SCIENTIFIC ABSTRACT PUZYR, V. - PUZYREV, S. A.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R001343720002-9
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: December 30, 2016
• Document Release Date: June 19, 2000
• Sequence Number: 2
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT


-GIDALI, G.; PUZYRI, V.
Striving for over-all mechanization. Mor. flot 22 no.2:17
F 162. (KRA 15:4)
Predsedatell pervichnoy organizatsii Nauchno-tekhnichaskogo
obshchestva vodnogo transporta (for Gidall). 2. Zamestitell
predsedatelya pervichnoy organizataii Nauchno-tekhnicheskogo

ZHOLOBOVA, M. (Rostov-na-Donu); SIICIIEGOLE-V, 14. (Rostov-na-Uorm); BRODSKIY,
A. (Kiyev); BARANENKO, S.; SU~BOTIN, G.; BASH14aOV, V.; KOVALEVA,
M.; GEF#%Rj-V.; YEGOHIYEVA, A., Vand.geograf.naukI,_fUZYR', V.;
GOLID, M. (g.Baku)
Readers' letters. NTO 4 no.1:26,27,29,41,50,56 Ja 16z.
(MIRA 15:1)
.1. Predsedatel' soveta nauchno-tekhnicheskogo obshcbestva Ukrainskogo
filiala Vsesoyuznogo nauchno-issledovatel"skogo instituta gazovoy
promysblennosti (for Baranenko). 2. Direktor Umskogo Doma tekhniki
nauchno-tekhnicheskikh obshchestv (for Sutbotin). 3. Uchenyy
sekretari Leningradskogo oblastnogo pravleniya nauchno-tekhnicheskogo
obshchestva energeticheskoy promyshlennosti (for Germer). 4. Zame-
stitel' predsedatelya Leningradskogo oblastnogo pravleniya nauchno-
tekhnicheskoCo gornogo obshchestva (for Yegor'yeva). 5. Zamestitel'
predsedatelya Latviyskogo basseynovogo pravleniya Nauchno-
tekhnicheskogo obshchestva vodnogo transporta (for Puzyr').
(Technological innovations)

PUZMTSKIY, S.S.
Participation of trade-union organizations in planning
geophysical operations. Razved. i okh..nedr 26 no.7:58
ji 6o. (MIRA 15:7)
1. Yakuts4ya TSentralInaya kompleksnaya geofizicheskaya
ekspeditsiya.
(Yakutia~-Prospecting--.Geophysica1 methods)
(Trade unions)

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S/048/60/024/03/01/019
Boo6/BO14
-_9~. 6POO
AUTHORSs Dzhelepov, B. 5.9 Ivanov, R. B., Nedovesov. V& Gg&.
Puzynovi-EE7=u. T.
TITLEa Alpha Emission of U233
ry _7F
PERIODICALs Izvestiya Akademii nauk SSSR. Seriya fizicheskaya, 1960,
Vol. 24, No- 39 pp. 258-260
TEXTs The article under review was read at the Tenth All-Union Confer-
ence on Nuclear Spectroscopy (Moscow,, January 19 - 27. 1960-). The alpha
emission of U2.?,? was measured in 6 series by means of an a-spectrometer
(two different u233 sources). A brief description of.results is given.
The spectral region between 4-7 and 4.8 Mev (first series) is illustrated
in Fig. 1, the region between 4.6 and 4-75 Hev (fifth series) in Fig. 2,
and that between 4-4 and 4.7 Mev (sixth series) in Fig. 3. In addition to
,the knovin lines, transitions at 29, 72, 126, and 195 kev were detected.
Besides, a particularly indistinct peak was found at 145 kev (intensity
tSO.01 per cent). All results are summarized in a table.
Card 1/3

Alpha Emission of U233 S/048/60/024/03/01/019
B0061BO14
energy of the Th2291evel intensity of characteristics of prohibition
I~eyl a-transitions the Th2291evel F

0 83 5/2 5/2 + 1.9
29t2 0.48tO.O8 5/2 5/2 200
42
3 14.6 5/2 7/2 + 5-8
;
72-2 0.28t0.06 5/2 7/2 1010
97 1-5 5/2 9/2 24
126t2 0.08tO.O2 5/2 9/2 280
(145t5) 40.01, - 7/2 1700
163�2 0.06�0.02 5/2 11/2 + 200
195�3 0-015tO-95 5/2 11/2 500
(240t5) ~
~C0-004 (5/2) (13/2 1200
316�2 0.033tO.oo6 3/2 +
~ 30
(364t5) 1: 0 - 004 ~5/2 130
The level scheme of the decay U233-),Th229 is shown in Fig. 4. The
authors thank L. L. GoIl din and G. 1. Novikova for supplying the u233

Card 2/3

Alpha Emission of U233 S/04 60/O24/03,.-/"'./r'1`
BO06YI1014
source, L. K..-Peker for his discussions, V. A._BgjjAkajr-and V-X~-
Delayev for their assistance. There are figures, 1 table, and 3
refi"r-encesq 2 of which are Soviet.
ASSOCIATION: Radiyevyy institut im. V. G. Xhlopina Akademii nauk SSSR
(Radium Institute imeni V. G~ Khlopin--of the Academy of
ScienceBq USSR)
Card 3/3

ROZAPTSIV, Ye.S.; PUZYREV, V.N.
"Effect of the time elemont in mining protective seams* by N.I.
Zhiz1ov, D.V.Dorokhov* Reviewed br I.S.Rozantsev, V.N.Puzyrev.
Ugoll Ukr. 4 no.1:43-44 Ja '60. (MIU 13-'5)
1. Vostochny7.nauchno-ionledovatellskiy institut Po
besopasnosti rabot v gornoy pormyshlonnosti.
(Coal mines and rdning-Safety measures)
(ZhIzlov. N.I.)
(Dorokhov, D.V.)

