SCIENTIFIC ABSTRACT GARETOVSKIY, NIKOLAY - GAREYEV, E.Z.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R000514320008-8
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: July 19, 2001
• Sequence Number: 8
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

ACC NR: AP6015729
A figure illustrates the effect of these
into the chloroprene rubber mixture. With
of th@e layer of adbesive substance (163,
adhesion of a abloroprene rubber mixture
increases (2.1, 2-4, 4.8 kgf/cm). Orig.
additions of polylsocyanstes
an increase in the2thickness
385, 585 grams/meter ) the
containing polyisocyanates
art. has: 3 figures.
SUB CODE: 11/ SUBM DATE: none/ ORIG REF: 002

GML'IOV5KIY, 14i.k.play.Viktorovich; POPOV, A.S., red.; ZMTSEVA,
L.A., tokhn. rod.
[How a state farm fund is formed and utilized] Kak obrazu-
etsia i ispolIzuetsia fond sovkhoza. MosWa, Profizdat,
1963. 30 P. (Biblictechka sellskogo profsoiuznogo aktivista,
no.3/15) (MMA 16:12)
(State farms-Finance)

G-A '. -,T ') i - T , G -i U 1-Y l,'l
Research work -on aFriculture and Vorestry in the Belorus-!,-n 57R.
Yensk, ilarkarmem. P,-37@R, lr-2@@'. 4f--! @@).
DA

0 R C'615E-- 1666f
ACC NR' AP7002882 U' CE 1@k@@_20d_/66/006_/@0_4/dff6
AUTHOR: Romanowski, S. R.; 1@arqts@i,
ORG: none
TITLE: Investigating the technology of accelerated hardening of reinforced
concrete structures-in a variable electromagnetic field
SOURCE: AN BSSR. Vestsi. Seryya fizika-tekhnichnykh navuk, no. 4, 1966,
76-81
TOPIC TAGS: concrete, reinforced concrete, hardening
ADSTRACT: The authors describe a new electromagnetic method, developed and
investigated at the Institute of Heat and Mass Transfer, AN BSSR, for the heat
treating concrete and reinforced concrete with the use of commercial- frequency
current. The heating of the concrete is carried out by means of internal and
external heat sources produced by the induction of ferromagnetic heat-releasing
elements without direct contact with the current -carrying parts of the power
plant. The steam treatment produces uniform distribution of heat , moisture
and pressure in the body of the concrete. The proce-,d of hardening involves
Card 112

ACIC NR'
AP7002882
uniform structurization. Formation of calcium hydrate occurs under favorable
temperature and moisture conditions, with no anomalous gradients of
pressure, that would lead to the breakdown of the structure. It was established
that the internal mass and heat exchange chemical reactions, and structurization
are affected by an external magnetic field. The Idesign flow chart of an industria
unit with a capacity of 50-75 thousand cubic meters o concrete per year, is
described. rhe unit for accelerated concrete hardening in an electromagnetic
field is designed for the application of various conditions of heat treating with
wide and smooth temperature control and field intensity and for shaping the
necessary parameters in accordance .vith the ambient medium. The design
features of the elements of the unit and some characteristics of the technological
process of heat treatment are analyzed. The test data of the pilot plant are
given and its technical and efficiency characteristics are presented. Orig. art.
has: 2 figures and 1 table. [Based.on authors' abstract] (NTJ
SUB CODr-.: 11, 13/SUBM DATE: none/ORIG REF: 004/
2/2

GARETSKIY, R.G.
- r@
Torekt7-@&7& primigeni&l &nticline in the western Mugodthar Hills.
Im
Biul.HOIP.Otd.gool- 30 no.2:67-82 Mr-Ap '55- X.-LRA 8:8)
(Rugodzhar Hills--Goolog7)

GARNTSKIY, R.G.
Clastic dikes. IzY.AN SSSR Ser.gool.21 no-3:81-103 Mr 156.
(MLFA 9:7)
l.Geologicheakiy inatitut AN SSSR, Moskva.
(Dikes (Geology))

YANSHIN, A.; GARNTSKIY R. G-,
;Ziii@ I
Celebration in honor of Academician N.S.Shatskii. Izv.AN SSSR.Ser.
gool.21 no.3:129-130 Mr 156. (MLRA 9:7)
(Shatskii, Nikolai Sargeevich, 1895-)
t,@- -
I , :

GARETSKIr, R.G.; KUZIMIIIA, O.A.
,--
New outcrop of oontinental Cretaceous deposits in the northern
Aral Sea region. Biul. MOIP Otd.geol. 31 no.15:63-73 S-0 '56.
(MLRA 10:3)
(Aral Sea k-egion--Geology, Stratigrp@hic)

GARETSKIY, R.G.; NMMOV, G.I.
Now outcrop of nummulitic beds at the northern coast of the #rItl Sea.
Dokl. AN SSSR 108 no.61141-114) Js '56. (XLRA 9$10)
1. Institut goologicheakikh nauk Akademii nauk SSSR. Moskovskiy
geolog6-razvedochnyy institut imeni B.Ordshonikidso..Prodstavleno
akeidemikom K.S. Shatskim.
(Aral San region--Nummulites)

SUBJECT: USSR/Geology 5-2-6/35
AUTHORS: Garetakiy, R.G;, Samodurov, V.I. and Yanshin, A.L.
TITLE: Pseudotectonic Dislocations of the Karak Mound in the Northern
Kyzylkums and Some Other Points near the Aral Sea (Psevdotek-
tonicheakiye dialokataii bugra Karak v severnykh Kyzylkumakh i
nekotorykh drugikh punktov Priarallya)
PERIODICAL: Byulleten' Moskovsko o Obahchestva. Ispytateley Prirody, Otdal
Geologicheakiy, 195M# 2, PP 77-103 (USSR)
ABSTRACT: The Xarak mound is located 120 km SSW of the railroad station
Dzhuaaly in the northern part of the Kyzylkum desert. It is
about 2 km long and 0-5 km wide. Its height is 40 to 50 m above
the surrounding plain, and its maximum height reaches 147 m in
the NE part.
In the Karak mound is neither a dome-atructure nor a graben, as
was supposed by the earlier investigators. Dislocations observ-
ed in the stratification of the layers belong to exodialocations
or pseudotectonic dislocations. They die out in the plastic
clays of the Upper Eocene and do not extent doeper than 175 m
from the zound's top.
Card T2 -- ---------

AUTHORi Garetakiy, R.G. 5-6-3/42
TITLE: Depth-Geology of the Kokpekty Anticline in the hfugodzhary
Region (Glubinnaya geologiya Kokpektinskoy antiklinali v
Primugodzharlye)
PERIODICALs Byulleten' Moskovsko o Obshchestva Ispytateley Prirody, Otdel
Geologicheskiy, 1957@,`# 6, pp 25-55 (USSR)
ABSTRACT: The "Aktyubnefterazvedka" Trust began the drilling of test
holes in the Kokpekty anticline in 1952, and this contributed
new material concerning the depth-geology of this anticline.
The author has studied the formation of the covering rocks
in the plateau located at the periphery of the Mugod'zhary moun-
tains, including those of the Kokpekty anticline.
The Kokpekty anticline is located 80 km south of the station
Emba. This anticline is distinguished on the geological map by
the outcrops of the Albian deposits. The outcrops extend from
the Batpak-kull lake to the 460 northern latitude. There is a
large break west of the anticline which extends along its entire
length.
TIB author gives a detailed description of the Lower-Cretaceous
and Jurassic deposits citing the spore-pollen content of indi-
Card 1/3 vidual rocks.

