SCIENTIFIC ABSTRACT VERTSNER, V.N. - VERTUZAYEV, YE.D.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R001859610003-8
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: September 1, 2001
• Sequence Number: 3
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

,-, U6:57-66 EwT(J)~
X ~ Rs APS015764
(m)/EWP(t)/ET1 IJP(c) AT/JD
SOURCE CODE: UR/0048/66/030/005/0778/0780
AU7HOE-.,. Vertenar, V. K.i Lumonov, R. I.; Chentsov, Yu. V*
ORG: none
TITIE, The use of low Vol ity electrons in an glectron scnnning_mici2!S222_5eport,
Fifth All-Union Conference on Electron Unroscopy-Tiold in Suny 6-8 July 19657-
SOUWN: AN sssR. rzvdstiyaq Soriya f Izichoskaya, v. 30, no, 5, 1966 0 778-780
TOPIC TAGS: electron microscopet electronic scan, electron beam, electron energy
ABSTRICT: An electron scanning microscope employing an accelerating potential of from
500 t,3 2000 V has been developed and a pilot model has been constructed. The use of a
low accelerating potential entails some deterioration of the resolving power but pro-
vides higher sensitivity 'to small variations of the electric and magnetic fields at
the aurface of the specimen. The low penetratin.- power of the low energy probe beam
makes it possible to detect very thin films of foreign material on the surface of the
specimen. Moreover, the secondary emission coefficient of some insulating materials
for low energy incident electrons is close to unity, and it/is accordingly possible to
study such materials without first coating- them with metal4-D A cross section of the
pilot model microscope is shown in the figure. The beam from the electron gun I is
focustied by lenses 2 and 3 onto the specimen 5. The boom in deflected by the windings
4, tl-.e currents in which, are synchronized with those in the deflection coils of the

[-AC-C- MRs AP6015764
kinescope on which the signal from the specimen, developed
across resistor R, is displayed. A decelerating potential
can be applied to the specimen holder in order further to
decrease the energy of the probe electrons at the specimen
The diameter of the probe beam at tho specimen was I mi-
cron, and the instrument was found to be sensitive to a
variation of 0.2 V in the potential at the surface of the
specimen. The size of the raster on the specimen could be
varied from 12 x 16 mm to 0.3 x Ool mm# corresponding to
magnifications on the kinescope screen ranging 1rom 17 to
700* Several photographs recorded with the instrument are
presentedo Orig. art. has: 5 figures.
Cross section-of low velocity electron scanning microscope
SUB CoME: 20/ SU13M DATS: QO/ ORIG REF: 001~ OM MW: 000
L_Card 2/2 1,1,7A-P

L 36,137-66 EWT(m)/WP(e) WH
ACC 11R, AP6015778 SOME CODE: UR/0040/66/030/005/0835/0839
AUT11011.: Zhdanov, Gl. S.; Vortanor, V. N. _'.';
a Z/
03G: none
ell
TITLE; Electron microscope observation of the formation and growth of ice crystals
fRopo--t, Fifth All-Union Conference on Electron Microscopy hold in Sumy 6-8 July 196571
SCURCA: AN SSSR. Izvestiya. Seriya fizichoskaya, v. 30, no. 5, 1966, 835-839
TOPIC TAGS: electron microscopyj crystal growth, ice, water, electric field
AMTRILCT: The growth of ice crystals on cold thin carbon and quartAilms was obqorv-~
ed with an electron microscope. The ice crystals formed by condensaiion of residual
vinter vapor which was present in the microscope chamber at pressures rnng~ng from 10-51
_3
to 10 mm 1(g. The accelerating potential was 80 IcV, the elect ion bean diameter was
5-10 microns, and tho current density in the Lenm was 0.01 A/cm - Under those condi-
tions heating of the substrate by the electron beam was negligible. Ilexagonnl, cubic,
nnd amorphous forms of ice were observed. Tho hexngonal form was stable over a wide
ranUe of temperatures; the cubic form could be obtained free from hexagonal admixture
only at hi-h vacuum and temperatures below 1450 K. A sharp change in the character of
0
the crystn1lization took place at 170 K; instead of the formation of large crystals,
there was observed the almost simultaneous appearance of a large number of nuclei whi
LC,rd 1/2

L
ACC KRi AP6015778
Treforontinlly in the pl. no of the substrate. On the quartz Etibstrates there
grew
were observed filamontnry Ice structures, which grew rapidly toward the Irradiated
portion of the film. nlieso structures are ascribed to the action of electric fields
duo to charging of the quartz substrate by the electron boam. From a compnrison of
tho promt Obsorvations with thoso of i.T.Unrtlott, A.P.van don Houval, and D.J.
Mason (Z. angew. Math. und Phys., 14, 599 (19G3)), it is concluded that the electric
field strength exceeded 500 V/cm. The polycrystalline nature of the filanentnry
structures was clearly evinced on the electron micrographs. The authors thank L.V.
Degteva for assistance in preparing the substrates. Orig. art. has: 5 ligures.
SUB C(DE: 20/ SUEM DATE: 00/ ORIG-REF: 002/ OM REF* 007

r-r1r, V Mq
--0;29 -66-91T ri -WP
N'(~'77AMM2456 SOURCE CODE:- n/oi 8 l/66/boB/oO V10
AIJTHORI:.* Zbdanov
G. S.; Vertsner V. N.
,_
ORG: %.one
TITLE: Direct observation of condensation and crystallization of
ercuri,~ 4
, 106-1-1-1nol-
Gl 1027--
, -v. 8- no. It
SOURCE:, Fizika tverdogo tela
, 1966
,
,
.
electron microscope,
TOPIC TAGS:- mercur crystallization, ny--tal film,
y, vapor condensation,
-- ---- _
par-tic-~:16-,r,--ollioion/Blimiskop I-electron microscope,
ABSTRA-M Inasmuch as moA elao-t-i~on--mi:croacope-Inveslv-iF,,ationa--of-the-
kinetifts of the growth of thin films produced during evaporation of
metals in the microscope directly display only the growth of already
produced particles, and not the more interesting process of their occur-
rencei the authors investigated in an electromicroscope the condensation
of meicury on cooled carbon films. The 'Ellmiskop 11 electron micro-

3cope~ with resolution 1 1.5 nm 5 was used. The mrcury
(10 1
7
vapor.:pressure near the object was estimated to range from 1 x 10-
-8
2 x I(' mm Hg, depending on the evacuation conditions. The carbon
Card 1/2'

Wd a WHOW M-
r7
L 29291-66
ACC NR, AP6012456 -
films %~re cooled to 190 125K. B--cauE!e of ice formation, slow con-
densatJon could-be ob--erved only at temperatures below 135K. At al).
temperatures from 190 to 125K, the mercury condensed In the form of
liquid drops. The liquid. mercury particles were not produced S11TIL11tane-
ously, but during the first few minutes of condensation, after which no
formation of new particles was observed in practice. With Increasing
temperature, the rate of condensation decreased. The lifetiME! of the
mercury atoms on the substrate at 135K and the binding energy with the
substrate were calculated from the results. The values obtained were
4
approximately 1.5 see and were found t- o be -1 x 10, sec and -10.5-kJ/mole.
The kiretics of the condensation of the mercury is described from the
point cf view that the condensa"s-dion begins with random collis".ons betvLlen
m.LgratJng atoms, and that the Initial mercury drops grow from condensa-
tion nvolei. containing only several atoms. Many of the secondary effects
occurrJng during the crystallization are briefly described. Orig, ~rt.
has: 4 figures..
SUB C01 jE: 20/ SU13M DATE: 29J'ul65/ ORIG REF: 0061 OTH REP: 009

