SCIENTIFIC ABSTRACT TARKHANYAN, A.S. - TARKOV, A.P.
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CIA-RDP86-00513R001755010014-7
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RIF
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S
Document Page Count:
100
Document Creation Date:
November 2, 2016
Document Release Date:
September 26, 2002
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14
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Publication Date:
December 31, 1967
Content Type:
SCIENTIFIC ABSTRACT
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109~~ --tir-diova cular Changes in Brucellosis
"Changes in the Cardiovascular System in Brucallosia," by
Ta. L. Lurlye and Ye. P. Tarkhanova' Trady Kuybishev6kogo
Reditsinskogo Instituta (Works of the Kuybishev Medical
Institute), Vol 5, 19540 pp 296-303 (from Sbovetskoye
ftditsinakoye Referativnoye Obozreniye, N ____"6__P 54,
Ostracted.by K. Go.rbunova) 0 20, 195
'Vhirty-eight patients suffering from brucellosis) principally the
~cbronic and subacute forms, were examined. All patients were subjected
to detailed clinical and serological. investigations. The Burnet test
was positive in the majority of the patients. Analysis of the data
obtolued led to the conclusion that subjective disturbance of the
,Cardiovascular system and physical heartdisorders were observed in a
considerable number of the patients. Upon electrocardiographic investi-
gation, changes in the electrocardiogram which indicated diffuse dystro-
phic changes in the myocardium were evidenced in the majority of cases,
and variations which reflected focal changes in the myocardium occurred
in a number of cases. The blood flow rate was retarded somewhat which
bore witness to reflected affection of vascular tonus. Capillaroscopic
investigations which were conducted in a number of cases revealed pro-.
nounced disturbances in the peripheral blood circulation -of brucellosis
patients," (U)
KARAPMANY MIWILIVA, A.M.
Hydration of vinyjnofAyI~-np to mpt-hyl ,rinyl kpiow- by means of
sulfuric adid -solutions of cupro--as oxidr.. Part 1: Solubility-
of vinylacety1pne in sulfuric said solutions of cuprous oxide.
Izv. 91 Arm.SSR.Nhim.naul-d 17 no,,14:398-406 IU*.
(MIRA 18:6)
1. Yerevanskiy~-fili~l Vsesoyuzriogo nnuchno-issledoVateltskogo
instituts alntpti,-,hesk~go Iauch-akn Im. aked. S*V.Lebpdpva.
!.Y qLl
Nyd ra t I c~:, cr ny a c!t~
0.1 U + I or
c;d!j-- Par', .2.,. Ppizfi,,,n f, v I n c c
Ul -f Uri nac--(,; :jolutl(,rl Cf' Tzv..A N Arm..SFF.
Ll "'6C, ~365 ' 65.
or
'FAHxHA.UVdm%GgV!,
A now silage crop. Izv.AN Arm.SfM.BIol.1 sellkhos.nauki. 3 no.9:
91 152. (MM 9:8)
1. Zaveduyushchiy Stepanavanskin goemortouchastkon.
(Stepanavan District--Rye) (Insilage)
'I T T
C.- C 1-,.1 n 4 C o 7),) t 1 -1 1 1 11 t 1~,- t om i n C u enc e d L) Y t h e
L I A 1 Lr ; ,, i i -
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I v- X 1 In sc-ne (ilia n tum-rlec 11,j ~, 1 c.t 1 Pr o b I l2nis the deformation of
atoms (JUC to OpLical transitions of the valency clectronr mu-'- be
taken intn account. In this paper I he spheric-illv-symi:ietrical
ji.i r t o f t c i i., ri g e ir p u t e ri t L s c x a :- i r-. e d r or, I L on. 6
with a
not too sta.-ill Z an aptiroximate calculation ca -i he carried mit
v j l. r i t y ol c-lectrons i ri h e
t oni r i n z 17 r oin c, i s son ~i:i T i or h r, f n o- -. Ti :,- c x p r e o n s
,I r 0 : I [ 1 " 0 C I Z I F, a 0 1.: 1 L, 0 t 0 r C, 0 v3 o C
lid Ll'f1CV e 11-C trO11S
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ACC NRs AP5022706 SOURCE CODE: UR/OISX/65/007/009/2688/2697/
Y Y
AUTHOR: TarkhgMan, Re Go
.'v 95--5
ORG: Institute of emiconductors AN SSSR.-Leningrad (Institut poluprevadnikov AN
SSSR)
It `4,
Y
TITLE: Magnetoresistance and themomaoetism-in a longitudinal quantizing magnetic
field in semicon3uctors of the n-InSb type
SOURCE: Fizika tverdogo tela, vo 7, no. 9. 1965, 2688-2697
11 ~c ;- S_ _k7
TOPIC TAGS: semicond tor theory, theoretic physics, Indium compound, antimovide.
longi tudinal. magnetic field, thermomagnetic effect, magnetoresistance `7
ABSTRACT: The author studies the changes in thermoelectromotive force and resistance
in semiconductors of the n-InSb type with regard to the deviation from parabolic fom
in the conduction band and electron spin in an arbitrary longitudinal quantizing mag-
netic field. It is assumed that acoustic scattering predominates. It is further as-
sumed that the electrons are non-degenerate and that their concentration is constant,
i. e. that it is indevendent of the magnetic field and temperature. The themoelec-
tromotive force is determlned by calculating the heat flux transferred by electrx)ns
in the electric field and then applying Onsager's equations. The relaxation timo for
electron-phonon scattering and the longitudinal kinetic coefficients are determined.
L;1-rd
L 9263-66 --------
ACC NR, AP5022706 'Itf, .9
In conclusion, I thank A- I. Ansel's for guidance in this w0rkv and Part'c'Pants in
a theoretical seminar a~ ~JjjNSSSR fZ!, discussion. orig. art. has: 51 fomulas-
SUB CODE: 20/ Sum DATE: 26Har65/ ORIG REFS 005/ OTH IMF: 008.
Crd 2/2 -------
R;
t 8845~66
ACC NRt
EwT(1) IJP(c)
AP5022733 SOURRCE CODE: UR/0181/IiS/0071009/2037/2042
AUTHORz Ansellm, A. I.;.Obrazt-sov, Yu. N.; Tarkhanyan, R. G.
Ll Q ~;-l
ORG: Institute of Semicond~ctors AN SSSR, Leningrad (Institut poluprovodnikov
AN SSSR)
TITM Quantum theory for thermomagnetic currents in semiconductors and metals
SOURCE: Mika tverdogo tela, v. 7, no. 9, 1965, 2837-2842
TOPIC TAGS: theoretic physics, quantum physics, thermomagne ic effect
ABSTRACT: The authors consider the problem of ~WtermLning kinetic coefficients in
equations for the momagnetic'phenomena in the quantum %:ase when there is a tempera-
ture gradient. It is sh6wn'that solutions of the motion equations for the density
matrix assuming local thermodynamic equilibrium lead to expt-essions for the current
density which were proposed by Ansellm and Askerov In 1960 (A. I. kmel's, 8. M. ~he
Askerov, FW, 2, 2310, 1960). The results coincide with data In recent papers on t
quantum theory of thermompetic phenomena in seniconductotv aad metala. Orig. art.
has: 29 famulmo
SUB COIDE: 20/ SUBM DATEt 03May6S/ ORIG REF: 005/ OTH FZF: 003
YU.N.,
ANSF-1,44, A.I.; CBRAZTSOV, - - - I cIurrents in semiconductOlO and
theory of thei*OllomagnOtiO 1842 s t65,, (MIRA 18t10)
Omntum 7 no.gt2837
.Metals. Piz. tver, t'312% 0v t4V SS,,,,R, laningrads
1. ,,,,titut poluprovOdlik
14NDZHOYAN, A.L.;TARKHANYAN, Z.K.
5-90thYlfr-rfural acetone. Sint. geterotalki. Isood. n0.3350-32 158
(Batenons)
(MIRA 13:3)
MNDZHOYAN, A.L.;TARKHLNYAN, Z.K.
5-Methylfurfuryl acetone. Sint. geterotsikl. soed. no.3:53-54 158.
(Batanons) (MIRA 13:3)
XOLOHIYBTB, B.T.1 LYUBIN' VOM.
(;onductivity and photoconductivity in antimony triIolonide films.
