SCIENTIFIC ABSTRACT MESHCHERINOVA, O. N. - MESHCHERSKIY. I. N.

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• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R001033620014-1
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: January 3, 2017
• Document Release Date: June 21, 2000
• Sequence Number: 14
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

'The- iftflueft6e, of. Baron On the~*i~roperltles ... o. .17,76/6z/odo/0971001/
r
S 0
sme tinglec nique;. m~przseq an i , - .
n ():the: test methodollogyj,.vihi6h. ca n%~e tigati n:of
ain,.::th&.ha-- the'm chanical:_i
-the.,growil~_:tendelic f the, gr denabilfty,of the ~:steel~ e
Yo
roparOes, te- "toughnes ivitv'to, stress concentration, and the
h s margin or sonsit
-t6rape r--~brittlene,s S tendency; '(3)-the wddation-.melthod employed, for. the determina.-
tion of the austenite-grai.,y site -(test re sults Shown in full-page table); .(4) the de-
te rminatioii of the hardena biIity b y.rneaias of. the' facial-hairdening :method,, (5) tests'
-es compri tasts-0
~fo t ising ten.sile andimpact tests and "RC
r mec anical-pnopei
(6) ~tests.~ ldr~- the. 11tourfhness. mardn'," which ware achieved by impact..tests at Vari-,
~ous remperatur'ds be"veea +20;and -1000G,,; which- th k a th
e impact wor nd e
a,) f the. fracture xvere- Iused as c'riteria* (r in full-pa-'ge tables)
Pea rance -,o esults~ shown
(7) tests-for the temper-brittleness s*enslitiviity, *.In which a. comparison of the impact
f the fracture
toughne s s, and The appearance o.. N~ra~s =- ade.,between. nonembrittled spe -
cim6iiij- which-had: been duenched in'oil and tempered for,Z. .5 hrs at -650'C and then
oil-cooled... zn.d. C_.-,ibrittled sn6cintlens, quenched in_oil, tempered for- 2.5 hrs at
~500 -nd;Airt 0 for 16 hrs; the4-
hertem pered in the. ermbrittlerzlent zone at 530 e
0
frorn +20 to 100 G e s t re sUlts summarized in 2 full pag es),
t, Cie S~ of fi~ur
'tion,
idai. -o,..B increases"the:hardenabil
Conclusions, ity. of all of,. the alloyed
steels tested appreciably; an addition of O.GQZ%'B.ir_, the presence of.17.3 Cr in
f 1 IN
intensely than the addition o
~;creases'.:th'e laaraenability- of 'the, steelmore,
Sthels tested ~.4ere naturally fine-grain upor. deo:ddation.,by the given method..,, -.2

PATRINAI N.A., kand. tekhn. aauk;jj~q~_q~Zglj;~,VA, O.N., kand. tekhn. nauk
Using boron steels in manafacturing automobile starters.
Av-t. prom. 29 no.8:27-29 Ag 163. (MIRA 16:11)
1. Nauchno-issledovatellskiy i eksperimentalln7y institut
avtomobillnogo elektroobor-udovaniya i priborov (for Patrina).

M'19~-65 EwP(~j d-
(a) Pa
-R/2776/65/00d/039/0024/0030
A CCESI, IM IIR: AT5016056
Hesh6herinova-"O. N.-
AUM~
- ---------
T Ir TLE; 'Effect of -manganese on the properties of. structural steels
iGOURC",': Moscow. Tsentraltnyy nmchno-issledovatellsk~y institut cherno metal".ur-
S6oxrnik trudov, no. 39, 1965. Spetaiallnyye stali i Splavy (Special steels
r -30
la ~Aloyrj), 24
TAGS: alloy steel, heat treatrrent, temer brittleness,-martensitic transfor-I
imact strength,~hardenability, -iso-therinal transformation, metal mechanical!
.1p ty
ropi,
!ABSTIA.M.- -Atte ts-wene made-to-reduce.the Ni contents-of certain alloy steels by~ -
Swi S' itutin n d B"Jifn iti-placei- and stiii-reta in comparable
properties. Seran
diff~ Mnt ~ steels vere., used containing 0.20-0-22%-C, 0.17-MG%, Si,--0.58-1.05%
10.93-1.03% Cr, 0.9-1.04% Ni, and 0-~0.0031%,B. Three of -the steels were commerciali
W. .- 0 17- The -e f f ea-1- of - Mn-an&- 13--off - -hardanab i
ty ar d grain size v_;dB f ound- to be a fteclable. An increase in the Hn . content from
16:r) la 1% doubles-the 'hardenabilftyllas determined by end quench techniquedt,while
raddi~%iolls of 0.0025% T-are equiv"Ilent to Or-102% Min in increasing har4enabilit~i Iso-i
Ina

