SCIENTIFIC ABSTRACT VISTELYUS, A.B. - VISYASHCHEV, V.S.

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• Collection: Scientific Abstracts
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• Release Decision: RIF
• Original Classification: S
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• Document Creation Date: November 2, 2016
• Document Release Date: September 1, 2001
• Sequence Number: 14
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

Fctrclogy
Disrersion of probabilit4es; answer to V.S. Drutriyevskiy., Izv. AN SSSR. Se:-. ceol.,
no. 1, 1952.
1952
9. Monthly List of Russian Accessionsf Library of Congress, May xt953. Unclassified.

VISTILTUS, A. B., BARSADSKIXH, N. N.
Sanatcri=3
Nature of chame in the minerulcjc-,!:. ccr,%~c-
- I-
0 .. I Ill'-,
sition of durin,, hin. c.1
sands. Zar. Vse5. mir 81, Nc- 2, IL952
Monthl List of Russian AccessLaaE. Library
of Con-:,,Tess, September 1952. Lr'CLASlj7Ei--T

VISTEILTUS., A.B.
Azerbaijan - Mineralogy
Mineralogy of aand-ailt deposits of the Miocene period in southern Azerbaijan. Dokl.
AN swR 8-5 No. 5. 1952.
Monthly List of Russian Accessions Library of Congress, December 1952. UNCLASSIFIED.

US
129.
11, vi'tf- b I(M. P. 271-M
r(r. it "
sclimidB
Ame 1954 curreas and su VIL I 'cisc 'Ild ~ 011,L)IC jums1% v
C.(;Oloe.,,y and Mineralogy
dia raill t,

1. V1 S. A. B.; WKLUKHO-MAKLAY, A. D.; RYABININ, V. N.
2. USSR (600)
4. Umatone-Tuarkyr
7. Devonian limestones from the red-colored strata of Tuarkyr, Dokl. AN SSSR
90 No. 2, 1953. (r" '31-230
T_ab Sni
t*'o'so !1- ~.O-~r7 fo ......i n o Ljj r) f~ -,71 e,-;.
In -i1-_jj TZI
of' tli'_ir
9. Monthly List of Russian Accessions, Library of Congress, April, 1953. Uncl.

------- VIY7~t74./ L) S , A, ;i'
VISTELIUS. ". doktor geologo-mineralogichookikh naukj SARKANOV. 0.T.
yrureavor, doktor matematichaskikh nauk.
Some remarks on professor P.A.Ryzhovls article 'On evaluating
the precision of mineral deposit estimates.* Trudy VKMI no.29t
200-201 154, OaRk 8:3)
(Mines ard mineral resources-Statistics)

VISTSLIUS, A.B.; YAROSLAVSKAYA. N.M.
Basic color characteristics of torrigenous Cretaceous gand
and silt deposits found In the Transcaspian region. Doki.AN
SSSR 95 no.2067-370 Mr 154. WaA 7:3)
1. Laboratoriya asrometodov Akademii nauk SSSR, 14ningmd.
(Caspian Boa region--Petrology) (Petrology--Caspian Sea region)

USSRI Geology Minerals
Card 2 1/1
Authors Vistelius., A. B.
Title Mineral associations and characteristic parageneses of the APT-Senoman
terrigeneous stratum of the Caspian Sea region
Periodical Dokl. AN SSSR) 97, Ed. 3, 503 - 5o6, July 21, 1954
Abstract t The characteristics of mineral associations of sands and silts of the
Apta, Alba and Senoman eras of the Caspian Sea region, are described.
The positions of the basic regions for these periods, are explained.
Twelve USSR references. Table, drawing.
Institution Acad. of Sc. USSR, Laboratory of Acromethods, Leningrad
Presented by i Academician, D. V. Nalivkin, April 5, 1954

V/ S 7- L-
U=/ Geology
Card, 1/1 Pub. 22 32/4-6
Authore I Visteliusp A. B.
Title I The Kirmakinsk formation of eastern Azerbaydzhan
Periedical t Dok. AN SSSR 103/1, 2-17-120,, Jul 1, 1955
Abstract I Scientific data are presented regarding the mineral. associatio;is found
in the Kirmakinsk strata of eastern Azerbaydzhan. Eight refer-ancee:
7 USSR and 1 Eng., (1933-1954). Tables; graph; diagram.
Institution : Acad. of Sc., USSIR, Laboratory of Aerormethods, Leningrad
Presented by : Academician D. V. NalivKin, February 14, 1955

VISTILIUS, A.B., IOROBIOV, I.A., ROKLNOVA, N.A., OMNOVICH. Y.Y.
On the age of the lover layers of red beds oa the Cheleken pen-
insula. Dokl. AN SM 105 no.4:786-789 D 155. (XLRA 9:3)
1. Laboratortys aerometoday Akademil nauk 6M. Predstayleno
akadealkom D.V. Saliftinym.
(Chelsken-Geology, Stratigraphic)

VISMIUS, A.B.; KIKWIHO-KiLlIAT, A.D.
The middle series of the productive stratum of the Apsheron Peninsula
and the problem of its genesis. Izv.AN SM.Ser.geol. 21 no.4:
77-94 AP '56. (NLVA 9:8)
1. Laboratoriya aerowtodov Al SM. Leningrad.
(Apsheron Pezinsula-Goology, Stratigraphic)

VISTILIUS, A,B,
Problems in the study of bonds in mineralogy and petrolog7.
Zap.Vaes.min.ob-va 85 no-1:58-74 '56. (MI-RA 9:7)
l.Laboratoriya serometedOT AN SSSR, Leningrad.
(Nizeralogycal ohemistry) (Petrology) (Chemical bonds)

VISTELIUS, A.B.
Mineral composition as an aid in establishing regional divisioas
of the recent deposits of eastern Caucasus and the northern
Caspian Be& region. DokI.AN SSSR Ill no.5:1068-1071 D '56.
(MMA 10:2)
1. Laboratoriya aerometodov Akademii nauk SSSR. Prodstavleno
akademikom D.Y. Nalivkinym.
(Caucasus--Geology) (Caspian Sea region--Geology)

VI!!T3LIUSO A,B.
..- --- ,
; Regional lithologic stratigrarhy and formtion of terrigenous
deposits In the southwestorn Caucasus. Trudy Ten. ob-va est. 69
no.2rl26-150 157. (mm 11:2)
(Caucasus-Rocks, Sadimentar7)

vis"Mus. -A.D.
Using qnantitatIve mineralogical, petrologIcal or chdmlc&l traits
to correlate Indeteratuate strata. zap. Toes. min. ob-wa 86 no.l:
99-115 '57- Wft 10.- 4)
lo Laboratorlya aerouetodov AN SM. Leningrad.
(Geology, Stratigraphic) (Mineralogy, Detorminative)

TISTNLIUS, A.B.
Statistics of vicrostractural diagrame. Zap. Irses. min. 4ob-va P6
no.6:691-703 '57. (KnU 110)
(Crystallography, Mathematical)