0
11

PUZTRXV. Aleksandr VROIllwevich,knadidat tekhalchookikh aauk; SORCKIN,
A 6r t4khalcheakikh sauk. redektor; VMLKINA. A.A.,
redaktor; KtRSAR(KA, N.A., tekhaicheskiy redaktor.
Clixaminaties and adjustment of ventilating equipment Is eater-
prises] Issledewaale 1 naladka vestillateleavWkh ustmaevok as,
predprilatilakh. Moskva. Isd-ve TTaNS prefisdat. 1955.141 pe
(ventilation) (Mw 9:5)

ZAPRUDANOVA, Varvara Pavlovna. Prinimali uchastiye: KASHIN, V.A.p
nauchn. sotr.; MAIM, A.F., nauchn. sotr.; SOIDVIYEV,
11.V., retsenzent; USFENSKIY, S.D.p retsenzent;.FUZYREVp
A.V., retsenzent; SHMNGART, M.D., red.
[Fundmentals of safety engineering and fire prevention
in textile enterprises] Osnovy tekhniki bezopasnosti i
protivopozharnoi tekhniki na tekstillnykh predpriiatiiakh.
Moskva, Gizlegprom, 1963. 202 p. (MIRA 17:6)
1. Ivanovskiy institut okhrany truda Vsesoyuznogo tsent-
rallnogo soveta profsoyuzov (for Kashin, Kutanin)*

KUTANIU, ikaatoliy Pedorovich; KASHIN, Vatelar Aleksandrovich; SMIRNOV,
Gennadiy Nikolayevich; DMITRIUVSKATA. Nina PetroTnaL_PUZYR1V,_
,LV.,_kand.tekhn.n&uk, red.; SORMIX, I.S., reteenzent;
SHUB, L.S.. retsenzalat; TMITSKATA, Te.X., red.; YrNOGRADOTA,
G.A., tekhn.red.
[Safety measures In dying and finishing shops] Takhnika bes-
opannosti v krasilino-otdolochnon proizvodetvo. By A.Y.Kutaniu
and others. Y4skva, I2d-vo uauehno-tekhn.lit-ry RSFM 1961,
147 p. (mm 14:12)
(Textile itdustry--Safety measures)

AUTHORs Puzyrovp B.9 (Tartu, E3tonian SSR) SOVI/107-58-2-13/32
TITLE: Manufacturing a Frame for Kinescopes (Izgotovleniye ramkl-
obramleniya dlya kineskopov)
PERIODICAL: Radio, 1958, Nr 2, p 23 (USSR)
ABSTRACT: The author recommends a method of manufacturing a cardboard
frame for a kinescope, which is to be installed into a TV
set which formerly had a larger picture tubeq and where it
is necessary to cover.up the additional space. A 1o5 mm
thick piece of cardboard is bent and cut to fit.
There is one diagram.
1. Television re--eivers--Equipment 2. Materials--Design
Card 1/1

L 2896o-66 1. EWT(d)/FSS-2/UC(k)-2. RBAST/GW/WS-2
ACC M, AP6019108 SOURCE CODEt UR/O_-A4/65/00O/0O4/0058AW
AUTHOR: PuzyrevL_j. M*
ORGi none
TITIA's." Experience in international spacs radio co-nication
SOURCE: Zemlya i vselennaya, noo* 4, 1965, 58-62
TOPIC TAGS: spaco commifiication, radio wave propagation, radio communication, moon,-:
radio telescope, artificial Earth satellite, radio wave absorption/Eeho-2 artificial-
Earth satellite
The article cited below discusses thd-expefiminC~ n space com-
ABST RACT:
the oint ei
-.mijnication carried out in February-March 1964through Eforts
.~'..of -the.Soviet Academy of Sciences, Jodrell Bank Observatory and N
Among the topics discussed are: the.propagation of very short waves,
-the Echo 2 satellite the possibilities of using.Echo'2 for space radio
communication, the tVansmitter at Jodrell Bank, the receiver at Zimenkakh,
tracking of Echo 2, and types of space radio communication. Particular
attention is.given to-the advantages and disadvantages of.using.the moon
.'rather than Echo 2 in space communication. Amung the advantages of:
~:transmitting of ultrashort waves via the moon is that'the radio contact
".c.an last several hours,.rather than only 12-20 minutes'.because the =Don
.,moves through the sky more slowly than_the*satellite*~ -Horeover,_the..__slowj
1/2'
ar d
~

--L 2go6o-66
ACC NR, Ap6o19108
motion of the moon simplifies po'intinig' of instruments and tracking.- For.
'example, in cloudless weather the pointing of the radio telescopeat the
Imoon at Zimenkakh is accomplished simply by means of a television appa-
ifratus whose camera tube is set in the facus,of the radio telescope dish.
IThe lunar image is transmitted to a kinescope mounted in the control
I f
.panel of the radio telescope. jn addition, the angular dimensions o
Ithe moon exceed by a factor greater than 500 the angular dimensions of
'Echo 2. Therefore, inthe case'of a constant angular directivity-of the -1
the ti~afiimittlng antenna (10.8) the effective reflecting surface of thei
,.moon is approximately 250;000 times greater than the effective reflecting'l
surface of the satellite. Among the shortcomingsof using the moon in
,comparison with the Echo satellite is,the far greater distance to the
.moon, which causes the attenuation of radio waves on the earth-moon-eatth
.path Eo be considerably greater than for the satellite. Moreover, the
junar surface'is.not electrically conductive and therefore the coef-'
Ificient of reflection of radio waves from its-surface is considerably'
less than from the metal surface of the.satellite. The experiments re-~'
,vealed that whereas the coefficient of reflection of a 1.85-m wave'fron
,the Echo 2-is 0.7-0.8, that is, if,70-80%.of.the energy is reflected'~
,and the remaining part'is scattered and is' absorbed insignificantly,~-;,-.-1~
Athe coefficient of refleiction of radio waves from the moon is~'only 0.05-
0.07, that is,- more than 907s of the energy of the'radio waves is,abs-
sorbed and scattered by the lunar surface.,' Since-the moon experiences,--..
Jibration t SIL nal reflected from the moonAk.extremely.unstable, Orige art* hast
R5
,U , . S A
CODE:
2 SUHK DATE: none ~8~
g
Ord

