SCIENTIFIC ABSTRACT SOLLERTINSKAYA, T.N. - SOLNICA, W.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R001652210011-2
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: August 25, 2000
• Sequence Number: 11
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

' ' ' N. ;
ti-e Eff-%Ct Of -,e p Yy I og pi c A I bretin systems
,net jy
@,n tr@e Ellr_-,@tricnl --r-tivity of tre cerebra-, cortex. ZhLr. evol, biokhim.
no.-i2gl-289 Vfy-Je 16-@.
flzlohgi@ tsen'ralln%l ner-moy ,31.ntemy i
'A mrvn,@y dey'llatellnosti chelnvekn Instituta
ilmem .3e,-r,,enO','A AN S.@IS_I., lArlinfZrad.

Category USSR/Soli(I Statc! Phys'im -Mechanical properties of crystals an-.1 P01Y- E-9
crystalline comVO&dg
Abs Jour Ref Zhur - Fizika, No 1, 1957 No 1377
Author Borin, F.A., Sollertinskaya, Ye.S.
Inst Moscow Inst. ror errous-Me--f-als and Gold, USSR
Title Influence of 'Zirconium on Certain Properties of Magnesium Alloys
Orig Pub : Metallovedeniye I obrabotka metallov, 1956, No 2, 8-13
Abstract : An investigation was made of the effect of Zr on the mechanical properties
grain size, and corrosive proper-ties of Mg-Zr and mg-t-4.1 - 4.8% zn4- zr
alloys. It is shown that Zr iftcreases considerably the mechanical properties
of the die-cast Mg-Zn-Zr alloys and the corrosion resistance of Mg-Zr alloys.
A refining action by zirconium on the magnesium alloys is noted.
Card 1/1

80216
s/i26/60/009/04/011/033
E021/E435
The Influence of Small Additions of Zinc on the Preference of
Crystallographic Directions of Growth of Aluminium Crystals from
the Melt
This is shown more clearly in macrophotographs of cross
sections at various stages shown in Fig 5. This
confirms the hypothesis of selective absorption of zinc
by the (111) planes of aluminium, which leads to an
increase in the preference of growth in the (111)
direction in relation to the [1003 direction. There are
9 figures and 10 references, 2 of which are Soviet,
7 English and 1 German.
ASSOCIATION:Institut ,Giprotsvetmetobrabotka
(Institute ,Giprotsvetmetobrabotka -11)
SUBMITTED: July 2, 1959
Card 2/12

LAYNXR, D.I.; PSTRUSSVICH, R.L.; SOLLIC INSKAYA, Ye.S.
Determining the orientation of aluminum single crystals by etching.
7,av.lab. 26 no-3005-3o6 16o. (XIBA 13:6)
1. Giprotsvetmetobrabotka.
(Alumininm--Ketallography)

s/-@81/62/004/0050/0513/055
B163/B-,36
T T -aya, Ye. S., and Pavlov , 0.
12 1 P(:trusQvich, 'J. Sollertins' a
Z.@@Chine of clislocaTions in -.he (111) plane of gallium arsenide
Fizik-': tverdoco tula, V. A+' no. 5, 062, 1376-1360
V
. aai;ents and condi-.iaris 'acre s,.udie,-' for the prepara-
X@2 `L.' r C, C, C h. 1 -16
c,n o@ s Of .-a-ilium, arsenide the (111) plane,
"hose G4vJ:,- results are en-.ered ir. the fol"owing table.
C a -a c, s i t o r, t ch 1, -10 Results Of etchini; Remarks
LI '131. o conditions
The (TITT) piano and all. oi@.er I%oa-

3
i 0-2 2
-3 jec-,
planes are polished.
Disloca-
selective
2 boilinza
"oas vl-=-ible ir. the
(111 ;lane
as etchant
conical ni-.s

H.F- 1 , H:-,' 3
4-5 min Freshly prepared and cold
N on -
0-2 3 ,
madium gives bluish selecc4ve
2 cold
i A."ter boiling, some
specimens
are well polished in cold state
nard 113
V

of dislocations in the
,/-;&Y-2/004/005/053/055
16 3 3138
C 0.-'. o 3t _4 on Etchine !Lesuits of etching Remarks
i a -arta ccnditions
or. all ulanes.

S
'-G -3,
" 3-5 min All rlanes in
cludind (TTT) are Non-
2
_@
) -I
H ()
( 30- in hot, polished. in t1he (111 ) @4isloca- selective
@
,
I
'@
,
2
freshly
pre- tions appear as conical pit$.
etchan
pared
e tch-ant -
1i'O 2-4 min I Dislocations appear in the (111) Selective
2
cold 1
I plarAe as conical pits.
a z c h an t
H 20-2
a 5:,"7)5 2 min, DislocatJons appear in the (111) selective
(30;O')-l boiling plane as triangular pyramids etchant
2 2

r1ard 2/3
V

-zc'- 4 ng of dJ s' oc at om in the ...
C
@.OMrC3it` Cn
n VC1. -"arts
-.-C-5cml
_-@'t ch 4- n - Results of etchin,3
U
Con-'itior's
0.5-1 min
'Do r"g
s/is 62/COA/005/053/055
;16 3Y211 36
Djsl.-@cations appear in the (l 11
surface in for= of triangular
pyra=idz
Re=arks
i
s a I a c -. jye
etchant,
used for
,z:- rman iLM
!!,0-3 1-2 =i- Dislocations appear ir. t@a (ill) Sedlective
boi-ling surface in forz. of triansular etchant
- 4 C/C""I-', H,SO, - 1 .64 9/C=
@2h,@ dansity of the acids -aaa: M10 1.@
3 3 -4
17@, _ 1 .13 Glc=). r1hare are 2 and 1 ta*o-
1.19 O/cm , .. I - La.
AS 3 C C I.J.".1 i ON @;oo*udarstvennyy i proyektryy
4nstitut obraboti =etailov, .1iosec-s (state
c i a n t i f I; c R a s a P_ r c h a r. d _--@ r o i a c t I n s t u t a I'or o r k i n g
Non-ferrous liatals, Losco-.-.)
S U january 15, 1962 (initially), February 10, 1962 (after
Card 3/3 ravIsion)

BENDIK, M.A.; PETRUSEVICH, R.L.; SOLLERTINSKAYA, -fe.S.
Effect of dislocations on cadmium diffusion in gallium arsenide.
Fiz. tver. tela 5 no.11:3247-3249 11 0631. (MIRA 16: 12)
1. Gosudarstvennyy nauchno-issledovatellskiy i proyektnyy institut
splavov i obrabotki tsvetnykh metallov, Moskva.

S/07o/63/008/002/007/017
2021/9120
AUTHORS i Petrusevich R.L., and Sollertinskays, Ye S
TITLE: The appearance of dislocations on (111) and (111)
planes of gallium arsenide single crystals by the
method of etching,
PERIODXCALs Kristallografiya, v.8. no.2, 1963, 243-247
TEXT: The action of various etchants on the surface or single
crystals was investigated with the aim of obtaining dislocation
etching pits and comparing their densities.@ Etching wis carried
out on gallium arsenide samples after sectioning singl: crystals
along the (111) plane and polishing the faces with alumina. An
HF H20 mixture in the ratio 1:3:2 was used an a polishing
-HN03-
etchant. This removed a layer 5-10 )L thick in 3-5 minutes. Various,
etching solutions were tried and microphotographs of the pits
together with the density of etch pits f@)r 3 reagents -are given in@
the following table. It can be seen that the density on a (111)
face decreased with subsequent etching with an inhibitor and AgN03#
which may be explained by an increase in the size of pits and,
in some caves, by.oveelopping* There are 2 figures and 1 table.
Card 1/2

JD
__t-il@'72-65 EV1T(m)/D1P(t)/E'dP(@) 'rjP(q)/SSP/AM/fiLSD(f )-2/RAF.M(&)/ESD(t)
ACCISSSIO' NR:. AP4646OF4Er---
SAO 7 If DOW WM7 2 "72.C
AUTHORS, -Petrusevich, R,-L I
TITLE: Displaying Alpha and Beta dislocation in S11111
.24
k- 11. single crystals
SOLtRCE: Kris tal log raf iya, v. 9, no. 5, 1964, 722-726
TOMC TAGS: dislocation effect# gallium arsenide, single crystal,
etched crystal, plastic deformation
-earlier.work by the authors
ABSTRACT: This is a continuation cf
(F.kz. tv. tela v. 4, 1378, 1962; Kristallografiya,v 7, 243, 1963)
devoted to the etching of*gallium arsenide for the'purpose of dis-_,:@J.
1closing dislocations. In the present-article an attempt is made to
!differentiate between the two types of 600 dislocations thai'dan be-',T_..
!produced in the gallium arsenide lattice (a and O'dislocations). Ti@'*-:'
Us endj, an excess of dislocations of,either type,was
produced in,

