SCIENTIFIC ABSTRACT PANOV, B. S. - PANOV, D. G.

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• Collection: Scientific Abstracts
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• Sequence Number: 15
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

PANOVY B.S.
M-F.-
Fluorite of the 0 )uthweatern margin of the Donets Basin. Lit. i poi.
iskop. no.3:104,iI7 My-Je t64. (MIRA 17:11)
1. Donetskiy politekhaicheakiy institut.

PANOV, Boris Semenovich; POPRAVKO, K.A... otv. red.; ALYABIYEEV,
N.Z., red.
rFluorite in the Donets Basin) Fliucrit v Donetskom
L
Basseine. Kharlkovp Kharlkovskii gos. univ., 1965. 98 p.
(MIRA 18:12)

BUTURLINOV, N.V.; PA1,11OV, B.S.; KCBFLEV, PI.V.; KARPOV, G.le.
New data on Devonian igneous activity in the sotithwestern
margin of the Donets Basin. Dokl. AN SSSR 156 no. 4'817--
820 Je 164. (MIRA 17-.6)
1. Donetskiy politeldinicliesl:i,, institut. Predstwileno akademikom
D.S.Korzhinskim.
P-P5

Find of copper mineralization in Devonian sediments of th
southwestern margin of the'Donets Basin. Min. sbor. no.15-.331-334
161. WIPA 3-5:6)
1. Donetskiy politekhnichoskiy institut, Donetok.
(Donets Basin-Copper ores)

PANOV, B.S
Fluorite in Donets Basin Devonian sandstones. Dop. AN IMSR
no.8.-1099-1102 '163. (NUM 16: 10)
1. Donetskiy politekhnicheskiy institut. Predstavleno ukademikom
All UkrSSR N.P. Semenanko [Semenenko, M.P.).
(Donets Basin-Fluorite)

BUTURLIKOV, N.V.; PANIOV, B.S.
Igneous rocks and ore formation in the Donato Basin. 2Ap.VBe9.min.
Ob-va 88 no.4:419-429 '59. (MIRA 12:11)
1. Donetslciy industriallnyy inatitut, g. Stalino.
(Donets BaGin-Petrology)
7=

PlaqCV, B.S.
Fluorite In the wbonate formation of the southwestern bordor of f
the DDnets Basin. DAL AN SWR 147 no, 531172-1174 D 162
(~= l6s2)
1. DDnetskiy politekhnicheski7 Institut. Predstarleno alka-
dmikom N.M. Strakhovyms
(DDnets Baoin-Fluorite)

Structure ano, ore-bearing potentisl of the Ghegarnikslciy dome in
tho NikitovkA mercury deposits of the Donate Basin. :F-sp.V9.mln.ob-va
86 no.3:365-174 157. Oaju lo: 9)
1. Donetskiy industriallnyy institut, g. Stalino.
(Donets Bnain-Ores) (Donets Basin--GeologF, Strw,.tural)

,?JaiOV, B.V., kand.tekhn.nauk
Strengthening steel parts by the method of double vork hardening.
Metalloved. i term. obr. met. no.1:7-12 A 163. (MIRA 16:2)
(Stetel-Cold working)
-N -A- im, N----

RT~U~ --Li.- V.
2. US!.,R
(600)
7. Effect of the Len,vth of the Arm of Rending Moment on the C,;nceritration of the
Strain in Chamfers, Herald of l4achine Construction l7lo. 1, Jan 4;3
9.: 01 witDilation of Info-mv-A.ion of the USSR Machine and Machine Tools Industry
laozntalned in Soviet Publications. ATIO.

S/572/61/000/007/006/006
D221/D302
AUTROR: Panov, B.V., Candidate of Technical, Scienceo, Docent
TITIE-s The fatigue resistance of work hardenel:shafts
SDURCE.- Raschety na prochnost' ; teoreticheskiye i sksperimentall
nyye issledovaniya prochnosti mashinostroitel!nykh konstrak-
tsiy. Sbornik statey no.*7, 1961, 390 - 405
TEXTs The results are.reported of experiments, oarried out for re-
vealii* the relative effectiveness of through and surface work hardening
of plain shafts a's well as shafts with stress concentrations. The specimens
were made of steel 20 and tested in the 14Y - 3000 (NU-3000) machine. Some
IJdmpIBs were left without treatment* whereas the others weire subject to
lororkhardening by preliminary torsion in K - 50 machine beiyond the yield
limit and to various stresses of work hardening,T The tests correspond-
ed to r -OCT (GOST) 2660 - 45, and amounted to 5 MA10ion cycles. The maxi-
rAum, increase of fatigue strength of plain specimens was obtained after
achieving a stress of work hardening equal to 90 % of uItImate strength -In
Card 1/-,

ne fatigue resistance of
S/57 61./000/007/006/006
D221YI)302
4torsion. The Bpecimene with a ring recess were made of stisel 20 with high-
or mechanical properties. Some were left without treatmen-tv and the remain-
der.wi~re twisted to various degrees with subsequent groove turnlDg. Pur~her-
more,, two batches from steel 65P (65G) which has a higher strength and -.0-.
y were produced in untreated as we'Ll as work unhardened, and*
wer plasticit,
grooved form. The experiments demonstrate that the fat_Lgue strength of
shafts with a groove is not smaller after work har"n-ing by torsi-Ong com-
pared to plain specimens. This proves that the sensitivity of the materrial
to the undercutting is little affected by work hardening, In the caae of
workpieces in steel 65G it was less affected than in otee! 20. In addit'on.
three batches of plain specimens in the latter steel we:re prf-d-aced and fes-
ted IM the NU-3000 maohine, Their blanks were annealed, and ozae batob va,~
left untreated, whereas the second batch wag t~wisted and then tvlrned to fi-
nis'a size. The third 'ba-,%-Ich was burnished by a rollers Al! specimens were
finally subject to artif-Icial ageing. The test 4.1en indicated that the fe.-
tiVa limit of 'Untreated speo-Imens and those which were work hardened: by
twl,sting and rolling attai".d the following prnport*-C~or!i~ 100, 120 ar.-I 132%,
In addition specimens of three batcchaB Of pla47
_1 a f n
Card 2/3

SOV/129-58-10-11/14
AUTHOR: -Panov, B. V., Candidate of Technical Scienceb
TITLE: Increasing the Strength of Steel Components by Twisting
(Povysheniye prochnosti stallnykh detaley skruchivaniyem)
PERIODICAl: Metallovedeniye i Obrabotka Metallov, 1958, Nr 10)
pp 50-5 6 (USSR)
ABSTRACT; On the basis of theoretical and experimental results
the following conclusions are arrived at;
1. Work hardening of steel specimens increases the
strength, the yield point and the fatiGue stren6th even
in cases in which the stresses caused by the work
hardening are tangential ax3d the stresses due to loading
during operation are normal.
2. There is a possibility of calculating in advance the
yield point of work hardened smooth specimens by kpplying
the hypothesis of strength which reflects the influence
of tangential as well as of normal stresses.
3. Application of work hardening is most effective In the
case of soft steels; for harder steels it is more
advantageous to improve the strength by heat treatment.
The increase in strength after viork hardening by torsion
Card 112 is the same as after work hardening by rolls or shot

