SCIENTIFIC ABSTRACT TOKAREV, L.V. - TOKAREV, P.I.

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• Collection: Scientific Abstracts
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• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: July 16, 2001
• Sequence Number: 6
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

I
AUTHOR KOZLOV, V.P., and TOKAREV, L,,V., WMI.F 11
TITLE Geochemical Charact-e-r-i-s-ttr.T--zf-Organic Substances and Dituoens
Dispersed in the Deposits of 'Coal Measures of the Jower Carbo-
niferous of the Kuyibyshev Near-Volga Region. 20-2-42/67
(Geokhimicheskya kharakteriatika organicheskogo veshchestva i
bitumov, rasseyannykh v otlozeniyakh uglenoenogo gorizonta hizh-
nego karbona Kuybyshevskogo Povolzhya - Russian)
PERIODICAL Doklady Akademii Nauk SSSR, 1957, Vol 113, Nr 2, PP 391-394,
(U.S.S.R.)
Received 6/1957 Reciewed 7/1957
ABSTRACT The deposits of coal measures of the (stalinogorsk) lower ICarboni-
ferous within the conventioal limits of limestones with a X urney-
fauna up to the bottom of the first intermediate layer from below
of the limestone with a tuljL-:fauna are on the whole formed by ter-
rogene rock. The thickness of the horizon fluctuates up to some
300-400 m. In the east of the area it has its greatest thickness
and is devided into layers:1. a chiefly loamy lower on which de-
veloped in a bay filled with fresh water at times, 2. an essential-
-y sand upper one which in its lower part developed under different
conditions: from a bay filled with frenh water to continuous sea-
coast marshes. Its upper part was mainly formed by mainland accu-
mulations: by lakes, swamps and rivers, and possibly also by their
deltas. In the present paper the organic substances and bitumens
Card 0 of these layers are investij,7ated from a geochemical point of view.

Geochemical. Characteristic3 of Organic Substances A&PS&W :z",
and .5itumens Dispersed in the Deposits of Coal _Measureb of tne
lower Carboniferous of thtX"kbyshev Near-Volga Region, 20-P.-42/67
Results show that also those rock varieties at which macrosopi-
cally no coal is noticeable have an increased content of organic
carbons The content of free bitumen A and the total content of
bitumen (A + C) generally falls from limestone inthe direction of
loam and further - coal, th&t is with increasing quantiy of the
organic matter. The content of the undissoluble organic residual
matter is high and increases from the aleurolites into the direc-
tion of coal. If the content of Bitumen is related to the quanti-
ty of rock (schelule 1) a different graph comes out. The yield
of the chloroform-extraction of the free bitumen A generally grows
with the Ancreane of the coal-organio aubstance in the rock. Kamen-
tary analysia showa that extractions even from a highly carbonace-
ous rock are reduced to the highest extent. This relatively also
concerns bitumen C. The combination of components of the A-extrac-
tion shows that the bitumen from loam and argillitene as well as
from the highly carbonaceoun alauroIttetne is relativelly more ra-
duced thRn that from slightly carbonaceous aleurolitene, carbo-
naceous slates and coals. Thus, the chlotoform-extraction of the
Card 2/3 bitumen in coal and carbonaceous slates according to its elementaiy

Geochemical Characteristics of Organic Substances MiMaZ234
and Bitumens Dispersed in the Deposits of Coal Measures 0~ -t-he lo-
wer Carboniferous of the Kyibyshev Near-Volga Region. . .2/67
2D-2-4
composition belongs to the most reduced ones, whereas, according to
the component composition, it belongs to the least reduced ones. On
the other hand in the carbonaceous loam and argillitene the opposite
is found. The oils originating from the least carbonaceous rocks are
the most reduced. The elementary composition of the benzol-resins.
from the chloroform-extract fluctuates in the case of single sorts
of rocks even less that of the oils. The chloroform-eictractions gra-
vitate according to their elementary composition mostly towards the
lines of the coal bitumens (i11.1). Thus it can be presumed that these
substances appoach the bitumens of the coal series. From the diagram
(i11.2) it is obviously that the main part of coals and aleurolite
bitunans are farthest distant from those of the mineral oil. Con-
sidering the paleaographical situation and the above described pro-
perties of bitumen it can be concluded that if a mineral development
here took place atall, it can only have been to a very limited ex-
tent. (2 ill.,3 citations from publications)
ASSOCIATION Allunion Scientific Geological Research Institute for Mineral Oil,
PRESENTED BY STRAKHOV, N.M., Member of the Akademy. Moscow
SUBMITTED 22-10-1956
AVAILABLE Library of Congress
Card 3/3

