SCIENTIFIC ABSTRACT SVYATKINA, K. A. - SVYATOSLAVOV, N.I.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R001654210017-4
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: July 13, 2001
• Sequence Number: 17
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

SVYATKINA, Klavdiya A rof.; MIULI, Anna Markovna,
'd6ki6i";ed. nauk; RAS'~~LQVA, Mariya Alo-kseywma, kand.
med. nauk; PONW-UkREVA, P.A., prof., red.; DETMOV.
Ye.P., red.
(Rickets] flakhit. 1.,Oskvn,, '-Ifeditsinap 1964. 221 p.

V" A I, K. Lw-~
the ra
Iltuoh. Irudy jaz. -4 :5Y---54J
f P~ I 1b i II t, o, t je~ 1~t- tI
-L 'u, inokc~.-o in,; i,-;_ tta

S',F~ATYPTA5 N. S.
Svyatkiria, M. 0'.
"Ibe children's libraries anrl reading rooms of the city of Tashkent, their
hygienic chara-:teristics and hy~-Jenic measures." Tashkent State Fedic'al
Inst imeni V. M. Mo3otov. Tashkent., 1956 (Dissertation for the Degree
of Candidate in Iledical. Sciences)
Knizh aya letopis
No. 21, 19,r-6. Moscow

SVYATNIII, B.K.; ~TIATKIXA, M.P.
Viliration sques.-JI-ng of molds under high specific pressures.
Lit. proizv. no','i2:17-20 D 161. (1-11MA 14:12)
(Machine molding (Founding))

SVYATKIN, B.K,.; SVYATKI*, M.P.
Improved drives on molding machine, with high specific #queeze
pressure. Lit.proizv. no.7sl7_18 JI 162. (MIRA16:2)
(Foundries--Equipment and supplies)

124-1957-10-11832
Translation from: Referativnyy zhurnal, Mekhanika, 1957, Nr 10, p 91 (USSR)
AUTHORS: Shemyakin, S. N., Svyatkov, S. N.
"ITLE: The LTA-3 Micromanometer (Mikromanometr LTA-3)
PERIODICAL: Tr. Vses. zaoch. lesotekhn. in-ta, 1955, Nr 1, pp 73-76
ABSTRACT: Description of the construction of a differential micromano-
meter deVeloped by the Authors. The apparatus consists of three
sloping-tube micromanometers connected in such a way that,
when a flowmeter tube is connected, one of the micromanometers
indicates the total gauge pressure of the flow, another micro-
manometer indicates the static gauge pressure, and a third in-
dicates the difference between the first and second micromano-
meter readings, i.e., the dynamic pressure head. A special
valve and conduit arrangement connecting the micromanometers
permits measurements to be taken both in impact sections and
in suction sections of a flow.
S. M. Zasedatelev
,:;ard 1/1

SVYATKOV, S,N,, kandidat takhnicheskikh nan .
The most advwAsgsans-shapes and.sizes for exhaust collectoris.Der.prom.
4 no.10:8-10 0 155~. (MM 9:2)
1.Leningradeksys, ordens Lenim lesotekhnicheskaya akademlya imeri
Kirov&. (Wooci waste)

SVYATKOV, S.N., kandidat takhmichaskikh nauk.
Hydraulic resistances in exhaust ventilators. Der.pron.5ne.6:14-15
Jo '56. (Mk 9:9)
1.LeningradskLya ordeza Lenina leastakhnicheakaya akademiya imeni
S.M.Kirova.
(Fams, Mechanical)

SEBNNINOVA, N.A.
Design of pneumatic transportation units with two evacuation
fans. Der,prom. 9 no-3:12-13 Mr 160.
(MIRA 13:6)
1. Iesotekhaichesk-aya akademiya im. S.H*Xirova.
(Pneumatic-tube transportation)
(Wood-using Industries--,Equipment and supplies)

"SVIATlio)L,-Sepgey-Nikolayevich; GIUITSEV, Yevgeniy Nonstantino7ich;
GOLJJBEVA, T.M., inzh., red.; FMICHEV, A.G., red. izd.-va;
GVIRTS, V.L., tekhn. red.
[Air fractionation of fine wood particles) Vozdushnoe fraktsio-
nirovanie melldkb drevesWkh chastits. Leningrad., 1961. 20 p.
(Leningradskii Dom nauchno-tekhnicheskoi propagandy. Obmen pe-
redovym opytom. Seriia: Derevoobrabatyvaiushchaia pronyshlen-
nost', no.5) (MIRA 14:12)
(Separators (Mazhines))
(Hardboard)

17.A.,. PUPY-Zif ITI.A.
oarcis.
w - w a -Ifacture of particle b
WIA. 14:2)
Dv-
alm,~,end-,-a im. S.M.Kdrova.
oso I I -- . o a
(I'a:t T--Qnrd", )

ICA RJIUI~K?q-~ OWFAMM
Som.-
ILIYEVp T.N-.--j~--SXUTKOVj, S.N.
Rite of soaring of wood particles. Der.prom. Uno.12:13-14
D 162, (MIRA, 16t1)
(Dynamics ofIa particlw) (Pneumatic conveying)

