SCIENTIFIC ABSTRACT MILRUD, S. S. - MILSHTEYN, I. M.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R001134320015-1
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: January 3, 2017
• Document Release Date: July 31, 2000
• Sequence Number: 15
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

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SAVIBVICH. I.A.. inzh; MILISHIM, R.S.., insh.; ZFIZLVAKOV, A.A., inzh.
High frequency moisture meter. Ogneupory 18 no-9:396-400 '53.
(MIRA 11:10)
.I.Saullukakly shapotny7 zavod.
(Refractory materialv-49ating)

137-58-6-13808
.Translation from: Referativnyy zhurnal, Metallurgiya, 1958, Nr 6, p 372 (USSR)
AUT14OR: Mil'shenko, R.S.
TITLE: High-frequency Apparatus for Rapid Determination of Moist-
ure of Green Brick (Vysokochastotnyy pribor d1ya bystrogo
opredeleniya vlazhnosti syrtsa)
PERIODICAL: Tr. Nauchno-tekhn. o-va chernoy metallurgii. M-vo chernoy
rne,.allurgii SSSR, 1957, Vol 12, pp 288-290. Diskuss. pp
299-347
ABSTRACT-. A high-frequency moisture meter (HFM) was tested and in-
troduced into production at the Semiluki refractory-brick plant
for determining the moisture of green brick, semi-dry-pressed
after drying, which usually fluctuates between 1 and 576. The
operating principle of the HFM is based on the variation in the
dielectric constant of a condenser-type probe depending on the
moisture of the green brick being tested. The arrangement of
HFM consists of two sonic-frequency generators, an amplifier,
a power-supply block consisting of a transformer and a keno-
tron, a dynamic indicator, and the condenser-type probe be-
Card 1/2 tween the plates of which the green brick to be tested for

137-58-6-13808
High-frequency Apparatus for Rapid Determination of Moisture (cont.)
moisture is clamped. The dimensions of the condenser-type probe are 120
x 200 x 300 mm, the weight 6.83 kg; the weight of the apparatus aside from
the condenser is 9 kg. The apparatus works on a 220-v A-C current. The
nondestructive determination of moisture on green brick by means of the
HFM requires 30 sec. The precision of the determination of the moisture
content depends on its absolute value. 70% of results fall into a range of dev-
iation of :k Z5o for moistures of the green brick up to 1. 1%; 9 1% of results
fall into a range of � 0.556 for moistures up to 5.756. The preservation of
whole green brick through nondestructive control determination of moisture
in dried products saves the plant 200, 000 rubles a year.
S.G.
1. Rcl-rac*Lory mazeriais--Moisture conten7~ 2. Refractory materials--Tesc results
3. Mjisture meters--Deoi,,-n 4. Moisture meters--Equipment 5. Misture -zieters
--Operation
Card 2/2

n*& rto d2 teswting frwom the prodne
"n ,
sttEmKo kogne
F

C'~70 f4eo-p i. q

a- blgh In Lfro
late from thdjfM'dM!uft
-I
So itlushenko. 0 "ry nhnl~!
---%tmWNWrExnrOduCed it t t M, gi 9 i1i WhlCb , Cr
.orcs Are reduced "d the MI tat arothe raw materi"r it now
61 refmctory. They castuda I (d-AhOl)
N42011AIA ("Ovorundum")- a an slan and
'0" it 0". 1
metal drorplets 2-6%. Th-a a1"11 content it rtlatively high
("%). ~ The optical propaties ot thL 0-cortindum are
U - 1.682 and I - 1.6m, but thtse may be Inercmd to 41 -
1.70-4,71gand's,-:1.69a !~- LrAs-hygiftil'of C(gh, The
dl

.7. r ~~ '.
AUTHORS: Zhi-kharevich, S.A. , Geman, I.A. , Kozyra-,a, L,A. , .1 -- 4 -0/
Savktvich, I.A., lfil'shenko, R.S., Konetskly, N.V
TITLE; The Producl"-Ion Techno-1-ogyof-El-ghly Aluminous DerL,,-. Prodi;c-~-.;
Using the Dispersed Concentrate of the Aktasb Ocourr-~nca
(Tekhaologiya proizvodstva vysokoglinozemislykh piotnykti :.zde1-.y
s primeneniyem. aktashskogo diasporovogo kontsentrata)
PERIODICAL: Ogneunozv, 1958~ Nr 4, pp~ 175-179 (USSR)
ABSTRACT: Experiments showed that this dispersed concentrate ia not eazily
caked together at high temperatures even if previous.'Lly V_n,.-:4y
crushed. Further, the result of petrographic investigations car-
ried out by N.V. Gul'ko is given. An illustration shows the prop-
erties of samplea from ioo~; aisperseJ concentrate of the Ak-1,&shSk
ocaurrence at a pressure of 200 kL7/cm2 &ln3 a burning temperature
Of Up to .47000. If the dispersed concentrate is bumed twi:;e it-4
quality ia improved but the working process is rendered more aom-
plicated. Experiments were therefore carried out in which previ-
am3ly burned and finely ground dispersed concentrate is u3ed 8-3 a
Card 1/3 dust-.like component of the fire-clay mass (dispersed fire c"'ay).

