SCIENTIFIC ABSTRACT SHUTOV, I.A. - SHUTOV, V.D.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R001550310015-0
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: August 31, 2001
• Sequence Number: 15
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

32043. sijurrov, 1. A. Trlaklioma
1411"di naselenif-i't Korf-akskogo nai-sional'
110(r0 Okniga KannIchalskol ohlasti; po
I*Cztll't,,Il.-Illli)I)Sle(l()N".Ijlil-llI 19-Isg. (Nrest-
nik oficalmologii, May-June [951. %-. 30,
X-N-p. :3. 1). 30 -131) Tille tr.: Trachoma
mong the population of tho Noryak
National District ()f Kamchatka Oblast,;
-tC(,oj-(jjIjg 1() I-CS111ts of 1.11(t l!)-18 jjjN,(-sJ.j,ra-
io It.
("Ontabis .1t report on ,I mass survev,
tInd indoctrination, lor,"'ellier
willi data on the geography, populati oll
and economics of the area. Resilits or
iliv survey, im-olvingr .5,396 jwm~ons-.,
lar,gely Russians, but also some 500
Norvaks and 1,000 Ttelmens, are pre-
sentl0d. Incidence of the. di-Sease NNas
found highesi antong Korvaks ', nex! in
Itelluells) least among Russians. Data
C/ 'Ira C, P
ct., Eye-
M T~j S v

it I k 4-1 a I mid(wi I. tv .111 it(, 1 !1.5
vyr). :3, p., 31) -3 1 7 'i I 1e I r. Trac I io n ta
limlig 1-he polmlati,)n tif 11to Noryak
Natioual Dist,rivi ()f 1~amchfdka
I 161~(iillg to result.,; ()f the HHs illvesli"'tel-
ioll.
('0111(lilis a 1*(!])()I't ml "I Illass survey,
tilerapy, aild illdmd rillatioll, togel 1wr
NVIIII data ml I'lle geography, p(q)tIlat,ioll
.III([ eummillies of the area. Rvsillts of
I lie sl Irveyy ill volvilig 5,396 1) v o 1 Is,
larvehr 101.1-;sIalls) ])III, also some 500
Koryaks and 1,000 Delitiens, are pre-
svilt-ed. 111cidem'-w ()f flic dkeasv Ivas
found highest allmllg next ill
Itchnellsy least. alliolig R-lissians. Data
are givell mt degrees ()f afflictioll" lit"Iss
I lie rapel I I i cmeasures, instruction ()f
local medical persmillel and of population.
COPY Seen : DSG.

O,W
S/148/61/000/007/009/012
E193/E38o
AUTHORS: Zamyatnin, M.M. and Shutov, I.A.
TITLE,,, The effect of heat treatment on the behaviour of
steel 3yrl (3kp) at sub-zero temperatures
PERIODICAL: Izvestiya vysshikh uchebnykli zavedeniyi Chernaya
metallurgiya, no. 7, 1961, pp. 142 - 148
TEXT. Hot-rolled steel 3kp is a useful constructional
material owing to its high ductility, good weldability and
relatively low price. The field of application of this
material, however, is limited by its relatively low static and
itapact strength at sub-zero temperatures and by its tendency
to age-harden and fall by brittle fracture. This often
necessitates its replacement by a more expensive low-alloy
constructional steel and the object of the present investigation
was to establish whether the desirable combination of properties
can be imparted to steel 3kp by a suitable heat-treatment. To
this end, tensile tests were carried out on both standard and
notched test pieces, as well as transverse bending tests on
notched bars and impact strength tests at temperatures ranging
Card 1/7

20)o68 s/i48/61/000/007/009/012
The effect of heat treatment .... E193/E38o
from +20 to -200 OC on small (6 mm in diameter) specimens (1)
in the hot-rolled condition, (2 quenched from 900 0C and
terapered for 45 minutes at 600 C and (3) quenched from 900 C
and tempered for 45 minutes at 20~ 0C (the condition of specimens
is described by these numerals in Figs. 1, 2 and 5). The steel
studied contained 0.15110 C, 0.42,0 Mn and traces of Si. When
notched bars were used, the notch (600, 0.5 nun deep, 0.1 mm root
radius) was situated either in the centre of the test piece or
itear its head. In some cases, the tensile load 'was applied
t.o notched test pieces not axially but at an angle of 0.
Benzene (cooled by solid CO . or liquid nitrogen) or liquid
nitrogen was used as the cooling media. The results are
2
reproduced graphically. In Fig. 1, the VTS (Cb , kg/=l ,continuous
2
Curve) and yield point (6T$ kg/mM broken curve) are plotted
against the test temperature (oC) in Fig. 2. elongation
(6: 0/" - continuous curves) and reduction of area broken
curves) are plotted against the test temperature C). The
Cai-d 2/-,

28o68
5/148/61/000/007/009/012
Tile effect of heat treatment .... E193/E38o
breaking load (P, kg, lefthand scale, broken curves) and
deflection (F, mm, righthand scale, continuous curves) in 0
transverse bending, are plotted against the temperature C
in Fig. 5. The results obtained can be summarised as follows.
The UTS and the yield point of steel 3kp both in the hot-rolled
and heat-treated condition, determined on standard test pieces,
increased rapidly with decreasing temperature. The difference
between the strength of hot-rolled and heat-treatment material
remains practically the same throughout the temperature range
studied. Elongation and reduction in area remain practically
constant down to -120 OC, after which they gradually decrease.
Whereas, however, in the case of hot-rolle material both 6
and ~-Y decrease almost to zero at -196 01, the heat-treated
steel (quenched from 900 OC and tempered at 600 OC) still
retains at this temperature a certain degree of ductility,
characterised by 6 = 14?,~. and %Y= 450%. The notched test pieces,
inclined at 120 to the direction of the applied load, lose their
ductility at relatively higher temperatures, the decrease in
6 and UTS beginning at -60 and -120 0C, respectively. The
Card 3/7

21063
s/148/61/000/007/009/012
The effect of heat treatment .... E193/13380
bending tests yielded similar result- The marked decrease in
the transverse bending strength found on hot-rolled material
at -60 OC was not observed in the heat-treated specimens until
a temperature of -100 oC was reached. Tile effect of heat-
treatment was, however, most striking in the impact tests. Where-
as the impact strength of hot-rolled material decreased rapidly
in the +10 to -30 OC range, the heat-treated specimens had a
considerable impact strength (4-5-7.5 kgm/cm 2 ) even at -60 OC.
It was concluded that heat-treated steel 3kp can be used as a
material of construction for critical parts, operating at sub-
zero temperatures and under complex stress conditions.
I.V. Kudryavtsev, M.V. Pridantsev and K.V. Popov are mentioned
in the article.
There are 5 figures, 1 table and 4 Soviet references.
ASSOCIATION: Leningradskiy teklinologicheskly institut
kholodillnoy promyshlennosti (Leningrad
Technological Institute of the Refrigeration
Industry)
SUBMITTED., October 27, 196o
Card 4/7

AUTHORS:
TITLE:
S/149/62 0 004/003/003
AOO6/A10l
Zamyatnin, M. M., Tsukanov, V. A,, Tomilov, M. Ye.,-Shutov, .1. A.__-'
The effect of low temperatures upon the mechanical properties of
alloys DT 3 (VT3),BT 5 (VT5), and grade 40 XC (4OKhS) steel
PE-RIODICAL: Izvestiya vysshikh uchebnykh zavedeniy,'Tsvetnaya metallurgiya,
no. 4, 19062, 152 - 156
TEXT: The mechanical properties of titanium alloys and improved allowed
steel were investigated by comparison tests at temperatures from +20 to -60 C,
itanium
Zn order to reveal the possibility of replacing high-strength steels by t
a"loys. Smooth and notched specimens were subjected to static tensile and bending
tests, skew and impact tests. It was found that the properties of VT5 and, in
Part.-cular, VT3 titanium alloys approach those of 40 KhS steel at all the test
temperatures. The proneness of titanium alloys to reduced ductility and plasticity
at low temperatures is somewhat greater than for improved steel; it islower in
impact tests. The results obtained show that titanium alloy parts can be success-
fully used at temperatures down to -60 0 C. There are 4 figures and 2 tables.
Card 1/2

The effect of low temperatures upon the...
m
S/ I 49/62/OW/00V00,3/W 3
A006IA101
AS-"OCIATION: Leningradskiy teki-mologicheddy instiltut kholodil'noy pronrjshlennosti
(Leningrad Technological Institute of the Refrigeration Industry)
Severo-Zapadnyy zaochnyy politekhnicheskiy institut (North-West
Correspondence Polytechnic Institute)
S U a". MPL-D: Jmuar-j 22, 1962
Card 2,12