AUTHOR: Vistelius, A. B. 20-117-5-39/54
TITLE-. On the Problem of Pre-Permian Volcanisr, in Western T!urkmert.'abE voprosu
o kharaktere dopermskogo vulkanizma v Zapadnoy Turkmenii).
PERIODICAL: Doklady AN SSSR, 1957, Vol. 117, Nr 5, pp. 867-869 (USSR).
ABSTRACT.' In this paper the volcanic rocks are to be investigated of the mono
tioned region and time, also with respect to the order of their forw
mation. The "marbles" of these rocks from the Permian conglomerates.
and the conglomerates of the basis of lower Triassic have a diametei
of approximativelY 5 cm and are derivatives of acid magma. quartz
porehyries are among them rare in pure state. Beside quartz allsemi-
nations they have a basic mass of microfelsite structure. The typical
quartz porphyries are followed by tuffs to a great extent distributed,
Vitro-clastic and lithoclastic varieties occur structurally. The sings
1e crystals are often broken here and consists of quartz or feldspar.
The latter is either plagioclase or potaah-feldepar..The splinters
occurring in tuffs are especially manifold: granite, quartz, porphy-
rites. Furtbermore in small quantities splinter& of blaatomilanite5'
and horn-atones (11ragovik") and round splinters consisting completely
of fine laths of colorless mica and splinters of vein quartz.were
Card 113 found in the lithoclastic feldspars and apparently in a part, of the

20-117-5-39/54
On the Problem of Pre-Fermian Velcanism in Western Turkmeni5u
quartz porphyrites. The main mass of the tuffs and of the quartz
porphyries adjacent to them is comparatively fresh, i. e. though the
meta3tasis is fully-ar-fstallized out the processes of the epidotizan
tion etc. are only to a smaU extent marked. Among the secondary als
teration processes of the tuff splinters a local carbonation and trans
formation into horrztone was found. Furthermore granophyre..microgras
nites, quartzxchaexolite..keratophyres, malchites, and splinters or
uar -- veins ~Hith Fo-Um-Mane were fouRd.-Vo`IUW2g concL~mon,97aF
T
q
be IF-awM.-T) gra-nIIUe--s,)porphyrites, quartz porphyries, as well as
products, of the hy~rothermal activity were formed as consequence of
the volcanic activity; they accompanied the volcanic activity. The
granites and porphyrites were the oldest. They were injected by quartz
porphyries. 2) The depth of the erosion section (Ileroziomrjy srez")
of the Pre-Fleratian formations volcanic was not great in the Permian
time. On the one hand comparatively only to a small extent changed
tuffs were eroded, on the other hand a vein system was destroyed
which accompanied the vok-anic activity and speaks of a rather not so
great depth of the formation of the latter. 3) the rocks:irrvestiga-
ted here and the total character of the volcanic activity are here
considerably approximated to those of the district of Krasnavodsk
(reference 4). The age given there! Carboniferous can be well brought
Card 2/3 into line with the data of the author. These latter., confirm by their

on the Problem of Pre-Fcrmian Volcanism in Weatern Tu-rkrenJy% 20-117-,t:-39/54
fauna the upper Limit, though they do not determine the lower age
limit of the investigated volcanic formations.
There are 4 Slavic references.
ASSOCIATION: Laboratory for Aeromethods of the A SUSSR (Laboratorilmaerometo-iov
Akademii nauk SSSR).
PRESENTED: July 3-7, 1957) by D. S. Korzhinskiy,,, Academician,
SUBMITTED: Ju-17 1-5, 1957.
Card 313

16(2); 3(5) PEASE I BOOK EXPLOITATIQN scyv/148o
Vistelius, Andrey Borlsovich
Strukturnyye diagramy (Fabric Diagrams) Moscow, Izd-vo AN SSSR,, 1958. 157 P.
2,500 copies printed.
Sponsoring Agency: Akademiya neuk SSSR. Laboratoriya aerometodov.
Reap. Ed.: N.G. Ken', Corresponding Member, USSR Academy of Sciences; Ed. of
Publishing House: Ye.A. Semenova; Tech. Ed.: M.Ye. Zendell.
PUMWE: This book is intended for geologists working in the various fields of
geology in which spatial orientation of objects is studied.
COVERAGE: The book contains a systematic presentation of the construction of
fabric diagram. Construction methods proposed by other authors are outlined
and the author's method for the construction of fabric diagrams, based on the
principles of probability tbeoryis presented. The first two chapters of the
book deal with the basic theory of projections and the fundamentals of proba-
bility theory and statistics, which are necessary for the construction of
fabric diagram. The author thanks Yu.V. Linnik, corresponding Member,
Academy of Sciences, USSR, for the evaluation of vector parameters for the
Card 116
2-

Fabric Diagrams SOV/1480
planar case, Professor K.A. Evonarev for his comments on the first chapter.,
Professor N.A. Sepogov for his comments on the second chapter,, and
A.P. Xhusu, for her help in selecting vectorial methods. There are 65 refer-
ences, of vhich 26 are Soviet., 31 English, and 8 German.
TAKE OF CONIMM:
Introduction 5
I. The Spherical Surface and Ito Plane Projection 7
Certain properties of spherical surfaces 7
Projections 9
Types of azimuthal projections 13
Graphical constructions vith the,aid of azimuthal nets 17
11. Certain Concepts of Probability Theory and Mathematical
Statistics 27
Probabilities ZT
Types of probability distributions 35
Uniform distribution 35
Normal (Gaussian) distribution 37
Poisson distribution 40
statistics 41
Card 2/4d~_

VISTALIUS, A.B.
Spectral brilliancy of Aptian, Albian, and Senoman sand-alourites
In the trans-Caspian region. Geol. Zakasp. no.1:31-67 '58.
(MIRA 11:11)
(Caspian Sea region-Silt--Spectra)

SOV/165-58-6-22/24
AUTHORSt Vistelius, A.B. and Korobkov, I.A.
TITLEs About Certain Questions of the Geology of the Western Turkmenistan
PERIODICAL: Izvestiya Akademii nauk Turkmenskoy SSR, 1958, Nr 6, pp 115-119 (USSR)
ABSTRACTs The authors criticize various omissions, inexactnesses and rashly
formulated conclusions in reference to specific problems In "The
Geology of Turkmenistan", which was published as the 22nd volume,of
"The Geology of the USSR". There are: 1 table and I photo.
ASSOCIATION: Institut geologii AR Turkmenskoy SSR (Geological Institute of AS of
the Turkmenian SSR)
SUBMITTEDs August 14, 1958
Card 1/1

AUTHOR'. Vistelius, A. B. 20-1.18 -6-31/43
TITLE; A Scheme of the Division Into Dintric'.'3 of the Alluvia!-
Sediments in the Pamir According to Their Yineral Association
(Skhema rayonirovaniya allywiallnykh otlozheniy Pamira po
ikh mineraltnym assotsiatsiyam)
PERIODICAL: Doklady Akademli Nauk SSSRj, 1958) Vol. 118, mr 6,
pp. 1158-1161 Mqsp.).
ABSTRACT.' The object of this work is to separate the mineral main-asso-
ciations of the alluvium of the Pamir-rivers. Regions with
characteristic minerals., Yiz, with a high content of such
minerals, or with pecularities Indicating a specificity of that
regionj should be separated. Average (x-) contents of the minerals,
their standards (s) aryl the number of analyses (n) which served
for tracing the respective district, are given in table 1. The ooze
provinces were named according to the specific minerals which have
the maximum values of the fraction t v 5E Vnla3. The following
associations which cover certain provinces, can be separated by
using the analytical tables, mineral specifications and the spes
Card 115 cific character of the hydrographic net: 1) Hematite-associa-