Depth-Geology of the Kokpekty Anticline in the Mugodzhary Region. 5-6-3/42
The Faleozoic foundation underlying Mesozoic deposits is
characterized by a distinct erosive dissection in the region
of the Kokpekty anticline. The ancient relief of the surface
of Paleozoic strata affected the present Paleozoic surface
relief reflecting also Meso- and Cenozoic tectonic movemente
which occurred later. In order to restore the ancient Paleo-
zoic relief the author uses the method of drawing a map with
isopachytes of deposits which filled in and levelled this
relief.
An analysis of isopachytes led the author to the conclusion
that the influence of the ancient relief of the Paleozoic foun-
dation can be noticed in distribution of thicknesses of Middle-
Jurassic and Lower-Cretaceous sediments.
Then the author describes the rocks of the Paleozoic foun-
dation citing in detail paleontological data and fossils dis-
covered by test drilling. Among the other materials, rich
indications of petroleum were discovered by drilling in this
region.
The author points out the coincidence of axes of the ancient
Paleozoic structure and the recent Kokpekty anticline, which
is an evidence of the inherited character of its development.
Card 2/3 The Kokpekty anticline was developing during a long period of

Depth-Geology of the Kokpekty knticline in the Mugodzhary Region. 5-6-3/42
time, and its structure became ever simpler from the deeper
layers to more recent ones.
The article contains 5 maps, 1 columnar section, 5 tables,
and 23 Russian references.
AVAILABLE& Library of Congress
Card 3/3

GARFTSKIY, R.G.; SHRAY13MAII, V.I.
Southern underground extension of the axial zone in the Ural fold
system [with summary In Snglish]. Sov. geol. 1 no.2:99-108 '58.
(HIRA 11:4)
A. Monkovskiy neftyanoy inatitut im. I.M.Gubkins AN SSSR.
(Ural HountAina-Geology, Stratigrpphic)

I/-, r@ fi@ "!@ "-, @ @,,,I@J, X)- 6,
@7-
GARNTSKIY. R.G.
@- -
Geological structure of the southern ftodzhar depression and Its
oil-bearing potential. Geol. nefti 2 no.l-.15-21 Ja 158. (MM 11il)
1. "ologiaheskir Institut AN SSSR.
(ftodshar7 region-Petroleum geology)

.'30'1/5-58-6-7/13
AUTHORS: R.G. , Merklin, R.L. and Yanshin,
Garets@kki,
@
A.
TITLE: The Marine Deposits of the Loaer Miocene
Period in the Aral Sea Region 1'1.!orskiye
nizhnemiotsenovyye otlozheniya v Priarallye).
PERIODICAL: Byulleten' Moskovshogo obshchestva ispy-
tateley prirody, Otdel geologicheskiy, 1.958,
Nr 6, p 99-108 (USSR)
ABSTRACT: The authors describe the sandy, shallow
marine deposits on the north-western shores
of the Aral Sea. These deposits belong to
the Lower Miocene period and contain the
fossils of Pelecypodae and shark teeth.
These deposits cover the eroded layers of
the Aral (L-Tiocene) suite containing Corbula
helmerseni Mikhai, and are in their turn
Card 1/3 covered by a sandy layer containing Rzehakia

SOV/5-58-6-7/13
The Marine Deposits of the Lower Miocene Period in the
Aral Sea Region
(or Onceph-)ra) socialis Rzeh. Similar
marine deposits are widely spread in the north-
western part of the Trans-Unguz Karakum moun-
tains. They represent the shallow water de-
posits of large bays of *Che Upper-Maykop
0
(Oligocene-L,iocene) sea and are singled out
in th@ local stratographic scale under the
name of the Kintykche suite. The following
geologists are mentioned by the author:
Ye.I. Belyayeva, E.D. Dzhavadov, L.S. Glik-
man, G.P. Mlikhaylovskiy, B.i;. Zhizhchenko,
V.I. Samodurov, A.G. Eberzin, V.I. Gromova,
V.V. Menner, B.Z. Uretskiy, V.P. Miroshnik,
Card 2/3 V.T. Balakhmatova, I. A. Prusova, A.S.

SOV/5-58-6-7/13
The Marine Deposits of the Lower Miocene Period in the
Aral Sea Region
Stolyarov, L.Sh. Davitashvili and G.D.
Kharatishvili. There is 1 map, 1 profile,
1 photo and 21 references, 17 of which are
Soviet, 3 German and 1 Czech.
Card 3/3

AUTHORSz Garetskiy, R. G., Samodurov, V. I., 2o-119-6-40/56
Yan3hinp A. L.
TITLEs The Marine Albian Deposits on the Western Shore of the
Aral Sea
(Morskiye allbskiye otlozheniya na zapadnom beregu
Arallskogo morya)
PERIODICLL: Doklady Akademii muk SSSR, 1958, Vol- 119, Nr 6,
PP- 1195-1198 (USSR)
iBSTRLCTt Is is known, the shores of this sea nearly throughout
consist of Tertiary rocks. Only on places where the
sections of antiolinal structure are intersected by
the coastal steep slopes, in their lower part rocks of
the Cretaceous system occur. 3 of such places exist:
on the northern shore of the Kulandy peninsula, on the
southern shore of the Tokmak-Ita peninsula and on the
eastern shore in the district of Cape ILk-Tumsuk (Tfihite
Rose") . The most ancient sediments in Kulandy are to
be classified with the Middle Albian (Ref. 13). In
Card 1/3 Tokmak-Ata Senomanian exposures are known (Refs. 1, 2).

The Marine Albian Deposits on the Western Shore 2o-119-6-40/56
of the Aral Sea
On Cape kk-Tumsuk Mesozoic layers were classified with
Upper Jurassic by an erraneous determination (Ref. 14).
A discussion on this subject is summarized: Nobody
supposed the occurrence of more ancient rocks than Se-
nomanian on Cape Lk-Tumauk, even, in this place the
occurrence of Senomanian and Turonian was doubted
(Refs. 7, 9, lo, 13). The authors succeeded in clearing
the cause of such a differing criticism of the occurring
Cretaceous sediments; i. e. individual researchers saw
and investigated different places. The more ancient lay-
ers, however, northwards gradually emerge out of the
sea. The authors propose the name "Kassarminskaya Anti-
klinal" (according to the Kassarma well) for the anti-
clinal structure of Cape kk-Tumsuk. It is not connected
with the Chushkakul'skaya anticlinal but separated from
it by a North-Ust'-Urt depression running in direction
of the width. The approximate sequence of the parcels
of k1bian layers south of the Kassarma well (from top
to bottom) is mentioned. The exposed 11bian sediments
Card 2/3 have a minimum thickness of 30 m. The discovery of these

The Marine 11bian Deposits on the Western Shore 2o-119-6-40/56
of the Aral Sea
marine layers together with other analogous finds of re-
cent times on the western shore of the Aral Sea can change
the hitherto existing conceptions in the way that the 11-
bian sediments notanly am of continental character (contrary
to Refs. 4, 13). Consequently, the transgressions at cer-
tain moments widely advanced eastwards. This happened along
that weskastern downwarping, which, since the Upper Pa-
leozoic separates the fold system of the Ural from the
Herzynian formation from folds of the Srfadryaya Aziya.
There are 1 figure and 14 references, 13 of which are
Soviet.
ISSOCIATIONt Geologicheskiy institut Akademii nauk SSSR
(Geological Institute AS USSR)
PRESENTED: November 13, 1957, by N. S. Shatskiy, Member, Academy
of Sciences, USSR
SUBMITTEDs November 11, 1958 (misprint)
Card 3/3

3(5) SOV/132-59-7-3/17
AUTHORS: Yanshin, A.L.
TITIE: The Kokpekty Buried Ultrabasic Massif to the South
of Mugodzhary
PERIODICAL: Razvedka i okhrana nedr, 1959, Nr 7, pp 9-13 (UGSR)
ABSTRACT: The author describes a buried ultrabasic massif in the
region of the At-Zhaksy River and its tr'@butarry the
Kokpekty River. The Kokpekty anticline was studied
before by A.N. Zamyatin, A.K. Buvalkin and V.I. Samo-
durov. In 1952, the Trest Aktyubnefterazvedka (Ak-tyub-
neftorazvedka Trust) made drillings for structure (N.
P.Duboveako) and A.Sh. Khadzhiyev and V.B. Vasillyev
started core-drilling operations by .,.,hich serpentine
deposits ivere located undel', the blanket of Ueso-Ceno-
zoic rock formations. Further drillings showed that
the serpentine formations were spread over mo4e than
200 sq km. Later, a gravimotric survey by F.Z. Poloyko
detected a considerable maximum of gr@_vitv embaacing
Card 1/3 the ahole Kokpekty anticline. As the ser@enUine rocks,