?is, War, tela I no.6:M-902 JS '59- (MIRk 12:10)
(Antimony selenide -Ilectrio properties)
RYnIN, S.M.; EDNOPMA, R.F.; MAS10VA, L.V.;- HANYTIV, O.A.; SMTKAN, N.B.;
TAWMIN, D.V.; IMOV, G.V.
Germanium photodiodes vith omll inertia. Yiz. tver. tela. 2 no.9:2199-
?-201 S 160. NM 13:10)
1. Loningradskiy fiziko-tekhnicheskiy institut AD SSSR.
(Germanium diodes)
3/120/61/000/002/012/042
AUTHORSI Vitov.kly. N. A.. M.I.Yew, P. I., M.tv.y.v. O.A..
~Y,h~L. ~_ S.M. and T.rkhin, 0. V.
TITLgi 8iliccn X-P-Count;rs ~OrHeavy CharSed Particles
Operating Vithout an External P:worg Pply
PERIODICALS Pribery I takhalke, okeptriment , I :01~ K9.2, pp.82-83
IrIT, "It ... ..... ":Vl ns an %pajunction or*& of
.b. I _2'u::d. '. " ad in rd , to I rain%ttels, hcounting
5 ort_ it*: 6
properties when operated a h circu r ctif r . I
saturation current In the countora studied was not over 0.1 UAI
the leakager 1,:.egohmaj. Undr.:uchcdnditl:aSS,
ls"t;n:n rea I
ohort-c rcu I I c I WIG b ins
u r .. I St us
25.k I.... In counters irradiated wl Ih a portlcl:s ,nl*r
th,:t;v;_;oodllIon. and toot adAI room tamper. U;.. .,. torlitudos
rest Yhno no!::* Thlap:rj:rm&n 1: :quals
"':1.1 SS'.
my w'!h.p':'n
that of counter r, I S p di but h too he
at or ease tnc;o&p
I t as0 rapidly with creast a. To
':r h.,:'l:Ud!;jff V*lt&f
both cameo (operating so rectifiers d pulse rise ttat
varloa from I to 3 Usec, Th. decay tis,* to determined by the X-C
of the circuit. This As shown In the oscIllogreads Fig,l. In
t2401
Silicon M-P Counters of ... 3/120/61/000/002/012/042
9210/9594
Fig.la the duration of the markers to I Usec. Fig.16 - 1-dins
edge of the pulsol marker duration 0.2 umac. Trigger delay 0.5 Usee.
WLth docr-oinx temperature the pulsomaqftuds and duration remain
unch&nX*d. Silicon D-p counters are regarded so highly promising
I roo:.t:lp:ra 0ypc;n operate as photovoltaic
I n tur:rth..
I rn I pow p
Comments me de during the proof-readingi The here described
so udoo.9 I 'son
'00"
.:!I,
r f c r r I he ;.p. Z
d. 1.
..11:1,19 f,.rr:p*u*I1.-:',7. A' present. the laboratory of the
h c, .
o
ut r. ma u r:...urf4c,-6xrr.1*.r ;1!.Icoo un which or*
I b f I ry amp It a 0 1 n l!:rath. 1% for
ou to is or Np.c I I l ui:o
CL- parIi.loo with oner At a of 5 .5 ..V). The consid:rstinn.
pr .~ :r. n p IncIple a plicoble also ;or such
.P:.tnt:d In Ihapp:::rt.,..i r p
r' IrI. n There are I figure and 3 Soviet
r.f.r.-e 0. .
ASSOCIATION , 'I Ik.-t.khnL.h..kiy lsaitit4t AN SAAR (Physics-
technical Institute AS USSR)
SUBMITT90i February 20. 1960
ZA-2"
974(a
S10891611011100310021013
B102/B,138
AUTHORS: Ryvkinp S. M., Maelova, L. V., Matveyev, 0. A., Strokan, N. B.,
Tarkhin, D. V.
TITLE: silicon counters in nuclear spectrometry
PERIODICAL: Atomnaya energiya, v. 11p no. 3, 1961j 217 - 220
TEXT: Silicon counters were developed at the Fiziko-tekhnicheskiy institut
im. A. F. Ioffe AN USSR (Physicotechnioal Institute imeni A. F. Ioffe AS
USSR) in 1960. The counters were small (active area: 2-2, 565, and 10-10
mm2). Their pulse height was - 1 mv/Mev, and resolution less than 1% for
Eix 5-5 Mev. They were produced by sputtering gold to n-type silicon
and diffusing phosphorus into the p-type silicon. The following character-
istics were investigated: (1) Volt-ampere characteristics. They were the
usual shape for p-n junctions. Reverse current was 0-5 - 0-05 Pa (at 40 v
for the small-sized counters, and increased proportionally with area;
breakdown voltage was between 50 and 60 v. (2) Capacitance-barrier voltage
dependence. The capacitance of the sensitive layer (the volume-charge
domain) was in accordance with the usual capacitor formula d - SOS/4nC
Card 1/3
27401
s/oo/O/oil/003/002/013
.B102/B138
(S area, eo dielectric constant)i since the thickness d of the
sensitive layer is proportional to TVTT t the oapaoitanoe deoreasee as
1/2 0
(V+vo)- with increasing voltage. (3) Pulse height-voltage dependence.
Pulse height was determined by Q - el (N - number of pairs formed 138
ionization); the mean pair formation energytet was measured for Pu
alpha particles (Q - 2-5-10-13 k):'C - 3-53 :L 0-15 ev; this value agrees
with that found in Ref. 4 (see below). (4) Pulse height-energy dependence.
Pulse height 0 as a function of voltage V was measured for the alpha
energy groups 8-78 and 6-05 Mev- For the short-range group, pulse height
reached saturation at , 15 v, for the long-range group at , 35 v- 0 (E Cd
was found to be a straight line. It is predicted that at V - 60 v linearity
will also be maintained for alpha particles of up to 10 Mev or for any
other particles with ranges of up to 60p. (5) AmiWude resolution. This
was determined on a 100-channel analyzer using Pu 61pha emission. After
correction for noise background, resolutio6 was found to be 27 kev or 0-5~o'
for the small counter, 1% for the medium, and 1 Wo for the large one. The
spread is attributed to inhomogeneities of the silicon. In the OIYaI at
Card 2/3
Silicon counter in nuclear
2701
S/08 61/011/003/002/013
B102YB138
Dubna the 10-10-mm 2 counter has been used for U 233_fission-fragment
recording with high alpha background; G. N. Flerov, Corresponding Member
of the AS USSR, has submitted a spectrum recorded with this counter to the
autho 'r8 of the present article. These junction counters may be used not
only*for recording of a-particles and fission fragments but also for fast
and slow neutrons. The authors thank G. V. Khozov, Engineer. T, A.
Lebedeva and G. D. Gusarina, laboratory assistents, and P. I. Gorshkov.
mebndnic, for assistance. There are 7 figures and 4 non-Soviet references.
They read as follows: Ref. 1: J. Blankenship, C. Borkowski. Bull. Amer.
Phys. Soc.., ser. 11, 5, No. 1, 36 (1960). Ref. 2: S. Friedland, L. Mauer,
J..Wiggins. Nucleonics, 18, No. 2, 54 (1960). Ref. 3: J. Me Kenzie,
J. Waugh. bull. Amer. Phys. Sec., ser. II, d, No. 5, 355 (1960). Ref. 4:
M. Halbert, J. Biankenship. Nucl. Instrum. and Methods, IL No. 1, 106 (1966.
SUBMITTED: March 18, 1961
Card 3/3
KAZARINOV, N.M.; MATVEyEV, O.A.; RyVXIN, S.M.; SOLOVIYE-V, S.M.; STROKAN,
N.B.; TARKHIH, D.V.
Use of semiconductor spectrometric counters for measuring the energy
of fragments. Atom. energ. 12 no.2tl53-154 F 162. (MIRA 15:1
(Nuclear fission) (Nuclear counters)
MASLOVAI, L. V.; M&TOM 0. A.f RYVM, S. M,-; STROKAN, N. B.1
TARKMt~D,- V.; h6iov, V.
Possibilities for using miUcon counters in nuclear research@
Izv, AN SSSR. Ser. fizo 16 no.22:3499-1505 ID 162.
(KMA 16: 1)
(Nuclear counters-Movign and construction)
ACCESSION NR: AP4041057 S/OIZO/64/000/003/OZ17/0218
AUTHOR: Matveyev, 0. A.; Tarkhin, D. V.