A Scheme of the Division Into Districts of the 2o-n8_6_31/43
Alluvial~Sediments in the Famir According to Their
Mineral Association
Card 2 15
tion (figure 1). Characteristic for the alluvium of the system
of the TEM-y-sRaya) ryzy1_Su-Sarkhob_Vakhs-h (up to the middle
course.of the latter), Kulyab-depression, Yazealem-river and
the Kara.Kult-lake. A high hematite-content in the ooze is ty=
pical. 2 types of hematite occur:,, a ) grey as steel, crystalline,
briUiant as metal and b) solid, crypt ocrys f, alli no. Red colored
cretaceous deposits served apparently as source. 2) A metamor-
phous association ca7ers the basin of the lakes hang-K~an~
Shor-Kul-1, as well as the rivers Ak-Su (partly), Murgab and Bar-
tang, as well as the section of the Pyandzh-river between Eartang
and lazgulem. A constant content of tourmaline and epidote which
exceeds by far the standard, is characteristic (table 1). Expo-
sures of crystalline slate on the rivers Shakhput, Zor-Burlyuk
and on the right, affluents of the Ak-Su, serve apparently as
source. 3) Association of apatite, in which apatite largely
prevails (28 o). The region embraces the upper course of Ak-Su,
the rivers Alichur and G=t, as well as the Southern slope of
the South-klichur-chain. Since both zirconium and monazite
(reference 2) were previously found in the Alichur-basin, it

A Scheme of the Division Into DL,3Lricts of the Alluvial- 20-11.8-6-31IL3
Sediments in the Pamir Accordinz to Their Efinrral ~5sociat_'-n
is obvious that an erosion of alkaline rocks took place. The
mostl,)r rounded apatite occurs in 2 varieties. Further 2 spe-
cies of garnet were found. 4) Association of andalusite
coverv a small disLrict in the South-West of the previous
association. It is situated between the Eastern end of the
South-Alichur-chain and the Northern slope of the Wakhan-chain.
Deposits of the proper sources of the Amu-Darlya (the brook
Makur-Chill-On and the lakes: Zor-Kull, Kuk.Dzhigit and Chakan~
Kull). Chlorite is always present too, and sometimes a great
deal of brown tourmaline (up to 330/0). Epidote and minerals
of the amphibole group form the main-background of the ooze.
A relative coarse-graininess is characteristic on the whole.
5) Garnet-association occurs in the oozes of the lower course
of the river Pgi~nan~ in the alluvium of Vakhan-Darlya opposite
the village of Lyangarr-Kosht.-Anenriehment with apatite is found
further down at the Pyandzh to-the Shitkharv. Still further down
to the Bartang and along the Shakh-Dare an enrichment with gar=
net, mostly of the almandine~type is found. Crystalline slates
and gneisses of the axial parts of the mountainous structures
Card 315 serve as source. This association is further found with the

A Scheme of the Division Into Dist--icts of the 20-118-6-31/43
Alluvial-Sediments in the Pamir According to Theii-
Mineral Association
Card 4/5
Pyandzh-affluents which drain the axial. parts of the
Hindukiish (Wakhan-Darlya, Kokcha). The valley section of the
Pyandzh between the mouths of Yazgulem and XyzylmSu contain3
the 2 following characteristib a.38ociations which should be
considered as independent; 6) 11agnetite"3.9ociation. It covers
the environment of the crossing of the Darvaz-chain 1)y the
Pyandzh. The alluvium of the river ob-i4ffiumbou, which is also
rich in epidote, belongs also to it.'The association is on the
whole approached to the previous one.~ The main source of erosion
is obviously the Darvaz-chain with U3 metemorphous masses.
7) Epidote-associat ion 2 Covers the course of Pyandzh belcyr its
exit from the Da-iVa-`F---cNain till to the mouth of the Kyzyl-Su,
as well. as the lower course of Vakhsh and the point of jurction
of the. lat!,er with 1.11~e Fyanrlzh. Hydrodynamic processes which
enrichl)relatively,the ooze with epidote, are obviously the
source. Concluding, a comparison with the associations of the
Kavkaz is given.

A Scheme of the Division Into Districts of the 20-118-6-31/43
Alluvial-Sediments in the Pamir According to Their
Lineral Association
There are I fiure, 1 table and 2 referencesj all of which
are Slavic.
ASSOCIATION: Laboratory of Aerial Pbotogmpby, AS USSR
(Laboratorlya aeropietodov Alrademii nauk S35R)
PRESENTED: September 2, 1957, by D. I. Shcherbakov, Academician.
SUBLITTED: September P, 1?57.
Card 515

1=1, Nikolay Georglyevich; VISTIMUS, A.B., doktor geologo-minera-
logichookikh nauk,-otf.iid-*';-'U=OVA, Ye.A., red.isd-va;
ZINMIg N~Ya.v tokhn.red*
[Measuring deoipherment of aerial photographs under field
conditions] Ismeritellnoe deshifrirovanis aeromdmkov v
polev7kh usloviiakh. Koskva, Isd-vo Amd.nauk SSSR. 1959.
3.22 p. (MIRA 12:6)
(Photograpb7, Aerial)

30)
A UTHOH i Vistel"u-S. A. B-- SOV/20-125-6-38/61

TITLEi On the Origin of the Cheleken Peninsula Red Beds (K vopros4
o proiskhozhdenii krasnotsvetnoy tolshchi p-o. Cheleken.' Eyp---z-
iera-- in the Absolute Age of Clastic Minerals in Solving
Lithological and Paleogeographical Problems (Opyt ispol'ZovaniYa
absolyutnogo vozrasta oblomochnykh mineralov dlya resheniya
zadacb litologii i paleogeografii)
PERIODICALs Doklady Akademii nauk SSSR, 1959, Vol 125, Nr 6, pp 1307-1310
(USSR)
ABSTRACTi In order to solve the problems of the formation of the sediments
mentioned in the title the author used the absolute age of the
minerals of which this mass consists. The following problems
were to be solved: (a) Where is the area supplied with
arenaceous-aleuritic material? (b) Is the formation of loams
Cla8tiC or diagenetic? The age of the minerals was determined
by the argon method (in the Laboratoriya geologii dokembriya
AN SSSR w Laboratory of Precambrian Geology AS USSR under the
supervision of E. K. Gerling). Table I shows the results of
the age determination of mica. The following conclusions are
Card 1/3 drawn from these datas 1) The age of mica in the Cretaceous