-OV/I;'2-59-7-3/17
The Kokpekty Buried Ultrabasic Massif to the South of Mugodzhary
already found in the dome of this anticline, are
characterized by their extreme density, it can be
presumed that this maximum of gravity is caused by a
huge buried ultrabasic massif. This Kokpekty massif
is well outlined on published gravimctric maps of the
region. It is situated on the same meridian as the
already-known ultrabasic Kempirsay, Khalilovo, and
Khabarninskiymassifs. These three massifs all contain
chromite-bearing deposits and by analoE,;y, the author
thinks, the Kokpekty aassif will also contain them.
By analogy too, he recommends the drilling of pro-
specting bore holes in places where the maxima of gra-
vity are particularly high: Daul, Sarybay-mola and
Kokpekty maxima. As in other ultrabisic massifs, these
maxima indicate the places of penetration of ultrabasic
magma, associated with the formation of chromitue ore
deposits. The author thinks also that an erosion crust
will be found in the zone of the Daul maximum, and
Card 2/3 such zones in the Southern Urals are associated with

SOV/132-59-7-3/17
The Kokpekty Buried Ultrabasic Massif t)Lthe South of Mugodzhary
the formation of siliceous nickel deposits. There are
2 maps, 1 diagram and 10 Soviet references.
ASSOCIATION:GIN AN SSSR (GIN of the AS USSR)
Card 3/3

GARETSXIY, R.G.
Jurasaics Jurassic-Triassic, and Paleozoic sediments of the
Chushka-Kull anticline south of the Mugodzhar MountaIns.
Biul. MOIP. Otd. geol. 34 no.5%103-117 3-0 '59. (MIRA 14:6)
(Mugodzhar Mountain Region - Sediments (Oeo:Logy)

GARETbKIY, R.G.; SAMODUROV, V.1.; YARSHIN, A.L., akademik.
Stiiii-igraphy of upper Cretaceous deposits of the Kassar-ma
anticline onthemestern shores of the Aral Sea. Dokl. AN SSSR
124 no.5:1109-1112 F 159. (MIRA 12:3)
1.Geologicheekiy Inatitut AN SSSR.
(Kasearma region--Geolog7, Stratigraphic)

GARETSKIY, R. G.9 CANo GEOL-MIN SCIV "INHERITED DIS-
LOCATIONS OF THE PLATFORU UANTLE@OF THE MUGODZHAR PERIPHERY."
i
Moscow, 1960. (ACAD SCI USSR9 GEOL INST). (KLI 3-61, 207).
91

GARETSKIY@Radim Gavr SIIRAYBWJI Vladimir IlIch; YANSHIN, A.L.,
jjgXjch4
akademik; otv.red.;YEROFEYBVA, I.M., red.izd-va;-KIJZ'14IN, I.F.,
tekhn.red.; GUSIKOVA, 0&'M. tekhn.red.
[Depth and structure of the folded basement in the northern
Turan platform (western Kazakhstan)] Glubina zaleganiia !:
stroenie skladchatogo fundamenta severnoi chasti Turanalcoi
plity (Zapadnyi Kazakhstan). Moskva., Izd-vo Akad. nauk SSSR,
1960. 89 p. (Akademiia nuak SSSR. Geologicheskii.ingtitut.
Trudy, no.") (Kazaklistan-Folds (Geology)) KUU 14:3)

YANSHIN, A.L.; GARETSKIY, R.G.
Tectonic analysis of thicknesses. ?'jetod.izuch.tekt.struk.
no.1:115-U3 '60. (KIRA 14:8)
(Geology, Structural)

GARKSKIY, R.G.
Upper Devonian and lower Garboniferous deposits of the KokDekty
anticline (Hagodzhar region). Dokl.AN SSSR 134 no.2:404-407
S 160. (MIRA 13.9)
1. Geologichookly institut Akademit nauk SSSR. Fredstavleno
akad. A.L.Tanshinym.
(Zhamantau region--Geology, Stratigraphic)

GARETSKIY, R.G.; YEGOROV, I.P.; NAUI-IOVA, S.N., SHLEZINGER, A. Ye.
Lower Carboniferous and upper Devonian deposits in the Zhanasu
region (the South-Emba gravity maximum). Dokl. AN SSSR 136
no.6:1418-1421 F 161. (MIRA 14-3)
1. Geologicheskiy institut AN SSSR. Predstavleno akademikom
A.L. Yanshinym.
(Emba Valley- Geology., Stratigraphic)

YANSIIIII, A.L.; GARETSKIY, R.G.; IIAIJMOVA, S.11.; SIIL,,-Z1111M;R, J',.Ye.
Position of tho bordcr of tti2 Russian Platfom east of
10,
the Caspian 3ea. Biul.!-!OIl,.-Otd.gOol. 36 no.4:76-96 Jl-Ag '61.
(MMA 14:9)
Oq"sian "l.-Itfe-

GARETSKIY, R.G.; SHLEZIRGERP A.Ye.; SHRAMIAR., V.I.; YANSHIN, A.L.
Prospects for finding oil and gas in the southern Emba gravity
maximum region. Sov.geol. 4- no.12:117-121 D 161. (MIRA 15:2)
1. Geologicheskiy institut AN SSSR i Moskovskiy in3titut,
nefte-khimicheskoy i gazovoy promyshlennosti imeni I.M. Gubkina.
(Fmba region--Petroleum geology)
(Emba region-Gas, Natural-Geology)

GARETSKIY, R.G.; NAUMOVA, S.N.; SHLEZINGER, A,U.o
---- @Stratigraphy and formational nature of upper Devonian deposits
in the region of the Scuthern-Emba gravity maximum. DAL AN
SSSR 141 no.4:931-933 D 161. (MIRA 14:11)
1. Geologicheski-y institut AN SSSR. Predstavleno akademikom
A.L. Yanshiny%..
(Emba Valley@--Geology,, Stratigraphic)

GARETSKIX R.G._- ]@NIPPER, A.L.; SAMODUROV, V.I.
__I__
History of the development and spatiall relationship of Paleozoic
structures in 'Llhe Kara-Tau and Ulu-Tau. Biul.?40IP Otd.geol. 37
no.1:43-56 Ja-F 162. OCRA 15:2)
(Kara-Tau-Geology', Str4tural) (Lriu-.Tau--Geology, Structural)

GARETSKIY., Racbra Gavrilovich; YANSHRIJ, A.L., akademik, otv.red.;
ZHURAVLL-V,
'V , red-.rzd-va; GUSEVA, A.F., tekhn.red.
[Inherited dislocations of the platform mantel in the periphery
of the 1-tagodzhar Hills] Unasledovannye dislokatsii platforixennogo
chekh1a periferii @Lgodzhar. @bskva, Izd-vo Akad.nauk SSSR, 1962
299 p. (Akademiia nauk SSSR. Geologichaskii institut. Trudy,
no.60). (MRA 15:7)
(Magodzhar Hills-Geology, Structural)

GARMKIY R G - IEYTES, A.M.
Second All-Union Conference on Tectonics. Iz7. Ali SSSR. Ser.geol.
27 no.12:128-131 D 162. (MIRA 16:2)
(Geology, structural)

GARNTSKII,, R. G-.* IzYTISJ, A.M.
Discussion of important problems in teotonis. Vast. AN SSSR
32 no.12t102-104 D 162, (MIRA l5t12)
(Geology, Structural-Corgresses)

GARETSKIY, R.G.
Structure of recent (Epipaleezoic) platforms and their oil and gas
potentials discussed at the Meeting on Tectonics." Sovageole 6 no.
8:137-140 Ag 163. (MBIA 16:9)
1. Geologichaskiy institut 0 SSSR.
(Petroleum geology) (Gas,Fatural geology)

