SCIENTIFIC ABSTRACT SMOLIN, M.D. - SMOLIN, R.P.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R001651720002-7
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: August 31, 2001
• Sequence Number: 2
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

ACCESSION NR: AT4045011
SUBMITTED: 07Janr.4 ENCL: 00 SUB CODE: EK, Ss
NR REF SOV: 004 OTHER: 001
C&d-: 3/3

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AP502o694
UR4~185/65/olo/ooe/0917/0919.
.Kalynovych. D. F.-
AUTHOR:
Kovens kyy, 1. 1. Smolin, K., V
YY, 5 3
TITLE: Diffusion mobility in solid solutions of nickel in iron
Yr
SOURCE: Ukrayinslkyy fizychnyy,zhurnal, v. 10, no.1 1965, 91T-919
TOPIC TAGS: nickel containing alloy, metal diffusion, solid solution
ABSTRACT: The diffusion of both components of two nickel-iron alloys with a nickel
content of 2 and 4 at.% was investigated. A previously described method (Ukr. fizychk".
.zh. v. 8, 1020, 1963) was used, employing wires 0.05 mm in diamett.-r and about 70 mm I I.-
long. A thin layer 2-3 mm long of the radioisotopes Fe55 and Ki03 were electroly~-
tically deposited on the central portion of the samples. After sintering in unij t
_ne4
atmosphere at various temperatures the activity distribution of the tagged atoms was
measured. Since the activity is proportional to the radioisotope concentration, the
ratio of the activities measured at two different points of the sample was equal to
the ratio of the concentrations at -these points. The diffusion coefficients obtained
by processing the data by tvo procedures were averaged and tabulated6.,.The tempera-,
ture dependence of the diffusion coefficients has been found-to follow the usual law.
Orig. art. has: 2 formulas and 2 tables.
ASSOCIATION: Instytut problem materialoznavstva AN URSR [Institut problem mat eri alo--
vedeniya JV? Llk-rSSR] (Materials Research Institute) AN UkrSSR)
l/2
L Card

I

KALINOVICH, O.F. [Kalynovych, D.F.); KOVENSMY, I.I. [Kovens'kyi,
Mobility of a*.oms in a molybdemm-twigstr-tr alloy. Ukr.fJz.zhjr.
10 no.123136'J-1367 1) t65.
1. institur, prvblem materialovedeniya A% Uk-SSR, iK-'y-c'jr,
Submitted It-lecembei-261 1964.

.J."
F It ~ilv('.Ill I C-Fy D~ I.; L FJY, I. I.; SMOL11J,
FIU--ci t rolyn ~ s 41 n sy,: llcm tunva ..
4,leRt,roldhinala I no~12~.148F-3.1-90 11 165. . (f,,-.;-A 1-9~1)
1. Tn.,-~t--tmt problfm Tn-,iterJalo-,rr-.dnrlyh 51-Om"I
ve-rcl~ 30Y 1965.

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ACC NRs
SOURCE b6Dk':..
5/001/012/148811490
1AUTHOR: 441novich, D. F.; Kovenskiv, 1. 1.; Smolin, N& D.
idgitute of Problems of MateriAls _,5_qLe=e,_Aq&d
tut problem mterialovodeniya Akademii nauk SSSX)
I - ~i
,hn the 1TIstenL-1001 denuM tM
ITITLEt Elect!21 sin
SOURCE: Elektrokhimiyaq v. 1, no. 12, 126S. 1408-1420
TOPIC TAGS: tungsten containing alloy, molybdenum containing alloy
(Instl
ABSTRACT: An investigation was made of partial and total transport of matter In tungs-
ten alloys containing 0.1, 15, 20, 25, 35 and 50 &tm I of No. Specimens in the form
of wire segments 0.5 mm In diameter and about 70 im long were electroplated in their
central part with a thin film of radiotracer Mo99 or WIS. The length of the deposit-
ed layer was 2-3 m. A special homogenizing annealing of the specimens Insured uni-
form distribution of atoms along the cross section. The starting position of the tag-
ged zone was measured with respect to the end of the specimen. A marker was made in
order to measure the total transport In the center of the specimen. Constant current
was passed through specimens in an Inert atmosphere. The magnitude of current was re-
gi%ated by rheostats and the temperature was controlled by an optic" pys star. Af-
terlGampletion of the beating, the distrikation of tagged atoms was again measured
Card
UDC s 541. 13

ACC NRs AP6012441
along the length of the wire. On the basis of these measurements it was possible to
calculate the rate of transport v*, where the total rate of transport v consists of
two components
where w is the rate of displacement of the central part. In all the investigated al-
loys, molybdenwn migrated to the anode and tungsten to the cathode. In tungsten al-
loys containing 15, 20 and 25% Mo the latter is predominantly involved In transport.
In the first alloy (0.1% Mo) almost all of the material transport occurs due to tungs-
ten. In tungsten alloys containing 35 and 50% Ko at 20000C, inversion of the sign of
Ithe overall transport takes places Belov this temperature transport of molybdenum
predominates and above it the transport of tungsten become pradminant. In the first
of these two alloys, transport of both components Is practically equal to 22006C.
loriz. art. has:- 6 tables.
SUB CODE t ll , 07/ SUBM DATEt 301W651 ORIG mr, oot#/ M ur: 005
Card 2/2