7: "T -'~!P(t /i-T1 1JP (c) JD
------ 6/6 1 17~
11)'OUICE, GOIW~: Uft 77 6/000/0)4/0 '10/0
GU' A.. P. Val U. "i.
URG: none
TITLE: Influence of carbon content on the coid-o-hortnessl.thxeshold of structural
steel
i SOURCE- '4oscow. T,,OnU'al1r1yy nauclino-it)al.ociov,,4tollokiy in3Litut chornoy
motallurgii. Sbornik trudov, no. 46, 1966. SpotsialInyp stali i oj)lavy (Spocial
steels and alloys), 170-175
TOPIG TAGS: alloy, steel, chromium steel, nickel st;ool, molybdenum steol,
mutallur6ic research
-:1iortnoso -o'd c.,
,C35T,-UtC;T. The effect, of the carbon content on the cold ;-. I
cL-xoriiu-,n-L-iickel-molybdenum steel was investigated. The specimons weiu quuacned and
subsequently annealed in two &tages to hardness FiC.- 20-125 and H?L = 30--35
r osp ec ti vely. The cold-shortness threshold was determined in terms of the fraction
of tne britLle component in the fracture of the 5pecimen. The cold-snortnesS thrL;
old temperature was taken as the temperature at which the fracture contained 10 z;-."
50'0 of the brittle component respectively. The experimental results are presented
in grapiis and tables (see FjLZ. 1). it was found tnat an increase in the caz .ooi
content in Cr-Ni-Mlo stool leads to an increase of ~he cold-shortness The
Card 1/2

c 6
r)0
0-
-40 -
-7~
C',
20
-40 10- 75hgc
0 c
?0
4~ -,FS
0,3 0,4 LI 5 0,7 0.8
carbon content
g
Fig. 1. 1 rf I uence of c~--rbon on
thc cold-siwrtness ti-Lre.-ihold
Is
of e E! a
c - 30-
CirclE,5 10,"
solid nqjarus~ P-
of 'ur-ittle cun-jonent; open
circ2es
souar
oi b itLle comioor(::It.

~TZJHCHERKINY V.
Some organizational problems of emergency medical care for
the rural population. Zdravookhranenie 5 no.5:45-47 S-0162
OURA 16:7)
1. Glavnyy vrach Karpinenskogo rayona, Moldavskaya SSR.
(PUBLIC HEALTH, RURAL)
(MOT AID ill ILLNESS AND IN1U-RY)

USSR/Cultivated Pla.1tq - PAat)us. Mel"'.s. N1
Abs Jour Ref Zhur Diol., No 12, 1958, 53642
Author Meshc!-.crov, E.T.
Tit-le :L:,. Ecderiic-t Li Hybrid Cucir.ibcr Seeds.
Ori. Pub Vestn. s.-kla. 1-kauki, 1957, No 6, 43-47
Abstract Anon~ tl,,,c secd saq,.)1cs reco-ived frDL! Sakhalin isl-incl.,
the authDr selectec~ plants of the famnle type which lie
used i.-- crDssLi,1- with differc:it varieties. The rusUts
prOduced varieties with a hiL,`i percc:ita._-e -,f fc-,~nle
plants which after havii.-~ been crossK11 with 3thar va-
rieties produced hid-i-yieldinc seeds. The auth.,r cinsi-
clers tnat by i-~cnaiis )f crossin'r, the quick hy-
brids of the first -encrati_,,i )f the fei.nle type witlh
quick ;.:aturinG varieties, it is feasible to .)'utaii: 'ii~;h-
yieldin.-.* hybrid cucumber seeds for the most northerly
re Jons S.Ya. Krayevoy
Card 1/1
Inst Testing smazion VM,
Plant' Husband-rY.
Title : Growing High-Yield Hybrid Cucumber Seed
Orig pub : Tr. po prikl. botan., genet. i selektaii, 1957, 31,
Wo 2, 223-225
Abstract : The experiment was done at the Maykop Testing Station
of the All-Union Institute of plant Husbandry. In or-
der to develop hybrid seeds by natural repollination,
the parental varieties (lo combinations) were planted
in adjacent rows on isolated plots- Hybrids derived
from varieties differing sharply in their morphological
characteristics (omskiy x Astrakhanskiy, Rzhavskiy x
Card 1/2
Card 2/2

