SCIENTIFIC ABSTRACT STRAKHOV, M.I. - STRAHKOV, N.M.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R001653420013-6
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 3, 2016
• Document Release Date: August 26, 2000
• Sequence Number: 13
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

STRAMOV, M.I., inzhonor.
... "... ". ", , , , ~- --'- - I
Fabric (pality certification. Tokst.prom. 16 no.!:45-46 Ja 1536.
(Textile 'fabrics) (MIRA 90)

STRAKNOV, M.I., iuz~iennr.
There's a iToat^r assortment of fabrrics at the Glukhovs Conblaso
Tnkst. prom. 16 so*3-.13-14 Mr 156. (MW 9:6)
(jki4usk-w-T*xtllq fabrlcs)

'-, STRAKHOY-U-N.4-
Now fabrics from the 0iwIcT combine. Tekst. prnm. 17 no.3t?-10
Mr 057. (Cotton Olabries) (KM 10:4)

STRAXH07A.-MOLMAL inth.po otdalke
Now footwear fabrics. Tekst.prom. 18 no.10:14-16 0 058.
(MM 11211)
1. Glukhovokly khlopahatobumashnyy kombinat In, Lenina~ '
(Textile fabrics) (Shoo Industry--Zqui*pwnt and su"Ites)

STRAIHOV, 14.1.
14ans of the Otate Ilank to be used for the introduction of now
techniques Tskst. prow. 19 no.Ilt95 1 '59. (MIRA 1322)
Noscow loonosio Region-Textile industry)

M;i i e unit f)r of texti'll, ';;Lricr. If-kst.t rj.,r.. Ll
n~)
GIOtovskiy ;-?,Iopctatohumaztnyy V.orrt inat.
I
(rpxtile machiner/)

STIaMIUVII M. I., imh.
Lowshrinkage finishing of rainymar fabrics. Tekstepromo Z2 uo*2~
52-5) F '62, (,4lkA 15 0)
1, Glukhovskiy khlopchatobL=zhnyy kombinat imni Lenina.
(Textils finishing)

J-
-STRAKHOV, M.L.,inzh. po otdalka tkaney
Shorter.mings of standards in force at the present time. Tekst.prom.
22 no.3:30-31 Yr 162. (MIRA 1513)
1. Glukhovskly khlopchatobumazhnyy kombinat imoni V.I.Lenlna
Mosobleovnarkhoza.
(Cotton fatTics -Standards)

ZiTHAKIfui, H.i., ir-sti.
I
Now col(r chart for i,lAln &!oing- 'ekst. prom, 22 no6*/:tl
JI 162, (MIRA 17: 1)
1. Glukhovokly khlopch&tobumazfjTy kcabinat,,

BALOVNEV, A. V.; �T%AXHOVj F. l., llnzhener p4o ol-Aalke tkAney
Now items in the assortment of tho Lenin Glukhovo Cotton
Combine. Takot. prom. 23 no.1:7-8 Mr 16Y. (MIRA l6tJ
1. Zameatitell glavnogo insh*nera Glukhoimkoro khlopohato-
tumashnogo kombinata imeni lenina (for Bal*vmv). 2, Glukhovskiy
khlopchatobumashnyy kombinat iment I*nina (for Strakhov).
(Glukhovo-Textile fabrics)

L O~4~-/-67 ~;-wr ( 1. Iii (c
ACC NR- A116034936 SOURCE CODE: LIR/0146/66/009/005/000310007
AUT1iOR: Sazonoy. A. M.; PsIonQ20Y. A. 11,; Erigor'yev, S. B.; Strakhov, N. B
_QLernov,Yy. L.
ORG: Leningrad Ele-c.t.r.otech-n-ical Institute Im. V. 1. Ul'yanov (Len n) (Leningradekly
elektrotekhnicheskiy Inatitut)
T I TLE: Spectrometer for the study of broad lines of nuclear magnetic resonance
SOURCE: IVUZ. Prihorostroyenlye, v. 9, no. 5, 1966, 3-7
TOPIC TAGS: spectrometer, nuclear iragneric resonance
ABSTRACT: An all-purpose nuclear maFnetic resonance s trone s been developed
.tss te~
fcr qualitative and quantitative analysis of inotopic concentrations, for the study I
of ultrasonic resonance absorption In the nuclei of some ilkili halide. crystals, and
for structural mea!;urements of naturil compounds. The device Incorporates corrrercisl-~,
type componenLs (see Fip. 1). The NMF detector Include-..% crossed coils and direct
absorption detectors which provide fiigh sensitivity, and a brond range of lif field
Inten,eftles. TIv-, detector can register the nbsorption siFnal or dispersion sIgnal
Isard 1/2 LtD(;: 535.322.2
. I-- _---- ----------

ACC NRI AP6034936
Fig. 1. Block diagram of
nuclear magnetic resonance
spectrometer
j I - NIM sensor; 2 - audio
generator; 3 - device pro-
To viding linear variation of
magnetic field; 4 - current
Y
stabilizer; 5 - phase inverter;
6 - block of NMR detector;
To 7, 13 - hf amplifiers;
U? a IjCZjOIr&Ph 8, 14 - detector and voltm-
eter; 9 - calibrator;
harrvAad
7 10, 15 - audio amplifier;
11 - 5.2-mc crystal-controlled
1-' _j oscillator; 12 - power ampll-
I Am
fier; 16 - synchronous detector
17 recorder; 18 - wave Ueter;
19, 20 - power sources;
21 ferromagnetic stabilizer.
separately without distortion. Ihe frequency range of the detector is 1-43 c#
Orig. art. has: 3 Irigures.
SUH CODE: 20 / SUBM DATE: 2SAug65/ ORIG REF: 003/ OTH REF: 001/ ATD PRESS: :104
Card 2/2 PeXYYN

smll.Ak
rvc Ir tI ~l r
a t mn ~ese. a and
cf *-e :rAnganeoo =Ineralisatitn
'!i. t Vcl. 165. (MIRA le,9)
C.:! '~nRVk ly

YXFRW)Y. HlkNall Timorayevich. K01"HUND.UVA, V.A.. red.; STRAKHOV,
N.I., red.; TASHIMIKINA, Ta.A., takhn.red.
(Seven-yeAr plnn of Kuybythav Province) Semiletnit plnn
Kidbyahavokol oblneti. Xulbyshev, Xulbyshavakoo knithnoe
izd-vo, 1959. IZ8 p. (MIRA 13:2)
1. Pervyy eekratarl Kuybyahovskogo obkom Xonnunistiallwaircy t)qrtil
Sovetakogo Sopiza (for Tefremov).
(Kuybyshev Province--Economic ;oiicy)