ACC N
AP6036901 SOURCE CODE: IJR/0226/66/000/011/0057/0061
AUTHOR
Nalinovich, D. F. ; Kovenskiy, I. L ;_S~molin, M D.
ORG: Institute for Problems in Science of Materials, AN UkrSSR (Institut problem:;
materialovedeniya AN UkrSSR)
TITLE, High -temperature mobility of atoms of components in a molybdenum-
tungsten system
SOURCE: Poroshkovaya metallurgiya, no. 11, 1966, 57-61
TOPIC TAGS: molybdenum, tungsten, high temperature effect
ABSTRACT: An investigation was mi ade of the diffusion of two components in
eleven alloys of the molybd enum-;- tungsten system, containing 0. 1. 15, 20. 25, 35,1
50, 6 5, 7 5. 80, 85, and 99. 9 at of tungsten. The temperature range of
experiments, carried out with. the aid of Mo99 and W185 tracers, was 600-1000C.
The values of Do and E (in cal/mol) were calculated for all the alloys-used for the
investigation. Orig. art. has: 3 formulas and 3 tables. [Based on authors'
abstract] [NTJ
:-VO' SUB CODE: ll/SUBMDATE-. WMarWORIGREF: 00610TH REP: 002/

REZNIKOV, A.A.; SMOLIN, M.S.
~ - -1 . 1- --
Immersiou photocolorimeter without clearing agents. Inform. abor.
VSRGRI no.4:141-145 '56. (na 10: 4)
(Colortmeters)

FATEYEV, V.A.; SMOLIN. N.A.
Signalling and control of the operation of the PP-350-IZ unit
for the formation of capron filament. Khim.volok. no.3:64-67
162. (MIRA 16:2)
1. Spetsiallnoye konstruktorskoye tekhnologicheskoye byuro
mashin dlya proizvodstva khimicheskikh volokon (SATB MV).
(Nylon) (Automatic control)

FATEYi~V) V.A., inzh.; SMOLIII, N.A., in"*
~ ~ - - .
Automatic regulation of the wltage of a Vnchronous generator in
a frequency regulated electric drive -%79tilh. Vest. alektroprom. 34
no.8:14-16 Ag 163. (MRA 16:9)
(Electric driving) (Electric generators)

FA,rEyEv, V.A.; SMOLIN, N.A.
Automatic voltage regulation of a eynchronous generator
in a frequency controlled drive system. Khim. volok. nc,.4:
58-59 163. (MIRA 16:8)
1. Spetsialtnoye konstruktorskc~-tekhn(~logicheskoye byuro
mashin khimicheskikh volokcommno

LEVINY V.N.; RABKIN, R.L.; 24OLIN, N.A.
Use of frequency converters in the electric drive system of
synthetic fiber molding machines. Khia. volok. no.3130-32 164.
(MIRA 17:8)
1. Leningradskiy institut aviatsionnogo priborostroyeniya
(for Levin). 2. Spetsiallnoye konstruktorsko-tekhnologicheakoye
byuro mashin lhimicheskikh volokon, g. Leningrad (for Rabkin,
Smolin).

VASILISKO, I.A.; GOTLIB, Ya.L.; RAZZOREMV, F.F.; SMOLIN, N.I.
~j -
Practical instructions for the study, of ice Jame. Meteor. i
gidrol. no.2:55-57 7 156. (MLRA 9:6)
(Ice on rivers, lakes, etc.)

VASILISKDV, P.A., inzhener; GOTLIV, Ta.L.',---inzhener; ZAYMIN, Ye.Ya., inzhener;
MR- .. uzhener; KLIMENND, A.K., inzhener.
Study of water accumulated under snow and calculatlon of maxiTm, accum-
mulations in planning hydroelectric power stations. Gidr.stroi.25 no-3:
37-39 Ap 156. (MIRA 9:9)
(Hydroelectric power stations) (Hydrology)

--ov-98-58-10-11/16
AUTHORS: Gotlib, Ya-L., Zaymia , Ye.Ye., Smolin, N.I., Engineers
TITLE: Ice-thermic Conditions During the Winter Filling of the Re-
servoir and the Starting Up of the Irkutsk GES (Ledotermi-
cheskiye usloviya pri zimnem zapolnenii vodokhranilishcha
i puske Irkutskoy Ges)
PERIODICALt Gidrotekhnicheskoye stroitel'stvo, 1P58, Nr 10, PP 37-43
(USSR)
ABSTRACT: The article describes ice-thermic observations made during
the winter filling of the reservoir of the Irkutsk Hydro-
electric Power Plant carried out by the Moscow section of
the Gidroenergoproyekt. Subjects of study were: drifting
of ice; sludge ice and ice discharges; the ice field and its
movement; the route of the ice and its surveying; thickness
of the ice and undersurface flow of the sludge ice into re-
servoir; water level and water discharge into the lower wa-
ter. The Irkutsk GES reservoir extends 55 km in length when
completely filled. The width of its upper part is 1-2 kilo-
meters, that of the lower an 5 middle parts 2-3 km. Capacity
of the reservoir is 2~1 * 10 cu m and it is 35-36 m deep
next to the power plant. The building of the power plant
Card 1/2 is combined with the dam. The results of various observe-