S/129/6'3/000/001/002./0-17
E193/E383!
AUMOR: Panov, B~V. Candidate of~Technical Sciences
TITLE: Increasing the strength- of steel parts~ by the method
of double, ifork-hardening
'PM-TODICAL: Metallovedeniye i termichesk.~Y~-obrabotka metallov:
no. 1, 19~3,1 -
TB)~.V; Mechanical' surf ace-hardening 4 e.g. by shot-peening)'
brings about an increase in the fatigue. strengt.h of metals, whereas
ng the,entire volume of it
i wo~rk-hardenin4 by deformation affecti
metal part increases 'mainly its resistance to static loads.. Th. e
object of the present investiga-Eion was to study the effect of
these treatments, applied singly and, toget r"
he on the, strength and
e e C,
fatigue properties of ste'l parts.. Stiel 15, containing 0-155,
0
0 # 370" Mn, 0-.150,1 Cu and traces of Si and annealed at 900 C, 'was
used in the first stage of the investigatioh in which the effect
of various modes of work-hardening on tho'static strength i~as
ries of test pieces Were Used. Voltune work-,
studied. Three so
hardening of the specimens in t~o first seri*es.'was affected by
plastic-deformatibn in torsionunder a stress _t~H 55 kg/mm
Card 1A

S/129/63/000/001/002/017
Increasing the strength E193/E383
surf ace-hardening was carr:~i'e'd out with a rotl-00 mm dia. profilo.'
radius 2 mm) pi-assed under" a load of .100 or,,150 k9 against the
specimen rotated on a lathe'at 1110 r.p.m., Che rate of feed of the
hardening roll being 0*08'mm/rev. When both these treatments were
applied (the so.-called "double-hardening treatment"), surface-
hardening was applied last. The specimens of the second and.third
(made of steel 15 in',the 'as-received' condition) were work-.;
hardened under a wide range of cbnditions'and then aged for 2 h
, 0
at 200 C. The various properties of specimens of.the first series,
before (figures in brackets)-and after the double-hardening tre2t",.
inent are given below: tensile yield stress
(35) and 63-3 1cg/mm
'UTS.(61-7) and 75.5 kg/mM elongation. (irr tgnsion).(21-3) and
7-5OjQ'-,. shear yield stress W.6) and 60 ks/mm shear strength
2
(6o)* and 64.z itg/mm shear straiii (190) and 900%. The hardened
and heat-treated specimens of the second and third series were
subjected to tensile and iorsion tests. The results inoicated
that in the case of parts~operating under static tensile' or shear
stresses the increase in"'the resistance to deformation brought
Card 2/11
UW1

s/l.zg/63/000/001/002/017
Increasing the strength .... C-1513/8383
about by surPace-hardening was marginal, double Wo'rk-hardening was
of doubtful value and sufficient increase in the mechanical properlio':-'~,",
ties could b6 achieved by volutito worl-i-hardeningalone. In the
second-stage of the investigation, the effect of double work-
hardening treatment on the fatigue properties of steel was studied-'
Three series of unnotched and one series of notched spec'imens were
(0. 25'-' d, 0. 12-'
used. In addition to steel 15, steel 30X (30101)
Si, 0-57',,',.Mn, 1.03050 Cr) was used. The fatigue tests were co C uc~t'l~d
iunder ben4ing-j- t-ehzvlle - and. sh car- -(torsion) stress as' . Typical res-
~"ults obtained 'fo
r unnotched specimens of steel 15, tested undrr
bending and tensile stresses, are reproduced in Fig% 2a and
respectively, thelvarious curves relating.to test pieces given the- .011
following mechanical treatinent: 1) double work-hardening;
2) surface work-hardening; 3) volume work-hardening; 4) no
-the
hardening treatment. Comlusions, a substantial increase in
maxinium, permissible stresses applied to steel,.parts operating under'
repeated loads can be attained in many cases,by proliminary,double
work-hardening; treatment of the type studied by the present author.
There are ?,,figures and 4 tables.
Card 3/4

S/129/65/000/001/002/017
Increasing the strength El 0/ E3 8 3
FiG. 2'.

1l
1-4
1 V1 I

Z
i A
I
I-

CL

CA'd 4/4
ir

PANOV, B.V., kand.tekhn.
naukl dotuent
FatigUO Strength of workhar-
no*7:390-45 I(qo~ dened roll(Irs. Rasell.na prochn.
(Steel-FatigLe) (MIRA 14:11)

1. PAIT011, - B. V.
2. USsR (600)
4- Strains and Stresses
70 Effect of the length of lover arm of object subjected to bending,
on the concentration of stresses in hollow chamfers, Vest. mash.,
33, No. 1y 1953-
J.t;
9. Monthl List of Russian Accessions, Library of Congress, . ALP~I P -1953, Uncl.

and e 14 r,- A
nC~.t- -1,17-32-5 163. - .,a:-; Tlj 117-- Arh. b2c. ,A-a L4
1. I-r)stjtut za
~n'z racla
Beograd
I - -

RADIOBIOLOGY
YUGOSIAVIA
KILIBARDA, H.; HARKOV:C, B.; ZIVANCEVIC, S. and PANOV.A... Institute of
Occupational Medicine of the Soci-aTl*i'E-W'public-;-f-dWb~i-a---Mnstitut za
medicinu rada. SRS,) Belgrade.
"Osmotic Resistance of Leukocytes Following Fractionated X-Irradiation of
Rats."
Zagreb, Arhiv za Iligijenu Rada i ToksikolEgiju, Vol 16, No 4, 1965; pp
353-356.
Abstract (English summary modified]: Whole,-body irradiation in rats exposed
to X-rays 1 r per min, 3 mA 70 kV-for 20 minutes weekly for 20 weeks was
followed by a progressive fall in osmotic resistance and longevity of
white blo6d cells. Tablep graph, 2 Soviet sind 7 Western references; ms
received 21 Jan 65#
j~ MEW
P,

KUCHEfffAYEVP V. A.; PANOV D A
ton
tM '.-.he Q'Iestion of the Cause Of the Anomalously Fast
Lodses.of Electrons from Plasmas "
in Ogra.
Report presented at the Conference onplasr.,
Stability, Culham UK r- ~
07-20 Sep 162

PANOV, D.A.,
Larvel feeding of the bream in Rybinsk Reservoir. Tru4q Inst. biol.
vodokhran. no.3:176-181 160.' (MIRA 14;3)
(Rybinsk Reservoir--Bream) (Larvae-FishesY
7~

PANOV,, D. A.: Motor Biol Sci (dine) -- "The biolopy of the young of tho
Black Sea saboon during the river period of their life". ypacc,,q, 1958.
12 pp (Kaliningrad Tech Inat of the Fish Industry and EcomrU), 135 copies
(KL, No 3, 1959, 109)

PANOV, D.A.
4W
We unity of the Block Sea oalmon w2d brook trout echools,
Nauchadol-clevystshkoly; biol.nnuki ni).1:46-48 158 (MIRA 11:8)
1, Predstavlena kafedro7 rybovodstva Moskovskogo tekhnicheskogo
instituta rybnoy promyshlennosti i Ithozyaystva Im. A.I. Hi~oyana.
(BLACK BRA-SALMON)
(CM~RNATA RIVER-TROUT)

. I PANOV , D.
Article by the Director of the Scientific Irformation Institute of the USSR
Academy of Sciences, D. Panov: "Study Yore Fully the Achievements of Sciencez
and Technology."
Pravda, March 15, 1955, page 2

PANOV D.; USHAKOV, I.
Joint coaference of the societies of operatiom research of the
U.S.A. and Ganada. Izv. AN SSSR. Tekh. kib. no.ltl98-199 Ja-F
165o (MIRA- 1824)