V. N. (Phys)
-72R.TzTrEll V 11 (Y" "Clinical Chir.-cteristic's of a Hixer In-
feetion of Scarlet Fever and Chicken Pox-.11 Sub 22 SeD 52.1 SCcond Moscow
State Medical Inst imeni I. V. Stalin. (Dissertntion for thf~ De-ree of
Candidate in Vedical Sciencf~s).
SO: Vechernay~ Moskva January-December 1952

V M SKER, Y.N.; IYANOVSKAYA, T.Te.
112"Wo .1 --'''.
I A case of fatal chicken pox in a one-year-old child. Pediatri-is,
no.1:78-80 Ja-F 154. (MIRA 7:3)
1. Is detskoy gorodskoy klinichaskoy bollnitsy No.1 (nauchnY7
rukovoditell - deystviteltuyy chleu Akademii meditsinskikh
nauk SSSR'professor H.A.Skvorteov, glavnyy vrach Ts.V.Prokhoro-
vich). (Chicken pox)

V1WSMj V.H.; KAZAROVA. N.M.
Clinical aspects of encephalitis in chicken pox. Pediatrita 39
no~4:44-49 Jl-Ag 156. .(MIak 9:12)
1e Is 1-7 Moskovokoy detskoy klinicheskoy boll nitey (glavW vrach -
SaBlushennyy vrach RSISR Ye.V.Prokhorovich. nauoluW rukovoditell
prof. D.S.Futer) i Gosudarstvennogo pediatricheekbgo instituta
RSIPSR (dire - )mndidat meditsinskikh nauk V.N.Kerachevtoova)
(CHICKEN Me compl.
encephalitis in child., clin. aspects)
('INCIIPBALITIS, etiol.,arA pathogen.
chickenpox in child, clin. aspects)

I V. ~N
Clinical characteriotice of mized infeatioba of diphtherist and
chickenp=* Pediatrila 38 no,908-62 0 160. (KMA 13M)
1e Is detakoy gorodokoy klinicheskoy bolluitay 116,1 Monkrr
(glavn~7 vrach - zaaluzbenrqy vracb RSFSR Ye,V,, Rrokbort;Aah).
(CH:ECMqPOX) (DIFTMU)

AWO-PER,jp~~;Ukolayevna; FRlDl-Wl, R.A.p red.; VATVEYEVA, M.M.,
tekhn. red.
(Chicken pox] Vetrianaia ospa. Moskvay Medgiz, 1963. 171 p.
(MIRA 17:1)

S/04,'3/16 i/027,1003/02 1/025
MHORS: Illin, M. M. SolovIyev, A. M., Vertsner, V. N
-76- - _o
Dutov, G. G., Kolchev, B. S., and fFork v, A.
UTLE: A oommercial L",IA?-l (MAR-1) inutrument for X-ray
microanalysis
PERIODICAL: Akademiya nauk SS5R. Izvestiya. Seriya fizicheekaya,
V- 27, no. 3, 1963t 420-426
TEXT: Thio paper describes in detail a new FIA?-i (I&AR-1) X-r.-y micro-
analyzer developed and tested in the Krasnogorskiy m,~khaniohesliy zavod
(Krasnogorsk Machine Plant~. The instrument consists of the 2-'ecordee-
and of the microanalyzer itself, comprising the electronoptica-. syote'm
pxolr_~. 2 X-ray apectrometers, a specimon chamber
ar.4 ;h-- Vaimqm
Laxwwami~~4-Thc-, Atlron- -6 d-urae'.Ua5i &T,,t 907, jeoVroaj~_ ~gU,~~
~ "V k'-
i
--ourface--of-1-the-~:apecimen - at a magnif ication Of 450-X i7i~,~at-ioa
_-X-ra wave-
being g I fL The non-vaouum meter anal-yzea yo -with a,
Card 1/2.
f

5/048/63/027/003/0?1/025
F . - ~ /Frz3a
comm rcial.
0
Isngth of UP to 1-5 and the vacuum spectrometer those from 1.5 to 10 A*
tie aPedtra-are analyzed using Johann's method. 12he Bragg angle3 range
from 1B to 400 The analyzer crystals are [134-0) quartz crystaLs witha
xadius of curvature of 500 w. The diameter of the X-ray source is 1-2U
t3is value dedenda on the diameter of the electron probe, which is cl~.
7ae amperage in the focused probe, is about 10-6 A and the curre-it
stability amounts to 0.5 IJ4 per hour. The instrument makes deternination3 on-'
tie specimen possible in the 1 - 2 range. Vihen the specimen is impermeable,
tie ohange in the Brag(.- angle of 'he elements from Mg to U can b~ leter-
irLned by using both spectrometers. The distribution of the element in the
s3ecimen to be determined in the given direction can also be detarmined.
Tiis is done by diaplacing the specimen under the alectron probe with
-eriatic
aa dectric motor at a fixed Bragg angle corresponding to a chara,34.
fc-equency. The dispersion and sensitivity of the instrumient wera studied;
t,e sensitivity in an aralysic o fconner viG the 7 I-o-,blet ras 0 1 14
Tiere are 6 figures.
Cird 2/2

SOLOVIUVI A.M.,,
Problem arising in designi an X-ray microanalyzer. IXVOAN SM.
Ser.fiz. 25 no.6s691-694 je 161, (KM 14 s'6)
, (X-ray microscope)

SOLOVIYEVO A.M.; VERTSNERj V.N.; IL'Iff, M.M.; TOPORKOV, S.A.; KOILfIEV,, B.S.;
DOTOVY
Industrial X-ray spectral microanalyzer MAR-1. Izv. AN SSSR.
Ser. fiz. 27 no.%1162~1165 S 163. (PaRA 16%9)
(X-ray spectroscopy)

EWT (m)/T ETPI te)H
- - __ _L _ - Tfff66[66bT0_06_[666_~job62_
ACC t~*61%24 SOURCE CODE: LMT6
jN`NENj.W_:_ Kutateladze, K. S.; Verulasfivili, ft. D.
OR( none
TBLE. Electrical insulatioixglase4l 'Class 32, No. 179884~ [unnovmccd by q~W. W
Insti Ve of Constructfo--n-TRE-eri-Tis Milftskiy Govudar-
Stite Scientific Researo-FF
stiennyy nauchno-issleaovat6_V_8kiy iristitut stroitellnykh materialov)]
SOURCE: Izobreteniya, promyshlennyye obraztsy, tovarnyye maki, no. 6, 1.966, 62
-TAGS:
TWIC - electrical imulation glass, dielectric glass
AB3TRACT: An Author.Certificate bas been issued.for an electrical insu-7ati!Dji glass
4i' h- gcod aieli-e-c-trIc - propertiesX-The - glass has the- foll-oving -composition, 16 Si02,
52-58%; Al 0 --- 8-10,%; F(1 2"31 -1-5-2%; MnO, 5-7%; CaO, 8-10.5~; m0, 4-6%*,
Ka 8_13~_N20, 2.5-0. In addition to -these ingredients the glass contains
T102'_ [BO]
st BCODE: u/ suBm DATE. o6ju16h[ ATD FRESS: 1~ 1 2
uDc: 666.112.3
CA 1/1 141 666.u7-9:537.226

