SCIENTIFIC ABSTRACT MASLOV, V.N. - MASLOV, V.P.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R001032810001-5
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: June 14, 2000
• Sequence Number: 1
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT


Z~w
VL/Lsllr.)V) V. il.
Alrao I-r. *'Kf~ I` jIj,.(j b_or,~ :7~f '~' 'Zv- '11.01d.
i, ! , . A. Ii SS,- R r - . ~ "74-P 1 ' ' I ( !I,, ~,., i -, :,7 )

k',-'T1-11OR: c) V
Sub-
'
' c~f Chrom.
~
h
TITLE: -
o
Alet
A
s t C e
"'o )C, (Ussjr-)

RIODIC,~,L:
'n 7 ~,e
BY73 11t
- of janu:~ry
-
3 14
11

T
C r
r

of' Chomic -1
19 56 s-b-
u G t 1-Y
- s h n. CUt
-'Clutions; cutting
f
,
-
-a
-"hi
cz t --i,. c --, S W i ttU: -
.
.
,
e o-
s by feeding 'he
tion proces I U
t-e d,,=A-4on of tne sel-ara
throu:~~h porous or
- -oluti~n into the coluzm
w a s h i n , I I
fiLt-ration level.

an -
: w---

DATYDOV, Vladiri.- lvanovic~).; ".A.,
AS,
Ilf~

LT D23-66 ElIT(!)/E'.'IT(m)/E,iF,~'i)/, (-)/Ei0-P(b) IJP(c) JD/GG
_2:
,ACCESSION NR: APS024566 UR/0070/65/010/005/0758/0760-56i
548.522
iAUTHOR: Masl0V,_V.__N.-L Shaforostov, M. P.
-W, 7 FY~
JITLE: Growth of doped acicular ani filamentary gallium phosphide cr-y-stals from
the gaseous phase 7/
SOURCE: Kristallografiya, ;r. 10, no. 5, 1965, 758-760
iTOPIC TAGS: gallium compound, phosphide, acicular crystal, semiconductor crystal,
crystal growth
ABSTRACT: The simplest equipment for growing doped acicular arxl riffbon-filammt crys-
tals of gallium phoslhide from the gaseous phase consists of a two-zone furnace.(wit6
a t'e4eratux:e *of 1100-- 12000 in the reactiob zone and 400-500C in "Jie i4.os- i
phorus beating naziLa) and a quartz rube 100 mm in diameter in the reaction' xone and
25 mm in diameter in the phosphorus heating zone. A quartz crucible is placed in
the reaction zone with a 20-30 gram charge consisting of a mixture of metallic gal-
lium with gallium oxide in a 3:1 ratio. A quartz boat is charged with 4-6--grams.)bf
.-ed phosphorus. The phosphorus vapor is carried by a stream of pure argon'to re-
act with gallium gubbat&6c vapor formed by the reactidn
Ga%Oj + 4Ga ~ 3Ga:O,
Cad 1/3

3593-469,
ACCESSION NR: AP5024566
Transparent yellow-orange acicular and ribbon-filament crystals 2-6 cm long are.grown
on the sides of the crucible in 2-3 hours. Since reaction products are removed from
the surface of the charge by the argon stream, there is no chance of a tough sur-
face crust of gallium phosphide preventing the evaporation of the gallium suboxide.
Chemical and spectral analysis show that the impurity content in the non-doped
crystals is no greater than the impurity concentration in the initial reagents.
Sulfur, zinc and tellurium were used as dopants. Sulfur changes the shape of the
crystals as well as the electrical and physical parameters. When 70 mg of sulfur
is added to 5 g of phosphorus, 100% formation of ribbon filaments results. Zinc
was introduced by adding zinc oxide to the gallium cnarge in the crucible, since ad-
dition of zinc to the phosphorus resulted in growth impairment and change in crystal
color to grayish-orange. A tNlrd heating zone was added to the firmace for doping
with tellurium. This doping methoe is more convenient than the other two since the
impurity content can be controlled over a wide range. This method was used for ro-
ducing n-ty-e crystals of gallium p"iosphide vith carrier concentrRtions fr M 101 to
1017 cm-3. Howqver, the dopant_cont~!nt in the crystals is not a single-valued function
of the tellurium vapor pressure cormsponding to the temperature in the tellurium
heating zone. An increase in thp temperature in the phosphorus zone reduces the
,charge carrier concentration i- the crystals. The temperature in the reaction zone
,also has a definite effect o- the impurity concontration. High 41opant'concentra-
Card 2/3

L 3593-66
ACCESSION NR: AP5024566
tions cause imperfections in the crystals which make them useless for applications
as finished xT although they make good starting material for producing_ppi-
taxial layers _ allium phosphide with the use of gas transport reactions. Orig.
art. has: 3 figures, 2'forlmulas. (14]
ASSOCIATION: Gosudarstvennyy nauchno-issledovatellskiy i proyektnyy institut red-
kometallicheskoy promyshlennosti (State Design and Planning Scientific Research_
Institute of the Rare Metals I idustny-T 11 -1.
SUBMITTED: 30DecE4 ENCL: 00 SUB CODE: SS
NO REF SOY: 002 OTHER: 001 ATD PRESS
Card -J~/'3

_L191L-~6 EVIT WlYkj-f (m)/~,NP( IJP (C) JD,/GG
ACCESSIM M i AP5018077 tu~/oo2o/63/i63/oDi/oO76/0078
AUTHOR: A.,,
_P~konqvj_ L. 1!';~ MasLov V.
j Sakbarav, -B.
TITLE: EVit&xW izrcrwi of single-!crystal gallium pbos bide
,/ - ~i F,
AN SSSR Ili'
SOURCE: . Do aO, v. 105, no. 1 19~~5Y6-778
TOPIC TAGS., epitaxial growing, gallium compound, semiconducting material
ABSTRACT: The purpose of the investigation wan to check on the applicability of
the sandwich method (E. Sirtl, J. Mys. Chem. Solids v. 24, no. 11, 5~~963) to
fid nv a
the production of large plate-like gallium phosphide single cry_s_t_ajr1~ 'to i e
tigate the main factors influencing the growth rate and the quality of the epitaxi-
al layers. The epitaxial growing was by means of the gas-transport reaction with
water vapor 4Gap + C-1120 c; Me~20 + P4 + 2.H2
using needle-like single crystals obtained from the gas phase by interaction be-
tween phosphorus -vapor and gallium monoxide in an argon stream. The details of the
growth procedure are described. Samples up to 700 p thick WEre grown in 70 hours
at a rate which &taxted at 3o--4o p/hr and sl(r4ed dawn to 7-15 p/hr. The presence
of moisture UrAdered the epitaxial growth by causing oxidation of the substrate
surface. The inarphology of the epitaxim.1 layers depends on the orientation of the
Card 1/2