TKACHENKO, N.M.; CHIZHOV, S.T.; KESRCLIEROV, F-T-; TKACHEV, R.Ya.;
DANIDDV, V.P.; KURZINA, LA.., red.; PROKOFlY&VA,,-l..v.,
tekhn. red.
(Cucumbers) Ogw-tsy. (B]N.N.Tkacheako i dr. Moskva, Sell-
khozizdat, 1963. 205 p. (MIRA 16:5)
(Cucumbers)

IZSHCHEROVg Kh.Kh.9 prof.. (Kazan')
.*therapy of uterine cancer from the hematological point of view.
Report No.2: Morphological obanges in the blood of patients treated
with radium. Kaz. med. zhur. no.6:48-51 H-D 160, (KERA 13:12)
(UTERUS--GANCM) (RADIUM-THRRAMTIC USE)
(BLOOD)

~WHCHEROV,. P~Jh. Prof. (Kazan')
Hematological characteristics of radiation effects under
experimental conditions. Kaz.med.zhur.no.1:1.5-47 Ja-F'63.
(MIRA 16:8)
(RADIATIOI,~-RMIOLOGICAL EFFECTS)
(BLOOD--ANALYSIS AND CHEMISTRY)

iESlICIEROV, Kh.Kh.., Kal "', , L.G.
Elnctrcphcx,~tic z3tudy (-,f the b,!.-,cd oer-um in
and late Nauch. "i-lidy Kriz. med. ns ':4
486 164.
II kafodru akiiolierstvo. i r1ricko-locrii (zav. - j,f-. Ki..Kll-
Meshcherov) KAvanskngo meditsinskri!yo ~n,~dtutn.

120-5-3/35
AUTHORS: Mironov, Ye. S. L. L. , ZvlagJn, S.B. , and Meshcherov,R.A.
TITLE: An Applicplion Df a Ribhon Len-, t,) t,],c FocuB~-in- of the
External Bea,-,,. -)f a Cyclotron (PrimeneLiye ientochr,,Oy
linzy dlya fokusirovki vypushchemaEo puchka tsi,~lotrona)
PERIODICAL: Pribory i TP'LV,I-,nika Mcsperimenta, 195/, No-51
Pp. 18 - 21 (USSR)
ABSTRACT: An electrostatic focussiiq;, device for the external bea,,,i
of the 1.5 m cyclotron (Ref.1) is de-~cribed. The systei.- is
shown in Fit.1 and consists of a syz:te,:. )f molybdenulr, ribbons.
The system foCUSSeS 4-j_ e bealL vertical direction focussim,
in- the perpendicular direction 'LeinL: carricd )ut by ~, Magnet
(not described 4 1, ti.'s diaper)'. Fil,-. indicates the performance
--::eits ob-.a':~ed usin,7 12 -ev
of the focusEiiic, device. e ;;easur
;protons. TI-e ri,, ~-~ o ns r. si.,.creases the density by a
factor of 10. Particle los--cs did not exceed i0%. The current
2
density at tile tai-Set was 15 I.Alcm
Ye.A. Minin and Yu.D.!. Pustovoyt a.L.L~isted "Lr. tl~is w--rk. The re
are ? diagrars aiid 1 Siavic ref~,.-,ence-
SUBMITTED: December 211, 1956.
AvAILAj3i,E: Library of uori~_ress
uardl/l

21.2100 78318
30V,/89-8-3-3/32
AUTHORS: Meshcherov R A., Mironov, Ye. S., Nemenov, L. M.,
Rybin, S. N., KTi-damovskly, Yu. A.
TITLE: Ion Acceleration in a Cyclotron With Azimuthal
Variation of the Magnetic Field
PERIODICAL: Atomnaya energiya, 1960, Val 8, Nr 3, pp 201-208
(USSR)
ABSTRACT: Thomas showed already In 1938 (see ref at end of
abstract) that charged particle motion In cyclotrons
can be made stable in case of radially increasing
fields if one introduces azimuthal variations in
field intensities. Technical difficulties and the
discovery of the self-phasing principle delayed,
however, the use of azimuthally varying magnetic
fields. The authors tested this kind of field in
1957 on a model of the 1.5-m cyclotron (112 natura!
size). They showed that a combination of' iron and
Card 1/_11 current corrective elements can produce a wide