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I Aoriy ;h-c-rno-jo r-~ ~.,-ya), Izd. AN 3-3.11 Z-i, iblishing House of the AcadeW of ~;ciencez,
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K v,.)jpr.:iwA o rpisproutm-,pnil mmEpeiltn v oon-lochnjkh porodokh.
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(Skl,j- A-10 If
.Leatno 9 A, I Toyetkovy-a) (Mt. k zn. 6-e-Ql. stro-"njvn ZZSr-., Nov. serl.",
v7p. -1

, N .1-1, .
0 zan.-hentl iovrecsnrq!-,.h oternykh I lagunnvkh vodoyomov i4ft FQznnniya
protoe.,mov oaadkoobrazovant,7-t. Izv. AN SSSR, 3arlya heol., 1,:~45, No, 1, 9 (-,-'-7e,
Fig., Tftbl. Utpr9tura la nAzb.

tll~y caod---)rlA?opl".,Ilyn , I.-Y. AN 33-S)R
~;firljf~ t;ool-, I'VI. No. 2, 1; a. :)-71,

STRAKEDY, X1kolV Mikhaylovich; TANSHIN. A.L., red.; KAPALITICH. B.3., tekhn.
- --- - - roc ---- 11
[Gooloj7 of ths, Kuncurian In the Inhimbay oil &"&] Ocharki goologil
Kungura IshImbaevskogo neftenosuogo ralons. Part 1. [Stratigraphy WA
tootonics] Stratigrafila I tek-tontim. 1947. 140 p. Moskva. Isd-vo
Moskovskogo ob-va Ispytatelet. pr1rody. (Natortaly k posuanitu geolo-
gicheskogo stroenila SSSR j&o.5) (MIRA 110)
(Bashkiria-Geoloa)

the f"Wislity 604 the m*40lan6sm A
flea W go* ?be al"t 1408 % %I *qf
flita, k4j. #41 It N , %. - to-4~ 1041, V., "l.-W!":
00 jArm. /~, 1947.11. -6~10 A ##,.ft - -.1, .4 tfw .00
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AW lot?
Soladto
*Carbonates in Contexporw7 IsSoon Basin szA rA*lr
awwtance for the Problam of Dolomite Ironatifto*
S. IL Strak2wv, 33 pp
03yull Moskov Obah Isp Pri, NOT& Ser, OtGal cools
Tal TrYT, No 4
DUmusess data an the carbonate regIm of the "agoon
ma salins lakes or the Azov, Black an& Caspisis sea-
ooests, and the carbonates In their bottca 6sposits.
Dlwt1nolsbee tvo tv"s of lagoonas 1) those with is-
poosite or calcite Owst exclusively, with ina4m4ri-
coat &a-' ure of dolaalte, au& 2) tbose vith oalolte
LC 49M
OW/Geoloff (ContA) Apr lgk7
&*"site or muLn wainity, an& vith calcite and
S"welte or high "Unlty, with Insignificant &A-
uIxture of aolculte. fty'.4% formiation of ao2=dto
"~ aspenaeut upon the C02 concentration In the air
ISA the alkali= reserve in the sea and logoon vater.

a 0

TISS "00 of 10~4 as Me f-00"16" cs,t~slv
N f .,.j 14.4 .%,

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VM/1174roloff Jul/Aag
Potamolow
Usinology
"DIstrIbution of Iron In the Sedimente of lake and
Sea Systems and Factors Controlling It,* N. M.
Stralchor, 48 py
"It Ak Xwk SSSR, Ser Geol' So 4
Tk4wte subject under folloving, (1) types of Iron
u1sralion In river vaters, (2) distribution of per-
--'oeotage concentrations of Iron in deposits of non-
aloeral lake and sea systems, (3) distribution of
absolute =sees In vater systems, (4 ) peculiarities
'AM /Rydrology (Coutd) Jul/Aulg
of the ore deposition process In Iron geochemistry,
and (5) geoeml schmee of iron distribution In
sea and lake systew. Includes ten tables, 19
diagram
17/49?"

UZ;3B/Geology - Sediment Formation Nov/Doc 49
"11v;-io,J1cPY anal Irreversible Evolution of Sedl-
m-nt Formution In the History cf the Earth,"
?I- M. 3tra~liov, 42 pp
"1z Ah Nauk =R, ~;er Crcol" Do 6
Analvzes factual data pertaining to the entire
area of contemporary continents to formulate the
laws of per1cd1c behavior of the sedimentary
process and to develop concrete characteristics
cf its Irreversible evolution in the history of
the ear*h.
W*
152T41

USSR/Oceanography - Sedimwntation Jan/Feb 50
Bottoms, Ocean
"The 1.aws and Mechanism of Marine Sedimenta-
tion- II, The Caspian Sea," N. M. Strakhov,
31 pp
"Iz Ak Nauk SSSR, Ser Geol" No 1
Discusses laws governing distribution of clastic
material, calcium carbonate, Iron, manganese,
phosphorus, and organic substances in present-
day Caspian Sea sediments. Gives comparative
characteristics of sedimentation process In
Black and Caspian seas.
.-Om i56T82

tl.(- tk-ncral 7",.o,,jrj r;f t4hu- by N. M. S'ITIAYJ,
f - I" Ak. A-Lk, Ser.

----: I - I -
I ~ I ,
C Fut)-13.Xh Poslroyenll7t LIto'.~&I--hookoj teorli. Te--Ifly.
lzv. AN S&M, Serilys Nc- -5,, a. 136-142.

KOROLTUK, I.K.; ~TRWIOV. HA'; GxKXKR, R.F.. redAter; SPRYGINA, L.I.. redaktor;
SHNVC.WIXO, G.H., t_ekhnIcheekI7 redaktor.
(Limestone hillocks and conditions of their formation in PodoliaJ Podoll-
akie toltry i uslovilla ikh obrazovantia. Moskva, Izd-vo AkAd.nauk SSSR, 1952
13P p. (Ak-Ammita nauk S=. Inntitut gnologichaskikh nauk. Triidy. no.110).
(KLAA 9:7)
l.Chlan-korrespondent AN SSSR (for Strakhov).
(Podolia-Physical geography) (Podolia-Corals, Possil)

11 1 , ,
. - 1.~ I ~
lr:~- ,;-" e:o, .
. . -1n."!".. I , " ~ " 1 r,,--- .- .. , .
. 1., 0, ', . 't - ~, ~~ -~C. ,~ I .*, 2
1 " *
.~~c n t, x 1, "Id= ~ 1, Ll-- ~,', T -~ -- LP r-r-- , - , ,: ,:.- , 1, . . .
I ~ c I %, S:l If !,PI.

