SCIENTIFIC ABSTRACT VASILKOVSKIY, D.N. - VASILTSOV, E.A.

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• Collection: Scientific Abstracts
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• Document Release Date: August 31, 2001
• Sequence Number: 19
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

S/18 62/004/001/015/052
The occurrence of a oarticular- B125YB104
device has shown that the steplike surface produced by heating tungsten
wire with direct current depends on the duration of annealing, on the
direction of current, and on the crystal orientation in the wire. The
steps formed on the surface by annealing for a sufficiently long time con--
sist of low-energy faces or similar formations~ A possible distribution of
steps is shown in Fig. 1~ d2 - d1Cos 16, R 6)2is the greatest distance from
the straight lint-, connecting the points of contact of r1jand r11T]to the
surface of the cylinder in the [110] direction.. The 11roo -tile structure"
forming in the (110) zone of a wire annealed with direct current is much
more distinct than that obtained by a.c. annealing. The structure
described above is formed only if the (110) planes appear at the surface
in the direction of the "negative" end of the wire,, In the inverse case-,
a fairly smooth surface is formed, The "abnormal" surfaccewhich are
sometimes produced by d,,c, annealing are due to large deviations of the
~110] direction from the wire axis., The "roof-tile structure" becomes
visible under an optical microscope after annealing for 10 - 15 hrs. The
ridges first appear near the boundary of the "roof tile" after 20 - 30 hrs,
become gradually longer, and finally cover the entire region up to (112).
Further annealing hqrdly changes the relief of the wire surface which is
Card 2/4

S11811621004100110151052
The occurrence of a particular ... B125/B104
slightly wavelike in the first stages. According to'L. D. Landau (Sb.0
poavyaBhohennyY 70-letiyu akad. A. F. Ioffe, P. 44Y Izd. AV SSSR, M.,
1950), a "polyhedron" with blunt edges and vertices corresponds to the
equilibrium shape of a crystal. It is noted that the phenomenon con-
sidered here cannot be explained by Johnson's mechanism, and that the
11rearrangement" of the wire surface duri.ng the'annealing process is
probably due to the decrease in free energy in the crystal. The relief
is produced by volume diffusion. There are 7 figures and 6 referencess
4 Soviet and 2 non-Soviet. The two references to Engliah-language
publications read as followas J. S. Koehler. Phys. Rev., M, n6, 19491
R.Landauer. whys. Rev., 82, 520' 1951-
ASSOCIATIONt Tashkentakiy gosudarstvennyy universitet im. V. I. Lenina
(Tashkent State University imeni V. 1. LW,n)
SUBMITTEDs July 11, 1961
Card 3/4

The occurrence of a particular ...
Fig. 1. (a) Cut through tungsten c,rlinder
ridge 17 consists of the (110) and
into the ridge formed by (121) and
(b) Step of the (110) zone with the
face. . :_- . I .
Legend: _~MO, zone. Fig. I
3/181/62/004/001/015/052
B120104
annealed with direct current;
(iOl) faces and goes over stepwise
(101), as shown by the steps.
structure characteristic of the sur-
A f f]
U,a (110)
110)
A
A
d 001)
(Iff
3oma (HO rift)
lit
7'a
3,
Card 4/4

AZIZOV, U.V.; VASILIKOVSKIY, D.N.; SULTANOT, V.M.
Preparation and indexing of large single-cr7stal tungsten catodes.
Radiotekh*. i elektron. 5 no.10:1631-1635 0 6o. (MIRA 13:10)
(Cathodes) (Tungsten)

. VASILIKOVSKIY
First two years. Pozh.delo 6 no.2:5 F l6o. . (MIRA 13:5)
1. Predsedatell soveta Ukrainskogo respublikanskogo dobrovollnogo
pozharnogo obahchestvp.
(Ukraine--Fire departments)

RABINOVICH, M.I., kand.tekhn. nauk (Khartkov),- BIZYUKIN) N.F., kand.med.
nauk (Khartkov); VASILIKOVSKIY, L.N., inzh. (Mmrlkov)
Apartment heating by means of gas hot-air heaters. Vod. i san.
tekh. no.20-6 F 162. (MIRA 150)
(Hot-air heating)