V1
IACCIX'SION NR.- AP4046048
the crystal by plastic-bendin'go- This ex ess wasthen displayed
c -by
different etchants. The results show that on the B surface
of @Fallium arsepides a Scholl reagent with amino additives,displays
only a dislocations, %4hile a Schell reagent with AgN03 displays both
Ct and 0 dislocations. On the A surface (111), acid etchants display@
both a and A dislocations. It is still impossible to determine the
irelative number of a and 0 dislocations,in the single-crystal of
igallium arsenide by means of etching. Orig. art.- hast 5 figures and..-
1 table.
ASSOCIATI
ON: Gosudarstvenny*y nauchno-issledovatel'skiy i proy
k
ny*3r institut splavov i obrabotki tsvetny*kh metallov, (State
tific-Research and Design Institute of Alloys and Processin!j of
Nonferrous xetal-s-T`
SUB14ITTED: 28Nov63 ENCL: 00
SUB CODE: 66 NR REP SOVs 002 OTHERs 005
2
- - - - - - - - --- - - - - - - - - - -

A -; I .-PRI31IT-EYNS, S.9h.
ZT@ -Tit P.1, Y--'-i ,
4-f Pt h plt@! !,I rlrigLe vrystals of ;,i-_;3.7-tYTb
I.m ,, !iy t - 9 l,,A.,:,73bct'-ka no.24:38-43 165.
- Wl
I I I'a (MIR& 18:al)

FEIMIX,. M.A.; PETRIZEWICHO P#L*,, SDl.lKi7ltZKAV.
Df! term! m@ng tha surfacia defleati-m rf @:-Aill-, @-:-Y'sstal.
from the riane (11)" ar@or2lrg tv the rhar:i rf
I I
the stih pf.t-i. rv?.24-S44-1,9 '65"
('mT*,4A ;8;@))

Z'l,=r!Trc.VMv YO.S.
=faat Q: th.) am-fam dofloctim of a mlormaUm ft= tho
ixlr= (=) cu tho d3toutabilitty a: - ('- and P,*, -dislomti=
in singlo crystaU of RaUlum arsenkle. Trudy M;rotimtwtobra.
br,tL-a no.2400-53 96% D" lain)

1 18847-66 EWTW/.T/EWP(-tY-. IJP(0 , JD
1= NK; AT5 06471 SOURCE CODE: UR/2680/65/000/024/0038/0043
AUTHOR: Petrusevich, R. P.; Sollertinskaya Ye. S.; Shillahteyna S. Sh.
!ORG: State Scientific-Research Planning Institute of Alloys and the Processing of
jNonferrous Metals (Gosudarstyennyy nauchno-issledovatell-s-My i pr*yektnyy instituff-
isplavov i obrabatki tsvetnykh metallov)
TITLE: Various kinds of etch pitting in,single crystal compounds of the type
@
A B
! III V
!SOURCE: Moscow. Gosudarstvennyy nauchno-issledovatellskiy i proyektnyy institut
splavov i obrabotRi tsvetnykh metallov. Trudy, no. 24, 1965. Metallovedeniye i obra-t!
botka tavetnykh metallov i splavov (Metal science and the treatment of nonferrous
,metals and alloys), 38-43
iTOPIC TAGS: gallium arsenide, Indium antimonide, single crystal, etched crystal,
!dislocation effect, defect Structures MetallOgraphic examination, semiconducting
.material
@ABSTRACT: Etch pitting was studied in single crystals of eais"@and InSb. & forma
I - - - - i--
Ition of small pitts on (111) surfaces and their redistribution upon heating were
Card 1/2-

.L 18647-66
'ACC NR: AT6006471
dissociated from the larger dislocation etch pits which generally form.after chemi-i
Cal polishing. The etching conditions for obtaining the* small pits were as follows.
GaAs--the polishing solution was 1 part HF, 3 parts HN03, 2 parts HZO (polished,ai
,room temperature for 2 to 3 min) and the etchant for small pits was 1 part HN039 3
parts H20, 0.5% AgN03 (at boiling point 1.5 to 2 min); InSb--l part Hr, 2 parts
:HN03 (polish at roorn temperature for 30 sec) and 1 part HF, 1 part H202, 8 parts
@H20, 0.5% AgNO3 (etch 3 min at room temperature). Micrographs (200 and 440x) show-
@ed that the small pits became larger and formed terrace-like steps and subsequently
ibecame flat and eventually disappeared. After repolishing and etching, they reap-
lpeared in about the same number indicating that they are caused by defects extend-
ing deep into the crystals. Some crystals were heat treated at 1100 and 4000C (60
hr), cooled slowly (1 day), repolished and etched. Small pitting reappeared except.
i
@far randomly depleted areas. Within the depleted zones, the larger dislocation
jetch pits could still be observed. These data indicated that the small pits were
not caused by dislocations but by clusters of point defects. Only the point do-
Ifects could have been affected by the heat treatment. Orig. art. has: 3 figures#
1 table.
SUB CODEs 20/ SUBM DATE: 00/ ORIG REF: 003/ OTH IRM. 007
Card 2/2 Ymb

ACC NR: A?70-00001 SOURCE CODE: -UR/0070/66/01-1/006/089610902
AUTWOR: Malikova, Yo. A.; Petrusevich, :@. L.; @ollertAMkgyA.@- S
OR,G: State Sciontific Research and Planning -L-istitute of Alloys and Treatment of
Nonferrous 1'1,@tals (Gosudarstronnyy nauchno-issle.-lovateliskiy i proyektnyy institut
splavov i obrabotki tsvotnykh metallov)
TITLE: Distribution and density of dislocations in bent and annealed gallium arsenide
ani indii@m antimonide crystals
SOMCE: Kristallooraftya. V. It, no. 6. 1966, 896-go2
TOPIC TAGS: gallium arsenide, indium compoundt antimony compound, single crystal,
crystal dislocation, crystal lattice deformation, annealing, x ray spectroscopy
ABSTRACT: The distribution and density of V@ - and @3 -dislocations on trie A surface
'(III) of bent GaAs and InSb crystals with different curvatures was studied by etching
@and with a two-crystal spectrometer. GaAs was etched with a reagent comprising (jr,
-1, H20-1, H2S04--3, and InSlo was etched with HF-1 HINO-2 C
!parts) H202 600a-3.
3@
The effect of annealing for 50 and 100 ho-urs at 11000C on the red'istribution 0
idislocations was also determined. Data obtained from reflection curves generqlly
agreed with that obtained by etching. The density of etch pits was compareAl with th o
;calculated theoretical density of dislocations to determire the relative proportion of@-
Card 1 /2 -__UDC 1_ W
1.4:

ACC NRs Apwooooi
excess d'Lslocations. Ln both of th,3 bent GaAs and 1r.-5b sa.-,plos the -i-nisity of
dislocations at the stretched and compressed surfaces -was about 4.--e s,7;ne, an-@
a minimum halfway botween (at the neutral pLtne of no stress). On annealino' GaAs U-1th
excess dislocations, the density of dislocations leveled out througho%@. the sanple
cross so,ztion, and the number found approached the theoretical, I.e.. their reLative 1@
:proportion approachod 100@. On annealing 1hSb there was a difference ir. the
rodistrioution of etch pits; the density of 0,,, -dislocations leveled cut, but that of
13 -dislocations dccreased. The relative proportion of oxcessc,',-dls@jcations 1r, InSb@
after annealing was Yy@, and that of /@S -dislocations was 55%. Altho,zh the absolute
stress In bending GaAs and InSb was the same, the relative stress for InSb was greater!
since its strength characteristics are inferior to those of GaAs# Orig, art* has;
3 tables, 2 equations and 5 figures-
SUB CODEt 20/ SUBM DATES 27Kay65/ ORIG REFS 004/ OM REFS 007
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YFREMENEO, B.A.; TSEINUIL., A l.; BAZFAL, I.G.; SUSJHOV, b.G.; 50@ LOJUD,
A.A.; BFLIE, Yu.11.
Autmation of' evaporation sections. Sakh. prom. 3@@ nj,11:39-4i
N 161. (MIRA 1-5:1)
1. TLIjentrallnyy nauchno-issledovatel'skiy institut sakharnoy
promyshlenno5ti (for Yeremenko, TSenzura, Bazhal, Susorov).
2. Ust'-Labinskiy zavod (for 5,,llogub, Belik).
(Sugar nachinery) (Automation)

SOLLOGUB A,A.
Technical and economic indices of the automation of single production
sections of the Ust-Labinskaya sugar factory. Sakh.prom. 37 no.2%
30(110)-34(114) F 163. (MIRA 1611:)
1. Ust'-Labinskiv sakharnyy zavod.
(Automation) (Ust-Labinakava-Sugar industry)

-SOLLOGUB. A.A.
No ---
Modernization of the inclined " double @Rlix diffuser.
Sakh. prom, 37 no.5'j37-,'+O My "63. (MIRA 16.,6"
1. UW-Labinskiy sakharnyy zavod.
(Diffuoers)

CLUM, A. N.
5
8
Acorns
StarinZ acrons. Les. khoz. 5 No- 9j 1952
Monthl,y List of Russian Accessions,, Librax7 of Congress, November 1952. Unclassified.