-Nikolayevich, dots., kand. tekhn. nauki KO
3VYATKOV,_,P~Fgqy RSHUNOV,
A.N.
., dots., kand. tekhn. nauko retsenzent; PAUSTOVSKIY,
G.A., ot-v. red.; BEZGODOVA, L.V., red.; URITSWA, A.D.p
tekhn. red.
[Intrafactory transportation; textbook for term and diploma
projeo.ts (for students of the faculty of woodworking
technology)] Vnutrizavodskii transport; uchebnoe posobie k
kursovamu i diplomnomu proektirovaniiu (dlia studentov fa-
kullteta, mekhanicbeskoi tekhnologii drevesiny). Leningrgd,
Vses. zaochnyi lesotekhnich. in-t, 1963. 164 p.
(MIRA 17:1)
1. Starshiy prepodavatell kafedry soprotivleniya materialov
i detaley mashin Vsesoyuznogo zaochnogo 26sotekhnicheskogo
institute. (for Paustovskiy).

L 1.1160;;63 EPR/EWP(-J-)/EPF(6)/~kn(im)/BDS-~;AM(;ASD.~;7-Ps-4/Plc4i/Pr~4,
RM/WW
ACCESSION NR: AT3002183 S/2917/62/000/242/0134/0147
ATIIFOR: Artamonov, V. Sp (Candidate of technical sciences);'Saatkovskaya, Ye. D.
(&gincar); Solntsev, Do I* (Engineer); Tikhonova, G. S. (Engineer)
TITLE: Polymer materials.for corrosioAprotection of railroad bridges
SOURCE: Moscow. Vsesoyuzxq*y nauchno-issledovateltskiy institut zheleznodoro-
zbn)go transporta. Trudy,, nop 242, 1962. Primeneniye plastmass na zheleznodoro--.
zhoja transporte.. 134-147
TOFIC TAGS: polymer-anticorrosion paint, bridge painting,, FL-03K primer..'FL-013:
priiier, KhV-113 enamel, SKUM-17 enamel, EP-51 enamel, E-4021 epoxy patty, FL-14P 7
Al i*wder enamel, VL-08 primer, PKhV26 enamel, PKhV-715 enamel, PkhV-714 enamel,
KhSO10 primer
AB31RACT: Experiments with various polymers intended for coating rr bridges are.
re 'pcrted. A review of bridge-painting practices in various countries opens the
article. Then some physical and che%ioal characteristics are presented of the
follolding coating matptials., __Ej=QLKfPheno1-formqAehyde primer, FL-013 phenol- t(
a]Jcyd primer, jgIS01OUtopolyaLer of vinyl chlorideNnd vinylidene. chloride, VII08
phosphate primer, protective zinc primer; PKhV-26,, L~KhV-715,, PKhV-714, and,KhVI.13.
Card 1/2
... ... .......
---------------

L 13.11 i0-63
ACCIZISION NR: AT3002183
vinyl perchloride enamKs; SKhB-17 enamel (copolymer of vinyl chloride end vInYI-7
butyl ester); SKhBM-l7 empael Fcopolyiper of vinyl chLoride, rinyl-butyl ester, and.
~jejO -6%poNy plus Al powder
methyl~-acrylate,~; F 26'Pand 2062- 'glyptal in-
F , ED _;
laectucr, FLo-14V$henol resin plus Al.powder lacquer!;! 16-5 titroalkyd-epoV enamel
E-4021. epoxy putty; divinyl-acetylene paint* Quality of coatings was tested in
laborztory., at atmospheric-corrosior~ stations, and on rr bridges (trial coats).
The,-e physico-mechanical characteristics of coats were determined: adhesion, im-,
pact strength, bending strength, thickness, hardness, and continuity. The sample
coatirgs were also tested in a hydrostatic- chamber, a 8ulfur-dioxide chamber# a
and at atmospheric-corrosion stations in Moscow and in Kerch.i
weatherometer
--Resu-It,s-of--test"re-described-in.-detail*---,M-e-best--remLUs-were-epchiV:ttp4--b5r the-
follo-sing materials which are, therefore,-recomended for coating the rr-bridges:
F,4021 epoxy putty, KhV-11:3 enamel over FL-03K.or FIr-013 primer, SKhBM-17 enamel
over- the same primers, EP-31 enamel over the above epoxy.putty, and FL-14 plus Al-
powdex enamel over the above primers. Orig. art. has: 2 tables.
ASSOCIATION: Vsesoyuzny-Ky nauchno-isi3ledovateltskiy-in.stitut zheleznodorozhnogo:,.
transporta (All-Union Scientific Research Institute of Railroad Transport)
a
SWaITED: 00 DATE ACO: logj~y63 ENCL: 00
SUB I !)E: 00 NO SOV: 010 OTHER: 001
Card 2,12

SAUI I IY, Ye.Jr.,, doktor fiz,-mat, 1.~~-,-,TISHCHMOO VOGO
A,Ye - DCBROTOLISIUY, A.D,; ZHITAaO, GMY, K.P.,
~-~ITMAYA, S,K,,, tekhn. red.
[Tffunaids of November 4-5,,19521 TSunami 4-5 noiabria 1952 g.
Moskia, IzcI-To.Akad. n=k SSSR. 1958. 60 j. (Akademiia nauk
SSSR. Sovet po goismologii. Biulleten' no 4). (MM UtO
I (FMIfic Ocean"Tidal ;;;eel