G=TSKIY R.G.; DALIYAN, I.B.; NAUMOVA, S.N.; SHLEZINGIA, A.Ye.
Relationship between the lower and upper structural stages of
the platform mantel in the Turan Platform. Izv. AN SSSR.
Ser.geol. 28 no-3:83-92 Mr 163. (miRA 16:;!)
1. Geologicheskiy institut AN SSSR, Moskva.
(Turan Lovland-Geology, Structural)

GARETSKIY, R.G.J. kand. geol.-mineral. nauk; LErTESJP A.M.
I- I
.
A disewsion on the problems of tectonics held at Moscow.
Vest. AP SSSR 33 no.5tlO9-311 YT 163. (MIRA 1626)
(Geology, Structural)

GARETSKIY, R.G.; KONOWOVAVI.B.; SHCHERBOVICII, S.F.
Upper Garboniferous and Lower Permian Bediments in the scruthern
periclinal trough of the Urals in the region of the Kokpcikty anti- ,
cline. Biul. MOIP. Otd.geol. 38 no.ls74-93 Ja-F 163, (MIRA 16:5)
(Ural Mountains--Geology, Stratigraphic)

dkWSKIY. R.G.
Second All-Union Cokerence on Tectonics. Biul. MOIP. Otd.geol.
38 no.1sl%-159 JaZ:P '63. (mm 160)
(Geology, Structural)
4 "1
A, t.,

GARETSKIY, R.G.; GORSFENIN, S.Te.
Discovery of outcrops of Upper Cretaceous deposits in the
Zhamanshin area (Irgiz River valley in northern Aral Sea region).
Dokl. AN SSSR 148 no.5:1152-1155 F 163. JMIRA 16:3)
1. Geologicheskiy institut AN SSSR, Aktyubinskaya kompleksnaya
geologorazvedochnays. ekspeditsiya. Predstavleno akademikom A.L.
Tanshinym.
(Bol'shoy Irgiz Valley--Geology, Stratigraphic)

BOGOMOLOVA., L.I.; GARETSKIY R.G.; GRIDASOVY Yu.M.; ZU4AUNOV, A.K.;
SHLEZINGER;-7EYe.
Subdglt sediments on the eastern ofte of the Caspim syneelise
(Kankiyak-Mortuk-Zhana-Zhol region). Dokl. AN SSSR 149 no.5*-
1147-1149 Ap 16). (I-URA 160)
1. Institut geojog:U nefti AN KazSSR, Geologichoskiy bistitut
AU SSSR i Trest Aktyubnefterazvedka".
(Caspian Lowland-Sediments (Geology))

GARETSKIY, R.G.; SMODUROV, V.I.; SIMEZINGER, Mo.; YANSHIN, A.L.
Tectonics of the platform mantle of the Turan Plateau. Trudy GIN no.92:
202-257 163. (MIRA 17:10)

GARETSKIY Rg@j. PLESHCHEY9V, I.S.
Paleogene sediments of Ustyurt. Blul. MOIP. Otd. geol. 39 no.b
109-124 Ja-F 164. (MIRA 18:4)

VC11,11,10VIO-Klyt I.S.1 qj@@Fl')KIY, R.G., Slil,FZTNCYF'i; A.Ya., ';Hr.AYFK*l, V@I-
Surface structure or the baaement of the Turn Plul.
geol. 39 no.6il9-29 N-D 164. fMTRA 18: 3)
POTP. Otd.

BELOUSOVI, V.V., red.; BELYAIEVSKI', N.A., red.; IDGDIJ;GV, A.A.,
re4,_i GLRET@ IL tp,, red.; GUBIN, I.Ye., red.; K
UOPOTKIN, P.N.j red.; LM'ES, A.M., red.; MAZAAMICH,
O.A., red.; MURATOV, N.V., red.; NIKOLAYEV, N.I., red.;
PAVLOVSKIY, Ye.V., red.; PEYVE, A.V., red.; PUNIUSHEVSKIY,
B.A., red.; FUSHCIiA:,'OVSKIY, Yu.'M., red.; SIMMIANN, Yu.M.,
red.; SF-IiMS, H.A., red.; YANSHIN, A.L., red.
[Problems of the comparative tectonics o;' anciont platforms;
materials) Voprosy sravnitellnoi tektoniki drevnikh platrofm;
materialy. Moskva, Nauka, 1964. 152 p. (MIRA 17:8)

HUAYEVSKE171 N.A., otv. red.; LEYTES, A.M., otv. red.; SHEE!1'1*VL1,11t'
Yu.?,,., otv. red.; BELOUS30, V.V., red.; EOGDA111OV, A.A., red,;
@MY; ;H.G., red.; GUBU', I.Ye., rod.; KROPOTFUN, P.N.,
red.;SliTHEYS, N.A. red.; I.UZAAWICH, O.A., red.; MU.,ATOV,M.V.,
red.; N.IKOLAYEV, N.I., red.; FAVLOVSKIY, Ye.V., red.; FEYVE,
A.V., red.; B.A., red.; PUSHCHARO'JSKIY, Yu.M.,
red.; YANSHIN, A.L., red.
(Tectonics, igneous activity and distributien of ore deposits;
materials] Tektonika, magmatizm i zakonorernosti razmeshche-
niia rudrrikh mostorozhdenii; materialy. Moskva, Nauka, 1961,.
237 p. (MIRA 17:8)
1. Soveshchaniye po problemam tektaniki, Moscow, 1963.

PEYVE, A.V., otv. red.; JELCUSOV, V.V., red.; GJUEETSKlY, E.G.,
r.7- - Ir@ @ .. --ed.;
red.; UXTIES, A.M., red.; FAVLOVSK Y6 r
YANSHIN, A.L., red.
(Deformation of rocks and tectonicsl Deforn.a4S4ia porod 1.
tektonika. 1,1,oskva, llauka, 1964. 274 p. (Doklady sovetskikh
geologov. Froblema 4) (MIRA 17.10)
1. flatsionallriyy kairdtot geologov Sovetskogo Soyuza.

GAR-,ETSKIY,,.IZ..-G.; PANTELEYEV, G. F.; FIDRENSKIY, P- V-; SHLEZINGER, A.
Ye.
Rocks of the folded basement in the central Usturt. Izv-AN
SSSR.Ser.geol. 29 no. 1:50-62 Ja 164. (MIRA 17:5)
1. Geologicheakiy institut AN SSSR, Moskva; trest "Soyuzburgaz"
i Moskovskiy institut neftekhimichaskoy i gazovoy promyshlennosti.

GARETSKIY ; KOTOVA, I.Z.; SHLEZINGER A.Ye.
,1@.A@R-
Upper Jurassic continental formations of the Usturt. Dokl. AN
SSSR 154 no-61:98-101 Ja'64. (MIRA 17:2)
1. Geologicheskiy institut AN SSSR. Predstavleno akademikom
A.L. Yanshinym.

MURATOV, M.V., otv. red.j PUSHCHAHOVSKIY, Yu.M., red.; KHAD,
V.Ye., red.; MAZAROVICH, O.A., red.; BKLOUSOV, V.V.;
red.; BELYAYE;VSKIY, N.A., red.; BOGDANOV, A.A., red.;
GARETSKIY R.G., red.; GUBIN, I.Ye., red.; KROPOTKIV,
A.M., red.; NIKOLAYEV, N.I., red.;
PAVLOVSM , Ye.V.p red.; PEYVE, A.V., red.; PETRUSHEVSKIY,
B.A., red.; SHEYNMANN, Yu.M.2 red.5 SHTREYS, N.A., red.;
YANSHIN, A.L., red.
(Folded areas of Eurasia; materials) Skadchatye oblasti
Evrazii,- materialy. Moskva., Nauka, 1964. 375 P.
(M@IRA 17: 11)
1. Soveshchaniye po problemm tektoniki. Moscow, 1963.