SOLLMM, V.B.
.-- .......
Modifications of the average velocity of elastic oscillation
propagation in the region of frontal depression of the Alpine
geosyncline region. Dokl.AN SSSR 94 no.3t545-548 Ja '53.
(KOA 7.1)
I.Predstavleno akademikom D.V.Nalivkinym.
(Carpathian mountains--Geology) (Geology--Carpathian mountains)
- I j

SOLLOGUB,V.B.
The tectonic structure of the depression of the Carpathian foot-
hills from satanic research data. Dop. AN URSR no.3:290-295 '55.
(KLRA 8:11)
1. Institut geologichnikh nauk Akadsmil nauk URSR. Predstaviv
diyonty chlon Akadonit asuk URSR V.G.Boadarchuk
(Carpathian Mountain region--Geolo", Stratigraphic)

SOLWGUB, V B - RATKHIR, L.D.
Som* recommendations for conducting seismic observations in
borehole testing. RazvedA okh.nedr 21 no.6.-43-46 K-D 155.
(MLRA 9:12)
(Prospecting--Geophysical methods)

USSR/Geology
Card 1/1 Pub. 2-2 - 41/54
Authors I Sollogub,, V. B.
Title i The boundary of the outer and inner zones of the Carpathian depression
Periodical I Dok. AN SSSR 3.02/5,, 1005-10081 Jun- lls. 1955
Abstract I Geologioal-mineralogical. data are presented regarding the outer i .UA
inner zone boundaries of tbe.Carpathian mountains In vestern Ukrainej'
Five'USSR references (1947-1954). Graph; diagram.
Institution .........
Presented b3r % Academician D. V. Nalivkin$ January 15, 1955

SOLLOGUB, V
Tectonic structure of the cis-Garpathian depression based on
seismic surveying data. Trudy Inst. geol, na4 AN MM. Ser.
geogiz. no.10-20 '56. (KLRA 10:8)
(Ukraine-GeoloGy, Structural)

SOV/1 24 - 57.- 7- 8294
Translation from: Referativnyy zhurnal. Mekhanika, 1957, Nr 7, p 13C (USSR)
AUTHOR: Sollogub, V. B.
TITLE: The Elastic Properties of the Rock in the Region of the Foretroughs
of the Alpine Geosyncline in the European Portion of the U. S. S. R. (Up--
rugiye svoystva gornykh.porod v rayone peredovykh progibov Al'piy-
skoy geosinklinallnoy oblasti Yevropeyskoy chasti SSSR)
PERIODICAL: Tr. In-ta gcol. nauk AN UkrSSR, ser. geofiz., 1956, Nr 1, pp 91-,
1 Z 6
ABSTRACT: Bibliographic entry
Card 1/1

SOLLOGUB, V.D.
, . .
Some data on the elastic properties of rocks found in the Koldarian
S.S.R. Dop. UN URSR no.4t370-374 156. (MMU 9: 12)
le Institut geologichnikh nauk AX&Aomii nauk URS-R. PredstavAono Wm-
demikom Akadomii nauk USSR T.G. Boadarchukono
(Noldavip-GOoloa. Structural)

SOLLOMB, V.B.
Conducting seismic prospecting in the outer sons of the Carpa-
thian pieduout fault. Oeol.xhur. 16 Ao.3:52-61 136. (XIM 9tll)
(Caftathian Mountain region-Prospecting-kephysical
mthods) .
I
I.

D'YACIIKOVA, A.Ya.; SOUDGUII, V.B.
Tracing faults by the seismic method using reflected waves in the
outer zone of the Carpathian piedmont fault. Razved.1 okh.nedr
22 no.8:37-42 Ag '56. (MLRA 9:11)
1. Institut pologlcheskikb nauk Akademli nauk USSR i trest
"Ukrnaftegeofizika."
(Seismology)
(Carpathian Mountain region--Prospecting--Geophysica1 methods)

VOPILKIN. M. (Klliv)-, GA!.U-bHKO. P.Yn. (Eliv); SOLLCGUB, V.B. (Kitv).
Seismic method for vensurin.- stresses In sa t mine pillnrn (with
summary 1r. Russian]. Priki-mak-h. 3 n3.1:229-232 '57. (KIY-A 10:9)
1. Kii7alkiy politekhnichnly institut.
(StAlt
f

AUTHOR: SOLLOGUBIV.B., GALUSHKO,P.YA., VOPILKIN,L.A., PA - r-653
PATIOKHAOA.M.
TITLE: On Certain Factors Influencing the Rate of Propagation of Elastic
Vibrations in Books. (0 nekotorykh faktorakh, vliyayushchikh na
veliohinu skorosti rasnrostraneniya uprugikh kolebaniy v gornykh
porodakh, Russian).
PERIODICAL: Daklady Akademii Nauk SSSR, 1957, Vol 113, Nr 1, pp 82 85
(U.S.S.R.)
Received: 5 / 1957 Reviewed: 6 1957
ABSTRACT* The present paper investigates one of the most important factors
influencing the velocity of layers, namely the static stress of
higher layers. For the study of the connection between the velocity
and static stress the authors carried out measurements of velocity
rock samples which were subjected to different pressures. In labora-
tory investigations of the propagation of longitudinal elastic
vibrations an impulse supersonic seismoaoope was used. From the
laboratory investigations discussed here and from the results of
seismic observations in drill holes the following inferences can
be drawn: The static stress of higher layers Influences the proper-
ties of the different dispositions considerably. The higher the
stress, the higher is the propagation velocity of elastic vibrations
in rock. If the rook resembles a perfect elastic body, velocity
Card 1/2 depends only upon static stress and not upon geological processes

On Certain Factors Influencing the Rate of Pro- PA - 2653
pagation of Elastic Vibrations in Rocks.
ASSOCIATION!
PRESENTED BY:
SUBMITTED:
AVAILABLE;
which have taken place in this region. Rocks differing from these
perfect elastic bodies have a remanent deformation. That is why
the propagation velocity observed does not only depend upon the
depth of the layer but also upon preceding geological history. The
propagation velocity of rocks of equal age in different regions
can therefore even be different if they are located in the same
depth. A detailed analysis of velocities in rocks may offer in-
dication8 as to the geological structure of the regions investigated
and as to major disturbances in depositions.
(2 illustrations)
Geological Institute of the Academy of Science of the Ukrainic SSR.
Library of Congress.
Card 2/2

AUTHOR Sollogub, V.8.
TITLE On the S-If 9oundary of the Russian Platform. (K voprosu o yugo-zapadnoy
granitse Russkoy platformy).
PMIODICAL Doklady Akademii Nau14 1.957, Vol- 115, Nr 3, pp. 605 - 6o8 (USSR.).
ABSTRACT In recent time geological and geophysical investigations were carried
out to a great extent at the southm and south western end of the Rus-
sian platform. In present paper the author tries to define precisely
on this basis some opinions on the boundary of the south western slope
of the platform with the throughbend placed before* The position as
well as the character of structure of the deposit zone of the upper
regions is in the first place determined by the behaviour of the cryb,.al-
line basis. In the west of the Ukrainian S.S.R. the deposit of the plato
form to the through-bend forms a zone which takes the direction north
west - south east which contains Yavorov., Gorodokj Zhidachev, Kalush$
Bogorodchany, Otynya and the south west of Cheraovtxy, It is characm
terized by an abrupt depression of the meso-palaeozoic rock complex of
a degth of from 15oo - 2ooo m, as an entire series of displacements.
Further details of the district are described in detail.* The district
of Botoshany is rather complicated. Here two directions of tectonic
disturbations cross: a north western and a meridional. one. In the
district of Balm the south western end of the Russian platform &-iiates
in its course from the meridional direction and takes a south eastern
Card 113 direction. The Jurassic through-bend before the Dobrudzha'sinks in north

On'the South-Western Boundary of the Russian Platform
20-'! -
western direction into a considerable depth* The relief of the crystal-
line basis in the district of the southern slope of the Ukrainian
shield (Ungeny-J1oznesenak) is. described by the contour lines of terrain
dramm by the author, In the area of the deposit zone of the platform
to the Jurassic through.-bend the crystalline basis sinks some kilometers
im order to form the through-bend pLiced before. Sumarizing, it must
be said that the south western flank of the Russian platform which
reaches from ravorov to the Dnestr-Liman has a very complicated struc-
ture. This is expressed by the fact that the platform border@ on.through
bendB which differ in age. In the north west of the district there is a
tertiary through-bend., in the Moldavian SSR..- a Jurassic ones and a
cretaceous through-bend in the vicinity of the Black Be&, The mentioned
structure is caused also by a series of disjunctive disturbationso They,
are expressed in the platform, especially in the Ukrainian shield as
well as in the through-bends which seam the south western end of the
Russian platform. The displacement and alteration of the boundary in
question occurs in the districts of crossing of displacements of vae
rious directions,
(There are I figure, 5 Slavic references).
ASSOCIATION Institute for GeologicalScience of the AN of the Ukrainian SSR*
(Institut geologicheakikh nauk Akademii naule USSR.).
Card 2/3