The Production Technology of Highly Aluminous Dense 13 r1r_- 4- ' 0/47
Products When Using the Dispersed Concentrate of the
Aktash Cocurrence
The properties of dispersed fire clay and of such made of technIcal
alumina and clay arr. given in table -1. The characteristic of the
masses and the properties of the onxde samples Z; be aeen frum
table 2, and -those of samples burnt at 15,200 from tab'.--! Flu-rthler-
more, an inlustrial quantity of blast farnace bricks of the Icype
D-2 was male. The gr9mulation of the firti clay is shown in table 4.
and the characteristio of the mass and the raw products are showr.
in table 5. Conclusions: -1.) By a joint application of the di--4-
persea concentrate and technical al-andna it is possible to ob~w_,r.
highly al=1r_,ouA dense products. 2.) The dispersei pro-
ducts with a porosity of less than !'--% ha-Te !L goo! s~-.ructur-,., -~hiy
are of low permeabilit,~ for smelts and gases, and ha-:i-e 9. -;;-ol:..ure
stability at 1500--1550 - It is ri)commenled ho intensify the sear.-h
for dispersed ores on the cond",tion that cost3 are considerably r-i -
duced. There are 1 figure, 5 tables, and 5 references, L of wh:~ch.
am Soviet.
Card 213

The Production Technology of Highly AluminouB Dense 131-58-4-10/17
Products When Using the Dispersed Concentrate of the
Aktash Occurrence
ASSOCIATION: Kharlkovskiy institut ogneuporov (Kharlkov Institute for
Refractories)
Voronezhakiy Sovnarkhoz (Voronezh Economic Council)
Semilukskiy ogneupornyy zavod (Semiluk-i Plant for Refractories)
Card Y3

15(2)
AUTHORS: Millsheako, R. S., Petrova, Y. D. SOV/131-59- 7-1 4/18
TITLE: Application of the Sound Method to the Classification of Chamotte
Products (Primeneniye zvukovogo metoda dlya pauportizataii ohomot-
nykh izdeliy)
PERIODICAL: Ogneupory, 1959, Nr 3, PP 141-142 (USSR)
ABSTRACT: The Semiluki plant of refractories carried out experiments together
with the Vsesoyuznyy institut ogneuporov (All-Union Institute of
Refractories) using the sound method determination of the coefficient
of elasticity for the control of the quality of chamotte products.
The dependence between the apparent porosity, the pressure-rupture
resistance and the frequency of ei6en oscillations of the products
was determined. For this purpose the device ICbb!K was used which
was produced by the Leninbradskiy elektrotekhnicheskiy institut im.
Ullyanova (Lenina) (Leningrad Electrotechnical Institute imeni
Ullyanov (Lenin)). This device permits the testing of whole bricks
without destroying them. Thus, a considqrable amount of bricks was
saved without any destruction. Usually the bricks had to be crushed
for the control-tests of the individual parts. This control method
Card 112 is to be applied also to other refractories.

SOV/131-59-3-14/18
Application of the Sound Method to the Classification of Chamotte Products
ASSOCIATION: Semilukskiy ogneupornyy zavod
(Semiluki Plant of Refractories)
Card 2/2

f ') N
"iTYORS - Mil'shenko, R. S., Kbosid,
M, BO!5/BO08
j,
_
_
E. Production of Ladle- and Regenerator Bricks From Raw
of the Arkalyk Deposit
~&neupory. 1960, Nr 2, PP 53-57 (US9R)
M The authors describe the two variants used for the
one with Itit-h alumina~~C'ontent and a basic ones Tti;-
cQrpo-,ItIon and refractorinend'of the raw materia'A~L
~L-)red ir- table 1, and the chemical composition
ir 2, The production of the chamottp with
ccy.'I~,nt for the experimental batches as well as the 1-1-1
invocti,mitiono of the raw masses are described neyt~
n3rison purposes, the masses A3 and A4 wore
hiph chamotte content, the grain of which crin bi~)
tlf'~Ir- 3~ TI-Le composition and properties of thf-.
the!;e batches are mentioned in table 4, The i)rodur-,ibn
bricks front the, variant with high alumina content
next~ The products complied with GOST 5341-50 an,:
1/3 ntandards for ladle bricks with high alumina