GARETSKIY, R.G.; KOLESNIKOV, YS.H.; MURAVIYEV, V.I.; SHLEZINGER, A.Ye.
Possibility of the determination of the absolute age of
folding baeed on authigenous minerals in sedimentary rocks
as revealed by a study of fold basement made in the southern
Ural Mountain region. DAL AN SSSR 154 no.4:829-832 F 164.
(MIRA 17:3)
1. Geologicheskiy institut AN SSSR. Predstavleno akademikom
A.L. Yanshinym.

ITOPOTKIN, P.N., otv. rod.; DEI,OUSOV, V.V.p red.; DELYMEMM',
N.A., red.; BOGDANOV, A.A., red.- G-A-METSK11, R.G.y red.;
GUBM', I.Ye., red.; LEYTES, A.M., red.; MAZM=11, O.A.Jq
red.; I-WRATOV, M.V., red.; IIIKOLAYEV, N.I.., red.;
PAVLOVSKII, Ye.V., red.; PEYVE, A.V., red.; PETH.USHEVSKIY,
B.A., red.; FUSHCIMOVSKIY, Yu.14.1 red.; SHEYMMI., Yu.N..,
red.; SHTREYS, N.A., red.; YANSHIN, A.L., red.
[Stnicture and the development of the earth's crugt;
materials] Stroenie i razvitie zemnoi kory, materialy. Mo-
skvap Nauka, 1964. 199 p. (MIRA 16:2)
1. Vsesoyu=oye soveshchaniye po problemam tektoniki. 2d,
Moscow, 1963.

r of th;@ Repe; eF. ;nct, t@anyrajna 1
cas'zrn Turlunenla. Duk-'. AN SS@;R 157?,
C,.--ol ogtchesk Ly rm t.1 tiit Ali S' -'P, I

G =JSKTy,,2_G.,_qtT. red.; YANSHIN, A.L, skad@lnlk, atv, red.;
AR
BELOUSOV, V.V., red.; BELYAYFV3KIY. N.A., red.; BOGDAI;OV,,
A.A., red.; GUBIN, I.Ye., red.; KROPOTKIM.N., red.;
LEYTES, A.M.; red.; MAZA10VICH, O,A., red.j MURATOV, M.V.,
red.; NIKOLAYEV, N.I., red.; PAVLOVSKIY, Ye.V., red.; PEYVE,
A.V., red.! PRTRUSHEVSKIY, B.' . red.; FUSHCHAROVSM , Yu.M.p
red.; SHMNY-ANNlu.M., red.,SHTITYS N.A,, red.
[Young platforms, their tectonics, and prospects for find-
ing oil and gas; materials] Molodye platformy, ikh tektonika
I perspektivy neftegazonosnosti; materialy. Moskva@ Naukar
1965. 223 P. (MIRA 18-3)
1. Soveshchani-ye po problemam taktoniki,, Moscow, 1963.

GARETSKIY, R.G.; SIRE7,1111GEIR, A.Ye.; YANSHIN, A.L.
Types of the structures of young platforms in Eurasia.
Geotektonika no-1:38-50 Ja-F 165. (@URA 18:5)
1. Geologicheskiy institut AN SSSR.

AVROVP P.Ya.; BULEKBAYEV, Z.Ye.;@_QARETSKIY, R.G.; DAL'YAN, I.B.;
ZHURAVlEV, V.S.; MULDAKUWV, K.Ye.; SHLEZINGER, A.Ye.
Basic characteristics of the structure of the eastern and southeastern
margins of the Caspian Lowland based on subsalt, sediments. GeotektonikeL
no.1:118-125 Ja-F 165. (MIRA 18:5)
1. Institut geologicheskikh nauk imeni Satpayeva AN Kazakhskoy
SSR i Geologichaskiy institut AN SSSR.

VASIPYFV, V.G.; VOLIVOVSKIY, I.S., GARFTSjITy
R.G.;
Rirdc tectonic elements in the western part of Central Asia.
1 165. (MIRA 18:7)
Neftegaz. geol. i geofiz. no.4;7-10
1. Upravleniye geologii i okhrany nedr pri Sovete Ministrov
Turkmenskoy SSR; Vsesoyuznvy nauchno-issiedovatellskiy institut
pr1rodnogo gaza-, 1G 101 S-SSR f Naiichno--Is sled ovate V sk,.Iya
Sredne-Aziatskaya geof.Jzichecknya ekspeditniya, kantora
Spetsueofizika.
0

GARETSKI-f, R.G.; KIRYUKHIP11 L.G.; PUSHCHEYPI, I.S.
TectonicB, and oil and @,as potentials of the northerr Ustyurt.
Neftegaz. geol. i geofiz. no.4;10-15 165. (MIRA 18j?)
1. Vsnsoyu-.nyy Fmrn,eo1.og1chcqkJy 1,reit X.Inls@vrstva geologii
i okhran-.r nedr SSSR.

GARETSUY, R.G.; KOTUVA) I.Z.; A.Y,:,t.
Various types of Neocomian cross aectlovq in the western part
of the Turan Plateau. Izv. All SSSR. Say gool. 30 rio.2:102-111
F 165. (MIRA 18:4)
1. Geologicheskly institut AN SSSR, Moskva.

'01 ty,;,V, , "". 7. -, sl:; @ : : 6 .. ". Ye.
:-,p, % -- -','F 7 YT) f ' ; IL .1 - i j ; -- K 0 " " ,' - " - 'I; I:'"- @ @
-Z, - --, ". 1. . , 1. '.. I - - I ...
Absolute wp of the follinv of the in V-tyurt.
Dokl. AN SSSR 160 no.3:665-668 Ja It"J5. WIRA 18:3)
1. Geolojlclieskiy instit'ut All SSSR- Sibmitted Septe-aber 15, 1964.

i' PA
V.A@; I , . .",... @. ,
V.m.; T"@:ARFVP A. Yi. ; 1".. '1. - .
New Ws-L-ciftrirg teglOn 1.11 the 4ral 11.0untairi rcgjc':,,
SSSR 162 no.2091-1-3W, My 16 5. OMTRA 18;
tul- ee o i c I @v sk k T,
kq'; AN
C:k3Teditsiya.

HIKHAYLOVP Oleg Aleksandrovich; GARMKIY, S.P. red.; BRUSHTEYN, A.I.,
red. izd-va; EVERSONO (deoeased]
Nathematical statistics and linear programing in ferrous metal-
lurgy) Hatematicheekaia statistika i lineinoe programmirovanie v
chernoi metallurgii. Moskvat Gos.nauchno-tekhn, izd-vo lit-ry o
chernoi i tevetnoi metallurgiit 1961. 159 P- (MIRA 14W
(Steel-Hetallurgy) (Linear programming)

VVEDEMIKIY, P.I,[VvedenBIIqi., P.I.J., prof.; GAREV, L.P.[Hariev, L.P. ] y
kand. ekonom. nauk; ALENINA, M.T.; AK9TIkkENKO,, G.M.' '
[Akhtyrehenko, H.M.)
Study of the use of coke gas as a raw material for different
branches of the chemical industry,. Komple vykO palo-ener s
res. Ukr. no.l*.243-256 159a (MIRA 16:71
1. Kbaylkovskiy inzhenerno-ekonomicheskly institut.
(Coke-oven gas)

ROBINZON, Ye.A.,- DYACHKOVA, Ye.A.,- K()MISSAROVA, N.I.,Q GAREVSKAYA,,-,G,S.;
SAIliff, P. I.
Use of the oxidation method for determining the struett'tre
of aromatic hydrocarbons from petroleum fractions. Nefte-
khimlia 3 no-4:598--608 Jl-Ag 163. (MIRA 161;ll)
1. Institut neftekhimicheskogo sinteza AN SSSI imeni A.V.
Topchiyeva.

GIMVSKI, L.
"The Dosaica hydroelectric power station." p. 64. (Elcktoprivreda, VOL 6. no, 2. Mare/Apr,
1953p geograd.@
East European Vol. 2, No, 9
SO. Month List of/XWSKM Accessions,hibrary of Congress, Sept )er 1953, Uncl.