TOKAREV, Lev Vladimirovich. Cand Geol-Min Sci -- "Study of the coal-bearing
carbon stratum of the Kuybyshev Volga region in connection with its petroleum-
0
bearing ~4, 11 Mos, 1961 (Min of Geol and Mineral Conservation USSR.
Petroleum
All-Union Soi Res Geol Prospeot&ng,,Ins-t "VNIGNI"). (KL, 4-61, 190)
_112-

GWYSHWA, G.A.; K0210V, V.P.;.TCKARET
tL GULYAYEVA, L.A., red.;
ji.1
KULYAHINA, T.A., vedushchiy red.
(Studies on the geochem;stry of organic matter in coal-bearing
deposits of the lower Carboniferous in the Perm area of the Kama
Valley with ieference o petroleum genesis] Op7t izucheniia
geokhimii organiches, go veshchestva uglenoonykh otlozhenii nizhnego
karbona Permakogo Prikamlia v eviazi a genezisom nafti. Moskva,
Goo.nauchno-isal.in-t nauchn.i tekhn.informataiis 1959, 59 po
(Perm Province--Petroleum geology) (MM 13:9)

TOKAREV L.V
Genesis of oil in the Kuybyshev upper Carboniferous coal for-
mation In the Volga Valley. Trudy TJT11GAZ no.4:65-77 ' 58.
(MIRA 11-012)
(Volga Valley--Petroleum geology)

KOZLOV, V.P.;-TOXARKV, L.V. M'......"-s'
Genetic classification of caustobiolites. Jjeft.khoz.33 Ii-e-341
no.9:44-47 S 156. (Caustobiolites) (MA 9:10)

KoZikjvy V.".
Gas distribution in iiedimentary-formtions- 1i ied b7 the stlidies
L;,,V.L;cr,2-. 4 x,o.7:19-33 JI 161.
(,,-,,rA 14:10
1. Vceso:--uznyr nauchno-Issledovatel'sMy instit --)riro ogo
ute. dn
gaza .
(Donets Basin-Gas natural, Geology)

TOKAREV, M., tekhnoruk
At the lowant cost. Prom.koop. 13 no.11:24 9 '59.
1 (MIRA 13:3)
1. Artell "Galanteroya," Llvov.
(Llvov--Plastics industry)

BA Lo,'l I Ff;i)X p. 0 r -

TOK AF
t I

VYSOKCSOV, N.V.;DOVGELI, B.A.; LEONOV, I.Ye.; POPOV, N.M., red.;
TOKAREV, M., red.
[Planning state farm production and financial operations) Pla-
nirovanie proizvodstvenno-finansovoi deiatelinosti sovkhoza. Izd.
2. Moskva, Vses.zaocbrye uchetnye kursy (VZUK). No.l. (Planning
state fam production (lectures tbree-six)]Planirovanie proizvod-
stva v sovkhozakh (lektsii tretlia-shestaia). 1960. 63 p.
(MIRA 15:1)
(State farms-Fimance)

TOKARF,V, 14.
Irecting, frameless large panel apartment house. Stroitel'2 no.6:6-7
Je 156. (MLRA 10: 1)
. (Apartment houses) (Precast concrete conatniction)

' ---.,~khail---~leedoroviclx,.~polkovnik; LEVIN, M.V., polkovnik. rod.;
TOKkjrLff
GAVRILOVA, A.M., tekbn.red.
[Soldier-builders] VoemWe stroiteli. Mosk7a, Voen.izd-vo
M-va obor. SSSR' 1958. 95 P, (MIRA 11:12)
1
(Construction industry)

RTABOV, Vasiliy Bergey8vich; TOKARNV-, X.F., polkovnik, red.;
KUZIMIN, I.F.i tskhn._ii6.`-'_ - :_ - _I:
[Soldier and cAtizen] Voin-grazhdanin. Moskva, Voon.izd-vo
M-va obor.SSSR, 1959. 63 P. (MIRA 12:7)
(Soldiers--Civil status) (Russia--Politics and government)