Yroduction of Ladle- and Regenerator Bricks From S/13
BO!r-. OOP
Raw ;11'aterial of the Arkalyk Deposit XB
characteristic of the experimental ladle bricks ic
in table 5. The properties of the regenerator br2cks Ti--',A-. 1--111
alumina content, which surpassed those of t-r-e
of the CMTU 5235-55~, are mentioned in tabl-~ 6. 01-c-rolLt-2
bricks from the basic Arkalyk variant were oressk!d
mentally on the press of type SM-143~ A wei7ht b%- volu-,- -2'
to 2,28-2.30 g/cm3 was obtained (Diagram). It iz3
elusion that ladle bricks having a much Crpafer
the customary ohamotte ladle bricks, can be ri~an-uf t
the Arkelyk variant with high alumina content without
additives. The regenerator bricks from chamotte Qf 11I.--
with high alumina content and Latnaya clay can 't(-
used in regenerators. They are less soiled by th(-,
smelting dust than chromium magnesite bricks,. Obamotti-;
bricks with the same stabilit as the customary lf-MI-I
of' the Borovichskiy kombinat ~Borovichi Kombinat?'
factured from the basic Arkalyk variant without nlay nLO-Ji.-
tives; By increasing the amount of pressure applied, tht.
Card 2/3 stability of the brick can still be increased. There ar..

Production of Ladle- and Regenerator Bricks From S/13l/60/000/02/002/014
Raw Material of the krkalyk Deposit B015/BO08
I figure, 6 tabjes, and 2 Soviet references.
kSSOCIkTIONt Seailukakiy ogneupornyy zavod (Semiluki Works for Refractories) .-"
Voesoyuzny,5 institut ogneuporov (All-Vnion-Inatitute of Re- -
fractoz
Card 3/3

STAVORKO 9 A. P. I tq~ ~HE Q*-R.46-
Production of blocks having a high alunins, content for blast fur-
nace we-Use Ognsupory 26 no. 2:53-58 161.
- (MIRA 14:2)
Is Sexilukokly ogneupornyy zavode
(Blaut furnaces) (Refractory materials)

89980
[!~-22_00 12,1~5 11~17~
S/131/61/000/004/001/003
B105/B202
AUTHORS: Voronin, V. I., Krasotkina, N. I., Stavorko, A. P.t
Mil'shenko.-R.",
TITLE: Experimental industrial batches of carborundum
refractories with silicon nitride binders
PERIODICAL: Ogneupory, no. 4, 1961, 157-163
TEXT: The authors study carborundum refractories with silicon nitride
binders. The production method has been developed at the Vaesoyuznyy
institut ogneuporov (VIO) (All-Union Institute of Refractory Materials)
and tested under industrial conditions at the Semilukakiy zavod (Semiluki
Works) in cooperation with the VIO. A test batch of these products was
produced with the masses being burnt at 15000C. This batch was
designed for firing with anthracite coal of a particle size of from
2 to 8 mm. The following parameters have to be taken into account when
producing the industrial batches: effect of the amount of sulfite
alcohol slops and the humidity of the mass on the quality of the blanks;
effect of various modes of introducing the blanks into the furnace on
Card 119

89980
S/131/6-1/000/004/001/003
Ex-perimental industrial batches B105/B202
the properties of the productsi effect of the duration of burning on
the properties of the products. The mass consisted of black carborundum
nos. 24, 30, 120, 150, crystalline silicon XP-1 (KH-1) with grains of
a size up to 0.06 mm. At a pressure of 5-6 atm products with
dimensions of 240 X50 X50 mm were rammed from the masses containing
80-70% SiC and 20-30% Si. The composition of the masses and the
properties of the blanks after ramming are given in Table 1. The good
blanks were dried on air during five to seven days. Subsequently, they
were burnt in the tunnel furnace in ceramic and carborundum casings
and in the muffle furnace. Porosity of the products after burning was
11-14%. Compressive strength and properties of the burnt products are
given in Tables 4 and 5, respectively. The free silicon content in the
products impairs their strength as was observed in earlier investigations.
Table 6 shows the indices of the test batch as well as of the carborundum
products with silicon binders of the Semiluki Works. The chemical
analysis was made by K. S. Kolobova. A. N. Alekseyeva studied the ground
sections and the immersion. The chemical analysis and the study of the
microstructure showed that with low burning rate only 2.7% of silicon
remains in free state, its major part, however, is transformed into
Card 2/9