SOV-98-58-10-1-1/16
Tce -thermic Conditions During the 'Ninsuer Filling of the Reservoir and the
Starting Up of the Irkutsk GES
tions are given in form of graphs and tables, The authors
conclude that a basic change took place in ice-forming pro-
cesses in the reservoir zone whereas in the lower water pro-
cesses remained unaltered. At a flooding speed of less than
G.5 m/sec, there was no underwater flow of the sludge ice.
Vlater level in the lower water rose bY 3.03 m because of
ice jam formations, There are 7 tables, 7 graphs and 1 dia-
gram,
1, inland waterways--USM 2. Ice--Properties 3. Water--Sources
Card 212

Tmiy
470 P. L--n;tL
2,0~K) op',;
Sponnorinr eper.~y: Olevrnoye up-ravlonly* g!e_rc,=cte0rclO9c1,cr-Y
pr' Scvet. x1natrov SSSR.
ResP. Ed.% V.A. Ury-vayow; Id.s V.S. Protopopoy; Tech. Ed.i X.I.
Braynina.
PURPOSEs This work is Intended for meteorologists, hydrologists, and
hydrophyniCthtsy p&rtlcUltLrly those engaged In the study or inow
and lea and evaporation process*$.
COVERAGRi This book contains papers on hydrOPhYsict which were pro-
sentod and discussed at the Third ill-UnIon Hydrological Conference
in Leningrad, October 1957. The Conference published 10 volumes
on various aspects or hydrology of which this is numb -or r'3 The
editorial board in charge of the series Includei V.A. U"vayov
(Ch&lrm&n)o O.A. Alakin, Yo.V. Blizn7ak (deceased), D.N. Borruk,
N.A. Valikanov, L.K. Davydov, A.P. DOmAn1t8kIY, G.P. Kalinin, 3.0.
KritaxiY, B.I. Kudelln, L.P. Manols, M.P. Msnkoll~ B.P. Orlov,
1. V. Popov, A.K. Proakuryakov, D.L. Sokolovokly, O.A. Sponglor,
A.I. Chobotarev, and S.K. Cherkovskly. This volume Is dIvided In-
to 2 sections. the first contains reports rron the subsection
for the study of evaporation processes, and the second contains
reports from the anow and ice subsection. References accompany
.3okol-nIkov, U.N. (Engineer, lAngidtp] PrObleas or the Ice and
Thermal Regimen of rRivers alk Romervalra In Water Power PrOJetta 3k8
Lylo, V.K... [Candidate of 000graphical Sciancom] Variations in
the GlAcIal-Thermal Regimen of the Angara River During the Fil-
ling of the Irkutsk Water Reservoir at a Time or intensive sluc*
Formation 353
09t1lb, To. L., To.Yet Za"in, and
Study 9 or
Winter Regimen of the + While Planning
HydrooloctrIc Power Stations 359
Alelcaandroy
BkiY, Tu.V. [Voo*nt, Candidate of Technical 3cj~nQ4q,),
aKa-A-.X.--M'Imen1m-T1ngln~or1 Planning the Winter Level Itegimn
of the Tall-water of Hydroelectric Power Stations 369
-Svetitek~y_YP~ (Nnginser, SAOOIdep, Uablownt] Winter Roglown
df__th_*__TEY_droQ lee tric Power station or the Chirchik-Dozinaysidy
Cascade 377
Rymsha. V_&_ [Candidate or Technical sciences, 00I Leningrad)
StOd-ying th~ Conditions or lea Development On Rivers Carrying
Sludge Ice 382
Jt-V-- [Candidate of Technical Sciences, 001 ZAningrad)
-Experimental Studies of the Physical Properties of Sludge Joe 391
-Ba
. r_dtr!.Jkox~V~P. [Candidate of Technical Bcl*ncs~, 001 laningrad)
Methods for Studying the Formation of sludge Jose 394
Kravcbmuka-I.-A. (Inalneer, UORS Moldavia, Kishinev) Formation or
Ice Blocking on the Pniestor River and Methods of Studying Then 401
bazA4z1QY_A.A. (Director or the Observatory, UUMS Lithuanian SM)
Reasons and Nedhanics of Ice Blocicing an the NY*uan RIv*r, Pro-
vontion and Control 406
plotrowich_Y-N. (Candidate of Technical Sciences, Tel? Moscow)
R::u.Its of studying the Noltiiig lee Cover on the Klymalainakays
A *rvoir 410

GOTLIB L
,, Ya.L., inzh.; KRAPIVIN, I.V., inzh.; RAZIORENOV, F.F., inzh.;
SMOLIN.-N.11,p. inzh.
Passage of frazil ice over the crest of the spillway dam of the
Bratsk Hydroelectic Power Station. Gidr. i stroi. 30 no.5:34-37
My 160. (MIRA 14:5)
(Bratsk Hydroelectric Power Station)
(Angara River--Ice)

GOTLIB, Ya.L., inzh.; LYLO, V.M., kand.geograficheskikh nauk; SMOLIN, N.I~,
inzh.
Ice-temperature conditions of the tail race of the Bratsk Hydro-
electric Power Station. Gidr. stroi. 3Z no.1:17 Ja '62.
(MJRA 15:3)
(Bratsk Hydroelectric Power Station--Ice on rivers, lakes, etc.)

VASILISKOV, Igor I Aleksandrovich, GOTLIB, Yakov L'vovich; ZAYMIN,
Yevgen.iy Yev.-enlyevich; 51,DLIN, Nikolay Iv8novich-
NOLCHANOVSKIY, A.S., red.; SHI-HOKOVA, red.
LStudy of the winter condition of rivers in water power
surveying]Izuchenie zimnego rezhima rek pri gidroenerg:l-
cheskikh izyskaniiakh. Moskva, Gosenergoizdat, 1962. 199 p.
(MLRA 15:12)
(lee on rivers, lakes, etc.)