On the Origin of the Cheleken Peninsula Red Beds. SOV/20-125-6-38/61
zxp~rience in Usingthe Absolute Age of Clastic Minerals
in Solving Lithological and Paleogeographical Problems
sediments agrees practically with its age in the granitoids of
Krasnovodsk (Ref 4). The loams of the red mass are, on the
whole, of elastic origin. It is assumed that they were formed
by the erosion of Cretaceoun sediments of the rocks surrounding
the red basin. 2) The mica of the arenaceous strata on the
Chelaken Peninsula belongs to the Upper Cretaceous. It is
possible that this mica was transported from another region
where Cretaceous intrusions or their destruction products were
eroded. The origin of tile mica from sand differs in principle
from that of the loam material. It is at present too early to
speak of the source of the material of Cheleken Bands. It is,
however, obvious already that their transportation was rendered
impossible by the Uzboy, since the Amu-Darlya transports in
its middle course older Upper Jurassic mica. Thus, the material
of part of Cheleken sands originated from the alpine geosynclinal
region. I.e. it could be washed down from the Paropamisus or
the Hindu Kush by an artery which in the middle and lower course
agreed with the presevtAmu-Darlya. Other sources are, however,
Card 2/3 possible as well (Refs 2,5). The first attempt of utilizing the

On.the Origi'n of the Cheleken Peninsula Red Beds. SOV/20-125-6-38/61
Experience in Usingthe Absolute Age of Clastic Minerals
in Solving Lithological and Paleogeographical Problems
absolute age was very successful. The investigations are
continued. There are 1 figure, 1 table and 5 Soviet references.
ASSOCIATION: Laboratoriya aerometodov Akademii nauk SSSR (Laboratory of
Aerial Methods of the Academy of Sciences USSR)
PRESENTED: November 29, 1958, by D. V. Nalivkin, Academician
SUBMITTEDt November 20, 1958
Card 3/3

14(2) '
AUTHORSt Sarmanor, O.V., Visteliyus, A.B. SOT/20-126-1-15/62
TITLEs On the Correlation Between the Percentage Variables (0
korrelyataii mezhdu protsentnymi velichinami)
PERIODICAM Doklady Akaaemii nauk SS3R9l959tVol 126,Nr 1,
pp 22 - 25 (USSR)
ABSTRAM Lot x 1, x2, ... 9'xntzlt z2' ..,zM be nonnegative random
variableag the sum of which is assumed to be 100% . Let only
the values s
100X 100Z.
x +...+x +Z +..+z x +x +..+:x +Z +..+z
I n 1 M 1 2 n 1 M
be 'obsezvable. The,new random variables qi and '5j are de-
noted as percentage variables.
Theorem t Let %I - const. If the correlation coefficient
between 9,/ ~;, and ~2/ 15, is calaulated, then the real
correlation coefficient between x1 and x2 is found.
Card 1/2

6
On the Correlation Between the Percentage Variables SOV/20-126-1-5i`~"'
Theoremr Let z I and z2 be independent of each other and of
the other variables. Theqllq2 are assumed to be positive.
The correlation coefficient R *- R(~,/Tj; Q~3-2) is 4, the
correlation coeffici 'ent-R - H(xl ; X2)' with respect to the
absolute value and has the same sign. The coefficients
R(~111- ) and R(xl ; x ) can only simultaneously
/ ') 1 2/52 2
vanish.
There are 3 references, I of which is Soviet, and 2 are
American.
ASSOCIATIONs Matematicheskiy institut imeni V.A. Steklovs, AN SSSR
. (liathematical Institute imeni V.A. Steklov,AS USSR)
PRESENTEDt November 26,1958, by S.N* Bernshteyn, Academician
SUBMITTEDt November 25,1958
Card 2/2

LIN
K I i 8 1
3 :1 - t t
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it
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VISTEMITS1--A, 73
Characteristics of germanium concentrations In coald In connection
-~dth- V.M. Mrshovie reviev. Izv.AN SSSR.Ser.geol. 25 no.8:100
Ag 160. (MIRA 13:8)
(Coal) (Germanium)

YIOSIUS , ri ~vich~-FIJSTOVALOVp L.V.p otv. red.; KUDRITSMO D.M.p
redi, izd-va,- ZE14DELIp M.Ye.p tekbn. red.
[Material on the lithostratigrapby of the producing formation in
Azerbaijan) Materialy k litostratigrafti produktivnoi tolshchi
Azerbaidy,hans. Moskvap Izd-vo Akad. nauk SSSR, 1961. 157 p.
(KM 14:7)
1. Chleri--korrespondent AN SSSEL (for Pustovalov)
(Azerbaijan-Geology, Stratigraphic) (Rocks, Sedimentary)

VISTELIUS. A.B.
Correlation of land of the middle of
of productive strata of the Apsheron
the Cheleken Peninsula; a follow-up
and V. G. Rikhter. Biul. MOIP. Otd.
(Caspian Sea region--Geology,
the Caspian between sections
Peninsula and red beds of
in articles by G. P. Tamrazi4n
gebl. 36 no.1tI48-151 Ja-F 161.
(MIRA 14:5)
Stratigraphic)

VISTEMUS, A.B.; KRYLOV,, A.Ya.
Absolute Age.of the clastic part of sandy silt deposits in the
southwestern part of Central Asia. Dokl*AN SSSR 138 no,2:422-425
Vq 161. (KM 146)
1. Laboratoriya aerometodov Akademii nauk SSSR i Radiyevyy inBtitut
im. V.G.Khlopina Akademii nauk SSSR* Predstavleno akademikom D.V.
Nalivkirgm,
(Turkmeniotan-Geolog7.9 Stratigraphic)

VISTELIUS, Andrey BoriBovich; ROI-L41,10VA.. Nariya Androyevnal- KULIYGV..
., r6d-.-Jzd---m-,-WUWEEVAp H.A.; tekhn. red.
[Red beds of the Cheleken Peninnaa; lithostratigraphy and
geo3.ogy]Kra,snotsvetrqe otlozheniia poluostrova Cheleken; lito-
stratigrafiia i geologicheskoe stroanie. Moskva, lzd-vo Akad.
nauk SM.. 1962-. 226 p. (MIRA 15:10)
(Cheleken Peninmda-Rocksp Sedimentary)
ft.

VISTELIUS, A.B.
Phosphorus in granitoids of the central Tien-S~,an. Geokhimiia
no.2:116-133 162. (KIRA 15:3)
1. Laboratory of Aeromethods, Academy of Sciences of the U.S.S.R.0
Leningrad.
(Tien-Shan--Phosphorus)

USTELIUS A B
Mathematical geology. Geol. i geofizo no,12:3-9 162. (MIM 16:3)
1. Leningradakoye otdeleniye Matematichaskogo inatituta imeni
V.A.Steklova AN SSJSR.
(Geology) (Mathematics)

VISTELIUS Andrey Borisovich;.TIKHIY, V.N., otv. red.; SHENGER,
N .
F, izd-va,- ZAMARAYEVA, R.A., tekhn. red.
(Phase differentiation of Paleozoic sediments in the middle
trans-Volga region and Volga Valley] F~Lzovaia differentsiatsiia.
paleozoiskikh otlozhenii Srednego PovolzhIia i ZavolzhIia. Otv.
red. V.N.Tikhii. Moskva, Izd-vo Akad. nauk SSSR, 1963. 202 p.
(MIRA 16:4)
(Volga Valley-Geology, Stratigraphic)

VISTELIUS, A.B. -
.4.,
11 ... Mathematical geology. Geol.i. geofiz. no.7s3-16 163. (KRA 16:10)
1. Leningradskoye otdeleniye Matematicheskogo instituta im. V.A.
Steklova AN SSSR.