L 107g=6
.3 E~R/F.PF(c)/7"(~)/EU(q -/E~T(T)/BM-A"W/ASD-Ps-h/
Pr-4--;-W/JD
ACCESSION NR: AP3002902 8/53/066/000/0153/0155
S/014
Y4i~
AUTHOR: Zamntnin, M. M..: Zh~lcbo~. V. V. Togmilov, M. Shutov 1. A.
'titanium and
TITLE: Effect of low temperature-on mechanical properties of
its alloys
'T,
SOURCE: IVUZ. Chernaya metallurglya, no, 0, 1963,.153-156
TOPIC TAGS: titanium. titanium alloys, mechanical properties, subkzero
temperatures
ABSTRACT- Because of insufficienc of available data, an- invest*tion -was
made of the mechanical. properties of the VT.1-1. ~ and Vtl-2 commercial-
grade titanium -and . titanium alloysW34-10. 0- 2. 0% Mo. 1. 50 _-2. 50fo Cr,
5- 6. 2% Al), VT5 (4- 5. 5% Al), OT4 (1. 0- 2. 0% Mn. 2. 0 -3. 5% Al) at,
temperatures ranging from 20 down to -196C.'~ Results of the tests ai-e shown
in Table I of the Enclosure. Org. art. 'has: 2 tables.
ASS: Leningrad Technology Inst. of the Refraction Industry. All-Union Alurd-r=-
Magnesium Instiktute
CWd

GREKOV, N.A., inzh.; ZAMYATNIN, M.M., kand. tekhn. nauk; ZIKEYEVA, T.F.,
inzh.; TOMILOV, M.Ye., inzh.; SHUTOV, I.A., inzh.
Effect of temperature on the mechanical properties of soft
solders and copper compounds soldered by them. Vest. elektro-
prom. 34 no.7:59-63 J1 163. (MIRA 16:8)

_(b z
v
L61035-65 EWT(d)/Ei~(Im)/60 hWA(6)A''*- )AAwtv
k)
Ewt D)/EWA(c) Pf-4 MJ-*/JD/~(0W1/4
A C ENS I N' /0137/65/000/9061BOWE0111
C 8 ON R: AR6017429 UR
'6E75
VBOURCE: Re.f. zh. Metallurglya, Abo.
AUTHOR: Fedorov, 'A,.K Shutov* I A 43.
4
pe rtie of -butt welds,
TITLE: The effect oflow tern ratures on the mechanical ]2rope
in steel tubes welded Vy Induction heating with high frequency~ 6urrents
CITED SOURCE: Tr. Vses.. n. -i. in-ta tokov vysokoy chastoty, 5, 1964,
43-50
0
TOPIC TAGS: butt welding, pipe,. low temperature effect, solid mechanical pr
t~,~ steel, induction welding, weld hea t treatment, 10 steel, 20 steel
.AAMLATION: Mecl)anical tests of butt welds~ in tubes with a diameter of.38 X
3
9 mm made of steel 10, -and 32 x 26 mm made of steel 20, welded with high fre
quency currents, vi6re carried out on elongation and static bending on an IM-4A;.-
nm 3
achine-in a special apparatus. Impact bending tests were made on an.bM-30
and toughness of butt joints in
-4pendulum drop ham'mer, The strengths ductility
tubes made of steel 10 d steel 20, elded by induction heating with high frequen
Card

DOLIN., P.A.; KHAVIN,, N.Z.; SHUTGVj. I.G.; VCRONIN, K.P., tek"red.
[Collection of regulations in industrial bygienel Sbornik
deistvuiushchikh pravil. po tekhnike bezopasnosti. lzd.3.v
peresm. i dop. Moskva, Goo.energ.izd-vo. Vol.2. 1962. 480 P.
(KERA 15:5)
(Industrial hygiene-Laws and legislation)
i

SHUTOV, I.. cinleii.
fla-.s dissemination of -oractices in the construction of the Kax'diovka Hydro-
electric Power Station. Frof.soiuzy 8 no-8:31-30' Ag '53. (MMA 6:8)
1. Prezidium TUentrallnogo komiteta profso-yuza raboL.Iikh elektrostuntsiy i
elektroprouWahlennouti.
(Technical education) (Kakhovka kydroelectric power station)

DOLIN, P.A.; IDIAVIN. V.2.; SHLITOT, I.Q.; SKVORTSOV- I.M.. tekhnichankly
redaktor. Awmml?
(Collection of safety eng1nearing rules now In force] Sbornik
deletvulashchikh prayll po tekhmike besopasnostl. 1s4. 2-3
peresm. I dop. Sostavill P.A. Dolin. N.2. Mavin. I.0. Shutov.
Moskva. Goo. energ. Isd-vo 1955. 696 p. (Mm" 918)
1. Russia (1923- U.S.S.R.) Ministeretvo elektrostantall.
(Safety onginserIM)

SHUTOV, I. *AWA--
T~e hourly bonus wage system for the repair of equipment In
eitctric power stations and net. Sots.trud. no.1:117-119 Ja
'57. (MLU 10:4)
(Mlectric power plants-Squipment and supplies-RepatrIng)

DOLB, P.A.; ENAVIII, N.Z.; SHUTOV, I.G.; VORONIN, K.P.., tekhn. red.
(collection of safety engineering regulations] Sbornik deistvuiu-
shchikh pravil po tekhnike bezopasnosti. Izd.3., peresm. i dop.
Moskva, Gos.energ.izd-vo. Vol.l. 1961. 751 p. (MIRA 14:12)
(Electric power plants-Safety measures)
(Electric power distribution-Safety measures)

L 31977-66 EWT (d ) _-N-6-676-6-i -_ -
ACC NRi AP6010786 SOURCE COD& UR/0106/66j /0009/0022
AUTHOR: lontov, L. Ye.; Lyubimtsev, A. A.; Shutov, 1. 1. 61
ORG: none
TITLE: Multipurpose equipment for multichannel multiplex systems for cable and
radio-relay lines 4
SOURCE: Elektrosvyazt, no. 2, 1966, 9-22
TOPIC TAGS: multiplex, multichannel communication, radio relay . FP. r 4VveA.' C
CeA.'VICIC-516A) 9 CS('14 X,9 7-,,OAJ
ABSTRACT: The development of multipurpose oscillator and frequency-conversion
equipment for multiplex communication systems is reported; the equipment is mounted
in cabinets with swing-out frames; it can operate within 410 +40C. Supply-voltages
required: 220 v � 30 ac; -21.2 v 2: 3% dc for transistors; -24 v:! 10% dc for signal
circuits; +206 v� Y16 de for anode circuits. The oscillator equipment is suitable
for Soviet-made K-21-2, K-60, K-60P, K-1920, R-600 systems; the frequency-conversion
equipment can be used in K-60P, K-300, K-1920, R-600 systems. The oscillator cabinet
generates a number of carrier frequencies (among them 120 kc for 12--108 ke linear
spectrum and 564 ke for 12--252 spectrum), 64, 84 '- 104, and 412 kc monitoring
frequencies, etc. Block diagrams of some oscillator units are shown.- The frequency-
conversion equipment is based on standard 12-, 60-, and 300-channel trunks which use
1/2 UDC, 621.395.

fi 74 4-tL I'--)

S"UTOVI I. "".
Shutov, 1. V. -- "Chemicals in the bight against Undesirable leloody Plants
in ~orest:~,,." Min Agriculture USSP. All-Union Order of Lenin Acaderay of A-
gricultural Sciences imeni V. I. Lenin. All-Union Sci Res Inst of Blant Con-
servation. Leningrad, 1956. (Disseration For the L)e,.-ree of Candidate in
Agricultural Sciences).
Fc: Knizh2~~Za Letopis', No. 11, 1956, pp 101-1111

fit
Oy L,
er t e a t
A -n - s n -a rn
S -. .1 i a an a I
il' .-i n L 011-1 3pj,- i e d o d i um
5i
ut.
it tiie ra t io o r a n t'-, "For t;ox"
f T
j.n dclee of 2 kA/ha. alld hi~aier

Sc-,. 20592
TITLE
fA
AJBSTRACT caused complete drying up of the leaves in all
speciesof willow.within 2 months. Oak, elas,
Tatarian maple, blackthorn and buckthorn were
highly resistant. In treatment with eaters of
2,4-D and 2,4,5-T the rate of liquid in spray-
ing, 100 liters per hectare, proved fully ade-
quate. 2-5 in a done of 4 kg/ha. caufted 70%
of tile willow to die. 1 significantly yielded
to them in effectiveness. 3 worked consider-
ably stro-ager on black poplar than did 2.
2/3

BELIKOV, V.P., kand.biol.nalik; SHUTOV, I.T., kand. eel I skokhozyaytj tvannykh nauk
New book on chemical weed control ("Chemical weed control in forestry"
by N.H.Dekatova. Reviewed by V.P.Ballkov. I.V.Shutov). Zashch. ,
rust.ot vred.i bol. 4 n0-3:61 Ny-Je 159. (MMh 13:4)
(Weed control) - (Forests and forestry)
(Dskatovao IF.B. )

VILICHKO, Ya.M., inzh.; SIIJTOV, I.V-, kand.sellskokhozyaystvennykh, nauk
Using arboricides In removing trees and bruebwood from
the areas to be inundated. Gidr.stroi. 30 no-7:35-38
J1 160. (KIRA 13*-7)
(Herbicides) 0,0droelectric power stations)

BELIKOV, V.P.; SHUTO I.V.
- 7-1--Y-
Batching vessel of the ORP-G sprayer for small-stse lots.
Zashch. rant. ot vred. i bol. 6 no.9:19 9 '61. NM 16SO
(Spraying and dusting equipment)