TITLE: Etching p-n junctions by strong chemical etchants
SOURCE., Pribory* i tekhnika eksperimenta, no. 3, 1964, 217-218
TOPIC TAGS; semiconductor, semiconductor material, pn junction, etched
crystal
ABSTI~ACT: Pincers with fluoroplaotic jaws are suggested for holding a serni.
conducior billet in an etchant. After 2-.. minutes, water is poured into the
etchantl~ and the washed billet is taken out. Ge-based (Z ohm-cm) specimens with
a diffusion 1-2 cmi p-n junction had a breakdown voltage of 200 v and a resistance
of 10 Mohms; Si-based (300 ohm ,cm) up to 5 cmIL specimens had a breakdown
voltage of 600 v and a few tens Mohms resistance. Orig. art. has; I figure.
ASSOCIATION: Fiziko-tekhnicheskiy ~institut AN SSSR (Physico- Technical
Institute, AN SSSR)
SUBMITTED: o6jui63 ENCL: 00
SUB CODE: NO REF SOV: 000 OTHER: 000
Card
t,U
~m ME
----ACCESSION NR: AP4029703 8/0089/64/016/004/0363/0365
AUTHOR: Matveyev, 0. A.; Ry*vkin, S. M.; Tarkhin, D. V.
TITLE:- Quick response silicon detectors of pulsed Xeradiation
SOURCE: Atomnaya energiya, v. 16, no. 4, 1964, 363-365
TOPIC TAGS: semiconductor detector, n p junction, n.i p junction, penetrating
n C
radiation, hard X radiation, quick response detector, hole type co du tivity
intrinsic conductivity~_spectral sensitivity
ABSTRACT: This report discusses semiconductor n-p and n-i-p silicon detect-
ors suitable for recording short pulses (about 10-7 sec.) of hard X-radiation
having . an energy up to 1 Mev. One of the two experimental quick-res-
ponse detectoru of pulse X-radiation was based on an n-p silicon junction which
was achieved through the diffusion of phosphorus into silicon with a hole-type
conductivity and a res is tivLty of about 1000 to 3000 ohm. cm. The secoW
type was with n-i-p silicon junction. The region of intrinsic conductivitl- was
J/ 2
rr
ACCESSION NR: AP4029703
found by compensating the initial hole-type conductivity by the lithium Ion drift
in the n-p junction field. The nature of the detectors' spectral sensitivity to
X-radiation of various energies was Investigated by the use of filters-made of
St-3 iron. ThuC operating on the principle of collecting non-equilibrium cur-
rent carriers in an n-p junction electric field, the n-p and n-i-p detectors
represent quick-response X-radiation sensing elements with a sensitivity close 6
10-7
the maximum possible for silicon and a responsetim of about to 10-8 sec,
Although silicon has a relatively low X-ralation absorption factor, the mention
ed detectors with a reapon se time of about 10- sec. are in a number of ways more
suitable for the recording of pulse X-radiation than other instruments. Orig.
art. has: 3 figures and 5 formulas.
ASSOCIATION: None
SUBAUTTED- 02Aug63
SUB CODE: w, NP
'Card i.2/2
ATD PRESS: 3047
"N'6 :,REF 'd6V' 002
ENCLt 00
OTHERt 001;
TARKRIISHVILI- A-A-. MIRIMOVA, D., red.; SAGARADZE, Sh., tekhn.
red,
k
(Oriental confectionery]Vostochrqe konditerskie izdeliia.
., Izd-vo Grusinskogo polit. in-ta im. V.I.Lenina i
Tbilisi
1961. 93 P. (Confectionery) (MIRA 15:81
- --
-- - - -- - -.- - -1 .-
Tar.khov, A. C,. "A 'New Yethod of !)etc-x-,unin-:r the ZLeraent!3 of ~. Vertical Dei Csit by
I ac u, No. 1'1~, 10/34, p~7-
Year.r, of !~Drfnetcmetric D,,~..." R-UZvS'll~Q "'0 0' ,
MUKROV, A. 0.
"Gooelectrical Field of Filtratioe. Iz AN SSSR,, Ser Geograf i Geofiz, No 5, 194c~ (4()3-4t8).
(Meteorologiya i GidrologiYax No 6 Nov/Dee 1947)
So- U-3218, 3 Apr 1953
Wn/060109081 Prospecting Mar 3947
DielsOrlos - Constants
%10 1 ~
Nelation of the Dielectric Constants of Rocks to
Their Mineralogical Coiqposition,' A. G. Tb:rkhoy,
All-Union Inst Cool Prospecting, LenIngred, 7
'11V Akad Nauk SSSR, Ser Geograf i Geoflz" Vol Xl,,
No 2
Pi.Wious papers on- subject have very Juportmt
fibbi~Lomlng, i. e., moisture e& samiplazz
Vas not taken into consideration. Zxperiamts win
4iva same results as calculations If carried out
lie arrectly. Notes that value of the dielectric
50738-
Mium/Geological Prospecting (Coutd) Mar 194-7
acid rooks lose than tha+, of the baxi
t
a
ke. Submitted by Academician L. S." laybenzen,
USSR/Geor.hysicr~ - Geophysical 1~rospectln-
ILI ill
Y'Vodelinr- of Varial-Ae ElectrOM-tgnntic Yiel~is for of 1 rosp-cl ~r-
uri osf%,
A. G. Tarkhov, 1~oscm Glool-Irosrecting inst im S. (--rdZI,mikid-c
1z Ak Nauk- SS-SR, Ser Geofiz., No 4, pr 31P-323
Discussos tho possibility of modeling processes that rovnrn the pror-ag-ition of vtria.Lln-
electromaRnetic fields in nineTal rocks. Briefly dencril%es a rnodelin,~,! arparatus eriployed,
in lab expts. Gives the rc-sults of observitions with conduct:ln~ plates; also 7ives resr-Its
of sulmerging plates in water. EstablisYes that tl-e induction current, rxeited ',y L'~
extcrnal field in massive conductors is of a vort-ical charact,~r. Pervirks that for '_.! 13
reason the d-.t, obtained in electroprosrectim7 by T-eans of ali~cmitinrr currents raist
be interpreted in order to rake r--ceiv,-rs accurate. ?65 TF11
PHASE I TREASURE ISLAND BIBLIOGRAPHICAL REPORT AID 6T4 I
1300K call No.: AF660087
Author: TARKHOV-, A# Ge
Full Title: Geophysical EXploration by the Induction Method
Transliterated Titlet aeofizicheskaya razvedka metodom Induktaii
PUBLISHING DATA
Originating Agency: None
Publishing House: State Scientific and Technical Publishing House
of Literature on Geology and Mineral Resources
Date: l9r'h No. of copies: .. 5,000
No. pp.: 95
Editorial Staff
Editor: Prof. A. I. Zaborovskiy
PURPOSE: A textbook to satisfy the requirements for a book on the
contemporary scientific level.
TEXT DATk
Coverage: The book is divided into an introduction, four chapters,
a conclusion, and a bibliography. The introduction gives a brief
historical review of the method of induction started in 1927 and
developed by I. G. Mikhaylov., A. M, Pylayev and A. V. Khoromskiy,
who introduced methods of observation and apparatus, The method
of resistance gave way to the method of induction by alternating
electrical currents which since 1946 has been in the process
of further research by a group of members of the Geophysical
Institute of the Academy of Sciences under A. N. Tikhonov,
1/2
Geofizicheskaya razvedka metodom induktsii AID 674 1
corr. mom. Chapter'I covers the physical fundamentals of the
induction method; Chapter II, field work with the application
of the method; Chapter III, sources of handicaps of non-
geological origin; Chapter IV, application of the induction
method to the solution of geological exploration problems,
enumerates in abstract form the conditions and results obtained
in the application of this method in nine regions of Russia.
In the conclusion, the author mentions the future development
of Wis method with emphasis on the modeling, the study of the
phase structure of the fields, etc., and discusses,, for example,
the method of exploring the electrically conductive sulfide
deposits. In view of the complicated structures of the deposits,,
the author attributes much importance to a minute geochemical
exploration. But this is impractical becausc of the time
necessary for the work and the high expenses, and may be sub-
stituted for by the geophysical Induction method. The text Is
illustrated by many formulae and 60 diagrams, graphs, photoplates
of instruments.
No. of References: 15 Russian (1933-1953) and 2 American
Facilities: None 2/2
T OT, A. G.