-jGA@ENSKI,A.; KUJUNDZIC,B.; RADOSAVLJEVIC,Z.
The dralfiage tunnel at the Vrutok Hydroelectric Plant. Pt.2.p. 365-
(Tehnika., Vol. 12, no. 3, 1957, Yugoslavia)
SO: MonUly List of East European Accessions (EEAL) IS, Vol. 6. no. 7, July 1957, Uncl.

GAREVSKIP TdqtO
RelLcs of a beaver in -&5 Mc@-Provac 11 cave m;ar Titxv V@Ies.
Fragm-enta Balk Skopje 5- no.!(`-;55-&3 'A-4r.
-1
i. Museum of Natural -Sr@lonces, ")kopje.

16.3200 7745)
50-1/-- 33-60 -1 -14,110
AUTHAORSi SNjllte. Yu. A. f T-hn1cxi sciences, rroCosnor),
Ts-@sv,ft,nko. A. F., @Vv. P.; K,kn1rcnxQ. V. D.,
Frant3ev, V. P.. &Y -On, 3.
TITM tle,troiiaf R-oltl,; or Ml
fleartm;
AM Stools
FRRIODICALt Stall, Or 45-50 (USSR)
ABSTRAM This Is a lescriptlcn or a *ttoy or ltohnOlCj',y or electro-
.Is, remelting Of* ShKhll , ShKrkll,30, v,J 1OKhNVA steels.
5
T114 chemical c"PolItt.n" or these steeim (it) %i ,fa ronow,t
ShXhl5. C. 0.95-1-10; Mn-- 1.4; 51=@0.35; Cr, 1.30-1.601
3-VO-020; P-SVO-C271 Nlm`r0-3; Cu:!@0-251 Shthlt,50. C,
O-W-1.10; Mn. 0.20-0.40; 51.0.15-0.3'% Cr. 1.30-1.6!it
S--5@0-020; P--CO.C27; Nt!@0-3; -nj f-. 0.25; &M
l8XhXVA. C, 0.14-0.21; Mn, 0.25-U-554.51, 0-It-0-37; 3
0 03; Pas; 0.035; Cr. 1.35-1.65; N1. CO-4.50; W,
Card 1/8 0:8_1.20. YU. V. lAt&fih Rrd B. 1. KLk8tmovlch Or the
A3S0CIATI0jjj Zapo-zh'ye Plachine BLI11ding Institute ALM
"DIgprospqt.Stall' plant (ZaporothA'Kllr roshi
.Stroyitellnyy Institut I jayod 'Dintprospeteatal'")
CAr4 8/8

SHULITE, Yu.A.; _GARZVSKIKHJ-A-;_ MAKSIMENKO, V.D.; LEYBE@70N, S.A.;
.-RjUJTSOV., V.P.; SMOLYAKOV, V.F.; STETSENKO, N.A.
Scale for the evaluation of nonmetallic inclusions in electrorefined
slag steel. Zav. lab. 27 no. 4:422-424 161. (mm 14:4)
1. Zaporozhskiy mashinostroitelinyy inBtitut i zayod nDneprospetsstalt."
(Stoel-Testing)

SHULITE., Yu.A., dokAor tekhn.nauk, prof-.; GAREVSKIKH, I.A., inzh.;
LEYBEIIZONI S.A., inzh.,- MAKSIMENKO,,V.D., inzh.; TiLEGUBENKO, A.F.,
inzh,,- SPERANSKIY, B.S... inzh.; FRAWSOV, V.P., inzh.;
SMOLYAKOV, V.F., inzh.
Defects in steel ingots made by the electric slag process. Stall
21 no. 4:322-326 Ap 161. (MIRA 14-.4)
(Steel ing:)ts-Defects)
(Steel-E.Lectrometaliurgy)

22315
S/11:W61/000/004/004/015
fr@z" A054@/A'127
AUTHORS: Shullte, Yu. A., Doctor of Technical Sciences, Professor;
Garevskiy, I. A., Engineer; Leybenzon, S., A.,, Engineer;
Iffaksimenko,.V, D., Engineer; Treg-abenko, A. F., Engineer;
Speranskiy, B. S., Engineer; Frantsov, V. P., Engineer, and
Smolyakov, V. F., Engineer
TITLE: Nature of flaws in steel ingots produced by the electro-slag
method
PERIODICAL: Stall, no. 4, 1961, 322 - 326
TEXT: The technology of electro-slag remelting was established by
the Institut elektrosvarki im. Ye. 0. Patona (Institute of Electrowelding
im. Ye. 0. Paton). A three-phase electroslag furnace (2250 kW) which can
smelt ingots 750 kg in weight and 300 mm in diameter simiiltaneously in 3
crystallizers has now been in operation for more than 2 years, In order to
improve the process, the nature of the flaws occurring in electroslag-re-
melted steel was studied and tests were carried out on ingots produced on
an industrial scale, whereas an A-550 (A-550) laboratory plant, designed by
Card 1/6-

22315
S/13 61/000 '/004/004/015
Nature of flaws in steel ingots produced by.... A054YA127
the same institute was used for the purpose of reproducing the defects. The
crystallizer of this equipment was 100 mm. in diameter, 600 mm in length, the
ingots weighed 30 kg, remelting took about 35 minutes (at 40 v and 1.2 ka).
In this process the ingot surface is not in contact with the atmosphere.
The slag bath is rising at the name rate at which the ingot is smelting,
while a thin slag layer forms on the crystallizer wall, the relief of which
is closely reproduced by the ingot surface. Three zones can be distinguish-
ed in the smelting process. A non-uniform structure, having a serrated sur-
face develops in the bottom zone during heating of the ingct. The metal
contains slag inclusions and flux, at the place of inoculation. This zone
could be reduced by applying a thermite mix (20@ saltpeter, 20ci4o' aluminum
and magnesium powder, 6VjaAH4-6 IAII-P-61 flux) at the exact centre of the
electrode. The slag bath develops more rapidly in the heating pericd when
maximum power is applied. By controlling the feed of the electrodes manual-
ly, any fluctuations in current intensity couldbe eliminated. At about
18000C a homogeneous slag bath is formed, while at the same time the smelt-
ing of the second zone of the ingot also starts; the thickne2s of the slag
lining on the crystallizer wall decreases to 1.0 - I.q mm. In this phase
Card 2/6-!,-

22315
S/13 611000100410041015
Nature of flaws in steel ingots produced by... AO5/4YA127
the electric system of the crystallizer is switched to automatic oporation.
The electrode is fed into the slag bath at a rate corresponding with the
optimum current intensity. Under these stabilizel con-iitions the slag balth
is regularly rising, leaving a smooth lining behind. The third, liquid-
slag zone is the actual smelting zone, both in respect of electric power
and physico-chemical effects. Here takes place "he smeltinG of 'he elec-
trode and the refining of the metal flow.. The height and volume of this
zone are the most important factors of the entire process The slag con-
%lent for all three zones was established. The greater the crystallizer-
diameter, the less slag was found in the lining (Table 1). The ingot sur-
face in the second zone is flawless, smooth and does not require any finish-
ing. This is one of the greatest advantages of this method, which, however,
can be obtained only by a stable electric system, faultless operation of the
automatic furnace control as the slightest disturbance in any of these fac;--
tors results in surface defects. These appear in the ma-crostructure and
are similar to the impurities usually found in electroateel In 1959 data
were compiled for ball bearing steel, showing the relation 1,etween the crys-
tallizer height, diameter and amount of defectu (Table 2). Thus, 'he great-
er the diameter of the crystallizer, the more flaws could be observed in
Card 3/a- S -