I F T -vr
HILTANKIN, H.S., akadealk, rodaktor; VLMCIT, K.A., redAktor; AFAMASITIT,
G.D.. redaktor; P3M, A.T.. rodaktor; PUSTOVALOV, L.Y.. redAktor;
STRAKHOT, N.M.. redaktor; TABUMOV. T.S.. relaktor
Resolution of a conference on sedimentary rocks] Reshente move-
shchanlia po osadochnym porodam. Xoskva. Iz4-vo Akademit nauk
SSSR, 1953. 31 P. (91crofilm) (KIJIA 7:10)
1. Chlem-korrespondent AN SSSR (for Strakhov) 7. Akadsmlya nauk
SSSR. Otdolenlys geologo-geografichaskikh nauk.
(Rocks, Sedimentary)

I - ,
t- ;, , e 1- . - . -
. 1 1. 1 1 1 1 i '. , _ , . 1. ~~ I I ~ -I -
I . I I I I I
- I I ~ - , ~ ~ ,, - ;~ ~,^ . - , " -

1'r, nc i "i I ~I ......
Mentions L classes with 2 types In each. (1) Alluvial orpst (a) ores
originatirg durirf weathering of rocks containinf, elerants usually associated with
the ores, and, (b) ores formed darinF usatherIne of rocks with an enriched mineral
content. (2) Fragmental sedimentary ores: (a) those created in the process of
mechanical sedimentation (scattering), and (b) tbose origirAtInt at the expense of
now deposits of earlier existing ore horizons (conglomerates). (3) Kemor:enic
sedirentary orest (IL) aedirentary (stratified), and (b) diarenctic (concrctlorwwy).
(4) Dedinentary effusive oresi (a) sedimentary (stratified, block formed), and
(b) dial;enetic (concretionary, disseminated). 25qTh3
0. Monthjl Li,.*t of Russloin Ae~!!-sstons. Library of Congrest, 1953, UncI

ARXRANGILISKIT, A.D., akadealk; ARSINITIV, A.A., redaktor; SHATSTIT, I.S.,
akademik, redaktor; Onu-My. akademik, rsdaktor; VAR74MOT,
M.I., redaktor; AR"GILISIATA, X.A., kandidat geologo-mineralo-
gichaskikh nAuk, redaktor; DOLGOPOLOT. N.N. red&ktor; AUZAN. I.P.
takhnie-hesirly redaktor
(Selected workel Isbrannye trudy. Moskva, Isd-vo Akademil nauk
SSSR. Vol. 2. 1954. 672 p. (XLRA 7:10)
1. Chlon-korrespondent AN SSSR (for Varentsov)
(Geology)

37RAKROY, U.N.; BROVSKATA, I.G.; KWYAZXYA, L.M.; RAZZHIYINA. A.N.-, RATNTST,
N.A,,# SAPM12111rOY, D.O.; SHISHOVA, Te*Ss; BILTARTIN, D.S., aka4omtkg
reiaktor [deceased)- RIZUTOT, P.L.. doktor goologo-vineralogichs-
0
skikh nauk, otyetstvewVy rodaktor; NOSOT. G.1.. re4aktor: AUM.
M.P., tekbnIcheekly redaktor
[Xftrine and continental sedimentation today) Obrazovante osadkov v
ovresennykh vodoemakh. Kooky&, lid-vo Akadoull nauk SSSR, 1954,
91 P. (XLRA 7slO)
;
(Sedimentiktion and deposition)

/

Tj;

7f

STRAXHOV. HM.; RODIOROVA, X.F.
Deochemletry of orpalo mattert 2~ Characterlstles of bitulons of
Devonian strata in thm Iluropean part of the U#3,S.R* Biul,MDIP,
Otd.geol. 29 no,60-25 " 054. (KLaA 8t2)
(Bitumn)

U.'MR/Geology -Hinorals
Card 1/1 t Pub, 96 - 3/40
Authors I Strakhov, N. M., Academician
Title I The fomation and distribution of useful mineral deposits in accordance
with definite laws
Periodical i Priroda 43A, 21-32, Apr 1954
Abstract I The origin of mineral-bearing deposits (particularly those containing
Iron eaid manfAneso) is discussed with a view to establisning a Certain
confortaity to fixed laws in their formation and to determine where they
may be prospected for. In the geological studies made by Soviet scientists
the procosses of former geolor rd to
,ical periods were analyzed In o or
establish the times at which deposits$ different in nature but containing
the saw useful metal# were forried, Drawings; graphsj maps&
Institution i
Submitted i

BUSHUMKIT, 0.1.; rkzUE=. KoKel skadealkg gl&YV redaktor,
SAPOZM,.... Ir.77.07tvOitstrennyy redaktor; 11060T, 0.1.:
rodaktor; XIMTVA, N.A., tekhnicheakiy redaktor.
Lithology of Cretaaeons deposits ofibe Dnieper-Donets
14wland. Trudy Inst.geol.vauk no. 156-3-307 154. NUA W)
(Dals"r Lowland--4*ology, Strat lgraphic )(Donsts Basin---
Geology. Strattgraphlo)

USM/C;#.-vlc,,-.y - Beck
card I /I I-u,,). 46 - h/a
Authors I trmMk ~V. N. nrld zal"'aminn, Ye. S.
Title I )f mithie(,n-lun fet-,is of it-on in
tinll its IL,portance to litholoEy
reriodical t 17.v. AN Sur. k;eol. 1. 34-51, Jnn-Feb 1555
Abstract I Tso, thr, c,:-nf,,m,mPy tel rinturF11 Inv nntr I itt
~,f ferro%jr! of tht. basic ')(_troj"rA,.tj1c
the c;,rtvk'r r-rt;!-,t nrd nnnl~zo:-c the; fc~ctnra which brinC
o~ dlntributi!~n. It out th,~ balonar! of
'i~i,n r 1,.(jcA ir.-n in svJ1m--ntnr,, rocki lind rrenentn
j I
~,f t?o, n-. ti i fee;-:0 L-n of :.,Ancx,7As in th.~ ferrk-',s
C W;47-1~,541'. Tobles; Cr;,phi.
U J: 1, t t

sa) vi (N , ij. m.
Concerntn#: B.11.9rotov's arrangement of chemic^1 differentiation.
Isv.AX S!;!,R. Ser.geol.20 no.4:144-146 JI-AC'55. (MIRA 8:10)
(Geochemistry)

SnUMIOV, 11.14
MAI-,
Some prcblems of sedimentary rock formation OPrInCIPIGS Of
lithology.0 L.B.Rukhln. Revieved by II.M.Strakhov). alul.901P.
Otd.gsol. )0 no.1:71-78 Ja-F 155. Wu 8:5)
(Rukhin. L.B.) (Rocks. Sedimentary)