elm=
/0
L 6529 -6 9WT(d)/mff(l)/FS(v)-3/F3S-2 TT/AST/GW
ACCESSION NRs AP5=55 M/CR93/65/00
629.1".28&U.39
AVMORSs off
Belik 'ch. V. BaWml V -48UP1,50011
YerukWl-m Tell
11 IU M PU309T 1. ill Ra T,
U. ~unili*.-H.-V po
vi
A. G.;%Che V
ff 5 V
TITIE: The results of an experiment on radio coprazni----~U via fgcbo 20 WA MW
moon at a frequency of 262.4, megacycles between the observatories oT-J;&*Il Ba0k,
and ZimnkJL
SOURCEt *Kossiches" iseledovanirep T. 3, no. 4P 1965Y (d$-Q9
TOPIC TAGSm moon, satellite cQzmmLGaUQn7isd1o tolesoope, radio trammaiLsolomp
satellite tiracking, scientific research coordination / Jodrell Bank radio tele-
scope, Zimenki observatory radio telescope, BESM 2 electronic computer
ABSW=t Durift Irobivary4brob 1964 the AnedoW of Memo of the SM, MA
of the WA, and Us General Past Offies Depsirtmisat of Great MrItain sawnsted an
experiment to establish one-way radio eamowleation at 162.4 separdoo w" Vo
passive satellite elabo-20 and ths now. Bobo me wed for 34 somminUm
CWd
I F~ I

L 65295-65
ACCEMION 11Rt AM1255
tests of 10-15 minutes (the time i6terval permitted by Echols orbit), and *the
moon was used for 15 tent runs between the Echo tests. The transmitting equip-
ment at Jodrell Bank and the receiving-unit of the Zimanki Observatory are do-
scribed In detail. Echo orbit information furnished by NASA, visual observationsp
and radio tracking data from fixed stations were fed to a BES11-2 electronic cal-
culator which provided programed tracking control. The received signal exhibited
strong fluctuations separable into two periods: 1) a 1-2 minute fluctuation so-
acciated with Echo-2 distortion from a sphere pnd vith tracking orrors; 2) a 3-10
second period associated with small aurface irregularities. The rapid fluctua-
tions varied with each testa Voice sigm1s, slowed by a factor of S. were barely
intelligible. Telegraph, teletype, anti photofaceimile tranardsolon, in general,
were unsatisfactory, but in periods of high signal-to-noise ratios Intelligible
mossages were received. The won transmissions we" not ap clear but did furnish
scientific information. Unexpected transmission losses Included 3-5 db for poles-.
ization losses and 1-2 db for wimown causes. The international ccapm%Um was
excellent, vith the Soviet submitting a coqAote report. Offers fw tw4hor cew
operation have bo*n eidonded. Orig. art. bass 3 tables, 7 flvwwp ~M 4 for-
Mulas.
ASSOCIATIONe none
suBHrMDt 18Apr65 &MCL# 00 M 00M# W
90 RAF SOWS 000, 1 OU

I
i-: ~ I'-:-,I-I- T -,T
" -1. . .

.:,,-i1T(d)/FSS-2/FEC(k)-2 RB/AST/G1W'/WS-2
SOU,11CE CODE: UR/0384/65/WO/004/005-3/0
APW19108
AUT ',T
.1OR: Iluz-j--ov, 1. 1-16
ORG: nono
TITWI: E)Terience in international space radio com=--cation
50MICE: Zomlya: i vsolonnwfa . no. 4. 1963, 58-62
TOPIC TAGS: space cotmi cation, radio vmv-o propagation, radio cormanication, moon,
radio telescope, artikicial Earth satallite, radlo'wava absorption/Echo-2 artificial,'
Earth satellite
ABSTRACT: The article cited below discusses the expef imhf'fi space COM-
m6nication carried out in February-March 196/4 thr.ough the joint efforts
of the Soviet Academy of Scienfas, Jodrell Bafik-Observatory and NASA_
Ami~n gthe topics discussed are: the propagation of very short waves,
-the Echo 2 satellite the possibilities of using Echo 2 for space radio
co=unicr.tion, the tYansmitter at Jodrell Bank, the receiver at Zimenkakh,
.,trackin- of Echo 2, and types of space radio communication. Particular
attention is given to the,advantages and disadvantages of.Using the moon V/
,r.ather than Echo 2 in space cc munication. Amutig the advantages of
,-transmitting of ultrashort waves via the moon is that the radio contact
*:can last several hours,.'rather than only 12-20 minutes, because the moon
--Dves through the sky more slowly than.the satellite.: Moreover,. the. a
Card

ACC 14i~, AP:01.91fil,
motion of Lite moor. almpLifies pointing of instruments anfal tracking. For
lexample, in cloudless weather tile pointing of the radio telescope at the
'moon at Zimenkakh is accomplished simply by ranans of a
~ratua whose camera tube is set in the foc-u-3 of Lhf-, ra,~ic teles~-:ope
iThe lunar image is transmitted to a kinescope mounue6 in the c,introl
panel of the radio telescope. In addition, the nngul.ar ditriensions of
~the moon exceed by a fRct:or greal."er thitj 500 the ungitkir di5tien'tons 01
.'r,cho 2. Therefore. in the case of 4 c ar directivity of tile 1
otistant anaul
tife transmitting antenna (10.8) tile effective reflecting surface of th e
.moon in approximately 250,000 times greater than the effective reflectinst
surface of the satellite, Among the shortcomings of utiing, the moon in
t
comparison with the Echo satellite ia the for greater distance to the
moon, which causes the attenuation of radif) waves on thti