VAZHIN, Fedor Afanaslyevich, podpolkovnik, voyennyy zhurnalist;
TOKARW-, H.F., polkovnik, red.; ANIKINA, R.F., takhn.red.
[Aviation in combat) Aviateiia v boiu. lfoskva, Voen.izd-vo
H-va obor.SSSR, 1959. 74 p. (MIRA 13:1)
(Hussia--Air force) (Air warfare)

BORISOGLZBSKIY, Viktor Valerlyanovich, general-mayor yustitsii;
TOKA-U-1. M.P., polkovnik, red.; KMIMIN, I.F., tekhn.red.
[Maintaining military discipline] Na strazhe voinskogo
poriadka. Moskva. Voen.izd-vo M-va obor.SSSR, 1959. 78 P.
(MIRA 12:12)
1. Prodsedatell Voyennoy kollegii Verkhovnogo suds SSSR (for
Borisoglovskiy).
(Military discipline)

KARINTSEV, Petr Fedorovich, polkovuik; TOKAM, K.F., red.; KRASAVINA,
A.M., tekhn.red.
[The Infantry on the offensive] Pekhota v nestuplanii. Moskva,
Voen.izd-vo 9-va obor,SSSR, 1960~ 78 P, (MIU 13:9)
(Infantry drill and tactics)
(Attack and defense (Military science))

woo
DBRUCKE009 Ivan Grigor'Yevich, Polkovnik v otgtavkq;
polkovnik, red.; BUOVUAU, H. 1?.
_A. Pte khn. re d.
114ilitarY drivers] TOennve voditeli,
M-va obor.SSSR, 1960. 99 P. MOOkvBo Voon,izd-vo
(2ransportation, Military) (MIRA 13:10)

MIMYEV, Yu.A.(- TCKARET, M.F.
a
Equipment for "small* Motion-picture studios. Tekh.kino I telev.
4 no.9:43-44 s 16o. (MM 13:9)
(Motion-picture Btudios--Equipment and nupplies)

MARTYNOV, M,-, in7h.,~ -unhustllyc~ BUDILENKO, L.F.,, TOKAREV, M.N.;
SIIAMI.
S V.P.~ POBROVA.~ M,A.
Auz.omati- control water boilnrei. 11spoll. gaza v nar. khoz.
no.'r.3226-230 16). (M'IfUi 1&--9';
1. Otdol kanstruirDvaniya sredstv makhanizatsil i avtomatiki
Saratovskogo gosudarstuarinogo nauchno-ts3ledovatellskogo i
proyektnogo Instiltuta po ispoltzo,.ani~ru gavi v narod-nom
khozyaystvo.

I -
V ,eljj~j.~JT N15
611.551
.T6
14nozhitellny,jo tan"blitsy dlya iechisleniya ob"yemov k-ruglykii 1e nykh.
ma-terialov po GOST 2708-4 (Factor tObles for the coninutation of the
volume of circular timber ntterials accordint, to G'03T Mockvu,
Gosles'blumizdat, 1955.
413 P. talblas.

TOKAREV, Mikhail SeMUtvich-14-AHNEV, N.A.J. red.; KIMMEL', L.S.,
red. 3.za-va; BACHURINA, A.M., tekhn. red.
[Multiplication tables for calculating the volumes of round
lumber in accordance with the All-Union State Standard 2708-441
MnozhitelInye tablitsy dlia ischisleniia ob"emov kruglykh les-
nykh materialov po GOST 2708-44. Izd.5. Moskva, Goslesbum-
izdat, 1961. 413 p. (MIRA 16:7)
(Lumbering--Tables and ready-reckoners)

TOKAREV, Mikhail Sergeyevich
[multiplication tables for the computation of the vo~-me
of round timber in accordance with State Standard 2708-44]
MnozhitellyWe tablits7 dlia ischisleniia ob"emov kruglykh
leanykh materialov po COST 2708-44. Izd.6. Moskva, LaBnaia
promyshlennostlp 1965. 413 p. (MIRA I8t12)

TRIFONOV-YAKOViEV, D. A., inzh.; AMATOV, N. N., kand. tekhn. nauk;
TOKAREV, M. V.; inzh.
Testing of an experimental soil packing machine with pneumatic-
impulse action. Energ. stroi. no. 16:27-32 160. (MM 16:12)
1. Moskovskiy filial Vsesoyuznogo instituta, po proyektirovanlyu
organizatsiy energeticheskogo stroitelistva.