L 3075-66
ACCESSION NR:
surface and on the perfection of "the substrate crystal structure. The best results
were obtained .)n substrates with (M) orientation. ALhough the Del-ye pattern of
the epi*vaxiaJ.Iy grown single crystals indicates the presence of only one phase in
the sample, the presence of several per cent of gal-Lium arsenide impurity hqs been
noi'iced. Although the content of this impurity can be reduced by 'Lowering the sub-
strate temperature, this leads to a deterioration of -the photolumineseent and elec-
trolnminescent properties of the sample. The gallium phosphide obtained had n-type
conductivIty, with carrier density 108--lo'B cre3, carrier mobility 114 cn?/v-sec
at densisy 2 x 1017 cir-3, and renAstivity 0.2 ohm-cri at room temperature, with a
gallium arsenide content of 6 niol.%. This report was presented by N. P. Sazhin.
Orig. art. has: 2 figures and 1 formula.
ASSOCIATION: Gos-Lidarstvennyy nauchno-issledovatel'skiy i proyektnyy institut red-
kometallicheakay promyshlennosti (State Scientific-Research and Design Inatitute me.
the Rare-Metal Industry)

i . -
-, V
. I . .- . .. "v- * , 1.1" !"", 13 ~~ ", ~ , ; , - - . . - , , - , , . - - . . .
, L ; I
r I I- . .,- I - - I
I -
.11

USSR/Geology
OMateriale for Investigation of Fossil Algae of the
USER. Fossil Chara, Their Importance, Anatomy and
Methods of Their Study," V. P. Masiov, 15 pp
"BYull Moekov Obah lap Pri,
Vol MM, No 3
After short review of importance of Chara. and of
usual methods for their determination, author sug-
Seats his own method based on the longitudinal trans-
pajvnt thin sectionn of the fose.11. Gives &imenBi=a
and brief characteristic sketches for four of the
oogonia fossils of the Kirghiz region- Chara marlani
Unger, Chara meriani -17er. delicate. var. nov., Chara
marlemi -var. acutalia. var.
Doll1us et Fritel Gi~ies
nov., and Char& crassa
distinguishin4g. character-

?'ASW,7, V.P.
Girvanella ali-~e ;ind stratir
,raphic sigm-ificance.
B17:1. MOIP. Ot.". ~Ip.,: . -- nc.,':P14-I0O 149. WIRA 11: ~5 )
Fossil)

17"43
USSP./Geophysics - Algae, Red Nov/Dee 50
New Data on the Reproductive Organs c--,7 AULle Most
Ancient Red Algae (Phodophyceae Rhodophyta),"
V- P. Maslov
"1Z Ak Nauk SSSR, Ser Geol" No 6, pp 119-128
Critically reviews existing representations of
foreign investigators concerning structure and
distinctive peculiarities of reproductive organs
of very early red algae, Improves on these repre-
sentations by using detailed Soviet data.
4WD% 177.T43

USSR/Onology Stratigraphy Jan 50
Algae
~5\ "Importance of Rhodophyceae for the Stratigraphy of
the U,13.1:3R," V. P. ?4aslov, 4 pp
"Dok Ak Naul, SSSR" Val LICX, TJ-- 1
ni-w families from collection of algae from
Western Georgia and Abkhazian ASSR, one of which
showed clear, comparatively rapid evolution and vari
ability during Cretaceous period. T)eBcribeE; one new
f=11y, Palaeophyllum gen. nov. , and discusses im-
portance of this family and other Cretaceous forms
of Rhodophyceae in Western Georgia. Table shows
155T21
USSR/Geology - Stratigraphy (Contd) Jan 50
vertical spread of Cretacnous Rhodophyceae and an-
other leading form for Ukraine and Mediterranean
area. Submitted by Acad D. 2. Belyankin 4 Nov 49.
155T21-

* -- --- - - I - -2

USSR~Geophystcs - East ~-'I'Upria may IJlln 9~:,
"Does an interruption Exist Betw--n MAddle Carif~rian
and Verkholensk Fo-mations in Eas-,ern -":lberia?" V.P.
Mas lov
"Iz Ak Nauk, Ser Geoog" No I, ii, Q' -100
Discusses controversial opinions ~n the connecl.ion
between carbonate Cambrian and red Verkbolerisk tor-
mation in eastern Siberia. EstablisheB existenc-,
of stratigraphic interruption bet-ween these era.,.
22,-T64

1. HASLOV, V.-P.
2. ussR (6oc)
I,. Concretions
7. Carbonaceous nodules of organic origin.
Biul. MOIF. Dtd. geol. 27. No. L. 1952.
9. Monthly List of Russian Accessiens, Library of CongresF, January Cmlassified.

S TXPAIV ~ V . V . y E, . -v , v . P.
Vasa'emrna -F-7,-Lg
, s t,-,na ~*s origi:i and Its d-urability in structureq.
~ I rl. Akadoml ' a nail K SS-:7R. Vo~ r, sy pet rogr&f ii I mineral ogii . Kos kva ,
19~~. Vc!-. 1, T..4bo-47j) (MLRA 7:4)
(Bunaiiig stones)

MASLOV, V.P.
Kethode of coWarjag sections in Garboaacecus strata. (In: Akade-miia
%auk SSSR. VoTrusy T~etrcgrafii 7c-'. 4,
1 mineralogii. Hoskva, '953.
p.477-4Q4) (XLRA 7:4)
~Ku.ybyshev Province-Goology) Oeology-Kuybyehey Province)

M,(-)nt h I v L. ~ ---! , ~ ' '~,-sz, iir. Ac--Ssl~ ns - ~- i t- rary - f Curigr-ss , I -, --, I-II;cI- .

Y,ASWV, Y.F.
Principles rf norle-liclature i-ria ice of strcnj-to:it#-v. lzy.,aN !;-SSR-
Ser.geol. no.4:105-112 JI-Ag '53. (gjaA 0: ~ )
(P&IeO:)Otu-%v

MASLOV, V.P.
Some rarieties of river rilople marks and their origin. Biul.Kom.chet7.per.
no.17:64-75 '53. (MlMA 6:11)
(Rip-ple marks)

.ran s -a "r-
L
e :,-a , IL '7
7!, c,r, a 0 ni zrnem s ilare
L.:)-i.-e r
-C
s
G
r 7 z 'j 0, 7,~o s cow, z -VC.
s

KASLOV,V.P.
Reply to I.I.Belostotakii, Biul.Kom.chetv.per. no.20-106 r55.
(Ripple marks) (MLRA 8:11)

1-I . - -..,
i ~", "

MASLOV.V.P.
Round carbonate enigmas (oolites, "onkolites," coprolites, congula,
and other similar microf ormat ions). Trudy Inst.geol.nank no.155:
156-164 '55. (MLRA 8:10)
(Rocks, Sedimentery)

WUIV V OF*
Intervals in sedimentary deposits in Cambrian and Silurian variegated
series of the southern Siverian Platform. Ixv.AN SSSR. Ser.geol. 21
no.601-" Je 156. (K[RA 9:10)
1. Geologicheekly insitut Akademil nank SSSR, Moskva.
(Siberian Platforn-Goology, Stratigraphic)

- mosommommoomm"
- 1". -,I,,, ,--. wil, :~ ., "1~ I ~z ~-- , - .
- . , I .- -q
- 4- I- , ", iiJ .
~-~ . ~, - ': -:,I, ~ , -~, , ..'..:-
,- - I - z~ - -- , - -

HASIM, VPVFO~~-.
1~
On la now f ossil family of Red Algae and two sev goner& of Blue-
green Algae from the Carbosiferoas. Dokl.AN SSSR 107 no.1:151-154
Mr 156. (MLRA 9:7)
l.Institut geologichaskikh w3uk Akademli sauk SSSR. Predstavleao
-k-d"mikon B.H.Strakhovym.
(Algae, Possil)