greatcr than [or ti ace I lite. Zkm.,cj~,cr, the
Yath to bo c,,;;Wzi1dera1,,1v L
ilunar surface is not electrically conductive and therefore the coef-
;ficient of reflection of radio waves from its surface is considerably
than from the metal surface of tile satellite, The experinenrs re-
vealed that Wheren.3 tile coefficient of reflection of a 1.85-m wavo from
.,the Echo 2 is 0.7-0.8, that Is, if 70-80% of the energy is reflected
the remaining part ia 5cattered and is absorbed insignificantly,
,ithe coefficient of reflection of radio waves from the moon ig i1aly 0-05-
.0.07, that is, more than 90% of Lite energy of tile radio waves iii 112-
and scattered by the lunar surface. Since the moon expc-riences
libration, ti Si nal ref lee ted f rom tile moon is extreately. unstable. Orj-r,.
(3
IL art. has:
zu, 22 S-U124 DIWE't norto A

Ilk?
FUZYREV, N.N.
Use of the tangent fo?=,]A in the solution of some probleup of goo-
metrical seismology. Goal, i geofiz, no.1l.-8&-94 t62. (MIRA 16:3)
1. Institut geologii i geofiziki Sibirskogo otdoleniya AN SSSRY
'Novosibirsk.
(Seismology)

U,

USSR7 cop s1dr- Physics of the Earth FD-1724
Card 1/1 Pub. 115-12/12
Author Puzyrev, N. N.
Title On I. S. Berzon's and A. M. Yepinatlyevals review of the article
'IMultiple-Reflected-Refracted Waves as a Factor Lowering the Quality
of Seismic Materials on the Russian Platform", by A. K. Urupov and
L. A. Ryabinkin
Periodical Izv. AN SSSR, Ser. geofiz., 190-191, Mar-Apr 1955
Abstract The author defends the article of Urupov and Ryabinkin against the
criticisms of Berzon and Yepiantlyeva. He cites a subsequent report
by Urupov in which the latter admitted some minor errors in his orig-
inal work, but also endeavored to substantiate most of what he had
said. A number of technical points are brought up in defense of the
author's assertions.
Institution None
Submitted

SOV/124 58-8-9191..''
Translation from: Referativnyy zhurnal, Mekhanika, 1958, Nr 8, p 124 (USSR)
AUTHOR: Puzyrev, N. N,
--------------------------
TITLE: Measuring the Seismic Velocities in Wells (Izmereniye seysmi-
cheskikh skorostey v skvazhinakh)
PERIODICAL: Tr. Vses. n. -i. in-t geofiz. metodov razvedki, 1957, Nr 3? 80pp, ills
ABSTRACT: An account is given of measurements made of the elastic-wave pro-...,,.
pagation velocities in rock with the aid of a well-type seismograph.
The author examines the hodographs of the transitory waves with res-
pect to their vertical profile, and he discusses: 1) Methods for logging
the observational data obtained, 2) the plotting of vertical hodographs,
3) reduction of the observed time function to a vertical reference,
4) calculation of wave velocities, and 5) evaluating the accuracy of
results. Discussing also proposed modifications in seismographic
well-logging techniques, he generalizes seismographic well-logging
data obtained from anumber of wells. The calculation procedures
are presented in an appendix.
G. 1. Pokrovskiy
Card 1/1

lit
rpy
It
gin
Ur ftif v

3(10), 7(8) PHAN I BOOK EGWrrATION SOV/3430
Pazyrev., Nikolay Rikitovich
Inter.pretatsiya dannykh seyawrazvedki mtodoz otrazhennykh voln (Interpretation
of Reflection Shooting Data) Moscow., Gostoptekhizdatj, 1959- 45ip. 6,&)o
copies printed.
Sponsoring Agencies: Vsesoyuinyy nauchno-isaledovatellskiy inatitut geofiziches-
kikh metodov razvedki. and UM Hinisterstvo geologii i okhrany nedr.
Eds.: I.I. Gurvich and I.K. Kupalov-Yaropolk; Exec. Ed.: N.N. Kuzlmina,*
Tech. Ed.: A.S. Polosina.
PURPOSE: This book is intended for seismic prospecting eqgineers and geologists
engaged in interpreting BeialdeLprospecting data.
COVEMM: This book deals with the interpretation of reflection shooting data.
The author discusses: 1) reflections under various seismological conditions
as vell as methods for controlling the correlation accuracy throu&1a the affli-
cation.of dynamic and kinematic criteria; 2) problem of the travel-tim curve
theory for nonhomogeneouz -media and curvilinear interfaces; and 3) phases of
compiling structural maps and charts as well as the selection of a suitable

Interpretation of Reflection (Cont.) SOV/3430
cross section for the maps. The material also includes infornatien on:
1) rating the accuracy of results obtained at various stages of interpre-
tation as well as on stricter averaging methods; 2) the relation between
effective and average velocities for nonhomogenous media and L-arvilinear
interfaces; and 3) approximation methods which take into account the non-
homogeneity of media in the construction of reflecting boundaries. The
author thanks the staff of the seismic laboratory of the All-Union Scientific
Renearch Inst. Lute of Geophysica,, including L.N. Khuddbina., T.N. Kullchikhina.,
R.S. Khromoina.. N.K. Nolodtsovap N.I. Klimovich and K.P, Vasik. He also
thanks I.S. Berzon, I.I. Ourvich, I.K. Kupalov-Yaropolk, the staff of the
Kazakhstan and Uzbek geophysical offices and the Nizhne-Volzhskiy Geophysical
Trust. There axe 182 references:, 161 Soviet and 21 English.
TABIE OF CONIIaM:
Foreword 3
introduction
Ch. I. Principles of the Reflected Wave Method
1. Dynamic Properties of Longitudinal Reflected Waves, 10
Reflection of plane var6s from a sharp boundary.
Computation for a free boundary-. Geometric divergence
Card 2/15