Determining the deptb of underground conduction bodies by
the induction metbod. RazvedA okh.nedr 20 n0-103-36 Ja,-F
154. (MM 9:12)
(Prospecti W -Geophysical metbods)
(Induction (Blectricity))
ARASIMWICII, V.14., dotsent; VESEMV, A.L. professor; VOWTKOVSKIT,
S.A., professor; ZHUKOV, L.I., dotsent; IMLITOV, M.D., dotsent;
KUTrUkMN, P.I.,doteent; KOMPANNSTS, V.P.. dotsent; HALAKHOV,
A.Te., professor; MWACHIN, G.I., dotsent; RrABUKHIN, Me.,
professor; SAKOVTSEV. G.P., dotsent: STOYLOV, B.A.. dotsent;TROP.
A.Te.,dotsaut; FEDOROV,S.A., professor; YAROSH, A.Ye., dotsent,
redaktor; TAMOV, A.G., redaktor; GAMBURTSIVA, Te.Ye., redaktor;
GUROVA, O.A-.7-TMMNTeWskiy redaktor.
[Collectioneof articles on geopbysical methods of prospecting]
Sbornik statei po geofizicheskim metodam razvedki. Moskya.Gos.
nauchnn-tekhn.izd-vo lit-ry po geol. I okhrane nedr, 1955- 109 P-
(MLRA 8:11)
1. Sverdlovsk.Gorig7 institut.
(Prospecting-GeopbYsical methods)
FD-2578
Card 1/1 Pub. 44 8/19
Author Tarkhovp A. G.
Title Waveguide properties of mining operations
Periodical Izv. AN SSM, Ser. geofiz, Jul-Aug 55) 358-363
Abstract The basic theories of radio waveguides can be used to study the
propagation of radiowaves in mine tunnels. The use of compara-
tively long waves gives greater effects. It is found that the
presence of transverse shafts and variable shaft croes section
cause changes in the field intensity. Artificial conductors in
mines sharply distort the field and thus make separate sections
difficult to study. Four references.
Institution : Moscow Geological Prospecting Institute imeni S. Ordzhonikidze
Submitted : February 1, 1954
TARKHOVI A.G.,- VANTSTAN, G.M.
ProspectIng bydroolectrometry, Usred.i okh.zedr 21 no.5:
37-" 5-0 '55. (=A 9--12)
(Geochemical prospecting)
(Blectrometer)
'PAR OV, A.G.
Using radio wave attenuation for determining the electric properties
of rocks. Izv.AN SM.Ser.goofis. no.3:399-608 My '56. (NLRA 9:8)
1. Wentrallayy geofisicheskly trest, Nookovskly geologo-rasyedoch-
nyy Institut.
(Radio waves)
(Rocks-Ilectric properties)
(Prospecting-Geopbysical methods)
~
Using magnetic progpecting methods In mining are", lsT.AJF SSSR,Ser,
980fis. no.8:.1005-1007 Ag 056; (MIRA 10:1)
(Prospecting--Geophyvical methods)
TAMr
~ktor fisiko-matematichookikh nauk.
~0,.PO~V~G,,. ~,d4~~
*Using the natural electrical field in electrical prospectine bjr
A.S. Semenov. iteviewed by A.G. Tarkhov. Isv, AN SSSR.Ser.geofis.
no.11:1364-1366 N 156. (HLRA 10:1)
(Prospecting-Geophysical mothod;)(Terrestrial electricity)
(Semenov.A.S.
TAMMOV, A.G.
Review of collected articles of Veophysical Prospecting zethods.s
Razved, I okh, nedr 22 no.9:60-63 8 156. (KLRL 9:11)
1. Moskovskiy Geologorazysaoohnyy inatitut.
(Prospeoting-Geophysical rmthods)
TARKHOT, A.G. I
%.......... W1.0,104or
.12141,114 1 ~,) ;x,;w.
Dispersion of electrical properties of rocks. Trudy WRI 29:234-242
156. (MLRA 10:4)
properties)
(Rocks-glectrical
YSHxw' GJ.; BRITAUT, M,D,; 'PAR V, A,G,- SHCHIRBAUT, A,V,j J=M,
T.M.. glarw rsd.;SH&2AWV To.T. zamstlUll glavzwgo red,;
mmoymm, B.Ne-v red.; ZZINH u DoA**- red.; Munuar. V.I.. red.;
NIFONTOT, P.T'O, red.; SKIBNOV. V.I.. red.; IMMOOT. N.A.. red.;
TAK~ZIN. A.A.. red.; XUKHIN, S.S., red.; ATMIUVA, ToA*, takhn,
red,
[Prowpecting for ferroms mital deposits] Razvefts.,mestoroshdonil
chernykh metallov. Moskva, Obs. mucbno-tekhn, lxd-vo lit-ry po
geol. i okhrane nedr. 1957. 102 P. (Natodicheekle ukasaulla po
proUvadetym geologo-raivedochufth rabot, no.11). (gru 11:1)
(Iron oreaY (Prospooting)
MMUSHCHOV,, N.A.; KOSOV, B.M*; POLIK&RPOGHKIN, V.V.,- BRI?ATWe X,D,; TO OT4,_
A,G,; SHOWMA OV* A.V.; EMMM, VIM'@ gli~vnyy red.; SHATA .4 p - Yoe, -&-T, I #
zamostitall glaynago red,; morlwo-BONO, red,; ZMOT, DeAs, red,;
DADNIKOV, V. 1.
. red.; NIPOMV, R.T., red.; SMIRROV, V.I., red,,
YMBIN, A,,A*, red.; VM2". I.V., red. lvd-ya; AVARKITATA, ?.A.,
tekhn. red.
[Proapactinc for molvbdenum, tungsten, tin, biamth, antinomy,
I
'anstoroshdanil molibdons, vollfram.
and arcury deposits Razvadka
ol6va, viammta. surluV i rtutis' Koskya, Oos. nauahno-tekhn. izd-vo
lit-ry po geol. I okhrane nedr, 1937, 130 PO' (Mstodicheskie ukazantia.
po proizvodetyu goologo-raxvsdochnykh rabot, no.6). (MrU 11a)
(Ore deposits) (Prospecting)
AMMASIANOV, A.Ae; BRITAYJVq M.D.; BYBOCKKO, A.Me; ZXMWg D.Aw; TARKHOTO
:A.G~j TSYGANKOO N.I.; SHCE3VIRaOT, A.V.; MWIM, V.M.P glavW
red'. MTALOV. Y&O'T.,.zamentitell glavnogo red,*; EMCWBm, B.I.,
red,; ZMKOTO D&Aa,'rede; KRASIIIKOV, V.Ie, red.; NIFONTOT, R.V.f
red.;.SXMNOV, V.Io, red.; KMSHCHOT, NeAs, red.; YAKZHIN, A*'Af,
red0; VWTAK, G.V. red. izd-va; AVJNIYBVA, T.Ae, tokhn. red.
[Prospecting for copper, lead, and zinc depositel Razvedka mesto-
roxhdaull medi, svintea i tainkEL. Moskva, Goo. iijiuchno-tekhn, izd-va
lit-ry po, geol. I okhrane nedr,,1957. 135 p. (Metodicheskie ukaza-
nil& pa)proizTodstya geologo-rawedoobnfth rabot, no.10).
(Ore deposits) (Prospecting) (KIRA 3.1 -.4)
SOV/169-59-2-1231
Translation from: Riferativnyy zhurnal, Geofizika,1959, Nr 2, p 31 (USSR)
AUTHORS: Tarkhov, A.0 , Barkov, V.S.
TITLE: on the Method of Electric Profiling in the Case of Nonuniform Overlyarden
PERIODICAL: B~ul. nauchno-takhn. inform. M-vo geol. i okhrany nedr USSR, 1957, Nr 7
(12), pp 34 - 37
ABSTRACT% It Is presumed that Vie apparent resistivity 91k obtained by the little
device will bs. indicating the influence of the overburden, while the
great device AB makes it possiblai to determJne the value of 9 k dependlpg
on the deep-seated rooks, when ons oarries out the investigations by the
method of symmetrical electri3 profiling according to the AAtMBIB scheme_
Sharp distorting influenoes occur, wh,.4n t1he overbur-ien Is non-uniform and
variable in Its thickness. It was attempted to repment the r,,,sults of Vin
electrio profilJpg in the form of the graphs 9k/91,, showing a considerable
simpliaity, for the purpose of ths elimination of the influences mentionsd.