Sew Devonian red algae from the Kuznetsk Basin and the
evolution of Corallinaceae. Dokl. AN SSSR 110 no.2:28D-
283 S '56. (HLRA 9:12)
1. Geologicbeekly institut Akademli nauk SSSR. Predstavleno
akademikom N.M. Strakhovym.
(KU2netsk Banin-Algas, Fossil)

AUTHOR WASLOV, V.P., PA - 3177
TITLE A Contr-MuNT-on to the Probiem of Classfication and Phylogenesis
of Charephytes.
(K vopresu o klaesifikataii I filogeali kharofitov - Hussiax)
PERIODICAL Deklady kkademii Nauk 85SR0 1957, Val 113, Nr 3.- pp 676-6Bo,
(U.SoSORO)
Reeeivrm; 6/1957 Reviewed 7/1957
ABSTRACT A mrrvey of the oharophytae still 6XiL*IRg and these which are ex&,
tinat is given. From this we soo what &A important part the fsssl~-
le of this type have played and how few groap8 of them are still
extant. A hypothesis on the connection of the great groups of *he-
rephytae in the past is given. In the Cambrium or in the Ordov-4
there were two ordersi the Sycidiales and the Troohlisoales. Another
group branched off from the sycidiales in the Devon which represents
a transition to the aharales and is possibly related to the Atapa-
sharaoese, This latter group maintained Its existanoe as a fossil
of this transition group te the real Charaphytao which is uLknown
to us~ The development of the Charales began in the Paleozoic age
and reached its climax in the Mesozoic and Kaneoic ages, Another
period of the Chrophytas began with the Perm and reached its oli-
max in the Tcrtiary.A number of kinds became extinct at the end
of the Tetrtiary. (With I illustration)
Card 1/2

PA .-- 3177
A Contributien to the Problem of Classification and P6ylogeneals
of Chrophytes,.
ASSOCIATION
PRESE17TED BY
SUBMITTED
AVAILBLE
Card 2/2
Imstitute for Geology of the Academy of Science of the USSR
STRAKHOV.v N.M_) Member of the Aoademy, 19,10-1956.
21~3-1956,
Library of Congress.

AUTHOR: Maslov, V. P.
TITLE: A New Repi;~4~"Cive Organ of a Devonian PlaLt
(Novyy organ razmnozheniya devonskogo rasteni
_ya
PERIODICAL: Daklady Akademi i Nauk SSS[(, 1,,117 , Vo I
(U.SSR)
ABSTRACT: Since spores of higl.ly organized plants were fourd i!. the
Lower Paleozoicum it haq become p.-o'.)at)le that therQ 0XILit
_9111Y 01'(~Iirlized than
terrestrial plants which are more 0 1
Pailophytes are in the Devonian and eailier. Some aiith(!--,
draw the conclusion that terrestrial, woods existed alrea(-~
in the pre-Cambrian period. Withot- takinE a stard on t,~is
conclusion, the paper under review discusses a sample f:
in Devonian calcareous rocks from the Russian plate
bin, Bobniysk Oblast, Belorussian SSR, depth 74'3-7'~~
The stone consisted ofcarbonate shallow-water rock wit, ad-
mixture of clay and rests of Altrae. In one of the polis~,?Sa
lon,3itudinal section of a formation has been found w",ic,. :%ay
Card 1/3 be considered as a propa4.ation organ of a plant (fig-iire,!

A New Reprodixtive Organ of a Devonian Plant
20-2-511u0
Nr 1 - 3 of the paper under revi The orglanic remainrier
is a clear yellowiah carbonated envelope of ci!-ar snape .
tapering towards the top and blunt at the base. Or~ t,,-,e t,
there is a dense-fringe of bristLes with preserved celiu'.Lil
structure. At both ends of the bag there are 1.ores ahic~, are
linking its interior cavity with the surrounding medium _'he
central part of the inner surface hae. round protuberances,
The length of the entire bag amounts to 3.5 mm. The aut~ior of
the present pqpr suggests for the above structure the nume
Hirsutocarpon extensum Fen. et nov. . :2he exterior
shape of the bag resembl,s thf, megasjnrophyll genus Lepiu~Ll-
carpon from the Carboniferou!j of Engla.-d, but differs in ills
inner structure and also in -.ts having ~:istles. Brist.:e3 and
a similar shape of the 'external envelope are known tc.
in Idiadesmia membranecea C. Bertrand, again from the
ferous of England, Lhe difference lies in the inner stn~cture
of, and in 'the pre.,~ence of several envelopes in the Erq-_Ias~,
form. Both of the above species belong to the class of L~g)po-
diales, group of Lepidospeririae. As the author of the papc-
tinder review is not in a position to identify tnis jer~tra
tive organ with the vegetative parts of any fossil plant.
Card 2/3 opecies described before, he places it presumptive-.,; Wlt~. !~!e
I

A New Reproducti.ve Organ of a Lr--V0nl8D PIBrt
L,ycopodiaceae. It remains u.,.~- :eur
berances in the interii.r ar~-- seit.~rate
wbich, after liavinf, m~tti.re,i, :e!,ej t,
If this assumpt-or, iLi -orre-t, wo
as a sporantiophor i:.ki
described above 1.9
considered as a ore ;-h!
Psilophyts *here are
ASSOCIATICN: Geological Institute AS USSFi eo I o;, 1
Akademii nauk S3SR%
PRESENTED: February 1 1 IL3~ it ;,.:h,~v
S U B11, 'I T T E DFebruary 6,
AVAILABLE% Library of Con--r-~~3
Card 3/3

! ~' T ) ' ,' ' .
_ P., 0. IC-,Dj",~Caj Lil- ~ , _r,j~;~jj ), ~ al -)z el. uLi)
~ aL- l 1_ . C _ i C
11~~al .reo~-5 i ~ss-i Al. -,,e ~,-- :.f-
': c A,- a e: , -i~ I c ~t -.- ~s - -- -, - - .
..)r tltis woi-i -- -ece."'ve" aa.--i ,,,
Prir-oria, ',,D. 2, 1,~~ . -P. 13-1-ILL -

AUTHORS: Vaslov V "trobin, V.N, S,w /11 -, 6-1.
7ITLE: fhe ':'Xppnsion of --ed Algae of the -erti--,,, ~---:~J r 7.-
Te rri tory of the -Tkra i n in n S-'R, a nd The ir Corre 1. a t
-ea Transg-pssions (Rasprostraneniye tretichnykh
vodorDsley 7krainskov SSR i svyn~, uh s transgress 1yam-1
morya)
PERTr,'D'CAI: Tzvestiya 4kademii nauk S7SR, ---,eriya peologicheskayR. -.CC.F,
,Nr 12, pp 7~-91~
I . - n j
ABSTFACT: The article gives an exhaustive geological survey of differen-
parts of the "krairian SSR where the Tertiary calcareo,.;s -red
algae (Rhodophyceae' has been found. This s,.rvey showed
at the Tortonian (TTpper Miocene~ stage a shallow sea covered
the plpteau parts of the Ukraine, and the expansion of -,n-2
red algae corresponded to definite stages of the development
of these sea basins. The following -.oviet geologists Pre
menticned by the author: V.G. Morozovq, A.7. Yoyseyev, V N.
Utrobin, L.V. Linetskaya, 1-.P,, Bashkirov, '.3. Vyqlo-i,
1"hizhchenko, V.P. Yozakova, M.Ya. Serova, L.N. Kudrina, V.;.
I
I,ivental', A.A. Rogdanova, V.V. Clushko, I..". Tishvqnrvfi,
Card 112 G.I. Molyavko, D.P. Naydin And V,P. Maslov.