89980
s/131/61/000/004/001/003
Experimental industrial batches ... B105/B202
silicon nitride and.si.licon carbide. Conclusions: The production
technique of carborundum refractories with silicon nitride binders which
has been developed by the VIO and in the Semiluki Works warrants higher
qualities than that with the ordinary silicon binders. Pinal conclusions
concerning the quality of carborundum refractories with silicon nitride
binders can be drawn only after checking their working stability. The
editors add that the homogeneity of the products from different muffles
and the change of the properties of the products with free silicon at
high temperatures must be studied in the oxidation medium. A method of
eliminating free silicon must be.developed. There are 3 figures, 7 tables,
and 1 Sovi.et-bloc reference.
ASSOCIATION: Vsesoyuznyy institut ogneuporov (All-Union Institute of
Refractory Materials) Voronin, N. I., Krasotkina, N. I.;
Semilukskiy ogneupornyy zavod (Semiluki Works of
Refractory Materials) Stavorko, A. P., Mil'shenko, R. S.
Card J/ 9

89980
s/i3l/61/000/004/001/003
Experimental industrial batches B105/B202
Legend to Table 1: A) Composition; 1) carborundum, %; 2) silicon 0.06 mm,
%; 3) sulfite alcohol slops; 4) humidity of the rammed mass; B) character-
is-tic values of the blanks 5) volume weight, g/cm3; 6) amount of waste,
%; 7) cause of waste; a transverse cracks; b) longitudinal cracks;
c) various
C."'As &MCC a CeONCTei CUPIta
KAP60P YNjt. % C. C . 6.
""OCT

24

20

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C Koillmeeng

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I
TOK
%

56 24 20 1,290 - 1
5 27 5o noylepeqnble Tpem"Iffil
184

2
56
24
20
1,28
6,2
3
3:
27
40
1
r1poAOnblibie TpetXIIIJbI
3 56 24. 20 1,28 5
1 35
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4 56 24 20 1 28 5: 20-
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1 2 7 to
5 56 24 20 1:27 4 0 2:0-
1:5 2:7 >1 Pa3ftll~)
6 49 21 - 30 1,27 4:5 2.0-1.5 2,6-2.19 2-5
Card 4/9

Experimental industrial batches ...
Legend to Table 4: compressive
strength or, in kg/CM2 after
;01
burning in the tunnel furnace
with T8 lorries per shift;
1) no. of the mass; 2).mean
value;
899~0
S/131/61/000/004/01/003
B105/B202
Ta6n"ua 4
flpejteA HSACANO nP" -CRATOIN
, "a CX
="
Ica/ext .
1 M r a 8 TY11MCAhWOA ReRR
C r1rorsAxwea"mem IS varoweTOK 8 CMeHy N
AOflOAMNTeJb1fOA RUAeP)KKOA tta47-9 nomi"m
r& A MACCU: GCM. KOICA,
1 2 3 MAN"

1290 1404 785 1159
1184 1140 1231 1183
1212 1334 1461 1336
1280 1170 730 1060
1400 - 940 1170
892 8W 1440 1074
qa?~4-5/9-

899SO
S/131/61/000/004/001/003
Experimental industrial batches ... B105/B202
Legend to Table 5: properties after burning in the tunnel furnace with
16 lorries per shift: 1) water absorption, ~6; 2) volume weight,
g/cM3 ; 3) porosity, A 4) compressive strength of specimens taken from
various points of the product; 5) mean value; 6) Si content in.the
mass;
Card 619

S/131/61/000/004/001/003
Experimental industrial batohes ... B105/3202
CmIcToa usAeaml nocae adn"ra a Tyoomeim9iol netom npoo npoTaimmsaim
18 oaroxaox a cutoy ma ffo3Ku"*x 40-51
BOAMWAD. 06MUNNI nopucTocTb fIPeA*A DPO-ONOCTR "PR CXNTMN 06PASQ06 WS PA3"b1X
14""" - Sec wecT msAeAnx. Nelem'
% % J* I J* 2 M 3 M 4 CPtAHMA
4 --3 -- - -1 - -
COAep)KaHme SI a macce 20%
- - 880 -- 1616 1812 1436
-4.3. 2,64 11;4 1530 t310 1096, - 1312
- -
840 1640 - 1480 1320
4,3 2,70 11,5 1750 1823 1824 1623 1756
- - - 1250 1610 1883 2380 1780
- 1520 1314 1461 980 1319
Cojiepwnitiie S1 a macce 30%

804
1540 670 1 1133 1287

-
1
1250
1
1530 1
1 1 art
Card 7/9

89980
S/131J61/000/004/001/003
Experimental industrial batches ... B105/B202
Legend to Table 6: initial composition of the masses and indices of the
products of the test batch: 1) composition of the masses, ~q 2) method
of intruction into the furnace; 3) number of lorries per shift;
a) good products; 4) number of pieces; 5) total weight, kg; 6) volume
weight, g/cm3; 7) porosity, %; 8) compressive strength kg/cm2;
9~ temperature at the beginning of destruction; b) experimental results;
c flat; d) standing; e) industrial products;
Card 8/9