AMATOV, N.N., kand.tekhn.nauk; TOKAREV, M.V., inzh.
New design of buckets for transporting concrete mixtures. I-nerg.
stroi, no.16:50-54 160o (MIRA 16:12)
1. Moskovskiy filial Vsesoyuznogo instituta po proyektirovaniyu organi-
zatsiy energeticheskogo stroitellstva.

1~- V,
.AMATOV, N.N., kand.tekhn.nauk; TOXAREV, M.V,, lnzl,-
The unloading and transB-6A*'aiion of cement at
Hyda,oslectric Power Station. Mekh.trud.rab.
(Stalingrad hydroelectric power station)
the Stalingrad
11 no-7:6-11 -T1 157.
(MIRA 10:11)
(Cement)

GRODZOVSKIYp G.L.; KUZNETSOV, Yu.Ye.; TOKAREV, M.V,
Approximate calculation of axisymmetric supersonic flows ur4er
internal problem conditions. Prom.aerodin. no.24il52-157 162.
(MIRA l6t7)
(Aerodynamics, Supersor4c)

TOXATW. N. (g. Dihambul)
People fight the elements. Pozh.delo 4 no.10:18 0 '58-
(MIRA 11:11)
(Fire extinction)

TOKAMO -N.A. .
The MW mounted universal stack carrier. Biuletekh.-ekon.inform.
no.g16l-62 16o. (MM 13:10)
(Avioultural machinery)

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TOKAREV, N. M. I IRIN.U(KHOV, G. S.
20,180
Ryh. k1hoz-vo, '~77-28.
SO: Letopa--' Zh-urnnllny~-h '~tatey, Vol. P, !-`,Os';,:O-,r, 11049
u

TOKAREVI N. N.
"Sorption of uranium from carbonate solutions and pulps."
report submitted for 3rd Intl Conf, Peaceful Uses of Atomic Energy, Geneva,
31 Aug-9 Sep 64.

L 46106~66 EWT(m)/90(t /ETI IJP(c) J
ACC NRs AR6000435 SOURCE CODE: UR/0137/65/000/009/GO18/GO18
AUTHORS: Laskorin, B. N.; Tokarev, N. N.; Vodolazov# L. I.-
TITLE: Continuous methods for sorptional extraction of- rare- and nonf errous metals
from pulps
SOURCE: Ref. zh. Metallurgiya, Abe. 9GI59
REP SOURCE: Sb. Ionoobmen. tedmologiya. M., Fauka, 19659 55-62
TOPIC TAGS: metallurgy, physical metallurgy, metal extracting, nonferrous metal
ABSTRACT: A filterless-oorptional method for extracting nonferrous and rare metals
is described. Under industrial conditions this method has been approved in 1953--
1954, producing excellent results (it assures the increase of plant productivity by a
factor of 1-5--3.0, increases the extraction of useful components by 5-100., raises
the productivity of key workers by a factor of 2-3, diminishes the use or chemicals
and auxiliary materials). Working plans and descriptions of static variant of the
sorptional treatment of pulp are presented, as is the method for the sorptional
treatment of pulp in the suspended layer of ionitle, in the moving layler of ionite, in
the apparatus with pneumatic mixing, and in the continuous method for sorptional
extraction of nonferrous and rare metals. 10 illustrations. V. Semakin ZTranslation;~
of abstract
SUB COM 11
Card 1/1 UDCt 669

L 45716--6L (t) /FT
cl_
_EWT (-Iqj..t
kcC N~, AF6025400 SOME COM Un/oo62/66/000/007/i267/1269
AUTHORt Vollnov, I. I.* Tokareva, S. A$ llimanovq Ve L; Pillpenkop 0. P.
< 13
ORGI Institute of General and Inorganic-Chemistry ~N, N, S, Kurnakov, Aoadea7 of
Sciences-I'SSR Unartitut abehahey i neorganicheskoy khimii Acade i nauk SSS
TITLEt Synthesis of potaosiuri ozonide via potassium superoxide suspended inlreon-i2
SOURCEt AN SSSR. Izv. Ser khimg no. 7, 1966,, 1267-1269
TOPIC TAGS$ ozonidej superoxidej, potassium compound
ABSTRACTI The reaction of K02 with ozone was carried out in Freon-12, a liquid inert
toward ozone. Potassium superoxide had the following compositions X02P 90-22%; X202P
3.85%; KOH$ 2.75%; 42CG~v 1-85%; H2,0, 1.33% (by difference). Its particle size was
0-05 mm or less. The ozone content of the ozone-oxygen mixture was 9 wt. %. The stop
of extraction with Liquid ammonia was omitted. Analysis of the ozonized product gave
3j 5.6 wt. %. The increase in the amount of KOH
KO~p 77.2; KC~s 6.4; KOHv 10.6; K2CO
and K2CC~ impurities in the and product as compared to their content in the original
potassium superoxide is due to the reaction of KO~ with atmospheric moisture and C02
during thit withdrawal of the samples foraTialvaial, despite all the precautions taken.
Orig. art. hast I figure and 2 tables.
SUB CODEs 07/ SUEA DAM 18Dec65/ ORIG REFI 003/ OTH REFS 003
2