-Zclv/ I i - ~ a - -1 2 - ,I" lc~
. a on t~--
The Expansion of Red 11gae o~ t!,-- 'ertJa::-y Per 40'
Ukrainian SSR, and Their -orrel9tion wit~i F~ea Transgressions
-here are 7 maps, .- profil.~s, 1 scheme, 1 table an!
ferences, 1n of' wKAch arp ;ovipt, 9 Polish and
ASSOCTATI,'~N- ;eologicheskiy inst-I Ltut AN 7,5SR, Mo.~'k~.% (The Goo", -~i- 1-5-
the A~, Woscrln)
T.,vovsk9ya P_ speditsiya 7krnef tegazraevedki " "~,e - v v
pedition o~ the 'Ikrneftegazrazvedka.
SUBMITTED: August 21,
Card 2112

AUTHOR: Maslov, V. P.
-1
SOV/20-121-2-451/5~
TITLE: New Finds of Algae in the Jurassic Formation of the Crlz~-a
(Novyye nakhodki vodorosley v yure Kryma)
PERIODICAL: Doklady Akademii nauk 535R, 1958, Vol. 121, Nr 2, ~,p- 35-3-7
(USSR)
A3STRACT. Since the collection of the soleropores and lino:)orelles in
the Jurassic limestone of the Kr3m-Yayla (Kryz,,ska~7a Yayla)
there have beer) no data on new types of alg-ae in this area.
only recently V. F. Pchelintsev and N. P. Kyansep mentioned a
farther spreading of the solenopores. The author fo-ind iiitL-r-
esting Siphonea of the Upper Jurassic in the westtrn 'fayla
They belong to the type C H L 0 R 0 P H Y T A , class ISO.'CN-
TAE, order SIPHONALES, family Dasycladadeaes genus Actinooorel-
krymensis sp.nov. Fie-ure 1 a - d, ant
la A'th., 1882. Act. (?
2 g. A de5criptiT-riof this new type is :,iven. Listributicn:
Karabi-Yayla- Genus Triplo.~horella Steinmann, 1880, Tril~!- kara-
biensis sp-nov. Figure 1 ye and 2 ye, zh. Munieria Deecl~e, 15133.
Mun. baconica Deecke, 1883. Distributiont limestone in the
Yayl=u~-th-ermore Actinop_orella sp. and Solenophora so which
Card 1/2 could not be determined to the genus, as well as rests of sev-

SOV/20-121-2-,,1_/5A
New Finds of Al.-ae in the Jurassic Formation of the Crimea
eral types of Coscinoconus Leupold were found. The fac~_.il
binding of Actinoporella krymensis and L'unieria baconica
seems to indicate polyaiorphoas I estones from deeper water
(not deeper than 50 m). Triplophorella karabiensis anc
Solcnophora sp. were found in coarse detritus lim.-st-_,ne,
i.e. in a facies of the shallow water near to the r_-ef or
shore. 'There are 2 fi-uies and 3 references, 0 of viich ara
Soviet.
ASSOCI-ITIC11: GeoloEicheskiy inctitut Ak-a-demi-i naak SSSR (Geo)o.-ical In-
stitute )AS JSSR)
PIUSLINTED: March 4, 1958, by 11. S. Shatskiy, Member, Academ,,, of
Sci~~nces, USSR
SUBMITTED: February 28, 1958
Card 2/2

AUTHOR: Maslov, V P SOV/2o- 121-3-41/17
TITLE A Fo,-ind of the Gen-L;a Coscinoconus Leuj)o.~' in the Jurassic of
the Crimea and t~.e Heal Nature of This Gemis (lTa'k:ho&a v Yure
Kryma ro0a CosciDoconud Leupold i yego istinnaya priroda)
,I
PERIODICAL; Doklady Akademii naiiv SSSR, 1956, Vol 121 , "r ')I
pr, 5,15 - 546 (USSM)
ABSTRACT: In 1935 Lou,-mold found tl-.e remnp-nts of t'.e or7anisms -entioned in
the title in Switzerl-t--d and called them foraminifera (Ref 3).
There tas no ~Iofinitr- decision on the po~-,ition of this ort,anism
ir, the system (Refs 1,2,5-7,) The author investi,-:.ted Coscino-
conus remnants found by L. G.Reznikov-- in the Kineridgian staj-,e
of the Crinea-Yayla (Krymskzya Yayla). Tl;e author succeeded in
fin'in- Leu-old's j1)1nion wrone as well as his m,~thorls of
descril,tion The author ~7ives q. new description of th;~ je.,,us
which he classifies amonl- tle type Chloroph,~,ta, class Isocontaez
order *Sii)honales, family Dasycladaceae, Tribus Acetabularieae(?).,
In 1935 the author described the type Coscinoconus alpinus Leu-
poll (Fio 1b) as ori,,ans of reproduction of the vihorl-lihc,
siphona-lil,e rtlgaae The ve ' tative pn 'rts renain unkrr,,,vn 6 new
Card 1/2 Coscinoconus types were furth-r described: C-fuciformis si;.nov.

A Found of the Genus Coscinoconus Leupold ir. the SOV/2r- 121 - '-4 1j
Jurasci(. of the Crireh and the Real "'.ri tL!re of Thiz
(FiCs la,2a,3b) from Krirabi-Yayla njid Aypetrii-Yayla (Aypetrins-
kaya3myla); C co,iicus sp nov, (Figs 2b,3d), Karabi-Yayla;
Che.-emoch- and Rybnitsa river, n-)rthern slope of the Carpathi,..ns
(severnyy shlon K.-.rat), materia- by L,V,Liric-t!-,I,aya;C,,-iinutiis
sp,noir. (Fig 3a) from Ay-Petri; C~obloi2~~ sp,nov.(Figs 2v,3v)
from Ay~,Petri; C.pagodaeformis Rigs 2 3u)from Karabi-Yayla;
C,,assymetricus sp nov from Karabi-Yayla,. At the end of the paper
the position in the system and the distribution of the mentioned
types are discussed Th--re are 3 fi.,ures and 7 references, 1 of
which :.s Soviet,
ASSOCIATION: Geologicheskiy institut Akademii nauk SSSR (Institute of Geo-
lojj7AS USSR)
PRESMi'TED: March 4, 1958, by 11 S.Shatskiy, Member, Academy of 5ciences,
USSR
SUBMIf."TED: February 28 195P
Cari 2, P

MSLOV' V.P.
Lime algae as indicators of factors governing the formation of
sediments. Sov.geol. 2 no.12:126-128 D 159. (MITIA 13:5)
(Algae, Fossil) (Geology, Stratigraphic)