S11311611000100410011003
Experimental indus tria l batohes B105/B202
To6AHLIA 6
MCKOANUA Co"aa M4CC 01 noKg3aTejjm N;ACA*A OnUT1104 V18PTHM
cocTs; wmcc
A, rOA"MQ P:;
APS
~
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f 19
J
9.
-
COAXO %OMPA.
-

for
81

Awa 11"611 U.
C71xTh ocx TypA
"Mqajla
81CA14 KICAI
% P03PYEUV
111111. ,c
Onb1 THUe

80 20 He VjtatUKj
, 16% 1589 2782 2.68-2,74 8-10 1300-!800 >1800
80 20 ,
v IS- 590 1032 2.68-2.70 10-13 1000-1300 >1M
80 20 * 18 1160 ION 2,67-2,50 11-14 800-1000 -
80 200*0 Ha Topeu(j 18 450 756 - - Boo -
70 30 Ha nASUMI(p 160 174 2V 2 68-2 70 10-13 1000-1300 -
70 70 9 18 423 710 2:68-2:70 10-13 5W-800 -
onpommmAetiH me 11SMimm
100 2,35-2,50 18-24 300-700 1530
Card 919.-

MIL'SH&NKO, H.S.; KARASI, G.Ye.
Modern methods of testing refractories and their quality control,
Ogneupory 27 no.2:94-95 '62, (MIRA 1_51:3)
1. Semilukskiy ogneupornyy zavod.
kRefractory materials--Testing)
(Refractories indU5try--(~uality control)

'HILISHENKO, R.S.; KARASI, G.Ye.
Rapid complexametric method of separate
Fe6031 and Al203in refractory materials.
57 63.
determination of
Ogneupory 28 no.12!
(MIRA 16-12)
1. Semilukakiy ogneupornyy zavod.
To

KAZAIMVICII) S.S.; MOSID3, G.m.; i-aKiIAYLO%'A, L.I.; KUM.TSiUY, N.V.; 1-11LISHLIKO, "(.6. "4
TIHIOn'YEW, A.F.; KAi~AW, G.Yo.
Durmed fireclay blocks for capILCity blast furnace stack-3.
0
Trudy Inst. ognoup. no.34:3-27 163. (1aAA 17: 10)
1. Vsosoyuznyy institUt o,,iiu,u orov (for ',lilchiLylova). 2. Somnlukskiy
ognoupornyy zavod (for Karaol~.

WLISHENKO, R.S.; KARASI, G.Ye.
Work carried an by the Central Factory Laboratory. Ogneupory 29 no.2:
92-94 164. (MIRA 17:1)
1. Semilukskiy ogneupornyy zavod.
,~?k;!-4
- -

MILISIMMO, ReSt; KARASt, G,Yeo
Use of high-alumina and ordinary grog burned Ir rolary klins.
OgneuporY 30 no.1:5-8 165, (MIFA 23-3)
1. Semilul:skiy ogneuponV7 zavode

-j;.)784
11/6 1 /'003/011/021/056
414
AUTHORSt Gubkin, A. N., and Mil'shina, Y,, A.
TITLEt The role of residual polarizat:t-:. -.r the electret effect
PERIODICALt Fizika tverdogo tela, V. 3, nc.,-,. -;96,, 3376-3382
TIM The conclusions drawn from the phen-,it--%~ -i:mg-'~:al theory as to the
important role played by residual polariza-I---;-, iz- the eleotret effect are
shown to agree with experimental data. principal characteristics
of the phenomenological theory of electret6 N. Gubkin, ZhTF, XXVII, 9,
1954, 1957) are discussed. According~to th',j Lhecry, the electret effect
is due to residual polarization. The resid%al pciarization was investigated
by the depolarization technique. Fig. 2 gi-ii-i --j. qualitative account of
experimental results, and quantitative data ti-fs t--,,.,mpiled in Tables 1 and
2. Experimental results obtained for vimposed of CaTiO 3 and
CBT (80-3% SrT 103and 19-7% Bi 203* 2TiO 2) are pre-,ented in Figs. 3 and 4.
Two groups of phenomena are observable ir, electrets containing
absorption charges and residual charges. V. irnthilate the latter, the
Card 1/11~

