SCIENTIFIC ABSTRACT NAGIBINA, I.I. - NAGIBINA, T.D.

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• Collection: Scientific Abstracts
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• Release Decision: RIF
• Original Classification: S
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• Document Creation Date: November 2, 2016
• Document Release Date: March 14, 2001
• Sequence Number: 15
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

ACCESSION NR: AP4009828
are suitable for production of laminated plastics and cast articles,
iwith good water-resistant and dielectric properties. These thermally
reactive materials based on divinyls are given.the general name dien-d
o1 S. Orig. art. has:-4 figures and 2 tables*
ASSOCIATION: None
SUBMITTED: 00 DATE ACQ: loFeb61+ ENCL: 00
,iSUB CODE: MA NR REF SOV: 001 OTMCO03
Card 2/2

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AA IBINA, -.. Z-.
"The J~Iffect of Ascorbic Acid on the Blood augar Level upon Admi-nistration
If
of Adrenalin and Insulin , karmakil. 1 4, No. 3, 1.441.
bibr. Exp. Lab., Dnepropetrovsk inst. Mvternal and Ghild Welfare -1A1-.

I ()V/I
AUTHOR: Nagibina, 1.1., Canciaate of' Phys-,*c,
- -Z-cf -en-c-C-Y-,,71-1-ov a ,C. A. , LnFirec r
TITLL: On the Mel i,oos ~& MEia:~111*trjj,~ tilt. widt!l ra, : t!.(
Contours on a eicture Obtaincc wP 'i a vabrIc-
Intertromct~-r (0 metodike i~-merr-n-iya sniriny kontUL-uv
spektrallnyk.,-, lin1y po kartint-, p-,iuc,:ayEmoy i-ri

Phr"'IUDICAL: Izvestiya vysshikh uc,-iebnykh Lave-eniy
Pribor~.,sti-,)yLniye, Nr 1, pi,
ABSThACT: Scieritil'Ic .1iterature contains a numbt-r ,I iiEtno(- 1~,i,
pr,icussing resuit5 ol' obseivbtions witri variuui;
Perrault stanciaru ass(-mbiies viitn a i;-.t-etriii :Lnstrunii-r.1-
i
The furmu'Lae FIven in litcr-turto n(-,t takf- into
consider--tion c:Ianges in the u1 the stanu-rt.,
This pa,er aeals witn mcasuring thu wicith of' a s,-i-etra'L
line without taking into account t:.(. ta~,k(,rcurc;, i.c.
I max is meaL;--reL~ from I m-,r,. As -;s
Card 1/3 fairiy iong vvinaec; (it re--uit,e~; a r,-~~ri--Tevi3tic r-,~,.-vc

On the Methods of Meanli-Ing ~!~ F~ 'h'-'
jn
a Picture Obta-,Lned wi I.h a Fa.:-
for the plate) a f Iliter fixt-,i-t, for the
input apertafe of the
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and s imp 'L i f! cs r (1,c es s in j~ r. t i picture,
The principie is ar, I a two
stage extenuafor, ~S fully
transparent ;~nd the se s ,rent
This ext1:n,iaf,-;,- i~; i.;a( f the
a ve r tur e o I' I h f2 c t r I. is
verticaaly ul;vi'iwj ir.tc 1
iine
on the
ring of one, ':Jf"- 4S ;i -,p n,~ing,
to I max anu in trit '-Onur j';~: 'q,)nding
to I max T. "I
measurement is e,-, E-,,
e Micr(~-"~;'-Ioto-
meter drum. a t
measuring- -L-1r,
CaIl 3-166 by I. of
the tested metal !.n az, ~.7i;ccr 1ji t',Ie
Card 2/3 measure(~ ring ar. givi-r., t I" E- me a s r n e

SOV/146-1-1-14;'~2
On the Methods of Measuring the Width of Spectral Line
a Picture Obtained with a Fabric-Perrault Interferometer
width being shown in both cases. The r,_pr;')Gucticz-,
accuracy of the measurements is 4% 'J% There are 1:
graphs, 2 diagrams, I schematic diagram, : f1gli-f5,
1 photograph, 2 tables and " Soviet
ASSOCIATION: Leningradskiy institut tochnoy mekha-n.4kL 41 c~~tikl
(Leningrad Institute of Fine Mechanics and Jitics.1
Card 3/3

NAGIBINA. I. m.--P 'Ind GEID&IUN, I. A.
11A~.plication of arbun Electrodes 'Ln 3),ectral Analy3is of 3,01utions".
.3b. 3tatey Leningr. in-ta Tochnoy Xekhan. i Optiki, No 11, Pp 108-115, 195",
Three methods of introducing, the solution into carbon electro(ies (". an
ac arc were investigated. They con5isted ;n imr~regnatinsy t.he electrode with
the solution in a ve8sel; derositinri drops on the tbr!ninal .C the hetLted
electrode; preliminary treat:uerit o!' the electrode with a 3% solution of
polystryrene in bezene with a subSen(1-2nt deposit and drying, bf the analyzed
solution. Tests of these methods :3~,.owed a different character of burning
of solutions., which may be exFlained by Jifferent interaction betw-en the carbon
and the solution in the first two methods, while no interaction vr7ls found in
the third case. Therefore th-- third method w~,s found the best. (RZhFiz, INO 9, 1955)
SO: Sum No 812, 6 Feb 1956