ANDUYN, V., inzh.;
Ethyl alcohol enamels are reliable anticorrosives for construction
elements. Na stroi.Mosk. 2 no.2:20-21 F '59. (MIRL 12:3)
(Corrosion and anticorrosives)
M~6v-(Otive coatings)

88428
S10561601039100610151063
E&6'/D056
AUT'~0173: Vovchenko, V. G., Gellfer, G., Kuznetsov, A. S.j
M
11 shcher-yalkov, M. G., Syvatkovskiy, V.
e
TITLE: Effect of N'uclear BindinG of Nucleons Upon t-he Shape of
Pion Ereri~-
j Spectra
PI.-',7-TODICAL: Zhurnal eksperimentallnoy i tecreticheskoy fiziki, 1960,
Vol. 39, No. 6(12), pp. 1557-1570
T!iI(T: A description is ~-~ven of experiments i-,hich were carried out
'th the ain, of obtaining, quantitative data on the effect produced by
vri i, U U L,
mucleon b:Lndings in deuterons and carbon nuclei upon the production of
char,ed -,):;ons. Conclusions -are dra~m vrith respect to pion production
processes on the basis of comparisons of the enerZ~r spectra of pions
produced in collisions of protons with free protons and Ath nucleons
h:)und in deuterons and carbon nuclei. The experiments were conducted
L-1 a wal ensuring strictly equal conditictis in t--akin- the spectra and
separptinco; the pF.- and pn-coflisions. The e>q) eriments ware carried out
on the six-meter synchrocyclotron of the Joint Institute of Nuclear
Research.
I

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ddpoolta of the Chlbin 1111114114 A F S-tlt
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J?Jl.; KULaKOV, V.S.;
DITERIMS , _ .; 2AVARITSKly. 4.N., Aka-
demik, glavnyv rtdaktor; KULAKOV, V.S. geolog; TROTSKIY, A.N. khImik.
Parasitic craters of Klyuchevokaya Supka, arising in 1932. Trudy Kamche
vulk.Bta. no.2:3-23 148. (MLRA'6:5)
1. Ramchatskaya valkanologichaskaya stautsiya. (Klyuchevskaya Sopka)

.5 V C , I - --> /c- 1-1,- ~, -/-~,
DOHROXHOTOY, ru.S.; SVTATIDVSKff, A-To.
Morpholoff and geological structure of volcanic cones in the Kostakan
Gorge. 1'rudy leb.aaromet. 3:89-95 '54. (KERA 8:8)
(Kostakan Gorge-Volo3noes) (Kamchatka-PbLotograpby, Aerial)

S7YATLOVSKIY, A.Ye.'
q 40m*.Vkw.~ mw"M~-.m
Applie-w",ion of geomorphology in the at-udy of volcanic regionse TrmW
Lab.vullc, no*8:226-235 1540' (MMA 8:4)
(Volc;~O*es)

PIYP,B.I.; SVYA'rLOVSKIY,A.Ye.
- -
Eruption of Krenitsyn Peak during 1952 Biul.Vulk.sta. no.20:64-
68 '54. (MIRA 8:11)
(Onekotem Ialand)

J
MAMOVSKIY, A.Te.; GORSHKOV,
G.P., redaktor; ALEKSEYEVA, T.V..
[Tsdnami, sea waves produced by submarine earthquakes]
Tsunami; tiorskie volny.pri zemletriaseniiakb.Moakva, Izd"vo
Akademli nauk SSSR, 1955. 21 P. (MLRA 8:11)
(Tidal waves)

d
USSR/Geology-Voleartip': action
Card j/1, Pub. 1~6-16/jq
Authors I Svy-a-t'Lovskiy A.E Cand.
Geol Mineral So.

M16- Eruption of Krenitsints volcanos
Nriodical t Priro6a~44/1~ 85-48, ~_Jan- 1955
Abstract
The v6.1cano known as Kren.its.in I s- rolcano-- on th e* islanct of Onekotan:,---
of - the".. Kuril group Is: described .lAn~account Is -given: of - how thiq
volcano, long dormant erupted.airain in 1952-with extraordinary...-.
violence, changing the appearance'of the landscape and affecting the
meteoiological condit-.,ons so -the t: there was frequent lightning..-
followed by wind.~ Illustrations. -
Institution Acad, Sc. USSR, Volcanological Laboratory
Submitted

SVTATIOVSKIY, A.Ye.
r
Earthquakes and characteristics of the tectonic structure of the.
Rurile-Kamchatka region. Biul.Sev.po seism. no.2:31-34 156.
(Kiwile Trench--Geolog7, Structural) (MA 9:9)