SEMEYEEVA., T.A.; SHAMAYEV., G.P., inzh.; SAMIN, P.A.; aHUjQY,--I.V_., kand
sellskokhoz.nauk; KALASHNIKOV, K.Ya., kand.sellskokhoz.nauk
Questions and answers. Zashch.rast.ot vred.i bol. 7
no-5;16, 41-43 MY 162. (MIRA 15:11)
1. Nauchno-lasledovateliskiy institut po udobreniyam i insektofungi-
sidam imeni Ya.V.Swnoylova (for Sorgeyeva). 2. Nauchno-issledovatel.1-
skiy institut lesnogo khozyaystva (for Samgin, Shutov). 3. Pushkinskaya
baza Vsesoyuznogo instituta zashchity rasteniy (for Kalashnikov).
(Plants, Protection of)

NIKIFOROV, I.; MAKAROV, A.; S14OLYAKOV, N.; SIPER, E.; YMILA, V.; LARIN, M.;
FILIPPOV, K.; TOKMAKOV, V.; BARANOVSKIY, V.; CHETWERIKOV, K.;
POZNANSKIY, A.; SHUTOV, M.; ROZENFELID, L.; RUD', A.
Mechanization of waterproofing operations. Stroitell 8 no.11:
15-20 N 162. (MIRA 16:1)
(Waterproofing~--Equipment and supplies)

SHUTOV,,_L4,., podpoJkovz--Lk
Chemica.1 warfare weapon and defense against it. Voen.znan, 38
no.5J5-36 Ry 162. (14IRA 15 -.5)
(Chemical warfare---Safety measures)

- ~ - 7 ~ .. ~ 1-1-11 1) ~17U 17J -- .
I - - I ;I . 17.
"Gegenwfli-t1ge Lage (lei, E'ntwicPJ.u%,fstendenzen im Bait analytislicer Gerlite"
report presented at the 17 ~7
Intl. Measurements Conference (DIEKO) Budapest, 24-"~O November-1%0

_T_
V.A. "tax A.C.. SItakit,
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TnLJt, mesa Sp. treft,ster for th; An:ly*i.
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voltage. , ,.Srkd,. kpt. at a
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Th. PoW-r C:---pd by ;he c.th.d d&4 not exceed 0
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COI ta.-An.1yj. Of %h.
Ionic and Nalecul" Couposition of tae Upper Layers of the
At.aapbar.
The Inatmeent has the rallow&ng chavacteristXca;
1. Ms. ~%M4. 1) 1 A. Z11 12 56
2. 9".Lattoa (Vall, vidsh
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3- Smac. or workis& pr.4--r--
in the aftelyoor -410-6
came of the massaluaLtak:r 10
41. Partlal se"Itavtty in the
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$1. sawtimath-valt4g* generator (PXZ. 6). I-Ithi.x
&Avc-4t,(F&t. 7) ad DC to .. rt.r (F.&. 8). Th... circuit.
ar:,p:r,tly trAn ri..4 eapL Oy Ln.L.t%rja*d '..op,.n.nt.
r .:ad. t we to
Id-. 1. , . AL tn. L.p I
b ' ': '.. .., ."!. t
ad t with he supply voltage ch
by : 10% Th. .... foods %at* the tolematric
-Yet - t~. C.Llawtz data,
le 1* 11 the Outputs of the ton current seplifier
rV,o
2) high-frvquency voltage;
3) curroat Or the cathode In tn* Lon source, and
41) P Y wattage (27.5 V).
Card 6/7
ll:t~,*al :.Oroalh!:U~t yp*c were used an rocket. to study
ShLan , I a,r "PO.Ltion of the atmosphere.
There or. 8 figures and !$ roforvnc*si 2 Sov&et and
5 V.&II.b.
&SSOCIATION: SP~t-i-Va-y. k-natruktarokoyo by-uro
&M,411tichookogo prtbomtrayonLya
(SP*Cisl Design 5-..u rer Amalytic.1
XNA"WAMOUt construction)
SUMUTT10% Octabor 15, 1939

SFUTOV) 1M. D. and PAWEN'EO, V. A.
l'I)ie Modernen Analytishen Mesegerate."
-T report presented at the 2nd Intl. Mleasurements and Instruments Conference
(IMEKO), Budapest, 2,9 June - 1 July 1961.

PAVLFJIKO,- V. A.; OMMOV, L. N.; RAFALISON, A. E.; ~~WTOV, M. D.
Experimental-production operation of the MQ0201 automatic
regulating maas-"ctromster. Zav. lab. 28 no.12:1525-1526
962. (MIRA 16:1)
1. Spetsiallnoye konBtruktorskoye byuro analiticheskogo
priborostroyeniya AN SSSR.
(spectrometer)

~ACCESSION NRO---AP4063737 S/0293/6j/001/002/U87/0Y95!
'AUTHOR: 'Pavlenko, V. A.; Rafallson, A. E.; Shutov; M, D,
,TITLE: Series,of small-scale mass spectrometers fqr*the study of
.ineutral and ionized games of the upper layers of.th.e atmosphere.
SOURCEt "Kosmicheskiye issledovaniya, Vii I., no. 2, 1963, 287-295
!TOPIC TAGSt mass spectrometer, radio frequency masa 'spectroo eter
Inonmagnetic mass spectrometer, MKh640l mass spectrometer,MKh6403 mass
I spectrometer, MKh6405 mass spectrometeX,,.Mpper atmosphere
!:ABSTRACT: The-MKh6401, MKh6403-i.-and MKh6405 m`& term (ba d:
:on.'the Befinet model) have been redisigne *d.The MKh640l.mass spectrom to' r
!is used for analyzing the -molecular and.16nic compositions of gases in
ia.mass ra ge of.1-4 and 12-56 amu. It clonsists of a miniaturized
1fiv %nalyzer with grid distances fixed by met.allic cylinders.
A beam of slow electrons emitted by a red~lhot c.ath.ode ionizes the gas a.
The analyser, with the ion source weigh's 2.1.kg 'and is filled with
i no
imixture of-hydrogen, helium, argo , and-neon at a pressure of 10-5mm HS.'
!The MKh6403 mass spectrometer-lidenticalin-range to that of the MKh6401, it'
'Card 1/3

-j

SION NRt AP406i737
perm
d
to automatic r Iange shifting. The' 'analyzer, the., ton source, an
Ithe on collector are located in a common metallic qase. In this-mode.1
'
e

iall .
#'form-:of. highly
transparent
of the ion source are In'the
he elements
d1
ri The iccelerationvoltage ii from-'70 to 380..'v,. and the frequency
'The MKh6405.nass spectrometer
autoviatically shifts from 30 to 8.6 Md. ' .0
.
which contains the basic elements of the MKh6403,.i --considerably more
analysts of gages
sens'itive than the MKh6403 and to suitable for the
.
contai*ning Ionized and neutral particles of i-r-Van.4 1.2-36 amu. All
three mass' spectrometers can work at temperatures iinging from-40 to
ties and are able to withstand considerable
+40C at low and high humidi
amouits of mechanical overloading. Durinj obsirvations, made with-the
pictrometers on 22 June 1959, at altitudes of 90-211 km, the
mas
pre ce of the following tons was recorded: 0+, H'O-R-" NO+@ 0 +0 For;
:,:
9 2
2
.
pqses of analyzing the.neutral components of the. upper.atmosphere,
pur
.
higher than 100 km, where the
iobs'ervations were performed at altitudes
.
presence of the following were revealed:'H, H N, 01, OH, 1120, N2,., -
2, A
Ar, C02. and N20- Orig. art. has: 6 -formulas,-7 figures,.and
0 2
l..table.
L

I Coid 2/3,

L 15688-65 E.7T(d) Po-4/Pq-'f/Pg-4/Pk-4/P1-4 ASD-3/,1,FFTC/ESD-3/APGC
ACCESSION NR: AP4047481 S/OIZO/64/000/005/015710161
40
AUTHOR: Levina, L. Ye.; Men'shikov, M. I ; Pavlenko, V. A.; Rabinovich,
1. S.; Rafal'son, A. E.; Tsy*rnberov, M. Ya.; Shutov, M. D.
TITLE: New MKh 1101 mass -spectrometric leak detecto
SOURCE: Pribory* i tekhnika eksperimenta, no. 5, 1964, 157-161
TOPIC TAGS; leak detector, mass spectrometric leak detector I )AKh 110 1
leak detector
ABSTRACT: The new MKh 1101 leak detector differs from previous types
(PTI-4a and PTI-6) in that, it has no oil-vapor pump, uses an oxidation-resistant
cathode. and is calibrated by a reference diffusion-type helium leak. Two lobar
rotary (Roots) pumps driven by a single motor provide the rough and fine
vacuums; the equilibrium vacuum is (2-5)x 10-4 torr. The cathode is stable in
operation at pressures up to I torr. The leak detector sensitivity is (1 -5) z IV
CWd 112