NAGIBINA, I. M.
Nagibina, 1. M. - "Investigation of the Dependence of the Widtb of the Spectrtm
Lines on the Concentration of Atoms in an Alternating Current Axe Discharge."
Min Higher Education USSR, Leningrad Inst of Precise Mechanics and Optics,
Leningrad 1955. (Dissertation for the Degree of Candidate in Physicomathematical
Sciences.1
SO: Knizhnaya Letopis', No 23, Moscow, June 1955, pp. 87-104

RAGIBIIIA.I.K.
Graduated graphs and spectral line breadth in a.c. are discharges.
1%v. AN SSSR. Bar. fix. 19 no.1:25-27 Ja-F 155, (KLRA 8:9)
1. Leningradakiy inBtitut tochnoy, makhaniki i ovtIki
(Spectrum analysis) (Spectrometer)

NAGIBINA, I.M., kand.fiz.-mat.nauk; ORLOVA. S.A., inzh.
---- Measuring contour vidth of spectrum lines by means of pictures
obtained on the Fabry and Perot interferometer. Izv. vys. ucheb.
zav.; pri. no.1:102-108 158. (MIRA 11:5)
1.Leningradski7 institut tochnoy mekhaniki i optiki.
(Interferometer) (Absorption spectra)

.-)0v/51-4-4- 1/24
AUTHORS: Dvornikova, I.V. and Magibina, I.M.
TITIE: Determination of the Degree of"Moo'if-'uniformity in DC and
AC Are Discharges ~Qpredeleniye stepeni neodnorod-nosti
dugovogo razryada postoyannogo i peremennogo toka)
PMIODICAL: Optika i Spektroskopiya, 1958, Vol IV, Nr 4-
pp 421 - 429 kUSSR5.
ABSTRACT: The present paper describes experimental investigation
of non-uni ormity in spatial distribution of excited and normal
atoms and ions in arc discharges. The investigation is based
on the theory of emission by a non-uniform source given by
Cowan and Dieke kRef 5) and on new experimental data of distri-
bution of temperature of neutral atoms across an arc discharge
~Refs 3,-4). The non-uniformity is determined from the deoth
of dips of self-reversed multiplet lines. The AC and DC arcs
were burning at atmospheric pressure. Von-uniformity was
d.etermined for neutral atoms of chromium and manganese and ions
of calcium and strontium. To measure the dip in self-reversal
lines, a Fabry-Perot etalon was used together with spectro-
graphs cf high dispersive power. The optical apparatus used
to study DC arcs is shown in Figure 4, while that used for AC
a�cs is shown in Fig-ure 5. In both figures light from are 1
uardl/4 was directed by a lens 2 onto a Fabry-Perot etalon 3. A

Sov/51-4- 4-1/24
Determination of the Degree of von-uniformity in DC and AC Arc
Discharges
focusing lens 4 projected a sharp image of interference rings
onto a spectrograph. slit 5. To study Dd arcs, an auto-
collimating spectrograph with a diffractio n grating (600 lines/
M4 Q
mm) 6 and a ulare ~_rrcr ~ wl~e used (Figure 4).. Dispersion
of the spectrograph 6 was 4 uo in the second order. In the
apparatus for study of AC arcs (Figure 5) a triple-prism glass
spectograph G-50 was used ~see Ref 7)., In the visible reFion
silvered mirrors with a coefficient reflection of 90% were
used in the Fabry-Perot etalon; in the ultra-viole'. region,
aluminized mirrors with 6,1,Yo relfectivity were used. Separation
between the etalon plates was caried from 2 to 5 mm.. The DC
arc discharge was produced between a copper anoue and a
nir,,kel-chromium alloy or calcium cathode, The AC aj-z was
produced between spectrally pure carbon electrodes The
multiplets of Ca II, Sr II, Cr I and Mn I are listed in Tabie 1.
rigure 6 shows photographs of self-.-eversed lines of green
and violet triplets of chromium,. By way of example. Table
shows the results of determination of the degree of non-
uniformity in the are discharges, 'n (as defined ia Ref 5)
from the data for lines Ca II at 3968.5 and 3933.'~ A Table 3
Gard,2/4

SOV/51-4-4-1/24
Determination of the Degree of von-uniformity in DC and AU JLrc
vischarges
gives the results of calculation of n based on the green
triplet of chromium. All results are summarized in Tabie 4.
The following conclusions are made: 1) AC and DC arc dis-
charges exhibit only a small degree of non-unifor it
kn = 1-5 for neutral atoms of chromium and manganese
2) Variation of the are current and concentration of atoms
in the arc produces some change in the degree of non-uniform-
itY; 3) For ions the are discharges are found to be more
uniform than for neutral atoms (e.g. n = 1.3 for Ca II);
ions are distributed in the central portion of the arc dis-
charge where temperature varies only slightly.
The authors thank v.K. Prokof'yev for valuable advice and
S.A. Orlova for her help in this work.
Card 3/4

Sov/51-4-4-1/24
Determination of the Degree of aon-uniformity in DC and AC Arc
Discharges
There are 6 figures, 4 tables and 10 references, 5 of
which are Soviet, 3 German, 1 Dutch and 1 in English.
ASSOCIATIOV: Gosudarstvennyy opticheskiy institut im. S.I~Vavilov
(State uptical Institute imeni S.I. Vavilov)
Len-ingradskiy institut tochnoy mekhaniki i optiki
~Lenj- rad Institde of Precision Mechanics and
Opticis
SUBMITTED: May 6, 195~
Card 4/4 1. Electric arcs--P~Vsicai properties