15-57-12-17181
Translation from: Referativn zhurnal, Geologiya, 1957, Nr 12,
p 65 (USSRTY
AUTHOR: -Sv,7atlovskiv, A. Ye.
TITLE: The History of Recent Vulcanism and Landscape
Development in the Region of Bakenin Volcano (Istoriya
noveyshego vulkanizma i obrazovaniya rellyefa v rayone
vulkana Bakenin)
PERIODICAL: Tr., Labor. vulkanol. AN SSSR, 1956, Nr 12, PP 53-109-
ABSTRACT: The volcano Bakenin is situated in the southern part
of Kamchatka in the regioli of the eastern mountainous
belt of the peninsula, at the junction of the Ganall-
sk'Ly and ValaginC Ranges. In the region of the
volcano, the oldest formations are the ValanginlAn.
beds, of Mesozoic age and ?aleogene* (?) porphyriti~
layers. These rocks form a beveled erosion surface,
Card 1/4 on which overlying andesite-pyroclastic.beds have

15-57-12-17181
The History of Recent Vulcanism (Oont.)
volcanic rocks of the Bakenin region beginning with the areal flows
at the Tertiary-Quaternary boundary (the andesite-pyroclastic beds)
and ending with the -last appearance of dying volcanic activity,
eruptions of basaltic, lava flows in the vicinity of the volcano.
The central depression in Bakenin is a caldera. During development
of the landscape of the region about Bakenin Volcano, there existed
a number of relief forms, changing under the influence of endogenic
and exogenic processes: 1) the landscape exi'sting before the for-
mation of the andesite-pyroclastic sequence, 2) the landscape de-
veloped after the formation of the andesite-pyroclastic sequence,
3) the form produced' Inside the caldera during the time the basaltic
extrusions occurred within it, 4) the form arising during ancient
glaciation, and 5) the modern landscape. Bakenin Volcano was formed
after the ancient glaciation. The mountainous region surrounding
Bakenin was formed by uplift and erosional dissection of the lava
plateau composed of the andesite-pyroclastic sequence. The form of
the modern landscape originated' during the dying stages of volcanic
Card 3/4

Translation from: Ref'erativnyy zhurrfal, Geologiya 15-57-7-10044
1957, Nr 7
pp 193-194
AUTHOR: Svyatlovskiy, A. Ye.
TITLE: The Southern Bystrinskiy Range in Kamchatka (Yuzhno-
Bystrinskiy khrebet na Kamchatke)
PERIODICAL: Tr. Labor. vulkanol. AN SSSRS 1956, Nr 12, pp 110-190
ABSTRACT: The Southern Bystrinskiy Range is the southeastern
end of the Eastern Range of Kamchatka. It is composed
of ancient rock series which occur at the base of
active and extinct volcanoes surrounding the range.
The Southern Bystrinskiy Range trends northeasterly
on the north, southeasterly on the south. The structure
of the range involves the following groups: The
Southern Bystrinskiy complex (Mesozoic), composed of
black phy1litic schists, graywacke sandstones,
Card 1/7 crystalline schists, and foliated porphyrites. The

15-57-7-10044
The Southern Bystrinskiy Range (Cont.)
of marine sandstones with layers of altered lava and tuff. Middle
Miocene molluscs are present. 2) The Poperechnaya River series
(lower Pliocene) is made up of sandstones, the fragments of which
derived from volcanic rocks, and graywacke sandstones, shallow-
water coquina. Fossils are abundant and the series rests unconform-
ably on older rocks. 3) The Vachkazhets Mountain sequence of
agglomeratic tuffs (Pliocene), contains agglomeratic tuffs, the
fragments of which come from altered amphibole-pyroxene and
amphibole andesites, with layers of tuffaceous sandstone. This
series is also unconformable. 4) The Irachkezhets River series
(upper lower Pliocene) consists of sandstones made up of fragments
of volcanic rocks and altered agglomeratic andesitic tuffs. 5) Post;-
Pliocene volcanic rocks comprise unconformable basalts, andesite-
basaltsI andesites, and rhyolites. 6) The volcanic rocks of the
Tolmachev Valley consist of black ba8ic blocky lava and flows ot,
basalt with ropy structure. Modern volcanic activity has been
described from the example of the Go:rely-y Volcano. The slopes of
Card 3/7

15-57-7-10044
The Southern Bystrinskiy Range (Cont.)
the caldera, above which the volcano rises, are covered by andesite-
basalt flows, tuff-breccias, and tuff-lavas, culminating the volcan-
ic activity of this region. In a geologic- petrographic discussion,
detailed descriptions of the petrographic varieties among the above
noted rocks are given. Intrusive rocks are also described (granite
in Akhomten Bay, diorite on Vachkazhets Mountain, monzonite along
the Karymchina River, and aplite along the Elizovskaya Polovinka
River). The tectonics of the area has been distinguished in
large-scale stratigraphic groups. The Southern Bystrinskiv group
is characterized by a northwestegly strike and a dip to th;
southwest at angles of 450 to 60 . The rocks of this group form
the southwestern limb of a large anticline overturned to the
northeast. The northeastern limb of the structure has been broken
by a fault treading northwesterly along the southern border of the
Avacha Valley. The porphyrites do not form well-expressed folded
structures. They dip at angles from 00 to 300. The folding of the
Tertiary series to the south of Avacha Bay has been subordinated to
Card 0