L 15638-65
ACCESSION NR: AP4047481
lmc/sec for helium and 5x 10-4 lms/sec for hydrogen. Setting the detector in
operation takes only 10 minutes. Orig. art. has: 6 figures.
ASSOCIATION; SKB Analiticheakogo priborostroyeniya AN SSSR (Special Design
Office for Analytical Inaruments, AN 555R)
SUBMITTED: 03Jun63 ENCL: 00
SUB CODE:IM NO REF SOV: 002 OTHER: 000
i card z/Z

tV
L7L_ J/FjML _U1 jQ V
ACTTA_,k_j"i70'015(3O SOURCE' CODE: Ul?/0120/65/000/006/0130/0135
AUTHOR: Tallroze, V. L.; Pavlenk V A
K_pj__
Grishin,_V. D.; Ozerov, L. N.; irill
ORG: Institute of Chemical Physics of AN SSSR, Moscow (Institut,
khimicheskoy flziki)
f0
TITLE: MKh1307 Ahromato -mass -spectrometer (Khromass-2)
SOURCE: Pribory I tekhnika sksperimenta, no. 6, 1965, 130-135
1
TOPIC TAGS: chromatography, mass spectr ometer
7,1
P-3
ABSTRMT: The design and operation of IAM1307 mass -spectrometer is
described. This spectrometer is formed by combining a chromatograph
with a two-beam magnetic mass-spectrometer. A laboratory version of
Khromass-2 spectrometer served as a prototype for LIM307 type. The
arrange*mont of VkhI307 chromato-mass-spectrometer is schematically
shown on Card 2/2. The chromatograph (1) Is connected via a dose-valve
(2) to the ion-source-(3) of th: n~ass-svectrometer which Is equipped
with two large (4 and 5) and tw small 0 and 7) collectors. By using
a switch (8) the collectors can be connected to a set of two electro-
meter amplifiers (9)* Double ion currents are automatically recorded
-Card 1/3 UDC: 543.51t543.544

T. 9771,q-66
ACC NRt AP6001560
t
ED F652
'M
j
7
Card 2/3
by an electronic potentiometer (10).
The Ion source was fed from an elee-
tonic circuit (11). The small coll-
ectors were used for measurements of
two mass-spectral lined while the
large ones collected the intensities
of two line groups. The spectral
peaks were measured for each of two
measuring channels and their heights
were compared. The peak ratio was
used for dofining tested substances.,
The design of chromatograph was ill
ustrated and described. it con be
equipped either with capillary or
packed columns. The ion system con-
sisting of ion source, mass analyzer
and ion collectors, was also.descri-
bed and diagrammatically represented
The ion source was placed in-the
magnetic field of a mass-analyzer.
A permanent magnet of about 6000
gausses was used. The resolving
power of the mass-speotrometer was

__I~_ ?770-66-
ACC NR, AP6001580
l
about 50. The ion collectors were designed for a simultaneous measure-
ment of two spectral lin6s differing in masses from 4 to GI,'I. A simul-
taneous recording was also provided for two groups of lines including
one group of 34 to 45 amu and the second of 48 to 100 amu. The electro-
nic circuit feeding the ion source was designed for cathode currents up
to 2 ma, accelerating voltages of 300 to 1200 v and ionizing voltages
of 50 to 100 v. The vacuum systemiwas also described and the 19M1307
apparatus was shown in a photo. Some results of measurements were sum-
marized in a table. A high sensitivity of the M1307.3peotrometer
permits defining the mixtures with contents up to 10-4%. Orig. art.
has: *5 figures.
SUB CODZ: 20 / SUBM DATZ: 50otG4 / ORIG RSF: 010 OTH REF: 006

FAVLEtfKO, V.A.; RAFALISON, A.E.; TSYMMFO'I, M.Ya.,; SHUTOV, M.D.
The M 1102 high-sensitivity maS3-Sp8CtrnmFtric. leak
detector. Prib. i tekh.eksp. 10 no.5.,196-194 S-0 165.
(MIRA 19.-1)
1. SpetRiallnoye byuro analliticheskogo pribo-
A'S 51"ISR, Len-ingrad. Suldi~41-',sd Sept.19, 1964.

GORBUROV, I.P.; GLUKHOV, Y.P.; KOTLUKOV. K.G.; MOSICALEV, V.D.: SIPIYLOV.
Tu.A.; S"TAN, N.I.; S=OV, K.I.; BTKOV, S.G., red.; KANZVSKAYA,
M.D., red.; BLAZILWKO .1..--E-ekhn.red.
[Training methods for members of civil air defense groups) Note-
dike podgotovki lichnogo sostava grupp samozashchity. Koskva,
Izd-vo DOSAAF. 1959. 165 P. (MIRA 13:3)
1. Vsesoyuznoye dobrovollnoye obahchestvo sodeyetviya armii.
aviateii i flotu.
(Air defenses)

SHUTOV., N.
IkLsburse social insurance?funds correctly. Okhr. truds, i sots.
strakh. 4 no.6:33-34 Je 161. (MIRA .14:7)
1. Starshiy instruktor otdola Visenoyusnogo teentralinogo soveta
professionallnykh soyuzov po gonudarstwennowu ectsiallnmu
strakhovaniyue
(Inmu-ance, Social)

SHUTTOV, N.G., kandidat tekhnichaskikh nim, , dotsent.
~--
Regulating and testing engines on-*hips under operating coaditiew.
Trudy GIIVT n0-13:157-175 1559 (MTRA 10:1)
(Karim engines-Testing)
~ S

STUWYA, Anna Yedorovna; k, ~ ROj -, A ~ 4 4 Y~ ; x v i pi ~vc, 4~
CLeading poultry farmers] Peredovye ptitnevody. [Gorlkii]
GorIkovskoe kn-vo. 1954. 36 p. (MLIA 9:10)
(Poultry)

ACC INR: AN76008100 SOURCE CODE': UR/9008/GG/000/06310002/0002
IiUTI-1011: Shutov P CNI a j o rGeneral of Artillelry, Hero of the Soviet Union)
013.G: none
TITLE: Training of antiaircraft missilemen at a missile firing range
SOURCE: Krasnaya zvezda, 17 Mar 66, p. 2, col. 1-4
TOPIC TAGS: antiaircraft unit, missile subunit, guided missile training,
training area, firing range, aerial target, supersonic target
ABSTRACT: The aut'nor analyzes problems of organizing and carrying out
simulated coi-nbat firing exercises of antiaircraft missile subunits acrainst small
sl rial targets flying at all altitudes, and under conditions of jamming.
upersonic ae
Xlissilemun can obtain a complete understanding of a modern combat only during
training exercises at a missile firing range where theory and practice are com-
bined. The antiaircraft missile firing range, in the author' s opinion, is really a
Missile academy. Shortcomings in combat firing and tactical training of some

ACC PIR: A N 6 0 0 6 100
ant;aircraft missile subunits are examined. Methods of rating combat firing
exercises are discussed. [NTJ
SUB CODE: 15/ SUBMI DATE: none/
c.,d 2 2

SIMIC', , F. A.
26566 Listovoye chrenkovaniye dekorativrorkh porod. Trudy azarbaydzh. Nauch-issled,
In-ta mnogolet, Nasazlideniy, T. 1., 1949, s. 63-66.
30: IZTOPISI NO. 35, 1949

1. SHUTOV, P. A.
2. US71R (6oo)
4. Water Lilies - Azerbaijan
7. Victoria in AzerbaiJan. Priroda 41 no. 12, 1952
9. Monthly List of Russian Accessions, Library of Congress, March 1953, Unclassified.

'1 1. - . ,
'~Iel' I -- , I I - . il i_ 'C "' "- - , n- ~.;.! Q -~ -.; L7 -1, -~.- - -'~,2.
, -, ~. ~; LL ~. ~ ~ .' -; "' J' ' '~ 4! - ,
11Z 4 11 ~ I -I I ! I " I - )
in,7~ n " 1- F , - " , -, ,I - , - I : . --, " - ,'.1 - , - ~ 4.
-.-- ., - , 2.nmnial 3
: SLu- 432, 29 I-a-, 51~,

SHRITOV, P.A.;ALEKPkMOVA, S.G.
Bay laurel milture in Azer&-iijan. Iz,.r. AF Azerb. SSR. Ser.biol.
i med.nauk no.7325-32 161. NIRA 16:7)
(AZERBAIJAN-LAUREL)

~HUTO~V,J.K.3 ROTENBW ,, I.P.; YESIPOV, G.Z.
Produetion of water-soluble low-phenol phenol--aldehyde resins usi~a
semicoke phenolates as a phenolic raw material. Plast.mg sy no.11:
57-58 161. (MIRA 14--5)
(Phenol concentration products)

SMOV, Petr Vladimirovich; SYNORTSOV, V.P., red.; IVANOVA, A.G., takhn.red.
[Mining equipment and machinery] Gornoprokhodcheskoe oborudovanie
i raekhanizmy. Moskva, Goo.nnuchno-tekhn.izd-vo lit-ry po gaol. i
okhrane nedr, 1959. 399 P. (MIRA 12:12)
(Mining engineering-Equipment and supplies)
(Mining machinery)

SlIvrovi F.V., general-mayor artillerii, Geroy Sovetskogo Soyuza
On the threshold of the now academic year. Vest.protivovoJ.obor.
no.12:10-13 D 161. (MIU 15:3)
(Mlitaxy education)