AUTHOR: Sov/51-4-4-2/24
TITLE: Determination of Concentration of Atoms in the Plasma
of an AC Are Discharge from the Width of Spectral Lines
(Opredeleniye kontsentratsii atomov v plazme dugovogo
razr7ada peremennogo toka po shirine spektral'nykh liniy.)
PERIODICAL: Optika i Spektroskopiya, 1958, Vol IV, Nr 4
pp 430 - 43? (USSR5~
ABSTRACT: The author measured absolute concentration of normal
atoms of manganese, cadmium, iron and of calcium ions in an
AC are discharge. The concentrations were deduced from
merzsurements of widths of non-self-reversed resonance lines
The method of measurements was based on Cowan and Dieke's
theory (Ref 8) and on discussion of this theory given in
Ref 10. The concentrations of atoms were found as follovs.
After experimental determination of the ratio u/6 (where
U = N _-~o 1 6 = half-width of the line for an infinitely
thin emitting layer) the value of an absorption parameter D
was found, for a known value of are-discharge non-uniformity n,
from curves given in Figure 1. Then from Eq.(4), which
relates p to the concontration of atoms N a and
Card 1/4

Sov/4-4-2/24
Determination Df Concentration of Atoms in the Plasma of an AC Arc
Discharge from the Width of Spectral Lines
oscillator strength f , the value of Na was calculated, if
f is known, The wavelengths of the spectral lines of Ca Il,
Mn I, F- I and Cd I and values of their absolute oscillator
strengths f are given in Table 1, together with values o4'
the degree cf non--uaiformity n . The values of f were '.a:~en
from Refs 11-14. The apparatus consisted of a Fabry-Perot
etalon and an ISP-22 spectrograph (Figure 2) An AC arc
between carbon electrodes was used as the source Df li~-h-t
Aqueous solutions of salts of Ca. Fe, Min and Cd were .:,lacec
on the end of one carbon electrode (previousiy zc.-.rered W.'Lt.,-
a layer of polystyrene) and evaporated to leave a thin
of the apl.ropriate salt. The experizental resu~us and caica-
lations of concentrations of atoms for all the lines Civen in
Table 1 are collected in Table 2. Figures 4-? Live the ey.,,eri-
mental dependences of the relative width of spectral lines on
concentrations of atoms in arc discharges. For all the
spectral lines studied, a linear dependence of u/~ on the
concentration of atoms or ions was found to be linear.
rigure 8 shows an example of ~iependence of tI;e absolute
Card2/4

Sov/51-4-4-2/24
Determination of Concentration of Atoms in the Plasma of an AC Arc
Discharge from the Width of Spectral Lines
concentration of atoms (or ions) in the AC arc discharge
on the relative concentration of the element studied in the
solution deposited on the carbon electrode. This dependence
is also a linear one. The author makes the following
conclusions: 1) Measurements of concentrations of atoms
or ions can be made under conditions where broadening of
resonance lines occurs without self-reversal in arc dis-
charges. The concentrations found were of the order of
10 12 _ 1013 per em 3 except for the Cd 1 3261 1 line for
which the oscillator strength f was small; 2) the ranEe
of the measurable concentrations depends on the properties
of the spectral line for which measurements were made,
Using various lines of one element, one may broaden the
limits of measurable concentrations. These limits may be
extended towards higher concentrations by usinE the methoa
reported in Ref 13; 3) If a mix-~llre of two elements of
different concentrations is introduced into the arc dis-
charge and the value of the oscillator strength f is
known for one element, the absolute values of oscillator
Card3/4 strengths for the other elements may be determined from

Sov~51-4-4-2/24
Determination of Concen-uration of Atoms in the Piasma of an AC A--:
Discharge from the Width of Spectral Lines
the measurements described in this paper The author
thanks Professor V.K. Prokof'yev for valuable advice and
acknowledges the help of S.A. Orlova and I.A. Berezhnaya
in this work.. There are 8 figures, 2 tables a,~d
referen,:~es. 14 of ,-.,1.ich are Russian, 2 German and 1 in
English..
ASSOCIATIO14; Leningradskiy inst-itut tochnoy rjek.'---aniki i optiki
(Lenin6rad Institute of Precision !.~echanicz ana C tics)
SUBMITTED: June 25., 1957
Card 4/4 1. Ej.eotri~,

AUTHOR, Nagibina~ I. M. SOV/48-22-6-11/28
TITLE, The Determination of the Relative Forces of Oscillators in the
Arc Discharge Prom the Width of the Spectral Lines (Opredelaniye
otnositel'nykh sil ostsillvatorov Y du~7wuk-azryade po ahirine
spektral'nykh liniy)
PERIODICAL: Izvestiya Akademii nauk SSSR, Seriya fizicheakaya, 1958, Vol. 22,
Nr 6, pp. 681-682 (USSR)
ABSTRACT, This paper uses the theory developed by Cowan and Dieke (Kauen and
Dike) for the purpose of measuring the concentrations of atoms and
ions in the aro discharge of an alternating current as well as for
the determination of the relative forces of oscillatcfs for some
-transitions. These measurements were carried out within range of
the curvature of the growth curve where the spectral lines begin
to vriden, but where their reversal still continues. Carbon eleo-
trodes were used for this experiment. A thin layer of salt of the
element under investigation was applied onto the surface of the
lower electrode. The width of line was measured according to the
theoretical curves of the ratio between this width and the absorp-
Cald 3 tion parameters, and also the concentration of the non.-exoited

The Determination of the Relative Forces of Oscillators SOV/4-8-22-6-11/28
in the Arc Discharge From the Width of the Spectral Lines
atoms Na was calculated according to the following formula:
P. 'a! . 1 M., where f denotes the absolute value of the
2mo 3ro
030IIIation force, 0 - thq width of -line of an, irfinitely thin
0
layer, and 1 - the thickness of the source. The ratio between the
vridths of the lines of Fel, MgII, KnII and CaII and of the ooncen-
trations of atomi or ions in the discharge was determined ex-
perimentally. The relative oscillator forces were determined by
means of the equation:
Pi - fl "2 , 0 are the absorption parameters
.T ~ T , where p, and P2
P2 10
for the transitions measured. the ,idth+f
141 210
lines in the case of an infinitely thin layer. Results are shown
by a table and the data obtained (filf.) are compared with the
results obtained by other author3. (Refs 3-5). There are I table
Carl 213 and 5 references, 3 of which are Soviet.