GOTLIB, Ya.L.; LYLO, V.M.; SMOLIN, N.I.
Calculation of the ice and temperature regime of the tail
water of the Bratsk Hydroelectric Power Station during
operation. Trudy Transp.-energ. inst. Sib. otd. AN SSSR
no.15:45-50 164. (MA .18:61,

GORDASHEVSKIY P.F., kand. tekhn. nank; KORNYUSHINA, A.P., inzh.;
SM6~N,v N.P., inzh.
Kilning processes must be determined depending on the use
of lime. Stroi. mat. 9 no.6:8 Je 163. (MIRA 17:8)

SMOLIN, q. IS., I(Lt Col)
SMOLIN, N. S., (Lt. Col) Scheduled to defend publicly his dissertation, "The Advanta.ge
of LarF,e-Scale Socialist Agriculture Over Small-Scale Peasant Agriculture and Lar:ye-
Scale Ca 'Atalist A,.,-riculture, 11 for the degree of candidate of economic sciences at the
Military Political Academy imeni V. I. Lenin, on 2 March 1954. (Krasnaya Zvezda, 20 Feb 54)
SO: SUi 163, 19 Jul:,- 1954.

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USSR/Cosmochemistxy - Geochemistry. Hydroche:niistry D.
Abs Jour Referat Zhur - Khimiya, No 2j 1957; 4170
Author
Inst :7Fs-Fitute of Geological Sciencos.. Academy of Sclences
USSR
Title Dedoloirdtization and Disdolomitization on Contact
Metamorphism of -,olctaites of the Aldan District
Orig Pub Tr. in-ta geol. nauk m SESIv, 1955, i4c, 165, 343-173
Abstract Description of the process of dedolomitization and for-
mation of per"clMsic mDrbles (~eci.)-,vposition of dolomite
vi th separe ti-or of ca.16--it-e at a teorperature -'7-, 600-7000,
~ e .1 4berate-a CC~n beiaG Yer-oved 'k.12rough the fissures)
AnL)ng the co-n-tact minerals were observed.- 1) fluorite
and h-waite., since Fe is the characteristic element of
the geocheimistry of contact areas withir. this district;
2) magnetite, the foin-ation of which is associatpd with
metamorphism. of Fe hylro:ddes that were pre5ent, in the
Card 1/2 - 6j. . -

KORWOV, A.A.; S14OLIII, P.P.
Changes in the bird fauna of the forest tract of the Timiriazev
Agricultural Academy of Moscow. Zool. zhur. 39 no.8:1232-1235
Ag l6o. (MIRA 13:8)
1. Irperimontal Station of Forestry, Moscow X.A.Timiry-azev Agricultural
Academy.
(Moscow-Birds) (Forout fatum)

SMOLIN, P. P.
Smolin, P. P. - "On certain methods of changing the nature of animals", Yestestvoznaniye
v shkole, 1949, No. 2, p. 29-31.
SO: U-411, 17 JulY 53, (letopis tZhurnal Inykh Statey, No. 20, 1949).

SMOLIN, P.P.
Book for young investigators of nature OYor young nature lovere."
N.N.Plavillshchikov. Reviewed by P.P.Smolin. lat. v ahkole no.l.,
89-91 Ja--F '55- (KLRA 8:3)
1. Nauchnyy sotrudnik Gosudarstvennogo darvinovskogo mazeya.
(Plavilishchikov, N.N.) (Nature study)

SMOLIN, P.P., metodist.
-~'- ?'-% 1-7- 6.t'~
Significance of vork on the protection and attraction of birds.
Ist.v shkole no-1:77-82 Ja-F '54. Off-RA 6:12)
1. Moskovskaya gorodakeLya stantslya yunykh naturalistov.
(Birds, W-otection of) (Birdhouses)

USSR/Chemical Technologj. Chemical Products and Their Application -- Silicates.
Glass. Ceramics. Binders, 1-9
Abst Jourral: Referat Zhur - Khimiya, No 2, 1957, 5145
Autt.or: Smolin, P. P.
Institution: In~t_it_uYe--6f`_G_eologi.cal Sciences Acade-ray of Sciences USSR
Title: Jurassic Refractory Clays of North Caucasus
Origir.al
Publication: Tr, In-ta geol. nauk AN SSSR, 1955, No 165, 47-70
Abstract: Description of the deposits of Kresnogorskaya and Uchkesenskay-a re-
fractory clays, their mineralogical and granulametric composition,
co-tam-inative admixtures, structure, chemical composition, and new
assuriptions concerning their genesis are made.
Card 1/1

15-57-2-1583
Translation from: Referativnyy zhurnal, Geologiya, 1957, lir 2,
PP 58-59 (USSR)
AUTHOR: Smolin, P. P.
TITLE: Dedolomitization and Magnesia Leaching During Contact
Metamorphism of Dolomites in the Aldan Region (Dedolo-
mitizatsiya i razdolomichivaniye pri kontaktnom meta-
morfizme dolomitov Aldanskogo rayona)
PERIODICAL: Tr' In-ta geol. nauk AN SSSR, 1955, Nr 165, PP 143-
173
ABSTRACT: The action of post-Jurassic alkalic and alkaline-
earth hypabyssal intrusions on Cambrian dolomitic
rocks in the Aldan region (near the village of Oro-
chen) led to the formation of various skarns, oc-
curring immediately adjacent to the contact, and
normal metamorphic rocks in the outer zone of the
Card 1/5 metamorphic aureole. The skarns range from 0.5 m to