Ion Acceleration in a Cyclotron With
Azimuthal Variation of the Magnetic
Field
Card 2//1l
78318
Sov/89-8-3-3/302
range of desired field shapes. In 1958 the authors
constructed new full-scale parts for the larfe
cyclotron whose shortest 26.7-m high-frequency
wavelen6th determined the upper limits of the
attainable particle energies. The azimuthal
variation of the magnetic field with a +15% depth
was achieved by means of three segments. The covers
of the accelerator chamber with the corrective elements
are shown on Fig. 1. To minimize the h-f losses, all
iron surfaces were electrolytically covered by arv 70~L
layer of copper. As seenelements 5 were placed in
the depressions between the segments and served to
increase field intensity towards the periphery.
Elements for fine correction were located on radii
between 190 and 260 mm. Figures 2 and 3 show the
central and off-center corrective windings. Character-
istics of the beam were measured by means of two
screened probes. An aluminum filter served to eliminate
charged particles of low energy. The ions originated

in a (~yclutcclll With
Ioll
A~~inwt,'iui Varl"itioll 01'
F ic-ld 7 8 10 "J
4
9
.5.
Card 3/11 see C~tj~(j .111/11

Ion -Acceieration in a
Azimuthal Var-iation of tfit~ Ma.'r;E~--'.
Field
iron element.3 aiid
accelei,ator- c~iiamljc,i-; i,ovei-L~ ot' a~- -elleval,,,-~i- c:iambe~-;
(3) OUtt:1- COPJ'~-' 1 V'-~
corrective elerrI(IfIt's;
(7)
covrective c, -e c v t:- w -! i1.1-,~ 11
C. 11.3 v a ~' J -i r,i
iri~,Ulatul,L; 13 uu bLe r, L;eal ill iJL v
fro m, a ,, t.,i ridar-J Ipc,r ~j~ We "t:
ti~autL-d -'ritu b~., it
ballioti~- 1-cv ~-,d tilt'. wit'l
an u(,cuvacy r)i'
ul, Lfw 1:1,1-i"I V:1110:'-,' ~A' H.
Card 4/ 11

Ion Acceleration in a Cyclotron WIth
Azim.uthal Variation of tiie Magnetic
Field
7, ~318
SOV,,"89-8-3-3/32
3 i
Fig. 2. Central correctlve winding: (1) cover of
accelerator chamber; (2) frame; (3) cop er tube winding;
(4) central disk; (~) copper screen; (6~ detachable
vacuum joint; (7) tubes for water-coolin,~ of frame;
Card 5/11 (8) tightening plate.

Ion Acceleration in a Cyclotron With
Azimuthal Variation of the Magnetic
Field
7831.8
Sovl8c -8 --413 2
2
3
1
Fig. 3. Corrective windings in the troughs: 11)
cover of accelerator chamber; (2) frame; (3) winding;
(4) detachable vacuum joint; ~5~ tubes for water-cooling
of frame; (6) cooper s,_~reen; 7 frame cover.
Card 6111

Ion Acceleration In' a Cyclott-on With
Azimuthal Variation of trie Ma,,-netic
Field
Card 7/ 11
78318
Fig. 6. Magnetic
field interu3ity versus
a riE 1 e(P

Ion Acceleration in a Cyclotron With
Azimuthal Variation of the Magnetlc
Field
78318
S011/89-8-3 -'/-~2
Figure 8 s~?ows the relationship between
the beam current and the radius R. The reiatively
small decrease of current with radius in the
cyclotron with azimuthal variations can be explained
by smaller phane losses and strong vertleal Cocusing.
The authors note that the central. corrective windings
showed no favorable effects and produced (with both
polarities of the added field) only a decrease of the
probe currents. Using an absorber of 190 m -/cm2 the
authors measured an energy of 21.5 mev at a radius
of approximat~:Iy 650 mm, and this agreed with the
calculated value within a 3% error. Energy spread of the
ions was approximately +1.5%, while in the.conventional
cyclotron this spread was approx. +3%. The authors found
also that at the 700 mm radius the beam acquired a much
larger width (more than 15 mm) which enabled use of
Card 8/11 much smaller deflecting electrostatic potentials than those

I-JL Loit L11 :1 (:y 2.1 )L L-')Ik W I Lit 01., J, 1."j
A.. 11,11it'll.-il V:li-.LLL loll (~I* t j;f- 0 V//,
50U0
4000
JOU0
2000
1000
a Ma Ann Rnn
Fig. 8. CUrrent versus radius of probe setting:
N when device woviced aLj conventional cyclotron;
2 for cyclotron with azimuthal variation of ttie
magnetic t'leld.
Card 9/11