TASLrf6KIY,, IA.; LOGINOV, 34, , ~ U,
11ZL. ;.Kuyt I-. SHUTOV, R. -(Vyksa.1 Gor Tkovskoy
obl.]; RUSAKOV, A.., nq-t-e--r (Angar5k); D&AIN, A.$ iush. (Serpukhov);
GAYDkMAK, A.; ZAYTiEV, I., (,bskvaj'; FIALYSHEV, N. (Moskva)
Suggested, creat;.d, introduced- Izobri rats. no.12:14-15 D 162.
(MMA 15:12)
1. Sotrudnik Gosudaretvennogo instituta po vnedreniyu peredovykh mtodov
rAbot i truda v stroitel'sWe 14inisterstva stroitel'stva RSFSH, ~bskva
(for Taslitskiy). 2. Master ruchnogo uchastka Dneprovskogo alyumizLi-
yevogo zavoda Imeni S.M.Kirova (for Gaydamak).
(Technological inxiovations)

SHIJTOV, R.A., starDhiy master
Deoxidation of 25L and 35GL steel in the ladle by ferromnganese.
Met&Uurg 7 no. 5:15-16 My I"' (MIRA 15-5)
1. Plavilinyy uchastok zavoda drobil',no-razmol'nogo
oborudavaniya.
(Steel--Zlectrometa,llurgy)

'4MAlly, L. I., Inzh . ; !~HIJTN , S.A., in-0i .
(J~itllno of ship rolmir and operational bnsen and a I)ic;ic! inflo~-
of tbnir work. Anch.tranap. 13 nc,.5:I-"?-38 07 "P.
(Ships-14hintonancr? and repair) 04IR;~ 12:9)

EW (1)/BDS/EEC(b)-2--AFFTcAsD/ESD-3--Pi-4--IJP(C)
L loo44-63
ACCMION b: AR3000375 S/0058/63/000/004/ZD66/ZO66
SaMEE: JRZh. FiZika,, Abs. 49"7
to
AIMOR: Kati IL V. ShUtoV$ S. D.
TITIE: Anistropy of electric conductivity and optical properties of antimomy
selenide crystals
CMM SWRM: Tr. po, fiz. poluprovodnikov. Kishinevsk. wl--t, vp. 1., 1962
47-53
TWIC TAW: antimony selenide crystals, electrical and optical properties,
semiconductors
TRANSIATION., The properties of single crystal of Sb sub 2 Se Sub 3, which are
characterized by a rhombic lattice with layered structure and therefore have
anisotrcpic properties, have been investigated. The results of 7the measurements
of the electric conductivity, as a function of'the temperature, along the tlxme
crystallographic directions show that the component pexperAlcular to the cleavage
plane is five times m-1 I er than the two others. A formula is presented for the
Card 1/2

L loo44_63
ACCENION NR: AR3000375
calculation of the temperature dependence of the components of-the conductivity
teensor, from which the width of the forbidden zone and the activation energy of
the lattice imperfections are found to be 1.06 and 0.14 ev., respective-ly. it is
shown that Sb sub 2 Se sub 3 is a 2-axis cz7stal, and the postions of the optical
axes are determined. The values of the refractive indices in the direction of the-
principal dielectric axes are given. The optical activation energy and the
refractive index for one and the crystallographic direction depend on the-
polarization of the light. Such a dependence indicates probably that the energy
beams in antimorq selenide has a. complex structure. V. Gurevich.
DATE AcQ: l*4ELy63 ENCL: 00 WB CM: PH
2/2
Card
----------

ACC
COD--: UR/OOGO/' /00ri/0221/0228
66 ow
A'U`:~M: Sobolev, V. V.; Sy-rbu, 11. N. Shut9yj S. D.
nRG: none
TITLE: Enercy structure of bands of certain II - V, V - VI, and III - V! compounds
SGUIRCE: AN' ~-'SSR. institut fiziki tverdoCo tela i poluprovodnikov. Xhimicheskaya
svyaz' v poluprovodnikakh i ter-modinamika (Chemical bond in semiconductors and thermol
dynamdcs). Minsk, Nauka i tel,&,nika, 1966, 221-228
TOPIC TAGS: semiconducting material, semiconductor band structure, light reflection,
optic spectrum, Brillouin zone, optic transition
ABSTRACT: The purpose of the investigation was to study the reflection spectra in
the region E > E, of a large number of anisotropic semiconductors (ZnSb, CdSb, ZTi4Sb3l.,,--
Zn3Sbz!, Cd,.Sb3, P/,113P21 Cd3P21 Zn3AS21 Cd3AS21~ ZnAG21 CdA521 Sb2S3, Sb;,Se3l Sb
2TC31
Bi2S3, BizZe3, Bi_,Te3l inSe, In2Tej GaSe, and GaTe) for the purpose of determining
the energy gaps at different points of the Brillouin zone and comparing them with the
band theories for anisotropic substances. The reflection snectra were investigated
in the re3ion 1 - 6 ev at T = 293K. Plots of all the spectra are present ted and tables'
of the reflection peaks for different energies are given. The main conclusion of the'
data is that most reflection maxima of the crystals are due to direct interband tran-,
sitions; their maenitudes on the energy scale are directly equal to the values of the?
corresponding interband gaps at different principal points of the Brillouin zone. The 1
Card 1/2 UDC: 541-57

ACC NRI A77003864
various peakz observed on the reflection spectra for the different substances are
interpreted from the point of view of the published theoretical and experimental
papers dealing with the different compounds. Orig. art. has: 1 figure and 4 tables.
SUB CODE: 20/ Sum nATE: 2oAug66/ ORIG REP: 011/ OTH REF: 008
Card 2/2

ACC CODE: - UR/oow/66/000/000/0240/02~0-
( A ) ;6 -
AUTHOR: Kritovu, S. G.; Sobolev, V. V.; Syrbu, N. N.; ShutovS., D.
ORG: none
TITLE: Energy band structure of crystals of groups IV, III - V, II - VI, and the
MgaSi type
SOURCE: AN BSSR. Institut fiziki tverdogo tela i poluprovodnikov. Xhimicheskaya
svyaz' v poluprovodnikakh i termodinamika (Chemical bond in semiconductors and thermo-
dynamics). Minsk, Nauka, i tekhnika, 1966, 240-250
TOPIC TAGS: semiconducting material, semiconductor band structure, light reflection,
optic spectrum
ABSTRACT: 'Ibe authors investigated the band structure, using the reflection spectra
of pure and alloyed, polished and etched samples, cleaved crystals, and dendrites of
groups IV and III - V, and polished and etched cryst-als of groups II - VI (Si, Ge,
GaAs, GaSb, InAs, InSb, InP, GaP, and AlSb), 14g_,Si., MZ2Sn, and certain solid solutions
of the systems InP-InAs, AlSb-GaSb, CdTe-HgTe, ZnSe-CdSe,. 14gpSi-1,;g2Sn, and
YZP-Si-YJ92-Se. The various peaks observed on the different spectra of the substances
are listed and compared with results obtained by others. Tables of the experimental
values of the direct interband transitions are presented. It is stated in the con- I
clusion that the lack of doncrete and sufficiently detailed calculations of the bancisl
and schemes for the chemical binding forces for most solids makes it very difficult
Card 1/2 UW: 541- 57
Card

L 92o4-66-
ACC NR,
SOURCE:
AUTHORS*
ORG:
EWT Cl)/FwT(M)/L-Wj!(w)/T/E;WP(t)/EWP (b-)--IJP(c)- GG/JD
U6000123 SOURCE CODE: UR/OO58/65/OOO/OO8/E054/E055
Ref. zh. Fizikap Abs. 8E409
Dinge., V. N.; lAinge, T. I.- Shutoy S. D.
none
TITLE: Anisotropy of microhardness
CITED SOURCE: Izv. AN Mo*ldSSR. Ser. fiz.-telqm -A matem. n .12,, 1964, 61-68
q y 1 5-
TOPIC TAGS4-nt ~�rW compound) crystal pr
operAy, hard
TRANSLATION: The scratching method was used to investigate the anisotropy of the
microhardness of Sb2Se3 Crystals on the planes (100)p (010). and (001). It is shown
that the magnitude of the microhardness, and also the external form of the scratches,
depends essentially on the direction of the scratching on the investigated face. On-,.
the (010) plane the maximum of the microbardness is observed in the scratch direc-
tions (301) and (301). An interpretation of the character of the dependence of the
microbardness on the direction on the (010) face is difficult. Apparentlyp in Sb2Se3
crystals the slip occurs along the (010) plane in the (100) direction. On the (001)
plane the minimum of hardness is observed close to the (100) direction, and on the
(100) plane the greatest hardness is in the (010) direction, i.e... perpendicular to
the emergence of the cleavage plane on the (100) face. It is also shown that in all
directions the hardness in scratching decreases upon illumination, i.e., a photo-
-iic-fianical effect taken place. V. Osvenskiy.
BUD CODE: 20