Puz,--REV, 11.1%

h0217
S/16 62/000/007/026/149
D228%307
AUTHOR: Puzyrev, N. N.
TITLE: ~Results of experimental work on the generation and the
recording of transverse waves in districts of Nizhneye
Povolzhlye
PERIODICAL: Referativnyy zhurnal, Geofizika. no. 7, 1962, 21,.ab-
stract 7A142 (V sb. Sostoyaniye i perspektivy-razvi-
tiya geofiz. metodov poiskov i razvedki polezn. isko-
payemykh, M., Gostoptekhizdat, 1961, 240-247)
TEXT: B'xperimental work was carried out in order,to: 1) test for.
the generation of transverse waves from powerful percussively and
explosively directed actions, with the aim of sharply increasing
the survey depth; 2) study the conditions, in which transverse
waves are generated and recorded, and ascertain the method's ex-
L>(
ploration potentialities under conditions of the Russian Platform;
3) study the velocities and the dynamic features of transverse
--waves in well observatiqns. The work's results show that it is
Card 112

S/169/62/000/007/026/149
Results of experimental D228/D307
p*l
possible to use percussive actions effectively. When driving 1 es,
developing an energy of 4000 - 8000 kg/m, waves were recorded up
to distances of 4 km from the source, and the profile was studied
to a depth of 1 km. Explosive actions can be used to generate
transverse waves,. Observations of complete correlational diagrams
show that tile transverse waves have sufficiently persistent kine-
matic and dynamic features.and are positively tradeable along pro-
files. The behavior of interfaces, which are of exploration in-
terest, can be investigated more accurately and in greater detail
by means of refracted transverse waves. Measurenents, made for the
first time, of the speeds of transverse waves at great depths
(down to 900 m), allowed the stratal velocities of transverse wa-
ves to be studied together with the correlations of the,speeds of
longitudinal and transverse waves, characteristic for terrigenous
and carbonate rocks. The absor,)tion of longitudinal and transverse
waves in different rocks was investigated, and it is concluded that
the absorption of transverse wav'es is not anomalously high. Other
dynamic features of transverse waves were.'studied. The main direc-
tions of further research are outlineds Abstracter's note: Com-
plete translation.
Oard 212

PUZYREV, N.N.
Sow problems in interpreting transverse and transformed waves.
Trudy Inst. geol. i geofiz. Sib. otd.'AN SSSR ho.16t201-213 162.
(MM 160)

ACCESSICK NR: AP4010876
A,
AUMORSS Kry'n"S.S. V*j
TITIX: Compatirc the effect of a curvilinear refr"ting boundaz7 In
scismic data
SOUPCE: Goolcigiya I 860fis*&# 10- Ut WX 3-U
TOPIC TAGS: seismic refraction,, interface, curved Interface, curvmnsar towl"17,
arriva 1 time, second order structure, seizzic survoy
ABSTWXT: The auThors point out the necissity oi computizW.distortions associated
with curved refnact'irg surfaces. In thelklest-arn:;'Sibarian LowlaAd it was nocozzary
to cc-n7Lta the i~.ffect of this factor duri reCi6nal studios on the surface of the
when the slope of chi-- surface differed ~from- the assu;-xd base by rore th"'
I -a pr--ctice it is advisable to use difrerent methods Tor computing tho affeejp:
choosinf; the best one by experirLental meana under actual conditions. Computations
ara br-sed on a smocnth curving zurfaco, local variatio=s being smoothed ovir
reason of -.hc fol--Ciainz. Because of difference In velocities in the two adjoining
lCirlar-, c.i--:-. tcz 4-.-. time of arrival of a wave (ardp consequently, in -;~-o
Ideter ed V--!La Of depL%) vill be j-.raater gaazurs by ~~.Q azd
Card

ACMS101111 NR: Ap4olo876

slope at points o1fintrance and exit than by irr4gularities of the interface
between these point6. The effect is more strongly manifest the greater tha velocVq
difference betueen:the layers. Also, the ray penetrates farther into the second
bed at convex segments of the interface. ~Local 'convex irregularities will, not bend
.
the ray; these undulations are "truncated," the iiave cutting across, and the ir-
regularit'les are .-ot represented in the arrival iime of the ~iave. Since the basic
task of regional in*estigations is delineation of second-order..,and higher struc-
tures, the smoothirig of local forms doesinot diminish the geolokical value of the
results obtained, Sharp local irregularities of the int'erface.at'_,~he points of
entrance and emergence of.the ray of the head wave may'appear prominently in the
arrival tire, however. They appear as jupps,in individual values of velocity and
dQpth and may-be considered as possible indicati6ns of higher-order structures. It'
is 'concluded that a survey may eliminate the distorting effect of curved interfaces:
by usi.%a composite travel-time curves. The possibility of recording small struc-
nas uill depend on the density of recording-stationss, Origs arts hass 7 figures
~U
and 30 formulas.
SSOCIATION: irstitut goologii i geofizihi Sibirzkogo otdclaniya MI SSSR,~ Novo-

T
-=titute of Goology and Gaophy~4 c.-~ S_-**raxiZn Departmant AN SSSR)
L
card 2/3