VASILtKOVSKIY, M.P.
Geouynclinal theory in the light of modern geology. Trud7 SNIIGGIMS
no.13*-56 160. (MIM 16t2)
(Folds-(Geology))

APIKEYEV, A.V., inzh.; VASILIKOVSKIY, N.A., inzh.
T:"jck haulage at the "Dallnii" mine of the "Kara3m*b:3trr'i
Hime Adjainintration," Met, i gornorud. prom. no.406-119
JT-Ag 162. (MIRA 15-9)
(KomsomcIl3koye-Rine haulage)

VASILIKOVSKIY, N.A.
Using conveyer haulage in stripping operations. Met. i gornorud.
prom. no. 206-57 Mr-Ap 164. (MIRA 17t9)
(1)

VASILIKOVSKIY, N. A., inzh.; USIIAKOV, A. I., inzh.
Mechanized quarrying of limestone. Mekh-i avtom.proizv.18
no. 5:28-29 My 164. . (NIRA 17:5)

VASILIKOVSKTYY N~A.; SVINUNHIN, Yu.-U, ; E.-RUPKiN, Ye.F.,~ SHFSlnVP 3114,
1.1 .1
Industrial testirig Of thrt-le--,03le' 14,1,s In ntr--4p jalnea ;f
- IL
the "Karakubskaye" Mining Adm-nistratlon~ M,',,. ! garnorud.
prom. noJM-71 I+/-,Te 164. (WIRA 17,110)

VASILIKOVSHIYP N. F.
Sapozhnikov, A. B. and Vasillkovshiy, N. F. "The investigation of the
possiblilities of appearance of surface layers in the simplest bimetallic
bodies," Trudy sib. Fiz,-tekhn. in-ta, Issue 26, 1948o p. 201-08, - Biblio,:.
5 items
SO: U-5241, 17 December 1953., (letopis 1zhurnal 'rWkh Statey No. 26, 1949)

VA3iLIKOi30-,MLmI,nIi
Data on trie tectonics of thd Uzbek S3r. far,-Iikent, Izd-vo Kvmife~.a ivitir'l-
27p.(5O-h8632)
Q~'315-V34
l.Geology-Uzbekistan.
a f, Structural.
2. ~eoloL-

VASIL SI:I-N_ m y .
:. p. , 1 ,. l'u, j
T ctonics and Snigiaic Condit-oris in the ' orth-astern part of
T3.shkwonts!,%~ R,,A~on. Pii-Iication of Usliek ~..ranch of US,-!", Acarlem~~
of Seimices. 60'.01.0 ~Ical -11:; Li. I'll tP. Talshlc(nitl 1~)10.

VASII.IKOVSKIY, N. P.
35868
voprosy geologii aredney azii v trudakh v. a. obrucheva. trudy in-ta
geologii (akad. nauk uzbek. SSR), VYF. 2, 1948, a. 8-11, c portr.
SO: Letopis' Zhurnallnykh Statey, Vol. 39, Moskva, 1949

VASILtKOVSKIY, N. P.
35869 K otkrytiyu posleyurskikh granitov v zapadnom tyan'-shane. Trudy in-ta
geologii (akad. nauk uzbek. asr.), vyp. 2, 1948, c. 23-27
SO: letopis' Zhurnallnykh Statey, No. 49, 1949

USILIKOVSKIY. N.P.
" , 1. - -. o"
1. .,- 11 : ~
Genetic types of now continental sediments in Central Asia;
deluvium, proluvium, alluviun. Biul. KOIP Otd. geol. 26 no.2-.
3-24 151. (KTHA 110)
(Soviet Central Asia--Geologr Stratigraphic)
(Sedimentation anti depogition~

1. VASILIKOVSKII, N. P.
2, USSR (600)
4. Geography and Geology
7. Strattgraphy and volcanism of the upper paleozoic of the southwest spur of the
Tian Shan'. Tashkent., Izd-vo AN IJz8SIO 1952
9. Monthly List of Russian Accessions, Library of Congress, J&nuarYp -1953. Unclassified.