Ion Acceleration in a Cyclotron With
Azimuthal Variation of the Magnetic
Field
Card 10/11
78318
sov/89-8-3-3/32
needed In conventional cyclotrons, arid to obtain
outside ion beams ot' energies up to 22-24 inev. The
authors stated that they were able to obtain (using
80-kv potentlals across the dees) molecular nydro_er,
arid deuter'ILINI beams of energies up to 21 mev arid
approx. i,000~1 a. At the maximum energy ot' 23.7
mev the beam current was of the or-der of 200~k a.
The shape of the magnetic field of the 1.5 m cyclotron
coincided completely with that of' the scaled-down
model. N. D. Fedorov, A. P. Babichev, A. S. Knyazyatov,
and V. K. Anokhin took part In the magnetic field
measurements; S. 1. Prokol''yev helped with the covers;
N. N. Khaldin gave advice and took part in constructive
designs; N. I. Venikov serviced the cyclotron; I. M.
Shnaptoev and A. G. Yadykin tested the vacuum; and M. A.
Ye,rorov, V. M. Komavov, V. I. Andruycv, and V. S.
Kalyayev perfoiined the mounting of the devIces. There
are 14 figures; arid 6 ref'erences, 2 Soviet, 4 U.S. The
U.S. reference6 are: E. Kelly, R. Pyle, L. Thornton, Rev.

Ion Acceleration in a Cyclotron With 78318
Azimuthal Variation of the Ma-rnetic Field
Scient. Instrum., 27, 493 (1958); F. H;-*-y.,i, Khoe Kong
Tat, Rev. Scient. Instrum., 20, 662 (1958); H. Blosser,
R. Worsham, C. Goodman, R. Livingston, J. Mann, H.
Moseley, G. Trammel, T. Welton, Rev. Scient. Instrum.,
29, 819 (1958); L. Thomas, Phys. Rev., 54, 580 (1938).
SUBMITTED: August 6, 1959
Card 11/11

893 5 2
S/08 61/010/002/002/018
13102YB209
AUTHORS: M-shcherov R. A. , Mironov , Ye. S.
TITLE: The problem of generating an azimuthally variable magnetic
field
PERIOD:'CAL: Atomnaya energiya, v. 10, no. 2, 1961, 127-130
TEXT; This paper presents a method of calculating the shape of the pole-
piece !3urfaces, which makes it possible to generate an azimuthally variable
magnet:.c field of a given depth and with given radial distribution ~~f the
field i;trength. The authors proceed from the assumption that the pole-plece
surfacs?s be equipotential surfaces. In such a case, the magnetic potential
may, i-i cylindrical coordinates, be represented in the form of
00 2k-1
P(r'T,Z) L: V2k- 1(r,f)z the coefficients can be determined through
k.1 1 'a 2V2k-1 1 lav2k-I I a2V2k--1
the recurrence formula v 2k+1 2k(2k+17 ( Or2 r ?r r2 a y 2
Card 116

P9352
S/06 61/010/002/002/018
The problem of generating B1 02YB209
It is evident that v1 ~ ( )/"Z)Z=o (r,y); the shape of the pole-pe-e
surfaces for arbitrary H (rq) distributions, which may be given analytinal-
ly as well as graphically, can be calculated by these formulas. This prob-
lem. has been solved e. g. by Thomas for Hz = H0 (1+Ar2+Brcos n?), but the
complex shape of the obtained pole-piece profile involves considerable te-h-
nical difficulties of production. However, a variation of the mapnetir
field may be brought about much easier by employing plane sectorial plates!
the field of such pole-pieces cannot exactly be computed, Therefore, the
field strength between the middle of a sector and the middle of a gap is,
for simplicity, assumed to depend on p in the same way as it does in the
case of plane parallel poles of the following shape:
P
-CO 11111,11AVA 11
2D
2d 4 R
P0
Card 2/6