3(5)
AUTHOR: laslov, V ~ P.
TITLE: Stromatoliths and Facies 'Stromatolity i fatbii)
PERIODICAL: Doklady Akademii nauk SSSR, 1959, Vol 12~, Nr 5, I)P 1085-10,~~B
(USSR)
ABSTRACT: Stromatoliths are the only widely distributed organic form.,-3
of the Precambrian. Not until the last decade have several
directional methods of description, nomenclature and classi-
fication stood out: 1) the paleontologic direction (Refs 1-3).
Definite stromatolith genera, which are assigned to the
Cyanoph,yceae, are described here. 2) "botanical" direction
(Refs 4,5), in which the microstructures of the stromatoliths
are considered as comparable with those of the recent Phaeo-
phyceae'and Cyanophyceae families, however, the exterior form
remaii3ed unnoticed. 3) lithologicpaleontologic direction
(Ref 6);!'\the micro- and macrostructures are considered to be
forms of bomplex origin. They are classified according to a
special morphologic system, which deviates from thb biologic
system. The traces of -lgae and animals are discussed
separately. 4) lithologic direction (Ref 7 and other.4). No
Card 1/4 special names are given to the stromatoliths or their
*- .0

Siromatoliths and Facies
SOV/20-12;-,-T'6/tA
structures. Their systematic is formed on the basis of the
exterior form and the character of the! stratification. Further
treutment occurs in the present work accordine to standpoint
3. This multiplicity of conceptions goes back to the complex
genesis of the stromatoliths. Various complexes of primitive
algae took part in their formation, depending on t'.,ie salt
content of the water, the quantity of terrigenous material
deposited, depth of the water, strength of water movement
(currents and surfN and further, origins unexplained for the
time being (eg. PH . Further, the presumed living conditions
of the stromatoliths and the formation of onkoliths and
ooliths are portrayed. The stromatoliths are more closely
connected with the sedimentation than with the petrographic
composition of the sediment. The familiar standpoint that
the stromatoliths are involved in the life activity of primi-
tive algae does not always explain the formation of some
structures which occur in them. The experiments of V. 0.
Kalinerko (Ref 9) have shown that the bacterial factor of the
carbonate deficiency may not be neglected. I-e bacterial colo-
nies are able to change the acidity of the iter locally. Thus,
Card 2/4 under favorable circumstances,

Stromatoliths and Pacies
SOV/20-125-c-36,'~i
microscopic spheres and grains are deposited with-in the
colony. All of these methods of deposition, including car-
bonate sedimentation by algae, are closely related to the
envirenm,--ntal conditions. The optimum conditions for the
growth of the stromatoliths suggest the boundary between sea
water und fresh water or the transformation of sea water into
a brackish water lagoon along with the dtherwise necessary conditions
mentioned. All of the factors acting on the stromatoliths are
closely connected with facies. The algae and bacteria could
be replaced by others in the course o~' geological time. The
sedimentation conditions were also changed. Perhaps the stro-
matoliths will be helpful in understanding these transforma-
tions. Thus tne conclusion is' drawn that the study of the stro-
matoliths as the result of sedimentation and an a guiding
stratigraphic index is very complicated. There are 11 refer-
ences, 6 of which are Soviet.
Card 3/4

.S*tromatoliths and Facies SOV/20-125-5-56/61
ASSOCIATION: GeologicheBkiy institut Akademii nauk SSSR (Geological
Institute of the Academy of Sciences,USSR)
PRESEKED: December 31, 1958, by N. S. Shatskiy, Academician
SUBMITTED: December 25, 1958
card 4/4

MkSIA)Vq Vladimir Petrovich; SHATSKIYq N.S.., akademiko glavnyy red,;
TAIMIAWMVP V.A. 9 otv.red,; ZELBNOVI, K.K.9 otv.red.;
IIIIAP N.S.P red.izd-va; YM ININP I.F.P tekhn.red,
[Stromatolites; taoir genesist riethod of studyt relation with
faciesp and geological significancep based on studies of
Ordovician deposits of the Siberian Platform] Stromatolity; M
genaziep.metod izueBeniia, W.Laz' s,fatsl-ami I geolog .Loheakol'
znachenie na primere ordovika Sibirskoi platformy, Mosk-vat Izd-
v,,% Alrad. vauk SSSRt 1960. 166 p. (Akademiia nauk SSSR,
~.Logicheskii fiwtitute Trudyt no. 41) (MIRA 1412)
(Siberian Ratform--Stromatolites)

HASIOV. V. F.
Acicularia and their significance for the stratigraphy of the
U.S.S.R. Paleont.shar. n0-3:115-122 160. (XLU 13.' 10)
1. Geologicbeekiy Institut Akadeall nauk SSSR-
(Algae, Fossil)

VYAWVv O.S. (MR).i MASIDV. V.P., (SSSR); WDDWIkMp St. (M.Bks);
OLTdICZs Z.R". (FO-lGE0-;-WVAK,, V. (Pollsha); SIAVIN, V.I. "UR)
MSUUMAJO N.1 (SSSR) VYALOVp O.S. (SSSR); EEERZIN, A.G. (SSSR)
BDNDUMHUKl V.;. (SW
Participation In diseussione. Mat,Kerps-BMeaesots. no,3.1157-
179 160, (MIU 14:12)
(Carpathian Mountain*-4jology)

PASWV, V. P.
Microscope object holder (system MD-I). izv. AN SSSR. Ser.
geol. 25 no.9:113-115 3 160. (MIRA 13:9)
1. Geologicheskiy Institut AR SSSR, Moskva.
(Microscopy)

)miauAj.
Coprolites dnd traces of boring orgamd-sms and
for 3ithologists. Izv. AN SSS7a. Ser. geol. 25
their significance
no.lOs8l,86 0 160.
(MIRA 13:10)
1. Geologicheskiy inetitut AN SBSR, Moskva.
(Coprolite)

3 (5)
AUTHORS: Zhulc-Pochekutov, K. A., Maslov V P. SOV/20-130-1-40/60

TITLE: Problems Re ardin --4;om the Botogollskiy Mountain
g Graphite
(East Sayan~
PERIODICAL: Doklady Akademii nauk SSSR, 1960, Vol 130, Nr 1, PP 140-142 (USSR)
ABSTRACT: Considerable deposits of hiah-quality graphite are knovm. to
occur iiL the alkalint Botogol'skly massif . 'raphite occurs
a'-most in all rocks, but the bulk of large graphite bodies is
concentrated in the northern part of the massif and is bound to
leucocrate-ne-heline-syenites and to alkaline and nepheline-
pyroxene-ayonites. Large individual granite bodies are bedded
in limestones or in their contact areas. Graphite either is
dispersed in rocks or forms little pockets and roundish or lens-
shaped bodiee of different size respectively. Larger deposits
(bodies to 50 times 35 m in diameter) are ellipsoidal or
roundish. Of this deposit, A. N Labuntsov (Ref 1) classified the
following graphite varieties: 1i massive, a olid- crystalline,
2) arborescent, 3 drop-shaped ("somatoid") and concent:Lical-
~
spheroidal, and 4
imbricating graphite. The first variety is
the most frequent one. The genesis of Botogolskiy graphite has
Card 1/4 not been completely explained. The age of the Botogol'skaya