3c'%
i"'/61/003/011/021/056
The role of residual polarization ... h-Z'-j/b',04
sample has to be heated above the polarizat-: n In all the
materials tested (for exceptions see Tables a;id 2), the absorbed charges
(6ab) and. the residual polarization (P) ran 1, `rv;reased by raising the
temperature and prolonging the pulse duratj.--.. The temperature-independent
relaxation time of absorbed charges is 1 m1n. The relaxation time
of residual polarization is 2 - 4 hr at 2,)C'1-C and increases sharply as
the temperature drops. If the absorbed are- not due to high-
voltage polarization, the observed residua- c.ar'lzation cannot be
explained as being due to the usual types ~f -inear polarization with long
relaxation times. A residual polarization ~A coulomb/CM2, which is
similar to that of inorganic electrets, is c'-~jerved in wax electrets. The
stable charge of electrets was calculated fi-1,--, th-.- experimental values of
P andr to be 6- 10- 10 coulomb/cm 2 for eleatrets and
M
10-8 coulombs/cm 2 for wax el*ctrets. A(~,;c:ding to theoretical
calculations and experimental results, the drawn from the
phenomenological theory as to the role of polarization in the
- ,I ~esnlts. Ferroelectrics
electret effect are consistent with exper-r.-~
Card ;X'~

lii 1/61/003/011/021/056
The role of residual polarization ... E125/B104
with a thermodynamically stable residual polarization need not have
eleatrat properties aince - and tend to infinity. There are 4 figures,
2 tables, and 5 references# 4 Soviet and I non-Soviet. The reference to
the English-lanpuage publications reads as followss B.' Gross. J. Chem.
Phys., 11, 10, 866, 1949-
ASSOCIATIONt Fizicheskiy in.stitut im. F. N. Lobedeva AN SSSR Moskv&
(Physics Institute imeni P. X. Lebedev AS USSR, Moscow)
SUBMITTED- June 12, 1961
Fig. 2. Order~of experiment and data.
Fig. 3. Experimental rusults for CaTiO electrets. Legendt 0)
2 3
Coulomb/cm ; (2) t time, hr
Fig. 4. Experimental results for CBT electrets. Lejend's For designation
see Fig.
Card 3~~

BARU5,
w
Concentration of ascorbic jLcid in lungs and other tissues of white
rate in experimentma silicosis. Ukr.*biokhim. zhur. 32 no.5z734,-
741 160. (KERA 3J,:.1)
1. BiAhimiche'Okaya laboratoriya
truda, g. Stalino.
(LUNGS,-DUST DISFASES)
Donetskogo inatituts. fiziologii
(ASCORBIC ACID)

SHANGIN, N.I.; MILISHTEYN. B.L. (Omsk)
Omsk, a gardbn city. Felld. i akush. 26 no.8s4l-46 Ag(161.
KIRA 14;10)
(OMK-CIVIC IITROVE201T)

S/165/60/000/005/001/003
A1o4/A12q
AUTHOR: Millshteyn, D.M.
TITLE: Tectonic development of South-East Turkmenia
PERIODICAL:' Akademiya nauk Turkmenskoy SSR. Izvestiya. Seriya fiziko-tekhni-
cheskikh, khlmicheskikh i geologicheskikh nauk, no. 5, 1960, 3 - 8
TEXT: The tectonic development of South-East Turkmenia since the Paleozoic
era is described on the basis of available geophysical and geological material.
It is assumed that the inversion of the sub-Paleozoic geosyncline occurred at the
end of the Caledonian and the early stages of Hercyan cycles. This opinion is
confirmed by: analysis of geomagnetic anomalies, deep seismic sounding of Ted-
zhen and-Karabekaul areas carried out by K.Ye. Fomenko, seismic data provided by
Yu.I. Sytin and N.K. Bulin, and the discovery of upper Paleozoic sedimentary
rocks in the Bukharo-Khivinskaya stage by V.Ye. Khain. Anomalies of the geomag-
netic field show a predominant northwest - southeast trend of base structures.
The base of the pre-JurasBic cover reveals a lower crystalline, and upper weakly
metamorphized, stratum. No data were obtained on the presence (or absence) of
Triassic deposits. Downcast slides of the Jurassic period are closely connected
Card 1/6