ACC NRI AT6028377 SOURCE CODE: UR/00oo/65/000/060/0118/0123 I
AUTUOR: Kondranhov, V. A. Mandellbaum, M. M. Puzyrev, H. N. Gurkovi,- V'# S.
ORG: none
TITLE: Technique of regional seismic investigations in Siberian platkoirm areas
SOURCE: International Geological Congress. 22d, New Delhi, 1964. Ge'dlojicheskiye
razulitaty prikladnoy gcofiziki (G~_,ological results of applied gcophy~i;#.)-, doklady
sovetakikh geologov, problema 2.,Moocov, Izd-vo Nedra, 1965, 118-123
TOPIC TAGS: scismolor
Zr, platform area, sedimentary cover, u"1svbi"'i=PaM"
seismic prospecting
'of Sibiiria
ABSTRACT: Regional seismic investigations conducted in platform areas
for the purpose of studying principal features of the deep structure are. 'described.
This work was performed mainly in connection vith oil and gas prospeciini.in the
area. To study the folded basement a special technique of single and.1inear *head-
wave soundings hasbeen developed which makes it possible to investidit6 forest-
covered areas. The results of the field work have revealed some featf2res'of the
basement structure which had previously not been detected, including-&fferentiation
of the basement into layers according to their elastic properties. Th6'idedimentary
cover is investigated primarily IV the-irflection method in its various m6~ftffcationsf
Card 1/2

ACC NR: AT6028377
For regional investigationsowide use is made of single reflection soundings which
are applied on a wide scale in the west. Siberian lowland. Using thj~e.-technique
in area of nearly 50,000 km2 has been surveyed. Also widely used is--p*L*.tebhnique of
regional scinmic-reflection profiles including profiles along.the rilets... These
investigations have resulted in mps and croas-eection diagram which.ahbw clearlyi
the effectiveness of the survey. Orig. art. has: 2 figures.
SUB CODE: OB/ SUBM DATE: -o6.Tan65
/2

ACC NRI AT6005055 SOURCE CODE: UR/0000/651000/000/0005/0070
AUTHOR: So* V.
(Doctor of technical sciences); Krylov,-
Fotaptyev, So Ve j
ORG: none
.TITLE: Point seismic sounding
SOURCE: AN SSSR. Sibirskoye otdeleniye.:. . .1.nstitu't'geolog-ii, i geofizik
Hatodika seysmorazvedki (Methods of prospecting)', Moscov'.
Izd-vo Nauka, 1965, 5 -70
TOPIC TAGS: seismic-prospiecting,,point seismic sounding, discrete-wave
correlation, seismic wave, seismic profile
ABSTRACT: The general principles of discrete wave correlation. general-
ly considered to be inadequately developed in regional studies and
prospecting work, are-discussed. The theory and procedures of polst
seismic sounding with refracted (head) w aves and reflected waves, and-
the advantages of using wave correlation with them, are presented.
The basic problems encountered in inter*preting the.resu lts of point.ob-
servationa (without travel.-;time curves) are discussed, with only
monotypical reflected and head waves considered. The possibilities,of.:,,-,
.simultaneous use in interpreting different types of waves formed at-.
the same discontinuity are discussed. The probles. of diteruining;the~"1'7
-77

AT6005055
positions of diacontinuities and the distribution of velocities in the,-
medium is discussed. The.selection of sounding par 'ameters, the density
of the observation network..and special procedures to be used in the..:~.
field to solve various problems are discussed in detail. Some special- 11
features of the practicaluse of previously described interpretation
procedures are given (methods of discrete correlation, constructiorC
of the t(x, 1) field, accounting for the effects of curvilinearity of,.,,-.'
the refracting interface, etc.) are presented. Examples are given of
the p~ocesaing of data from point observations in the West Siberian
Lowland. Problems encountered in estimating the accuracy of results
in determining the depth and the velocity parameters in the medium
(e.g., computational errors and.errors due to simplifying assumptions).
are discussed. The procedures proposed here were tested in a number
of regions with data from.previous observations, and they have begun
to be used extensively ~n regional investigations of the surface of
the basement and of deeper*discontinuities in the earth's crust in
Western Siberia. Comparisons of the results obtained from point sound--
ings with,refracted waves and data from deep boreholes with those
derived by the correlation method for refracted waves indicated suffi-,
ciently good accuracy of the proposed method in the West Siberian Low-
land. Errors in depth usually did not exceed �100 m (with depths on
the order of 3 km) and �150-200 m/sec in the boundary velocity. Ex-
tensive use of this method of point observations permitted a change-
over to a planned regional study of the basement of the West Siberian
Card

ACC NRt AT6005055
Lowland by a series of river traverses and an area network established
by air transportation. , In 1962-1964, 7000 km of river traverses were
covered, with a productivity of 1000 km of profile by each party in a
working season, as compared with 150--200,km of profile--produced by
each party with the usual method. Recommendations for further develop_
ment of the method of seismic sounding called for concentration on the
following points: 1) further development-of methods of discrete wave
correlation; 2) further development of the theory and methods of sound-
ing based on the complex utilization of ditierent types of woven;
3) ddvalopment of instrumentation with Improved accuracy and reliabilitil
ensuring wider selectivity of optimal receiving conditions and more
channels. also portability*and ease of operation; and 4) testing
sounding methods to improve and develop them for regional and proupect-~
in& investigations under various seismological conditions, Orig, art.,
has; 35 figures and 67 formulas. CEO]
SUB CODEt- OB/ SUBM DATE: 30Sep65/ ORIG REFs '026/ OTH REP.. 001
Card 3

ACC NR, AT6005060 SOURCE CODEJ UR/0000/65/000/000/0127/01 35
AUT110Rj Lebedeva, Go No; Lebedev, Ke As; Puzyrevs No No Poctor of
technical sciences
ORGI none
N
TITLE: Selection of seismic waves by polarization.for sources with
horizontal directivity
SOURCEI AN SSSR. Sibirskoye otdoLe.nLys. Institut xsolojj_~k. i
Metodika Moscow*o"--
Izd-vo Nauka, 1965, 127-135
!TOPIC TAGS: seismology, seismic wave selection, polarization, phase
inversionl signal filtration
ABSTRACT: A method is proposed for selecting transverse waves (irre-
spective of the direction of polarization) out of all other waves
(longitudinal exchange waves, multiple waves, etc.) arriving at a
receiver. This selection is based on the nature of their polarization
at the source. The significant property of the transverse waves is that
when there is a change of 180*-in the direction of the effective forest
the phase variations in the Lopulas of the transverse wave also change
lby 180" (phase inversion), while other typos of waves remain unchangede
Card 1/ 2