STRAIWIV,N.M.; RUDIONOVA,K.Y.; ZALWCON.E.S.
Geochemistry of petroleum~bearlng deposits (lower Frotsuian series
of :-,r!-nd 3aku). Trudy Inst.geol.nh-;k no-155:3-115 155.
(HLRA 9:10)
(Second ORku--Geology, StrRtigraphic) (Second Uku-0sochmalstry)

DOLGOPOLOV. N.N.; BUMIXOT, P.L., redaktor; BUSHINSKIT, 4.1., redaktor;
OIKKOLOYARB. B.M.. redaktor; ITANOV. A.A., rodaktor;
it"
skadeolk, otvatetvannyy redaktor; FXSMO, I.A., redsk HoFT"A P#
r; A &
A.Y., redaktor Isdatelletva; AUUN, X.P., takhatcheekly redaktor
(Problems In the geology of agronomic minerals] leprosy geolocti
gronoutchaskikh rud.. Moskva. 1956. 239 P- MRA 9:11)
*4cademiyo nauk SSSR.Otdoloniye geologo-goograftcheskikh nAkuk
(Geology, Scohonic) (Yartiliters and manures)

STRAXHUY, N.M.
, ,
Investigation of diaesneals. Top.iln.osad.obr. 3/4.-7-26 056. (KM 9:11)
1. Institut reolopichoiskikh n&uk Akudemit naulc SM. Xoskvu.
(Rocks, Sedimentary) (Geochealstry)

4 1 t
Ot
i~- J~r t 1'~a likrwm Pat!
;, ::- , '. '~r nip, ~,I~ lyiop vi 5AAt"m
I L I In-.vIprIv. S.
'~r 1~4 ll~ *.~y

(~,n. till

-.5 , ~', I I ~. . '' I I , . :":. - .~ .. I 1 .1 1
-LX ~-A - - - I - - - - --- --- --- --
J!

MUM.

in atarv rorks. I of. Al~ ~v J, J! if

STHAUIOV NJL -,-
-
Types of sedimentation and formation of esdisontary rocks. Artiellp
1. lzv.AN SSSR.Ser.geol. 21 to.5:3-21 my 156. (" 9:8)
N
1. Geologicheekly Institut AN S M , Hooky&.
(Sedimentation and deposition) (Sedisentary rocks)

~;IICHRRTIAXOV, D.I., Akwtsnik; SIIATSKITJI.S., Ak-%d~njk;HIRMM, S.I., akadersik;
STRAYMOV P, A',catisnlk: KOWMINSFIT. D.S., AkMomik; BUTEMIN. A.G.e
ALIVETs, D..'.. akAdonlk; POLKANIT. A.A.. %Yadontk; AFANASI-
TMV, q.D.; VLASOV, K.A.; CHUMIRN. F.V.; IX~rrSKIT. O.D.: PAMNSKIT.To.T..
prorfivar,)r-, BARSAII07, G.P.. prolr*ssor- YX'tS*;!(V, A.D.; IVAIJOV, M.;
TARWYM, V.S.. ARDASIMIXtVA. S.D.
Acittion1clan Vladimir AfnnA8'*TICh Obrucher, haro of socisillst labor;
Obitunry. Isy. AN S!;SR. SAr.gpol. ,.i tio.60-10 Jo'56# (14TRA 9:10)
1. Chlerr-korrespon4jent AkAtle-iti,
Chakhray, Lovitskiy).
(Obruchey,
nank S:'SR (for AfAnAxlyav. Vlasev.
Vladimir Afan*#'yamJrh, 1963-3~1116)

STRAMOV. N. M.
- --- - P - -
"s of sedlmentaj7 process &nd sedtmentar7 rock forvAtions.
ZzY.Al SSSR.Ser.rool. 21 no.8:2940 AC 156. (KM 9: 11)
1. Geologicheskly Institut kkadeall nauk WM, Moskva.
(Hocks, sedimmntary) (Geoloa. Strattgraphle)

Abs Jour: FIli-12i, No lq~`,
Authc~- Strakhov, j;.
Ins t
Conl-,~rnmg Some yethcAulog.'cal Errors In the uf
C.7henk.-al and FliologIcal Deposition and D'kagvnv:i-u (A
Orig [-,L"t;: llyul. 0-,,a lonyt. Pr1rody, 73cologic Sf~--tlcn, 7o1 ~31, Nn 2,
3 -
Abstra--,t: A critique of the scheme proposed by G. 1. Tecdcro-,,1c), (F.!J-Jlllm
2, '1
A 'ro- the "o-..al.-on of dolon."4ez.
Cani 2~; -

STRAIGICY. N.H.. akadomik, otyetstvannyy red., BUSHUSKIY, G.I., doktor
red.; PUSTOYAWT, L.Y.. red.; MABALOY, A.Y.. kand.
P,sol.-min.nauk, red.; KHVCROVA, I.V., doktor geol.-vin.nsuk:
RABIb7SEW, N-I.. red. lid-va; KOU)SKOVA. N.1.. rod.1ti-ve-. UTIII.
M.L., re.l.)7d-vs; XRYNOCHKIIIA, K.Y., tekhn.red.
(Methods for 3tudying sedimentary rocks) Metody izuchenits osadoch-
rWkh porod. Moskva. Goo. nauchno-takhn.itd-vo lit-ry Do geol, I
okhrFine nedr. Vol.?. 1957. 563 P. (MIYA 11:3)
1. Akademiya nauk SSSR. Goologicheakiy Inatitut. 2. Chlen-
korrappondent Ali .5bSR (for Pustovalov)
(Rocks, Sedimentary)

4NIX110T. Konatitntin Kona tantinoy irh; VRAM% N.M
glay"y red.; BUSHINSKIT.
va; FOLUKOYA, T.V., takhn.
rod.
[Lithology of lower Cambrian deposits In the northern slope of the
Aldan mmalf] Litologlia nishookesbritskikh otloshouit savernago
eklonh Aldanskogo mosiva. Kooky&, 1xd-vo Akad. nauk 33MI 1957.
121 p. (Akadoutta nauk SSSR. Goologichaskil inatitut. Truo No.8).
(Aldan Hichland-Rocks, 6adisent"y) (MIRA 11:1)