VASILIKOVSKIY, N. P.
Problem of the Conditions Governing the Formation and Age of the Salt-
Bearing and Gypsum-Bearing Strata of t~e Tertiary Deposits in North-
western Fergana
In the northwestern part of Fergana, in the Ak-Bell, Ak-Chop, and
other strata, in the lover part of the thick tertiary thickness have been
distinguished two strata with large amount of chemical sediments: the
lower stratum, A,, is saliniferous, and the upper stratum, A2, is gypsum-
bearing. The problem of the conditions for their formation and age is
moot. The author disputes with M. N. Gramm (Izv. AN Uz SSR, No. 4, 1953),
who considers that the saliniferous stratum was formed under continental
conditions at the end of the Ylocene or even at the beginning of the
Pliocene. In the authorls opinion (in contract to his earlier views con-
cerning tha Sumsar age of stratum Al), both Al and A2 preferabl~y correspond
to the Massaget stratum in the scheme of 0. S. Vyalove (RZhGeol, No. 6. 1955)
Izy- AN Uz SSR. No. 4, 1953, 67-73 (ftbekistani resume)
SO. Sum, No. 744. 8 Dee 55 - Supplementary Survey of Soviet Scientific
Abstracts (17)

VASIL INOVSICIY, N.- P. , and- VAYNER, - L. -A.
"Geological Investigations of Academician V. A. Obruchev in Central Asial
Tr. In-ta Geol, An UzSSR, No 11, 3-6, 1954
In the course of 3 years (1886-1888) V. A.Obruchev investigated the western
part of Central Asia, from Zeravshan Bange to the Steppes of the north Caspian
region. The main problem studied was that of loans formation. On the basis of
investigations in the Karakum desert V. A. Obruchav classified the sands ac-
cording to the differences In genesis and morpholocy and proposed practical
measures in the struggle against shifting sands. no noted the unique Tien
Shan type of tectonic structures in the Central Asian folding block mountains.
(BZhGeol, No 6, 1954)
SO: Sum. 492, 12, MV 55

0. V
lot
t
USM/ Minerals - Book review
dad: 1/1 Pub. 46 16/21
&thors s Vasillkovskiyp N. P.
-Title- Genetic connection of ore formation with granitoid intrusions
-pe'riodical % Izv. AN SSSR. Ser. geol. 20/2l 3.35 - 3.40, 14ar-Apr 1955
Astract t A review is made of a books "Gonetic Connection of Ore Formation with
Granitoid Intrusicns," by Kh. M. Abdullayev. The author appears to be
an adherent of the theory of dixect genetic connection between post-
m apatic ore formation and granitoid intrusions, a theory which the re-
viewer finds to be generally ac,3epted but latterly subjected to some
doubt. In general, the book is not found to add anything substantial
to the science of mineralogy.
Institution :
Submitted : December 22, 1954

ABDULTAMM, Xh.M.; TABIVIOVSKIT, N.P.
Outline history of geological studies and the development of geolo-
gical sciences in Central Asia under Soviet hogemony. Trudy Inst.
g9ol.AN Us.SM no.13:118-147 156. (KM 10:2)
(Soviet Central Asia_-Geology)

VASILIKOVSKIY, N.P.; NEDZV)b'TSKIY, A.P.
Section of the Zastern Kara-Nazar upper-Paloozoic formations
compared with the section of the Chirchik-Angran Basin. Dokl.
AN Tadzh.SM no.17:13-17 '56. (KLHA 9:11)
1. Institut geologil, Akademii nauk Tadzhikskoy SSR i Institut
geologii Akademii nauk Uzbekskoy SM.
(TaJikistan-Geology, Stratigraphic)

ABDULLILYBY, Kh.H.; VASILIEDVSKIT, IT.P.
e e - -
N.PjasilIkovskiPs reviev of the second edition of my book 'The genetic
affinity of mineralization to granitoid intrusions." Izv.AX SSSR Ser.geol.
21 no.3:108-111 Mr 156. (MLRA 9:7)
(Ore deposits)