The Southern Bystrinskiy RangE (Cont.) 15-57-7-10044
flowed down the slope of the ,iolcano and into irregularities of the
landscape. The lava forms a -plateau. ' In early Quaternary time the
water-divide area of Southern Kamchatka was a zone of tectonic
subsidence, and a site of central-type eruptions. The formation
of individual calderas and stratovolcanoes continued in post-glacial
time. There is a characteristic linear distribution of volcanoes
in a northern group and a central disposition within the sunken
Quaternary lava plateau. The geological history and the volcanism.
are described briefly in conclusion. The composition of the rocks
of the Southern Bystrinskiy group indicates that this region in
the Paleogene, after the Laramide orogeny, entered a long-term
continental cycle characterized by extensive volcanic eruptions.
A marine basin formed in the region of the Southern Bystrinskiy
Range in the Neogene, receiving a thick sequence of sediments.
Lava continued to be poured out. in the coastal zone to the north
of the range. At this stage the region had a geosynclinal char-
acter. The marine basin became shallow toward the end of the
Card 6/7

STYATLOVSKIY, A.Ts.
I
Two unusual volcanoes of Tolmaebev Valley. Biul.Vulk.sta.
no.24:52-60 156. (MLRk 9:10)
(Tolmacbev Valley-Volcanoes)

SVYATLOVSKIY, A.Ye., kandidat geologo-iiineralogichaskikh n&uk.
Utilizing the heat of the earth's interior. Priroda 45 no.6:90-92
-Te '5 6. (Kok 9: 8)
1. Kamchatskaya geotermicheskaya ekspeditsiya Akademii. nauk SSSR.
(Earth temperature) (Volcanoes) (Springs)

MMOLN~W--wo
-K'i
AUMOR: Svyatlovskiy, A. Ye. Call Nr: GC 221. B85
MLE: Ts=ani#,, Destructive Wavew#,,'Caused by Submarine Earthquakes
in Seas and Oceans (TS=BZA!; razrash:Ltelln-yye volny,
voznikayushchiye pri podvodnlfkh zemletryaseniyakh v moryakh
I okeanakh)
PUB. DATA: Izdatellstvo Akademii nauk MR, Moscow, 1957, 69 pp.,
5000 copies
ORIG. AGE=: Akademiya nauk SSSRtSovel; po seysmologii
EDITORS: Responsible Editor: Prof. G:)rsbkov, G. F.' Editor of
j?
Publishing House: Gurov, K. P.; Tech. Ed: Guseva, 1. 9.
PURPOSE: The pamphlet's purpose Is to acquaint the reader with the
phen non of seismic sea waires called tsunamis, which has
caused widespread destruction along the littoral of the
Pacific Ocean.
Card 1/4

Call Mr: GC 221 -. S85
Tsunamis, Destructive Waves.~Caused by Subm&rine Earthquakes in Seas and Oceans
COVERAGE: A tsunamis Is the effect of an earthquake on a body of water.
Gravity waves produce a vertical displacement in a faalt or a
submarine landslide. Such tectonic phenomena, which may be
caused by crestal stress adjustments, suddenly produce a great
mound of vater over a large urea. The pa*hlets deals vii;h the
physical and geological aspeets of this phenomenon, evaluates
methods and possibilities of predicting the onset of dis-
turbances, relates the experience of witnesses, and makes suggestions
on how to avoid extensive ftutge to life and property. The
observations are based primrily on the very destructive tsmamis
occurring on November 5, 1952, which hit Japan and the north-,
eastern coast of the USSF. Dozens of earthquakes of submarine
origin are recorded every ye&r by Soviet and Japanese selftle
stations. The epicentre of the displacement zone for thEs paxt
of the Pacific is locatedL al(mg the western side of a htk7,e trench
on the floor of the ocesm, s(we 150-200 kilometers avay from the
eastern coast of the KmnchatA:a. Peninsula and the Kuril lileaft,
and reaching the area east of the Japanese archipelago. The
Card 2/4

Call Nr: GC 221 - S85
Tsunamis, Destructive Waves,,!Caused by Sub*xine Earthquakes in Seas and Oceans
pamphlet mentions also other Tsunamis regions in the Pacific Ocean,, Photo-
graphs accompanying the text show the extent of the devastations oJ! the
Tsunamis of November 5, 1952. Maps shav the wrin regions exposed to the
effect of such sea 4uakes. Four appendices analyze the intensity cf the
Tsunamis and the ex-cent of the damage. No personalities are menticned.
-itere are 27 references, 13 of which are USSR, and 14 English.
TABLE OF CONMITS:
Introduction
3
Mnmmis on the Soviet shores of the Pacific Ocean 7
Tomenis on the shores of other countries 30
Causes of the generation of Tsunamis 36
General characteristic of Tsunamls 40
Card 3/4

STUTWVSKIY, A. Ye.
.
tectonics af th.e Klyuchovskiy volcanoes in Kamchatka.
Biul. Vulk. sta. no.26:114-120 15% (KIRA 12-5)
(Kamchatlm--Volcanoe 9)