The Determination of the Relative Forces of Oscillators SOV/48-22-,6- 11/ 28
in the Arc Discharge From the Width of the Spectral Lines
ASSOCIATICN: Leningmdskiy institut tochnoy mekhaniki i oT)tiki
(Leningrad Institute of Precision Mechanics and Optics
1. Electric discharges--Analysis 2. Spectroscopy
3. Atoms--Energy 4. t4eatals-Electron transitions 5. Mathematics
Card 3/3

2 4
AUTIIOR Nagillina, I. M.
T IT i.E The DetezLuinatic-n c~f t- C-,.
of Arc dis---har-e3 Fr)m thin li'in-rh
Ce~nnecti)ns 'Ietqei~n -3 -~c, qnd
E-1 a s e 3
PERIODICAL: lzves-ti,va Akade::-'i nauk 35SR.
V 0 " 2 ~` N r ') , p - , , r, ~ 1 'o --~. r) 1 7 S S TZ
ABSTRACT- Pine of' the mos'. -,m-zortant
analysis is that cf t"-.e '-i n,,
of the investigated alemsnl~ in -.r, sam,.1,5 ar.J t`:e C-,i,-.entra-
tion of at(,mF3 or ions in 0~6 !~a~ 3c.ir:e.
T-is problem is sclved ty the I-, e:t
c6ncentrati3ns in the
vere carriGd wit bly B. S. MPI h,~ r k R,,~ f Ei ro! I j A
Pr 11 e z h a y e v a a n d V . N , G,: :r R laper
the reaultn 3btained bi
and i3ns in the cloud rX alt!~rnexiin~, t a t, 3 (,?)ar i,,e a
in consideration uf the degieq ;;f ~,f tile radlia-
tion source, i.e. of the 'I;e
~f the excited and -f at~;--q
Card 1/3 and ion-concezitrati-~n wafj -n- tne '-a8ie

5OV/48 -2~ -)- 21'-,"
The Determinaticn 5f the Conrentration Df Atome J~. thr-' :;1a3mia of
oharges From the Width of 3pectral LineE3 and the Connections 3~tneen the
Concentrations in Solid and Gaseous Phases
of absorption phenomena, in which ,;see the arc--discharge
model introduced by Cowan and Dicke was taken into account.
In the case of a sufficiently great particle density, a self-
reversal is found to cccur in inhomogeneously excited light
sources, and for this case a formula is given for the purpooe
of determining the concentration. The self-absorpticn i, de.
termined by the influence of the paramneter p in (0:
fN = 2mc6 p; (f denotes the powar --.f the oscillator N t,,.
1e2 3
number ~;f atoms per cm t~e len6th of the source. and 6
the width cf lines for an infiz--'tely long layer. The other
notations are of the uz3ut-4.1 'Kind). The experiments -are then
described. Measurements of LL-ie--width were carried out by means
of the ISP-2 spectrog-raph at varicus element concentrations,
The measuring meth3d employed by the author was already used
by I. V, Dvornikcva (Ref 7). Investipations vvere carried out
of metal salts dissolved in water and the lines of manganese
Card 2,13 calcium,, magnes-Lum and calcirm.-ions were mensured. .. direct

-y' /,A r', - 22,
"he
I Determ~nati~:,n of the Concertration ~f A'~;,ms -*n ',,.-.e 1~'a:3-a -.f
charL~es From the Width ~)f Spe~,,tral~ T.ineg qnj ;-,a n r.et et'Al e e.rl t he
C,~,ncentrations in Solid and Gase(,--~ Phase~i
rro-orti~,nality wag foirvl 'L~?tw-:,an atom- an! .On ~;-,ncentra-
t.ons in the and In' '.!.E _nvestigL~ted ~..oluticns
(Fiffs ' 2j. In thp se,,-.c.nd -,-Lrt cf the investi~~atinn ".)ie
cloud ef the dischLrge f two different ell,,~ments Yvas investl
Zated. When carbon Al-3-tric-des weE,? the quantitative rata.0
of atoms in the ]-~!3charge was found to be similar to
t
,hat in the samplr,, tne error being -i-.ren as tr,
The behav-4(;r -)f the sLbstanc,~ ir, tl.e di-a-chari3e -~s~
hoNvever, much more uilf,.rm if c.:pp,-.r plates are usej instea4l
of carbor, ele-_,tro~es. The auth;_Ir fina-I'Ay thank-? V. K. Prokof ye,
for super,iising the work. The studer- G. A' . I'letrova assisted
in oarrying out ireasurements. There are 2 f i,~~ures 2 t,,iblt!9 ,
and 7 references 6 o f wh ich ar e 'Oov i---, t .
ASSOCIATION: Leningradskiy iratitut mekhaniki i optiki
(Leningrad ",~chani,:s and 0-tics)
Car~ 3/13