I
TOK~iP-E,V, 11- S- .. -k,
. . 1, 't, 1-1,0 terlon. 1 1,1
Ek 0 2 (2)
Card 2/3

-69/6 39078
S
/ 2/0007006/011/093
7t
zner.-Y estimation of' D228/D304
in -uhe case'under investigation the surface wave energy constitutes
96.6~'j of the seismic wave energy. Therefore -Iffie (estimated) value
o.-;L' tae -roup velocity of Love waves -- c 1.87 km/see -- is ta-
C)
ken for c. The method's relative error does not exceed 10% (with-
out taking into account the uncertainty of the magnitude of POIL),
wrUch follows from the comparison of the results of calculations
Of Ek for 9 earthquakes according to formulas (1) and (2), when
E,11, ffrom (2) exceeds,Ek from (1) by an average of 3.9%. This a-ppears
to be related to the fact that (2) takes the earthquake "tail"
into account. Z-Abstracter's note: Complete translation.-7
Card 3/3

ACC NR, AT6036298
AWNIOR: Tokarev, P. I.
OHG: none
TIME: Seismicity of the region of the nortlvrn Kamchatka volcanoes in 1961;
SOURCE CODE.'- ~Yjl'66*lodojoh 1/0015 /00
SOURCE: Mi SSSR. Sibirskoye otdeleniye. Institut vulkanologii. Byulleten'
vulkanologicheskikh stantsiy, no. 41, 1966, 15-19
TOPIC TAGS: earthquake, seismicity, seismologic station, upper mantle, volcano/
Kamchatka
ABSTRACT: The present article analyzes the seismicity of the region of the
northern Kamchatka volcanoes during 1964. Only tectonic and volcanic earthquakes
not directly associated with eruptions are investigated. A table of earthquakes
recorded in 1964 is given which shows date, origin time, coordinates of the focus,
and log E of the earthquake (where E is the energy in joules). A map of epicit:nters I
shows two distinct epicentral zones! the Sredniy Range zone with 76 earthquakes
qnd depths of 0-20 km, and the Kumroch Range and Khapitsa River zone with 20 earth-
quakes of which 10 have focal depths exceeding 70 km. * The strongeat earthquakes
recorded were shocks with log E = 12. A great increase in seismicity at focal depthst
of 80-270 km is noted in the area. It'is attributed to the eruption of Sheveluch i

FACC --NR.---AT-6o 36~~C~-
Volcano on 12 Novenber 1964 confirming the author Is earlier deductions thEct
seismicity due to earthquakes at depths of 70-200 km and volcanic activity of the
Kurile -Kamchatka region are the result of tectonic processes in the upper mantle.
Orig. art. has: 1 table and 1 figure.
SUB CODE: 08/ SUBM DATE: none/ ORIG REF: 002/ ATD PRESS: 5108
Card 2

ACC N'R- Am6022705 Monograph ui~
Tokarev, Pavel Ivanovich
Eruptions and:sesmic regime of volcanoes in the Klyuchevskiy group,
1949-1963 (Itverzheniya i seysmicheskiy rezhim, vulkanov KlyuchevskoY
gruppy, 194941963 gg) Moscow, Izd-vo "Nauka", 1966. l16 p. illus.,
biblio., tables. 700 6opies printed.
TOPIC TAGS: 4arthquake,~ seismology, volcanic activity# sajamologic
station, geodynakcs / Kamchatka peninsula
PURPOSE AND COVERAGE: This booklet,, based on seismic data collected
at the Kamch~tka Volcanological Station and the Klyuchi Seismic Station
by the author, B. I, Piyp, and G. S. Gorshkov, investigaites earth- I
quakes associated with the Bezymyan
nyy and Klyuchevskiy volcanoes
-to determine patterns of behavior between the
Ap a,~tempt is.maoA.,
.seismic activity of the vol&moes and eruptions. 1~haracteristic seismic data sigial-
ling the cnset of.an 'eruption serve as the basis of a system of forecasting exploz~ye
-existing statlond__(Kly~c
Kozyrevsk-,Apakhonichi) in
the region, the author calls for the establishment of at least one mcre station near-
1/3 UDQ,. 551-2 +624.n4;)-7