AUTHOR SVYATLOVSKIY A.E, PA - 2931
TITLE Subdivision of Thermal
Underground Waters of the Kamchatka.
(0 gidrogeologicheakom rayonirovanii termalnykh podzeanykh
vod Kamchatki.- Russian)
PERIODICAL Doklady Akademii Nauk SSSR 1957, Vol 113, Nr 1, PP 175 - 178
(USSR)
Received: 6/1957 Reviewed: 7/1957
ABSTRACT As is well known great artesian thermal water basins with
high pressure are formed in the frontmost sags on the borders
of alpine mountain chains or - tables as well as in the
depressions between the mounte,ins and in structural sags in
the zones of recent volcanic activity. The lack of natural
geysirs does not mean that there are no thermal water basins
in the depths, Closed-up arteiiian basins are usu4,lly only
discovered by deep drilling, :[n the areas of r_!:~oent vulcanism,
however, the usual vertical chemical and tnermarzonality
is disturbed and unfler the in',"luence of vulcanic centers
strange symptoms occur. On Kajachatka no test drillings have
hitherto been carried out in search of thermal springs, and
therefore the author depends on the analysis of geological
CJUM 1/4 41

PA - 2931
Hydrogeological Regional Subdivision of Thermal Underground
'Waters of the Kamchatka.
structure, geomorphology, hydrogeology and vulcanism. Highly
developed recent vulcanism E,nd many natural wells of high
temperature mineral waters lead us to suppose that the arte-
sian waters of Kamchatka have higher temperatures than is
the case elsewhere. With regard to structural-litholog'.oal,
geomorphological and hydrogoological details the following
areas may be assumed to be.possible artesian basins of
thermal water: 1) the lowlands of the western Kamchatkit.
2) the depression of the central Kamchatka 3) the zone of
active vuloanoos in the eastern Kamchatka and L[) the
volcanic zone of the southern Kamchatka. Mountain chains (up
to 2 km altitude) which are heavily drained and Tolcanic
mountains (of UP to almost 5 km altitude) serve as infiltrat-
ion zones for artesian basins. This causes high pressure in
hydraulic systems. The water-,,.arrying layers are massive
synclinal layers of tertiary terigenic, and vulcanogenic
deposits. They are covered by quaternary sedimentary and
vulcanogenic rocks. Greater parts of the artesian basins are
closed.
CARD 2/4

Fvdrogeological Regional Subdiyision of Thermal PA - 2931
Un-'cr.--To-zind Waters of the Kamchatka.
The author declares that, like in the Caucasus and in TTans-
caucasia, thermal waters are to be found in depths of fxom
1500 M - 2000 m in Kamchatka.
Geothermical differenoes decrease in the zones of thermal
levels.' In the first 10 - 30 n the temperature often attains
more than 1000. The geothermical difference gradually
decreases with depth. The theTmal fields of the Kamchatka are
formed in dependence of the distribution of quaternary
volcanos. The isothermal levels show their highest values in
the areas of volcanic massife and decrease in intervoloanic
depression. Volcanic formation is aocompanied by structural
lift and by the formation of eracks through which the hot
waters bubble out. The investigation of the olosed thermal
water basins in the struatur&l-depressions near human
settlements would be of great importance for the national
economy of Kamchatka. The hot water supply of the majority
of the settlements could proba;bly be secured by coniuoting
CARD 3/4

SAVARENSKIY. Ye.Y.. doktor fit.-mats rOLukj.TISHML=O, V*G,; 3VYATKOVl'X^ITg
A,Ye.-,._DCBROVOLISKIY, A.D.; ZEITAMO, A.V - GUROV, K.Mi-g-'re 'Ii
I
tekhn, red,
[Tsuna miis of November 4-5,.19,f,'2] I'Sunami 4-5 noiabria 1952 g.
Moskva, lzd-v6 Akad. nauk SSSF4 1958. 6.0 j. (Akademiia nauk
SSSR. Sovet ljo saismologii, Blulletent no.4). WRA ll::6)
(Pacific Ociean-rTidal waves)

MATLOVSKIT. A e,--
r-- Recent movements of the earth's crust and volcanoes in the Kurille-
Kamchatka area. Trudy Lab.vulk. no*13::39-98 158* (MIRA 12:3)
(Kamchatka Province-Geology, Structural)
(volcanoes)

SVYATLOVSKIY, A.Ye.; FLORENSOV, N.A.
Some characteristics of Cenmoic volcanism in East Africa
and the lake Baikal region. Trudy Irk. un. 14:83-98 118
(Africa, Fast-Volcances) (MIRA 16:7~
(Baikal Lake region-l'oleanoeB)

SVYATIjOVSM, A.Ye.
- Genetic classification of Kamchatks, volcanoes. Biul. Vulk, sta.
no.27:60-65 158. OGRA 11:10)
(Kamehatka--Volcanoes--Clasei&lication)

VSK114.4a-YA .; KELL i , N.G., otv.red.; PIYP, B.I., otv.rede;
PAYMOOLITS. K.N., red.; MGARTIN, V.P.. red.; SOLOVIYIV.
SP.. doktor geol.-~in.na~k. red.; LADTCHUKj L*Po# rDdo
izd-va; SMUUZTSKIY, I.I., tekhn.red.; POLENOVA, T.P.,
tekhn.red.
(Itlas of the volcanoes of the S.S.S.R.] Atlas vulkamov SSSR.
Sostavitell i avtor teksta A.E.SviatlOVBkii. Moskva, 1959.
173 P. (MIRA 12:6)
1. Akedemiya nauk SSSR. Laboratoriya vulkanologii. 2..Chlen-
korrespondent AN -SSSR; Laboratoriya aerometodov AN SSSR (for
Kell'). 2. Chlen-korrespondent AN SSSR; Laboratoriya vulkanologii
AN SSSR (for Piyp). 3. DeystvitelInyy chlen Akademii nauk Ar-
nWanskoy SSR (for Faffengollts). 4..Chlen-korrespondent AN SSSR
(for Ren&VLrten).
(volcanoes)