A similar method of treatment was applied to engineering geological prospec-
ting in the Far East and in the Perm' region. The graphs of the ourves
Card 1/2 9 ~' 9k, ar-d 9 k/ V k' obtained in the Perm' region for A I B' - 100 m and
SOV/169-59-2-1231
On the Method of Electric Profiling in the Case of k6r.-Uniform Overburden
AB - 400 m,and recorded in the region of karst limestoneslare presented. The curves
9 k and ? k mark the karst zones by maxima in the ourve, but similar extrema,are ob-
served also in other points out of the karst zones. The curve,of the 9 4/? k ratio marks
the kar5t zone by a very distinct minimum. The curves V k, 9 k, and p k/ 9 L obtained in
limest?nes without karst formation are also given. It is noted Pat the curve of the
9 k/9 k ratio has a smooth character, but the curves 9 and 9 k are very jagged. The
author summarizes that the practice confirms some advantages of the relation method.
An analytia wMlanation cf the relation method is given. The author recommends the
testL,,,g of this method in geological mapping and in prospecting for mineral resources.
E.N. Kuz'mina
Card 2/2
--- --- -- ---TAz!K;IQV, --- --- -- -- - - - - -- - - -- ---- - ---- - -- - -- - -- -
-1 -- -
Blectric reconnaissance techniques for detecting pure anomaliec.
Izv.AN SSSR-Ser.geofiz. no-8:979-089 1,r, '57. (HLRA 10:8)
l.Soyuzny7 teentrallnv7 goofizicheskiy treat.
(rrospecting--Geophysical mothods)
(Mag-notlem, Terrestrial)
-TA A. 6~
TARMTe A*Gv
Kethod fol' deterninlug'the capacity of pumps* Plasyed. I okh. zedr 23
n9.9s34-r35 4 '57,. (NIU lotil)
1. Moskewskiy goologorazvedochnyy institnt in. k Ordshonikidne.
(Pumpirg machinery)
DAMOV, V.N., prof.. doktor geol.-minero nauk; S-014LIVICH, Tu.S.. kand.
telchn.nauk; , prof., doktor fix.-mat.nauk, red.;
KkWrZAROV, A. ., vedusbchly red.; PMTOVA, I.G., takbn.red.
[Exploration and working of mineral deposits; proceedings]
.Razvedka i ratrabotka polezrgrkh iskopaeuWkh. Hoskva, Goa. nauchno-
tekbn.izd-vo neft. i gorno-toplivnot lit-ry, 1958. 250 p.
(MRJL 12.-l)
1. Vaesoyusnaya nauchno-takhnichovkaya konferentsiya, po pri-
meneniyu radicaktivrqkh i stabilfrifth izotopov i i2luchnniy v
wxndnom kbozyaqatva i nauke, Moscow, 1957. 2. Moskovmkiy
neftyanoy Institut Im. 1.M. Oubkina (for DakbuoT). 3. Institut
nefti All SSSR (for Shimelevich).
(Radioisotopes--Industrial application)
(Mines'and mineral resources) k0il wells)
BARMOV, Oleg Aleksanclrovich; BLINOVA, Nina Hi.k~aylovna; VnORNYKH, Sergey
Fedorovich; GULIN, Yuriy lleksandrovich; DAIMOV, Vladimir Nikolaye-
vich; URIONOV, Vya6heslav Vasil 'yevich; , XHOLIII, Arkadiy Ivanovich;
,:WUWQSvA4A6,vdqktro f lz.-m t nauk, prof*. retsensent; SHCROKBDTAi -
L.loo.vedusbchty red.; PU)SINA, A.S., tekha.,red.
[]Radioactive methods of research in oil and gss wells] Radioaktivuye
metody iseledoventia neftianykh i gazovykh okvazhin. Moskva, GOB#
naucbno-tokhn.izd-vo neft. i gorno-toplivnoi lit-ry, 1958. 314 V.
(Oil well logging, Radiation) (HIRA i1:6)
TARrHUV A .- G.-
"Statistical Treatment of Findings in Mass Determination of
Physical Properties of Sample3 of Rocks."
-2517 C2.
P
::n
TAWOVO A,Ge 'a" Igy. y1g. uchab. &v.., geol.
d sophysima pro Otings 2
UAd6rgroun mu iis6)
i v,,sv. no.ItIO7-123 Ja '58- ingtitutI Goofisichaskiy faloill-
1. HOObDVskiy 9001090-rasv6dochM7 a
tat** (pro opeating-%opbysical mthOds)
4f~ K, ) V~
N
AUTEORSi Authors c'
Prospect ins,-11
TITLEs Remarks on
symposim
tekhizdat,
na sbornik
tekhizdat,
PERIODICAL: Razvedka i
132-58-3-12/15
VIRG EVMposium on "Geophysical Methods of'
the Review by A.G. TarkboV of the VIRG
"Geophysical Meth6ds of Prospecting")Goageol-
1955 (Zamechaniya po retsenzii A.G. Tarkhova
VIRG "Geofizicheskiye metody razvedkill - Gosgeol-
1955)
Okhrana, Nedr, 1958, Nr 3, pp 57-59 (USSR)
ABSTRACT: The above mentioned book was published in 1955; the review
of the book by A.G. Tarkhanov was published in this periodical
(1956 - Nr 9). This article is an answer by various authors
of the articles included in this book to the reviewer's cri-
ticism. The authors' names are not mentioned.
AVAILABLE: Library of Congress
Card 1/1 1. Geophysical prospecting-USSR
TARM
Underground observations of the natural electric field in ore-bear-
ing provinces. Izv. v7s. ucheb. zav.; geol. i razv. 1 nd.121-114-122
D. 158. (MIRA 12:12)
i*14ookovskiy geologorazvedochnyy institut im. S. Ordzhonikidze.
(Blectric fields)
TARMOV, A.G.
Statistical methods of working up mass measurement data on the
physical properties of rock specimens. PrikI.geof is. no.20:259-268
158- (prospecting-Geolaysical methods) (MIRA 11:11)
10-1 _V A.G., prof., doktor
WHMV. Vladimir Nikolayevicbj professor- TARKIP
ftsiko-mat.nauk; PERSHINA, Te.G.. YWITOTA. I.Go'
tekbn.red.
(Industrial geophysicei methods of Industrial geophysics. apparatus
and equipment, electrical methods in oil wall loggliAl. Prorwelovaia
geofixtka; metody promyslovoi geofisiki, apparatura I tborudovanie.
alektrichaskin metody iseledovanita. skvashine Moskva. Goo. nauchno-
tekbn tzd-vo neft, I gorno-toplivnoi lit-ryt 1959, 694' p.
(MIRA 12.-2)
(Prospect~vg--Geopbyslcal methods) (Oil well loggirig)
SOV/49-59-4-19/20
AUTHOR: T kh
TITLE: On the Relationship of the Geophysical Fields (0 vzaimnykh
svyazyakh geofizicheskikh poley)
PERIODICAL: Izvestiya Akademii nauk SSSR, Seriya geofizicheskaya,
1959, Nr 41 PP 635-637 (USSR)
ABSTRACT: The author gives a short account of 4 books on the above
subject. The books, which are listed in the 4 references,
are as follows:
(1) On the determination of electric characteristics of the
Earth's crust, by A. N. Tikhonov.
(2) A method of investigation of the seismic phenomena, by
G.A. Ivanov.
(3) The relationship between the potential anomalies of the geo-
physical fields and their complex interpretation, by A. A.
Nepomnyashchikh.
(4) The relationship between the electric and gravity anomalies,
by Yu. P. Bulashevich. There are 4 Soviet references.
SUBMITTED: May 12, 1958.
Card 1/1
-- - --- --- - -- --- --- -- --- ---- - - ---- - - - - - - -- - -- -- -- -1
- . - ALIPIN L.M.; TARKHOV Atg~.-
I ;ing
Geophysical Department of the Moscow Geological Froopecl
.Institute, Trudy MRI 36:3-6 '59. (MIRA 15:5)
(Prospecting-4eophysical methods)
I,
TAPJMOV, A. G.