89352
-ie problem of Ceneratlin,- s/089/61/C)10/002/CO2/C)18
B102/B209
11',iis assumption is justified if Ra~) d and R(2n/n - a)~,, d, where R denotco
tLe radius, a the anE71e, and n the number of the sectors. FJC. 2 illus-
4c
Crates the re,-ions on the complex planes -,7 and-z vh. h by means of (4)
+ 2
W d In-
D in e j+ X2
A I/e a~ +1+ ell +11
7iay be transformed,,into one another; (it = d/D). The field between t.he steD-
11-e x-, ( r, z _/d) + 1
,)ed nole-uieces is given by H(W) = HU+iH v = 7iH max "T- 2 5).
1exp(nz/d)+n
and (5) were employed in calculating the distribution Hv = f(u) in the mid-
dle of the plane between infinitely la:~ge stepped pole-pieces; Fig. 3 shows
the result. In many cases, Hv=f(u) ma7 favourably be represented in the
Card 3/6

89352
S/089/61/010/002/002/018
V-e problem of generating B102/B209
form of the equivalent step field (Fig. 2); in particular, this is the case
with the study of ions moving in an idealized field. (6)
.0
A If, (u) du -
0 -X)
11.311C du -
0
Clot In L+12~ - In IGXI (6)
X I-X (I - X2P
is the characteristic parameter of such a field. For comparison with the-orl,
measurements were made at an electromagnet with 370 mm pole-piece diameter
and 90 mm Cap width. Two steel disks (16 mm thick, 370 MM in dioameter)
with sectors (a-52.50, 5 mm thick) attached to them were inserted between
the cylindric poles. The gap between the sectors was 40 mm ;-iide. Thus,.*
d was 20 mm, D = 25 mm, % - 0.8; the central field strength amounted to
Ho . 60OOoe. Agreement between experimental and theoretical results was
Card 416

!~.935'?
S/089/61/01 0/002/002/018
The problem of generating ... B102/B209
the better the longer the distances from the center were. In the case of
50'R--~es
Trudy M01P. Otd. biol. 9227-29 164. (MITRA 18:1)
1. veditsinAly ins,.i*,.uT-, g. Bla~--mreshcheisk.

SIKACHEV, V.A.; MBSACqIT;N~~YA, M!,
7.
Com~arator manufactured by the Experimental Optical and Mechanical
Factory of the Central Scientific Research Institute of Geodesy,
Aerial Surveying and Cartography. Geod.i kart. no.l.'32-36 Ja 163.
(HM 16:2)
(Masuring instruments)

3(5) PHASS I ODOX KXPL401TATIOII SOV/22 14
UPSH. OlAwnoya upravlonlya geQ20gll I okhrAn7 n*dr
Goologl:ys I neftegaxonoanout' Voatochnoy Sibirl (Geology and Oil- and
Gas-bearing Possibilities or Ustern SI. beria) Moscow. aostop-
takhudat. 1959, 486 p. 1,650 copies printed.

Additional Sponsoring Agency: Vostochno-Sibirskly neftegeolOgiChookly
%mat.
Zd.a V 0. Vaell'yevI ftecutive gd.t To-.0. Pershinal Teoh. 2d.1

FMPWII The book is intended fm geologists Interested In the
strattgraphy, lithology, tectonic*, and the all- and gaa-bearing
posai4ilitiss or the Eastern Siberian platform and Zabaykallye.
COTBRAM This aoilection or articles contains materials on the stra-
t1graphla 01ASWication. and 11thologic crA-rac terio tics or sedimento
of the Cambrian system and of the so-called 'ancient" bada devel-
oped along the northern slope or the Eastern Sayan Mountains and
_
t
the western lit oral ~r n th
~" Baykal. Extenfilva informa'ilon 0
PQtrQsTaph7 and paleontology of theag deposits in Presented. A
number Of articles don I Ith the tectonics Of the 60utfto~ part of
tha Siberian Platform and its Oil- And 9AB-boaring poobibilitto8
Of the BAYkal-typs deproamlans. There are 40 tablea, 74 risures,
and 4 obarta. There are 205 Soviet references.
TAMA OP CORTUnTs,
From the Sditor 3
Ka"amV. ". Lith010610 - StrRtlgraphlo and 0400hoMical
Characteristics Of Rocks Of the Southern Part of the
Siberian Piatrarm 8
Tdakkawvskiy, N.A. ComparIng the Str&tigrAphIc Sootiona of
the larly ftlaoxoia Series in tha 3outhorn prIngea of the
31bel-lew Platform 287
X"YukhlA&, A-V. Lith-10910 Characteristics and the Outlook
for gas- and 011-bearing Possibilities In the Motakaya
Sulta Of the Lower Cambrian Of the Southern Siberian
Platform 249
00272onev, A.Z. Faclea of the Lower Cambrian Sedimenta In
the SOuth6rn Part of the Siberian Platform 268
111yasova, Z.Kh. and L.A. Lyeava. Spores In the Lower
Cambrian Sediments of the Southern Part or the Siberian
304
Platform
imova. Pauna of the
1
lAbod'. and
.
0a
'
'
a - F rl d n .
t
h
M.-r h
,
;laAe U;T Lan Pe Southern rart or
d
the Siberian Platform 312
za"huk. P.3 1A.H. Per1kova, and Yo.H. NO oil-
aacumulati~8_P-F0-P_0RfG_4 01
Sediments 325
Cambrian Sediment* of the Middle Course
Ox
xwa River 336
Now Data an the Tectonic* of tno Southeastern
SiberiAn Platform 356
jamarajoy, I.M. and V.V. 3a=aorqv_, Geological Structure and
the Oil- and 0an-bearind POSSI-billtlea of 'he Solonginakayn
Depression 435