7s~,~A,TECV SK ~v
!I ~
a
s
oat IV V,
v
it all I
a.4 Aq
1 4 1 A
ot
!a .3 Ail A I
3 J .,20
Oil
3
9
it's

3(9) SOV/26-59-4-22/43
AUTHOR: SY~5:atlovskiz, Candidate of Geological and
~e.
Mineralogical Sciences
TITLE: Tsunami on the Pacific Coast of the USSR -(Tsw2ami
Tilchoo,'Xeanskogo poberezh"ya SSSR)
PERIODICAL: Priroda, 1959, Nr 4, pp '33-97 (USSR)
ABSTRACT: In this 'article the ailthor describes.tsunami - immen-
sely high and big waves,- as a naturalcalamity
threatening the Pacific:coasts. It has been estab-
listed that tsunami usually originate in existing geo-
synclinal regions surrounded by island chains accom-
panied by their deep-water depression --'-n the north-
west section of the Pacific. The main reason for the
formation of tsunami are tectonic earthquakes at the
bottom of the sea, 0ocasionally, they -are also the
results of volcanic .-ruptions. The author gives va-
rious examples and sbresses the need of taking mea-
sures to protect the population on the Soviet Pacific
coast threatened by th_46is phenomenon. Tsunami reach
Card 112 as high as 20 m and their moving speed comes up to

SVYaTLOVSKIY, A. Ye, Dr. GeOl-MiTLeral. SCi - (diss) "Volcanism and
Quaternary Tectonics In Xamchatka," Moscow, 1960, 32 pp, 110 co-iaz
Aw
(Mos~:aw State U im M. V. Lomonoscv) (AL, 46/60, 124)

SVYATLOVSKIY. Aleksandr Yevgenlya-vich; DOBROMVOVA. K.0., red.; ICONOVALYUK,
. -1- I.X.V mUdshiy ied.~J"KOSIMLTVA, S.M., tekhn.red.
[To the Kamchatka volcanoes] 1: vulkanam Kamchatki. Moskva, Goo.
izd-vo geogrAit-ry, 1960, 99 p, (KIRA 3.):6)
(Kamchatkw,-Volcanoes)

- SVYATMVSKIY, A.Ye.
KamchatIm's ultrabasites and their position in the tectonic structure
of the peninsula. Sov- bleol. 3 no-3:40-47 Mr t6o. (KM 13:11)
1. Laboratorir.L-vulkanologii AN SSSR.
(Kamchatka-Ultrabasite)

SVYATLOVSKIY, A. Ye.
ThL'Ichinskiy-Tolcanc-in the'UntrAl Range-of &Wwhatka; structural
characteristics. Trudy Lab' 7ulk n0-_1805-42 160. (MIRA 34:3)
(Ich~;Slkiy Volcano)

SVYATLOVSKY; A.YE.
"Main stages in the i~;-Cto-volcanic hist4iry of Umchatka and the'
Problem of uniformitariamiasm in pale ovolcanological reseam-hes."
tpr-y 12th rAwral Assenbly of ths
-t -76o.

AVZRIYEV~ V,,r.j-1-~~T;PVSKIY-r-LJA*
Toleano-tectonic structureaof southern Kamehatkas IzvAW SSSR,
Ser.geol. 26 no.6.-98-IM To 1611o (KWA 14:6)
1. Iaboratoriya. vulkanologii AN SWR.. Moskva#
(Kamohatka-Gsology,q Struaturm.1)

SWAILo~_=,-~eks_an!~3LYevgenlyevichI doktor geol.-miner. nauk;
TIKHOVIROV, V.N., red.; ATHOSFCHENKO, L.Ye., tekhn. red.
rVolcEmoes and electric power plantslVulkany i elektrost-an-
(b.
tsii. Moskva, Izd-vo nZnanie.," 19620 31 P. ovoe v zhiz-
ni, nauke, tekhnike. XII Seriia: Geologiia i goografiial
no.16) (HIRA 15:11)
(Volcanoes) (Electric power)

V.-K NIW-440-~
a~ 4q-
ACC MR: AP7013163 SOURCE CODE: UR/0210/66/000!00910126/OIP7
AUT14OR: Svyatlovskiy, A. Ye.
ORG, Institute of Volcanology, Siberian Department, AN SSSR Petropavlovsk-
14mchatskly (Institut vulkanologii Sibirskogo otdeloniya.AI; SSS R)
TITLE: Thermal 'aerial survey in geological Investigations and possibilities of
interpretation of the deep heat f told of platform. and orogenic regions
SOURCE: Geologlya i geofizika, no. 9, 1966, 126-127
TOPIC TAGS: volcanology, aerial survey,. geodynamics
SUB CODE: 08
ABSTRACT: The use of a thermal aerial survey in combination with other aerial
survey methods increases the volume of information,obtained in geological
ln~estigations' and makes it possible to Interpret the heat flux of open
structures in different re-ions. Such thermal aerial surveys can be made fo
r
.study of regions characterized by considerable heat anoumali6s associated with-
the emergence at the earth's surface of ii heat flux formed by the convective
transfer of heat from the earth's deeper layers -- voicanic heat, heat Of
subterranean hot waters, heat formed in petroleun and gas regglons, etc.,.as well
as in surveying areas 'of thermal radiations formingin the heat transfer of
radiant energy received f ro,,-,i the sun I dnd other external energy sources.
card -- - --- --.UDC: -550.836 07-33 00
OF"