S/165/60/000/005/001/003
Tectonic development of South-East Turkmenia A1o4/A129
to the Alpine tectogenesis. Intensive sinking of the geosyncline and the south-
ern region of the stage accounts for the considerable width of Jurassic and Cre-
taceous deposits, i.e., 4.5 - 5.5 km at Kugitang, 5 - 6 Ian in the Karabill4elif-
skaya Depression and 3 - 4 km in the Mary area. Further sinking occurred during
Paleocene and Eocene periods which acquired a marine character; continental de-
posits are occasionally found in Oligocene. Intensive tectonic movement contin-
ued in Miocene and Pliocene, particularly in the geosynclinal area. A rise of
moderate intensity took place during the Quaternary period. According to seismic
prospecting and drilling results rocks up to the cover of lower Cretaceous depos-
its were subjected to neogenic erosion (Repetek structures). Final movements of
the Alpine cycle formed the mountainous structures of Kopet-Dag and Paropamiz.
An important part was played by the zones of breaks which acted as boundaries of
tectonic elements, the Repetek zone being one of the most important. The basic
structures of the pre-Jurassic base are shown in Figure 1. Here the Repetek zone
divLqWs the Bukharo-Khivinakaya stage from the Central Turkmenian zone of raised
base surface mentioned by Yu.N. Godin (Ref. 3: Roll razvedochnoy geofiziki v ot-
krytii novykh neftyanykh 1 gazovykh meatorozhdenly v Turkmen1stane, "Izvestiya
TSSR, seriya fiziko-tekhnicheskikh, khimicheskikh i geologicheskikh nauk", no. 1,
1960), which borders on to the complicated East Turkmenian transient between stage
Card 2/6

S/165/60/000/005/001/003
Tectonic development of South-East Turkmenia A1o4/A12q
and folding zones. Yu.N. Godin designated it as the East Turkmenian outer zonw~
whereas L.N. Smirnov (Ref. 6: Murgabskaya vpadina - perspectivnyy neftegazonos-
nyy basseyn, "Geologiya nefti", no. 10, 1957) calls it "Murgabskaya vpadina".
In most cases these outer systems formed 6 - 7 km deep strata of pre-Jurassic
bases. Complicated tectonics were discovered in the area between the Murgab and
Tedzhen Rivers.* Seismic prospecting from north to south along the Murgab River
revealed three major elements; 1) a depression in the base filled with strong
Mesokainozoic deposits; 2) the width of Neogene exceeds 1 km near Sandykachy
stantsiya; 3) the stratification of sedimentary formations of the Saryyazinska-
ya Depression corresponds'latitudinally to Karabill-Kelifskaya Depression. It is
observed that the Saryyazinskaya Depression has weaker Neogene deposits whereas
Paleogene and Mezozoic deposits appear stronger. Conclusions: Pre-Jurassic
movements have-formed the greater part of the South-East Turkmenian territory as
a stage resting on a base composed of a lower (lower and medium Paleozoic) and
upper stratum with varied degrees of dislocation and metamorphosis. The southern
region of the stage was subject to intensive oscillation during the Alpine period
which resulted in Mesokainozoic strata and the formation of complicated outer
systems. The deposit cover reveals two structural stages divided by Jurassic-Pa-
leogene and Neogene-Anthropogene unconformities. The latter consists chiefly of
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Tectonic development of South-East Turkmenia A104/A129
continental phases, show hardly any dislocations and are stratified on the eroded
surface of the Jurassic-Paleogene complex, revealing a Jurassic and Cretaceous-
Paleogene structural stage. The formation of structures of the former complex
were completed during the Neogene period, before upper Neogene-Anthropogene de-
positions. In some.cases plutonic formations are to a certain extent reflected
in the upper structure stage, e.g., upheavals of the present relief, all great
rivers being attributed to zones of base breaks, zones of deep neogenic erosion
situated near or above buried upheavals, etc. Zones of break played an important
part in the formation of the present tectonic relief; they occurred in the pre-
Jurassic base and zones of intensive tectonic activity conformed to them at later
dates. Thero is 1 fi&re and 8 Soviet-bloc references. I
ASSOCIATION: Upravleniye geologii i okhrany nedr pri Sovete Ministrov Turkmen-
skoy SSR (Administration of Geology and Protection of Mineral Re-
sources of the Council of Ministers of Turkmenskaya SSR)
SUBMITTED: March 1, 1960
Card 4/6

.~~~~~_Pand.
tures of Tectonics
1961P 22 pp (Acad.
and Chem. Sol. Turkmen
259).
Creol-Mineral. Sol. . (diss) "Basic Fea-
of SoutheaS-tern Turkmenistan," Ashkhabad,
of Sol. Turkm. 83R, Dept. of Phys-Tech. Geol.
5tate Univ.) 250 copies (KL Supp 12-61,

MIURSKIY, G.I.; lgjt~M~D.M.; %IIRNOV, L.N.; KOLPAKOVA, N.N.j,
red. izd-va; FLUTKOVA, S.G.0 tekhn, red.
(Recent structure and basic characteristics of the tectonic
development of southeastern Turlanenistan]Sovremennaia struk-
tura i osnovnye cherty tektonicheskogo razvitiia IUgo-
Vostochnogo Turkestana. Ashkhabad, Izd-vo Akad. nauk Turk-
menskoi. SSR, 1961. 67 p. (KERA 16:1)
(Turkmenistan-Geologyp Structural)