VISTELIUS9 A.B.
- aw"R&O
Probability distribution functions of phosphorous concentration
in granitoids in Switzerland, Guiana, and Equatorial Africa.
Dokl. AN SSSR 152 no.6sl449-1452 0 163. (MIRA 160.1)
1. Gruppa matematicheskoy goologii Leningradakogo otdoleniya
Hatematicheskogo instituta im V.A. Steklova AN SSSR. Predstavleno
akademikom S.N. Bernshteynom.

VISTE'LIUS; A.B.; DEMINA, M.Ye.
Scattering of clastic material in "e~: Aptdan-Senomanian basin of
the southeastern U.S.S.R. Dokl. All 3-35H 150 no.6:1319-1322
Je 163. (MIRA 16:8)
1. Leningradskoye otdeleniye Matematicheskogo instituta im. V.A.
Steklova AN S33R. Predstavleno akademikom D.V.Nalivkinym.
M,-issia, Southern-M sanls-Analysis)

VISTELIUS, A.B.
Problems of geochemistry and information meas%r"S. -
no.120-26 D 164. 1-8:4),
1. Leningradskoye otdelenlye Matematichaskogo instituta Im. V,A,
Steklova AN SSSR.

VISTELIUS, A.B.
Mathematical methods in geoloa. Sov. geol. 7 no.12:148-149 D 164.
fWRA 18:4)

VISTELIUS, A.B.
Basic types of mathematical solutions for problem in present-day
geology. Razved. 1 okho nedre 30 no*6.le--25 is 16," CaFA l7sIO)
1. Leningradakoye otdoloniye Matematicheskogo instituta im. Steklova
All SSSR*

VISIT,LlUS, A.B.; ROMANOVA, M.A.
~ ''
Distribution of the heavy fraction in the sandy sediments of the
central Kara Kum. Dokl. Ali SSSR 158 no-4:860-863 0 164.
(MIRA 17:11)
1. Gruppa matematicheskoy geologii Leningradskogo otdeleniya
Matematicheskogo instituta im. V.A. Steklova AN SSSR. Predstavleno
akademikom A.L. Yanshinym.

VIIST71,111-~,
Va- I ii t4 .jri.,i a t*-L tn z.,~ f.:; lri Q.F" sec n,
Urall,,. LoPl. U* 164, nc-5:1115-1118 0 165,
Illysh of the
(MIRA 18:10)
I# Gruppa mato7-atlcheskcy gec'.o,gi~ Leningrarishogo otdel.eniya
MatematicherAcgo instluta im. V.A.Sieklova AN SSSR. 'Julmitted
1,11arch 33, 196-3.

, VTSTEIM-3t IT7GE7LliGN, T.S.
Stratification theou. Dokl. AN SLS? 164 no.1:158-160 S 165.
(~Un '.Big)
1. Gruppa matemat'Acheskoy geolog"! Loningradskogo otdelen'Lya
Matomatiche3l,cfm instituta in. V.A. Sto--klova AN SSSR. Submitted
Mhrnh 2.3, 1965.

VISTEL11J,-,, A.B.,- FAAS, A.V.
Characteristics of the alteration of layers in some cross
sections of sedimentary formations. Dokl. All SSSR 164 no-3-,
629-632 S 165. (min 18:9)
1. Gruppa matematicheakoy qeologii Leningradskoy geologii
Loningradskogo otdelen-Aya MAtematichaskogo instituta im.
V.A. Steklova AN SSSR. Submitted Plarch 13, 1965.

L 32772-66 EWT(1) GW
ACC NR.- AP6012925 SOURCE CODE: UR/0020/66/167/005/1115/11 18
AUTHOR: -Vistelius, A. B.
ORG: Leningrad Branch Mathematic Institute im. V. A. Steklov? Academy of ScienceE
--;e
bbbRy--
idelpniye Matematicheskogo instituta
~n ~1;
a s o o Akademll nauk
SSSR
I '~-
TITLE: The formation of granodiorites on Mt. Beloy in Kamchatka (an experiment in
stochastic simulation)
SOURCE: AN SSSR. Doklady, v. 167, no. 5, 1966, 1115-1118
TOPIC TAGS: simulation, mathematic model, mineral T7VC111?5T1C- PROCFS-3
4 e e.'e'F 7-1 e, "/ I
ABSTRACT: The author approaches the problem of the origin of granites from the point
of view of stochastic simulation. This involves the construction of a theoretical model,
followed by a determination of the degree of agreement between this model and observed
data. It is possible in this way to obtain a certain number of models which will not be in
disagreement with observations and, through their refinement, to select from them a
model which will most reliably predict essential properties of the object. It is this model
which is then to be selected as the nearest to reality. In this paper, an attempt is made
Card 1/2 UDC: 552.31/33+552.311

L 32772-66
ACC NR: AP6012925
to construct a model based on the premise" granite Is the product of the crystallization of
magma, " with this model then checked by means of a study of formations from Mt. Beloy
on Kamchatka. The proposed model is based on the supposition that, during crystalliza-
tion, minerals are liberated from the magma until residual fusion takes on a eutectic
composition. For purposes of investigation a sample was taken of granodiorite from the
peak of Mt. Beloy. It Is shown that the hypothesis of the magmatic origin of ternary
granitoids from Mt. Beloy is in agreement with observed data. The model and the method
were checked against a large body of data from an investigation of the Kyzil-Tas massif
in Central Kazakhstan. Herej, also, good agreement with observed data was achieved.
The author expresses his gratitude to V. K. Rotman and B. A. Markovskiy for their
assistance, as well as to. D. N. Ivanoy and V- Faula- The paper was presented by
Academician D. S. Korzhinskiy 3 Jan 66. Orig. art. has: 4 formulas and 1 table.
SUB CODE: 08y SUBM DATE: 28Dec65
Card 2/2 is

-7~ 1 1 n

SVIRIDENK0, F.F., inzh.; KRIVENKO, P.T., inzh.; Yj,~Tp~qVSK_I.Y, N.T., inzh.
Characteristics of the procedure for converting phosphorous
pig iron in redesigned open-hearth furnaces operating on natural
gas. Stall 23 no.8:700-704 Ag 163. (MIRA 160)
(Steel--Metallurgy)
(Open-hearth furnaces-besign and construction)

LEPORSKIY, V.V., inzh.; BULISKIY, M.T., inzh. (deceased]; SVIRIDENKO, F.F.,
inzh.; VISTOROV.7.IY,, N.T., inzh.
Rapid filling of the riser-head part of ingots. Stall 23 m -3t
705-706 Ag 163. (MIRA 16:9)
1. Metallurgicheskiy zavod "Azovstall."
(Steel ingots)

T
GERSOCTUip M.A.; SVIRIDENKO, F.F.; KAZAPNOVSKIY, D.S.;
POPOVA, A.N.; FRADINA, M.G.; Prinimali uchastiye.. T7:Fj~,'~'%"
.;, 5.
RJDOLISJUY, N.L.; SIFTY.4.11EV, N.P.;
Ya.S.; BULISKIY, M.T. [deceased]; ARKHAVCIELIE~KfY, yu.,,,.; tj-~,r-et-j V,
B.A.; VISTOROVSI~TY,___~.T.; RAKIIANSKIY, B.I.; -SA110,711KOV, V.ye.;
RYABININ, N.G.; YJP.AKULINAp R.R.; FADEYEVA. A.M.; D.A.
Improving the production of high-strength ralls (11loyllir
them with granulated ferrochromium In the ladle. Stall '21~
no.5:408-412 W 165. 64TRA 1-8:(,,)
1. Ukrainskiy nauchno-issledovatellskly institut metrallov I zavod
"Azovstall".