V^ /I_'A_OtIS ~c I Yj A P,
GABRILIYAN, A.M., d-r geol.-mineral.nauk; XA�~WKOVZXIYj Y.P., d-r
gool.-mineral.nauk, otvetstvenny7 red.; NOVIKOVA, Ye.I., red.izd-va;
GORIKOVAYA, Z.P., tekhn.red,
[Lithology, paleogeography and problems of the oil-bearing
potential of the Upper Cretaceous and Paleocene of the Fergana
Depression] Litologlia, paleogeogrpflia i voprosy, neftenoonoati
verkhnego mela I paleogena Fergnnskot depressil. Tashkent,
Izd-vo Akad.nauk Uzbekskoi SSR, 1957. 396 p. (MIRA 11:1)
(Fergana Depression--Petroleum geologjv)

15-57-10-13473
Translation from: Referativnyy zhurnal, Geologiya, 1957, 1jr 10,
p 2 (USSR)
AUTHORS: Abdullayev, Kh. M., Vasillkovskiy, N. P.
TITLE: Historical Sketch of Geological Investigation and the
Development of Geological Sciences in Central Asia
Under the Soviet Rule (Ocherk istorii geologicheskogo
izucheniya i razvitiya geologicheskikh nauk v Sredney
Azii za gody sovetskoy vlasti)
PERIODICAL: V sb: Ocherki po istorii geol. izuch. Sredn. Azii
(Tr. In-ta geol. AN UzSSR, Nr 13) Tashkent, 1956,
pp 118-147
ABSTRACT: Development of geological investigations in Central
Asia in the Soviet period can be divided into four
stages. During the first stage (until 1920) no geo-.~-
logLcal investigations were conducted; during this
C>
Card 1/7 period some 20 to 30 works were published, all of

15-57-10-13473
Historical Sketch of Geological Investigation (Cont,)
them having been based on materials collected by previous geo-_
irgical investigations in Central Asia. In the second stage (1920-
1928), during which the natioaal econory was reconstruct ed , there orig-
iriated.' an intensive investigation of' the geological structure of
Central Asia. In 1920 tile Gentral-Asiatic University was estab-
lished, and was followed in 1924 by the establishment of the Turke-
stan Bureau of the Geological Commission, which was reorganized in
1926 into the Central Asiatic Division of the Geolkom. The article
describes a ten-mile geological survey in Fergana, Kam Tau, the
Kirgiz Range, Talas Ala-Tau, 'the Karema ancl Chatkal
Mountains' ana the Turkestan Range. The work described also the
occurrences of hard coal, petroleum, 'Lead ores and raw materials for
the manufacture of cement. In 1925 the Geological Commission pub-
lished a geological map of Turkestan, drawn to the scale of 40
versts to an inch; in 1926 a book by D. V. Nalivkin "Geological
Sketch of Turkestan" made its appearance. The Third all-Union Geov'
logical Convention was held in Tashkent in 1928. The third stage
Card 2/7

15-57-10-13473
Historical Sketch of Geological Investigation (Cont.)
(1929-1941) corresponds to the first five-year plan and is charac-
terized by further broadening of the geological works and geologi-
cal explorations. Local scientific-invesz;igational organizations
were strengthened and new schools were established, the latter pro-
ducing large groups of native geologists since the early 1930's.
In 1938 the Central-Asiatic Organization for Geological Exploration
(which had grown from the foundation of a small Central-Asiatic
Division of the Geological Commission) was subdivided between the
geological administrations of the Uzbek, Fdrgiz, Tadzhik and Turkmen
Republics. I in the same years within
these republics there originated fiiial branches of the AS USSR.
Starting with the third decade, geological maps drawn to the scale
of 1:200 000 began to ffiake their appearance; at the beginn in of
the fourth decade geological mapping to the scale of 1:500 01 was
started for almost the entire upper part of Central Asia I while the
western plains were being mapped to the scale of 1:1000 00(l Three
volumes of Geologiya Uzbekskoy SSR (Geology of the Uzbekskaya SSR)
Card 3/7

