnr the 7th Congress of the INQUA (li.S,A-
1965)] Less, op, svoistva i sviaz' -, geograficheskol
srt)doi; k VII Kciigressu IIIQUA (l',:,l,',hA, 196-5)~ M f, - ~ Vv', t ,
Vauka, 1965. 2,1 1, 1-, 1 1 . (PURA le-Cll)
0,611",mv , (I 'I,; V ()I,., ON I NA, 11 . F.Itllo";h V 1T j N , A, I "
' ia, " D ' '
i - ~ -i-. '..r. tc-g lar! 1 11 ii cd. , -jk 1. ..'i '~ 162 ric, , I J, ", :- I I I ti
I lvanov~ik!jva ec~olog~,razv(-.Aorhnaya 'r- ;,,--
I. . 11 ...
grialooicheskop'.) 117ravler.'Ya i Ger'l-;p"hi-skly 'N
- - .;,"S;t.
.1
, - I ~ ll~ v . .
VW"", B, YTTV - ~ F-L V l a -1 1 al, I, Cvi c I ~ ; .1 -~: - E", . ; 1, 1,~, , . 1: 1'-r- v I c
"11TIV ek.~;jncr lvr~nfjv~
--?,
'vilurk pract.1-ces c Il t lie J 5 (jarx z~ at
the loakogoy-ka J,j.j. 71 bs~r pmor- --,i :e, 1.,Yt
y na oitrxcorz-~,jl~ii sliirj,akt~ fi~, c, _el-..,-
perevalocitnui bazy. s ?, w, ,
.-.-I rvi-.Li, ~. i.
iluzi - --
"On Conductivity cf the
Open Slots in a Stator
Nauk 3SSR, Otde:L. Tr,,I-h.
Submitted 1 Jul 1040.
Gap (zazora) vith
and Rrt.-x, 11 Iz, AIC,
Nauk, No. 1, 1941.
Report U-1530, 25 Oct 1951
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MG-1010411,1110" J-1. 1.
"On sparkless switching-in of an electromepet", by Doctor of Technical
Sciences A, I, --- W , at the Power Ener. Inst. im KRZHIZHANOV'JY.IY
of the Aced. See. U 9
SO: Elek-trichastvo, ITO 5. Moticov, May 1947 (U-5533)
VOIKIVIr~ITIIO A. T
.0 L I A A L.
"Electrical machinery witbout reducing gears", by Doctor of Technical
Sciences A. I. Moskvitin, at the Power Engr. Inst. im KRZHIZEANOVSKIY
of the Acad. See. USSR.
SO: Elektrichestvo, No 5. Moscow, May 1947 (U-5533)
ROSKVITIV. A. I.
PA 70T32
MOSWITIN, A. 1.
Sazonov, N. A. defended his 3octorlg dissertation in the All-Union Institute
of Eechanization of Agriculture, USSR, o,,. 16, Nij 1950, for tht academic Je,-,,ree
of Doctor of Technical Sciences.
Dissertation: "Transient Phenomena in the 3tartin,,, of SIuLrrel-Cagle Electri-c
Motors".
Official Opponents: Profs. El. G. Yevreinov; D. P. Morozov ani A. I. Eoskvitin
(Doctors of Technicitl Sciences).
SO: Elektrichestvo, No. 7, Rosc~)w, August l')')3, pp 37-92 (',.-~/29344, 1, Apr '.4)
MOSKVITIPJ, A. 1.
Yakobi, Boris Semenovich, 1801- 1874.
B. S. Yakobi's activities in designing the first electric motors, arid in develocing the
theory of electric machines.
Izv. AN SSSR Otd. tekh. nauk No. 4, 1952.
9. Monthl List of Russian Accessions, Library of Congress, November 1952. UNCLASSIFiED.