- -I - - -'- -- - -
, - I . . ~ . ~ , I ! . -
- :;:/C-, I I .. I." I,,.,- I , "/~-
?( i.' !Iiif 't.., -, (;~'

VT'~T;: -~7, A, ,-I Tcr
n Occ,!~icr, 01 the
Vol. 13/12, lgr",D.
F 1, W -(, T F, r~, T'--; ~T C , R
So: Fist FiirOTIPan tkc-7-~.-Acn, Vol. 4-, 1:0. 1957

VISTRICKA, ZVOWIMIR
?A 7OT39
IL94T
lRootiflerso Nor""
FAilroads, lleotrla
Olbroury psatif Jws In Substati(me of Xlectric Ran-
mys,w zvmimir Vietricks) 3 PP
wjQad:L xLektrotehnicar" No 6
Describes mercuu rectiflers. inaludem cut-avay
pioture vith nsms of parts) dlagrm) and vlev of
sub$tAtiCn interl4r- ROfOrD to no BPSC'flo r&"-
70"

VISTRICKA, Z. _-_
,r. . . _ _
qleasures and systems of units" by M. Brezinscak. Reviewed by Z. ' J st r-; e:k z -
Stroj vest 7 no. 4-5:119 c 61.

VISTPUCKA, Z.; URE2-IOVIC,.I.
Anirwer of the authors of "Coimection schemes in electrical ere-tetri-,,-,
to the reviewer. Zavarivac 6 no.2/300-51 ICL.

VISTRICKA, _Zvonimir--
4-
1111.1casures and systems of units"' by (inz, I Marijan BrezInscake Reviewed
by Zvonimir Vistricka. Elektrotehnika Hr7 /+ no.1/2:51 162.
1. Glavni uradnik "Tehnicke knjigem,

VISY, Zoltan
Coordination of the work of the construction reseqrch or-
ganization. Epites szemle 7 no.11/129345-351 163.
1. EpItOIII~-,.fi KLItatasi Koordinacios Iroda veze-
toje.

VISY, ~944n-
---
Coordination of architectural research In the Council for
Economic Matual Assistance member states. Epites szemle 6
no.6sl82-183 162.
1. Epitoanyagipari Kozponti Kutato Intezet tudomanyos oaztaly-
vezetoje.

rk N
, ~ 4j
SOV/78-4-4-'5/44
.
AUTHORS: X-ovalenkc, K. If., V-'styak, L. 1.
TITLE: Concez-ring the Zinc Citrate Complex in Aque7,us Sclution
(0 ts--t--ratnykh kompleksakh tsinka v vodnom zastv,-,re)
PERIODICAL: Zhurnal neurganicheskoy khimi,, '1959, Vol 4, Nr 4; Pr 6-"*.--807
(USSR)
ABSTRACT: The romplex formation by citrase and zinc ions was --;n-.r- & ti, gate-1
in aqueous solution by mea.-ur.-ng the electric conductivit.,,
and by m9ars of potentiometri:,, titration. By the determinat~--,:-
of the aie~,tric ccnd~ictivity it wa3-found that the
the components in the complex is 1:1. The potentiometric t-.tr&--
tion with NaOH of a solution containing zinc sulfate and
sodium ait-rate showed 'hat at the point corresponding to t;-~~
4n
za.mi. 1:1 cf -comp nents P. sudden change the pH 7d-.-
oppear3. The stability of the --omplex was inv,~stiga,~zd at
variau8 pH va~-ues. The complex is stable up to -j. pH ~J 8.b;
higher pH1 5 a decomposition takea plaop. At pli >8. 6 in so.,at
with a 30-fold excess in sodium citrate a basic zin;
1 2- and a stab1lity
forms with the composition [Zn(OH)C,H
0
Card 112 7
5
r.;o-istant o~ 1.2.10-11. The dependence of the strength cf th-

SOV/78-4-4-15/44
Co~lcerning the Z-ri--% Citrate C3,mplex in Alueous Solution
aion L---rznt cf the --nc u;~~n the ccmpcsir~.-,r--
in the reductfor at the mercury elr-ctro,-;~-
-~hF~ :;cmp-~ ex formation. ir, the s:vstsm, ZnSO,-Na,C~
H-10 ant 4-~~ -lie somposition of the co-npl~--x. The
ronfirmed tvh;~ formation :,f 'I z:!.n,
':7::it wi`h the Bam,3 I : 11 ratio of zompolen.6. The
;.apv~ZT~ -Lhe f-:,-, I ~)w`ng tab! -s: The :f
iz'Le ~-tr` :a.! ~--,nductivity to the ZnSO4 : Na3C it f:'
2" Rgsults of the potentiometric tiLr t4o-~
scl.u'.-Lon ~~-,-,taining eq4fmc',-~.ar am6unts of ZnSO4 and NFL3C1 t.
D~.pender:~e of the potentlial of the zinc upcr the
---f Na Dependenct; -~f the pote~-~tiai of the
3C.- *,
thp. pH val--.ie of the sclutior.; 5) Depenaleme of t1le
of ft,~ diffusion zurrint of the zinc upon the
NS3 There are 6 figures, " tables, and 9 referen,.-..,
7 of w-11ch axe So-iet.
SUBMITTED: Tan%iary 17, 1958
Card 2/2

KOVALINKO, K.N.; VISTTAK, L.I.
Citrate complexes of zinc in aqueous solutions. Zhur. neorg. khIm.
4 no.4,-801-807 Ap ,59. (MIRA 120)
(zinc compoimde)

VI-SUSOR, T.A.
3430.5. VISU-SOVA, T.A. Isseldsvanie sisterW platina-pallndiy-nikell.
Izvestiya sektova platiny. Drugikh blagorod. metallov.(In-t
obshch i neopgan. khimii im, komakova), vype 24, 1949, S. 5-14
-BibUogr: 8 Nazv.
SO: Letopial Zhurnallnykh StateY Vol- 34, Moskva 1949

VISVARATAN, R., profeesor (Indiya)
Uperimental pulmoaar7 atelectasto. Probl.tub. 34 no.2:68-69
Mr-Ap 156. (KLRA 9:8)
(AT]ILECTASIS, experimental,
(RUB))

SUR=1-2, Given llama
Countr7s Czechoslovakia
Academic Degreess /not given/
ATfiliations /not given/
Source# Bratislavaq Nasa Vedap Vol VIIIv No 4v 1961p pages 238-243,
D&W IfIn the Ocuntry Of DismorA Splendor mid Shadow."
Authorst BUCKOp Stefan
VISVADER, Prantisek
GFO 9816%)

r a n t i s e k
SUFCiA!~E, Given Names
Country: Czechoslovakia
Academic Degrees: /not given/
Affiliation., /not given/
Source: Brat-islava, Nasa Veda, Vol VIII, No 10, 1961; pp 622-624
Data; "Bizerte, the Port of Buried Illusions."