U63R/Nuclear Physics C-5
Abs-jour : Referat Zhur Mika, No 15, 1957, 11239
Author : Bezrukov, L.S., Panov, D.A., Timoslauk, D.V.
Inst Not Given
Title Dependence of the Transverse Cross Section of the
Reaction L17 (d, p) LiB on the Deuteron Energy in the
Interval 1.1 -- 4 Mev.
Orig Pab .1%tom. energiya, 1956, No 4, 149-150
Abstract A measurement was made of the excitation function of the
reaction LiT (d, p) LiB for 4.0-� 0.05 Mev deuterons
from the 70 cm cyclotron of the Academy of Sciences,
USSR. The yield of the reaction war. determined from the
(3 activity of the Li8. The multiply-repeating cycle of
measurements consisted of exposing the target during one
second, interruption (one second), and counting the
Card 1/2

USSR/Nuclear Physics
C-5
Abs jour Ref Zhur Fizika, No 5, 1957, 11239
activity of the Li8 for three seconds.
The excitation curve obtained has maxima at deuteron
energies of 2.0, 2-5 and 3.7 Mev.9 corresponding to the
levels of the internediate Be nucleus with energieR 18.3,
18.7 and 19.6 Mev. Data on the existence of the Be-7 le-
vel with an energy 18.3 Mev coincidg with the reaulto of
Investigations of the L17 (d, n) Be' reaction.
(Referat Zhur Fizika, 1955, 24063)

MIMI ..........

66593
I I. J 10 0 SOV/26-59-7-2/55
AUTHOR: Pan.ov, D.A., and Semashko, N.N., Moscow
TITLE: Thermonuclear Magnetic Traps
PERIODICAL: Priroda, 1959, Nr 7, pp 13-18 (USSR)
ABSTRACT: The article describes how thermonuclear reactions are
achieved and comments upon the principle of thermonit-
clear magnetic traps. In the USSR, the idea to use
a thermonuclear magnetic trap in the shape of a straight
cylinder with a longitudinal magnetic field with in-
creased amplification toward its ends was first ex-
pressed by G.I. Budker in 1953. Recently the Institut
atomnoy energii AN SSSR (I.-astitute of Atomic Power
of the AS USSR) has developed (under the guidance of
P
I.N. Golovin) a large thermonuclear magnetic trap,
the 110gra" (diagram on p l'? and photo on p 18).
It will serve for research into thermonuclear reac-
tions. In the ionic supp;y chamber of the "Ograls"
Card 1/2 injector, deuterium ions of as much as 200 kiloelec-
~y

66593
SOV/26-59-7-2/55
Thermonuclear Magnetic Txaps
tron-volts are created. The trap's chamber made of
non-magnetic steel is 1.4 m in diameter, and has se-
veral diffusion and sorption pumps. The "Ogra" is
supposed to pj2duce high-temperature plasma with a
density of 10 ions per cu cm. It will thus help
to solve the problem of accumulation and holding back
of the plasma in thermonuclear magnetic traps. There
0 -
are 4 diagrams, 1 photo, 1 graph and 2 Soviet refer-
lances.
Card 2/2

A V C
22292
S/053/61/073/004/005/007
B125 I/B201
AUTHORS: Golovin, I. N..f Artemenkov, L. I., Bogdanov, G. F.2
Panovj__Z_L_A,_, Pistunovich, V. I.,. Semashko, N. N.
~TITLE: Work.vith the the'rmonuolear installation 110grall
.PERIODICAL-.. U6pekhi fizicheskikh nauk, v~ 73, no. 4, 1961t 685-700
TEXT: The principal.data concerning the' installation 110grall were alreadii-
published in 1958 by I. V. Kurchatov, 110 nekolorykh rabotakh Instituta
atomnoy pnergii AN SSSR po upravlyayemym 'ermoyadernym reaktsiyam"
.(Atomnaya energiyh 5, 105 (1958)). Both this paper and 1. N. Golovin's
lecture in London (1959) are presupposed to be known. Pinch current
strength-an6 conditions required-for a dense plasma to accumulate in the
110grall. In PfDinch" operation, the density of plasma is made equal or
larger than f-he. (1,7,1..sity of hydrogen. -The accumulat.ion of hot plasma in
Uhe 110grall is abo ~_'all dcppndent upon the fol lowing four cross sections:
-~AZon cy, of a molecular ion H+ in hydrogen,
on cross s
(a) the. dis. 2
c*. -o.~- the. dissociatio bf-a_inolecular ion H* by
(b) the cros.9 section d
2
Card 1/6

t--: WM, -'f n -71
22292
S/053J61/073/004/005/007
rk with th
the
o
cle
r
B201
B125
rm
e
nu
a
..
/
prot-ons-, (c)'the cross section a of the charge exchang4~' of protons in
ex
hydrogen, (d) the cross rection of hydrogen iohization by protons.
aion
The values of Cr used by the authors in 19f;O had been measured by
d
N. V. Pedorenko at LFTI '(Leningrad Institule of Physics and Technology)
in 1957. For conditions in the 110gra", tbe equations for the balance of
ions and neutrons read
nav
,
0 (2,1)
_Jq,=nOnGnV8+-LnQI (2,21
The equ'ation for the pinch current reads:
2 ax I a*
Jnep 011- - P
pa2 X2 *a
2.3)
4 O
-T IF
a
n Vau
A
A
for pinch:
bhe density of plasma or hydro,,en-at, the
nnep Oil
LT* P (2,4)
eax U
JI
A VU13
Card 2/6
0p
_J
NO

2 220
B/053/61/073/004/005/0'07
Uork, with the thermonuclear... 3125/3201
and -Xj.SA*
P
q q (2,5)
no flep OJJQA .
CA*P
var,
respectively. The plasma-filled. volume in 'the 110grall amounts to
6 3
8.10 10M Fig.. . 1 shown the Drincipa-l-cross sections characterizing
the accumulation of a plasma in the 110gra". Reference is made to meas ure-
ments carried ou*t by V. A. Simonov at the 'Nauchno-issledovatellskiy
vakuumnyy institut (Vacuum Scientific Research Institute). Part 3 deals
with the ' stab*ility, the space cLrge, and 'the cooling of ions by electrons.
M.'S. Ioffe and V, G. Tellkovskiy have studied the adjustine instability
(perstanovochnaya neustoychivos't). According to 0. B. Firsov, a strong
asymmetry of the plasma may, in case of a positive azimuthal drive, lead
11o an ordered flux of ions tbrard the chamber wall. Part 4 deals .7ith
results of experiments made vith the 110grall: at the time while the
present paper val written, oQrtain parts o:~ the 110grqll emre redeuigned
with a view to #plifying the..induced flux of H+ ions, and to improving
2
Card 316

22292
S/053/61/073/004/005/007
'Work rith.the thermonuclear ... 3125/B201
the vacuum conditions. I.-G. Goncharov and Yu.. N. Dnestrovskiy have
devised a method, Pf measuring very lor, electron densities in the 110grall.
V. T. Karpukhin has developed and built an interfeiometer.operating on the
3-cm mavelength and-serving'for the measurement of the highest electron
'There are alrayo two plasma COmDonents in the chamber, a "hot"
e
one and a cold'one, the density of the cold component being considerably
higher than that of the "hot" one if the pressures of remanent gases
,
-7
-7
exceed -10
At. pressures below 10
mm Hg, the dens4ties of the
mm Eg.
tvio components become equal. The cold component has a considerably longer
life than the hot one. -The apparatus constructed by A. N.'Karkhov permits
receiving the magnetic radiation of ions in the whole snectrum.
Yu. L. Sokolov has wor 'ked out spetial spectromeiers for measuring the
energy of plasma- electrons from ultraviolet recombination radiation and
from bremsstrahltin!! in the range,of 1000--l A. ?art 5. Conclusions:
Prom experiments with the 110grall: in the case of Yeak amperages in the
trap (10-20 milliamperes) the ion motion fits well the theory of motion

of slngle particles,-and the m ar
zean free path of molecul ions is longer
than one kilometer. By,a proper cliolce of the form of the magnetic field
Card 416
2
Nm ORg Mi,;14