777~;,. Theoretical *Athology and Its troblems ;'0 tooreticheskoy
I! to I opi 1 1 yeye pro b I emakh)
F -FF- Izvestiy% Akade=ii %auk SSSR, :;eriya :;eologicheskaya. 19,51.
d 11, p Ir-51 (USSR)
"_LRACT: "he author subdivides the science of lithology into three basic
7he first Includes the methods of field and labor-
atory studies of sedimentary rocks. The second pertains to the
ntudy of petrographic types of rocks. The third section consists
of Invostigatione of the general processes and the rules of
rock formation on the earth's surface during the entire geologic
levelopment. For the formation of sedimentary rocks the author
listinguishes two different phases: the Actual forming or
11thogenesis and the subsequent transformation or metagenesis.
!!e denls in detail with the different factors affectine the
formation of sedimentary rocks, such as climatic conditions.
the Influence of organic matter, C021 methane and other gases
nnl tectonic movements. Not only the magnitude of sedimentary
rocks, but also their composition. local distribution and goo-
chemicnl properties are Influenced by the basic structural con-
1/~ litions under which the forming toik place, and are classified

t i cn 11 1 th~, looy nnd Its Froblems
iini in the magnitude of corresponding, zones on different plittejo
nt 4ifferent basic composition of rocks ani at
llilfc~,rent tectonic structure of the plateau can be established
~~n thr- other hand.
1. 4:xperlmental work for the purpose of checking genetic
~.,,,-nc 1,as ions drqwn froaa the otudy of plateau strata must be
r-:lnluctel.
". The exploitation must be bRsel on the total mum of ob-
tq,1r,(A 4qts on the general theory of plateau motagtneals.
r:i ry o If Corgress
r,i

7-- 4 tF
i
f t -, - . -1 :1

5 ,FOrW4IV* -, -
1
YACIOW8 r"l&tIMn0* between low cincontrations of elerients and
riccumillitti,sne of th#jse elevients in high c,3rrentration to deposits
of the !%unl! son*. Zap. Test. Mn. ob-va P6 no.2.-19?-722 '57.
(oro depisits) (Rocks. Sedimentary) (9LRA 10:6)

STRAY'M,V.N.M.. toknl.. c,.Imvr:i.,-, --I., otv. --i.. DOLOCKLOT,
1 3. 1., r-1. ?OV:!IOVA,?.P.. t-'-Ihn. roi.
.1.N.; NOSOVO
[Mlnqrelog,~r 'nni ortein of 'hs=ites, oke t Iv, llr~i n I r - - I or:l to i
gqt,.,3zjs. flopirva, 1959. 4913 0. WRA 11:10)
A, Airaismiya nauk SSM. Otil-glentys geologo-gsogrefichasiclkh neuk.
(Bauxites)

KlIVOWIVA, Irinn VaRiI'yPvnn;. gumm, N.M., akn4emik, glaynyy roi.:
I 1 4
RWITUSKIT, G.I., dokttr gool.-min.nauk, oty. red.; CHIPIKOVA,
T.4.. rstaAtA-va: IY)VICIT.OVA. N.D.. togkhn.red.
(Atlan nf carbnnnto rocks occurtne, in tho ntddlm and upper
Cnrhnntferous of thm Rusistan PIntforml Atlas karbontitnykh porod
nrmAnmro t varkbnogn kArbonn Rijaskot pIntfnrvT. Monkya. ltd-vo
Orti.nank SSSR, ll)Sfl. 169 p. (MIRA v11)
(RtiaslAn Phtfnm-Whonittes (Hinornbry))

N]CMCHXNKO. V.S.: BOCHAROY. M.D.; KRISTOSTURITAR. N.G.; CHERXASOV. V.1.;
AMMUNOV, V.V.; KAUMkN, Y.M.; PAKML&-VOV. V.r.; ZVORTZIN. A.A..
otv.red.; A!iIC!iKOV. N.M., r"d.; BARDIN, I.P., red.; BLAd(MTOT.
A.A., red.; VVEMNSLIT, B.A., red.; ~RUORO M. A.A., r94.0,
XAPUSTINSKIT. A.F.. red.-. KOLHOGOROV. A.S.. red.; NIMTWT,, A.A.,
red.; OPAR1N, A.I., red.; PTMV. P.N., red.; MLMYO T.N., red,;
STaAKHOV, N.X.. red.; YIaOjOVSEIT. N.A.. red.; KOSTI, S.D.. tekhn.red.
[Biographical dictionary of leaders In the natural sciences and
tachnologyj Biograficheskii slovarl daiatelel. estestymanlin
I takhniki. Vol.l. A - L. Otvetstvennyi red. A.A.Zvorykin. Red.
kollegiiii! I.N.Anichkoy I dr. Xoskva,.G*s.nauchn.Izd-vo 'Bol'shals
Sovetskala Utalklopedila." 1958. 548 p. (KIRA 12:4)
1. Redaktslya istoril estentvosnaniya I takhniki Bol'shoy Sovetakoy
Intelklopedil (for Neschanko, Bocharory, KristosturOyan, Charkasovi
Andreyanov, Xaufman, Pnkhmnov).
(Scientists)

--V-- -
. - 4.~; il ~ 9 , I . ...
_-
in ~Tjr'ne LPJA-~Sit3o
m, nrt i.resmVil i t the 5 U 11 ritl . `Aimcntol o,,jr s. ~Pnrva/LAusanr o.
1.
2-7 June 1958.
"C.'. U.,;~~N Moscow

A'j Th~ It - t 'r 1.;"I. t~y '__%. 31
TITTIA,~,- Facto and Hypotheses Concerning the Formation of Dolomitic
flock:) (Fakty i gipotezy v voprose ob obrazovanii dolomi-
tovykh porod)
PERIUDICAL: lzveatiyu Akademii Nauk SSSR, 3eriya Geologichookaya, 1953,
Nr 6. pp 5-22 (USSR)
ABSTRAM Tho author reviews information collected during the last
10 years on the formation of dolomitic rocks. He distin-
guishes two petrographic typos of rocks 1) stratified
dolomite; 2)metasomatic dolomite. After carefully study-
ine all available material, the author comes to the con-
clunion that there is no genetic difference between these
two groups. In both cases the dolomite forming aitterial,
containing magnesium, was deposited from bottom water
durint; the sedimentary genesis stage. The general process
variel for both groups, but the main process was the same.
3tratified dolomites in Paleozoic deposits represent the
primary or se4imentary formations. The metasozatic dolo-
mites are sedi=entary diagenetic bodies, ani dolomites
shich fill fissures, pores or caverns, are spigenotic
'.arl 1/1 7.1ineraln. Their different chemical composition is the

11-58-6-1/13
Facts anJ Hypotheses Con--erning the Formation of Dolomitic Rocks
result of changes in the surrounding atmosphere and water
during different erae.
There Is I table, 9 fieures, and 9 reforences, of which 8
are Soviet and 1 American.
Library of Congresa
Rock-Determination