-.-ARULAMILI V 1.
V-MW.-X=WAVW
ConditiMs for the tranwdsaion of Taxoplamm gondil from mother to
fetus, 'Dokl, AN SSM 149 noo4t999-1000 Ap 163. OaRA 160)
1. Vtoroy Moskovskiy maditainakiy inatitat ta, N.I.Firogova*
Predstavlano akademikm TeARavlovskim,
(TOXOPLASMOSIS) (FIMS-DISEASES)

i4k "jZ~TjB"1P?t)1vPw
i--A-a-aR-,-AP6O13575 IJP(c) JD SOURCE CODE: URI)032165IQ3110081.102DA(',.,Icl'
AIMOH: Lomberg, B. Vertman, -A- A.: Y-t-i-k-o--b-ls-o-n-----A^*-.Mj-*----Zhelidtiovi--Ve
Polyakov,
ORG: Institute of Metallurgy im. A. A. Baykov (Institut metallurgii)
TBLE: Unit for measuring the interphase metal-slag tenaionat high temperatures
N
SOLRCE: Zavodskaya laboratoriya, v- 319 no. 8, 19659 1020-1~1
TO] TC TAGS: furnaceP slag, thermocouple, vacuum seal, x ray application, molten
melal, corundumv magnesite
AB! -TRACT: This devicel a- resistance furnace with a two-filament, heateri
A i.-rucible is placed a the isothermal zone of the heater on a magne*ite
su)port. The melting point is measured ,dth a platinum-platinwv-rhodium
th)rmocouple sot on the bottom of the crucible. A device mounted on the
to.3 cover permits adding of slag during the experiment. SozLling of -;he
as3embly is done with vacuum seals. Vicding windows are covered with
O.'~-0.2 min thick aluminum foil. Construction of the unit permits it:)
operation in either a vacuum or in a neiitral gas atmosphere. Experiments
were conducted on corundum and magnesita cruciblesp 35 M :W diamotor.
A-substrate cut from a cylindrical crucible of ;imaller diameter made of the
sane material is placed an the bottom of the crucible. Diameter of the
metal drop on this substrate is 18-20 mm. To obtain an upper edge.of the
Ca,,d 1/2 UDC% 620.1.052
now

L 3214-66
AC( NRI AP6013575
Gub strata border in the lem of a true sphere., it is polished with convex
and concave spheres. This prbvided for wjanetry of the liquid metal dropo
X-riys were takenwith an RUP-1 x-ray device.
Because of the protective shields and the intensive water cooling of the
fur.aace housing it is possible to place the fi2m at a minimum distanca from
the object. The film is placed in an aluLd-num cassette protected frota
scattering radiation by lead plates, 2 mat thick. Distance from the center
of the drop to the film is 10 cm and 3-10 cm to the focal point of the tube*
A clearimage of the metal drop in the slag is obtained when the voltage on
th( tube is 180.kilovolts, current force-15 milliamps) and at an exposure
tinTe of 40-60 seconds. The interphase stress is calculated cccording to the
dimensions of the drops found. The interphase tension of certain nickel-
bate alloys with slags was determined. The unit can be recomended for
moi~ouring.thel.,iite.rphaee..terision, between metals and slags of different
cojipositions. Orig. art. has'. 2 figures and 1 tables EJPPZI
SU 11 CODE: 13 SUBM DATE: none ORIG REF.6 001
__g Ird 2/2

ITRT-ONO A.
"EM NOLOGY
"ERIODICAL- BUE01-111CM0 PRZ-o2ffSUJWE. Vol. 7. no, 9, Sept. 1958
'rEP-TUN, A. Evalustion of tl~e possi'Oilities of realizing a project,
-,)erfomed vith the assistance of future patrons, postulated to avoid
,iistakes in dwelling plannin,,-. p. 59.
MontIly List of East European Accessions (EEAI) W Vol. 8, n). 4.
April, 19'9, Unclass

7 J
VERTUY, A.
The methodology of dr,,wing up projects of organising construction work in the light of
recent decisions and instructions.
P. 32 (Budowdetwo Przwwslowe) Vol. 4. no. 6. June. 1955, Warszawa, Poland
SO: MONMY INDEX OF EAST ELROPEAN ACCESSIONS (EEAI) LC. VOL. 7. NO. 1. JAN. 1958

v..1 - /' ~ 7 1" / 11,.
VERTU11t A.
Graph-1c charts for annual plans in construction.
P. 58'(Budownictwo przemyslowe) Vol, 49 No, 91 Sept,, 1955o Warazawal Poland
SO: HONTHLY INDEX OF EAST EUROPEAN ACCESSIONS (EEAI) LC, VOL. 7,NO. 1, JAN. 1958

- - -
I-,- - - - -- -----
VlaiTUNO A.
Stages in planing the organization of construction and work.
F. 31 (BUDOWNICTWO PRDIYSLVdv-) Poland, Vol. 6, No. 9, Sept. 1957
30:
I Monthly Index of East Equopean Accessions (AEEI) Vol. 6, No. 11., November 1957

VMl um~ A.
TECIMOLOGY
VERrUM, A. Evaluation of the possibilities of realizing a project, performed with
the assistance of future patrons, postulated to avoid wistakeB in dw-1.1ing planning.
P. 59.
Val. 7, no. 9, Sept. 1958.
Yonthl.y Index of East European Accessions (EEAI) LC, Vol. 7o No. 12f Dec. 158.

GOiOWSKI Tadeuvz; VERTUN-GOROWSKA Barbara.
ilyperfunctioning'nodulir goiter masked by circulatory Usufficlency
(masked thyro-cardiac syndrome). Pol arch# mad* wesineto 34 no.-8:
1(Y73-1(779 164.
1. Z I Katedry Chorob Wewnetrznych Studii Dokaztalcania Lekarzy
Akademii, Medycznej w Warszawie (Kierownik: prof. dr. med. W.
Hartwig) i z Oddzialu Chorob Wowne'v'rznych Szpitala CzernW.Ovskiego
w Warazawie (Kierownik: prof. dr. mod. M. Felgin).

YAYEV,
A.A. pr
KI J)RY AVTS&V f catt26#
an -k
and prLTer- !.r, (10-RA ISSIO)
rC--52
42 r

KIDRYAVTM, A.A., prof.; VERTUNOV I"
-.-A.- starshly naucbnyy sotrudnik
Application of radioac#vu iaotopea in stockbreeing. Zhivotnovodotvo
24 no.9t73,-71+ 8 162. (WA 15i22)
lo Veenoyuznyy institut eksperimentalino vaterinarii,
Avery
(Radioactive tracers) tinary physiology)

VZBTUN I. elo~
Autmicropipet. Trudy VIW 26slW-189 vu (MU.1612)

KMWAVTSBV, A.A., prof.; VIRTMV, A.I., nauchnyy sotrudnik
Use of radioactive tracers in stock breeding an4 in veterinary
medicine. Vaterinarila 36 uo.9:U-17 S 159. MRA 12:12)
l.laboratoriya fisiologil Veenoyuznogo instituta okeparimentallnoy
vaterimarii (TIEV).
(Radioactive tracers) (Veterinary medicine)

-AA- Lnd A. 1.
"Appl.11,10.1,wil of
p-ilanuted at Ufv C'mf-,renro va Uz;,p Ool of in Aflnntl MoloZ7
In 141dical Gejonroll, Virlco Cit,7, 21 11,07 - I VOC 2261.
ldb. or Nertral rnd Pettholcgl"l PhjnJolnjV, AU 7tIprbirrjy F410A. Innt. Vi-it.

VVRTUNOV L.N.; TSEKHWYETRYUK, A.K.
Possibility of using clay from the Tertiary sediments of the malyy
Orgochor anticl-ine for making clay muds. Izv. vys. ucheb. zav.;
neft' i gaz 4 no.303-36 161. (MIRA 16:10)
1. Frunzenskiy politeklinichaskiy institut, Issyk-kultakaya
ek"ditaiya.

VERTUN LY
Y ,
flew data on the occurrence cepth of Paleozoic Igne(r-is rocks in
the Chu Valley. 1zv.vys*ucheb#zav,; geol. i razv. 7 no-3:11,1-
W mr 16.4. (MIRA 18:3)
1. FrunzenskAy politekhnicheskiy institut.