22292
S/053/61/073/004/005/007
Work,mith the thermonuclear... B125/B201
It is. possible .to augment the mean free path evert further, and 140
accumulate a plasma to proton densities of 1o7 cm-3. Currents of 300 to
4Mmilliamperes can be reached. If necessbLry, it is jossible, by
improving the vacuum conditions,'to, reduce the current required for a very
dense plasma to some dozen milliamperes if the energy of H+ ions is raised
2
t6 250-260 key. 'Thus, the problem of accumulation of hot plasma with a
.-density of .109'f ast ions per am3 and'evdn nore'is by no means solved'.as
9 so tar only reached the limit of those plasma
yet. Research viork ha
densities, belor, which.the ions move as non-intM~acting particles, and
above, which the hydrodynamic properties of plasma and the collective
interactions of particles make themselves noticeable. The processes
taking place in t:he 110grall have.not been oompletely clarified by experi-
ments. For example, it has' not yet been-expiained why the plasma
potential in.some variants of the experimen*,s attains dozens of kilovolts.
Various possible explanations are offered. There are 12 figures and
15 references:* 5 Soviet-bloc and 10.non~Soviet-bloc. The two inost recent
references to Enklish.language publications read as follows:
G..,F. Bo'gdan6v, b. A. Panov, N. N.'Shemasko, Life time of fast ions in
Card 5/6

t UZI' 1JPC- i9 tFIFIq t 4I'~r,~_-,~t~1-Y-~~~,~~t~~l-Ir~~~~ :- - ;' . ~ . ~r , .: - , ; , ~ , :. -- ,- -, r~ - '-, ~ -.-, -; ~ ; , .- -. , ~ ".-s ~- ~' ~ ~ , .

22292
B/053/61/073/004/005/007
'Work with the thermonuc lear: B125/B201

Ograf.J. Nucl.- Eiergy,'pa:rt C, 111, 106'( 1961); R. F. Post, R. E. Ellis

B-C. Fird, and 71. N. Rosenblut
ht Stable ,
Confinement of a high temperature
~
plasma, Phys. Rev. Lett. A, 166 (1901o).
Legend. to, Fig. 1: The most

important cross sections fill

determining the process of.

lasma accumulation in the
p
110grall cross sections
+'
2
cm
): 2, product.ion of H
2-
i h
n b
dro
e
t

S -7 ~
n
y pro
ons,
y
g
dissociatio
f H+ i
h
d
n o
n
rogen
y
h
3, Fedorenko; 4,
stma- Z' 11,74W H, -
Hamblen-Suitypan; 5, Gerjoy;
6
t
f
l
ure o
e
, cap
ectrons by T I
p,rotons; 7, dissociation of
+
H
by protons, 8
energy of
'
,
2
h
d
rogen ions
(ev).
y

1. 4f 9 10 10J
Card 6/6

ACCESSION XR: AT4025312 S/0000/63/000/000/0223/0232
AUTHORSt Rucberyayev# Yu. A.1 Panov, D. A.
TITLEs Use of electron and ion beams for the measurement of the
electric.field of the space charge of the 10gral plasma
SOURCE: Diagnostika plazmy* (Plasma diagnostics); ab. statey. Moo-
cow, Gosatomizdat, 1963, 223-232
TOPIC.TAGS: plasma research, plasma confinement, plasma sheath,
particle collision, field intensity, magnetic mirror, space charge
ABSTRACT: Two methods are described for measuring the field of
plasma-space charge. In one method the deflection of the electron
beam due to drift'in crossed electric and magnetic fields is mea-
sured, while in the other method the electric-field pickup is a beam
~of cesium ions moving in the boundary region between the plasma and
the chamber wall. The measurements were aimed ai determining the

ACCESSION NRt AT4025312
field distributions and the collective processes occurring in an
HOgra" device* The electron source used was a three-electrode gun
placed in one of the magnetic mirrors of the "Ogra," and the electron
beam receiver was a television-tube screen with low persistence.
The construction and operation of the a;paratus are briefly~described
The quantities measured were the radial distribution of the radial
component of the electric field of the-plasma space charge, the
elefctric field near the walls of the chamber, and the correlation
of the electric field near the cesium probe with the signal from the
fast-ion detector. it is concluded that the use of interaction be-
tween the probe charges and electromagnetic fields of the plasma,.
and also of atomic and nuclear collisionc with the plasma compo-
nents, yields a'variety of information on tbd plasma properties. 'An
advantage of such diagnostics is the fact that it hardly disturbs
the, investigated object. Orig. art. bass.6.figures.,:
i-ASSOCIATIONs None

SCROKIN, Yu.J.j PANCV, D.A.
Balance of tha &mmd and cowmption of foW b.-, tlis Lr,3am larvae
at various stages of their development. Dokl, 4,N SSSR 165 no,2:
454-456 N 165. (MIRA 18:21)
1. Instit-it biologii, vnutrann!:Kh vod AN SSSR. Subm.Itt,--d
Jarruary 4, 1965.

f i 017qX-11-4911 W M.Wji
V~Q
E, -Z~3
E. 137., 1 T,
R
NR; ATW!Ca~4! U
LUMOP i Paucrv V. A.
fl TLE r inves-zaga,~ion ox a iaw uanuiLy Y-me-m
o. lar hydrogen long
ecu
a
Mop f~17,w Tn~;+-itu-- A-aip- -,v enera~'-',
Lcnov Yodorada) 1-329
n
S '71 PA C' T Tli s i s a C' r 0 r, 1 Pi c- s T' s c r~ a 0-,
1:,~Ions ucvar-'aw _Q "lie p-atli:,~~.
vrd 112

gc~pw~ r-
ct end#- on--111ag=-'d0n ai=ent Aift:the-trap The subj6et
A
'headings axe: 1. Introduction. 2. Ydnetics of plasma accumulation. 3. Experi-
~:-aental conditions. 4. Meazurement of the rarge of molecular lors and attempts at
:ipasuring the iifetime of etort~ ions. yleasli~lng of' thp (ipnsl~v
Generall law governing the flUing of Ogrt irith ions. t. P asma ~ol '-ss
-)r!s -rnm the I
nEnts. E. B. Kadomtsev. Ye. P. VeI'--61--~nv, A. I.. Mikhaylo'Vr'~Ly,
none
LSZOCIATIOF i
3~MTTED: 00
01 A
IF, F-" 401v.
2
ENCLi 00 TJB CODES iq
0TV211 M

PANIOV A.,
Feeding habits of the latvae of some species of fish in Rybinsk
Reservoiri Vop. ekol, --5%157-158 162. (14IRA 16:6)
1. Institut biologii vodokhranilishch AN SSSR, Borok.
(Rybinsk Retervoir-Larvae-Fishes)
(Rybinsk Reservoir-Fishes-Food)

PANOV, D.
"On the Oripin and Periodicity in the Glaciations of the Earth," Dok. AN, 51, No. 5, 1

2'7T4
A*O
q
IIABndbook for Polar VAn' by S. D. lappo, Min Ad-
nUlstration for the Northern Sea Route,," D. G.
P"Ov, 2 yp
"Iz Vaesoyuz Geog Obahchestva" Vol I NO 3
snis is a review of a'423-page book, which Is of great
-~~Value. to myme ~&o expects to go into the Arctic re-
41bap.. Ab* teno Of geographlcal-f6atur.VB~ fauna
azicl flora of the Arctic regibn, and methods for sur-
*Ival In the Arctic. -31vas a-description of sea lee,,
bit no information regarding the -forecasting of loo
_~;,aondltlma. Glves the administrative divisims.of.