ACC NR: AT6005060
The model used as an example is a horizontally layered medium. Two
cases are investigated: 1) a horizontal force directed perpendicular
to the profile (Y-action) and 2) a horizontal force directed along the
profile (X-action). Two identical horizontal forces or moments of
rotation acting in opposite directions produce vibrations which are
recorded by a seismograph or group of seismographs. Pulses from
transverse waves caused by both actions are-added, while pulses from
all other waves are subtracted (addition of opposite phase@). This
method was tested in the field in the summer of 1963. Several experl-
ments were conducted on a crystalline basement covered by about 20 a
of alluvial deposit . 1;ongitudinal heado transverse, and exchange.wavee~.
formed at the bases:nt surface were clearly recorded near the source
(100-150 a away). *It was found that the effectiveness of this method
of adding (or subtracting) vibrations from two oppositely directed
actions is determined I to a considerable extentg by the *quality of
signal amplitude. This so *thod Is described as offering saw po~*L-
bLlLtLes for separating waves that say not differ In apparent velocittairs
frequency'characteristLce.-"or amplitudes. Orige acts bass 3 figurese
[so)
SUB CODEs 08/ SUBM DATIs 30Sap65/ ORIC RRF1 003/
rard 22

ACC NRt A-16oo5o6l SOURCE CODE: UR/0000/65/000/000/0136/oi46
AUTIIOR: Puzyrev, N. N. (Doctor of technical sciences)
ORG: none
~
TITLE: Methods for constructing reflecting interfaces from exchange-wave travel-time
curves
GOURCE:. AN SSSR. Sibirskoye otdeleniye. Institut geologii i geofiziki. Metodika
seysmorazvedki (Methods of seismic prospecting). Moscow, Izd-vo Nauka, 1965, 136-146
;TOPIC TAGS: seismology, seismic prospecting, seismic wave, exchange wave, reflecting
wave, interface reflection, travel time curve shock wave reflection
ABSTRACT: A discussion is presented on some of the methods of constructing reflecting.
interfaces, chiefly from PS-wave travel times; it is assumed that the velocities of
both types of waves (Vp) and (VS) are given. Only the two-dimensional problem for
a homogeneous medium is considered. The discussion involves the following methods:
1) method of time fields; 2) construction of areas by known apparent velocities, with
formulas for determining the length of a reflected ray and the direction of the
normal from the reflecting area; 3) method of envelopes for constructing the inter-
face; 4) method of circles -- justified for exchange waves if the distance between
source and receiver W is such that the law of tangents can be used instead of the
law of sines (this condition is adequately satisfied if 4 1 h and may be valid in
I Card 1/2

Card -2

ACC. NRI AF0023317 SOURCE CObEs liFf/dii-6166-/oo6/oo2/oo88/o695F
AUTHbR: Puzyrev, N. N.; labodev, K. A.; Lebodeva, G. N.
0
ORGs Institute of Geology and Geophysics, Siberian Branch AN SSSR, Novosibirsk
(Institut geologii i geofitiki Sibirskogo otdoloniya AN S5SR)
TITIZ: Excitation of transverse seismic waves by explosions
SOURCE:. Geologiya i geofizika. no. 2.,1966, 88-99
TOPIC TAGS: seismology, seismic prospecting, seismic wave, elastic wavet transverse
wave, go ologic survey
ABSTRACTs The.paper deals with seismic methods of geologic survey. The application
Df transverse wave! supplementing the longitudinal olastic*waves results in an
Increased accuracy and greater resolving power in seismic investigations. The authors
iovelopod a now method for excitation of transverse waves by producing explosions in
-avitles with walls suitably covered on five sides by absorbing materials thus
creating waves propagating in one well defined direction. Previously, it has been
axporimentally found that the pressure P(in atm) of the,shook wave in'a moist ground
(sand-clay) is related to the distance from the'explosion (in sisters) and the weight
Df the charge (1~ kg) by the expres.sion'-
(3
(2)
Card. UDCs 6W.834 -

6M
Cwd 2/2

f'ACC N~, jj7662079 SOURCE CODE.: UR/0030/66/000/012/0021/002~
AUTHOR: Pu~rp!y N. (Corespon4ing member AN, SSSR)
ORG: Institute of Geol .ogy and Geophysics, 51berlan Division, Ace"" of Sciences $$SRI
.('nstitut gsologIIL,1 goofisiki S,ibirsko *go otdalenlys, Aka.demii nauk MR)
TliLE: New methods ior seismic investigations of the Earth's crust
ISOURCE: AN SSSR. Vestnik, no.*12, 1966. 21-26
TOPIC TAGS: earth crust, seismic wave propagation, rock elasticity, elastic wave
propagation,,ieismic prospecting
ABSTRACT: New seismic methods of Investigating the Earth's crust, Includi 'n& point
soundings, aerial bombing, and the use of shear waves are reviewed. The method oU
point sounding, used primarily in inaccessible regions, is based on the recopition
and identification of the characteristics of deep waves recorded at isolated
observation points (point correlation), theuse of different types of waves (re-
flected, head, refracted). and on special data-processing techniques. Under Ideal
recording conditions the method of point observations can yield valuable data on the
structure of the:Earth's crust on the basis of only one-tenth the volume of field
measurements by continuous profiling.' The use of aerial bombs to generate waves in
inacessible regions hes been successful on many occasions.-Using this method, waves
have been recorded at distances, up to 110 ka from the point of bomb strike. A remote
Card 112