15-57-2-1583
Dedolomitization and Magnesia Leaching (Cont.)
7 m in thickness. Among the massive skarn5 are found magnetite,
diopside, magnetite-diopside, magnetite-pyroxene, olivine, pyroxene-
hornblende, actinolite-tremolite, diopside-phlogopite, phlogopite-
hornblende, and phlogopite-garnet varieties. The outer zone of met&-
morphism, adjacent to the'skarn, is locally more than 100 m across
(Zvereva Mountain). This zone is composed of calcite, brucite-
calcite, dolomite-calcite, and dolomite marbles, containing ad-
mixtures of contact minerals. The calcite marbles contain pargasite-
tremolite in addition to calcite. Two varieties are distinguished
among the brucite-calcite marbles, corresponding to almost pure
pencatite and predazzite. These marbles contain minor amounts of
forsterite and associated antigorite, gummite, spinel, and magnetite.,
Secondary dolomitization is typical of a number of rocks. Dolomite-
calcite marbles are the most widespread of the rocks in the outer
zone of the contact aureole. The'CaO.MgO ratio in them ranges
widely. In places, contact minerals are abundantly developed
(forsterite, gummite, spinel, magnetite). Dedolomitization cannot
be cle rly recognized in these marbles. The chemical compositions
Card 2~5

Dedolomitization and Magnesia Leaching (Cont.)
15-57-2-1583
of the contact carbonate rocks of the Aldan region are shown in the
accompanying table. Contact metamorphism, with the formation of
periclase (dedolomitization), was associated with a gaseous phase.
Hydration of the periclase, with formation of brucite, occurred in
a later hydrothermal phase. A still later stage in the contact
process involved the solution of brucite by hydrothermal waters rich
in carbon dioxide (magnesia leaching). This process is indicated
by redeposited brucite and secondary dolomitization.
Card 3/5

Dedolomitization and Magnesia Leaching (cont.)
15-57-2-1583
Components 4
S! La :t u LO u
.0 6; -0- cj S 0
>
u
'c
0
0
0 0 :t--
0
v
:t to
.c
> -
-
E

0 0
- o

0 E
u 4
E- fS
n 0
-0
n F
0
A - n
Si02 6.49 3.99 0.36 10.86 16.67 0.37
T102 0.02 -- 0.03 0.05. 0.09 --
A1203 1.45 o.69 0.17 1.34 8.24 0.51
Fe203 0.40 0.19 0.15 0.20 1.89 0.26
FeO 0.07 -- not detl --
Card 4/5

Dedolomitization and Magnesia Leaching (Cont.) 15-57-2-1583
MnO 0.01 tr 0.01 0.03 0.03 0.03
mgO 14-77 2.17 13-97 20.07 18.67 21.10
CaO 38.20 52.25 39-08 34-07 27-78 37.02
Na20+K20 0.1~2 0.15 tr 1.14 2.10 0.38
H20+ o.18 -- 0.1~1~ 1.07 8.27
H20- -- 0.12 0.09
P205 tr tr -- 0.05 o.16 --
C02 37-50 40-07 46.95 31-55 22.60 31-75
s o.o6 o.o6 0.03 0.23 0.24 0.01
Total 99-57 99-55 99-75 100-03 99.61 99-79
Card 5/5 V. P. Ye.

SMOL1N P.P.
-
Volcanic rocks in Devonian deposits in the region of Solov'yevsk
in Amur Province (upper Amur Valley). Izv.AN SSSR.Ser.geol. 21
no.5:39-47 My '56. (MLRL 9:8)
1. Institut geologii rudnykh mostorozhdaniy, petrografii, minera-
logii i geokhimii AN SSSR, Moskva.
(Amur Valley--Geology, Stratigraphic)

SIAOLIN, P. P. Cand Geol-Min- Scl. - (diss) "Contact Processes of the
Postjurassic MAXIM Intrusions *9w, Aldan.." Nbst 19571-'. 12 pp 22 cmi,
-s Petrography, Mineralogy
(Inst of ttte,Geology of Ore Deposi~, , , and
Geochemistry, Academy of Sciencee',eUSSR), 140 copies (KL,,18-57.',95)
- 15 -

SHOLINO P.P.
~ ~_". ~.:_Cbmpo*-
- sition and genesis of clays in Timpton District, Yakutia.
Trudy IGAM no.10:92-98 157. (KIRA 11-$O
(Timpton District--Clay)