22315
S/-, 33116!100010041004101.;
Nature of flaws in steel ingots produced by... A054/A127
the ingot. As regards the smelting time, it was "ound that the first and
the last periods produced the greatest number of defects. MetalloCraphic
study of faulty rods revealed sickle and spider-shaped cracks, lenticular
inclusions, differing in colour from the flawless parts of the metal, in
some templates occupying more than 50cio' of the total surface, In microhard-
ness tests it was observed that in 'the impurified zones the hardness @oeffi_
cients displayed a wide range of values. It could aisc be observed that
the flaws penetrate fairly deeply, indicating that the factorr_@ impu."ifying
the casting are active a lonc- time (Fig, 5), Petrographic tests proved
that the inclusions are similar to 'those forming in free crystallization
and contain mainly calciumfluoride globules, needle-shaped corundum crystals,
aluminum-calcium compounds. Among the impurities slag-inclusions, I - 2 mm
in size, were found in irregular arrangement Inclusions were present in
the low-temperature zones of the metal, promoting the nixiiij; Of slag parti-
cles in the liquid metal. The lower the crystallization temperature, the
more flaws were found. The viscosity of the metal increases due to inten-
sive cooling and this promotes the capturing of slag particles. Based on
the tests with the A-550 equipment the permissible minimum length of the
Card 4/8-3 -

22315
S113 61/000/004/004/015
Nature of flaws in steel ingots produced by... A054YA127
bottom part of the ingot was defined. It was also possible to prevent the
formation of impurities in the top of the ingot by ensuring stable electric
operational conditions until the end of the process. The optimum power was
obtained with 55 v instead of 40 and 6 ka. However, even the optimum elec-
tric parameters only yield flawless casting provided the power conditions
are very stable throughout the entire process. By applying these new elec-
trical parameters the impurities could be decreased from 31.6'i@c to 0-7@1'0'- In
some tests Ya. I. Spektor took part.
Card 5/&

S/032/61/027/004/008/028
B110/B215
AUTHORS: Shullte, Yu. A., A" Maksimenko, V. D.,
Leybenzon, S. A., Frantsov, V. P., Smolyakov, V. F., and
Stetsenko, N. A.
TITLE: Scale for estimating nonmetallic inclusions in electro-
scoriaceous steel
PERIODICAL: Zavodskaya laboratoriyal v. 27, no. 4, 1961, 422-424
TEXT: A high-purity metal is obtained by the electroscoriaceous method
of melting. Inclusions in electroscoriaceous steel differ from those in
ordinary steel in kind and character of their distribution. Traditional
scales, therefore, cannot be used for the correct estimation of
impurities, especially oxidic inclusions. The examination of nonmetallic
inclusions in a large number of melts of eleotroscoriaceous steel allowed
the development of a new scale (Fig.) in which the total area of dis-
oriented inclusions; their number within the field of vision, and the
admissible dimensions of the individual inclusions are taken into account
(Table 1). Oxidic and sulfidic inclusions are shown in the photographs
Card 1/6

S/032/61/027/004/008/028
Scale for estimating nonmetallic... B110/B215
of the new scale. Large globular, oxidic inclusions are measured with an
eyepiece micrometer. The degree of impurities in the ground face is
estimated according to the field of vision with the largest number of
impurities. The authors tested the scale and controlled 682 specimens of
200 electroscoriaceous melts of ball-bearing steel types LlIX15 (ShKh 15)
and[UX15CP (ShKhl5SG). At the same time, the specimen wao estimated by
the traditional T70CT801-47 (GOST 801-47) scale (Table 2). The indices
of estimation by both scales differed but slightly, although the estima-
tions of the individual melts differed largely from the control. Examina-
tions of nonmetallic inclusions showed that the scale can also be used
for other steels melted out by the electroscoriaceous method and for
estimating melts in the vacuum arc containing the same typo of inclusions.
Ye. I. Boykols collaboration is mentioned. [Abstracter's notet Complete
translation]. There are 1 figure, 2 tables, and 2 Soviet-bloc refer-
ences.
ASSOCIATIONi Zaporozhakiy mashinostroitellnyy iiistitut (Zaporozhlye
Machine-building Institute); zavod IlDneprospetsatal"
("Dneprospetsstall" Plant)
Card 2/6

S/133/62/'000/001/003/010
A054/A127
AU'@iORIS,
Shullte, Yu. A., Maksimenko, V. D., Speranskly..
B. S.
TUU The advantages and problems of improving the electroslag remelting of'
steel
PERIODICAL: Stall, no. 1, 1962, 39 - 41
TEX-": Investigations and experience show that a major factor affecting the
efficiency of electroslag remelting (the intensity of the heat-transfer and refin-
ing) Is the formation of liquid drops separating from the Ingot, serving in the
process as a self-baking electrode, immersed in the overheated (425 - 5650C above
normal temperature) slag. The characteristics of the electrode drops were studtsa
on industrial-scale equipment, at 55 V and W. The drops were taken partly from
the bottom zone of -,.he slag lining,.partly from the slag "cap" on the ingot.
Their zizes were between 2.37 and 0.25 mm or even smaller. The drops are charac-
terized by a high purity, visible inclusions can hardly be found. Coarse oxide
inclusions disappear almost entirely, spheroidal inclusions decrease considerably.
The statls+Acal analysis of 2,140 samples obtained in 526 heats of ball bearing
Card 1/3

S/133/W000/001/003/Oib
rne advantages and problems of ... A054/Ai27
S'r.eel (in 1960) showed that remelted steel displays a high degree of purity, most
probabLy dtie to the intensive refining of the liquid steel by syrithetl@,. Iron-
I rt-_ @31ag af. InCreased temperatures. The sulfide Inclusions disappear In propor-
qo!z @Aie :;,;If a r content of the initia I material. When remelt I rig ba I! tear Pip,
'_@fel , @.tie degree of desulfuration attains '15 - 30%. For this kind of s"eel
r--,de-1,tgot. musf. not contain more than 0.007% sulftir. When reme1f.-Ing
a 0,0014 sulfur content, in the A 550 (A 550) equipment, witt, a 100-mm 31'aft-
c.-tm,r mold, rkie z-ulfur conten@ after remelting, decreased to 0.003f, and no :,A@Ide
i-,oiALd be observed on the forged products (110 and 25 mm in diam0t?,),
d rop-f orima@. ion, the composition of the fluxing agent. tl,-o affeci-s ..he re-
I.1,
.11!-,w 2,955 aamples from 500 heats of ball bearing sl.eel were t-errc-14,c-d,
J-. t7lj; 0 -F-6) fluxing agent containing 14.8 - 32-9 r1n.? n1 W,!e r
the AM -," (AN % Al,,03'
the 5"eL '
e alvrnip@,m ox.1de content of the flux, the purer was _@.. was f ourld .
1@ probabIV due to the fact that aluminum oxide in @he fljx lncreaa,@A
Jesldfuri zing actIvIty of the slag (which consists of 14-me-, rluorit@, aluirlu.-m
o-t-,des) . 17he struc ture of tile slag made f luxible with vario-us ktndi@ of ager.' B,
was also Sf-udied. Fart of the slags (Group A) is ligbi-yellow coloLired Cen `rs
t r tji r-e --a r fac,@@, its gTains are well-developed, have a rf_a,_i @olojr and are
'@;_;rd -2/3

3/133/62/000/001/003/OICI
'The advantages and problems of... A054/A127
1.hey contain calcium fluoride in the form of oval grains, which are surround@!d by
an easily melting component, lighter in colour and with a refractLve index of
1,6o4 - 1,610. Both phases are present in about the same volume. Moreover,
there Is also some corundum in this &ructure. Slags with such structural char-
acteristics permit a smooth remelting process with low power consumplUon to be
carried out, In some cases, howover, tho slag has a less bright cololn, arld a
coarse-grained structure, (Group B). The coating which surrounds the calcium
fluoride grains is about 5 times less voluminous than In the former group. Large-
prismatic corundum grains make up about 30% of the -total volume. With such a
,structure, the slag coating becomes coarse, remelting takes longer and more power
Is consumed, while the amount of sulfide and spheroidal inclusions also increase.-7.
The mineralogical composition of the fluxing agent, therefore, has a marked effect
on the steel refining process and needs further improvement. There are 7 fixares V/
and 10 Sovier-bloc references.
ASSUCIATION: Zaporozhskiy mashinostroitellnyy institut (Zaporozhlye Mechanical
Engineering Institute)
Card 3/3