PR()XDFIYKV, V.K.; NAGIBINA, I.M.; PETROVA, G.P.
Determination of the absolute values of oscillator forces from the
spectral line widths. Opt. i spektr. 8 no.3:376-381 Mr 160.
(MIRA 14:5)
(Tin--Spectra)
(Spectrum analysis)

MOSKAT-PV, V.A.; KHESIN, G.L.; NAGIBINA I.M.
- -
Interferometer for studying stress fields in transparent models.
Izv.vys.ucheb.zav.; prib. 5 no.4:80--84 162. (MIRA 15:9)
1. Leningradskiy institut tochnoy mekhaniki i optiki. Rekomendo-
vana kafedroy spektrallnykh i optiko-fizicheskikh pribonov.
(Strains and stresses) (Interferometer)

NAGIBINA. Irina Hikhaylovna; PRIJKOFIYEV, Vladimir Konstantinovich,
prof., doktor fiziko-wtem. nnuki FRISH, S.E., retsenzent;
VASIL'YEVA, V.P., red. izd-vmj ~AFDINA, A.A., tekhn. red,
(Spectroscopic instruments and techniques] Spektrallnye pri-
bory i tekhaika spektroskupii; rAovodstvo po prakticheskint
zani-,tiiam. Pod red, V.K,F'rokof'yevn, Moskva, Mashgiz, 1963.
270 p. (MIRA 16:5)
1. Chlon-korrespondent Akarlpmil n8uk S,iSR (for FrIah)..
(Spectrum analysim)

NAGIBINAY I.M.; KOROLEV, A.N.
Some characteristics of a Fabry-Perot etalon with a small
transparent aperture. Opt. i spektr. 15 no.3:421-423 S 663.
(KIRA 16:10)

- GI WADJ,H.
Spectroscopic studies of the gaseous cloud of an are discharge
during the down-feeding of powdered samples. Zav. lab. 2?
no.6:680-682 163. (MIRA 16r6
le Ianingradskiy institut tonkoy makhaniki i optiki.
(Spectrum analysis)

'ACC NR; -(-A) CO
AT7002129 sou'ticlz DE: Uti/0000/66/000/uo'_/O~j2 I 13~,28
Vorontsov, V. L. i 'iloakalev, V. A. ; NaCiJbinCL, 7. 1,1_
0.~' ': none
TLE: Dotcrmin~nc the sum of principal stresses .h the, aid of lnterf~;r3m(_-tez-3
S O-J7-~ 'I'sesoyuznaya kon-ferentsiya po polyar4-zp-'~siorL-io-oT.)tiche.-Iko,,-:a metcr.-
'ss!edovzui,.ya napryazheniy. 5th, Leningrad, !964. Polyarizatsionno-optic-.ez;~,-iy meatod
I
i3vaniya na %
Ss IeL pryazheniy (Polarizing-optical method of investiTating otreose:31;
+ -'U
dy `onfe-entsii. Leningrad, izd-vo Leningr. univ. , 1966, 521-523
TOP-7C TAGS: stress analysis, optics, optic measurement, optic method,
i,iterference, interferometer, multibeam interferometer
j~3STRACT: The construction and perfori;-.ance of a device u3ed for the Z
principal stresses in materials are described. The work was done at tht-. ~tzri-nj-'aa
:nstitute of Precise Mechanics (Leningradskiy institut tochnoy mek-nanikij arl~~
'iloscow Structural Engineering Institute (11,loskovskiy inzhenerno-stroitel-'ryy
The device is the triple-Dlate interferometer IT (see Fig. 1). The ;_nterferozeLe:-
consists of three light-separating covers A, B, and C set on glass plates. T'ne
paths are shown in Fig. 1: rays 1 and 2 form the interference pattern of greatest
intensity, and all calculations are referenced to these two. The variation of the
1

ACC NR. AT7002129
Ar
A
)17 ;m0 81~ 1C
0, C 0"
OR
17,
2 Cal
4
Fig. 1. Triple-plate interferometer: a principal diagr~~n of the devi::e;
b - optical diagram of the interferometer; -17 1 -DRSh-250 I-amp; J72 STLi-
0 rotating mirror for source shift; X - condenser; D, inpuz
' !amp; 31
7
diaphragm; Co - light filter; 0 collimator objective; 02 - camera
objective; A,B,C interferometer plates; 3 2 - rotating "ocular-photo"
mirror; D and D output diaphragms; TT - rotating ocular prism; 3,
2 3
OTT - photo attachment
distance between the light-separating covers may be equated with the lenrth of the
optical paths of the first and second beams. The path difference between paths I and
2 is given by ="N,% 26f (n- 1) P"
Card 2/3

ACC NR- A-7002129
N is the order of interference; the wavelen.,th of t*-(-' :i~h.;
an at za
. ion of thi6aiess of the model; n refract.1c'n Index o.,
model. Also, from Hooke's Law
+ -Y)
and for 6-_ - 0, it follows that
-~~ (a. +
E
where --:' and Lt are the modulus of elastiC4ty and Poisson's coefficient, res-,c-.~.veiy.
Principal stresses are then related to the odder of interference by the eci"'Llon
2tjL (n - I
N_ EX ) (:- + (C11 + -2)
The authors illustrate by example how the device may be used to dete:-Mlne _!,U.:z 0i,
principal stresses and each principal stress individually. The device --tje-1 --.g
noted as being simple in construction and in use, GOMPaCtj and stable wit"-i _-ej~ect to
vib~ration and temperature variation. Orig. art. has: 5 figares and 5 eqUa'-G-qb-
SUB COD-E: 20, 13/ SUBM DATE: 14Jun66/ ORIG REF: 004/ OTH REF; 007 z
i Card 3/3