SVYATLOVSKIY,- A.Ye., dolktor geol.-mineral. nauk
-- - - --------
Shevoluch Volcarto has waked up again... Pri-roda 54 no.5:50 YT 165-
(141RA 18: 5)
1. Kamchatskaya v-ulkanologicheskaya stantsiya.

SVYATNENKO, A.T., inzhoner.
M~ MMUMOW
New pipe-bonding machine. Ilsk.sta. 27 no.9:50 S 156. MEL 9:11)
(Pipe bending)

SVYATNTENKO, Kh. P.
5715. SVYATNEKO, Kh. P. Tsvetovodstvo. Krasnodar, Kn. lzd., 1954. -90s. a Ill.
22sm. 101000 Ekz. 1r 45k-(55-1471)p 635.9(47.,093)
SO: Knizhnaya, letoPis, VOL lp 1955

SVYATNENKO, N.I.
Formation of ship claes and type designations in the English
language. Trudy LKI no.28:95-106 159. (MIRA 15:5)
1. KafedrIL inostrannyll yazykov Leningradskogo korablestroitell-
nogo instJ.tuta.
(Ships-Terminology) (English language-Etymology)

MUKHIN, Petr Vasillyevich; BUTENKO, Dmitriy Borisovich;
SVYATNMO.Vasi.liy Filippovich, YMIIAK, Viktor Ivanovich;
GOLOSHCHAPOV, I.M., inzh.-polkovnik, red.; SOKOLOVA, G.F.,
tekhn. red.
(K-750V motorCyClE,; its construction, maintenance and opera-
tion] Mototsikl K-750V; ustroistvo, ukhod i ekspluatatsiia.
Moskva, Voenizdat:, 1963. 225 P. (MIRA 17:1)
(Motorcycles)

S/121/62/000/002/003/004
D040/D113
AUTHOR: __~vyatnyy, !.I.
TITLE: New automatic regulation devices
PERIODICAL: Stan.,ci i inctrurient, no. 2, 1962, 43-44
TEXT: The design and operational principles of four now autoi-,tiatic reCulati,)n
systems for grind~-ng machines developed at the Sibz--vod are describod. Thc-
devices measure the diameter of the shaft or bore being oround, and can auto-
--la.'-4cally stoT) the grinding process and retract the grind-rig head when the
req-uired diameter is reached. Three of the devices are equipped with pneu-
7.atic feelers produced by the zavod "Kalibr" ~Kalibrl' Plant). The first of
includes an electric bulb and an f(fK-1 (PSK-1) photoconductor. A
float, in a- vertical pipe interrupts the light, bea-.-. at the moment mhen the
commiand has to be given. Two relays are used for switchinrr on a magnet that
s--4tches Cie valve in the hydraulic system, or actuates the control handle Of
th'e grindinp~.- machine. The second device has a :44.crometir-ic scre-a closing the
orifice of the hydraulic nozzle )when the required work diameter is reached.
Card 1/2

LIVINTSEV, A.G.;_..gVYATNYYI V
Studying the dynxunics of the nydraulic system of a den-gitometer
for measuting coal pulp density on a 11,11"T-7 electz*nic computer.
Ugoll 39 no.2:47-49 F 164, (MIRA 17:3)
1. Donetskiy politekhnichoskiy inotitut.

LIVRITSEV, A.G., Inzho; inzh.
Investigating the dynamics of a flowmeter measuring system using
an electronic computer. Izve vyse ucheb* zave; gore zhurs no*8:
143-147 164 (~fflu 18:1)
1. Donetskly politekhn-*-,heskly institute Rekmmdovana kafedroy
obogashcheniya polezn7kh iskopayemyk-h.

ALEKSANDROV, G.V. (Moskva),- SVYATODUM~ V.K. (Moskva)
Controlled motions of winged flying craft,of various systems in
a plane of symetry. Inzh. zhur. 3 no.li-3.11 $63. (MM 16t1O)
(Aerohiutics) (Aircraft-Dynamics)

E,-.-I -'al 1V 1
17"
ne r7-~ -jz
Ti-.e eq
of motion for a c,-Uciform wicked rclcksC in cylindrical
a 3-,~Tvexi
undar
r -r --a -Z Vx 3J~y equatiGns are
tta --hange In the pra~ac-
car,.L,,:~-Of--mass Valcctt7 tile x-a-x~~F ar,7,A ar rotation -a'.a
L
;.r. 1 a C, f d -a

M7.31 -A16 61 - M'W"
M,,= M~"'W. m 6"
see n e o su re; ~he c-ondition