The
YAal1'rjV- Y-G., 3 H, (LA0hkLQvtcft. and E.N_L~~hnev*K
Problem of Interpreting Gravlaotric and Magnetic Data for
the Southern Part of the Seat Slborlan Platforc, 475
Paleontologic Plates 409
AVAILAWAs Library of Congrosa
KM/ad
a-20-59

S'009/601/000/008/00r-/00~;
B027/BO76
AUTHORS: Per1kova, Ya. N,, Meshcherskaya, Ye. N.
TITLE: Reservoir rocks in Lower Cambrian deposits of the Irkutsk
Amphitheatre
PERIODICAL: Geologiya nefti i gaze, no. 8, 1960, 28-33
TEXT: In the general problem of oil and gas prospecting in Eastern
Siberia the search for reservoir rocks occupies a special place. In the
territory of the Irkutsk Amphitheatre research work is being carried out
by the geological Trust Vostsibneftegeologiya, mainly in the Lower Cambrian
deposits. Drilling has already shown here that oil and gas were present,
and that, moreover, this cross section is the best sealed off. The lower
part of the layers consists of carbonate sulfate deposits and the upper
part of terrigenous rocks. Two types of reservoir rocks were determined,
i.e., granular and cracked. Among the granular reservoir rocks, the
sandstones in the region of Moty which were divided into four layers are
of interest. The first zone of these layers extencb -111ong the Sayan Range
Card 1/2

S/00 60/000/008/'005/005
Reservoir rocks in Lower Cambrian depositB ... B027YB076
from southeast to northwest and shows the highest porosity and
permeability. The second zone frames the first one and is less favorable
with respect to the properties of the reservoir rocks. The cracked
reservoir rocks were studied according to the method of Ye. S. Romm and
L. P. Gmid, coworkers of VNIGRI, which consists in determining porosity
and permeability in flat parallel sections over large areas. The study
of the carbonate cross section of the Lower Cambrian was carried out in
two horizons, i.e., the Osa horizon an] the horizon between Bellsk and
Usol'ye. These two horizons, especially that of Oua, show a marked crack
formation probably extending over the whole investigated part of the
Irkutsk Amphitheatre. There are 5 figures and 2 Soviet-blcc references.
ASSOCIATION: Trest Vostsibneftegeologiya
Card 2/2

Y A,

/,I
, ~ -- ~ V
- " ~C~
/) ~-: ~, ~~ ': ~ , I;-- . ,-) e /, I
KZSHCHERSKIY, A.; TAGAROV, Z.
- wom~-,-
Y: historicogeographical data
89 no.4:359-362 JI-Ag '57.
(Amur
on the Amur. Izv.Tses.geog.ob-va
(MIRA 10:10)
River)

RITIN. I.1., Imnd.tekhn.nauk; MESHCHERSKIY, 1.11.
From the e-,-?~3rlence of leveling in regions of Mgh 7~,.-,intains. Geod.
i kart. nc.t:?-10 Je 15e.
(Leveling)

- LAESHCHERSKIY, I.N.
Invar rods with a single graduation scale. Geod.1 kart. no-5:60
W 161. (MM 14:6)
(Surveying-Instrumenta)

WSHCMSKIY, I.N.; ENTIN, I.I.
Study of the NB-4 level. Geod.i kart. no.4332-34 AP 162-
(KRA 15S12)
(Level (Surveying instrment)-Testing)

I.N.; FAMN, I.I.
Leveling errors caused by the use of invw rods.
Trudy Tsmiuix no.147:65-91 162. (MM 15:9)
(L-eveling)