Geothermal methods in the petroleum geolOff; review of
D.I.Dijakonov's book. lzv.vys.uchob.sav*; 9*ol.i razv. 2
041RA 13:4)
no.qa35-141 S '59-
1, Hoakovskiy goologorasvedochnn institut ineni 5, Ordzhonikidze*
(Barth temperatur e)- (Proi~sating-Goophysical methods)
Wiskonov, 1).I.)
TAMOV. A.G.; SIDOROV, A.A.
Working up geophysical data by mathematical methods. Izv.Ali
SSSR.Ser.goofiz. no.10;145~)-1457 0 160. (KIRA 13:9)
1. Moskovskir geologorazvedochnyy institut.
(Prospecting--Geophysical methods)
3/169/61/000/012/027/069
D228/D305
AUTHOR: Tarkhov A. G.
TITLE: Present state and prospects of the development
of high-frequency electrical prospecting
PERIODICAL: Referativnyy zhurnal Geofizika, no. 12, 1961,
37, abstract 12A357 4zv. vyssh. uchebn.
zavedeniy. Geol. i razvedka, 1960,5no. 9,
98-113)
TEXT: The expansion of the geological possibilities of
electrical prospecting can be expected during the subsequent
extension of research on the processes of the passing and for
mation of electromagnetic fieldso especially those of a high-
frequency. The author cites theoretical graphs, computed by
V. N. Nikitina, for the horizontal and vertical components of
the anomalous constituent of a magnetic field created 'by a
flat electromagnetic wave above an inclined conducting vein;
Card 1/2
8/169/61/000/012/027/089
Present state and... D228/D305
these are coincident in their character with the relationshipc
established by modeling. Recent advances in the creation of
apparatus for radiowave X-raying and induction are described.
The need is emphasized for the quickest compilation and publi.-
cation of handbooks and manuals of high-frequency electrical
prospecting, as is the desirability for the further expansion
of scientific research work in this field. Z-Abstracteris
note: Complete translation._7
Card 2/2
VARLAMOV, A.S.1 MIXHAYWV, I.N.;
-TARKHOV,, A. G.
RKITIN, A.A.1 PUCHKOV, YO.P.;
Some features of the method of processing the results of gd.6-
phyoidal reseai6.in direct prospecting for di4monds in tho
Yakut A.S.S.R. Izv. vyo. ucheb. zav.; geol. i raiv..3 no.1230s-
97 D 160. (MIRA 34t 5-y
1, Moska7Bk..Iy goo-Lugorazvedochn5y inatitut imeni S. Ordzbonikidze.
(Yakutia-Diamonds
(Prospecting--Geoph7sical methods)
S/169/62/000/003/020/09a
D228/D3014
AUTHORS: Bogdanov, A. Sh. and T~,~
TITLE: Development of ore prospecting by electrical methods
in the next few years
PERIODICAL: Referativnyy zhurnal, Geofizika, no. 3, 1962, 24, ab-
stract 3A207 (Razvedka i okhrana nedr, no. 7, 1961,
31-37)
TEXT: It is noted that electrical prospecting can be expediently
applied not only for direct orebody searches but also for closely
studying a mineralized area's geologic structure. The replacement
of the current methods of lateral electrical sounding and d.c. el-
ectrical -orofiling by more mobile and productive techniques is of
great significance. In this respect frequency electromagnetic
sounding, whose apparatus weighs,-200 kg, is promising; the me-
thod's depth potential extends down to 400 m. The method of poten-
tial sounding is progressing. The customary eqi-tipment of the re-
sistivity method is used in this technique which is distinguished
Card 1/2
S/169/62/000/003/020/098
Development of ore ... D228/D301
by its hin~h productivity and simplicity of interpreting the obser-
vational results. The new methods of d.c. profiling and magnetic
and phase-amplitude measurement, for which the All/j-)_(AFI-2) appa-
ratus that has been successfully proved in different areas of the
USSR)has been created, are promising. Aerial methods of electrical
prospecting which have successfully replaced surface operations
in some districts, are acquiring especial significance. New equip-
-ient has been developed for the method of induced polarization,
(VP-59), which, on being somewhat modernized, can also be
applied for operations according to the method of field formation.
The methods of high-frequency ground and aerial electrical-pros-
pecting -- radiopiles -- are being practised widely. The well and
shaft versions of the technique of radiowave X-raying are extreme-
ly promising. Z-Abstracter's note: Complete translation.-7
Card 2/2
BONDARENKO, V.M.; DEMMOVICH, O.A.; TARKHOV9 A.G,
Arst results of the combined use of geopbysi&a methods of direct
prospecting for diamond dep6oits In the Yakut A.S.S.R, Izv.vyo
uchebozave; geolei razv* 4 no*2:3.18-132 7 161* (KLRA 14 s 6)
1. Mskovskiy geologorazvedoohnyy institut imeni S,OrdzhonJkJdze.,
(Yakutia-Diamonds) (Prospecting-Geophysical methods)
TARKHOV, A*-Go--; VANTSYAN, GOMO--
Determination of the electric conductivity of rocks and ores
based on the transient grounding resistahce. R&zved i Wch
nedr 27 no.2:53-56 F 161. (MrM 1415)
1. Mookovskiy geQlogurazvedochnyy institut, (for TaIrkhow).
2. Institut eologicheekikh nauk Armnnskoy SSR(for Vantoyan).
(gres-Electric properties)
44568
S11691621000101210291095
D228/D307
MV ITIOR: Tarkhov,
TIM': Electric prospecting by the radio comparing and
direction finding (Iradiokip!) method
PERIODICAL: Referativnyy zhurnal, Geofiziha, no. 12, 1962t 44,
abstract 12A353 (Razvedka i ol-.hrana nedr. no. 1,
196. It 29-34)
TEXT: The radiolcip method is based on the fact that it
t,tudics the e lectrom "-,,,,ncl tic field in the distant wave zone of radio
station emission. When the dimensions of.areas under investigation
are limited, the electromagnetic wave spreading along Ihe ground
surface can be regarded as Alat, and the intensity of the normal
field can be taken as constant. Complex radiowave diffraction pro-
casses, which distort the normal field and create anomalies, arise
if discontinuities, tectonic dislocations, orebodies, etc are pre-
sent beneath the fround. Data are given on the technique and pro-
cedure of field operations, and the equipment is described. The
Card 1/2
Electric prospecting ...
S11691621000101210291095
D228/D307
scope of the investigation is considered. In the author's opinion,
provided the conditions are favorable, the radiokip method can be
expediently used in solving a number of problems,. for example in
acological mapping, prospecting for ore deposits, approximately
estimating the thickness of deposits and solving engineering geolog-
ical and h rological probleris (findin~,r poclwts of fresh water among
salt water .
abstracter's note: Complete translation
_7
Card 2/2
/62/000/011/013/077
S/169
D228/D307
AUTHORS: Sondarenko, V.1-11., Kovalenkoj N.D. and Tarkhov, A.G.
TITLE: Geophysical investigations of uranium deposits by
the method of radio wave translucence
PERIODICAL: Referativnyy z1jurnial, Geofizika, no. 11, 1962, 56,
abstract 1W37 (Izv. vyssh. uchebu. zavedeniy,
Geol. i razvedka, no. 2-, 1962, 71-82)
.TDCT: The Kafedra razvedochnoy geofiziki 11GIRI (Exploration
Geophysics Department of.the 11G-'tI) undertook an attempt to -apply the
radio-wave translucence method in two uranium deposits and also car-
ried out modeling on models of finite ponductance. The usual shaft-
type e-quipment, including a iiide-baud (from 0.37 to 20 Mc/s) genera-
Itor with 20 fixed frequencies working off a rod antenna, was used in
.the field investigations, as was a standard MA -12-2M (11?-12-21-1)
Ireceiver. In the latter the output was changed from the pin to the
.screened operating antenna. The modeling work aimed at exposing the
possibilities of a new electromagnetic profiling method, allowing
Card 1/2
S/169/62/000/011/013/077
Geophysical investigations ... D228/D307
loperations to be conducted from one mine working. The model had the
form of a box of organic glass plates. In the observations the box
was filled with mineralized water having a variable NaOl concentra-
tion. The results of the modeling confirmed that the radio-wave
translucence method can be applied on objects with low conductance,
In the field work the absorption factors of aft orebodyand its host-
rocks were determined at many points of the deposit. Within the
same horizon the magnitudes of the absorption factor appeared to re-
main practically const-ant; for the deposit as a whole, however, they
are characterized by a rather high scatter. Ore zones differ in com-
parison with host-rocks in their reduced resistivity; this is evi-
dently explained by their jointing, hydrothermal alteration, and sul-
fidization. Observations by the radio-wave translucence method were
,made on.a known ore zone, exposed by a drift and a crosscut. The
ore zone was displayed on the observed curve. The electromagnetic
profiling method was also*tested in drifts. The possibility of map-
ping fault zones is shown.