SMOLIN, P.P.
Brucite marble in the area of Satka. Trudy IGIIK no.17:34-45 157.
(Chelyabinsk Province-Wrble) (MM 11:6)
(Brucite)

r
U L_ I N I
Dinvertationu. Branch of Goologloal-Ooographical Sciences Jul.-De-c 1957
Vast. Ak ftuk 8M, Vo. 4, pp. 118-119, 1958-
At the Institute for the Geology of Ore Deposits, Petrograpby,, Mineralogy and
Cleochemistry the following dissertations vere defended for the degree of a Candidate
of Geoloelcal-Mineralogical Sciences:
GAWINj, N. Ye. Pecularities in the Structure of the Deposit of Beloueovsk
in the Altai.
--R!% ~,P.~F. Contact Proceases of the Post-Juranoic Intrusions of the Aldan.
At the Geological Institute the following dissertations for the degree of a
Doctor of Geological-Mineralogical Sciences were defended:
ASIANW, A. T. - Reglocal Geology of Armenia.
GIMMIFARB, B. M. - Essential Regularities of the Fhosphorite Deposits of the
USM and Their Genetic ClasWication.
LUCHNSKIY, I. V. - Volcanism and Tectonics of the Devonian Depressions of the
YAnusinsk Bending of the Intermediate Mountains.
POGULYAYEV, D. 1. -Geological Structure and Mineral Resources of the Smolensk
Region.
At the Institute of Oceanology the following dissertations for degree of
Cand. of Geographical Sciences were defended:
ARKHIPMA, Ye~ G. - Thermal Regime of the Caspian Sea.
ULISTP V. 0. - MOrphology and Developmental History of the Field of Marine
Accumulation in the Summit of the Gulf of Riga.

AUTHOR: Smolin, P. P. SOV/2o-121-1-44/55
TITLE: The Fundamental Traits of Metamorphic Zonality at the Contact
of Post-Jurassic Subalkaline Intrusions and Cambrian Dolomites
of Aldan (Osnovnyye cherty metamorficheskoy zonallnosti na
kontakte posleyurskikh subshchelochnykh intruziy i kembriyskikh
dolomitov Aldana)
PERIODICAL: Doklady Akademii nauk SSSR, 1958, Vol- 121, ITr 1,
PP. 155 - 158 (USSR)
ABSTRACT: The upper structure stage of Central Aldan ( the northern
part of the Aldan-Timpton watershed - Aldano-Timptonakiy
vodorazdel) consists of Lower Cambrian dolomites (uD to 400 m
thick) and of Middle Jurassic terrigenous fresh water sediments
(450 m) which rest horizontally upon a peneplained Pre-Cambrian
fundament. Mainly in the dolomites numerous Post-jurassic
intrusions are localized (Refs 1-3). They are represented on
the whole by alkali syenites and form bodies of different
size and shape, often typical lakkolites. Metamorphic zones were
detected by means of detailed investigations of thle contact
aureoles. They change according-to size, shape, and composition
Card 1/4 of the intrusions. This material is a- tYpical example of the

The Fundamental Traits of 11.1etamorphic Zonality at the SOV/2o-121-1-44/55
Contact of Post-Jurassic Subalkaline Intrusions and Cambrian Dolomites of
Aldan
contact metamorphism of the dolomites. Thanks to the distinctly
marked contact aureoles the transitions from the rocks, which
are to a g7,eat extent metamorphized, to the unchanged rocks
may be easily seen. Table 1 shows a scheme of the typical
zone formation of the aureoles. The total thickness of the
inner zone of the aureoles sometimes amounts to several dozens
of meters, in most cases, however, to only some meters. 3
fundamental zones were seDara-~ed in the skarns: 1)Calcareous
skarns (garnet-, garnet salite-, and salite epidote skarns)
which developed mainly at the endocontact and contain syenite
relics which may be substituted; 2) IMagnesian exoskarns of
spinell-diopside, phlogopite-diopside, and hornblende-diopsidei
3) An outer zone of the magnesian exoskarn of spinell-forsterite,
phlogopite-forsterite, and humite. The outer normal"metamorphic
zone in the contact aureoles of the great intrusions some-
times amounts to a width of more than 1 km and a height of
several hundred meters. Their inner zonality on the whole reflects
a progressive temperature rise towards the intrusions. Thiis
Card 2/4 is expressed by th4character of dedolomitization, furthermore

The Fundamental Traits of Metamorphic Zonality at the SOY/2o-121-1-44/55
Contact of Post-Jurassic Subalkaline Intrusions and Oambrian Dolomites of
Aldan
by the thermal breaking of the dolomite into a periclase- and
calcite aggregate (1 : 1). Periclase is then substituted by
a fibrous brucite which forms very characteristic pseudomorphic
aggregates. The processes of the retrograde metaMOrDhism of
the brucite marble influenced beside the dedolomitization,
though to a smaller extent, the formation of the metamorphic
zonality. The author's observationsdo not confirm the opinion
of.Yu..A.Bilibin.(Ref 2) t-hat a considerable thermal meta-
morphism,.above all a skarn forming metasomatosis is caused by
alkali intrusions only. The author found-the greatest skarn
zones at the contact with alkaline syenites (Shaman mountain.)-.
Forsterite-containing marble is formed around small nepheline-
syenite intrusions, as well as'at the contact with the alkaline
intrusions of similar size. There.are 1 figure, 1 table, and
8 references, which are Soviet.
ASSOCIATION: Institut geologii rudnykh mestorozhdeniy, petrografii, mineralo-
gii i geokhimii Akademii nauk SSSR (Institute of the Geology
Ctird 3/4 of Ore Dql)osits,Petrography,llineralo7j, and Geochemistry
,,AS USSR)

The Pundamental Traits of Metamorphic Zonality at the- SOV/2o-121-1-44/55,
. I
Contact of Post-Jurassic Subalkaline Intrusions and Cambrian Doloiiites olp
Aldan
PRESENTED: March 24, 1958, by D.S.Korzinskiy, Member, Academy of Scie%nces,
TTSSR
SUBMITTED: March 21, 1958
1. Geology--USSR 2. Geological iime--Determination 3- Doleni-ite
--Geology 4. Geochemistry
Card 4/4