P,W)V
Nov/Doo 47
Arotio Studies
*Rev,iev of 'An Upedition CA I*ho Alrplan*'WM-N-
169.$'* D. G. Panovp 3/4 P
"1z v-s Goosraf Obehohl Vol =IX, No 6
Book contalim soientiflo kasalts of 1941 Arotio
flight. Published by GlavseimoryUt~,
A (!T 5: 5

PANOV, -.0. G.
"World Gcomorphological Chart of Ocians and Seas", report presented by
D. G. Pariov at one of the eight meetings of the Commission of Geomorphology
&nd Paleogeography iri 1948-
SO: Tram #312, 15 Aug 51

1. MNOV, D. G.
2. USSR (600)
Geology and Geography
7s Fundamental Problems of Geomoxl)holoW, Y,. K. Markov,
(Moscow, Geograpy PIT.SS, 1,9118) Ibvioviod by D. G. Panov,
Sov,, Kniga No. 31 39149.
9. ]WReport U-3081, 16 Jan, 1953. Unclassified.

,r,?* 7~
21475 PAINOV, D. G.
Sovremer.nyy-e problemy geomorfologii i~.rktikl.
Trudy Vtoropo Irsesopiz. reoCr. sllyezd,,;. I. P.M. IC,14?
s. 341 - 58, s. kart. Bibl.*IoFr: 11, INAZV
SO: Letopis' Zhtirnallnykh Statey, No. 29, Y'oskva, 1949
d

-PA
-NOV D.G.--
"On the Problem of the Submarine Canyons," Zemlevedenia, t, 2 (42)y 1948
U-1709, 27 Feb 52

PANDVi D. G.
Panov, D, G. "Landncapes of the Arctic in the Quaternary Periodt" Uchen
zaplski (Leninp
,r. COs. ped. in-t im. POkrOvskO90), Vol. VI, 1940, p, 23-91
Bi-bliog: 93 items
SO: U-3850, 16 Jime 53, (Lmtopls 'Zhurnal. Inylch Ratey, NO. 5, 194?~
a

-c,'JI"V, D. G.
Panov, D. G. "Gemorphlogy and Era-diaetrv," Uciaen. zapisla (Leninfr. Fos. ped. in-t
im. Pokrovslcogo), Vo: . -Ili, 1T;;~-Iv pq 111-5-) - ; 8 i "Cra's
SO: U-31'50, 16 june 53, (Letopis 'Zhunnal Iny-'Ji Statey, '~To. 5, 1949).

G. "The :-eo7xD tical di o'rib---t' n, d t pes cf ene-Ji rr-~-m4 c ncvements, Lichen.
an
Z~I-i id (Lenilngr. fl'os. me:'. In-t L:~. Vol. VI, lW' 51-' _aOL7:
itcl-as
SC: U-31`15:1.t 16 June 53, (LetorAr, '-~-,hurnal In-71-h -':'tatf-,y, "o. 1'.~49)-

PkNOV, D. G. PA lO/h9T97
Bbok describes Iaptev Sea and omstline.
Iliblished by Glav8ovMorPatl,,- 1947.
10/49T97,

PAIIOV, D. G.
PA 10/49T48
Wapriew of #0n the 81,-bIryakor and Mtke ftwgh the
Ar6tic Ocean' by V. IV. VIsel" D. G. Panor, I
p
wIz Y-s Geograf Obehoh" Vol LMMO No 4
:bescribee voyages of wSibiryak-or"- and "Litke* and
their. importanoe in 1,distory of Northern Sea Roate.
Pablished by GlarSe0forPati, 1946.
LdRIIIL

-pk-10/49T96--
PANOV, D. G..
48
-USSM/Ocleanology Jal/An
Sea Bottoms
"]Results oil.' Charting the Sea Bottoms of the UM
Seas," D. G. Panor, lc~ PP
"ILv--s Geol; af Obahch" Vol IYU, No 4
Seabottom, relief is of four types: (1) teotqmor-
phio; (2) 11.1thomorphio; (3) relic; (4) contemporary
acemnalative and denuded. Describes progress of
USSR in We field and future needs.
10/49"6

Sep/Oct 48
veograpby
Glaciation
"Reviev of D. M.. Kolosovis 'Problems of Early
Glaciation of the Fortbeastern Fart of USSR,
CK No 30i D. G. Panov, li pp
"It v-s Geograf Obahch" Vol LT-19-11 NO 5
C%j 'Work ma'kes good. use of available material
and much Interest is adiclel b,.,r frequent refer-
once to Kolosov's expeditionz~, Valuable ad&i-
tion to UWR geographical literature. Dis-
cusses geomorphological aspects of DWR, and
outlines some (lefinite fielas vbicU nee& further:
26
UM)Geographjv sei/o-t:48
4~
investigation.; Glavsevmorput, 1947, 167 PP, tvo
nape.
49

PANOV, D. 3. PA 26/49T5o
USSR/Geoipaphy Sep/Oc*t 48
Arotto Studies
"Review of V. 1. Akkm-atovis 'In High Ietitudes,t"
D. G. Panov, 1 p
1Z V-0 Goograf Obahch" Vol T No 5
Chronicles the experiences of a polar aviatoril
1936-1946. Purely historical account of variolas
flighte into the polar regiona. GlavBemorput,
194T.
.26/49T5o

1. PIWI,' D.' G.
2. USSR (600)
I+. Physics and Mathematics
7. Great Northern Expedition. G. V. Ymikov. (Moscow, Geography Press, 1949).
Reviewed by D. G. Panov. Sov. Kniga, No. 2, 1950.
91.1W Report U-3081, 16 Jan. 1953. Unclassified.