J=OV
Authiganous minerals and some problems of the paleogeography of
Cenozoic formations in the Issykkull basin. Nauch. trudy TashGa
no.256 Geol. nauki no*22tlO9-IU 164 (MIRA 18t2)

VSRTUNOV) L.N.
Faciso analyois of neogwdo Molasoo depooito of the
southeastern part of the Chu Depression based on the
materials of ueep borings. Dokl. AN SSSR 147 no.1:174~176
N 162* (MM 15:11)
1. Frunzenakiy politekhmichookiy institut, Prodstavlono
akadWkom D.V. Nalivkinym. stratigraphic) .
. (Chu Valley6-Geology

VERTUNOVV L.N.
Problem of oil and gas poteatials-*C Tertiary continental molasse
sediments of the ooutbweotern Iss:rjc-Kull Basin (*Drthern Tien Shan).
I2v.vys.ucheb,zav,; neftt i gaz 3 no.30-8 16d. (IMMA 3-4: 10)
v
le Frunzeaskiy politekhnicheskiy institut.
(199YkAhl' region-Petroleum goolop)
(Issyk-Kull region--Gao,, Natural-Geology)

VERTUNOV., L.N.; GRIDNEVI N.I.
Minero-petrographic characteristics of recent alluvial-colluvial
deposits in the Issyk-Kull Basin. Izv.AN Kir. SSR. Ser. set. i
tekh.nauk 4 no.7tlO7-111 162. (KMA 160)
(Issyk-Kulf region-Petrology)

VERTUNOV, L,N.1 ILIYASOVA, A,S.
.1 1. - -, ,
Mineralogical composition of the Tertiary continental sediments
in the southeastern shore of the lake Issykkull. Zap. Kir. otd.
Vaes, mine ob-va no.3t8l-92 162. (MIRA 17:11)

VXRTUROV, L.N.
Authigenous tou=allne In Cenozoic Release deposits In Worthorn Yorgana.
Dokl.AN Tadsh.SSR no.14:29-30 155,, (xM 9:9)
1.3ndnonxiatakly gesudarstvenury universitot iment M.Lonina. Prodstarle-
no chlonea-korrespondentom AN Tadshikokoy SUR RaBoDaratovyw.
(Forgoma-Goology, Stratigraphim.) (Tourmaline)

TIBMOV. L.N.
Facies of Cenozoic molavae of northern -vergana. Tru4 Inst.geol.
AN lir.= no.8:57-77 156. (MLBA 10:2)
(7ergana-Geolog3r, Stratigraphic)

VE MML ~Lx
Lithology of Cenozoic molasses in the Mayli-Say anticline (northern
Fergana). Izv.AN Kir, SSR. Ser. est. i tekh;hauk 4 no.7:19-38
162* (?MU 16:3)
(Fergana-Rocifo, Sedim ntary)

- ... ~ - -.-- r~ I I - I .., ~ - - I ~ , : ~1. ~- 1 . -, I I~--k ~ i !- I:,,-.
. - ~1111 . VW pu~. ~,--
MMTUNOV LUN.J. TSZOMTSTRYUKs A-K-
~ - = j - = . .
Gas showings in the Neogene sediments of the Iavyk-Kull
Basin& Gazo prcm. 9 no.60-5 1641 (KMA 170)

VERTUNOV9 L.N.
-
Cover thickness of Falaosoic igneous rocks in the Chu Depression
(Kirghiz S.S.R.), Izv.AN Kir. SSR. Ser. eat. i tekh.nauk 4
no,7iI03-105 162. ~ I OURA 160)
(Chu Depression-Rocke, I&eoua)

VERTUNOV., L.N.
0-
Facies characteristics of-the Tertiary continental molnese
sediments I" Oe southeastern part of the Iosyk-Kull trougli
(NOrthem Tien Mum), Izv, AN Far, SSR. Bar. ant. i rekh. nauk
2 no.9:121-130 T60. (MIRL 14--7)
Iosyk-KiLl (Tien Slum)--Geology stratigraphic)
I. gocks., Sedimentary)

L.N., aspirant kafedry petrografit I litologil.
Petroloa of &oil* In the Tashkent depression. bbor.nauch.trud.
asp.SAGU no.li75-79 152. (MLRA 9:5)
(Tashkent Province--Petrology) (Tashkent Vrovince--Soils)

15-1957-10-13963
Tilanslation from: Referativnyy zhurnalp Geologiyap 1957, Nr 10,
pp 88-89 '(USSR)
AT ITHOR ,Vertunov,, L. N. 7-
VME: %6 Cenozoic Volasse Facies of Northern Fergana (Fatsii
kaynozoyskikh molass Severnoy Fergany)
PERIODICAL: Tr. In-ta geol. AN MrgSSR, 1956, Xr- 8, pp 57-77
ABSTRACT: The outline of the subdivisions of the molasse in Fer-
gana is based on periodic alternating phases-of sedi-
mentary integration and differentiation, changing from
one to the other in definite sequences. The Cenozoim,
molasse of northern Fergana belongs to the genetic facies
type of the piedmont-fan zone and is subdivided by the
author into a number of smaller facies which are com-
bined into zones. 1) The fan-elastic (fanglomerate)
zone is charactarized by various conflomeratic facies;
pebble-cobble breccia is most abundant, followed by
sandy granule conglomerate and by boulder conglomerate.
alard 1/4 The facies of this zone are divided into 1) the torren-

...The Cenozoic Molasse Facies of Northern Fergana
Card
15-1957-10-13963
lit.-
tial 'boulder facies, consisting of irregularly and poorly round-
ed boulders 25 to 85 am across; 2) the torrential pebble-cobble
facies, occurring in thick layers or lenses (from several meters
to several tens of meters), consisting of pebbles 3 to 4 am
across or, less commonly, of cobbles 8 to 9 am across, and gene-
tically subdivided into dry-vpLlley, stream, carbonatized, resi-
dual, and mud-ball varieties;'and '3) the torrential granule fa-
cies (similar.to that described above), occurring in thin lenses
and distinguished by smaller fragments, and containing dry-
valley-carbonatized, dry-valley-manganiferousp and stream-car-
bonatized varieties. 2) The fan-loess (fan-siltstone) zone is
very extensive in northern Fergana and consists of fine-elastic,
varigrained sand-silt rocks, They are subdivided into a) the
channel facies, characterized by coarse, irregularly uorted de-
posits; b) the flood-plain faciesp distinguished fx~jm the chan-
nel faoies by better sorting and finer grain size; c) the loans
facies ' veri abundant among the molasse sediments, which forms
thick beds several tens of meters) and is very persistent along
the strike; and d) the shoe-string facies, represented by mixed
2/4

15-1957-10-13963
The Cenozoic Molasse Facies of Northern Fergana r-%*
rocks and by masses of fine7grained material with individual
rains of sand (or even granules). 3) The fan--stagnant-water
playa) zone occurs in the peripheral parts of the piedmont
T
plains, in dammed-up and swampy lowlands; it consists of silty
muds and exhibits well-defined and thin horizontal bedding.
Genetically and lithically it my be subdivided into a) the
ornamented facies, formed of buried soils with fine networks of
plant root impressions, carbonate 'Oeocoons," and similar fea-
tures; b) the meadow facies, distinguished by spotted, ethereal,
reddish-ochre colors and bluish-gray, irregularly scattered
spots, and by great variety in elastic content in different
regions; c) the playa (periodic stagnant-water) facies, charac-
terized by very thin and distinct horizontal bedding and by
fine-grained oomponents;,d) the lacustrine-paludal faciesp
formed in the lowland parts of the piedmont plain in water-
filled basins containing plants, and consisting of silty car-
bonate lutites with abundant plant remains; a) the epigenetic
carbonatized zone--very dense marls of cryptocrystalline cal-
cilutitas; and the fan-eolian facies, characterized by very
Card 3/4 -

I
15-1957-10-13963
. The Cenozoic Molasse FacieB of Northern Fergana .. ~- &-
uniform, predominantly sandy composition and by croijs-badding,
Data are cited on the mechanical composition and tilt) mineralogy
of all the facies enumerated above, and the conditions under
which the rocks were deposited are discussed.
, ',lard 4/4 V. G. Rikhter