FEKETE, Agnes; TARABA, L; YTSY,, Maria
Splanchnicotomy affords protection against acute renal failure
in dogs. Acts. physiol. acad. sci. Hung. 26 no.3t245-249 165
1. Institute of Physiologyp University Medical Schoolo Ekida-
peat,

L 136~3-46
ACC Nit: AP6007052 SOURCE CODE: 191/00lt3/65/()17/(,'rjJ/0326/0331
AUTHOR: Balint, P~ter; M.
ORG: Medical University of Budapest, hirftitito of Physiology (Budaposti
Orvostudomanyi Egyetcm, Elettani IntenO.)
TITLE: Relationship between Itrue creatininel and lp.,3eudocreatlninel concentrations
in dog plasma
SOURCE: Kiserletes orvostudomany, v. 1.7, no- 3, 1965, 326-331
TOPIC TAGS: dog, blood plasma, organic nitrogen compound, biochemistry, animal
physiology
ABSTRACT: The Popper, Mandel and Mayer (1937)
method of creatinine determination, when combined with adsorption on Lloyd's
reagent, is suited for differentiation of the chromogens of Nxly fluids
which also give a positive Jaffe's reaction. The following findinCs were
made,. 1) In normal dogs, only about 56 per cent of the vlasma chromocen
content is 'true creatinine', the other 44 per cent is pseudocreatininel;
2) The values of 'true' creatinine clearance are in aereement with the
inulin clearance and are suited for GFR calculations. The chromogen clearance,
however can not be used even for an approximation of the GFR in non-,tal
dogs) 3) Following nephrectomy, the chromogen concentration rises parallel
with the NPN. In the azotemic animal. a much smaller fraction of the chromo-
Card 1/2

L 13633-66
ACC NR: AP60070-52
gen is,derived from the lpseudocreatininot than in normal dogs, that is, the
rise in chromogen is mostly related to the increase in Itruef creatinine
concentration. Orig. art. has: 3 tables. (JPRS1
SUB CODE: 06* / SUBM DATE: 31Dec64 / CRIG REF: 004 / OTH REF: 027

;~I:;Tt ?4;
Or
Trm cmatWiro" and n-.wc- AoamatLr, Ina* in flood plawn
of tho dq;a Aota phyolcl, noad. acie Tirg, 2C noo3t265-272
1 65,
Is Distituta of Vbpialoeyp I...-Avoraity 14odloal Sohoolp
BLularpost. Sulnitted Janum-y 70 3.965.,

FEKETE, Agnes; TARABA, Istvan; VISY, Maria
Effect of splanchnicoto" on the prevention of acute renal
damage in dogs. Kiserl. orvostud. 15 no.6.-664-668 D 163.
1% b1dapesti Orvostudomanyi Egyetem Elettani Intezetenek
koslemenys. HER[RECTOW) (ACUTE RENAL FAILURE)
MANCHNIG NERVES) (NEUROSURGERY)

L 43o16-66
ACC NN, AT6031826 SOURCE COIDEt HU/2505/65/C26/W3~/0245~W49
AUTHORt eke&g, Ames: Taraba, Istvan; Visy,, Maria-Vishio N.
ORO: Institute oL Physjolog7. Medical UniMrsit_v_of BudaRaRt (Budapeati
Orvostu-Ud-manyi Egyetem,. Elettani Intezet)
TITIE: Protection afforded by splanchnicotomy against acute renal faLlure in dogs
SOURCE: Academia acientiarum hungaricae. Acta physiologicap v. 26,, no- 3. 19659
2145-249
TPPIC TAGS: dog,, pathology, animal physiology
AkTRACT: A syndrome analogous to acute renal failure in man has been induced in
dqge by unilateral nephrectomy and the temporary clamping of the artery of the
reomining kidney* The same intervention was not followed by renal failure and An
thological changes disappeared after 14 days when the animals were splanchnicotomis
the left side at the time of right naphrectomys The differences between the
length of survival in the two groups were statistically significant. Neurogenic
factors are suggested as playing an important role in the development of acute renal
failure. Origo art. has: 1 figure and 1 table. (Origk art. in Fag.] [JPRS1
SM CODEj
06 / SUBM DATEI 22Dec63 / OTH REF: 017
MLP
0

Obstetrics and Gynecology
1 pe, RY
V,.-,,Dj, Pal, Dr, 1113Y, 'Yaria,. or; 1-'j:6ical 11niversity of Bu,,iappst, IL "Yne-
colo(,ical Clinic irector: ZOLTAN, linre, Or) (Budape5ti Orvostudomanyi
Fgyet,-m, 11. Nol Klinika).
11 The Provision of a Fetal Type of Blool Circulation and Gas Fxchanie in
Human Fctuses Outside of the Yaternal Or;;?,anism."
Budapest, Orvo5i Hetilap, Vol 107, Nlo 43, 23 Oct 66, pages 2-027-2028.
;.bstract: [Authors' Hun,7arian surrimary] The P0551bilities of maintenance of a
fetal type circulation outsidt~ of the maternal orgranism are discussej. The
authors' own experiences are described in the course of which 6 human fe-tuses
of 250-500 g weiFht, obtained from spont;ineous abortions, were kept alive for
25-60 minutes by means of an oxyEenator inierted between the umbilical artery
and vein. The perfusion was arranged in such a manner that aspiration of the
fluid by the fetuses could not take place in case of their eventual breathing.
In this manner, the fetal type of circulation of an additional two fetuses was
transformed to one of pulmonary type. 2 Hungarian, 9 Western references.

L 04468-67
ACC NRt AP6028467
SOURCE CODE:
HU/0018/66/OW/003/0313/0321
AUTHOR: Balint, Peter; Fekete, Asmeg4_ Tara a V' Maria
--ka
ORG: Institute of Physiology, Medic L! University of Buda st dapesti 117
Orvostudozmnyi Egyetem, Elettani Intezet)
TITLE: Effect of anaestheQ a on the survival and renal function of dogs after loss
of b120
SOURCE: k-serletes orvostudomany, no- 3, 1966, 313-321
TOPIC TAGS: dog, blood circulation, anesthesiology, kidney, blood, tissue physiology;~
ABSTRACT: Oligemic shock was induced in
dogs by removal of blood; the arterial pressure was decreased to 50 mm Hg
.for 90 minutes, followed by re-infusion of the blood. The following ob-
servations were made. 1) When carried out under chloralose anaesthesia,
more of the dogs survived the immediate consequences of the trauma ( 2 days
survival) than in the alert group. 2) Of th,_ 16 dogs which survived for 2
~days after the bleeding, 6 died of acute renal insufficiency within 2-8
days; the 10 which were alive after 15 days can be considered sur-
vivors. 3) In one group of.dogs, an acute experiment was carried out between
.30 hours and 14 days after the blood removal. According to the observations,
in the period immediately following the trauma, renal blood flow decreased,
renal resistance increased, glomerular filtration and FAH extraction'
considerably decreased. When the tests were carried out 14 days after the
;blood removal, no disturbance in renal function was observed. 4) The rela-
tionship between renal-02 consumption and renal blood flow or tubula. 'r__ 11'a
re-absorption was identical in the normal and experimental animala.