STRAKHOV, N.M.
- -
.Collected studies OXineralogy of sedimentary formation*#* book 3/4.
Reviewed by N.M. Strakhor. Isv. AN SSSR. Ser. pol. 2) no.8:
124-125 Ag 158. (KIRA 11311)
(Rocks, Sedimentary)

AUTHORi Str&khov, N. M., Academician 20-11&4-50/61
TITLEs on the Types of Iron in Sediments of the Black Sea (0 formakh
zholoza Y osadk&kh Chernogo zorya)
PERIODICALo Doklady Akadomii NaukSSSHo 1956, Vol- 118, Nr 4, pp 603-806
(USSR)
ABSTRAM At present the geologists are of the opinion that the sulfid-
*at hydrotroilito and FOS2 form the only saULIgowum-minoralog-
ical iron typo in the water of the Black Sea which is polluted
with H23. NobodjY has examined this idea in the sediment itself.
Sinos the author is not of the same opinion (reference 1) he
tried to find out to Oat extent this is true. For this
purpose in autumn 1956 samples ol the sediment were taken by
the ship "JLkademik V&ViloVn at 18 places along the coast of
Keykaz in depths of from 50 to 1625 m. The samples tort ana-
lysed according to a several times described method (refor*he-
*a 1,2). The results are given in table 1 and fio-~zre I (I - 111).
Hence 3 main facts are to be founds 1) The iron of the pyrits
and hydrotroilits does not form in any of the samples from the
deep B23 zone the only authigenia-mineralogical ircn type.
Card 114 Lower ferrous oxide, carbonate, or loptochlorite Is alwkys

On the Types of Iron in Sediments of the Black Sea 20-1,18 4-50/61
total water quantity if their content of Car as high as
that of the sediments of the Black Sea (accoldIng to reference
2). Hence follows that the conceptions concerning the 'Aron
types of the sediments of the Black Sea and other similar seas
with H23-containing ground water are completely disproved by
the results of the investigations of the deep sea sediments
of Black Sea. The reason of this wrong opinion was that the
real types of the iron occurring in the seas are not taken
into account. They are by no means solutions, but mainly mech-
anical suspensions of hydroxides and other minerals in river
water as the author points out several times. The ratio bet-
woon suspension and colloidal as well as real solutions
amounts to 97,3 and 1,4% in Rioni,.to 98#9 and 1% in Chorokh,
98,7 and 0,3A inKuban', 91,2 and 2,2~ in Dan, 80,8 and 19,2%
in the Dnepr river, and finally 96,8 and 1,6~ in the Dunay
(Danube) river. These suspensions have considerable sizes of
particle ani consist of an only to a little extent reactive
iron typ: Fe +. In falling to the ground they pass quickly
through the H23 zone and the tine is tooshort to reduce them,
therefor* they are deposited in an unchanged state. Their
further development in influenced by the C -content in the
Card 3/4 sediment, i.e. by the same factor which isoNcisive for iron

On the Types of Iron in Sediments of the Black Sea 20-118 -4 -50/61
also in etas with a normal oxygen regime.
There are 1 figure, 1 table, and 2 Soviet references.
SUBIVITTEii December 9, 1957
AVAILMEt Library of Congress
Card 4/4

STRAKHOV, N.M., nkndemik. oty.red.; SINKIN. S.S., red.izd-va;
NIMMMI, V,Y,, takhn,red,
[On the dimonesis of sediments; collected Articles) K posna-
nitu dln4anaza onadkov; sbornik statel. Moskva. 1959. 295 p.
(KIRA 13SO
1. Andomlyn nnuk SSSR. Konisslys po oendochnyu porodam.
(Rocks, SedtwntAry)

W
HORS
TITLE:
SOV
jtrakhov,
T)ock For=ation anj Tllcr
St,,,,(Js of eii-.101-tvary -1 1Aq I y a
cl) the (0 jtadyakh Vro(loo~.razO
lomenClatur
ik.h nainenovanit)
PERIOnTCAI,: Dolklafly Ak-110',lli nfiuk SSSRv 1J5)? 'Jol 12';f Vr 21 11'
(USSR)

I.RSTRACT

d 1/4 oat stril3s hat ',,--.e ~,iaell =a" in the
In n:)ite of the er in rece.-,t sejimentary
stilly of authigenic min-,ral A
rocks (Rpfn 1, 2, tilare iu, ro -jr.1fromilj .'r. Vlne
in its V.-a
jj,~.ntification of itv c%a,us an- I
author:3 suZjest a syitez~atizutijn of tho 1 -~,3 in
thin fiell. 1) Here mechanical 4.3structio.-I Prevai-'I,
chenlical 40cor"PODItion. 2) ~,.-Arir
1,reronderantly alkaline hy4watior, llmac,.-iine *f
the silicates with the for:;ation of hydro~-,Ie-an q.~-i
1, C"t-LI-el under

I - I
#--'-.Iorite3. 3) COrtin.;atiOr, 0 A,
prepon-lerantly neutral ar-1 ac'Id c~;r!itiOns: Oxilu%10" ani
hyJrolysis of the 3.-licritOs resul.Ing in 1.te of
ka-linite Ariera!.3.
tion of chomical decomiositiorl! cl=!.lete ixldaticn or,-, hyAro-

"r, t!:c, Stai.-oi of Selimentary R-.~A Fur-_~a%.47.n Tlielr
.1 .. on e-~ -it r:!
Ivnin with the forz-atlon .~f _-!.hre, a-1
...Ypercene3ls rms throzoh -il- tha f,)-.- i~-,l lji~;- a at
one of them accorling lo:all Er-.j3l-,.. r-.'-.Tcs rise
to ', wo ty-les cf prolu..;J: il~ ;art!.-lqv ef i f f t-.-ent
Siz.0a rin] nowl
y f -D vn, e o 1 1 J Vi:?!i-j are h;~
_r ked
mincraln, which re:~A`n a 'i na r
wori ther al c1"1 at; !n': 4 ra, c;. -"R-' .1 Z h V 0
. u ., " a i c
remove-i frv= the crust an! a r-'_ a I izr,3. T'
ba callai '-,:-qrsp~rt
~n: to which the fc*Ll.,-JwinF a,; a sh o
"t I"
of the se, limebntary mattor" (I. or, R 3fu I
In rr-~ I '.-, ir it
is by tlia aijthor3 conzilar-11 4 "r:.
1!7 c~ontrnstul 'to f,~~;ma*VYJr.. Alte- 01,
trann;~ort and a.-j ~,%t 2 ns;e,;tl rif A-.' the
'I- -i,.#* I -
tn
tti+ forziation nt,ijo of Cog !je liment, !r 'Abor vi.;,rt. i, TLe
s" I ir-.en ot:
,! n n -i i n ( 11 3 t r a k 1--) t '.1 m , 3 t I d C! I t I A" I 9d
rifter !fjrc we differentlato v_elvapn 2
-onjecutive ntaf~e-, : I ' Se_li=ent3-en~aiu of the 31op.-.valley
leltas, 'In'l 2) of V.e cr~'.,:~hme%t ar~-rn. The rasL'Ats oll state
1) tire oft-m le3tr--~YZIA by
Cari 2114 oo U.al. in n iture no-itly tl.fj rnvillf-~ olf ntrij-,e 2) nre Cr.,zarvedo