MAGIBINA, L.P.
Heterobothrium affinis (Linton) and its position in the system of
monogenstic trematoda of the family Diclidophoridas Fuhrmann.
Trudy Zool.inst. 13:137-144 153. (W-aA 7:5)
(Trematoda) (Parasites--Fishes)

lv,q C-, / i'l / iiq
., " r,
BTK:HOVSKIY, Bje.: NAGIBIHA, L.F.
New representative of marine monogenetic trematodes from the
Pacific Ocean. Zool.zhur.33 no-1:30-38 Ja-F 154. (KLRA 7.2)
1. Zoologichaskiy institut Akademii nauk SSSR.
(Pacific Ocean--Tromatoda) (Tromatoda--Pacific Ocean)

USSR/Zooparasit31o,,,Zr - Helminths. G.
Abs Jour Ref Zhur - Biol., No 15, 1958, 67486
;mthor Bykhovskiy, B.Ye., Nagib---na, L.F.
Inst
Title The Monogenetic Trematoda- of the Sheatftsh Silurus -,Ianis.
Orig Pub Parazitol. sb., 1957, 17, 237-250-
Abstract On the basis of an tavcsti(ption of collected matcrial and,
1-4ve spucimens (1953-1954 in the Volga Delta) it has b,:en
dete.,.-mined that under thc title Ancyrocephalus siluri
(Landt, 1924), yaringuti, 1937, three species are actuaily
to be found: ;~. siluti, A. vistulensis (Siwak, 1932),
Y-=.,aguti, 1937, and 'L. --grius sp. n. (descriptions ~irc
-iven of the three species).
1. 7ooloLicheekly inetitut 1-17 SF-'37,
Card 1/1
5

CHINA / ZooparasitoloEy. Parasitic liorms. Helminths
In Animals.
Abs Jour :Ref Zhur - Biclov-iya, No 5, 1959, No. 19680
Author :Bykhovskly, B. Yo.; Nagibina, L. F.
Inst :Not -1ven
Title :Anchorophorus sinonsis 3yehowsky ot
NaZibina ;_~un. n., sp. nov. - A Roprus,Jntatlvo
of a New Family of Monogenotle Trematodes
Orig Pub :Tung-yu hsuoh-pao, Acta zool. sinica, 19558,
10, No 1, 1-7 (Chinese), 8-18 (Russian)
Abstract :A description and Illustrations of A.
sinensis from the gills of the Black Sea
fish Cynoglossus semilaevis. A nt~,w family,
Anchorophoridae fam. n., Is based upon this
new species and genus, which Is armed with a
Card 112

CHINA / ZooparasitoloFy. Parasitic dorms. Hleminths G
in Animals.
Abs Jour : Rof Zhur - Biologiya, No 5, 1959, No. 19680
characteristic chitinoidal fastning disic.
Its diagnosis in submIttud.
f~ard 2/2
9

--NAGIBINA, LI. F. and BYKHOV3KIY, 11. i~.
"New Material. on the Tayonor.y of Foly'-p-netic '-'rF-iaatrAe--."
Tenth Conference on Parasitological Proble,-.is and Lise;-.;es with Natural
tieservoirs, 22-29 October 10,59, Vol. II, lublishing Hou5e of Acudpmy (.)!*
Sciences, UJSi, Mosrow-I-eningr~,d, 1959.
U6,ft Academy of ociences Zoology institute (Lenlrit;r~:d)

BMOVSKIT. B.Te.; MAGIB.IA.-L.Z..
3Y9teMtics of the genus Diplozoon Hordma= (Monogenoidea).
Zool.zhur. 38 n0-3:362-377 Mr 159. (MIRA 122:4)
1- Zoological 368titute of the Academy of Sciences of the
U.S.S.R. Leningrad.
(Thematoda) (Parasites--carp)

BYKHOVSKIY, B.Ye.; GUSEV, A.V.; NAGIBINA, L.F.
Monogenous trematodes of the fam. Tetraonchoididae Bychowsky,
1951. Trudy Zool. inst. 35:140-166 165. (MIRA 19:1)
1. Zoologicheakiy institut AN SSSR.

NAGIBINA, L.F.
-encidea
New species of Lhe genus D-'Flozoon 'D.'L .:cno-
sr:ocotylidae, 11
I
lrudy Zool. inst. 35:lb?-17~, 16-5 . 19:
1. Zoologicheokiy in5titut A'.' SSSR.

rig. u CIO, AL )t) m I. x 43 M
W11.11 I
too
too
off
lot
w-f
jr .-ttjj,'jwd Aild )mlw pur. '~Illmlq Ive
Alw pu, tit P. .13111two 'U"ll, qj.,
,%14 urqj -VtMOA tit, Aml, jrqj Amstj% utati, NuIA rdistal-, I
jr-ums .11, plir -Jjj~ljj I" w1ma, -"qd-Yw1.uj pur
11"prinjo) -jw!jj"..p jt~ ju 4pni. NJ.,) I
, ,-t! 4J,j 11111"j, I
It "I
'"'"Jbm - N" -jjNjq oil .1410N, I'lly 114.1111 "1'l I
W*VqS"U;H W1429S JO fltW9P GAIfnj;f ROMA OU
es
t, try
tr a I '1 1,
A A 9 0 0 9 0 1 g pig 9 0 0 0 0 0 0 0 0 0 0 0 a
0 0 00 10
at& a 1k *a 0 * * : : a
T -00 9 0