VMTUNOV, LON.; KARACHKOVSKAYA, A.N.
Barite and celent4nA from the cont1hental sedIzents of ths
Chu Depression (Kirghisistan). Zap. Kir. otd. Va#s. min. ob-va,
no-3tlO5-107 162. (VJ.RA 17:11)

15-1957-3-3081
Translation from: Referativnyy zhurnalp Geologiya, 1957, Nr 3#
p 93 (USSR)
AUTHOR: Ver tun MJti.N
TITLE: Analcime in the Cenozoic Molasse of Northern Fergana
(Analltsim v kaynozoyskikh molassakh Severnoy
Pergany)
ISRIODICAL: Zap. Uzbekist. otd. Vsese mineralog. o-vap 1956,
Nr *_ 91 pp 61-62
1,WTRACT: 'Authigenic analcime has been identified in the cement
of dark bluish-gray varigrained channel sandstones
which occur in the upper parts of the Sumsar
and Marguzar sections. It forms colorless,
tabular, pseudocubical grains, ranging from 0.04
to 0.2 mm on the longest edge; it is isotropic and
~J'ard 1/2 water clear. %ie.~mixieral-.Js associated with carbonates.

Aralcime in the Cenozoic Molasse of Northern Fergana
The author suggests that the analcime may have formed by
chemical decomposition of volcanic rocks in an alkaline
environment and a warm climate.
Y4.S.K.
Curd 2/2

VIRTUNOV, L.N.; SOTIRIADI, X.A..
Brief description of mineralogical and petrological characteristics
of upper Cretaceous and Paleogene deposits in Kassan-Tau. Trudy
SAGU no.63:31-38 '55. MU 9:5)
(Nassau-Tau--Geology, Stratigraphic) (lassan-Tau--Mineralogy)

TSEKHMEtSTRYUK, A.K.; KOIESKIKOV, Ya.I.; VERTUNOV, L.H.
Thermal waters in the Iseyk-Kull basin. Priroda 52 no.6:115
,63. (MM 16s6)
1. Prunzenskiy politekhnichookiy, institut.
(No subject headings)

ACC NR, AF6021477 SOURCE CODE: UR/04l3/66/ooo,1oll/olo3/ofo4-
1:
INVENTOR; Autsgraf, F. Zh.; Vertushkin. B. A. Golovin, V. V.. Kon kcn,, Yu. A.
Fedoseyev, R. Yu.
OAG: None
TITLE: A pneumatic relay. Class 42, No. 182416
SOURCE: Izobreteniya, promyshlennyye obraztey, tovarnyye znakio no. 3-1, 1966,-
103-io4
TOPIC: TAGS. pneumtic device, nonelectric signal e(ruipment
-ABStla'OT: This Author's Certificate introduces a pneumatic relay which containsa
hous,.ng made in the form of disc plate*s with channels,-a diaphragm unit which forms
a nLu iber of chambers , and nozzles mounted in the flow chambers. Short 'circuiti,ig
cond%tions are prevented by making the face plates on the rigid center of the dia-
phra4;m unit from an elastic.material, e. g. rubber, and putting a greater distance
betwiten the pXanes of these face plates than between the edges of the nozzles.
LC04-- 1/2- uDc; 681.142-525

I ACC NR AP60214TT'.
j Z
4
1,.rdisc platesS 2.,chwmela$
3~tace plates; 4-rigid can-
mteri 5--diaphraga unit; 6-,
nozzles
so ccDE: 13/ sum DATs: olmar65
C6rd /2

VERTUSHKINP V. K. (Moskva)
'w
Ipproximation of th9rwonamic f=ctions of air, Insh. Sbur.
2 no.4:343-344 162. (MIRA, 16:1)
(Air-Thermal properties)

44677
5/258/62/002/004/016/019
E032/E314
rrHOR; VeirtushkiTli V.K. (Moscow)
A
l.
'TLE: ynamic functions for air
T:1. Approximate thermod
P:;MIODICAL: Inz~enernyy zhurnal, ve 2, no. 4, 1962, 343 344
-'~Xv: Existifig approximate expressions for enthalpy, asa
T
function of pressure and temperature cover the temperature range-
.0K* it is now reported that in the temperature range
500 - 16 ood
17S 000 -20 000 OK and pressure-range 0.04 -,10 atm., the
enthalpy is approximately given by
2
h(e, P) a In bP-'-(l*- In P) (2)
4 165
wAere a 2.84 x lo b = 3,o65 X c =.0.09 and d =.O..064
(P is in atm;,,~ is in g/cm and h is ingeal/g). The
relative Orro in most cases less than + 3%V as compared with
tabulated values. The above expression for'the enthalpy may be
used to integrate the equations for the steady-state flow of
al non-viscous gas without bringing In the equations of state.
a re
There is I table.
S UBMITX ED IMay 7, 1962
Card 1/1,

__ACC_NR; --AP6007748--- SOURCE CODE: UR7o2g-37~6-iffo-~4-Fo(Ti-!6f6i-/6-i
AUMOR: Vertushkin, K.
OR;: none
TIME., Supersonic air flow past a sphere with equilibrium radiation taken into
account
.SCURCE: Kosmicheakiye isaledovaniva, v. 4, no. 1, 1966, 162-164
TITIC TAGS: aerodynamics, hypersonic flow, radiative heattransfer, thermal radia-
t'.0n, shock wave, entropy layer, enthalpy, thermodynamic equilibrium, boundary layer
KISTRACT: Radiation effect on distribution of gas dynamic parameters behind a shock
wive in an equilibrium air flow at escape velocity Is investigated. The radiation
A)sorption is neglected. A system of equations Is derived describing the flow of a
~'rfect radiating gas past a sphere in a spatial coordinate nystem, with the energy
P
'. ___---ZAW
_coni -ng::-a -"dit-iDual-torm-expressing-r4dtation!, An effect ve factor x
sie-ed-t- __ internal-en
Ailich is the ratio ti-e-6 he -rea e-rg_y___1_s-rn_t_r~gc~d:_-
W o_ _~a
Amcount for the real gas eiffect, while the equation of state is of the form---
there P is the pressure. The system was solved by a previomily developed method
('~tvestiya AN SSSRMekhanika I Kashinostroyeniye, no. 4, 1964, 60) which consists in
L C Lrd 1/2 UDC: 533.601.155

AC C NM AP6007748
ti acing n rays in the region considered and approximating the intermedinte values
01 the unknown functions with respect to the values of functions on rays. This makes,
il possible to express the variable with respect to 0 (angle between a ray and axis
0:! symmetry) through the values of functions on rays, thus reducing the initial sys-
ti -m to asystem of ordinary differential equations which may be integrated along the
r; iys. The -solution consists in selecting such ctand-of f distances on the raysat'.Wch the
b)undary condition u -:* 0 is satisfied on the body surface. The results from computa-
tLons of the flow past a sphere of 100-cm. radius at a speed of 11.4 kn/sec and atan
aLtitude of 60 km are presented in graphs. Iliey show that the effective value of
i - 1.13 accounts well for real equilibrium properties of air, and that the boundary
condition u - 0 is satisfied with accuracy of not less than 0.1%. Th(~ effects of
zadiation show up most strongly upon the distribution of density ane enthalpy and
substantially less on the velocity distribution and flow pattern. The additional
.(ooling of air due to radiation leads to an abxupt reduction of enthalpy and to an
Increase of density near the body surface# which is evidence of the presence of a
A- on-the-bGundary-layer-an!4---b4a~t~--,-__
Lrans fer". processes# - ----The - author- ~thanksi-_Academiciaa G.- 1. Petrov.-for remc
1 rere taken into -account by the author in -revising the article. -orig.- -art. -has: -
_ji figures and 1 formula. [AB]
71
IUB-COM-20P SUBM-DATF.:-- 153an65/ ORIC RM 003/ OTH PT OGI/ ATD PRESS.
ird 212 not