Problems Regarding Graphite From the Botogolfskiy SOV/20-130-1-40/69
Mountain (East SVan)
intrusion is determined to be Lower or Middle Devonian. MVt
researchers agTee that limestones are the source of carbon.
Opinions, however. differ as to the formation cond-itions and
the sedimentation age of graphite. According to B. M. Kupletskiy
(Ref 2), besides organic remains of limestones, carbonic acid
which was released during the CaGO 3 dissociation, also took
part i-xi the graphite development. Hydrocarbons were able to
g
liberate carbon with CO 2 separated frc-m the limestones during V
the interaction of gas-saturated magma. N. A. Florensov and
V. S. 3obolev agree as to the source of carbon. However, they
hold the opinion that graphite was developed by the CO
decomTjosition (reaction of Boudoir) in the obligatory presence
of bitunen. Graphite sedimentation set in alr6ddy juring the
mag-matic stage,, Its bulk, however, was deposited 'oy post-
magmatic hydrothermal solutions. According to V. P. Solonenko
the transformation process of limestones into ayenite
favorea the carbon concentration. The hydrothermally deposited
Card 2/4 graphite is said to be of organic origin. Fiaally the authors

Problems Re6arding Graphite Prom the Botogollskiy SOV20-130-1-40/69
Mountain (East Sayan)
describe a new tubelike variety of graphi,~e from the
Potogcllskiy massif (Fig 1). It forms gr,)ups of parallel
tubes with an intermediate space of 1-2 mm, a length of 20 mm
wid walls 0.1-0.3 mm tbick. The middle part of the tubes is
filled 'hy zonated minerals In the 95quence: calcite, pyromene,
microcline, nepheline (from outside . Thick tubes dichotomize
in a sharp angle. The authors arrived at the conclusion that in
this case graphite was separated earlier than minerals of the
syenite part. The latter are of metasomatic origin. Graphite
tubes originally )x-y have been composed of organic carbon
compounds. In theix embedding they remained hard and became
graphite without considerable mechanical deformations. If this
assumption is true, this problem is to have a name: Botogolia
saianensis gen. et sp.n. These "Organisms" (as a working
hypothesis) probably belong to algae of the species
Phaeophyceae. Finally the authors are of the opinion that it
is much simpler to explain the formation of graphite by this
theory than by the assumption of a complicated carbon
concentration by metasomatic processes. The authors also
Card 3/4 mention S, V. Obruchev. There are I figure and'4 Soviet

Probloms Regarding Graphite From the Botogollskiy SOV/20-13V-1 -40/69
Mountain (East Sayan) -
referoncen.
A5.';OCIATION: Geolooicheskiy inutitut Alr-ademii nauk SSSR ( nstitute of
Geology of the Academy pL Sairince , USSR)
PIU~SJ-iTZD: July 5, 1956, by IJ. S. Sh,,k,rkiy, Academician
SUBIUTTED: July 71, 1956
Card 4/4

KASLOV, V.P.
Now Cretaceous algae from Kopet Dag (Turkmenistan). Dokl.AB
SSSH 134 no.4:939-941 0 160. (MIRA 13:9)
1. Geolbgieheekiy inetitat Akaaemii nauk SSa. P-edetavleno
akad. N.S.ShateLim.
(Kopet Dag--Algae, Fossil)

MASLOV V.P.
Biohenps and algae as indicators of facies. Geol.sbor. [-Ivovj
no.7/8:4.41-449 161. (MIRA 14:12)
1. Geologicheskiy institut AN SSSR, Moskva.
(Reefs)
(Petroleim geology) (Algae, Fossil)

MASLOVY V.P.
Algae and carbonate sedimentation. Iz-7.AN SSSR Ser.ge-ol.
26 no.12z81-80' D 161. (,\aRA 14-:12 )
1. GeologJc-heskiy institut AN SSSR., Mosk-va.
('11gar.)

YAS
tc) ; BOLKHMTIU., N.A.,q otv,red.,- VEWTAK., G.V.
ed.lmd-va,* GUSIKOVA, O.M... tekhn.red.
[Fossil red alga in the U.S.S.R. and their amociation with
faclesi IskoparMs bpgriazqe vodoroo:Li SSSR i ikh oviamle fataiiami.
Hbskva.." lzd-vo Aksdonauk SSSR 1962,, 2U p, 36 plateo.
(Akademiia nwAl MR. Geologicheskii inotitut. Trudy, no.53).
(Ahodopbyceae,, Foovil) (MIRA 15:7)

Concerning E. V. Romaneva's article ONeepne Chara species frolm
eastern Kazakhstan.' Faleonto zhur. no.1:174 (162.
MIRA 15:10)
,. Ggologicheskiy institut AN WSR.
46
(Emakbotan-Algas, Fossil) (Romanoval E. V-)

KRIVIR, A.L. [deceased); WLOVO V.P.
fiew data on algae and the stratigraphy of the Upper Cretacems
and Lower Faloocene of the Marmarosh Masmif. Izv. AN SSSR.
Ser.pola. 27 no,, 12:63,71 D 162. (MIRA 16:2)
1. Geologicheskiy inatitut AN SSSR, Institut geologii
poleznykh iskopayenykh AN Ukr=.
(Tranuccrpatia"-4Geologya Stratigraphic)
(Transcarpathia--Algaej, Fossil)

ViASJ9V,- V.P.
Paleogene stromatolitee of the Givsar Range. Dold . ~J~' 6!ZR 14~
no.3:690-691 Ja '62. (HIRA 1.5-1)
1. Geologicheskiy institut 0 SSSR. Predstavleno akademikom N.M.
Strakbovym.
(Gissar Range-Stromatolites)

FAXIBEEM, B.G.; WISLOV, V.P.; KCRNILOV, G.I.
I
Bemote, control of surface substations at the S.1-L Kirov Mine.
Sbor. nauch. truc4 KG.RI no.19:30-35 162o (MM 16:5)
(Krivoy Rag B Asin-Electric substs~tions) (Remote control)
.fto

FAIMMM, E.G.; KCRNILOV, G.I.;
Apparatus for remote control of block-type fans in the S, M, Kirov
Mine. Sbor. nauah. t7ad. KGRI no.19,'35-38 162. (MM 16:5)
(Krivoy R3g Basin-Fans, FIlectric) (Remote control)

HISLOV, V.P.
Remote control af the operation of automatic shuttle belt conveyors.
Sbor. nauch. trud. KMI no.193105--108 162. (MIRA 16:5)
(Conveying machinery) (Remote control)

!~ASIDV, Vladimir Yetrovich; GOLLERBAKH, M.M., otv. red.; VAKHRAMEYEV,
V. A.F otv. red.; PEYVE, A.V., glavnyy red.; MARKOV, M.S., red.?
MENIIERJO VV... red., TD40FEYEV, P.P., red.; VANYUKOVA, O.M. , r!td.
izd-va; CUSIKOVA, O.M., tekhn. red.
[Introduction to the study of fossil charophytes.] Vvednie v
izuehenie iskopaemykb kharovykh vodoroplei. Moskva, Izd-vo Akad.
nauk SSSR., 1963. 103 P. (Akademiia nauk SFSR. Geologicheskii
institut. Trudy, no. 82). (MLRA 16: 11)
1. Chlen-korrespondent AV SSSR (for Peyve).