On the South-Western Boundary of the Russian Platform.
I PRESENTED by Academician I.S. @Shatqkiyp
SUBMITTED June 18 th s 1956.
. AVAILABLE Library, of Congress.
Card 313
20-3-51/59
... @-
December 10, 1956.
M@ ,

KRAVETS, Valentin, Vasil'yovich (gravots'. V.V.).- SOLLOGUB, Y.B1, kapd.
t0ol.-mln.nauk. otv.red.; M'111K, G.F. 0 F*W-.'IiA--Vi@@
Sh-LYAMM, V-Ye. [Skliarova, tokhn.red. 0
[Using the high-frequency seismic prospecting method for studying
the tectonics of thn weqtern part of the Ovruch Ifidgel zasto-
suvannia vy9okochastotnol selamichnoi ro--vldl-,v dlIa vyvchannia
tnktnniky zat-bidnot okraiTW Ovrtitalkoho masyvu. Kyiv, Vyd-ve Akad.
nauk Ukr. URS., 1958. 11 P. (Akademila nuak URSR, Kiev. Instrtut
Peolor,ichr7kh muk. (Trudy]. Seriia gentektoniky i gaofizyky,
no.6) 64IRA 12--9)
(Gvruch Ridgn-GooloI7, Structural) (seismic waves)

SOLLOGUB. Vaevolod Borisovicb; SUBBOTIN. S.I., otv.red.; MILININ, G.F.,
-tWeShIU, V.I.. tdaha.rud.
[Mwsical properties of rocks In the southwestern and southorn
regions of the 3kropean part of the U.S.8;4j Fizicheekie .
avoistva gornykh porod iugo-sapadnogo i iushnogoraionoy Dwropeiskoi
chasti SSSR. Kiev. Izd-vo batd. nauk, Ukr. 6SR, 1958- 99P. -
(Akademiia nauk URSH, Kiev, Instytut geologichnykh nauk.
[Trudyl. Serila gootektoalky I geofizyky, no. 4) (MIRA 13:8)
1. Chlen-korrespondent AN USO (for Subbotin).
(Rocks) (Seismic waves)

SOLLOWB, V,V.
--- Tectonic structure of the f orepart of the Dobruja bond and the
I southwestern boundary of the Russian Platform according to
geophysical data. Trudy Inst. gool. nank AN URSR. Ser. goof iz.
no.2tl5-26 1580 (NIU 11:6)
1, Institut vologichookikh nauk AN US3k
(Noldavia--Goolog7, Structural)

SOV/169-59-5-4384
Translation from:
(USSR)
2-L,I. I&
Referativnyy zhurnal, Geofizika, 1959, Nr 5, PP 15 - 16
AUTHORS: sollogub, V.B Galushko, P.Ya., Vopilkin, A.A., Patiokhi, A.M.
TITLE: On the Propagation Velocity of Longitudinal Elastic Waves'In*
Rocks and Its Dependence on the Static Load and on the Ru idity
PERIODICAL: Tr. In-ta geol. nauk. AS USSR, Ser. geofiz., 1958, Nr 2,
pp 130 - 137
AB3TRACT; Investigating the effect of the load on the propagation velocity
of elastic waves, the authors exposed a rock specimen with cubic
form to a one-sided compression by means of a hydraulic press,
The velocities of the supersonic waves were measured In intervals
of pressure of 20 kg/cm2. The velocity of wave in sandstone in-
creased by 5 m sec-1. atm for the pressure increasing from 0 to
120 kg/cm2. Increasing the load from 120 to 4*) kg/cm2 causes an
insignificant increase of the velocity, but a further Increase of
the load beyond 420 kg/cm2 causes a decrease in velocity. Under
Card 1/3 a pressure of 610 kg/cm2, the specimen collapsed. The similar

sov/169-59-5-4384
on the Propagation Velocity of Longitudinal Elastic Waves in Rocks and Its
Dependence on the Static Load and on the Humidity
course of behavior of the velocity was observed by testing lime-stone, but
the values of load corresponding to the points of inflection of the curve, and
also the values of velocity were different. The observed variations of the
velocity correspond to: 1) The decrease in the porosity under the pressure
effect; 2) the redistribution of the elementary particles of the rock. A de-
crease in velocity with a further increase in pressure can be explained by the
formation of cracks. A certain dependence exists between the density of the Vl(
rocks and the propagation velocity of the elastic waves. It is possible that
this dependence may be used for practical purposes. In halite specimens, the
velocity of longitudinal waves perpendicular to the applied load decreased
considerably with increasing pressure; but in the plane parallel to the
applied load, the velocity Insignificantly decreased. The saturation of the
rock specimen with water Increased the velocity; but the variations of
velocity in chalk and for coquina were smaller than in less porous sandstone.
The investigation of the variation of velocity under multiple cycles of loading
and unloading showed that a residual deformation is not observed in dense rocks
Card 2/3

SOV/169-59-5-4384
On the Propagation Velocity of Longitudinal Elastic Waves in Rocks and Its
Dependence on the Static Load and on the Humidity
(sandstone). In more porous rocks the value of the velocity Increases in
comparison to the Initial velocity In consequence of the residual deformation
after taking off the load. Be repetitive pressures, velocities increase
again and attain higher values than during the first cycle of loading. Con-
sequently, it can be assumed that the velocity of propagation of elastic waves
In rocks depends on the geologic history of the region in question. In regions
where numerous changes of sedimentation and of denudation occurred, the
ro-^ks were submitted to a greater compression and must be characterized by a
higher velocity than the similar rocks in regions where the change of the pro-
cesses took place not so frequent. Bibl. 10 titles.
I.K. Kupalov-Yaropolk
Card 3/3

SOLUMB, V.B.
In monory of G-rlgorii Alpksancircr7ich Ga=burtseT. Trady Ins-lb-. eeol.
nauk AN URSR. Ser. geofiz. no.2:198-199 158. (xm 11:6)
(Gamburtsev, Grigorii Alelmandrovich, 1903-1955)

GALUSHKO, P.Ya., dots., kand. tekhn.nauk; MPILKIN, A.A., dots., kand.tekhn.
nauk; SOIJOGUB, V.B., dots, kand.tekhn.nauk-; YUREVICH, G.G., iazh.
Expdr-fm-on*rat'~in~ve'~s"t'igation of the effect of blasting on the
stability of stope pillaro in Solotvino salt mines, Naucho dokl.
v7s. shkoly; gor. delo no-3:13-19 '58. (MIRA 11:9)
I.Predotavleno Imfedroy razrabotki mestorozhdenir poleznykh
iakopayemykh Kiyevskogo ordena Lenina politekhnichookogo Inatituta.
(Solotvino--Salt mines and mining)
(Mining engineering)

SOLIADGUB, V.B. [Sollohub, V.B.]
"_ 136undary of the Russian platform in the Ukrainian S.S.R. Dop. AN URSR
no.6:65&-660 158. (MITIA 11:9)
1.Institut goologicheakikh nauk AN USSR. Predstavil akademik AN USSR
V.G. Bandarchuk LV.H. Bondarchuk].
(Ukraine--Geology, Structural)

SOV-21-';S-8-16/27
Rondarchuk, Y.G., Member of the A3 Ukr3SR, Kondrachuk. V.Yu.,
Krutikhovskaya, Z.A., Lebedev, T.S., Mikhaylova, N.P., and
Sollogub, V.B.
TITLE: Hypsometric Chart of the Surface of the Precambrian Foundation
of the UkrSSR and Some Adjacent Areas (Skhema gipsometrii
poverkhnosti dokembriyskogo fun@pmenta USSR i nekotorykh
sopredelln.vkh territoriy)
PERIODICAI- 7orovidi Akademii nauk Ukrains,koi R-3R, 1958, Nr 9, pp 863-e66
(USSR)
AFSTRACT: The old charts of the PrecamW.an foundation within the Ukraine
compiled by A.D. Arkhangellskiy (Ref. 1) and other investigators,
of which the most detailed is the chart by E.E. Fotisdi (Ref. 15)
are mostly obsolete and do not -orrespond to the present level
of the veologico-geophysicRl knowledge of the Ukraine terri-
tory. Making use of charts compiled by F.A. Rudenko, G.M.
Kozlovskaya, V.T. Syabryay, K.M. VArava, R.I. Andreyeva for
individual regions and based on the results of electrosurveys
by V.I. klushin, gravimetric investigations by S.I. Subotin
and prospecting drilling, in 1957 the authors compiled a hypso-
Card 112 metric chart of the surface of the Precambrian crystalline