MSHCHERSKIY. I.N.
Sow sources of errors in the operation of an M-2 level
with a compensator. Trudy TSNIICAU no.147:93-98 162.
(MIRA 15:9)
(Leveling)

ENTIV, I.I., kand.tekhn.nauk; )SSHCHERSKIY,...J.N.--
Determination of vertical displacements of the earth's crust in
the Surkhob Valley, Trudy TSNIIGAIK no.154:91-106 163.
(KIRA 16:9)
(Surkhob Valley-Earth movements) (Leveling)

MSHCHERSKIYi I.E.
---, 1 , ~- -1 --- -, , ~r- '-'- ---
NJ-b3 level with a self-adjusting line of sight. Gaed. i kart. no.6:
6-11 Je 163. OMI.U 16:9)
(liungary-Level (Surveyin4 instrunent))

YESHCHERSKIYY I.n.
Making allowance for systenatic errors of self-reducing levels.
Geod. i kart. no.10:77 0 163. (MIRA 16:12)
vl~ -p--- :2~

ACCESSION NR: AP4038949 S/0006/64/000/005/0018/0023
AUTHOR: M.eshcherskiyp I. No
TITLE: Investigations of the Level KONI 007
SOURCE: Geodeziya i kartografiya,, no- 5s 1964, 18-23
TOPIC TAGS: surveying instrument, surveying level, earth measurement, level KONI
007, level NB 4, level Ni 004, level NA 1, level No
ABSTRACT: The author described quantitatively the results of field and laboratory
tests evaluating the surveying level KONI 007. Data were presented on the optical
qualities, weight, and size of the instrument; measurements of longitudinal and
transverse precision were taken and presented in tables. Further tests were
performed to quantify the instrument's behavior under varying distance and ambient
,temperature conditions and also for various manners of inatrument setup. Tabulated
results include mean quadratic error calculations. Field tests involved observa-
tionz of instrument performance in foul and windy weather and under conditions of
vibration. The author indicates general satisfaction with the instrument's
characteristics. The levels NB-4.. Ni-004, NA-1. and NG were used in making the
Card 1/2

ACCESSION NRs AP4038949
tests. Orig. art. hasr 2photographs, 8 tables, and 10 equations.
:ASSOCIATION% acne
~SUBHWTMt 00 '0.
,;SUB OODS: PS NOW SOVS 001
C6-rd 2/2
ENCL: 00.
OTHERt 000,

L 44243-66
ACC NR, AT6011151 SOURCE CODE: UR/3197/65/000/002/026i/0266
AUTHOR: Meslkc~e I. N
ORG: Central Scientific Research Institute of Geodesy, Aerial__1__L//___
Surveying and Car o__ -(To e n -tr al I nij r~au3 ovatellskiy
e~~aphy
"t tut geo
aeras"yemki i kartograf i i
TITLE: Repeated leveling at the TsNIIGAiK polygon
SOURCE: AN EstSSR. Institut fiziki i astronomii. Sovremennyye
dvizheniya zemnoy kory. Recent crustal movements, no. 2, 1965,
261-266
TOPIC TAGSi geodetic leveling, geodetic polygon, rexpe
1=eN_--eiAng, instrument
ABSTRACT: Results are preMen 0 for the first-order repeated leveling'
(1958, 196o, and 1963) of the TsT1IIGAiK polygon located just north of
Moscow. The accuracy of the leveling was evaluated by three different
methods, and conclusions have been drawn concerning the changes in
relative elevation between adjacent bench marks. The total mean square
errors (m,, M29 M3) per km for the first-order reciprocal leveling,
along lines 9-10 km in length were m, = tO.53 mm/km (deviation of
individual measurements of relative elevations by sectors from the mean
Card 1/2

L , ".I ii6
ACC NR: AT6oill5l
values from all repeated leveling), M2 = 10.50 mm/km (closing errors of
closed loops and M3 = k0. 40 mm/km (by the differences d = hfor - hback)*
At the turning stations and wherever the soil conditions are unfavor-
able, better results are obtained if smaller polygons are established
with 5 or 6 bench marks. These should then be leveled several times
in the interval between successive repeated first-order leveling of
the whole line. Thia method will provide an opportunity for using
only the moot reliable bench marks for the study of contemporary crustal
movements. Inherent large errors in third-order leveling make it
unsuitable for studying contemporary movements or determining bench-
mark stability. Orig. art. has: 3 formulas and 3 tables. (Sil
SUB CODE: 08/ SUBM DATE: none/
Card 2/2