L 1003C~63 EWT (11) /BDS/M (b) -2-AFFT0/A8D/Y,8D_3 -id (6)
ACCESSION NR: AR3000374 s/0058/63/000/004/EO64/EO64
SOURCE: RZh. rizi1m, Abs. 4034
AUMOR: Kqt, M. V.; Shutov, SeD.
TITIE: Some electric propertie of crystals of antimony triselenide
CITED SOURCE: Tr. po fiz. poluprorvodnikov. Kishinevsk. un-4, vyp. 1, 1962, 54-56
TOPIC TAGS: antimony triselenide crystals, electric properties, semiconductors
TRANSIATION: Homogeneous single crystals of Sb sub 2 Se sub 3 of the n and p
type were obtained by doping-with tin and antimony. The tin is a donor
impurity, while the antimony, without changing the hole charracter of the
conductivity of the stoichibmetric crystal, increases the electric conductivity
by four orders of magnitude. The electric conductivity and the thermal emf were
investigated with nurrent flowing along the cleavage plane, that, in the
direction of the [POl) axis. From the data on the electric conductivity
Card 1/2

L 10030-63
ACCESSION NR: AR3000374
of crystals, the activation energi6s of the donors and acceptors are
calculated, found to be 0.04 and 0.03 ev, respectively. on the basic of
measurements of the thermal enif in the region of intrinsic conductivity it is
established that the mobility of the holes in Bb sub 2 Se sub 3 is almost three
times larger than the mobility of the electrons. V. Gurevich
DATE Acq: 14may63 ENCL: 00 SUB COME: PH

SHUTOV, T.I.
Crustless cheese in a polymer packing. Infom.biul.VDNKH no.1IjIO-U
N 164. (MIRA 1812)
Is Direktor pavillona 'Molochnaya promyshlennost'" na Vy-stavke
dostizheniy narodnogo khozyaystva SSSR.

EHOTW"FOVA, NY, TROIT,)'KAYA, N.K.; CjjTj4f3j.FCj, A.M.; DOMBSKAYA,
C. B. SH UTOV r.l.,
rxh,bitlons and display.,3 of special items. inform. blul.
VDNKH no.10:9-11 163. (MIRA 18:5)
1. Pazdel "Fri borostroyeniye i sredstva avtomatizatsiill
ppwillcnit "Mash;nostrovenivell nh Vystavke dostizhenly narodnogo
khf~~zyqystva (for Khobotov.). 2. Czlavnyy inzh.-metodist pavillona
"Mashtnostroyenive" na Vystavke clostizheni-y narodnogo khozy-ystva
(for Troitskaya). 3. Glavnyy metodist razdela "Geolog-Vall Ob'l-
yedinennogo pavillona "Toplivnaya promyshlennostil i geologiyall
n~t Vyst,Hvkf- drstJzheni-v narednogo khozyaystva SSFR (for Dominskaya).
4. Direktor pavillona "Moloclinaya promyshlennosil" na Alystavke
dostizhen4Y narodnogo khozyaystva SSSR (for Shutov).

KUROVY G.J. kapitan 3-go runga; SUM, V.., kapitan-loytenant
Communists of the foremost warships. Nomm.Vooruzh.Sil I
no.17:58-59 S 161. (14IPA 14:8)
(Destroyers (Warships))

SM!TOV.7 1~-. D.
SHUTOV, V. D. - "Frag7rRntal Feldspars of the Productive Stratum of
Azerbaydzhan and Their Paleogeographical Significance." ~~ub 30
May 52, Inst of Geological Sciences, Acad Sci USSR. (Dissertation
for the Degree of Candidate in Geological and lUneralogical Sciences).
SO: Vechernava Moskva January-December 1952

uwR/Geology
Card
Autbars 1 Kossovskaya., A. G. and Shutov, V. D.
Title s Conditions leading to the accumulation of the productive stratum of
Azerbaidzhan
FOrlOd1cal I Dokl. AN SSSR, 97, Ed. 1, 141-- 143, JulY 1954
Abstx=t The geological conditio;s resulting in the genesis of the petroleum
rich productive stratum of Azerbaidzhan (Az-SSR), are explained.
Five USSR references.
Institution
Presented by Academician D. I. Shcherbakov April 14, 1954

USSR/ Minerals Mineralogy
Card 1/1 Pub. 22 39/49
Authors j Kossovskaya, A. G.. and Shutov, V. D.
Title I Nature of changes in cla~tic biotite during epigenesis
Periodical I Dok. ANT SSSR 10113, 541-554, Mar 21, 1955
Abstract I Lithological-petrographic data are presented on the changes occurring
in clastic biotite (magnesium-iron mica) during theprocess of epi-
genesib. Graph; illustrations.
Institution Aced. of Sc.i USSR, Inst. of Geol. So.
Presented by: Academician D. 1. Shcherbakov, November 209 1954

KOSSOVSKAYA, A.G.; SHUTOV, V.D.
-111&41f.t~-"~"' .~ ~
Zones of epigenesis in the terrigenic complex of the KeDozoic
and Upper Palsozoic deposits of the western Terkboyansk Range.
Dokl.AN SSM 103 no.6:1085-1088 Ag 155. (KW 9:1)
l.Predatavlono akademikom N.M.Strakhovyu,
(Verhoyansk Range--Geology, Stratigraphic)

KOSSOVSKAYA, A.G.; SHUTOFI, V.D.
,
Zonal alterations of terrigenous rocks during epigenests and
early-stage metaporphism in a geosynclinal zone. Vop.min.osad.
obr. 3/4:452-467 156. (KLRA 9:11)
1. Institut geologicheakikh nauk Akademil nank SSSR. Nookwa.
(Geochemistry)

SHUTOV, V.D.
Now method for studying clastic feldspars in terrigenous rocks.
Vop.min.osad.obr. 3/4:647-653 '56. (MLHA 9:11)
1. Institut goologicheskikh nauk Akademit n&uk SM, Nookwa.
(Feldspar)

S -H FO V~ V _P4
7.
P'Tho c6racter and distribuda of MuRral iieogeucs In a
L.,
nV
kb
P
id d
sits
f West
k
It
fil
f M
-
o
eso r
or
a
ozo
oyans
.
epo
o o
o
~fo
G.- Kossovskiya -. aid bUtoiO, TrWy Gcol.
I A10V

~rThe min-
Itui., * -Akad., SAS. R'~ 10
e
cral sequence In-th Mcsozok and We Pale4zole periods
Is studied and classified -The ceniviting. substance in the
~
lx
tjokafly. muscoVite, -01ocite, cir quartx.
upper Permlid
_(with-b
In the jurassic-Triassic It Is chi6dtc
pal
Y
-
-Critkoo~w, Ca zvolit
or quartz); IA the lower 4t=y
.
-forming'. c~mpouents, ~ an -mme6vil
The tock x; chloritej
andesint plaXioclaw, ' and quartz * In, the - uooer- Permian
d -
t
th
ti
u
i
b1
l
W
n.
ar
z
o
&
te, pWoc
i RA
Q
e j
_
Common
and hydmted cidonue:1 bluilte in the cretace~.
Accessory minerals an: ~ Permian Oldote te, rutilef
low

iuscovite, * Jurassic-TrImajisic, 41dote. to, 50hene'.
Wid
and v
ilmtwte. anatase, htoolcitej leumene, epiclote"
Cretaceous

--5.m 1 \V D. --- - --- - -
V 7(~v -- I--. --- -
I -.- I -- - -
7 . - . . . - I - - , . - -- - -- --- -,
~ , ~ 1 --7~ 7., --- ~ -- -.- -1 --. --". - - - - .. - I I - - --

USSR/Cosmochemistry. Geochemistry. Hydrochemistry. D
Abs Jour Ref Zhur - Khimiya, No. 89 19~79 26~58.
Author Kossovskaya A.G.,. Shutov, V.P.-
Inst Geological Institute of Academy of Sciences
of USSR.
Title Character and distribution of New Mineral
Formations in Cross-Section of Mesozoic and
Paleozoic Deposits in Western Verkhoyanlye.
Orig Pub Tr. Geol. in-ta, AN SSSR, 1956, vyp. 57
135 - 168.
Abstract No abstract
Card 1/1

lb -57 -4 -4-513
Translation from: jZe,f'(jrL-t-,.vr---v zhurnal, '.,eologiya, 1957, N"r 4,
p 73 (USSR)
AUTHOPS Kossovskayn, A. G., Shatov, V. D.
TITLE: Zonal Alterutions in Clastic Rocks During Epigenesis
and Incipient Metamorphism in the Geosynclinal Zone
(Zorallnost? izmeneniya terrigennykh Dorod pro epigeneze
i nachallnom metamorfizme v usloviyak~ geosinklinallnoy
zony)
PERIODICAL: Vorp, mineralogii osadoch. obrazovaniy. Books 3-4.
L'vov, Llvovsk. un-t, 1956, pp 452-467.
AF S T R A C TIn the east-west part of the Verkhoyansk mega n ticlinorium
along the right bank of the Lena and Aldan Rivers, an
almost uninterrupted section of sedimentary beds,
ranging in age from Lower Cretaceous to Lower Permian
(a thickness of more than 11 000 m), has been studied.
These rocks are uniformly fragmental. Large-scale zones
have been distinguished on the basis of rock structure,
Card 1/4 nature and comoosition of the cement, groUDS of newly