4
it is I S. n 16 11 4 "pall dill
7 1 AA 46
A

botryogioci from Kirnwatt
-
- -00

I'll. tittle W114crol, to.
N.C. - w. R
,:ii J HT'li,
f

xeferst. Zkur. 1939. No
- M. 21.- IkAly,well (A I.A.ic 'Ill. -00

(Ate Of AIC and Pel(lil WAS (U111111 ill V, -;- -"- " - ""' "'it 1 '1'. .9*
Study of the mineivill, after all undefliwittsol titl- in Ill.

es 8
~, ,% KI 4.1 'it I Coo, I,1.11
Kajac sloatc Id the pyrite too Kk
tewumAirst. -00

0: and suppons lot the AiAlt as a tk"Ip. d appfux- 40'.
,
1L) F
46
C
O 0
59
i
d F
o 2
M
Ah lif
b -00
~
.
r
.nta
r
u
.
m
.
,
,
9
4
24. Sh 3X.7d, HP 31.15. Ve acid Cu replace
AhOs 0,
j i, Algiftittlorpbli-ally. Tbe a lorsph

" 44 A 1111111, 4fid UWAY hAVV the fiAlfill (1101 Knit (41111)
'J livid (12%1) and (010); bardtiew 2.11, d. U'Af. coo
color yrilowish red, %trungly plembruk; the plaux tot the
1
doplina ax" Wait .
0101 ant) or, C. W. R. Heart

'aoe
.0 0
Lei zoo
IT see
-r-
zoo
-v 0
40

1
I0
1
M L
4 1 to I k 6 .1 6CA
P
4
LAt CLAI
1AMk&K&L 1,41(1
4 , I 1 4-
-
'
.
L" to t I
.
t a a It a PC a tt it (q . 111
VIAIAI %arm o 4
W13 1% 1 It 41
to
Coo a
'
0 111 0
0 It OR s
I
0 0 0 0 0 0 6 0 0
0 0 0 0
0 0 0 0 Ob 9 0 40 4e

AN"Y"M fill U23 UM bSV "'Miled"i III 'i
IN
A6 I L
')g pqst.
44-M.-PiA.A. I I
MVkI qtIOMMI115. W lk 00, 411 ti-Witi "in" art ek-mvit."I
Aimmi;
the prraufts of comhudim see 4 AM 0 PRIUMV, pytthsothr.
tworislitc. mcriedir, nl""Ifir, frorow1u..'Mi1r. "Wkniefite.
Pkanite, 1kirovilir, ruptisLiaotifir, chak-embitc. porked" -
III, 111TOPIA01 It, shmArliff. twify. is; thrw Isell
twill vary 111111 "Ith I - IcIllp of r4mll.
0.
.00
-0
use
see
8,2.14
146'~D" i. ;;~' -4.4
oe
411pip oil wa *a $111114:11 1114111101 is
9 gig 0 0 o a a o * 0 0 lie 0 111 9 0

~J*144140*96000900041
00 pl"
004 -4041
Nook S. S. S. R.-SK WF4fMlY`PWtH*Pr eft cuts
00A in d"w - Aspva"n; It b" ti. Vk!th
00C warAw extUdia of 8D to NO, sod tolo of
rm b"Ied avel " opm dow evulv" Its wata of crymn.
OW to U, fimay forwing a bud. twktk Wcakly 00
: ""411WOO "Od"Ic- it -*l-AWQVft I" It-0- ShOwbW "Id J-60
PIN,
-is au"" RO to CMSW $A: 10100
tigm. rwthd IWAY
it
WM-Z 3.45%. Pet) IXI% wId Cut) 0.91%.
a nbrw whb 1679. p"wI k$ AMAW
aft*ud. I t b " I=. - .00
WAWWR46le "W of six *kcl-
004 10 111, 1 'eka wm drod ex, F#O I ASO' :00
004 " ok 00
W 070
01.,,.74 7SAM the M1145P
400
004 AlLlsmh If 0. U. K001.44pol
00
COO
soe
00
iboo
to 00
Item livisla.Q ".60
0; b u a 1, -0 ALI MR A s 0 ho 0 10 4
0 0 0 0 0 0 0 Al 0 0 0 0 0-0 0-0 0 :_0_04 0- 0 0 0 0 0 6 0 0 0 a

A07. V11,14 Q17ARTZ FRf)U VEINS OF till( EASI-IiIIN ol, I'llft
V"At-14-G. N. V mrodw jIA4A*jfr) Aa. .'14 0. tt R S, S if
ar co 8~m m r go
I No f i"-0 g.w V 4 u r wo. im
bocurd"Ifl 14 oukro-InXt". and P111tir 11Y tht ArADMIAtkOn 44 fh* IWIUWY Iloarto.
y j.po"awd on a w~wmlary mictmip"m
I* t1wes pW* om voim quads is usualI
Ag - to W WWrA with cmplk&W intsm"Now. OA sulphidos, am of later
Iffmilatkm tuo mr, quarto. *N,.* pnmerv*l c
tzq=kmad In veins whkh bave
omwrww 111110 "WIS"U"141(wds call 1.0 "Oftl as I ro- moterial

Rk 15T
VzIaUSHKOV2 G.
um/Quartz Ajr 1947
Mineral deposits
"Foliated Quartz from the EhrustalIkAja GOra in the
Urals," 0. N. Vartusbkovp 8 PP
"Zap Vee Min Ob" Val LXXV, No 4
Deposit of quartz near Sverdlovsk In the Ural
Mountains. Study of the vitreous, transparent quartt
from this region.

3587D Pirofinit s pripolyarnop urala.-V ogl: M. A. Vertuskjov. Zapiski
. i urallskogo geol. o-rva vyp. 2, 1948, a. 31-32
SO: Letopial Zhurnallmykh Statey, No. 1+9, 1949

VZRqUSii;=' G. n.
Vertishkov, G. N. "Deposits of the alpine type in the Central Urals," Tz-Lidy Corno-geol.
In-ti (Akad. nauk SSSRP Uralls!dy filial), Issue 14, 1?48, P. 3';-48 - Bibl.ioC: 20 items
SO: U-3850, 16 June 53, (Latopis tZhurnal Statey, No. 5, 15,49).

G. N.
Vertu.3hkov, G. 11. "Broc,ldtc from ?Icyvc--iudyanII'f Trud.y"orno-,,:ed. ~-n-tn (Alkad.
SSR, Irallsk-17 filial), issue 1114, p. - 31;-~jjoC,; 5' Itain
SO: V-3850, 16 Jwic 53, (Letopis 'Zhurnal tr~vlt StateY, No. 5, 1949).

VL.-l,3lj3,il`.Ov, G. N'.
. VerttjSI,kOV, I
G. 17. "Shec-lite crystals from the Kelrovs'*iy de,,xs-'Lt," Trudy Gorno-rcol.
in-4a (Akad. nauk SSSR, Uralskly f1lial), Is.~tic 14, 1948, p. (14-68 - albliog: 6 itellis
SO: U-3850, 16 June 53, (I--topis 'Zhurn,-l In-ikh StaLcy, 140. 5, 194-9)

VEEETUSM)V ~ G. N.