Pt,:-;,QV,- D. G.
28 277
,or, jj~)r~jl 1--ax-inkh -orycy SSSIR. UcyYe-,
Lo
Frob"yerin, Fyc-c)iorii i
Arkt. mor. uchl-M silcl"Trl. im. adn,,. im!:amva.
1P40, S. 138-515 - Dibllorfr: 3:',k nuzv-
SO: 11TOTIS) N,- 34
INR
- Kv

PATIOV., D. G.
25600 PAN(YV, D. G. 0 Proisk-kozhdenii I Istorii iozvitiya 0-keanov,. Vopprosy
Geografii, SB 22, 1949, s 183,204
SO; Letopis' Zhurnall NYkh Staten Vol. 34, 'ikfoskva, 1949.
iIIN
Rt-R-F:; g~
IF

PANOVt 1). 0.
25575 Obzor oenovnoy ltteratur7 Pc Vaprosu proiakhozhdaniya I Razvitiya ol-.eanicheakikh
vpadin. Vopropy Geolrafii, 18B. 121, 1949, S, 221-~2-Bibliogrs 24 NAZV.
SO: LetoPU.' Zhurnlalwkh StateY, Vol. 34., Moskva, 1949

PANDV, D.G.
Division of tho Arctla ixto physiwgeogrs;ft&Aj regions. Uch.
zsp.lejww.mo#:124:314--370 149. (MIU 9: 6)
(Artic raglome-e-Physical geography)

-VSSR/deophysics; Earthqui&es Jul/Aug 50
Literature
"Review of G. 11. Gorshkoy's Book 'Earthquakes
in the Soviet Uni on, D. G . Panov
"Iz v-s Geogra:1 Obshch" Vol LMII, No 4,
.pp 423, 424
Favorable revii.-v of subject book, which.gives
regional breakeftown of earthquakes in the USSR.
Only criticismp are that author did not give
enough attentieim to reasons for earthquakes
and to earthquakes in the Arctic.
40W

PANOV, D. G. PI, 175T73
,~w$R/Ociauogr!Vb,y;-,~Lindecoves - I Dic 50
"Submarine Laiadscapes of the World Ocean ,
D - G. Panov
"Iz v-s Geograf Obshch" Vol LMII, vo 6,
pp 582-6cq
Makes first kaown attempt to analyze factors detg
formation of 'andervater landscapes axid to .outline
-acteristics
their major types. Details main'chax
~of follovine; landscape types:~:(l)_offshore
zone of sbas and oceans; (2) landscapes of the
,-bottom of sea basins; (3)-zone of continental
shelf; (4) zorne of continental slope (oceanic
semidesarts); (5) zone'of the bottom of oceanic
basins (oc6anic cold*.deserts).
175T73

U$SR/Geophysics Geomorphology- WOV/Dec 50
Paleontology
"Reviev of 'Works (Vol 43) of the Institute of
Geography, Acaidemy of Sciences USSR Papers
on Geomorphology and Paleogeography, D. G
Panov
"IZ v-S Geograf Obshch" Vol I II., No 6,
pp 627, 628
Reviewer states that symposium contains much
neii interesting material,-on geomorphol and
paleogeog of the USSR. Some of the articles:
N. V. Dumitrashko reported on ancient glaciation
175T.2.5
USSR/Geophysics GeomorpholOgy Nov/Dec 50
(Contd)
Of the Caucasus Minor, L. G. Kaman~An described fbrm..
of micro-relief in the northern rim of the Dnepr
terraced valley, and P. V. Fedoro-r traced evolution
of mollusk fauna of the Caspian Bazin in the Quater-
nary period
17.5T25

?A iq6ro
ys~cb Sibli 1*/Apr 51
-rfte*iew.of-D.-G. Pahov's Article 'On Submarine
capes of.World Ocean,"' A. V., Zhivago
*Iz kk Nguk, Ser Geog" No 2, pp 81-84
This-artielq,,ap~earing in "Iz v-s Geograf Oshch"
~No 6, 1950, is a Ist attempt to study interaction
of hydrosphere and.sea bottom.- Discussed are
,:factors forn!ng the.submkLrine landscapes, such as
.su4Igbt., therm&l amplitudes and hydrodynamic
activity. Me article presents a progressive
stop in study of seas and oceans.
196M

PAWV D
2. UssR (600)
4e Dipolichko, I. Go
"Climate &TA land Burf-1--s Of the past."
Isv- AN SSR. Ser. 9009. No. 5. 1952
Pidoplichko, 1. 0,; X&keyvvl, pe Be Rev'ewed L7 PanOv., Do Go
9. y List of
MMt-h-k A iu-S-Slan Lccessiols
~ _, Library of Congress, Janua27 1953. Unclassified.

PAI~Oy. P.C.9 prof. -
Ocean Bottom - Pacific Ocean
Origin of the greatest depths of the Pacific Ocean. Priroda 41 no. 7, 1952.
9- M2Lt-hl-v- Li-st af- Lu-s-sian ~L-cessions, Library of Congress, Naxembsr-19.52-jptA, Uncl.

,UMR/Geophysics Floating lee Islands Feb 53
Tloating lee Islands in the Polar Basin," Prof
b. G. Panov, State U imeni Molotov
"Priroda" No 2, P13 113-114
Describes ice conditions according to information
from K. 0. Emery and R. Revelle's article "Large
Floating Islands of the Artie Ocean," which ap-
peared in the Bulletin of the Geological Society
of America, Vol 62, 1951, No 3, P 325.
244T86

PANOT9 D*G9
meotectonic OcvmentB In the North Polar region. Dokl."- SSSR 104
noj:462Jj65 s #55. (KEMA 9:2)
loRostwokly 90$ud&rltvenW universitat Jusni Y.N.Molotova. prod_
gt&vl*nO &kademikom N,K.Strakhovym.
(Artie regions-Geology, Structural)
REM
0: N 01hr M i i
12
v :9. W ri~
4 `i R, MM M-N!

PANOV, D. G.
Tectonics of the coutnil Arctic. Dokl. AN Sm 105 no-2:339-342 155.
(HOA 9 - 3)
1- R*Bt*v*kiY na-Donu gonudaretvonnyy univeraltat imenj v.m.
Molotov&. PrOdOtavlanto akademikom N.S. Shatak-Im.
WOW vagious-08816gy, Stractural)

PANOV, D*00
geomorphological outline of Antarctica, Izv, AN SSSR*Ser.
,geogi no.-6:17-35 11-D 1560' (MIaA 10: 1)
1. Rostovskiy, gosudarstvannyy universitet.
(Antarctic regions--Physical geography)

professor.
Forms of shore erosion of the 18imlyanslaqa remarvoir. Fr1roda 45
no.8:94-96 Ag 156. (KIZA 9:9)
l.Rostovskiy gosudarstvewWy universitat imani V.M.Molotova.
(TSimlyanskaya Reservolr--shore lines)
7i

PANOV, D. G.
Goomorphological contout of a hypno&T&Pbic CW'TO- IST-V202-geog-
ob-Ya 88 no.2:169-173 Mr-Ap 156. (OBA 9:8)
(Physical geoVrapby)

PAN(F, D.(4
Genetic claself1cation of the world-ocean bottoms Dokl. AN SSSR 108
no.6.-lo6l-lo64 is 156. (min 9:10)
le Roatevskiy nn Donu gosudarstrannyy universitat imeni V.M. Molotora.
Predetavleno Pkademikom N.M. Strakhovym.
(Ocean bottom)

PA p,. G. - -
Tectonics and the origin of the central Arctic Basin. Biul.MOIP.
Otd.geol. 32 no.1:21-37 Ja-F 157. (MLRA 10:5)
L1.j" (Arctic regions) .