AUTHOR: Smolin, P.P SOV/11-59-1-5/16
TITLE: The blica-Bearing Pegmatites and the Absolute Age of Post-
Jurassic Intrusions of the Aldan (Slyudonosnyye Degmatity
i absolyutnyy vozrast posleyurskikh intruziy Aldana)
PERIODICAL: Izvestiya Akademii nauk SSSR, Seriya geologicheskaya, 1959,
Nr 1, pp 45 - 49 (USSR)
ABSTRACT: Coarse-grained rocks of pegmatite type were found by the
author only within the boundaries of the Yakut compound in-
trusive block, south of the town of Aldan. This block,
measuring 6.5 x 3.5 km, is composed of different alkali
rocks with numerous intrusions of augitic syenites in its
north and north-west parts. The composition of these syen-
ites varies from monzonites to granosyenites. The author
gives a detailed description of this block. The definition
of the absolute age of various rocks of the block by the
K-Ar system showed that they all belonged to the same single
post-Jurassic magmatic cycle, and that the whole intrusive
lard 1/2 block was formed in the Upper-Jurassic period. The names

SOV/11-59-1-5/16
The !flica-Bearing Pegmatites and the Absolute Age of Post-Jurassic intru-
sions of the Aldan
of M.G. Zamurayev, E.K. Gerling, S.S. Sardarov, Yu.A. Bili-
bin, I.V. Belov, Yu.K. Dzevanovskiy and Ye.V. Pavlovskiy
are mentioned in this article. There is 1 map, 1 table,
1 photo, and 9 references, of which 8 are Soviet and 1 Ame-
rican.
ASSOCIATION: Institut Geologii rudnykh mestorozhdeniy, petrografii mine-
ralogi-i i geokhimii (The Institute of Geology of Mineral
Deposits, Petrography, Mineralogy and Geochemistry of the
'AS USSR) Moscow
SUBMITTED: October 25, 1957
Card 2/2

SMOLIN, F.F.
I-
Principlea of efficient classification of metamorphosed car-
bonate rocks. Isy.AX SSSR.Sor.gaol. 24 no.12:)6-53 D 159.
(MIRL 1)18)
1. Institut geologii rudzWkh mostorozhdeniy. petrofrafti,
mineralogii. i geokhimit AN SSM. Moskva.
(Rocks..Carbonate--ClaBsification)

SMOLIN, Petr Petrovich; PETROV, V.P., doktor geol.-mineral.nauk, otv.red;
r
d
e 12d-va; DOROKHIlk, I.N., tekhn.red.
[Contact processes in AlUn Post-Jurassic intrusions] Xontaktnye
protsessy posleiurskikh Intruzil Akdaaa. Moskva, lzd-vo. Akad.
nauk.sssH, 196o. 122 p. (Akademiia nauk SSSR. Institut geologii
rudnykh mestorozhdanii, petrografti, mineralogil i geokhimii.
Trudy, n0-38). (MIRA 13:9)
(Akdan Plateau--14etamorphism (Geology))

IOLYAKOVA, N.L.; SMOLIN, F.F.; WDELIKIND, A.M.
Ironless talcites from the Kirgitey depOBitS. Stek. i ker.
17 no.9:28-33 3 160. (MIRA 13:9)
(Tale)

.SXOLIN, P.P.. kand.goologo-mineralogicheokikh nauk
Intrusions of southern Takutia. Priroda 49 no. 12:95-97 D 160.
(KIRA 13:12)
1. Inetitut geologii rudnykh mostorozhdeniy, petrografii,,
mineralogit i geokhimii -AN SSSR, Moskva.
(Takatia-Rocks, Igneous)

SMOLINY P.P.
Characteristiep of the distribution of magpesium si-Ildate minerals.
Geol. rud. mesotorzh. no.2:139-141 Mr-Ap 161i (MIRA .14-5)
(Magnesium silicates)

cn
Co'j'~7-, -lon ci, the
d-
ut -,etrc
Im
-.J-1 5, ME:
aeral c
si]

SMOLIN, P.P., kand.geol.-mineralog.nauk (Moskva)
Iron-free talc. Priroda 50 no.5:57-60 W 161, (HIM 14:5)
(Talc)

smovm, P.P.
-I'-
Kirgitey deposit of talc with a low iron c Altent in Krasnoyarsk
Territory and the origin of' new Industrial tale ores. Trudy
IGEM no.63:66-101 '61. (14IRA 14:9)
(Angara Valley--Talc)

EVOLIN, Petr Petrovich, --kajijq. geologo-miner. nauk-; !VJRNOVA, N.P.,
- red.; ATROSIMBRIKO, L.Ye., tekhn. red.
[New life of underground treasures) flovaia zhizn' podzejm3ykh
kladov. 1,Ioskva, Izd-vo "Manie.." 1962. 44 p. (Novoe v zhizni,
nauke, tekhnike. XII Seriia: Geologiia i Geograftia, no.9)
(Geology, Economic) (MM 15:7)

SMOLIN, P.P.
wGeology of the industrial rocks and minerals"
Reviewed by P.P. Smolin. Geol.rud.mestorozh.
N-D 62.
(Geology, Economic)
(Bates, R'~bert L.)
by Robert L. Bates.
no.6:119-120
(MIELA 15:12)