AU_ NKI AM6022705
Bylinkina Crater in order to ensure the precise determination of the
foci of volcanic-generated earthquakes. The booklet has about 100
referenebs.'
TABLE OF CONTENTS:
Introduction -- 5
Ch. 1. Research on the seismic activity of the volcanoes ini,the
Klyuchevskiy group in the period 1949-1956 -- 7
Ch. 2. Activity of the volcanoes -- 12
Ch. 3. Apparatus and methods of processing materials 29
.Ch. 4. Seismic activity of the northern volcanic group on
Kamchatka --,43
Ch. 5. Seismic activity of the Bezymyannyy volcano -- 51
Ch. 6. Relaiionship between the seismic activity and the eruptions of;
the Bezymyannyy volcano 64'
Cord 2/3

ACC NR- Am6022705
Ch. 7. Relaeionship between the seismic activity and the eruptions
of 'the Klyujhevrkiy volcano -- 84
.Supplement -4 106
References 114
ISUB CODE: 08/ SUBM DATE: llFeb66/ ORIG REF; 073/ OTH REF: 021/

IX,M&q&PZ-K.. A.M. (IMncdOL~A"!~ -(urallsk)
Surfacv,.Is admitanV, of ,rcodeoi-c not ert=ined b7 tbg
mt an-ac. volzho mate aLor. r-o&l:ly:,-114 163a
Mul 19: 1)

TOKAREV, P,,,.
Recording of
1 1962. Biul.
the eaplos!ons of the. Klyuchevskiy Volcano in
vulk. sta. nc.37352-59 164. (MIRA 180)

TOKARKVP P.I.
Earthquake swarms of the Sheveluch Volcano in May 1964.
Biu. vulk. sta. no,318;41-44 164. (MIPA 1P,;)j'

MEN
MARKHII,TIN. Ye.l~.; TOKARF-11. P.1.; TILICT"lu'll, ".B.
StlidYing the state of -~hn 7olcancen of the Kly-uche~15kc)r F_G-
_ ;p
C-
and the sheveluch 1161(mno in 196-1. Bill 1. vulk..,3,,n. z! -3./:31*
(niRA 17:10)

MARKHININ, Ye.K.; SIRIN, A.N.; TIMERBAYEVA, K.M.,-.TOKAREV.-P.I.;
MAKHORKIN, I.F., red.
[Volcanoes of Kamchatka
Kamchatki i Kurillskikh
Kamehatakii, Knizhnaia
and the Kurile Islands] Vulkany
ostrovov. Petropavlovsk-
red. "Kamchatskaia pravda," 1959. 85 P.
(MIRA 17W

TOKAREV) Pole
Some problems in the geometrical theory of the second var-ation
in Lagrange's variational problem. Trudy Sekt. mat. i mekh.
AN Kazakh. SSR 2:49-51 163. (MIRA 16:10)

MARKIIININ, Ye.K.; TQM PUGACH, V.B.; DUBIK, Yu.M.
Eruption of the Bezynyanrryy Volcano in the spring of 1961.
Biul. V"Ik. sta. no.34:12-35 163. (MIRA '16slO)

TODREV P. I
Seismic observations at the Kamchatka Volcanological
Station in 1958, Biul.Vulksta. no.33:20-43 162.
OMM 15;12)
. (Kamchatka-Sgismology-Observations)

TOKARE'V., P. I *
Rectilinear Networks Non-determined by the Net Angle on a LOEACIEE73~ay
P1 ans P .13
Ax '~w ;IiTz-
j

-MEAREV-y-P,14 BMISOVA, V.N.
Eruption of the Bezy*annyy Volcano in April 1960. Riul.Vulk.sta.
no.31:23-27 161. (MIRA 15:2)
(Bezymyannyy Volcano)