3)OV_1fl-5q-8-l6/27
Hypsometric Chart of the Surface of the Precambrian Foundation of the UkrSSR
and Some Adjacent Areas
foundation of the Ukrainian SSH And certain adjacent areas on
a scale of 1 : 750,000. The contemporary surface of the Pre-
cambrian foundation has a peculiarly disjointed relief which
in its fundamental features accords with the features of the
tectonic structure of the areas considered.
There is 1 geologicnl chnrt And 16 Soviet referentes.
ASSOCIATION: Institut geologicheskikh nauk AN UkrSSR (Institute of Geo-
logical 5ciences of the AS UkrSSR)
SUBYTTTFD: March 18, 1958
NO T E :
Russian title and Russian names of individuals and institutions
appearing in this article have been used in the transliteration,
1. Geology--USSR 2. Geophysics--USSSR,
Card 212

3(5) 6OV/21--59-3-17/27
AUTHOR: Sollogub, V B.
TITLE: Some Data on the Block Structure of the South of
the Ukrainian bSR (Nekotoryye dannyye o blokovom
stroyenii yuga Ukrainskoy SSR)
PERIODICAL: Dopovidi Akademii nauk Ukrains@koi RSR, 19501, Nr 3,
PP 301-305 (USSR)
ABSTRACT: Using reference material as a background, the au-
thor examines the structure of the Pre-Cambrian
foundation of the southern slope of the Ukrainian
crystalline shield and the adjoining fore-deeps,
substantiating his conclusion8 with data obtainedby
geophysical and geological survey work performed
during recent years. The southern slope of the
Ukrainiin crystal'ine shield, as well as the area
L
of the Crimea, consists of a series of sunk and
raised blocks. The movements of the various blocks
are different in tha northern and southern arens
of the zone of a single joint, i..e. if the blocks
Card 1/2 sink in the north, they rise in the south. The

SOV/21-59-3-17/'27
bome Data on the Block btructtire of the "ivith of the Ukrainian
,88R.
latitudinal strike zone is neutral, Constituting a
joining of the Russian platfo-rm with the fore-
deeps. The names of geologists 0. Kh,, Dikensteyn
and G.A. Lichagin are mentioned in the tex-t, There
are 1 maD and 8 Soviet references,,
PRESENTEDi December 11, 1958, by V.,G. Bondarchuk., Member of the
AS UkrSbR
Card 2/2

BONDARCIDJK, V.G.; SOLLOGIJB '. WORACIIIJK. V-Yu.; KRUTIKHOVSKAYA, Z-A-;
IMFMV, T.S.; MIKHAYWVA, N.P.
Surface relief of the pre-Cambrian crystalline foundation in
the Ukrainian and Moldavian S.S.R. Sov.geol. 2 no.1:41-55
Ja '59. WRA 12:4)
1. Institut geologicheskikh nauk AN USSR.
(Ukraine--GeoloMr, Structural) (Moldavia-Geology, Structural)

LEBEDEV, T.S - SOLLOGUB, V.B.
11 =- . ---
Contribution of Ukrainian scientists to.research completed under
the program of International Geophysical Year. Mezhdunar. geofiz.
god LKiev] no.2:3-31 160. (MIRA 14:1)
1. Institute of Geological Science of the Academy of Science of
the Ukrainian S.S.R.
(Ukraine-Geophyaical research)

SDENENKO, N.P., akademik, otv. red.; SUBBOTIN, S.I., ak&deaWt red.;
TKACHUK, L.G., doktor geol.-miner. nauk, zamo otwe red,;
LAZARENKO, Te.K., red.; BELEVTSEV, U.N., red.p POPOV, V.S.,
red.- SOLLOGUB. V.B. -kand. geol.-miner. nauk, red.;
ZAVIRYUKHINA, V.N.9 @;d.; MELINIK, A.F.,, red.; DAKIWO, Yu.B.,,
tekhn. red.
[Materials of the Fifth Conference of the Carpatho-Balkan
Geological Association)Materialy V s"ezda Karpato-Balkanskoi
geologicheskoi asootalataft. Kiev,' Izd-vo Akad. sauk URSR,
1962. 309 p. (PURA 16:4)
1. Karpato-Balkanakaya geolpgicheskaya assotsiatsiya. 5. a"yezd.
2. Akademiya nauk Ukr.SSR (for Semenenko Subbotin).
(Carpathian Mountains--Geology@
(Balkan Mountains-Geology)

SOLLOGUB, V.B.
---- I__.___
Division of the southern part of the Ukraine and the Kuban into
tectonic district based on geophysical data. Geofiz.abor. no.l:
1
3-10 162. (MIRA 16:3)
1. Institut geofiziki AN UkrSSR.
(Ukraine--Geology, Structural) (Kuban--Geology, Structural)

SOLLOGUBI V.B.; CHEKUNOV, A.V.; KHILINSKIY, L.A.; GARKALENKO, I.A.
Results of experimental seismic studies of the internal structure
of the crystalline basement in the northern part of the Krivoy Rog
Basin. Geofiz.sbor. no.1:24-31 162. (WRA 160)
1. Institut geofiziki AN UkrSSR.
(Xrivoy Rog Basin-Seismic prospecting)
(Krivoy Rog Basin-Geology, Structural)

SOLLOGUB, V.B.; LOSSOVSKIY, Ye.K.; KHILINSUY, L.A.; GORBENKQ, V.S.; SOKOLOV, B.N.;
- ------VrX-90@XKP B.S.
Use of higbp-frequency seismic prospecting for dividing metamorphic rock
complex in the Beloze4a ironr-ore deposit. Geofiz.abor no.2:46-,4
162. iMIRA16:3)
1. Inatitut geofiziki AN OkrSSR.
(Belozerka regioz% (Zaporozhlye Province)-Seismic pr4spectift)
(Beloz6rka region (Zapp3;ozhlye Province),Crystalline and metamorphic)

PETKEVICH, Georgiy Ivanovich;,50LLOGUP, V.B., doktor geol.-
miner. nauk, otv. O.P., red.; RAKHLINA,,
N.F., tekhn. red.; DAKMIO, Yu.B., tekhn. red.
[Factors determining seismic wave velocities in a
geological cross section as revealed by a study made in
the cis-Carpathian region] Faktory, opredeliaiushchie
skorosti se-ismichaskikh voln v geologicheskom razreze (na
primere Predkarpatlia). Kiev, Izd-vo AN Wcr.SSR, 1963.
113 p. (MIRA 17:2)

�q14PGUB,V.B.; CHEKUNOV, A.V.; KALYUZHNAYA, L...; MILINSKIY, L.A.;
k1wECHKO, G.Ye.
Internal structure of the crystalline basement in the south-
western part of the Korosten' pluton according to seismic data.
Geofiz. sbor. no. 5:122-130 163. (MIRA 17:5)
1. Institut geofiziki At' Ukr SSR.

SOLLOGUB, V.B.; CHEKUNOV, A.V.; KALYUZHNAYA, L.T.; KHILITISKIY, L.A.
Deep-seated structure o."' Korosten' pluton according to seismic data.
Dokl. AN SSSR 152 no-5:1215-1217 0 163. (MDU 16zl2)
1. Institut geofiziki AN UkrSSR. Predstavleno, akademikom V.S.
Sobolelrym.

SUBBOTIN, S.I., akademik; SOLLOGUB, II.B.; GHEKUNOV, A.V.
Crustal structure of the basic etructural elements of the Ukraine.
Dokl. AN SSSR 153 no.2 il.40-443 N 163. (MA 16:12)
1. Institut geortziki AN UkrSSR. 2. AN UkrSSR (for Subbotin).

SOLLOGUBP V.H.; GIIEKUNOV, A.V.; PAVIENKOVA, N.I.; UILIN.MY, L.A.
Nature of the Novotearitsynskaya gravity anomaly in the
Crimean plain according to seismic studies. Geofiz. sbor.
no.8:3-12 164. WRA 18:6)
1. Institut geofiziki AN UkrSSR.

"OLLOGULI. V. B. KIUNOV, A. V.
ara c 'le ri s t! cn of t1le elastic waves from the
baseTe.-.t in the sou,,,nr-rn part of Lhe &!J-czeria irur,
or,- region and its subsurface structure. Geofiz. 8bcr. no.8;
14-43 161+. OURA
lrs,'.-@tut geofiz'-k-, AN

SOLLOGUB, V.B.; CIIEKUNOV, A.V.; PAVLEMOVA, N.I.; GARKAIXNKO, I.A.;
'--I.---- `- KHILINSKIY, L.A.; SHPORT, L.P.
Crustal structure of the Crimean plain and Sivash region
according to geophysical data. Sov. geol. 7 no.8:44-56
Ag 164. (HIRA 17:10)
1. AN UkrSSR.