WLO
Articulate red algae of the genue Janis 4rom Ffiddle Sarmatian bioherms in
Moldavia. Paleont.2hur. no.1:311,-322 163. (,%,(IRA 16-4)
Is Goologicheakiy inBtitut AN SSSR,
(FIoldavia-Algae., Foosi.1)

MULOVI V&PO
Find of a line corolla and the structure of the apical part of
the fruit-bearing organs in fossil Charophyta, Dokl. AN SSSR 149
no.4t97A-956 Ap 163. (NIRA 16:3)
1. Geologicheskiy inetitut AN SSSR. Predstavleno akademikom
N.M.Strakhovym.
(Algae, Fosell)

MkS,TGv, V.P.
Germination of the oospore in fossil charopWEes, and a new
form-genus. Dokl.. AN SSSR- 152. no.2:443,"5-S '63L (MMA 16:11)
1. Geologicheskiy institut AN SSSR. Predstavleno akademikom
N,M. Sti-akhovym.

MASLOV, V.P.; RENGARTRI, N.V.
Find of fossil calcareous
no.3:579-581 N 164
algae in loess. lbkl~ AN SSSR 159
(MIRA 18-.1)
1. Goologicheskiy Institut AN SSSR. Predstavleno akademikom
N.M. Strakhovym.

MA-SLO':, V, P,
Kcpetdagarla, a new tribe of vf;rti~-I'Ilate -'-',,honeae (green algae).
Dokl. III SSSR 164 no-5:1154-1157 0 165.
(MIRA 18: 10)
~. Geologicheskiy institut AN "'SSTI. bubmittee December 8, 1964-

plas 16 L), c I)
UM/Theoretical Physics B-4
Abs Jour Referat, Zhur Fizika, No 5, 1957, No loB63
Author maslov) VOPO
Inst
Title Correction to the Quasi-Classical Energy Approximation.
Orig Pub Tr. 3-90 Vses. mtem. s"ezda. 2. M., AN S&M, 1956, 164
Abstract No abstract.
Card 1/1

NASLOV, V. P. Caad Phys-Math Soi -- (diss) "Certain problems of the theory of
disturbances." Mos, 1957. 4pp 22 am. (MOB State Tjniv in M. V. Lomonosov). 110 copies.
MO 15-57, 104)
-6-

so* 0.0
dos I
IS A K 2-
ST. OR
wellem 4w lots npu" 48 w" wpudm. K. K.
Amdrwv and V-P-Madow..., Cipseps. read, amd. sa. .00
V. P. S. $Z= 111=0'n hwish)-7*0 MAN of ooo
'g2pis. w" to 011m. WA kow" pre"Um
-laid tbt otbar M hisb pmantm) to amcmaln tie make .00
ct-fas I* , on "M npkdvn md to p_g the ej pb @A& p%cr4 is a aile am) &m4 Ue '00
br& wt faO In (C. A. 3% 40M. In the am Orm (1), tetro- (91) 1
a aim twbe. 25 um, in dium. and 1.5 0. ions, =141 jW) mm tgWed. Now of tb- ex- '00
eta Was AW wkb 0 H-0 Ida. alltr evacustim, and a sums eithff explo&d or, wbevitbesumenjaw.
w wbm U and III wcTv logo
ww. d c2pkohv (dw a adiditied = 0 law=! =njtw pmwure d 3 *13M., c
Tum pbred on a pk" at Fe in trr Of I Ism The Fb StUlt 20 IA "VftlWiWt" CXVIO-
sea The U-0 mixt. was detomi"i t1ty firinj pt 13 rnjr. ellwv wo for Ps pressam of 7w. 400
210 ratu. In tbe 2rAd I 1 1. as dectrolytic g" muxt .
so, was inuvdamd into on evaccullmll Bud tube (38 mm. bmr golll
and I n. 1=g) &W epWW by pb sji& as beleft-
mnw DK3t whb 1, 111 am bl"d2s platin
D; at ago*
""MM M &a SOL bM or CXP"
5 and 10 alms. it bunwd wilboat cimmins the tube: 090
'blk at aim hish" p"fint" It elpw" and, be tubt WS.
Allf = to *Mi. IUl (C") waq I-A to laum of r% - '06
lft& at 6 (w 11) alms.; at 15 alms, = '10 Zi .00
pww at 20 ftmi.; twhise III (powd.) em
1.5atins. Jw"foundtotv-&tZ)&W24&txu.&Wex- "04,
that lbtfriwis
Wit
umaimd ag"n the &-ductiom snn& from lbvir cakav. '00
Flank Goll" e 0
and theary.
SOON SIT'sal" *Dow 60"Aftv Wei
few MAP Vv a&( ug"C"I mi4arl an am All
a w " #A I I a
1 311 9 do 0 2 6 v
By to Alle, so I Ift 0 0 ; 0
0744 0 : : :1 0
000000 dos* 00 IF1 00.00 WO 0 * 0 0-0 0 0 0

-film
ARM
_91) v

SUBJECT USSR/MaRMTICS/Functional analysis CARD 1/2 pl~ 17';
AUTHOR MASL9X V,p
TITLE Ti-r-fai-baion theory at the transition from a discret f?pL,4
to a continuous one.
PERIODICAL Doklady Akad. Nauk 4 267-270 (1956)
109,
reviewed 11/1956
The author generalizes his earliar results (Doklady Akad. NaukQ.A_
on the approximations for the one-dimensional Schr6dinger equation to the more-
dimensional case. He establishes that for the eigenfunctions of a more-
dimenaional Hamilton operator in a certain sense converge to the comb,'nationa
of more-dimensional 6 -functionig. This result holds for an arbitrary quantum
mechanical operator which corresponds to a physical magnitude which can be
measured. If in the three-dimensional ease there exists a function R such
that with respect to the norm n
All +-!U(X,Y,Z) R
2m n 1h n 71 0
for h ---> 0 and ~A n(h) them Rn ia the asymptotic of the eigenfunctic-i of
the Hamilton operator. The fwrattan rn(71) gives the awymptotic of the elgen-
values forh ----> 0 in the three-dimensional case of the Schrddinger equation
if the potential function possesses a minimum. Here the distance of neighbored

Doklady Akad. Nauk 109, 267-270 ('956) CARD -212 PG - 3174
. pointa of the apectrum has the order IS for /on(t) ---o -A .
n 00
t --* 0
INSTITUTIONt Lomonossow University, Mosoow.

P1 P.
-4 51P.M4
Theory of perturbations of linear operator equations and the
problem of the small parameter in differential equations.
DokI. AN SSSR III no-3:531-534 N 156. (WRMA 10:2)
1. ~bskovskiy gosudarstyenrjy7 univercitet imeni N.V. Lomonosova.
Predstavlono akademikon N.N. Bogolyuboy".
(Differential equations) (PnWonal analysis)