15-57-10-13473
Historical Sketch of Geological Investigation
were published in 1937, and in 1941 they were followed by "Geologi-
cal Map of Central and Southern tarts of Central Asia". Much suc-
cess was achieved in the hydrogeological. and engineering-geological
investigations of the territory. In the third decade the Institute
of Ground Waters in Uzbekistan published fifteen issues of the
"Materialy po gidrogeologii Uzbekistana (Hydrogeological Papers of
Uzbekistan)". The 'understanding of petroleum, coal, kaoline clay,
precious and rare metals, antimony, mercury, arsenic and others was
greatly broadened. An important part in learning the interior of
the land was played by the Tadzhik-Pamir expedition of the AS USSR,
which lasted for several years. In the fourth stage (the second
world war and the subsequent years) the activity of geological bu-
reaus of the Central Asiatic republics was greatly intensified.
During the war the Turkmen .., Kirgiz , and Tadzhik - affil-
iated branches of the AS USSR were organized, while the Uzbek '
branch was reorganized into the AS Uzbek.. . 33R. In the last dec-
ade most of the geological maps were produced to the scale of
Card 4/7

15-57-10-13473
Historical Sketch of Geological Investigation (Cont.)
1:50000~ 1:10000of 1:200000. A great achievement of this sta&e was
represented by the publication of five volumes of "Geologiya boyuza
(Geology of the Union)", produced by the employees of the geologi-
cal bureaus of the republics and dedicated to the republics of Cen-
tral Asia. Other great achievements in these years consisted of
studies of petroleum in Turkmenia and Fergana, brown coal in the
Angren, . . Basin, a number of iron ore occurrences,of potassium
salts deposits, etc. Soviet scientists brought in much knowledge
of the paleontology and stratigraphy of Central Asia, and especially
the paleontology and stratigraphy of the Paleozoic. A general
stratigraphic system, worked out in 1926 by D~ V. Nalivkin, was used
as a basis for all the subsequent investigations. In the 30 years
since the publication of his work, almost all the subdivisions of
the Paleozoic were found within the territory of Central Asia, the
fauna of these divisionswere studied and numerous monographs dealing
with the groups of fossil organisms were written. The Mesozoic and
Tertia r~ deposits were particularly well investigated because of
Card 57

15-57-10-13473
Historical Sketch of Geological Investigation (Cont.)
their relation to the coal and petroleum deposits. The coal-bearing
deposits of the upper Triassic and Jurassic led to the publication
of numerous paleobotanical works, the study of oil-bearing deposits
--to the detailed work of the Cretaceous stratigraphy. In the
realm of petrography of the sedimentary rocks and also in the lithol-
6gy,-. great successes were achieved in subdividing the red Creta-
ceous deposits and the continental Cenozoic strata in Fergana. A
new criterion was applied to the correlation o'L sections--the rhythm&
*trat Jgraphi call! - -_ ' criterion. Works of V. 1. Popov, the author
of the monograph, "Litologiya Kaynozoyskikh molass Sredney Azii
(Lithology of the Cenozoic Molasse in Central Asia)", were very
important in the development of lithology. In the subjects of
tectonics, volcanism, regional geology, the investigations pro-
gressed mainly along the line of clarifying the system of D. V.
Nalivkin, according to which Central Asia was divided into the
northern (Caledonian), central (Variscan) and southern (Alpian) arcs.
With t~e progress of time this system became clearer in details and
Card 6 7

15-57-10-11,473
Historical Sketch of Geological Investigation (Cont.)
underwent some changes from the original works of V. A. Nikolayev,
V. I. Popov, A. V. Peyve. Investigations of A. S. Uklonskiy, the
proponent of the views of V. N. Vernadskiy and A Ye. Fersman, were
outstanding in the sciences of mineralogy and geochemistry. In
petrology and metallogeny the works of Kh. M. Abdullayev, V. I.
Smirnov and A. V. Korolev are particularly interesting. One of the
main features of metallogen iC 4nvestigations and genetic clarifi-
cations of Kh. M. Abdullayev lies in his study of magmatic rocks;
this study is considered basic in the metallogeny of hypothermal
complexes. Writings of N. A. Smollyaninov are dedicated to the
petro&aphic investigation of ore depos~its. Many works were
written on the subject of sedimentary mining resources, on coal
and oil reserves, on the nature and balance of ground waters and
on engineering-geological properties of loess.
Card 7/7 D. I. Gordeyev