SFM41,NKt). 'j.B. , IVARFISHIN, M.N., CH,' Kf'NOV,
tucture of th,@ tibyE3al znnes of thp esirthS crust in thf@
11krain!an Crystalline Sbleld. geol. 7 no.11-148-60 N 164.
(MTRA jPie",
institut VPoflzlkj AN Ukr:-I'@'I"

GRTNIP Niki-Iny Yevylolft-Imovirlb (Ilryn" -soux-twi V.ci. V.Bqj)
dcktor geol.-c-'mro rtpvA, 31-vo re.-d.; @@.DYUF, 0J., ro-d.
1"o@r)rfer&nes and uave spe@Arm in 3615mli- prs@rro,71!nol
1
Inter ft@rontsilm 4. avik't" kF-11 u aaLs%u)rozvidl.-':E. rv@v,
Haulcova dumki, 1.965. 126.F. (mim 28-8)

Sa:ENENKO, N.P., akademik, otv. red.; TKACIRIK, L.G., doktor geol.-
miner. nauk, zam. otv. red.; VYALOV, C.S., red.; FORFIRIYE1
V.B., red.; -1-IJBBOT0, S.I., red.; 1AZAREYK0, Ye.K., red.;
DELEVTSEV, Ta.N., red.; POPOV, V.S., red.; SOLLOGUB, V.D.,
doktor geol.-miner. nauk, red.; CHEKHOVICH, N.Ya., red.;
BYCHKOVA, R.I., red.
[Materials of the Sixth Congress of the Carpatho-Balkan
Geological Association; reports of the Soviet geologists)
101aterialy VI Wlezda Karpato-Balkanskoi goologicheskoi as-
sotsiatsil; doklady sovetskikh geologov. Kiev, Naukova
dumka, 1965. 461 p. (MIRA 181lo)
1. Karpato-Balkanskaya geologicheskayu assotsiatsiya. 6.s"yezd.
2. All Ukr.SS11 (for Semenenko). 3. Chlen-korrespondent All Ukr.SSR
(for Lazarenko, Belevtsev, Popov).

SOLLOGUB. V.B.; GARKALENKO, I.A.; CHEMNOV, A.V.
Tectonic structure of the northwestern part of the Black Sea based
on geophysical data. Dokl. AN SSSR 162 no.61l374-1377 Je t65.
(MRA 180)
1. TSentralInaya geofizicheskaya ekspeditsiya Gosudarstvennogo geologi-
cheskogo komiteta SSSR i Institut geofiziki AN UkrSSR. Submitted August 20,
1964.

SOLLOGUBV V.B., doktor geol.-min.nauk; CHEKUNOV, A.V.; KALYUZIINAYA, L.T.;
)WILINSKIY, L.A.
Structure of 'the upper part of the crystalline crust in the Obruch
synecline region based on seismic data. Geofiz.abor. no.l-.18-26
165. (MIRA 18:1-2)
1. Institut geofiziki All UkrSSR. Submitted June 19, 1964.

doktor geol.-miri.nauk; CHEKUNOV, A.V.; PAVLENKOVA, N.I..
KALYUZHNAYA, L.T.
Some characteristics of the wave pattern in the crustal fault
zones of the Ukrainian S.S.R. Geofiz.sbor. no.1:32-39 165.
(MIRA l&12)
i. rnstitut geofiziki AN UkrSSR. Submitted November 10, 1964.

ACC NRt A117005453 SOUAGI;- C 0 1) 7_" n' 100211661000100912.19'q.- 197
Sollorub, V. D.; Cholcunov, A. V.
0..)
_C@: lmtit@to of Goophysics AN UkrS.Sq (Insty-tut goofizy1v All' Ula-SS,-t)
'21M@: Crustal struct turo in the vicinity of mountainoua Crimea
SOIT.,C--',: AN Dopovidi, no. 9, 1966, 1194-1197
,.021'c :,oliorovicic cliL;coatinuiLy, Physical Coolo,@y
L35,2.'.."...@'2: T'110 C.:istenco of Grii-,aztn r@ountain "roo'k-,s" is provua at; a of Oo_-L;.:Uc
@-c!;carch. "':-,o ::olhorovicic discontinuity is L;ubrLorgcd ur4cr -iho nountain:; alon@; zor,-;:;
of ;:x!cinal al)y@sal fracturou at a depth of 50 krit. Tho basl-Itic layer is found to lb-0
va-@-Jr ttacc ind its sui?faco it; upliftod. It is one of Lactors cauuin,@ 't@,o pro--
Sorleo o.-C pojitivo gravitational anomllos in mountai;-.ous Crimoa. 'Zhis paper was pro-
i;c.ntlcd by Ac-ado.-tician AIN UllwSll S. 1. SWbbotin. Ori(-;. ax-t". has: I fiL-,aro.
r-_
L.ji-s: y3.6-lff
Sj-" CODE: 03 / SUDIM DA-je,: 16Sop63 / ORIG REF: 017 / OTH lt3r,: 007
Card 1/3.

ACC NRs AT6028370 _-SOUR-CE-CODE-: UR-/0000/651000/000/005610069
(N)
AUTHOIlf Subbotin, S. I.; Gurevich, B. L.; Sollogubp V. B.; Chekunov, A. V.;
Chirvinskays, M. V.; Kuzhelov, G. K. (Deceiiiid)-
:ORG: none
TITLE: Deep-seated eXructure of the Ukraine, based on data from geophysical investi-
ISOURCE: International Geological Consress. 22d. New Delhi. 1964. Geologicheskiye
I cs); doklady
lrazulltaty prikladn" geefitiki (Geological results of applied geophyst
isovetakikh geologov,,problema 2. Moscow, Izd-vo Nedra, 1965, 56-69
TOPIC TAGS: tectonicS upper mantle, earth crus tp stratigraphy
Ukraine
'ABSTRACT: Geological and particularly,geophysical investigations have located a
great number of deep-seated faults in the Ukraine.. These faults have mainly
northeast and northwest strikes. The northeast-strike faults uredominate in the
Ukrainian shield, the Black Sea depyession, and the northern part of the Black
S.ea basin, while northwest-strike' faults are typical of the Dneprovsko-Donetskaya
depression,: the Trans-Carpathian depression, the folded Carpathians, the Carpathian
foredeep and the southwestern part of the Russian platform. For the area, as a
whole, it has been found that the macrostructural-features of deep-seated faults
haVe longitudinal or'transverse strikes. Tectonic movements in the Earth's crust
'Card 1/2

ACC NR, AT6028370
are mainly caused by compression and expansion of the mantle associated with poly-
morphic, phase and electron transformations, or chemical alterations. Deep-
s'eated 'faults originate in the upper mantle hundreds or at least tens of km deep.
I
!The main types of faults located in the Ukraine are: 1) ancient Proterozoic faults
!in the Precambrian basement; 2) faults of different ages, expressed in the basement
as major stages and separating principal structural features or their components;
and 3) transverse (sometimes longitudinal) faults cutting across the main structures
and separating them into individual.blocks. In addition, there are many faults in
the sedimentary strata which are directly or indirectly associ 'ated with the block
movement of the basement. The study of the deep-seated crustal structure of the main
'geotectonic features of the Ukraine is based upon geophysical, mostly seismic, in
vestigations. The .'block-type structure of the crust has been established, and a
number of deep-seated faults have been located. A general feature is increased
crustal thickness under uplifts and decreased thickness under depressions. It has
been found that the granite layer contains shallow gently sloping seismic discon-
tinuities, which may either separate different structural stages and rock complexes
or represent purely physical boundaries. The Ukraine has been divided into structural
zones*on the basis of geological and geophysical data, and detailed.characteriatice of
all.zones are given.. Orig. art. has: 2 figures.
SUB CODE: 08/ SUBM DATE: 06jan65/ ORIG REF: 025/ OM REF: 006/
Cgrd 2 / 2

14 (j,
iACC NR: AR6024835 SOURCE CODE: b-11/0169/f
AUTHOR: Subbotin, S. I.; Gurevich, B. L.; Kuzhelov, T. K.; Sollogub, V. B.;
@Chekunov, A. V.; Chirvinskaya, M. V.
TITLE: The plutonic formation on the territory of the Ukrainian SSR according to
data from a geophysical study
iSOURCE: Ref. zh. Geofizika, Abs. 4G13
1 REP SOURCE: Sb. Geol. rezul'taty prikl. geofiz. Geofiz. issled. stroyeniya zemn.
kory. M., Nedra, 1965, 56-59
TOPIC TAGS: geological survey, area description, geomagnetic field
ABSTRACT: The main relationship between the anomalous gravitational field and the
geological structure of the territory in question is the linearity of the field in
the regions of deep submersion of the Precambrian foundation and the mossaic-like
arrangement of the7shallow surface Precambrian bed. The geomagnetic field anomlies
mainly reflect the internal structure of the Precambrian foundation, i.e., Proterozoi4
filded linear regions and prehistoric plutonic locfalized objects of the basic and ul-
trabasic rock. In the regions where large subcambrian deposits were formed the geo-
magnetic field anomalies mainly reflect the presence of shallow effusive bedrock. A
large number of plutonic breaks and "feathered" cracks were established from the data
of seismometry, gravimetry, and by other geophysical methods. The thickness of the
Card 1/ 2
UDC: 550.311(477)