MILISHTEYN, D.H,
Using seismic prospectizzg for studying the subsurface structure of the
southeastern Turkmenistan. Geol. nefti i gaze vol, 4# no.4:16-20
Ap 161. (MIRA 14:5)
1. Vostochnaya geofizichookaya ekspeditsiya Upravleniya geologii
i okhrany nedr Turkmenskoy SSR.
(Turkmenistan-Seismic prospecting)
(Turkmeniotan-Geology, Structural)

MILISHTEYN., D.M.; SMIRNOV, L.N.
Tectonic basis for the seismic zoning of the territor7 of the
Turkmen S.S.R. Izv. AN Turk. SSR. Ser. fiz.-tekh., khim i
geol. nauk no.6tl4-22 164. iMIRA 18:4)
1. Otdel razvedochnoy geofizlki t seysmologii AN Turkmenskoy SSIR.

iPMS 60'1"98)4/_F'q-q Gi SOURCE __COD8_- UR/0169/i56-/GOG-/002-/GO01/GO02-,-
N
AUTHOR: Millshteyn. D. M.; Avagimov, TA.; DubrovBkiy, V. G.; Lykov V.I.:
Pavlenkin A. D. o1okhov, V. V. Shikhanovich, E. L.
TITLE: The formulation of new trends of research on the structure of
the Earthrs crust and upp.~~r mantle in Turkmenistan by geophysical
methods NT ~Ie
SOURCE: Ref. zh. Geofizika, Abs. 2G6
REF SOURCE: Sb. Geol. rezulltaty prikl. geofiz. Geofiz. issled.
stroyeniya zemn. kory. Ft., Nedra, 1965, 33-44
TOPIC TAGS: Earth crust, upper mantle, electromagnetic field,
magnetotelluric probing, seismologic testing
ABSTRACT: Information on the structure of the Earth can be obtained
g__p '4ethod of observation and interpretation
by a j"ia,,*net~otqjX rq~ing
of' tche recordings of various type3 of elastic waves, generated during
natural earthquakes, and by studying the variations with different
periods of the natural electromdgnetic fteld of the EarthYyThis
method is based on the study of the ratio of variations in the elec-
tric and magnetic components of the Earth's electromagnetic field.
.Ccard UDC: 550-311:551-111(575.4)

L 47108-66
ACC _NR,
Magnetotelluric probing stat4 ons provide 'he possibility of studying
variations of the electromagnetic field during a period of 10 seconds,
to 24 hours. For Improved seismological 0, and such
that the functional (1) attains the minimal value awng all such controls ue The
scheme of the majority of problems of optimal control is constructed so t
second point, in genw&Uy fIxedO while the first taken an arbitrary powititol.tMin
this pVer the first podU* (for definiteness,, the origin) Is fixed, and th* second
is chosen arbitr=Uye the author wkes exterAive use of tooWques of R66 Bellza&
As an exaVIe he Audi" the problem whers the systm of equations (2) hu the
form
where A and B area n-diomisional matrices with constant coefficientas B is a non-
singular matrix uA u Is an n-41mensional controlling vectoro Theregion of coil-
Cora 2/3
--- ---- - ----- - -

trol satisfieso at each mmut of tiftip the Cordition
do i a (4.+.m (a) a.
where B(z) in an a-dimensional um-eirwAw natrix vhOss GOOMOUntf dSPGDd On the!
pluse coordinates. Me mthor Is grateful to Ye. A. Balbashin for his discussion
of the rematg of this artpjclso~ Orige art,* hms 38 forml"o
ASSOCIATIONs none
00
DATS ACQt Mpv(4 ZMGM
so C06ES, m NO RV $No 005 M=s 003
card 313

.71
1UTHOR0. LKIJahtgn, G. N.
ORG: Urgjlfate University Im. A. - M. Gorlidy (Ural'skly gosudarstvennyy univerattet)
TMX: The boundsx7 pfvblan for a system of two differential equations
SOURCZ: DifieraftWIM" unvnmdp, y. 1, no. 12, 19659 1628-1639
TOPIC TAGS: bowWW7 value problem, Boar differential equation, first order difforeatial
A90
equations a N an nil order differseW sqution 'two automatic coobvl systm -
AUTRACT: The Wotan of two Urat-order differsaW equations
P (16 X, Y)9 Ly - Q(to xe Y)
dt
with *s, solutions sadobft the boundsia cooftions
X(a)-XQX(b)-XI (2)
to discussed und-W dw mmm*dm dot the A&M-hawl aid" of Eq. (1) are specified and

A= M ANU4171
contionow together vAlk Owir first-order partial derivatives with respect to X and Y in the
sWp, 8 defined as
S:a~14b. -(w