Z-ASBtracter's note; Complete translation2
Card 2/2
S/169/62/000/009/021/120
D228/D307
AUTHORS: ~arkh~ov, ~A.G.~and Sidorov, A. A.
TITLE: Some applications of the information theory to explo-
ration geophysics
PERIODICAL: Referativnyy zhurrial, Geofizika, no. 9, 1962, 25, ab-
stract 9A161 (In-col,lection: Bostayaniye i perspekti-
vy razvitiya geofiz. metodov poiskov i razvedki pol-
ezn. iskopayemykh, M., Gostoptekhizdat, 1961, 135-141)
TEXT: An account is given of the question of using mathematical
statistical means in geophysical methods.. All tHe ways of mathema-
tically processing geophysical data aim at distinguishing an ano-
maly against the background of obstacles. The volume of useful in-
formation is not thereby increased, but the anormaly/impediment ra-
.tio grows in consequence of the euppresaion of harmful information
This position is illustrated in examples. The set problem is sol-
ved by-means of using different methods of the information theory.
-One of these methods -- the technique of inverse probability -- is
Card'1/2
'S/169/62/000/009/021/120
Some applications of D228/D307
stated. The effectiveness of this method's application is shown in
the example of the processing of the &Z curve for one of Armen*ials
polymetal deposits. The characteristics of the methods of succes-
sive averaging and of successive differences are given. In conclu-
sion it is noted that the creation of specialized computers will
further the successful application of methods of statistically pro-
cessin geophysical data. Z-Abstracter's note: Complete transla-
tion.!~
Card 2/2
KOVALENKO, N.D.; TARKHOV, A.G.
. -.1- --
Prospecting by the use of radio waves in mine workings, Uch,
zap. SAIGIMa no.8sl45-157 162. (MIRA 17s1)
1. Moskovskiy geologorazvedochnyy institut.
-TARKHQX,-A-G..O-doktor fiziko-matem. nauk, prof., red.; KWHINA,
R.N.0 ved. red.; POLDSINA, A.S., tekhn. red.- ---
[Handbook of geopbyaics] Spravochnik geofizlka. Moskva,,
Gostoptekhizdat. Vol.3. (Electric prospecting] Elektro-
razvedka. Pod red. A.G.Tarkhova. 1963. 582 Pe
(MIRA 160)
(Electric prospecting)
DAYEVI D.S.; SERDINOV, A.I.; TARKHOV A.G,-
Mode'ling p*roblems in the method of radio wave probing. Izv. AN
SSSR. Ser, geofiz. no.6t936-945 Je 163. (KM 16:7)
1. 14ookovskiy-geologo'razvedochnyy institut imeni S.Ordzhonikidze.
(Blectrom agn etic prospecting)
Blokh, Ya. 1.. MT. Bondarenko, Find A. G. Tarkhov. _Geornagnetizm
--YT-3-6 3, 003 C,,-?2 i-,2-;
aeron,-)n)Iy;,, v no.
A recent Soviet experiment usitig underground measurements of cosmic rays
to df--tect and delmepte nn -r- beady was f-arri-d out in thc- Central Urals with
a narrow-diiection, 3-v.,ay recor-"ing courae-,- te'.escope. 7!-ie resolu*..-on T,.,re
of the countc~r circuil, was about 5 "sec- and th.- effective iLrea of the telescope
A~ as --hi- ~:nr! thr~ wer-P pow-e.-j bv
t- Was the !~rrl
b-C;Ps- c'); per
::r 4. 58 ::-r. -,i n~! r- r, ia rt z - s e e
r,rn:fita 1,) 3 2' crn-~ , and ouar'.z-a!b,,*.e 7 4 rn
C RAY fEr-OIRDIMS [Contld~ 6, ( L>03/63/003/002 '021 5/02-7
UNDL-AGROMM COM-Ir
The cover rock along the 600-m section was 315-350 m -chick. Radiation was
easured a' 3 points under tile ore body and a, 2 in the country rock. The
r -
m
reFults demonstrated that actual rock densitit-s comparod favorablIv with the~-r
I U. Cos 71i ray m
,heoret-Ically co,-n;tutpf-J v2ities and that ,i,1 vi c easur,'mer,!F
5e -,,.~i-j ~:e 7:1 : "X zi r-..F of --)6 Srv~~
polms and me micmesBe5 ot ovuriying
Card 2/ 2
ISATENKOj M.P.; RUSINOV, L.A,j- SAAKYAN., P,S,; SERDMOVA., A.Se;
TA OV, A.06
-0000000mm-
Reviev of (prof., deceased] A.A. Ikkzhin's book "Prospecting
for urani= deposits," Izve vyos uchebe save; geol* i razv. 6
no.2tl27-130 F 163. (MIRA 3.6:6)
10 Moskovskiy geologorazvedoohnyy institut Im. S. Ordzhonikidze.
Uranim ores)
RAkshin, A.A.)
DYUKOV, A*Ie; TARKHQY,, A*G.
--l- I
"Geophysical methods in areal structural geology" by B.A,Andreov.
Reviewed by, A.I.Diukov, A.G.Tarkhov. Izv.vys.ucheb.zav.; geol.i
razv. 6 no-3tl33-135 Mr 163. (MIRA 16:5)
1. Moskovskiy geologorazvedochnyy institut inieni S.Ordzhonikidze.
(Prospecting-Geophysical methods)
(Andreev, B.A.)
TARKHOV I A.G.; YAKUBOVSKIY# Yu.V.
Review of V. Fritsch's book "Electrical measwements In large
conductors as used in applied terrestrial electricity work."
Izv. vys. ucheb. zav.; geol. i razv. 6 no.91149-150 S 163.
(KIRA 17&10)
1. Moskovskiy goologorazvedochnyy institut im. S.Ordshonikidze.
TARKHOVt A.G.
Effect of rocks on the propagation of radio waves. Radiotekh. i
elektron. 8 no.7:1282-1286 Jl 163. (NIRA 16:8)
1. Moskovskiy geologorazvedochriyy institut im. S.Ordzhonikidze.
(Radio waves)
ALIFIE, L.M., prof., otv. red.i_'j'1f0!OV A G prof.j ZRIM. otv.
red.; YAKUD0V-7'KIY, Yu.V.', doto., rec.
[Transactions of the Ili-Union Inwruniversit~ Sc--'Lentific
Conference rn Inductive Methods for Ore Geophysics] Trudy
I-lezljvuzovskoi nauchnoi konferentsii po in-luk-tivrWr, metodam
rudnoi geofiziki. 11-11osskva, lzd-vo "Ned-ra," 11A4. 123,3 p.
(NIRA 17:7)
1. Vsesoytmnaya mezhivuzovskaya nauchnaya konferer-tsiya yo
induktivnym metodam rudnoy, geofiziki, Mozcow, 1961.
2. Moskovskiy geologorazvedochriyy institut im. S.Ordzhonikidze
(for Tarkhov).
191 NTSLim, Z.G.;
7-91 --!T-DU1N1 [Ldu Shu-tun], P-r,;~~j-~.Lnt
('"'I tayikaya Nam draya Re,:,. .a"
Practice In the statistical procesoing of geothen:r -1 ob,:f--i,-,
.Vation data in the holes of the Krivoy Rog Basin. IL,r. vys.
ucheb. zav.; geol. i razv. 6 no.12tl-17-122 D 163
1. Moskovskly geologorazvedochnyy institut lm. S. Urdnhc,iti~ldze.
130N1)AjTJiKOy V.14.i TARK20VVA,
u
"sing penetratIng c3smin radlaticn to ieterm`ne, the zean density cf
rocks. Razved. i okh. nedr 30 no.L:30-3".1 Ap 16,
(MRA 17:12)
1. Moskovskiy geologorazvedochuyy lriotltut Irravil tl,'ecgo OrdAWkifteo
BI,OyJi,, Ya.L.; DONDAUNKOx V-M-; -KOVALENKOp N-D.; TARKHOV, A.G.