ACC NR: AIR6024835
Earth's core and the depth of the Konrad surface bed are estimated from the seismic
and gravimetric data and foundation rocks. Generally speaking the geophysical methods
are very tmportant in the exposure of structural forms at various depths and in the
detailed study of large and small tectonic elements. (Translation of abstract)
M. Speranskiy
SUB CODE: 03
2/2

SOIRI CE CODE: U-R/ 3169/ 6 o/ 0061 C6, U-k-W 00.1 8
Sollo@,,ub, V. B. ; Garkalenko, 1. A.,Trifonov, P. G.; Chekunov, A. V.;
Kalyuzhn 1) a---, 11. t. - Khilinskiy, L. A.
0 it G :Geophys ics. InsLitute AN UkrSSR. (Institut geofiziki AN IrkrSSR); Dneprogeofizika:
Trust (Trest "Dneprogeo"Lizika")
TITLIH: Deep SLructure of the Earth's crust in the Belozersk iron ore region based
on seismic data
SOURCE: AN UkrSSR. Gcofizicheskiy sbornik, no. 18, 1966. Geofizicheskiye
@issledovaniya stroyeniya. zemnoy kory (Geophysical investigations of the structure
of the earth's crust), 3-18
TOPIC TAGS: geoiogic; survey, earth crust, seismology, petrology, mineralogy
ABSTRACT: Seismic investigations of the Belozersk iron ore region revealed that the@:
basement in the region is composed of the earliest Precambrian formations and the
basaltic shell is greatly uplifted. Hence it is natural to assume that a block of
the Earth's crust has been elevated in the Belozersk region relative to adjacent re-
gions. This upliiting of the block of the basaltic shell occurred along the ancient
Belozersk submeridional deep fault zone and was accompanied by the penetration and
fusion of basic and ultrabasic. rock varieties in the upper levels
of the crust. A comparison of the structural map of the surface of the basaltic
-Card ___1/2L.._

ACC Nit. AT7003831
em T
sholl rri.t1i tile gravimetric map revealed their good qualitative agre eat. 1hus
c'-w gnavi.ty anomalies in the Belozersk region are due not to petrographic inhoma-
geneitic-s of Oic basement but mainly to the surface relief of the basaltic shell.
It is assumed that in other regions of the Ukrainian shield the main gravitational
effect is also produced by density boundaries within the Precambrian strata. In the:@
overall qualitative conformity of the gravitational map of the basaltic shell of the@
Belozersk region, no direct relation was found between the magnitude of the anomalies
and the depths to the basalt. This was apparently due primarily to density inhomo-
geneities in the basaltic shell itself.. Orig. art. has: 10 figures.
SUB CODE: 08/ SUBM DATE: 20Nov65/ ORIG REF: 025

ACC NR, AT6034514
SOURCE CODE: UR/0000/66/000/000/0156/0162
AVnIORt Sollogub, V. B.; Chekunov, A. V.; Pavlenkova, N. I.
ORG: none
TITLE: Structure of the Earth's crust in the southern Ukraine based on deep
seismic sounding data
SOURCE: 94 SSSR. Otdcleniye nauk o Zemle. Nauchnyy sovet po kompleksnym
issledovaniyam zemnoy kory i verkhney mantii. Glubinnoye stroyaniya Kavkaza
(Abyssal structure of the Caucasus). Moscow, Izd-va Nauka, 1966, 156-162
TOPIC TAGS: Mohorovicic discontinuity, granitic layer, basaltic layer, earth crust,
seismic velocity, crystalline basement,
ABSTRACT: The results are presented of regional seismic investigations conducted in
the southern Ukraine in 1961-1962 by the correlation method of refracted waves
and deep seismic sounding using continuous profiling. Borehole and available
geophysical data were utilized in compiling a structural schematic map of the
Crimean Plateau and Prisivash'ye along the surface of the Paleozoic basement. It was
established that the basement has a block structure. A system of submeridional and
sublatitudinal faults disects the territory into a number of large structures. The
Paleozoic basement lies at depths ranging from 0-1 to 6-9 km. The seismic data
do not confirm that the'tranoverse Perekop uplift is the boundary between the
Karkinitskaya and Sivashakaya depressions. The Novo-Tsarin gravity anomaly is

ACC NR' AT6034514
attributed to the deep-seated fault containing intrusions of basic and ultrabasic
rocks. A seismic-geologic iron section of the Earth's crust along the voronzh
massif-Black Sea profile was prepared from available deep-seismic data. Up to
4 interfaces with boundary velocities between 6.6 and 7.1 km/sec have been estab-
lished at depths of 1.5 to 10 km below the crystalline basement in the area of
UIV suuthern slope of the Ukrainian shield. The basaltic layer with a boundary
velocity of 6.6-7.4 km/sec is found along the whole profile at depths between
5-8 and 18-20 km. The Mohorovicic, discontinuity with a boundary velocity of
8.1-8.2 km/sec was also traced along the whole seismic line. The depth to the
Mohorovicic. discontinuity varies from 22-30 km in the region of the Black Sea to
45-50 km in the Crimean Mountains and the Dnieper-Donets aulowgene; Orig. art.
has: 2 figures. IWA-794)
SUB CODE: 08/ SUBM DATE: 26Feb66/ ORIG REF; 023/
Card -
.. - 2

KOZHXVIN, V,G.; AYONIN, A.A.; YAT'YANOV, N.M.; 'SOLLOGUB, V.P.; KOZYUBEM,
Aly., gorny7 inzhener; PRYAKHIN, V.A., 9f1Wft1Y; LT.; SUMCHN,
D.A.
let's be read7 for the tenth celebration of Minor*' ARy with now
Industrial achievements. Ugoll 32 no.8:4-17 Ag 157. (NIaA lotg)
1. Kemerovekly Sovnarkhox (for Koshovin). 2. Olavnyy lnxh*nor tresta
Pervomayoku,goll (for Afanin). 3. GlavW inshoner treats, Xesvetay-
antratait (for ratlyanor). 4. GlavW inshoner treats. Kopeyokugoll
(Sollogub). 5. Ayutinakoye shakhtoupravlonlys (for Kosyuborda).
6, Shakhta im, RunVantseva treats, Ulininugoll for Pryakh1n). 7. No-
chal!nik ordens, lenins shakhty No.9 treat& Sheshnyanantrateit (for
Shinkovskiy). 8. Nachallnik shakhty No.2Z Oloomintsevskaya trests,
Shchakinugoll (for Sukhachev). (Coal mines and mining)

S/169/61/000/008/030/053
A606/A101
AUTHOR: Sollogub, Z. R.
TITLE: Synoptic conditions of glazed frost formation In Northern Caucasus
and in the south-east of the European territory of the USSR
PERIODICAL- Referativnyy zhurnal, Geofizika, no. 8, 1961, 50, abstract 8B332
("Sb. po regionalon. sinoptike", no. 4, Moscow, 1960, 69-95)
TECT: Glazed frost in the south-east of the European territory of USSR
and in Northern Caucasus arises within a period from October until March. In the
limit months of this period the number of cases is insignificant, and a maximum
Is observed in December ' The majority of cases of glazed frost (70%) arises at
a temperature of -0.1 to -0,40C (-12 C is the extreme limit temperature) and at
weak and moderate winds of eastern and south-western directions. Groups and
types of synoptic processes causing glazed frost of different intensity were
established. Most dangerous Is the outbreak of@southern cyclones from the Black
Sea when the glazed frost is most Intensive and prolonged. Recommendation as to
the prognosis of the intensity and localization of glazed frost are given which
are based on a detector of synoptic processes mentioned. The forecast is deter-
Card 1/2

3/169/61/000/008/()30/053
Synoptic-conditions of glazed frost ... A006/AI01
mined from the temperature in warm and cold air masses near the ground and 850mb
surface height, the velocity of front and ayalone movements, and the prevailing
nature of precipitates. The results of experimental forecasting are entirely
satisfactory. There are 12 references.
L. K.
[Abstracter"s note: Complete translation]
Card 2/2

SOLI)DRY I Jerzy, mgr inz.
Export and anti-import. Chemik 16 no. 51:159 My t63.
1. Politechnika, Slaska, Gliwide.

KOWALSKA, Eugenia, doe.; SOLLORZ, Jerzy, mgr
Complexometric deteraination of calcium in orthophosphoric acid
solutions after Feparation of phosphate ions on anion exchangers.
Chem anal 9 no.2049-352 164.
1. Department of General Chemistry A, Technical University, Gliwice.