W(,%)/EWT(m)/BDS-@-AFFTC/ASID-JD
ACCESSION NR: AP3003.37 S/0148/63/O(*/OO5/Oo76
100,061
AUTHOR: Shul e, . Ya.,A.; Garevskikh,, I. A,; Yeksimenko, V. D. j: Speranskiy,
B. S.
.TITIE* Problems of (w1stallization of electroslag-meltedingots
I'D I ----S
SO(IM: IVUZ. ChengLya meta3lursrlya, no. 5., 1963) 76_8@
TOPIC TAGS: electrojilag melting, ball-bearing steel- impurities, nonmetallic
nclusions, r'4791j.
i ingot dituneter effect,-56-th depth effect, solidification rate
ABSMACT: The Zaporozhskiy MipffiinostroitellrWy.Institut (Zaporozlilye Machine
Building Institute) In cooperation with the Dneprospetsstall Plant has studied,
to
the process of ing crystallization in eli-etroslag melting in an attempt
determine melting conditions that vould ensu:qe the beat metal quality.
Iabox-atory- and production-s" tests showed that -the ratio of ingot diareter
D to the depth of liouid metalMath h is the mostAndicative characterist- ic
of the process, and that D/h = 2 is the optimum value for ingo-.s 100--300 r-r, -In
diwater, Higher D/h values imucate that the temperature of metal and slz-.6
Card -1/2

L 8-63
ACRICK RR: AP3001376
baths is too low, which leads to poor separation of slag from metal and
increased anount of slag inclusions. Lower D/h values mean tliat the metal
and slag temperature is too high, which results in extensive seixegation,
cmgul-stion of nonmetallic inclusions, and an increased am,-A-lnt of impurities.
With inc-reas-L-ig ingot diameter, the solidification rate decreaGes, for
instance, from 1. 25, cm/min for 100 mm, dill Mter to 0. 64 for 300 un (at D/b2
This also promotes segregation. Ingots C; ShM5 steel [AISI E52100] 100 -.n
in diamter had considerably less segregetion Rd mmller Inclusions than
i--igots 300 in diameter. Orig. art. has: 3 figures and 2 tables.
ASSOCIATION Zaporozhskiy mashinostroitellrjyy institut (Zaporozhlye I x
Ruildir@g Institute)
SUBNITTED: lUug62 DATE AOQ: oljul63 ENCL: 00
SUB CODE: 00 No iw sov: oo6 OTMM: 000
ph/V
Card 2/2

SPERANSKIY, B.S.; SHUL17E, Yu.A.; GAREVSKIKH, I.A.
'L@
Temperature conditions in the electric slag process.
Avtom. wwar. 16 no.1:9-14 -Ta 163. (MM 16:2)
1. Zaporoahskiy mashinostroitelinyy institut imerd
V.Ya. Chubarya.
(Electric welding)
(Thermocouples)

SMOLYAKOV, V.F.; SWLITE, Yu.A.; 1,9TOVAR, B.I.; 9A@@-V@K Iq', I. .;
@_- A
IATASII, Yu.V.; TSIVIRKO, E.I.; 7ABALUYEV, Yu.I.; TOPCIIIY, S.F.
Ponmetallic inclusions in electric slag refined l2Kh2N4A
structural steel. Met. i gornorud. prom, no14:35-37 J1-Ag 164.
(IMIFA 18:7)

ACCESSION NR: AP4041869 S/0133/64/000/007/0640/0642
AUT11ORi Cabuyev, Go Kh.; Yel'tsov, K. So; Shul'te, Yu. A.; Mikhaylov,
P. A.; Garevskikh, 1. A.; Leybenzon, So A.; Tsivirko, E. I.; Medovar,
B. I.; Latash, Yu. V.; Frantsov, V. P.; Pakhomov. A. I.; Kaganovskiy,'
Go P.; Voinov, So Go; Shalimov, A. Go; Kalinnikov, Yea, So; Smolyakov,:
IV, P.; Kosoy, L., F,
TITLE: Improvement of the quality of electroslag-melted ball-bearing:
1steel
SOURCE: Stal', nos 7, 1964, 640-642
i TOPIC TAGS: ball bearing steel, electroolng melted steel, high
purity steel, steel electroslag melting
@ABSTRACT: Several variants of electroslag melting have been tested
in an attempt to improve the quality of ball-bearing steel. The
analysis of electroslag-malted steel showed that nitrides and car-
lbonitrides constitute the greatest part (up to 75%) of the nonmetallic
inclusions present in the steel. These nitrides derive from the
initial material. The electroslag process eliminates large nitrides
tover 20P in diameter, but does not eliminate the smaller ones,
Card 1 /,8,:-

!ACCESSION NR: AP4041869
:Therefore, the nitrogen and titanium contents of the initial metal
!must be reduced to aminimum, This can be done, for example, by
:refining the metal in the Ladle with synthetic slag. Electroslag
,melting of open-hearth steel refined with synthetic slag eliminated i
all the inclusions larger than IOU and reduced the number of smaller
tiinclusions by more than 50% and the nitrogen and oxygen contents
Ito 0.0053 and 0.0020%, respectively. To produce ultra-high purity
:ball-bearing steel.the double electroslag melting was applied with
I
is combination of various fluxes. The use of ANF-6-ANF-.6 fluxes in
';double electroslag melting or of AN-29-ANF-6 fluxes produced best
iresults. Ultra-high purity steel, fully satisfying requirements
ifor critical ball bea rings, was obtained. Orig. art. hits: 2 figures*
ASSOCIATfONt Dneprospetastal' (Dneprospatostal' plant); Zaporozh-
skiy mashinostraitollayhy institut (Zaporozh Machine-Building InstL-
tute); Institut alektroevarkL Lm Yee 0, Patons, (Electric WeIdLng
lnstLtute); TeNLIChM
Co,-d 2/A'..

VALEYEV, Kh.S., kand.tekhn.nauk (Moskva); GAREVSKIY inzh. (Moskva);
KOSTMOVY N.S., kand.tekhn.nauk (Moskva
Change in the electrical strength of high-v4ltage porcelain
subject 49-the action of high-voltage d.c. @ith lon diration.
Elektrichestvo no.1:59-61 Ja 163. WA 1632)
(Electric Insulators and insulation)
(Porcelain-Electric pi-operties)

1, @C M F'I'L 4J. F.7%
Selection of Parent forms for apple breeding. Izv. Ro,. aqda
AN Kir. SSR no.1.5-11 164.
Apricot breeding in the Botanical Garden. lbid.:13-17
(MIRA 18.@6)

UAKUET@ @;.Z.
22388.-Gareyev, E.Z. ' Botanicheskiy Sad Kirgitakogo Filiala Akademi-i Nauk
SSSR. Byulleten' Glav. Botan. Sada, Vyp. 2, 1949, S. 59-61
SO: let-opial No. 30 1949

GAREYEV$ E. Z.
20891. Gareyev; E. Z. Michurinakiye aorta yabloni v kirgizii. Sad i ogorod, l9h9,,
No. 6, a. 27-29.
SO: LETOPIS ZHURNAL STATEY - Vol. 28, Moskva, 1949.

GAREYF.V,, B.Z.
--QMwqpm"
Preliminary results of apple breeding in Kirghizia. Trudy Biol.inst.
KirFAN SSSR no.3:37-52 150. (MIRA 8:5)
(KIRGHIZ ISTAN-AITU)

GARMYEV, R. Z.
Formation of apple blossom buds as related to the presence of
leaves and the growth processes. Trudr Biol.inst.KirFAII SSSR no-3:
53-60 150. Mn 8:5)
(APPLES)

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C. A.:". @- @ , - . z .
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Nichurian variety of fruit bearinc r)l,,nts i, K1rvH7.lf--
1 0
Tzc;-,.,o Akwlemii wiuk 101 . . (5.1- 3 @@( I r, )
SE-"54.6.R9G3