SOV/20-125-2-4 3/64
On the Stai7ea of Sedi-entary Rock Formation and Their Nomenclature
In the following s%age - that of diagenesis - the se4iment
is transformed and turned into a selimentary rock. Diagenesis
(according to N. X. Strakhov) comprises: 1) oxidative mineral
formation; 2) reductivo mineral formation; 3) redistribution
of substances ani formation of concretions. The treatment of
diagenesin an a petrification stnee (L. D. Rukh1n) Is inap-
propriate, as the.,r Is no lithification as a rule. Nor to
there any reason for the insertion, between sedimentogenesis
anJ diagenesis, of a syngenesis stage (L. B. Rukh1n). The
ahifting Into the stratisphere by earth crust movements) of
the newly-formed nelimentary rocks marks the onset of the
secondary changes in the PoJimentary rocks. The initial stage
i2 that of k a t a g e n e 9 1 a (A. Ye. Fersmftr, Refs 11 2).
The term "opigenesis" In no% a very happy choice. After kata-
~:eneala, tho selimentnry rocka still remain sod1mentary. In
the middle ;arts of the geoayn,,.l1nalsq the Soliments are sub-
jeoted to more profolAnd chanres, which turn them into meta-
morphoced 3elimen%s (initial metamorphism or metagenosis,
Ref 5). At the metageneato stage, reqrystallization process*#
preponier&te. ..fter a ninkihg to even greater depths a couplets
Cari 3/14 metamorphosing of the sediment takes place. It to transferred

SOV120-125-2-431164
On the Stages of Selimentary Rock Formaticn ani Their Nozonclatuie
into %he class of fully motamcrphit rocks. At this stage the
rock may, however, arain e=or,-,e to the surface and bo sub-
jooted to veatherin,~, 1,rocessen. There are 13 Soviet references.
SlIBIMITTED: December 26, 1)58
Card 4/4

arltwov I N.M. f
Types of aliwitic zonations In the Pont-Proteructi history of the
earth and their significance for geology. ltv. U1 SSSR, Ser. goal.
25 no. 30-25 Mr 160. (MIRA 13:12)
1. Geologichaskiy institut A SSZM. Moskv4s
(Pulsoclimatolorld,
.4

STRWICV9 N.M.
Theory of uediment formation in the h=id V-1t...
geol. 35 no* 3s14-50 My-Je 160.
(Sediments (Geology)) (Ore deposits)
Blul, MOIP, Otd.
(KIM 140)

sTRAMIDT, Nikolay Kikbayloviohl BUSMMIT, 0.1., oty.red.
(BAqcs of the thaory of lithogerseals] Oanavy tacril litolpoess,
Koakvn, lzd-vo Aked.nauk SM. Tol.2. [Composition ond distrlbu-
tion of tmaid sedloantal Ikkonamrnostl sostave I rssmashchenits
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(Petroesnoals)

STRUM, N.M.
r *3
Climate and phosphorus &.cumulation* 0,901. rud. mqstro%h. no.l. -15
Ja-Y 160. (MIRA 130)
It G,3o' institut AS SSla, Kostvat.
(Pboophorus)

STRAXHOV, Hikolity Miklwylovich; 4iJUMINSKIT, G.I., otv.r(M.: 1,100Y. I.I.,
redAzd-va; FOLMOVA, T.P.. takhn.red.
[Principles of -).-w theory of lithogenesis) Osnovy tooril 11to-
gonega. KC9kvn: Izd-vo Akad.nauk SSSR. Vol.l. [Types of litho-
gonesia nnd their occurrences on the earth surface] Tipy lito-
eenez4 i ikh rnimeshchante no 5overkhnoati zemll. 1960, 209 p.
(Pe -- (MMA 13:9)
t,

31 itAKIIRA , :-F. - al-ndur i I L red, ; YAiALK V..'
red.. NOS(N, G.I., reJ. 17.d,vh ii.:UYjUU;p VJ., tokhn. red.;
TIKIA*U':.-0VA', toklin. rtd.
(;,cient. qcdlrx~nts of sons and o2enns; tmnpnctions of a
-onleri~n-,Y 'int?ld on Pay 24-27, 19tCl .3ovromennye osAdki morei
i okennov., trudy -~ove:-,hchnniia ~/.~-Z7 zain 1960. Moskva, lzd-vo
Aktid.nimk SSSR. 1961. p. (MIU 15
1, Aknd-.zlya nauk SWR. KorAssiya pi u9ndoiYnym rodam.
-~--heskly Institit A14 55.Th (for Strnkho-v 3. Invtitut
civeful,)"orii AN SSS4 (for bezru;cov).
, (SuWarine j-~eol,,gy)

~"/169/62/000/010/050/071
D223/,j3O7
0, ,;ul'.!tir conversioa factors in 31ack %'Jea
."Cre-ativny, --al., Gco',`ika, no. 10. 1962, G,
I I a M- 6 1 A.
IL I
abnt-ract 1011,54 (1:1 collection: Sovrem. osadki morey
1961, 634-642)
-r0. tr
p ..0v, =14~ .3.
of Crt =0., 1.1. Vol!
- r, 4nificance
sane colInction.)
OZ WaZer dyna;Ac:-. C.:; a -.Ictor --*'.'I ..,C nCa-,AloZr dirt'ribvition of free
,; I- -_ L. ` the orL;anic mat -
I,', C., -he sa.-.C; t~Gic role oA.
pound The - for-
ter in t,,C comcrnion o-,- j co.-I, Is in then.
1. - r, - f t',-,C hydro-,cn
mation oZ -`rcc ~; in ccii , xc(I in 661c, zone of contact o Aj
A -200 me
n,"12ide and o::ygen rc-,on!-. of the -;!._'C4 Jea at a deptli of 150
w' -c too to in'Luence arl I t1
I:c d y Ic
icre t1ic water novc,::i!in',:, , ~L
e. - - , - ter. L'a diaz;rrras,
r ans i t - on xarl d i r. t r i *-)',, t i on 0 inc.. . an/ ..a ~
.1 o-` ; j-., ncdimcnts a-.-,d the or-anic
.7 Icre tl-.c anounts of VIri,)u5 A. t,
-axis
contcnt in thcm are re:s,,)cc'.:ivvly on the y- and the x
Czrd 1/2