SMOLINP P.P.
Distribution of commercial talc deposits in the U.S.S.EL and
criteria of the localization of especially valuable talc with
a nonlron content. Zakonom. razm. polezn. iskop. 6:493-548
162. (MIRA 16:6)
1. Institat geologii rudpykh mestorozhdenly, petrografii,
mineralogii i geokhimii. AN SSSR.
(Talc)

SMOLIN FeLtr xzric]p kand, geol,traner, naak, ANDqANOVP, V.M,..
-Par .,4-
red., NAZAROVA,, tek~ai., red,
(Metals of the 20th canturylMetally XX veka, Moskva, Izd-
vo "Znanie," 1963, 45 p~ (Novoe v zhizni; nauke,, tekhnike,
XII Seriiaz Geologlia I geografila, n0-5.) (MIRA 16:4)
(Light me-ta1s) (Metals, RaT8 and minor)
(Rare earth metals)

SMDLIN, P.P.
Plew American manual on petrography. Izv. AN SSSR Ser. geol. 28
no.11-101-103 N163. (MJRA 17:2)

SMOLIN, P.P.
Developmert of 'InIc deposits and the tale industry -in the 9,S,S.R.
Trudy IGEM no.95~,29-48 163. (YdRA 16;12)

SMOLIN, P'll.
4
Formation types of ultrabasites and their mineragenesis. Dokl.
AN SSSR 155 no. 3:586-588 Mr 164. (MIRA 17:5)
1. Institut geolgoii rudnykh mestorozhdeniy, petrografii,
inineralogii i geokhimii AN SSSR. Predstavleno akademikom V.I.
Smirnovym.

s.V. maskaleva ' o tran!3f orm! sL conct!1--t -nE Gf'
ultrabas odds. lzv. r. c-eoi. 29 no.-:
ites ana ga-,-
i00-105 3 ir-". ( KITERA if 7: 1

11-1,~'.
Formation tames of altrabasites and the4r o'g-r.
- 'L
Dokl~ AN SSSR 159 no.2048-350 11' 164. -,7,1"-~,
i
1. Institut geologil r-udnykh mestorozhdenl-y, petrografii, T-.:neralogii
i geokbimii AN SSSR. Prodstavieno alcadefraikom 11,1. Sm.4mov-yr),

SMOLINY P.P.
Felation, of the petrochemical dispersion of Klarks to the periodic
system of elements. Dokl. AN SSSR 163 no.l.-212-215 J1 165. (MIRA 18t7)
1. Institut geologii rudnykh mestorozhdeniy, petrografli, mineralogii
i geokhimii AN SSSR. Submitted November 21, 1964.

otv.
urn-, c and Tnue ta-
fr~Lqii inetamorfl-
o r c MC,3k,,fa,,

F-2a c tc a! rl: c a e o f -,, h -,.e ~ur 0 c a 1 di s s, e r. i n aCn
SsS
of albunda~lce Dol:l. All, -a 16" no.1:20' 21L ja
(",=-A 19:1)
1, Insti-` rLjdrj~,rlx~:, maszoro~;hdeniy, 'ill-'02'~lf'iy
U
:7.-;neralo,,-i i Ji- e o i,-,ui AN S~R. S-dbmii~ted Mayr 20', 1965.

S14OLE.L R . P. , D_7RC=;, A. i. mid LAFIEV, D . I..
___(Krasno~~arsk)
"Studies of the Temperature Yagneetic Hysteresis on the Points of the
Eysteresis Lioorj."
'Nickel and Iron-nickel alloy samples had been autdied for this purpose.
p"r proa*atad at the A11-7~hioa =atimg am Yagmtic Stmoturs of Ferromagmatics
Jmis 1958, In Kramnoymk, Mbeting spimeorad b.V Im", of Phygics, Acad. Sol, UMMO
wA Comm. for Makpotiam, Dept Pbys-Math Soi, AS TZW,

PW= I BOOK EXPLOITATION SOV/5526
Vzesoyuznoye sovenlichanlye po magnitnoy strukture ferromagnet1kcv,
Krasnoyar3k, 1958.
MaSnItnaya strixictura forromagnettkov; materialy V3caoyuznoZo
sov.~ahchaniya, 10 - 16 iyunya 1958 g., Krasnoyarsk 0,',agnetlc
Structure of Ferromagnetic Substances; Mlaterials of the All-Union
Conference on the Miagnetic Structure of Perromagnetic Substances,
Held In Kraonoyarok 10 - 16 June, 1958) Novosibirsk, Izd-vo
Sibiralcogo otd. All SSSR, ig6o. 2119 p. Errata slip Inserted.
1,500 copies printed.
Sponsoring Agency: Akademiya nauk SSSR. Institut fiziki Sibirzkogo
otdoleniya. Komissiya po magnetizmu pri Institute fiziki metallov
Resp. Ed.: L. V. Kirenskiy, Doctor of Physical and Ma4.hematical
Sciences;_Ed.: R. L. Dudnik; Tech. Ed.: A. F. Nazurova.
PURPOSE: This collection of articles is intended for researchers In
ferromagnetism and for metal scientists.
Card 1/11

!,:agnetIc Str-acture (cont.) SOV/5526
COVEP.J%G7_: The collection contains 38 scientific articles presented
at the All-Union Conference on the MaCnetic StructurQ of Ferro-
riaZnctic Substances, held In Krasnoyarsk In June 1958. The r~ia-
terial contains data on the magnetic structure of ferrcizzgnetic
matt~rilals and on the dmamics of the structure In relation to
m