Uoe Of cosmic radiation for the Purposes of underground
geophysical Prospecting. Prikl. geofiz. no-38:142-157 164.
(MIRA 18:11)
ACC Wo AT6028388 (Ah. SOURCE CODE: UR/0000/65/000/00'0/027~/0288
AUTHOR: Bondarenko, V. M.; Kovalenkoj N. D.; Mdrerteova, Ye. A.; Tarkhovo A. G.
ORG: noni
TITLE: Underground geophysical exploration
SOURCE: International Geological Congress. 22d, New D.Plhi, 1964. Geologicheskiye
rezul'taty prikladnoy geofiziki (Geological results of applied geophysics); doklady
sovetskikh geologov, problema 2. 1Moscow, Izd-vo Nedra, 1965, 275-288
TOPIC TAGS: borehole, tellurometry, radio field', ore prospecting, anomaly, gradient,
geophysical prospecting , Gr-,oPi1Ef%5fC 9XeeD1T100J 5 /QA6410 WOIVE. 6F0e_e)v1C_
-45
ABSTRACT: Vield geophysical measurements conducted at the surface are not always
sufficiently deep. An important contribution to this problem can be made by conduct-
ing underground observations in the available or specially provided mines (boreholes).
Radio-wave surveying,which detects differences in rock conductivities is one of the test
available methods. It measures intensity and phase structure of radio-frequency fields
Different modifications have been developed for single mines (boreholes). At present
the method is used for ore prospecting (massive, impregnated, sulphide, and even
uranium ores, the latter generally slightly mineralized). The method may be recom-
mended for locating zones of high water content vhich may be dangerous.for explora-
Card
ACCWR3 AT6028388
tion. The specific character of underground gravity measurements depends upon the
low intensity of the auomalies. This method requires high accuracy of measurements
and allowance for interference (relief, walls of the mine, empty cavities, collapse
zones). Three-dimensional templets have been prepared for small objects. Complex
measurements include general gravity surveys and gradient meter observations. The
method helps to locate the position and to determine the thickness and extension of
the ore bodies which have been missed during mining fcopper and iron). Intensity of
cosmic rays decreases with the increase of the rock mass through which muons pene-
trate. Underground measurements provide the data on'the average density*of the over-
lying rocks (for making corrections of gravity data) and located overlying geological
objects. Tests operations (for copper, iron, and complex metal ores and tunnels)
have been successful; To raise the effectiveness of underground prospecting and
mining, it is necessary to apply other geophysical methods such as magnetometry,
seismic prospecting, thermometry, and various modifications of electric proopecting.
Particularly interesting in combinatioh of surface.and underground geophysical inves-
tigations. Orig. ar~. has: 8 figuresi*
suB om- o8/ E;uBm DATEs o6jan63/ orao nEF: olo/ o7H Rus C02
TARKHOV. A.I., inzh. (Stalinabad) I
Automatiqu in cotton watering. Gldr.1 mel. 12 no-3:20-23 Mr
'6o. (Tagkistan-Irrigation) (MIRA 13:6)
-TARrHOV',-A.il_t_.Inzh. (g.Stalinegad)
V
Shortcomings in the design and construction of Irrigation systems.
Gldr. i mel. 12 no. 1~111 .L5-19 D 160. (MIRA 14il)
(T&JIkietan-Irrigation)
,TARKHOV, A.I.0 inzh.; GUSHCHIN, G.I., red.; MIROHOV, N., tekhn. red.
[Pneumatics and automation of irrigation) PheTmatika i art*=-
tizatslia pollvov. Stalinabadp Izd-vo M-va oellkhoz, Tadzhikokoi
MR) 1961. 42 p. (Irrigation farming) (MIRA 15il)
3 (5)
AMTHORS: Musatov, Do Ial Tarkov2 As Pe SOV/20--126-6-49/67
TITLE: On the Problem oi the Tec'tanic Structure of the Central Part of
the Sayano-Altayokaya Folded Region (K voprosu o tektonichookom
stroyenii to'entrallnoy chasti Sayario-Altayokoy sklad.,hatoy
oblasti)
PERIODICAL: Doklady Akademy nauk 883R, 19599 Vol 1260 Hr 6; PP 1323 - 1325
(USSR)
ABSTRACT: The tectonic division into districts of the Caledonian ?orma-
tions of the Kuznetakiy Alataup of the northern part of West
Sayan, of the.western part of East Sayan and of the foundation
of the Minusinek-inter-mountain-baaine is basLd on a formation
analysis and aeromagnetio knowledg4. The authois separated the
following types of main structure -alements (see Scheme Fig 1):
A. Projections of the foundation of the Caledoni&n geoayncliae
(reiss, amphibolites etc.) a) whioh are reaching the surface,
b hidden under a layer of Middle- and Upper Pale)bo.o,sedi-
M to. a. are characterized by negative magnetic anemalies (po-
tential - naprya,zhennost' up to 700 gamma). Sections of a weak--
Card 1/4 1y positive magnetic field correspond to the case b. The agj of
On the Problem of the Tectonic Structure of the BOY/20-126-6-49/67
Central.Part of the Sayano-Altayakaya Folded Region
the rocks is here Proterozoic. B. The fractures in depth accom-
pany the geosynclinal troughs which consist mainly of terrigen-
ous masses and volcanogenic formations of a basic or middle
composition. The troughs have a distinctly marked linear shape.
The troughs are distinctly distinguished in the magnetic field:
linear bands ofan abruptly varying positive field correspond
to theml limited by zones of great horizontal gradients of the
ATa-values. 7. Geosynclinal downwarpings have a reduced thick-
niss of the cross section. Differentiated acid intrusions are
widely distributed here beside basic ones. The magnetic field
varies here considerably and has a changing sign (more often
positive). G. Geosynclinal elevations have also a reduced thick-
ness, carbonate formations prevail here. Intrusive activity is
inconsiderably developed. Great zones of negative magnetic ano-
malies occur here. The scheme (Fig 1) shows moreover, intrusive
complexes of different age as well as the main structure ele-
ments of the Upper Paleozoio inter-mountair.-baoirsof Minusin-11k.
The following rules governing the tectonic structure of the
said district are found on the basis of the totality of the
Card 2/4 geological and geophysical knowledge: 1. The cross section of
On the Problem of the Tectonic Structure of the SOV/20-126-6-49/6Yf
Central Part of the Sayano-Altayakaya Folded Region
the Caledonian geosynaline begins irith a terrigenous-volcano-
genic formation of a Riffian age (Kuvayskaya series in East
Sayan, Iyusakaya and Portal'skaya nuites of the Kuznetskiy
Alatau; Dzhebashokaya series in Went Sayan). II. The Caledonian
eosyncline developed in the placen of the trough downwarpings
ef 2). 111. The oldest Caledonian structures are orientated
N
in the Kuznetakiy Alatau in north-irestern direction pa=allely
to the trough zone. Structures of ".he north-eastern- and sub-
parallel direction are younger. No 3 downwarpings of the
Kuznetskiy Alatau are the moat connervative ones. Others were
reconstructed. V. The geosynclinal intrusive complexes are
bound in the whole district to downwarping zones with the ex-
ception of the great homogeneous granitic complexes (Ref 3).
VI. The joint of the Lower Paleozo4lo fold structures of the
Kuznetokiy Alatau and of the Fast Sayan is a series of nearly
parallel arcs,the vaulted side of which in orientated to the
north, West- and Fast Sayan are attached to one another in a
similar way. VII. Ths system of the Minusinak inter-mountain-basins
is bound to belong in its totality to the category of the over-
Ca:Fd 3/4 lain stru6tures. VIII. 5 rules governing the interrelation of
On the Problem of the Tectonic Structure of the SOV120-126-6-4916
Central Part of the Sayano-Altayakaya Folded Region
individual types of the Upper Paleozoic and of the Caledonian
fold structures were found. IX. The Devonian intrusions of the
alkaline and subalkaline type are bound according to certain
rules either to intra-geosynclinal elevations or to downwarping
sections. A brachy-like shape of the folds of the Lower Paleo-
zoic masses is characteristic of them. There are 1 figure and
3 Soviet references.
ASSOCIATION: Vaesoyuznyy nauchno-iseledovatellskiy geologicheaki~ institut
(All-Union Scientific Geological Research InstJ
PRESENTED: November 10, 1958, by A. L. Yanshin, Academician
SUBMITTED: November 5, 1958
Card 4/4