S/16 61/000/009/010/056
D228YI)304
MUM Vasil I oyakjy,_N~~
TITLE: Theory of the earth's crust
PERIODICAL: Referativnyy zhurnal, Geofizikaq no. 99 19612 12,
abstract 9A91 (Tr. Sibirsk. nauchno-issled. in-ta geol.,
geofiz. i mineralln. syr1ya, no. 5p 19590 95-128)
TEXT: Different data on the composition and structure of the earth
and inner geosphereaq amongst which the structure and development of the
crust is described in more detailq are brought together. The genetic
classification of crustal types is examined. Large sedimentation troughs
arise as a result of the initial stages of orogenesim. Basalt is melted
out of the peridotite mantle; the granite layer is formed through the
granitization of the basalt layer (or of part of it) and the products of
its disintegration. Orogenesis is explained by the earth's contraction-
in consequence of the compaction of the core and the lose of part of the
mantle's material--and by the increase in the volume of the crust. Sub-
Card 1/2

Theory of the ...
S/169/61/000/009/010/056
D228/D304
crustal currents are allowed. The problem of endogene ore-formation is
considered. There are profiles illustrating the stages of crustal d:- V/
of the distribution of different types of crust
velopment and
a map
11 -_
the earth, Bibliography--07 references. fAbstracter's notes Complete
translation.-7
Card 2/2

VASILIKOVSKIY, N.P.
Geological role in the champs of the level of the vorld .ocean.
Trudy S171IGGM no.13t79-.89 160. (MIRA .16:2)
(Oceanography)

VASILIKOVSKIY, N.P.
Devonian and Pre-Devonian intrusives in the Angren basin.
Trudy Sred.-Az.politekh.inst. no.12:121-127 161.
(MIRA 18:12)

;SOURCE: Ref. zh. Geofiz., Abs. 4G11
1AUTHOR: VasilItU Radkevich, Ye. A.; Smirnov, A. M.
TITLE: Role of gecohysics in tha study of tie Pacif.c Ocean zone and the
proposed plan for geophysical work
CITED SOURCE: Byul. Tikhookeartsh. kom-ta po geol. i metallogenii Tikhookeansk.
rudn. poyasa, ". 1, 1962, 56-66
TOPIC TAGS: superdeep drilling, 4eophysi-cal exploratio earth crust, seismic
sounding, earthquake, gravimetry, gravimetric eur-vey, airborne magnet=Cter 13urvey
TRANSLATION: The proposed geoptivsical wcr'- _n the eastern part of the SSSR w111
be an trtegra' Pqr( !he -tnT,V a and
lie M8 e. - e, -4 S 1 1' pt'. W: 47-"
_'ev e -.e -.;~ (-. : ~_'
clarification of the most impnrtant det -i f r~,4_ ec~ 1-g! rg 1 9 t ruct -ire r~! 'ht'
Card ,I j

L 24435-65.
ACCZSS1 ON XR: -AR4039992
Soviet sector of the Pacific Ocean zone, having decisive importance for the
idetermination of the pattlerns of distributian of m1nerals. There is a brief
discussion of general theoretical problems requiriig imediate solution. The
authors note the possible ways cc golve -hei5? prcb'em-i by geophvgic-al Merhr-ds and
discuss the problems of regional gecphvsical inves-,igations for clarificac'~~n ct
the peculiarities of the sLructuce of the Soiiet sector of the Paciftc Ocear -4-b-
ile rone. It is ernphaitzed rhar
e zi: i i ,-v eaitr 5 --iB, '-- 4c,-. ;,-a- JtffflerenL reglon~
snlved complexly. Among such intearated eaciihvs1ral irrj~at!gitfn-T,.s, 9! P7-1
"~-e g:'o7~ .- , e . . M. -- ;' :,:,. .I4rAV'1Zne11 111C 5~jrve~~
An.!
plosions. A tipecific plan is rrnpesi-c, ~~r i,vecr igar!(-n -f the earrl- s
the Fit-, Fa8' t~~ Lr-,e -Aeep B em R'J~gp~!
princllpal f, r W 0 r
Lhe jea ci Japan, .1)1)(n,-( e-Ailn Mqr-rr4- 1 -~4' iI;pa -f kh c ! Er n-
e Cri. S&SR K-AMCrle a. ---!K4'