SUBJECT USSR / PHYSICS CARD 1 / 2 PA - 1997
AUTHOR KASLOV,V.P.
TITLE A~e ~as
~ed on the Perturbation Theory for the Determination
of the Spectrum of Ordinary Differential Operators with Small
Parameters for the Oldest Derivative.
PER10DICAL Dokl.Akad Nauk 111, fase-5, 977-980 (1956)
Issued: ; / 1~5_7
Lot fAkJ be assumed to be a aeries of self-adjoined operators with discrete
spectrum which converges considerably in the direction of the self-adjoined
operator with a continuous speotrum. If ? (11) and E(1) denote the asymptotic
k k
behavior of the eigenfunctions and eigenvalues of the operators Ak in the case
of large k, the first correction of the asymptotic behavior of eigenvalues ca~i
be expressed in the following manner, which is similar to that adopted in the
case of the ordinary perturbation theory:
(cr(l) (1))/(T(1) V(1))) - E(l). This naturally holds only if T(l) belongs
k 9 Ak % k ' k k k
to the definition domain of Ak and if T(l) (i.9. the eigenvalue in first
k
is not degenerated. For the purpose of determining the following
approximation)
approximations it is necessary in each concrete case to make use of one or the
other modification of the perturbation theory. The method discussed below is
suited for the purpose of solving boundary value problems in the case of ordinary

bokl.Akad.Nauk 111, fasc.5, 977-980 (1956) CARD 2 / 2 PA - 1997
linear differential equations with small parameter in the case of the "Oldestf,(?)
derivative. The author explains this method on the basis of the SCHROEDIRGER
equation: - (F,2 /2eA)(d2/dx2) T. +fu(x) - En ~ Yn - 0 with the condition
rQD 2(x) dx < oo . Here ~ 2/2 is considered to be a small parameter, and
L OD 2 2/dx2)
the HAMILTONIAN operator R 12e,)(d + u(x) at h---> 0 on this occasion
converges considerably towards the multiplication operator u(x). H.A.KRAMERS,
Zs.f.Phys., a, 828 (1926) found the first so-called quasiclassical approxima-
tion for the aforementioned SCHROEDINGER equation, and the following approxima-
tions are discussed in the course of this article. In this connection u(x) - E
in assumed to have two simple roots. The first approximation of the eigen-
values of the SCHROEDINGER equation investigated here is found with the aid of
a BOHR eqrAtion. For the determination of the following approximations a re-
currence formula is set up which connects the (i+l)-th formula with the i-th
approximation. On the basis of the asymptotic behavior of the BESSEL functions
it is possible to write down the second approximation for the eigenfunctions
of the problem under investigation. In conclusion, the determination of the
asymptotic behavior of the eigenfunotions is described.
INSTITUTION., Moscow State University.

KASLOV, V.P.
-"~- --- --- *~
- -- - ti'i'if-ehange of quantun mechaEics to classical. Vast. Hosk. un.
Bar. mat., makh.. antron. fiz., khim. 12 no. 6:107-116 '57.
(MIRA 11:10)
1. Kafedra matematiki dlia fizicheekogo fakullteta Moskovskogo
gosudarstvennogo universiteta.
(QUaLtum theory)
(Mechgnlcs)

20-5-11/60
AUTHOR MASLOVIV.P.
TITIX Degeneration ca Passing from a Discrete Spectrum to a
Cj
ptinuous and Transition from Quantum Mechanics to Classical
Lechanics.
(Vyyozhdoniye pri perekhode ot dAskretnogo spektra k ne-
pr kvnomn i,perekhod iz kvant,-.,c4, makhanlki v klassiches-
kuyu%- Russian)
FERIONGAL Moklady Akademii Nauk SSSR 19571 Vol 114, fir 5t PP 957-960
(USSR)
ABSTRACT te k S here denotes the aystem (k - 1,2,... of the orthcj-
i
normed bases in a certain HILBERT'S space H; a certain
sequence of whole numbers depending on k. Further
lim nk - co ic true. Furthermore, the index m jnj is
k -.*. o o
eliminated here. First, the conceptions "element pf the
space K 0 [ek] " and "element of the space 9 [ey- I are
defined. Also the elements equivalent to zero are defined.
In H C ek I a scalar )?roduct is defined. The apace
n i
N k is a separable HILBERT space. If at cD the
CARD 1/2 . [oil

20-5-11/60
Degenration on PRssing from a Disarete Spectrum to a
C~ntlnuous and Transition from Quantum Mechanics to Classical
Mechanics.
difference (n-no) -> co then the spaces U
[e ki and
i
n
M I te~3 are orthogonal in the sense of the scalar pruduot
n t
k L
i ' 'Y
r- e
614
lim (xk xk 6- M
, F- e
n
1
k
n
I
k 4 oD
Now [AkA Is assumed to denote a sequence of selfadjoined
positive definite operators with a discrete spectrum with
the ei,~Tenfunotions Lxkj and with the eigenvalues
i
These operators strongly converge towards the selfadjoining
operator A with a continuous spectrum. ?\is assumed to
denote a point of the spectrum if the operator A; the space
M
[ -x
j The following theorem
Akj is denoted by M
I,
n
,
applies: The conclusion of the operator ~ A,~ in Mit ~A~
is the operator of the multiplications with the number A,
(No Illustrations)
ASSOCIATION: Moscow State University 11M.V. LOMONOSOV11
PRESENIED BY: N.No BOGOLYUBOV, member of the Academy on 31-10-1956
SUWTTED-. 17-10-1956
AVAIL"Ll; Library of Congress.
GM 2/2

ULSLOV, V&P.
--w] ~5'fikdiv for the passage from the quantum to the
clabsical limit. Hauch.dokl.vys.skoly; fiz.-mat,nauki
no.1:63-67 '58. (KRA 12:3)
19 Moskovskly gosudaretvewWy univerdtet Im. H.V.Lomonosova.
(Quantum theory) (mechanics)

AUTHORS: -NjaaIax,-V-2-.-,Samarskiy, A.A., Fomin,S.V., SOV/42-13-6-31/33
and Shirokov, Yu.M.
TITLEs I.I.Golldman and V.D.Krivehenkov, Collection of Problems for
Quantum Mechanics, Moscow, Gostekhizdat, 1957, 275 Pages,
15000 Copies, 5 Rub. 15 Kop. (I.I.Golldman i V.D.Krivchenkov,
Sbornik zadach po kvantovoy mekhanike, M., Gostekhizdat, 1957,
str. 275, tirazh 15000 ekz., tsena 5 r. 15 kop)
PMODICALt Uspekhi matematichoskikh nauk, 10,58,Vol 13,Nr 6,pp 234-237 (USSR)
ABSTRACTs This is a very appreciating review of the above book. For
the further editions it is commended to consider the group-
theoretical methods of quantum mechanics and to give
instructions for some difficult problems.
Card 1/1

240), 9(9) SOV/20-123-4--14/53
AUTHOR: Maslovz. _V-P.-
TITLE: The Asymptotic Behavior of the Ei.,-enfurictions of theEqLntionA,.i+k2u=O
Nith Boundary Conditionr .'. tlon,:~ Equidistant Curves and the
Scattering of Electroma(,mt~tic Waves in a Wave Gaide
(Asimptotika sobstvennykb funktsiy uravneniya Au + k2j, _ 0 a
krayevy mi usloviyami nu ekvidistantnykb I-,-ivykh i raoseyaniye
elektroma,gnitnykh voln v volnovode)
PERIODICAL: Doklady Akademii nauk SSSR, 1958. Vol 123, Nr 4, pp 631-631,
(USSR)
ABSTRACT: The author investi,,,,ates the equation Ayk + k~k ~ 0 in a
certain domain which is bounded as follows: a) either by
2 closed equidistant curves, or b) by 2 equidistant curves
and 2 verticals to the3e curves, or c) by 2 equidistant
curves extendin(T towards infinity. ~kjP is assumed. In the
two first cases the spectrum will be concrete, but in the
third case it vri~l be continuous. Thearc length s of the
inner equidis.ant curve and the lenl-tli r of the correspond-
ing normal are introduced as a new system of coordinates.
Card 1 An equation for ~k(r's) resuitin(., under these conditions is