2) J. Is A
AA
M
Ratilf hom the Subbolf Swoonsak Croak "&r KyAlyin,
a 11 6 1
Ursk. G. N. "'Pb*QN. Z ki Viineyms. Misrr4.'
f*'AWA45hW 0011i ;W'SirlsC M n&AI.) 78. %0, 1, 19-2A
f 1901). - In the r4W%MfACl &4W 44 the EMilt UMW"V Of
Yffiliffe-114kok, qwrtt vvim ;irt Imnd whk% bem
UtIUSitAlly 14tgr fUtilC "Y%(AtS. IUMMM 44 6 ke. Weight 4
and im-ce are f4pund ev"yolwv in the alluvial sedhimats
tO tlw NAN4 11hirmult Cmek. The reins Ima In the
he"Mitr, 1*41110tht, flAor. 104400. MMU11vilf.,
ne, and apailte, but only ruille. mictdoilhe, and tpd-
1
1:10CM lAfP iUdJV41UAIS. OMIS. MIIJ417141 CJ fV0101 see
TiChV5.W,S^O.fi4. AIAO 431"
0! Mot) trace. The ~k- history o( them ratile ;;=' formed on the sutfoce of the mule to it ahwull"lius-
0, is very rewrkAW: fimt cavities were opened In the 9 phase wbkb fanned IcklaW and blothe. Is a 16111o"
Fr4 ite at the neightxxing garnel-bornblende rocks. an Ptage all them minerals wem earloard In quads wkkb
a ~ can plody filled the cavities. The prinsary ratile ay"%
.1. W2116 Of Whkh the MtilC CrWAIS Pew 10 0 length 0( !zoo
Af rni. and a thickness t4 S 8 cin. Latri Ypheat was cmWwd admixts. of Cr. Al, and Fe in their Wtim. but .
11 so
them solid KAm. Vew unstable. TbeirambWa1bgm-' I
lice, 11mmile. and owne Cr spinel btanSht abold a class. x0:
Oj J41 Settristic mWas Intefgrowtit stnwtum In which tU tAu-
V L%r Inclusions am oriented parallel to the (am c4 the acute
byprramida Pull or 15011. hyd -ocactaneorpW -.90
stim" Sulne"PO cracks win fornied aloas wwtk we so
adnerals oft deposited. Probably this sulatrall"tion
took Puce A-ulu"Musly with an SMA'Autbon and
depoikica. IACW dW Whole Cocapica of the Vdft
went strong dymm"etanionew Mena am Wao.- 41;
a
tim. the quarts was gmnulattd, and the nmil 1--.0o
ShOW thMbY POIYSYUthetiC tWift StetKAWKS, And
beta shapes.
W.
46
.-j' all
*4
MA I a a
1.4
ff .1 of rt
0 0 0 0 0 0
0 0 00 00 0 ooo O.oo'o 0-ofo e 06 00000000*6096

VE.RUSHKOVIV G. N.
USSR (600)
Sverdlovsk
AmIeny of Sciences Geologists Sgpf 50
wNeri problem of Genetic Mineralog3rt" Prof D.P. Grigorlyevs Priroda, No 9 PP 22-30
Mentions the following persons as contribpting greatly to the development of the
sciance on the USSR: G. G. Lemmleyn, Leningradp Moscow; I. I.
Shafranovskly, Leningrad; G. N- Vertushkovt

mausla0y, N.
Kustanay Province Ana~aita
Yesselite from the Kustanay Pro7ince. Zap. VL-.--!:a. ran. ob. 81, NO. 3, 19-52.
Monthly Ltst of Russian Accesslons, Lillbrarl; of
Congress, December 1952. Uncluusif'ied

VIR2USWL'OV, G. N.
Anapait.--Kustanay Province
. Messelite from the Kustanay Province. Zap. VsFs. nin. ob. 81 no. 4, 1952
.lonthjX List of Russian Accessions, Library of
Congtas, December 1952. Unclassified

J,
Ghowleal Abst-
Vol. 48 go. 4
rob. 259 1954
_qpl GhemlotrY
HirAnlogical ILM GeojoLi
Quarts (rom the K*ChjWA region, brials.
V- V- XPIrkq&x il&r fqctk-tXUd1o_Y_sVT_
;MRV.Vy"_W~48. Mi"raralt. CPAWkSM: ?M&i. sm. russe
min4nd.)V. 217-IO(IgM.--Quxd.tcrystabjocaay-!d
"Yesumets-ch6els." of pemlkw cloaracteristics, occur in
Alpfne-type Au-quart;,. veins. Owing to pressure effects, fbe
cryitals are cracked in regular o6tutation parallel to the!
c-axis, with systems of pseudocleavages aced. X under anglq
of W)* and 12D*. The crystals therefore often apWar to be
subdivided to tritonal-PrIstualle fortas of columnar type.
"Chisel" quartz crystals we always water-deer, white the
cry"3 am abundantly inter-
Sww" with andAturile, nalimanite, rutile, and chlorite. On
tht cmcks, ustudly fine films of FeAh hydrates, or a clay
desiosited. Pscudorkavages of quartz tmrAllel
v described In 18r, by Vernad*A; further, but
distinct pseudadeavap has lwo observed with wpn.
faces vertical to 100011, and a third pseudodea is
40* to the c-axi Vz
oriented under 5, tch a
to &MY in (1011).
Mon. (am In the 0:: '(00*01)"IMO)v PMWM
This Utre Is abumlantly covered (sy fitclusions. The same
crack.4 have been observed its chilled quartz crystals after
heating. the cracks In (00ol) and (1610) an known only,
under tweptional conditions of one-sided p'"Wre at
temps. < 200*. W. Hiiet

VInWHKOV, G.N.
00 , -?"- ~,
n FPO ow-*, " - ,-
Stalactites of quartx in a limoults goods from the central Urals.
Z&p.Vses.min.ob-va 83 no.3.-249-251 154. (MIJU 7:11)
1. Sverdlovskiy gorrqy,institut Im. Y.V.Vkbrusboya, Kafed:ra miners.-
logii i kristallogrefii.
(Ural Mountains-Limoutte) (Geodes)

VIRMHKOV. G.N.;, SVUUIE, N.V.
Uply to I.Y.Lobanov's book wIden tifloation of mineral& by their
solubility In vater and acide.0 Zep.V9es.mIn.ob-va 83 no.3.287-
289 '54. (KM 7:11)
(Mineralogy, Determinative) (Lobanov, I.P.)

VARV, IMq. -a-Ii. -
Norphology of drusy cristals of quartz and feldspar fros a
pegmatite vein of the Adui depocits in the Urals* Zap.Tses.
minoob-va 83 no.4:319-327 154. (XLRA W)
lo ll&fedra mineralogii Sverdlovskogo gornogo instituta im.T.V.
Vakhrusheva.
(Adui region-FeldePar) (Adul region~--Quarts)

VIRTUBHXq,.- ~
o
W
n ~ 5~
Minerals from tamoth tusk's. Xln.sbor.no.9:309-312 155.(NM 9:9)
1.3verdlovek, Gorr4y institut imeni VA.VaMrushava.
(Tusks, Fossil) (Mineralogy)

v c~
VXVUSUOW.G.N.; ORIGMIYWOD.P.
Konstantin Xonstantinovich Katvaev; 1875-1954. Zup.Tses.min.o'.')-va
84 no.2:251-252 155. (MMA 8: 10)
(Hatveov, Ironstantin Xonstantinovich, 1875-1954)

v i~- J? r L (S /L/ k 0 u 6 1 N .
AVDONIN,,T.N.; VXRTUSHXDV. G.N.
I Amethysts from the Beraxovsk gold ore deposit in the Urals.
Trudy Byartgor.inste no,26:93-94 156. (XIM IOS3)
(Berazovsk region--Amethysts)

VnTUSHKOV G.19
Limonits goods from the Bakal iron ore deposits* TrUdjr STeragore
insto no*26;94-98 156, (KLU 10:3)
(Bakal-Idmonites) (Geodes)

Ilmenite-magnatite ores form dolomite Teins in the Urals. Trudy
Sver6gorsinsto no.26:98-104 136. (KM 100)
(Ural Hountgins-Kagnetite) (Ural Mountains-Ilvenits)