1 11-1 tern t1i ons in Cl-.s tic Flocks (Cont.)
10- -.1 b 13
f'orried minerals , and compo3ition and degree of' recrystallizati on of
y m1i te rl u I . I T e zon(,~ nP clay cement embraces the upper
Lhe c In
prrt of the Lower Cr'(AUCeWs rocks, over 500 m thick. The sandy-
3'Lity roc~.s are cementcd, by pore filling. The clay cement consists
of finely comminuted clastic material (quartz, feldspar, and raica)
an-_1 a weakly polarizing matrix, in places containinE chlorite; rarely
t'rie epraerit shows calcitic corrosive features. n-agmental Lornblende
and acid plagioclase are most intensely corroded; quartz and biotite
f3r- least affected, 2) TI-le zone of chlorite and chlorite-quart-z
ce-nent includes the lower nart of the Lower Cretaceous and the Upper
J u ros s Ic . The rocks are chiefly 3andy-sillEs with subordinate mud-
s tones , The chlorite -cement fills pores end forms as a crust on the
mineral grains. In the upper part of the zone the cement consists
of chlorito nnd chlorlto-opnl; more rarely laumontite &nd calcite
are Felo"'I
present., renerally producing b poiki 11i tic -like structure,
In the section, the opal gives way to chalcedony and quartz. Vie
epigenetic transformation of ti-ie clay cement culminates in the lo-arer
hor-'zcns of luftis zone. The biatite tias been ~iydrated; at tne base of
the zone it has been converted to chlo.-itic minerals. 301 T~-.e zc-:~e
Card .0/4

15-57 -4 -4513
nal 'l ter a ti ons J c Rocks (Con t.
of quartz -recrys talli zed cement (qua-rtzitic structure) embraces the
section from the "liddle Jurassic to the Permian, a thickness of 4000
m to 6000 m. The sandy-silty rocks have a quartzitic structure,
produced by the recrystallization of grains of quartz and feldspar,
The biotite is chloritized. Intense development of hydromicas is
observed. Newly formed minerals include rutile, ilmenite, laucoxene,
sphene, anatose, brookite, epidote, and apatite. Crystalloblastic
growth has been noted in the lower parts of the zone. 4) The zone of
quartz- recrys tallization and micaceous cement embraces the Lower
Permian rocks, up to 4000 m in thickness. It is characterized by
comDlex auartzitic structure and sandstones with muscovite cement.
Commonly the muscovite has formed along fragmental grains of feldspar
and quartz. In this process the ootassium feldspar has been replaced
along the entire surface of the grain and shows no recrystallized
rim. Such features indicate an instability in the epigenetic
environment in the deposits of the geosynclinal zone. The biotite
is completely converted to muscovite and chlorite. Epidote and
--zoisite are widely developed, and anatase and sphene are also
present. The zones as distinguished correspond to structural
Card 3/4

15-1957-3-3014
Translation from: Referativnyy zhurnal, Geologlya, 1957, Nr 3,
p 82 (USSR)
AUTHOR: Sh utov, V. D.
TITLE: A Now Method of Studying Fragments of Feldspar in
Clastic. Rocks (Novyy metod izucheniya oblomochnykh
polevykh shpatov v ierrigennykh porodakh)
PERIODICAL: Vopr. mineralogii osadoche obrazovanty, Books 3-4p
L'vov, Llvovsk4 un-t, 1956, pp 647-653
ABSTRACT: A new method is proposed for studying the quantita-
tive distribution of different feldspars in send-
silt rocks. The Federov stage is used on a
preparation of grains mounted In Canada balsam.
The method combines the principles of immersion
and universal-stage technique. It is especially
convenient to use grains in the 0.1 to 0.5 mm
Card 1/2 range for study. The preparation is illustrated

15-1957-3-3014
A Now Method of Studying Fragments or Feldspar in Clastic Rocks
diagrammatically and the feldspar grains are counted (to a
total of 300). Identification of the type of feldspar
may be made by the optic sign and by comparing the Index
of refraction of Canada balsam with the principal optic
section of the mineral* This section may be properly
oriented on the universal stage. Among the feldspar
fragments# it is possible to distinguish and account for
11 types# and these are listed with their dlignostic
properties* The method is recommended for use with fresh
foldepaS fragfuents as well as with detrital grains.
T* A. Yao
Card 2/2

AUT14ORS: Kossovskaja, A. G., Lugvineziku, 11. V., 20-2-37/50
Shutov, V. D.
TITLE: On Various Stages of Formation and Alteration of Terrigenous
Rocks (0 stadiyakh formirovaniya i izmenenija terrigennykh porod)
PE-RIODICAL: Doklady AN SSSR, 1957, Vol. 116, Nr 2, pp. 293-296 (USSR)
ABSTRACT: The study of the stages of the sedimentation-rock formation can
be generalizingly called the stage analysis. Its task is: the de-
tection of paragenetic mineral-associations of the texture-and
structure variations, as well as of physical-mechanical parame-
ters which characterize the different stages of the~iBtory of the
formation- and existence of the rocks: i. e. the sedimentation-,
the diagenesis- and epigenesis stage and finally the stage of the
initial metamorphism. The final stages of the formation of the se-
dimentation rocks mean either their transformation into metamor-
pl,ous rocks or the surface weathering and destruction. Thus the
stadial analysis has to contain a series of processes which dif-
fer verj much in character and orientation. The first and last
sta -es are the best known. The study of the thick cross sections
of terrigenous deposits in geosynclinal regions~nd in~transition
areas to the latter facilitated the detection of a certain zona-
Card 1/ lity wh 4 Ch characterizes the sedimental rocks -..hich were subjected
.L -

20-2-37/50
On Various Staoes of Pormation and Alteration of Terrigenous Hocks.
Q. %
to a various depth of depression and thus to a different stress
action. The zonality is expressed in a specifically mincralogi-
cal-petrographical composition of the newly formed mineral com-
ponents, in certain structure-texture characteristics of the
rocks and in their physical-mechanical properties. The zones of
the epigenesis and of the early metamorphism occur on the thick
vertical cross sections of the sedimentary masses as -well as on
their development surfaces. The collected material of the Soviet
and of the foreign petrographs shows that the history of existence
of the sedimentary rocks represents an uninterrupted and orientated
process. It is divided into series of stages: These are the fol-
lowing: 1) diagenesis, 2) epigenesis, 3) metagenesis or initial
metamorp~llism, and finally 4) regional metamorphisa. The epigene-
sis is characterized by: a) a gradual solidification of the rocks
by the increase of their volume weight and decrease of the poro-
sity, b) alteration of the original splinter structures- and tex-
tures, then by "so-tening" of the same structures by a recrystal-
lization of the clastic grains of the arenaceous rocks and by
the formation of mosaic structures. c) Considerable reworking of
the argillaceous minerals by their increasing recrystallization
degree, vanishing of a series of argillaceous minerals with exi-
Card 2/4 sing intermediate layer water (montmorillonite-group) and by an

20-2-37/50
On Varioa~; of Furi:tation and Alteration of Terrigeno-Is 11tocks.
intensive water mica transfor,aation of t1he kaolinite, finally by
the occurrence of the association hyero-chlorite. The depth epi-
.-enesis takes place metasomaticalli. The epigenesis is divided
into an initial and a depth npigenesis; Meta,~jenesis or early me-
tamorphism is a transitiun itate from the sedimentary rocksTn
general to the metamorphous ones. The volume and the specific
weight of the rocks increase, minerals with a more solid struc-
ture of the crystal lattice occur. The original characteristics
of the texture vanish, the metasomatose process gains importance.
A division can be found, like in the case of the epigenesis. The
regional metamorphism is connected with the metagenesis stage by
gradual transitions. The formation of the mineral association of
the muscovite-chlorite-zone characteristic of this stage begins
already in the epigenesis. In the metagenesis this association
determines the mineralogical-petro.,raphical type of the schist.
Quality alterations of the as.;ociation occur only in the biotite
zone where the occurrence of biotite is fixed which is produced
at the cost of the interaction between muscovite and chlorite.
The alteration of the association is connected with a further
temperature rise. Also the specific weight increases up to 2,86.
In th-- case of deprtssiun a progressive e,;igenesis takes place,
Card 3/", in the cai;e of general elevation, however, a regressive epigenesis.

20-2-37/50
On Various ~;ta~,es of Yormation and Alteration of Terrigenuus Rocks.
It has no orielLtated character and does not change considerably
0
the results of tile progressive epigenesis. There are 1 tdble and
16 references 13 of which are Slavic.
ASSUCIATION; Geological Institute All USSRjKhar1kov State University (Geologi-
chLski.v institut Akademii nauk SSSR 1~ Kharlkovskiy gosudarstvennyy
universitet)
PRESE14TED: March 4, 1957, by N. M. Strakhov, Academician
SUBMITTED: April 15, 1937
AVAILABLE: Library of Congress
Card 41/4

KOSSOVSKAYA, A.G.; IA)GVINISKO, N.V.; SHUTOV, V.D.
Various stages in the formation and changes of terrigenous rocks.
Dokl. AN SSM 116 no.2:293-296 S 157. (KIRA 11:2)
1. Geologicheskly Institut AN SSIR i Kharlkovskly gosudaretyennyy
universitst, Predstayleno akadealkon N.K. Strakhovyu.
(Rocks)

and
"Zormlity in the 5tructurc. of Terrigene Deposits in Platform and Geosyncline
Regions."
report ixesented at the 5tb Intl. jedimentology Congres5, Geneva/Lausame,
r
2-7 June 1958.
Acad. -Sci. WSR, Noscow.