ZHIROV, Nikolay Feodos 'yevich; -Lk44k~,
_P.~'G.j dok'or geogr. navk,
prof., nauchn. red. ; KURI.;rCES, 3.11.) red.
(Atlantis; main problems of studies on Atlantis] Atlantida;
osnovnye problenW atlantologii. Moskva, Mlysl , ) 1964. 430 P.
(11,111A 17:9)
Z
Rk
-a "AM V
N 0.1~1_;-,-_,
NO
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MR
V
NEI

V .ji
AU THOR PANOV 1). G. 20-1-43/54
TITLE --09rT&T-n-P_eouliarities in the Tectonics of the
Bordering Parts of the Pacific Plat'form.
(Nekotoryyaosobennosti tektoniki krayevykh chastey
tikhookeaziskoy platformy.- Russian)
PERIODICAL Doklady Akademii Nauk SSSR 1957, Vol 1159 Nr 1v
pp 157-160 (USSR)
ABSTRACT According to a current opinion the major part of
the bottom of the Pacific lying outside the andesite
line forms a large plateau. The study of the relief
of the bottom of the Pacific during recent years
disclosed many of its peculiarities. Shatskiy showed
that the exterior contours of the craters are deter-
mined by straight or slightly-curved lines of the
extensive fractures of the earth's crust. Their in-
dividual sections in the bordering part of the
craters form a number of exterior and interior
,angles with characteristic varied conditions of the
relation between the plateau and fold formations.
The Pacific plateau is in the west bordered by a
broad belt of recent geosynclinal seas and accompany-
ing islande and by the frontal deflections of the dee-
CARD 1/3 peat oceanic trenches. The andesite line coinoides in

20-1-43/51+
Certain Peculiarities In tht., teotonios of the
Bordering Parts of the Pacific Platform.
CARD 2/3
position with the outer boundary of the geosynclinal
region in the west and runs alo-ag the coasts of North
and South America. Recent data on the morphology of
the abyssal oceanic trenches indicate their great
similarity. It is known that an anticlinal elevation
of the bottom of the ocean runs along the cutside
border of the trench, parallel to it. It is accompanied
by lines of fractures,..and a system of underwater moun-
tains of volcanic origin..gigh SeIBMism and the existen-
ce of reservoirs of deep-fooal earthquakes indicate
that*the oceanic abyssal trenches belong to the lines
of deep fractures of the earthts crust of a type known
from deep ruptures of the continental surface. The
boundaries of the Pacific plateau like those of con-
tinental plateaus have cornered contours with interior
and exterior corners. Among the exterior corners the
following, which are morphologically and structurally
beat known, can be separated:
1. the Aleuthian-Kanobatka; 2. the Karolinian;
3. the Central American exterior -orner. In the region
of the adjoining continent an active volcanism exists.
The signs of a fresh submersion may easily be connected

20-1-43/54
Certain Peculiarities in the Tectonics of the
Bordering Parts of the Pacific Platform.
with the conception of the submersion of the entire
Pacific platform in the Cainozoic. To the interior
corners belongs the corner formed by the projection of
fold formations in the region of the Fidshi and Samoa
islands. Thesd formations belong to the Australian
orogeny which abruptly changes in extension here. The
boundary of the platform is indicated here by the abyssal
trenches of Tonga-Kermadek with the concomitant fractures.
In the north the boundary is formed by -the andesite line.
The data given here give rise to the assumption thit the
rules governing the relation between platform- and fold-
formations, determined by of the sea. Shatskiy, cab be
extended to the platforms of the bottom.
(2 Illustrations, 9 Slavic references)
ASSOCIATION: Rostov-na-Donu State University.
(Rostovskiy na Donu gosudarstvennyy univereitet.-Russian)
PRESENJED BY: Shatskiy, N. S., Academician, DiRcember-25
1956
SU314ITTED: ,
6.8-56
AVAILABLE: Library of Congreau.
CARD 3/3

2h656-65 Ev-1 (1) GW
ACCESSICN INIR. AP4049995 E-1/001 1/134,100O./Of-7 /010',;" 910-1
4~
.-AUTHOR- Panov, D.G.
TrTrl,'F-
R(l] TIZ(-V- )Q qczqf..~ 17,
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HASE I

OOK EXPLOITATION

64
Geograficheskoye obshc'hestvo SSSR
Antarktika; materialy po istorii, issledovaniya i po fizicheskoy
geografii. (The Antarctic; Materials on the History of its
Explpration'and Physical Geography) Moscow, Geografgiz, 1958.
445 p. 5,000 copies printed.
Resp. Eds.: Pavlovskiy, Yd. N., Academician; Kalesnik, S. V.,
Corresponding Member of the USSR Academy of Sciences; Ed.:
Grishina, L. I.; Tech. Ed.: Gleykh, D. A.; Map Ed.:
Kiseleva, Z. A.
PURPOSE! The book, written-in a semi-popular style, is intended
kor, the large circle of geographers interested in the Antarctic
region.
CArd l/ 8

The Antarctic; Materials on the History (Cont.) 464
COVERAGE: The present volume, sponsored by the Geographical Society
of the USSR, is a collection of articles authored by several
geographers summarizing up to date information on the Antarctic
region. It provides an account of exploration and discovery
since the first Russian expedition into the Antarctic in 1819,
and describes the region's geological and geomorphological
structure, glaciation processes, and the water currents of the
south polar seas. The last chapter contains a glossary of
Antarctic place names which is appearing in Soviet literature
for the first time. The book is profusely illustrated with
diagrams, photographs, and maps.
TABLE OF
CONTENTS:
Editor's,Note
Card 2/8
3

The Antarctic; Materials on the History (Cont.) 464
Shvede, Ye. Ye. Discovery,of Antarctica by Russian Navigators
in 1819-1821
Introduction
Preparation for
General plan of
Scientific results
expedition
5
5
this expddition 6
the expedition 30
of the first Russian Antarctic
43
An account is given of the first Russian Antarctic expedition and
the discovery of the Antarctic Continent by Bellinsgauzen and
Lazarev. Personnel, equipment, preparations for the trip, the
plan of the expedition, navigation in the Antarctic waters and
discoveries are described in detail. The hydrographic,
cartographic, oceanographic, clithatological and physical
geographic observations carried on by the expedition are commexited
on in brief.
Card 3/8

The Antarctic; Materials on the History (Cont.) 464
Aleyner, A. Z. Basic*Stages in the Geographic Exploration of
the Antarctic 54
Discoveries along the Antarctic coast in the XIX century 54
Studies of the. antArc-:--ic by land and sea-during the first
quarter of the! XX century 66
Latest studies in tl4e Antarctic by land, sea and from the
air 78
Bibliography 90
The author pr ovides brief accounts of the various expeditions,
Almost exclusively f-oreign, into the Antarctic from lk9 to 1954
and mentions the different bases established.
Aleyner, A. Z. History of the cartography of the Antarctic and
the Extent of its Cartographic Coverage 95
Cartographic representations of southern polar regions prior
to the discovery of Antarctica by the Bellinsgauzen-Lazarev
Russian expedition of 1819-1821 95
Card 4/8

The Antarctic; Materials on the History (Cont.) 464
Psnov, D. G. Geomorphological Characteristics of the Antarctic
237
General-description of Antarctic relief 237
Geomorphological regions and types of relief in the
Antarctic 255
Conclusion-$ regarding the geomorphological structure of
the Antarctic region 281
Bibliograp~y' 285
The author depcribes the geomorphological structure of the Antar~tic
region, i.e. the Antarctic Continent, the antarctic and subantarctic
islands, and the ocean floor between the continent and the islands.
Panov, D. G. Current placiation in the Antarctic 288
Fwa rZrg-in the current development of glaciation in the
Antarctic 289
:Types of ice formati-ons-in-the Antarctic 293
Card 6/8

The Antarctic; Materials on the History-(Cont.) 461
Brief description of the areas of current glaciation in the
Antarc~ic 298
Bi~liography 317
The author discusses the types of ice formations and the background
conditions and factors In the current glaciation of the Antarctic.
At present only an estimated 0.02% of tfie surface of the Antarctic
Continent is ice f5ee, and together with shelf ice it covers an area
of 13.5 million km. The Antarctic region compri6ts 87% of the total
glaciated land surface of the Earth and 85% of its total glaciated
area,
Buynitskiy, V. Kh. Waters and Ice Formations of the Antarctic 320
Waters 320
Ice formations 356
Extent of the ice cover in diffetent parts of the Antarctic 393
Bibliography 405
Card 7/8