BETEUTINO A.G.; VOLIFSON, F.I.1 GrMlNt A.D.; DUBWNSKlY, V.N.j YEROFETEV,
B.N.; KONSTANTINOV, R.M.; HVEMKOV, M.P.- SOXOLOV, G.A.; STEWQV,,
N.E.; TATARIINOV, P.M.; TORSON, I.N.1 SHADbi, T.N.; SHATALOV, Te.T.;
SHIPULINO F.K.
Meg DmitriWch 14VItakil; obituary. Geol. rud. mestornh. no.2s
3-6 Mr-Ap 161. (MIRA IZ:5)
(Levitskil, Meg Dmitrievichp 1909-1961)

ABLIULLAYEV, Kh.M.; ALTAVDIIN, Y.F.; VJW~SLANOV, A.A.; AllIKEUV, li.P.;
AWOV, Yu.A.; 1WVIOV, G.P.; LMLYAYEVSXIY, N.A.; BOUT, G.P.;
BORUDAYEVSKAYA, X.B.; GOVURUV, I.N.; GODLEVSKIY,, X.N.; SHCHEGWV, A.D.;
SUMOVj F.N.i SHILO, NoA#,- TARMULMl VA*; DRADKINi I,Y*o;
YEROFLYE;Vt B.N.; lEii6HOV, A.D.; IVAK4IN, P.F.j ITSIKSONO M,lo;
KARPOVA, Ye.D..; KASHIN, S.A.; KASHKA1, M.A.; KORZHIMK11, D.S.;
KOSOV, B.M.; KOTLYAR, V.N. KRETTER, V.M.; XUZXE-fS0V, V.A.; WGGV,
S.F,; MAGAXIYAN, I.Gv; MATLIKOV, M.P.; OEXUrSOV0 H,M.; PAVLOVp Ya*Ss;
SATPAYEV, K.I.; SIMIRNOV, V.I.; SOBOLEV, V.S.; SOKOLOV,, G.A.1 STRAKHOV,
4.H.4 TATAIUNOV, I.M.; KHRUSHCHOV, N.A.; TSARaaADSKlY, V.A.) --------
ciluxm0life.v.
In memory of oleg Dmitrievich Levitakill obituraryt Sov,geolo 4
hos51156-158 IV 161. (MM 14s6)
(Lovitakii,, Oleg Dmitrievich,, 1909-1961)

ALITGALUN, M.N.; QNSBURG, I.!.; DUbCVSY.AYA, M.V.; UITUIuV, A.D.;
MZWV, V.G.; W31KIN, RXIMOVA, Yo.V.; -~a~)qLOVNJL;
MiRUSHCHOV, N.A.; SIMIMCHKOV, I.V.; SIICIZ-:~KOV, D.I.;
YANSHIN, A,L.; AMIRASIANOVp A.A.; Comm"i, Ta.D.; ZLINC-V, I.N.1
KOROVXAKOV, I.A.; ORLDVA, P.V.; MOVA, F.G.; SAAKTAK, P.S.;
MURVIEVA, K.F.1 SIIANOBSKIY) L.M.; CIL-Rl=VITOV, Yu.L.j
MIC)IRBINA, V#Vo
lUrii Konatantinovich Gorotakii; obituary. Sov.gool. 4 no.12:
19-155 D 161. OURA 15:2)
(Gorotakiip Iurii Korwtantinovich,, 1912-1961)

AFAKASOYEVp G.D.1 BkR4ANOV, G.Po; VLASOV, KA.; XORZHINSKIY, DS,;
KIRCHDM, M.F.; NALIVM, D.V.; PAVU)VSKlY, Ye.V.j FEM, A.V.;
SMIRNOVO V.I.; N.K.; CHUKMOV, F.T.; SHCHMMKOV, D.r.;
umxcv 0 V.S. _�T- I. . ....-
Olog Daitrievich lAvitakii; obiturary. Izv.AN MR.Sor.gool. 26
no.6tllO-.Ul Jo 161. (KIM 14 t 6)
(lovitakiis, Olog Dmkitrioyich,, 1909-19Q)

h-.YV --' , .'..V . ; .'.T,, -i,- ~ ".') . .
~G.Mtj Of thoi in tb, fiold GI theon'ticel
1-mr,1~1" tx.l[ :~--l-21 ~ 141. (H"?Ji
I
"a0jc,jc.-.aakiy institut AL 1'.csk-va.
j
(Goology)

STRAKB'.V, Nikolay MilkhAyiovich; BUISHINSKIY, G. 1. , oty. red.; NC-SoV, G. 1. ,
red.izd-va; SHEVCI(ENXC.,,, G.N., tekhn. red.; SIMXINA, G.S., tekhn.red.
(Fundamentals of the theory of lithogenesiflOanovy teorli 11togene-
%a. Moskva, Ixd-vo Akad. nauk SSSR. Vol.3.[Charecteristica of the
composition and distribution of arid sediments]Zakonomernosti so-
stava I razzeshchentia aridnykh otlozhenii. 1962. 549 p.
(MIRA 16:2)
(Arid regions) (Rocks, Sedimentary)

U; 1,11'raday rt~xr._-k, LALyrr-at Lordnakoy
-ed.; "LSCV, G.I., red. I -v&;
AS',",IOV, A.V., red. izdl-va; NLIMIC17A, l4eklui. red.;
I v tj i
lN , r' , I ~ . y t e k tz~ . r ed
(Fundar.entals of the theor-y of lithogenovdal Cvnkovy teorli !IV---
';Sl'.
getio za. zd.2. Yo.-kva, Izd-vo kkad. nauk S.
lithogenesle, nl-.d tht~ir distrIbution on the Z~hls surfAMONiFy
litogeneza I M. -lkzr.erYchenle na povorkYmocli zzorli. 19(~~2. 211 p.
Vol.p. (Characteristier, of tLe comiosition and diatribution of
Fl(JUPOU.1 CO(HUZA.111 7.n-k-oncrArnosti rontav-q t razmAchchenlia r~!-ld-
r,-,,:kl-, a Q o7.hc-,,. I J .10(.:. 573 p. 15:
(.;o,As.. kdlmniary)

0;.;~k3toV, A.; I.
Signiricance u.' -.hp. volcaniz ij '-~x for-mation of sedi-entary
rGckJ- jOV-9001- 5 no-9.'F-23 'j 1 G!. (.AdrA 15:11)
1. Gooloricheskly in.,stitut Ali ~ZSIJ.
(Vulcwile aah, tufi'f 0--tc.) (hocks, Sediwntar7)