Jkr/Apr 1948
wStruotural Disintegration of the TransbaykW H.S.
Nagibina, I.V. IALch1takiy, 7 pp
Olz Ak Sauk S=, Ser Geologw No 2
Bases system of structural disintegration of the Tram
baykal an results of geologic surveys of the Wt ton
years.
lm
67T43
P;L-6,,,r43

NAGIBINA, M. S.
UM/Goology - vu-Icanolow Rea/Vot, 50
*fte Age of the Transbaykal Vulcanogimous Forms-
tIOW , M. S. Nagibina
"Id Ak Nauk SSSR, Ser Geol" No 5.. PP 86-96
Br1efly sumwizes data on strattgryWu"d -~gge
of.vuleanagenous sedimentary strata of the Trans-
b"W.-Concludes these strata constitute single
formation,,' with age fixed in interval between Up-
per Paleozoic and Upper Jurassic.
168T43
16ST43

KATUSHEVOK, 1. 1. and NAGIBINA, M. S.
"Yhe Geologic Stnicture of the Region of the Upper Course of the Ur,-unka-n River,
1951.

NAGIBINA. M.S.
I ~. ,-- ~-i.
ransbaikalia. Trudy Lab.geol.doksm. no.1:107-116 '52. (KLRA 7:2)
(Transbaikalia--Geology) (Geology--Transbaikalia)

1 . NAGIBINA, V1. S.
2. USSR (6oo)
4- Urkan Valley--Geology, Stratigrai.hlc
7. Age of the Paleozoic deposits in the lower reaches of the Urkan
River (basin of the Zeya 1,1,iver), Izv. AN SSSR. Ser. geol., No. L,
1953-
9. Monthl List of Russian Accessions, Library of Congress, i:~pril, 1953, Uncl.

NAGIBUIA, ',j. S.
I
The Committee an Stalin Prizes (or the Council of Ministers USSR) in the fields of
science and Inventions announces that the following scientific works, popular sclen-
tMe books, and textbooks hwre b4mm w1baItted ror competitlan for Stalin Prizes for
the yews 1952 and 1953. (Sovetokwis MItura, Ybecow, go. 22-40, 20 Feb 3 Apr 1954)
ft= TJLtle of Work
IlTectr US T'
j-,qic .-~Pp
(Sc-l~ !:-,
SomInated by
sta~.a !T
SO: W-10604. 7 JUv 1054

ra n a e z
"10SCOVI, z
0 -IT r v
!'h a 1 3 E-~ 3 U V S i r 1 0 f
_a Dccurr' r r. t -c
"O%Ia and, Llelcmuz~la
Uri(,.,-rCormJ ti es are-
tD tdmio r!,
!,n cs i,', ;s ) --quu r ~z me tam-, r-
)-7turh tus ; phyliltu.3 :r'ica_cj_!
s, rLcl r-:-! -aceous-3iliceiao , Lind 91.:.;
a r,,, g c s r.):,4:1 y altered voicani I

a z D --'c 'il tra t -* ;--r& z,.
sands tores , and 1-irres tones (-ai t,-, u to ta-1 t,-Iickness of severa'
kilo-ieters); 21, Upp(,r roc~rs ~:,,)--Inti.-rl ' edded
1 .1 c e s s :-Y-i
arlrc-~silc sandstones, sar-`-: s*-1&1(.;3, arEI.I.Iacejus s 1 1
s-u',o---;-!nate layers o' an.
an~'. 3) -)re-Devon'r:~~ r,--',c~rs -n to l.'O'j -.) iri the has1r,
a
n(3 ve r t: - s t-' -i-zar tz co-r-- iomera t es s, rd s r~
a nd c- o - t a I n g Mi r, e r s a c, e K t ru S;
v es ; I iMe S t 7 ne s t e E:
r t F-. ','i r, s Tne F. r o , r j s w7.' c
snore al--zndart
s-ilc!IvI~i1rr tl',e :*,c: ',f--iu1z..a serles and as3!,,ninr ai.,,~s
o ~ r h e t h r e r o, in ~3 a - Q v r, I (,, I ow I n t, ho bfA si n o i' t ne !~o ra k:
the apper ---j-ip rests wl' tri a marbled unconformity on rocks tha t
co-, ta ~ ~ cinarac ter is t! c Si -lurian f oss ils . In similar formations
farther west, Uppt-r Devoriur, 'L.raci-.1opods and bryozoans had prevlo,,:--
beer. found. 'iew c3liectlons of such Upper Devonian forms have
teen made. Siluriar: loss-4-s have 'Leen four.d at many places in roc~-
of the :-.Iddle gro~ap. Late Ordc>vlcian brachiopods aad previously
f,)und in the upper reac~ies of the 'vSarayn River, indicating that t"i-
sequence of rock I)egar-. to form toward the end of the Ordoviciun.
rocks of the middle group overlie the Tukuringra series with al-,
Card 2/3

Paleozoic Stratigranhy of t,,,,e Zeya-Selemdzha (Cont.
15-b7-5-_t749
angular unconformity and the conFlomerate at the base contains
cobbles of metamorph-Ic rocks. ConFlomerates occur at a numIr-er o'
places in the Tukurn~,~a series, and these contain cobbles of cr:'~stal-
line Archean rocks. T us, r.',je a~,-e of tne Tarj_~liringm series is pr-e-
Ordovician: Caml,rian -Pro ter,,zo -!(- ,T-~p author discusses the E:eo-
lop-ical historv of "-.e :,e;-. Tie BunAnAdy _.Ia3si 'L hAd been isolated
bv lower Paleozo'c time, as s-own bj maximum volcanic activity along
the borders of the Ma3Sif, recordle-I 1r, the Turkuringa series and in
the Silurian rocks. The Middle Devonian rocks withIn the Fareya
massive were tut sliFhtly deformed and rest on Silurian beds with a
marIked angular unconform-Ity. .'art.-ier .,iest all the Devonian. rocks
(irciudin~,- the Middle Devoniar~) -Le witri apparent conformity on
Silurian deposits.
Card 3/3 V. V. Kh.