PANOV, D. G.
Genetic typos of islands. Wauch.dokl.vys.zh)-.olV; geol.-goog.rmuki
n0-1:34-41 '58. (MIRA 12:2)
1. Rostovskiy universitet, geologo-geograficheskiy fakulltet,
kafedra fizichookoy geografii.
Uslanda)

3(.7)
AUTHORS: Panov, D. G., Malik, S. A. SOV/50-58-12-17/20
TITLE: A Useful Help (Tsennoye posobiye)
PERIODICAL: Meteorologiya i gidrologiya, ig5a, Nr 12, P 51 -5171USSR)
ABSTRACT: The first part of the "Kratkaya istorioheakaya spravka po
razvitiyagidrometeosluthby na Severnom Kavkaze (i amezhnykh s
nim-rayonov, vkhodyashchikh v obsluzhivayemuyu SK UGMS
terr:Utoriyu)" (A short historical information on the develop-
ment of the hydrometeorological service in the Northern
Caucasus (and the adjacent districts within the competence of
the SK UGMS)) is discussed. SK UGMS (Severo-Kavkazakoye Uprav-
leniya giarometeorologicheakoy bluzhby - Northern Cau(rasus
Administration of the Hydrometeorological Service) pub-
lished the information Imentioned in its Infoftatsionnyy
sborAik (ttformation compilation)t Nr 3 (21)t 1950. Hitherto
& summary on the history of the service under review in the
Northern Caucasus, the lower Don and Volga has been I'acking,.
It was very necessary since it contains important data on the
darelopment of hydrology, meteorology, and-climatology of the
area menti-oned. The resea. of the Kafedra fizichookoy geo-
Card 1/2 qrafii, Roatovskiy n/D gosudari3tyennyy,universitat

A Us.eful Help SOV/50-58-12-17/20
(Chair of Physical Geography of the Rostov -cm LAM10 -if-,
State University) hope for a successful conclusion of this
valuable work. A. F. Belyayev one of the veterans of the
service in the district mentioned has given particularly
valuable assistance for this work.
Card 2/2

AUTHOR: Panov, D.G. SOV-11-58-9-6/14
TITLE: The Types of Plutonic Breaks on the Bottom of Oceans (TiDy
glubinnykh razlomov na dne okeenov)
PERIODICAL: Tzvestiyn Akademii nauk SSSR, Seriya geologiohesknya, 1058,
Nr 9, pp 84-86 (1!99R)
ABSTRACT: Citing -numerous Soviet and U.S. geologists, the author finds
that plutonic breaks on ocean bottoms played an important role
in the formation of different structures in the different
oceanic basins.
There are 22 references, 15 of which are Soviet and 7 American.
ASSOCIATION: Rostovskiy n/D gosudarstvennyy universitet (The Rostov-on-Don
State University)
SUBMITTED: February 6, 1958
1. Oceanogrgphy 2. Ocean botton--Geology
Card 1/1

sov/16g-59-7-6807
Translation from: Referativnyy zhurnal, Geofizika, 1959, Nr 7, p 42 (USSR)
AUTHOR: Panov, D.G.
TIM: The Structure and the Neotectonic Development of the IOce
Floors
PERIODICAL- Uch. zap.,Rostovsk.-n./D un-ta, 1958, Vol 55, pp 285 - 307
ABSTRACT: The author distinguishes the fundamental types of structures of
ocean floors as follows: 1) the marginal continental type,
embracing the continental half; 2) the continental slope
characterized by a sharp dipping of the base and increase in the
thickness of the loose surface deposits (up to 3 km); 3) the
oceanic ranges, subdivided into.- a) fault-block ranges or vaulted
ranges within the boundaries of platforms), b) geosyncline ranges
(caused by recent folding, very much dissected, seismically active,
showing recent volcanism); 4) oceanic plateaus, the structure of
which comprises a cover of loose deposits of a thickness up to
500 - 700 m upon the granitic sub-structure or upon volcanic rocks;
5) oceanic platforms occurring in the main in depths of more than
Card 1/3 4,000 - 5,000 m, show two types: a) platforms having a thick layer

sov/169-59-7-680*1
The Structure and the Neotectonic Development of the Ocean Floors
(up to 2,500 m) of loose deposits (abyssal oceanic accumulative plains),
b) platforms having a less thick layer (up to 400 m) of loose deposits
(dissected abyssal oceanic plains). The former formations are characteristic
for the zones of recent submersion of the platform base, which was accompanied
by an active accumulation, and the latter characterizes the more steady zones
of the floor, which are subject in the course of the tectonic evolution to
intense breaking down, accompanied by the development of active volcanism;
6) the abyssal oceanic troughs are characterized by considerable variations in
the thickness of the loose deposits (from 5GO m up to 1-0 km) and by the great
depth (20 - 29 km) of the Mohorovicie interface. The difference in the depth
of occurrence of the Mohurovicic interface beneath the continents (25 - 80 km)
and the oceans (8-5 - 12 km) is a fundamental demonstration of the difference
between the continental and oceanic structures. The present differences in
the structure of the earth's crust beneath the continents and oceans are not
age-long in the author's opinion, but caused by the evolution process, having
different directions, of the homogeneous "granitic" crust of earth, Breaks on
a planetary scale develop on the floor of the ocean under the effect of the
Card 2/3

sov/169-59-7-6807
The Structure and the Neotectonic Development of the Ocean Floors
neotectonic movements. The wide-spread evolution of plane-crest mountains
points to the recent sinking of the oceanis floor. The morphological
features of the abyssal oceanic grooves testify their recent immersion. The
similarity of the neotectonic evolution of the ocean floor and the continents,
manifested in the presence of sections having different'degrees of mobility
and different directions of movement, distinctly points to the similarity of
their structure. The division into "primary" and "secondary" oceans is devoid
of substance: the ascendent evolution of the continent relief and the descen-
ding evolution of the ocean floor indicate tho ganeral prooo,%8 of evolution
in tha structure of the globe, which is accompanied by the equilibration on
accotrat of the displacement of the subcrustal masses. Bibl. 46 titles,
V.F. Kanayev
Card 3/3
7Y;-

RANOV. D.G.
Age of the Pacific Ocean. Hauch.dold.vys.shkoly; geol.-geog.
naWd no.2:3-9 '59. (MIRA 12:8)
1. Rostovskiy-na-Donu univerBitet, geograficheskiy fakul'tet,
kafedra fizichaskoy V ografti.
(Pacif ic Ocean)

PAW V, -D.. G. ~
Morphological structure of the central part of the floor of the
Pacific Ocean. Dokl.AN BSSR 3 no.2:66-69 F 159.
(MIRA 12:5)
1. Predstavlano, akademikon AN BSSR K.I.Lukashevym.
.(Pacific Ocean)
.(Submarine geology)

PANOV, D.G., prof.
Causes of different distribution of dry land in Arctic and
Antarctic regions. Inform. biul. Sov. antark. eksp. no.9:5-8
'59 (MIRA 13:3)
1. Rostovskiy-na-Bonu gosudarstvennyy universitet.
(Arctic regions--Geology, Structural)
(Antarctic regions--Geology, Structural)