4
$$Study of Transistor Charar-teristics on an Oscillo-
graphic Characteriograph," by A. M. Bonch-Bruyevich
and U. B. Solmatoy, Radiotekhnika i Blektronika, No 3,
Mar 57, pp 311-316
Due to a considerable spread in the properties of transistors
manufactured, their characteristics have to be checked for each
unit separately to establish their fitness for specific application.
To facilitate the testing of transistors manufactured, a device was
developed to record simulataneously four families of static charac-
teristics. Such a device was called an oscillographic charac-
teriograph.
The circuit of this characteriograph consists of the following
components: multivibrator, intensity gate generator, saw-toothed
oscillator, step-by-step voltage generator, emitter feed block,
collector feed block, and oscillograph. Characteristics of tran-
siatre 51B and PIA were studied for various ambient tesperaturos. (U)

2 -x La -s t i, - 7, ;,ece- s ns

OL-/ern -(7-5
S/195/63/004/001/006/009
B075/9436
AUMORS: Shollmoshi, F., Reves, L.
TITLE: of reactions in the solid state. Thermal
decomposition of ammonium Perchlorate in the presence
of iron oxide
PERIODICAL: Kinetika. i kataliz, V.4, no.1, 1963, 88-96.
TEXT: The kinetics of the decomposition of pure NH4C10@'were
studied first, -The-decomposition between 215 and 234.5 - '
occurred to the extent of 31 to 34% with the activation energy
ranging from 29.6 to 34.9 kcal/mole and induction periods from
61 to 218 min. Above 240*C the decomporition proceeded more
rapidly, also to the extent of 31 to 339, and with an activation
energy of 31.6 kcal/mole.,- With the addition Of P0203 the
decomposition below 240*c took place'with shortened induction
periods and slightly increased rates. For the mixtures containing
50% Fe20 the extent of the decomposition reached 40 to 45%.
Between a4O and 300*C, 60,to 95% of NH4ClO4 was decomposed with
short induction periods (9 to 23 minutes). 'The decomposition rate
was doubled when the content Of F0203 increased from 2 to 20%.
Card 1/2

S/lq5/63/0o4/ool/oo6/ooq
Catalysis of reactions see E075/9436
Mixtures containing 2, 5 and 12% F0203 were also investigated
between 300 and 380*C. At these temperatures the first stage of
the reaction (approx. 30% decomposition) was completed in 2 to
3 inin followed by a slow further decomposition. The activation
energies were 40.9, 30.9, 25.7 and 22.0 kcal/mole for the mixtures
containing 0, 2, 5 and 12.5% Fe203- By comparing the activation
energies for the decomposition of pure NH4CIO4 with those for the
decomposition of its mixtures with F0203, it was concluded that the
mechanism of decomposition of the mixtures in electronic by nature.
Apparently Fe203 accelerates the transfer of electrons from anions
to cations, i.e. it promotes the formation of NH4 and C104 radicals
which decompose to gaseous products. There are lo figures and
10 tables.
ASSOCIATION: Institut neorganicheskoy i analiticheskoy khimii pri
UnIversitete g. Seged,-Vengriya (Institute of
Inorganic and Analytical Chemistry at Szeged
University (Hungary)
SUBMITTED:@ December 12, 1961
Card 2/2

viewwon orioditia PiaiwS Om gar Fee PWP
their ebaracteristles. H. Dtuel, L. Anyas-Weisz. and.j.
'resh sufW-j
Wins. Gn. Cukrownim $6, 110-12(1956).-F
bemvere'graund, extd. with 601i'O ate. at 70', and dried', A
the yield of the air-dried residue was 5.4%; theamt.olpec,@ .'M
-tic acid (1) 10.72-16.75 and CHICOO groups 3.44-5-&5%
(if the residue. On sapon., followed by acidification, CaCh
pptll., IICI-ale. washing, treating with a NO Cale resin,
and ale. pptu. Na pectate (11) was obtained In t it aint. fif
36-5V,70 of the I present in the beet dry pulp. Thrve
dIfTerent, preptis. of 11 showed the following analyses: %vatcr
8.2-8.4. ash 6-21-7.9. eure 1137.4-53.?, and cattcd. residual
4ubstamcts 30.4-48.04 /0.

DIMITRIU, C. C., Prof.; RIMNICFANU, R., dr.; GEORGESCU, St., dr.;
SOLMU, I.0 dr.; BULIGESCU. L.. dr.: HULUBEL, F.. dr.
Study of the effects of beparin In angor and in sequelas of
myocardial infarct; clinical and elactrophoretic results.
Ned. 1nt.. Bucur. 8 no.3:375-379 July 56.
1. Lucrare efectuata in clinica medicala Spitalul "dr. Carol Davila."
(AJIGINA PECTORIS, tberapy
beparin, clin. & electropboretic results)
(MCARDIAL INFARCT, complications
ther., haparin, clin. & alectrophoretic results)
(HIAPARIN, ther. use
angina pactoris & seq. of myocardial infarct. clin. &
eloctrophoretic r9RUlt8)

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4:`-11-%P
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t

YUGOSIAVWN,iclear Physics - Elementary Particles. C
Abe Jbor : Ref Zhur Fizika, No 9) 1959) 19620
Author : Jaksii, B., Soln, J.
Inst : Zagreb, Yugoslavia
Title -Meson Decay and the Non-Conservation of Parity
Orig Pub Glasnik mat.-fiz. i astron., 1958, 13, No 2, 125-137
Abstract The energy spectrum, the an&,Uar distribution, and the
polarization of electrons emitted in the decay of pola-
rized mesons are calcUated for the four-fermion inter-
action of general form under the assumption of an arbi-
trary degree of parity non-conservation in..iA decay
(see also Ref Zhur Fizika, 1958, No 8, 17433)-
The formulas obtained contain ten real parameters oki,
which are bilinaar combinations of ten, generally, speak-
ing, complex copling constants, that enter into the
Card 1/2
8

SOLNA-R, Vladimir
European Symposium on Criminal Law in Bressanone. Vestnik
CSAV 70 no.5t742-743 161.
1. Clen korespondent Ceskoslovenske akademis ved.

SOLNARS VIAMM4
.Z.184,
International Aosociation for Criminai 1,;w, Veatnik CSAV 71
no.5.-576-577 162,
1. Clen korespondent Ces3coslovenske akademis ved.

B . ( jjZJIVA IIDU, Vol.
St."
ri by an e P.
113h,an,ers of lrlurrj@.Ijs as 5P- ec,.,jOslovav1a-)
U:53, pra-qa, Oz
no. knr.
2 7) iiay ILAICI-
List C).r @;aslv Euro-IjP-all, Access--lis)

L I-q4159-65 EWT(d)/EWP(1) PO_4/Pq_4/Pg_4/Pk_4/P1_4 I4P(c)/AEDC(a)/.
SSD/ASD(a)-5/ASD(s)/AFMDC/AFETR/RA,EN(a)/AFTC(p ) RA,6H(d)/ESD(dp) MLK/BC
ACCESSION NR: AT4047744 S/0000A641000/000/008-2, -"'7
AUTHOR: Solnet;hny*y, E. M.
TITT E: Crudity of system rrot"Lon and crudity of linear sy.,t.!ma with consta.st
paraiLtieters
SOURCE: AN MSR. Institut avtomatiki i telemckhaniki. Tecriya i primeneniye
avz.-. aatiche_sj@igch sistern _@f@e_jr_yind application of automtIc systems).
Moscow, Izd-vo Nauka, 1964, 82- j?,
TOPI@; TAGS: automatic controt, automatic control design, automatic contrit
systi.-in, automatic control theory 1@ I
ABSTRACT: The concept if crudity introduced by A. A. Andri..-.ov. et al. ("Theory.
of Oscillations, 11 Fizmatgia, 1959) is applicable only to synterns describable by
ordinary Cauchy-type differential equations with time -independent right-hand
members. The present article proposes a concept oi crudity which is a get:erali-
zation of Lyapunoves stability and applicable to the individual motions of a system.
Some indicants of the crudity based on a Laplace transform.oi a motion -describing
Card,

L 19465-65
ACCESSION NR: AT4047744
function are established. A definition of the "crudity of motion, i.e., the
stabifity with respect to a parameters is formulated. as well as necessary and
sufficient conditions of crudity in a single-variable syste.m. A concept of
ftgeneralized crudity" is introduced to cover linear systems with motions
containing S-functions or first-kind steps. The crudity of response of a linear
stationary system to an input variable is considered; the system is called crude
(or j,,enerally crude, or asymptotically crude) with respect to a parameter if the
system's transient respoase is crude with respect to this parameter. The crudity
of a linear system with concentrated parameters and delays is also considered.
Fin; Uy, the concept of ar. "integral -square crudity" in introduced and defined.
Ori,,. art. has: 2 figureo and 67 formulas*
A, OCIATION: none
S. 3MITTED: 06Jun64 ENCIA: 00
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SOLNICA, Witold
Galvanomagnetic phenomena. Przegl elektroniki 31 ro.10:-.25-
629 0 162.