TMTUSHWT' O.N.
Aleksandr Vasillavich Kalugin, Ine of the first collectors of
minerals, in the Urals. ZapJaes.min.ob-m 85 no.1:95-99 156.
MRA 9:7)
1.1afedra mineralogil Sverdlevokogo gornogo instituta imaxi
V.V.Vakhrushava.
(baugis, Alskeandr Vasil-evich, 1857-1909)

T-
l
"

l
,
A
M

USSR/Cosmochemlstry - Geochemistry. Hydroc stry, D
Abst Journal: Referat Zhur - Khlmiya, No 19, 1956, 61300
Authori Vertusbkov, G. W., Tarosh, Fe Ta.
Institution: None
-the Urals
Title: Black Chrysotile-Asbestos from the B&zhtMrvsk Deposit
Original
Periodical: Dokl. AN 1956, lo6, No 5, 907-910
Abstract: Chemical composition of black asbestcs (in, %): Mgo 41.98, CaO%12,
MnO 0.08, FeO 0.39, Fe2O-A 1.07,, A1203 0.28., Si0,_, 41.22. On tr
c-
ment of this asbestos with var'-(Pls oxidizing aglEmts (H202, BN03 etc)
changes in the black colorati-on occurred -with different transitions
from black to vhite. E:Lack color of the describedoisbestoo can be
attributed to Fe(2+).

vXRTUBMW, GoN.; ODONIN, V.N.
Metamomatic ahanp of morpentiMtex into OxIcaites, (211adity)
surrowding a quartz vain In Wount Xbrastalluaya In the Urals,
Zap. Voss. nin. ob-va 86 no.1:65-71 #57. (NMA 10:4)
1. Kafedra m1noralogit Sverdlovskogo fornogo instituta.
(Ural Mountains-Serpentinites)

VE~TUSHKOV, G.N.
Rhythmic phenomena in a coarsely dispersed medium during the
formation of limonite, geodes in the Billabey crystalline
limestone deposit. Izv. An SSSR. Ser. geol.. 24 no,6:108-
112 Js 160. (KM& 14:4)
1. Sverdlovskiy gornyy institut.
(Bilimbay region-Geodati)

QIERTUSPI.Py I P. ~!.
Dendrite crystals of microdine iL micrographic intergrowth vith
quartz from the Rezh region in the Urals. Tru-4.y Gor.-geol.
inst. UR~11 SSSR no. 42:99-106 159, ('11IRA, 14:2)
(Ural Mountains-Ricrocline crystals)

-VZRTUSHKOV a N
Morphological types of phenocrysts of acid plagLoolase fron the
Sverdlovsk plagioclase-blotits porphyry. Trady Gor.-geol. inst.
UFAN SSSR no. 35:201-207 160. (KIRA 14:1)
(Swerdlovsk-Phenoorysts) (Flactoolame)

C, VjRTU , G. N.
-~;a~rgini a from the Rizavetinskly iron ore, deposit In the Uralia
Zap. Vaes. min. ob-va 89 no-5:570-572 160. (UM 13: 10) 1

-.0-0
Granitization of ferruginous quartzites in tho eastern contact
zone of the Ufaley granite massif In the Uralis. Izv. v7s. ucheb.
zav.; geol. I razv. 1 no.12:80-94 D 158. (MIRA 12:12)
1.5vardlovskly gorW institut. -
(Ural Mountains--Quartzites)

15-57-5-6512
Translation from: Referativny zhurnal, Geologiya, 1957, Nr 5,
P 114 (USSRT
AUTHOR: Vertushkov, G. N.
TrrLE: Ilmenite-Magnetite Ores from Dolomite Veins in the
Urals (Illmenito-magnetitovyye rudy iz dolomitovoy
zhily na Urale)
PERIODICAL: Tr. Sverdl. gorn. in-ta, 1956, Nr 26t PP 98-104
ABSTRACT: The Sugomak deposit, at present having only minera-
logical value, is situated in the Kyshtym district
of the Chelyabinsk region, on the southern continu-
ation of Sugomak Mountain. The district in which the
deposit occurs is composed of massive antigorite
serpentinites, grayish-green in color, and containing
dust-like inclusions of magnetite. The serpentinites
contain veins of dolomite up to two meters thick. The
veins have sharp contacts with the serpentinites,
Card 113

Ilmenite-1-14agnetite Ores (Cont.)
15-5?-5-6512
which, at these places, are strongly sheared. The schistosity,
arallel to the selvage of the vein, dies out away from the vein.
8
re minerals form bands and accumulations of irregular form in the
dolomite in the body of the veins. The ore minerals represent 20
to 30 percent of the total volume of the vein. The ore minerals
are represented by a granular aggregate of ilmenite and magnetite
filling fractures and cavities in the dolomite, cementing dolomite
fragments, and partly replacing the dolomite. Those relations
indicate that the ore minerals are younger than the dolomite. The
ore is predominantly magnetite. The Ti02 content is 25-42 percent.
Grains of ore rarely show crystal form and are everywhere allo-
triomorphic in relation to each other. The size of the grains ranges
from 0.01 mm to 0.03 mm across. Grains of ilmenite and magnetite
both show intergrowths of hematite, the result of decomposition from
solid solution. The absence of any indications of transection and
replacement of one ore mineral by another, and also the equal degree
of idiomorphism, lead one to conclude that the ilmenite and
Card 2/3

Ilmenite-Magnetite Ores (Cont.)
15-57-5-6512
magnetite formed simultaneously. Apatite is present in considerable
quantities in the ilmenite-magnetite aggregate, The veins originated
where fractures formed in the serpentinites because of tectonic
movements. These fractures were the sites of formation of the dolo-
mite! veins. The vein mineral was deposited from hydrothermal
solutions containing C02 and combinations of Cl and P at high
temperatures. After the movements in the veins, the ilmenite-
aggregate was deposited in cavities and by metasomatic
replacement of the dolomite. The Sugomak deposit is genetically
most closely related to veins of the alpine type in metamorphosed
basic rocks. During metamorphism of these basic rocks, Ti does not
enter the lattices of silicates but is concentrated in independent
minorals. In the described occurrence, the elements of the Sugomak
hyperbasite mass that did not enter into the composition of minerals
in the serpentinite accumulated in structural fracturas in combi-
nat-fon with H2*; and CO 2'
Card A. B. B.

TIMUSEMOV, 0.1-
Ketaworphism of tho Nusa-type iron-titanium deposits. lauch.
dokl. vyv. shkol3r; gool.-geog. nauki noo3:139-143 158. (MIRA 12:1)
1.STerdlovskiy gorWy institut, kafedrs, kristallografil i wineralegii.
(lusa region--Ore, deposits) kPatrology)

VIRTUSHKOV, G.N.
bffect of gravity on the natural growth and dissolving of crystals
Zap. Veen. min, ob-va 87 no,4-.469-473 138. MIn 12~.- 1;
1*Kafedra mineralogii 8v*rdlov~k*So gornoge Instituta.
kCrystals-Growth)

'rJ=SHKOV, G,N,; SOKCLove Tu~jL,
PIU21101blonite md pyromorphite from D~per Ufaley in the Uralg,
71~p. Vsea. =in. OD-Va 87 no.1:96-100 kXM Ilt6)
10 Kafel:~= MinGralogli BrardlovalcogO gornogo inatituta.
(Ufal8Y Rmge-Lead ores)

PLAITOVSKIlt A.N.; Y!~RTU
Division of the total co~fficieut of mass transformer into
partial coefficients. Khim.prom. no.9%700-703 8 f63. (MIU 16:12)

PYANOVSKIY, A.N.; BUIATOV, S.N.; VBRTUZAIZV, Ye.D.
Design of sieve-plate column extrUctorso Xhimprco no.5.-364-3&7
My 1629 (Extraction apparatus) WRA 15:7)