Can 2/2
ACC NR. AP7002079
control device called the "Tayga." has been developed for use in the aerial bomb
technique which considerably speeds operations. A method of utilizing shear waves
has been successfully developed by the Institute of Geology and Geophysics and the
All-Union Scientific Research Institute of Geophysical Prospecting Methods. Several
ways have been found to generate the necessary shear waves using this method. Most
important are the techniques of setting off charges In cavities filled with an,
absorbent, the use of a special device to accumulate the energy of deep waves, and
the use of vibration. A new method has been developed for the selection of shear
waves on the basis of directivity at the source. This method, which employs a
magnetic memory unit, eliminates the effects on the records of a large group of
interference shear waves which are caused by the high level of longitudinal waves
generated in the nonideal madium In the vicinity of the source. Orig. art. has;
2 figures.
SUB CODE: 08/ SUAK DATEs none/ ATD PRESS: 5110-

uz F
Ek-LOITATION SOV/5592
Vaesoyutnoye soveshchaniye Po reniyu radioaktivnykh .'ZotopoV i
yadernykh Jzlucheniy v khozyaystvc SSSIZ. Riga, 1960.
Radioaktivnyye izotoPy, i izluchoniya v narodnom
kho-yay3tve SSSR; trudy znogo soveshchaniya 12 - 16
aprolya 1960 g. g, Riga, v makii. t. 4:' I?oiski, razvedka
i razrabotka 1,01 "n"Id' mykh (Radioactive 'Isotopc3 and
Nuclear Radiation in th~ ? . al Economy of the USSR; Tran-
aactlon3 on th April 12 - 16, 1960.in
* Symponjurt H # in Riga,
4 volumea. v. 4: urvaying, and PlInIn or Min-'
eldiizdat,
oral Dopoaitz) MOSCOW 1961. 2N p. 3,640
copies printed.
nauchno-tekhnicheskly.kom:Ltet
Sponsoring AzencY: #r*IWJFM-
Sovota Mlnist:,ov SSSR. stverinyy komitet Soveta';Mniatrov
SSSR po Ispoll Izovaniyu ;tot energli
Eds. (Title page): N. A. Fetrm L. 1. Fetrenko, and P. S. Saviltskly;
ed. of this volume: 14. A. -anskiy; Scientificed.t M. A.
Speranskly; Frecutive Eds.: N. KuzImina and A. G. lonell;
Card 1/11

Radioactive Isotope3 and Nuclear (Cont.) SOV/5592
-tech. Ed.: A. S. Polo_~Ina.
PUPPOSF : The bcol, is intended for englneer2 anal -,e,:hn1ctans
dealing with th-a problems involved in the spplicaticn of
radioactive iEotopes and nuclear radiation.
COWMAGE. This collection or 39 articles is Vol. 4 of t!ie T-rann't-0- 7
of the All-Union Conference of the jntroduc;!~Ion of Hadlo-
active isotop&s and Nuclear Reactioni In the Nat-11.*nall Econemy
of the USSR. The Conference was called hv thA Go3udarf-tvennyy
nauci~nc-tekhn:,aeskly komitet Sovet Mirxz.-;trovSS3R (Stat.e
Sclail~V1.fle-Technical Cornlttee or the Counsil of Mtnluters *f
the USSR), ACL&My of SAcnces USSR, Go4plan 35SF. '5tate Planning
CcmrAtz;ee of the Counail of M-InIrtera of th%- ~,"30,
nyy 1comitet Scveta 111nintrov SSSR po avtmat1::a11,31.1 1 maah:.no-
atzroyeniyu (State Committee of the Council of T-UnIsters of the
USO'R for Automation and Machine building),and the Ccuncil of
vinlater5 of the Latvian SSR. The reports zummarized In th4 a
publication deal with the advantages, pro5pects, and
Card 2/11,

Radioactive Isotopes and Iluclear (Cont.) SOV/5592
development of radioactive methcdo used in p roapoc tin g, rur-
veying, and mining or ore3. Individual reports present the
reaulta of the latest scientific research on the development
and Improvement of the theory, methodology, and technology of
-ladlometric Inveotigation3. Application of radioactive method"
in the field of engineering geology, hydrology, and the cGn-
trol of ore enrichment procoazea is analyzed. No pernonalitle-3
are mantloraL There are no references.
TABLE OF CONTENTS:
Aickseyev, F. A. Present State and Future Prospects of Applying
'ethod3 of Nuclear Geophysicz in Prospecting, Surveying, and
the M
'ILI 5
-ning of Minerals
Bulaihevich, Yu. P., G. P1. Voskoboynikov, and L. V. !hzzyukin.
Neutron and Gan=-Ray Logging at Qrc and Coal Depo2its 2.9
Gordeyev, Yu. I., A. A. Makher,and D. M. Srebrodollskiy. The
Card 3/11

...........
lootoie3 and Nwalear (Cont. SQV/5592
of Mlerccomponent3 of Natural Iwlater3 255
!~T:lyanova, Ye. M, K. A. Kuznetsova, 1. D, 1IVazkcvnk3ya, F.
-nd D. A. Sokolov. Preventive Controll of the Dr-1-Mrig
Eackne From a Coal Seam While Drilling clined Borehclea
in Lean Seams 26o
Abdullayev, A. A. Ye. H. Lobanov, A. P. Novikov, And A. A.
r!:--lyflarc~V. R;Ipld D,~,termlnatlon of the F~,,rcentaEe of lead In
OL-~jq and condentratLa
Plakniin, 1. N., V. N. Smirnov, and L. P. Starchik. ATY,~Ito:atlon
of Alpha Radiation for the Automatic Regulation of thi Material
Compo3ition of Enrichment Products of Certain Ores
Lenin, S. S.Saintillation Fzanameters 2-:6
Card 10/11

FUZYRFY P,

re -a I c s2 Z~ 1 Li n f i I n u a rat,s

1. biboratoriya kon trulya j, avtomatiki V--eooyuznoec nau,-.hlo-
instituta j--odZemnoy gIzifikatoil. ugley.

of thiu anrle of inclination of tho DGS-2 bit in boring
lin.-I-nontal L