1. CA 4 6,2 - C- -~
--- -1
ACC NRt AP6028467 I
The authors thank Bacealmasy Emilne, Ki-iment Olga-and Szalay Elemerne for
assistance with the experiwnts. Orig. art. has: 2 figures and 1 table.
r --- -Y ---I i

Z. "ITI-17Y.
"Accelerated Procedure for Calculation of Frame Structures uith Yovable An-le
Point." p. 11,",' Sz=11c, Vol. 3, no. 3. 'Mar. 10,51,3 Buda--nest-)
'101. 2, no. 9
SO: Yonthly List of East "wopean Accessions./Library of Congress, Sept 1953, 'Uncl.

VISY, Zoltan
----ii~search conference on architeature arranged by the Council for
Economic Mutual Assistance member states. Epites szemle 5 no.8:
249 161.

VISY Z.
Iterative method for the ccalculation of moments on hi6ly economical
reinforced-concrote beams. In Znglish. p. 13.
ACTA TECHNICi,. (Maeyar Tudomanyos Kkademia). Budapest, Hungary, 'Vol. 22,
No. 1/2 , 1958.
Montbdy List of East European 4ccession5 (EEAI) LC, Vol. 8, :,.f0. 7, July 1959
Uncl.

VISY, Zoltan
Results and immediate tasks of the collective scientific
research organized within the framevork of the Permanent
Comtniosion on Construction,. Cuuncil for Economic Ib.1tual
Assistance. Epites szemle 7 no.9:271-275 163.
1. Epitesngyi Minlszterium Kutatasi Koordinacios Irodajanak
vezetoje.

S/ 124/59/000/09/32,"036
AOrj21A0O'.
Translation from: Referativnyy zhurnal, Mash inostroyeniye, 1959, Is'o- 9, r
35826
AUTHOR: Visyashchev, V. S.
TITLE: Tho Strength Calculation of the "Fir-tree" jold-of art
Gas Turbine Working Blade Under Conditicns of Creep
1):~ -) - - ~,j
PERIODICAL; Sb. statey. Chelyab. polA-ekhn. in-t, 1957, No. 11, Pp, 80-102
TEXT: The calculation of the joint during the phase of larEteady ,riep
is based on relationships obtained for two states of the Joint: -Llie _Inltlp"
elastic state, and the steady creep state. One of the existing designs o, a
"fir-tree" joint with six pairs of serrations Is discus*ed as an example.
M. A. 1.
Translator's note: This is the full translation of the original Russian
abstract,
Card 1/1

MYAGIT, 11.1. DWIjA~~:.D
C 1 195~
sa RL
1962/6
ChEINUSTRY

VT.Wilici- I - .- !.. ; ~,!- j--T '-I, ~-
- i-' - . ' 1. i .
Science
Riches of the salt lakes of Kulunda. Novosibirsk, flovosibirskoe obl. gos. izd-vo,
1952.
Monthly List of Russian Accessions, Library of Congress November 1952. Unclassified.

KIRGINTSEV, AbN.;_VISYAGINA,,,L.,N.
Cocrystallization of lead sulfate an.1 3tronti-x-I at IOCPC. Zhwr.neorg.
khim. 9-no.1:233-235 J& 164. (11DA 17:2)
1. Institut, neorganichesRoy khirdi Sibirskogo otdolenlya All SS5R.

KIRGINTSEV, A.K.; VISYAGINA, L.N.
.. ~ . 0
ThermcbmamieB Of Bolid solutions NH4ql eBr at 25
- NH4
Zhur. neorg. khim. 9 no.3:698-701 Mr 164.
(MMA 17:3)
1. Inetitut-neorganicheekoy khimii Sibirskogo otdeleniya
AN SSSR, Novosibirsk.

KIRGINTSW, A.M.; -,T~bYAGIMA, L.M.
Analogy between two types of di&Vams of pbase equilibrium*.
Izv. Sib. otd. AN 53U no. 10:64-70 160. (MIRA 13:12)
1. Institut neorganiehaskoy khimli Sibirskogo otdeleniya AN SSER.
(kMse rule urd equilibrium)

PEKSHEV,Yu.A.; I221SKIY,B.V.,-AVSEIfOV#Yu.M.;MII,CWOV,V.S.;KISVYAIITSEV,L.A.;TELDGIN,
Ya.I.; POTAPOVt V.I.; IMMUSOVt A.A.j ZYKOV# A.A.; KUDINt B.M.;KAKSI-
MOVAp A.P.; NIKOLAYENKO, Zb.l.; VOIXOVt N.V.; SHVETSOV# N.I.; PLAKSIBj,
S.V.; POPOV9 N.N.; KARSHNOV9 L.11.;,YAK1KOVAj T.A.; SHALASHOVt V.P.;
Vigmz~L Y1ktk.-j laUNOV, L.V.; FUSENKOVp N.N.; IVANOV9 N.L p red.;
=..I red.; SLADKOVSKIYp M.I., red.; LEPNIKOVA, Ye.j red.;
KOROLEVA, A., mladshiy red.; NOGINA, N.9 tekhn. red.
[Economic development of the people's democracies; survey for 19591
Razvitie ekonomiki stran narodnoi demokratii; obzor za 1959 god. Pod
red. N.I.Ivanova i dr. Mosk7aq Izd-vo sotsiallno-ekon. lit-ry, 1960.
305 P. (MI11A 14:6)
1. Moscow. Nauchno-isoledovatellskiy kon"yuk urnyy inotitut.
(Europe, Eastern-Economic conditions)

TATARINTSAV, N.M.; VISTARINA, V.P.; KVVMLI, R.N.
Clinical considerations on Omsk hemorrhagic fever in children.
Pediatriia, Moskva no. 6:49-53 Nov-Dee 1952. (CLKL 23:5)
1, Of the Faculty Therapeutic Clinic (Head - Prof. R." M. Akhre*-
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UWR).

SHUR, Yu.B., inzh.; VISYASIICIIEV, A.N., inzh.
Location of dairages in electric power transmission lines. Elek.
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m
VISTASHCIW, V,S,, inzh,
1twVW---.
Investigating the distribution of strains and stresses in Iherringbonso
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the elastic state of mterials. Sbor. at. ORPI no.llt5g-79 157.
(Airplanes-A3gines) (Gas turbines-Blades) (KM 11:4)

VISYASHCMff, V.S., inzh.
1, , ,
Calc,-alatizig the strength of wherringbone" joints of airplaw gas
turbine moving vanes taking Into consideration the creep of metals.
Sbor. at. MPI no'11:80-102 157. (NIU 11W
(C;oep of metals) (Airplanes-lIngines)
I (Gas turbines-Blades)

MAVRISHCHEV, V.S., kand. ekon. nauk, VISYULU' F.P.., kand. ekon.
nauk~ STRbKOVA, V. I . , kand . V. I.
kand. ekon. nauk% LOPATIN, N.V., kand. ekon. nauk;
SOSIN) L*M,,p kana. ekon. nalik; ZYATIKOV, Ya.M., kand. ekon.
nauk,- LYSOV, N.Ye., kand. ekon. nauk; IIEVELISKAYA, K.I.j
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V.Ya., kand. ekon. nauk
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Khiml2atsila promyshlennop proizvo(l8tva Bel,.)russll. Minskp
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