KOSSONSKAYA, A. G. and SIIUTOV, V. D.
"Factors Detemining the Mineralogical Compsosition of Clay Rocks in Platform
and Geosyncline Regions."
paper distributed at the Internationl Clay Minerlogy Congress in Brussels, Belgium,
1 - 5 Jul 58.
Counient: B-3,116,859

SOV/5-58-6-4/13
AUTHORS: Kossovskaya, A.G. and Shutov, V.D.
.................. ....................
TITLE: To the History of the Development of the
Western Part of the Upper Yana Region and
the Vilyuy Depression During the Upper
Paleozoic and Mesozoic Eras (K istorii
razvitiya zapadnogo Verkhoyanlya i Vilyuys-
koy vpadiny v verkhnem paleozoye i mezozoye).
PERIODICAL: Byulleten' Moskovskogo obshchestva ispy-
tateley prirody, Otdel geologicheskiy, 1958,
Nr 6, p 42-57 (USSR)
ABSTRACT: The history of the development of the Upper
Yana and the adjacent regions during the ac-
cumulation of the terrigenous deposits during
the Upper-Paleozoic and Mesozoic eras (from
the Lower Permian up to Upper Cretaceous time)
is distinctly divided into two large cycles
of accumulation of sedimentary deposits:
Card 1/7 the Upper Paleozoic (Lower Permian - Middle

SOV/5-58-6-4/13
To the History
the Upper Yana
Upper Paleozoic
of t1- Development of
Regi,n and the Vilyuy
and Mesozoic Eras
the Western Part of
Depression During the
Card 2/7
Triassic times) cycle,and the Mesozoic
t4
(Upper Triassic - Upper Cretaceous U.mes)
cycle. The formation of the sedimentary
layers during the first cycle occurred main-
ly within the limits of the Upper Yana geo-
synclinal region. In the second, Mesozoic
cycle, it spread to the adjacent parts of
the plateau region and to the Vilyuy depres-
sion. Both cycles were similarly built and
subdivided into a series of litholoEic for-
mations, replacing each other in time, and
corresponding to separate stages of the de-
velopment of each cycle (see table on p 46-
47). The Upper Paleozoic cycle began with
the formation of deposits of the lower
sand-schist complex (figure 1) formed under

SOV/5-58-6-4/13
To the History
the Upper Yana
Upper Paleozoic
Card 317
of the Development of
Region and the Vilyuy
and Mesozoic Eras
the Western Part of
Depression During the
marine conditions of the Lower Permian
transgression. Its formation was complicated
by two regressive movements. In the next
stage of this cycle, which also occurred un-
der marine conditions, deposits of schist
facies were formed. Its layers were formed
of black argillaceous schists with a large
content of thinly dispersed organic-matter.
A general regression began in the Upper Per-
mian time and a submarine cordill*M,dividing
the western and eastern slopes of the Upper
Yana ridge, was also formed at that time.
Deposits of a flyshoid complex were formed on
the western slopes, whereas argillaceous schists
were formed on the eastern slope. The second
part of the Upper Permian time was character-
ized by a further differentiation of vertical
movements. On both cordillera slopes conglo-

SOV/5-58-6-4/13
To the History
the Upper Yana
Upper Paleozoic
Card 4/7
of the Development of
Region and the Vilyuy
and Mesozoic Eras
the Western Part of
Depression During the
merate-sand-argillaceous deposits were formed
at that time. A large sinking zone was formed
in the central part of the western slope, and
the coal-bearing non-productive complex was
formed in the depression, coal bearing layers
alternating with sand-schist layers. The end
of the Upper Paleozoic cycle was character-
ized by regional elevations, which in the
Middle Triassic time included the whole
western part of the Upper Yana region and
the adjacent Vilyuy depression. These ele-
vations shifted the sea basin to the north
and east The Mesozoic cycle began with the
accumulation of sand-conglomerate sediments
which form the Upper Triassic - Lower Liassic
deposits in the western part of the Upper
Yana region. The sea from the east again

SOV/5-58-6-4/13
To the History of the Development of the Western Part of
the Upper Yana Region and the Vilyuy Depression During the
Upper Paleozoic and Mesozoic Eras
covered the western slopes of the Upper Yana
ridge and the formation of deposits of the
sand-conglomerate complex took place under
conditions of an increasing transgression,
acoompanied by two regressive movements.
During the next stage, in the Middle- and
Upper Linssic times, the aleurolite-argil-
laceous dep-:,.sits were formed. The stage of
an increasing regression began during the
Middle Jurassic period, characterized by a
diminution of the marine basin and by a large
accumulation of sediments of the upper sand
complex, of a semifacial texture and composed
of maritime as well as continental layers.
In the Upper Jurassic and Lower Cretaceous
(up to Aptian) periods, a thick coal-bearing
Card 5/7 complex was formed. The zone of intensive

SOV/5-58-6-4/13
To the History of the Development of the Western Part of
the Upper Yana Region and the Vilyuy DeDression During the
Upper Paleozoic and Mesozoic Eras
sagging moved to the Upper Yana region and
the Vilyuy depression. Intensive mountain-
forming processes, accompanied by regional
ruptures and volcanic activity, took place
at the end of the Lower Cretaceous period.
This fixed the last stage of formation of
the Upper-Yana Kol:yma folding region, and
the Upper Yana ridge became a chain of moun-
tains. General elevations in the Upper Yana
region drove the zone of sagging into the
Vilyuy depression where, in the Albian and
the whole Upper Cretaceous periods, a com-
Card 6/7 plex of kaolinized alluvial sandstones was

SOV/5-53-6-4/13
To the History
the Upper Yana
Upper Paleozoic
of the Development of
Region and the Vilyuy
and 1."esozoic Eras
the ';,*estern Part of
Depression During the
formed. The following Ceologists are men-
tioned by the author: N.P. Kheraskov,
A.A. f.ezhvilk, N.S. Shatskiy, N.M. Strakhov
and Y.M. Flashebarovskiy. Thcre is 1 set of
profil,,,,s, 1 table, 1 dia,-ram and 21 Soviet
references.
Card 7/7

AUTHOR: 7hu to V,V 11-5S-7-2/12
TITLE: Lithologric and Stratigraphic Subdivision and Sedimentation
Conditions of Permian and Lower Triassic Deposits of the
Verkhoyansk Range (i.i-tologo-stratif;rnficheskoye raschleneniye
i usloviya osadkonakopleniya permskikh i nizhnetriassovykh
otlozheniy Verkhoyanskogo khrebta)
PERIODICAL: Izvestiya Akademii nnuk Seriyn geoloricheskaye,
1958, Nr 7, pp 20-36 (113~!R)
ABSTRACT: The author proposes a scheme of subdivision and comparison of
Permian and Lower Triassic Deposits of the Verkhoyansk mountain
ranges. This region was explored in detail by many groups of
geologists sent by "different Soviet orEanizations, and the
author himself worked many years in the repion. He sums up the
information gathered by V.N. Andrianov, A.S, Kashirtsev, A.V.
Vikhert, A.V. Zimkin, A.V. Leyptsig, G.S. Borushko, V.M. Mell-
nikov and others and connects them with information obtained
from the study of bearing profiles by members of the Scientific-
Research Tnstitute of Arctic Geology T.P. Atlasov, A.A. ?Iezh-
vilk and others, male more precise b-.- other expeditions of this
Institute tinder the direction of 11.Y. La--urkin. The author
Cardl/ 7 identifies 5 different comDlexes or formations thnt form the

11 -c5 8-7 -2/12
Lithologic and Stratigraphic Subdivision and Sedimentation Conditions of
Permian and Lower Triassic Deposits of the Verkhoyansk Range
Upper Paleozoic cycle. These complexes represent strongly syn-
chronous formations and form separate stratigraphic levels.
The paleontologic remainders collected by A.S. Kashirt-sev,
Ye.M. Lyutkevich, A.V. Zimkin, Yu.N. Popov, A.F. Yefimova,
I.T. Tuchkov, V,N. Andrianov, B.S. Abramov, A.V. Vikhert and
the author in Permian and Lower Triassic profiles of various
parts of the region, confirm the following divisions:
1) Lower sand-shist complex was formed in condition of trans-
gression development and characterizes the basic transgressional
stage of the cycle. This complex was formed by two layers cor-
responding to the deposits of Sakmara and Arti (Lower Permiqn)
stages which could be traced through the whole Verkhoyansk
region. (The author divides the whole region in three sections,
determined by the characteristics of their profiles). The
lower layer has different names in the three sections. It is
formed mainly of argillaceous shists and by its paleontologic
remainders it is identified as belonging to the Sakmara stage.
The upper layer is identified as belonging to the Arti stAge,
Card 2/7 It has different names in the three sections, but on the whole