1~-57-1-1070
Translation from: Referativnyy zhurnal, Geologiyal 957, Nr 1,
PP 171-172 (USSR)
AUTHOR: Nagibina, M. S.
TITLE: The Geological Structure Along the Left Bank of the
Amur River from Kuznetsovo to Blagoveshchensk
(Geol6gicheskoye stroyeniye levobereZhlya r. Amura ot
s. Kuznetsovo do g. Blagoveshchenska)
PERIODICAL: Tr. In-ta geol. rud. mestorozhd. petrogr., mineralogii
i geokhimii, 1956, Nr 3, pp 212-235
ABSTRACT: From previous investigations (P. K. Yavorovskiy, V. A.
Belov) S. A. Muzylev, and A. Z. Lazarev), with ad-
ditions and supplementary data introduced by the
author in 1951, the author describes the stratigraphic
section along the left bank of the Amur River in the
indicated region. 1) Archean. Ancient formations of
Card 1/4 various compositions: gneisses and gneissic schists,

15-57-1-1070
The Geological Structure Along the Left Bank (Cont.)
cut by granite gneisses and granites. 2) Proterozoic to lower Proter-
ozoic. Beds of interlayered varieties of schists with seams of
white and gray crystalline limestones. 3) Intrusions of rose-colored
alaskitic microcline granites. 4) Paleozoic (Silurian ?). A
sequence of interbedded greenish gray and rose-colored metamorphosed
arkosic sandstones and sandy shales, yellowish white limestones and
violet calcareous shales, sheared and epidotized diabase porphyrites,
agglomeratic tuffs, and quartz porphyrites. 5) Intrusions of biotite
and biotite-hornblende granites. 6) Jurassic to Cretaceous. A
sequence of coarsely fragmental conglomerates and sedimentary
breccias, sandstones, and shales. 7) Hypabyssal intrusions of grano-
diorite porphyries and quartz porphyrites. 8) Upper Mesozoic. Vol-
canic formations (layers of basalts, andesites, and quartz porphy-
ries). 9) Upper Mesozoic to Cenozoic. Yellow and light gray sands
with layers of clay and brown coal and Quaternary alluvial deposits.
The author gives a detailed description of each stratigraphic unit.
The attitudes of the above-mentioned rock groups are observed only
Card 2/4

15-57-1-1070
The Geological Structure Along the Left Bank (Cont.)
along the riparian zone of the Amur Rivei7, in numerous exposures on
the banks. Away from the river, bed rock is covered by a thick
layer of unconsolidated Neogene sands. The following structures are
found in the investigated region: on the; southeast occurs the
Blagoveshchensk extension of the Precam~,rian basement (the western
margin of the Bursinsk mass); on the noilthwest lies the Novo-
Innokentlevka extension, which joins th~ Kuznetsovo-Yermakovo uplift
to the north; the rocks consist of a seq~ience of metamorphic varie-
ties of Proterozoic or lower Paleozoic a~e, cut by intrusions of
granites and plagioclase granites of mid(Ile Paleozoic age, and over-
lain by coarse-grained continental Juras"Ic deposits. Both the
older rocks and the Jurassic sediments = transected by numerous
faults. The central part of the described region is composed of
young upper Mesozoic volcanic rocks, also~cut by faults. Between
the region of young volcanic rocks and th~ Blagoveshchensk extension
lies the Sukhotinskiy synclinorium (a Sil~rian volcanic-sedimentary
complex). The author concludes that the t~ 1. stablishment of the
Card 3 4

15-57-1-lL,.70
The Geological Structure Along the Left Bank (Cont.)
Paleozoic age of the volcanic-sedimentary geosynclinal sequence,
earlier considered to be Mesozoic (Triassic), and also the strati-
graphic and structural data from neighboring regions, permit the
assumption that the region along the left bank of the Amur River is
a district of Hercynian folding.
Card 4/4 T. A. G.

SHATSKIY. N.S.; BOGDANOV, A.A.;BELYAUVSKIY. N.A.; TkMESHChAGIN, V.I.;
ZAYTSEV, N.S.; KOSYGIN, Tu.A.; KROPOTKIN, P.N.; MURATOV, M.V.
Y.N.; PAVIAWSKIY, Ye.V.; PErIE, A.Y.;
PUSHCHAROVSKIY. Yu.m.-, SALOP. L.I.,; SOBC"VSKAYA, 7.N.;
KW&RITONOV, L.Ya.; KHbaASKOV. N.P.; SffiffNMAN, Yu.M.; SHTRETS, N.A.;
TANSHIN, A.L.; VERSTAK, G.V. redaktor izdatel'stva; GUROVA, O.A.
tak-hnichaskiy redaktor
[Tectonic map of the U.S.S.R. and adjacent countries on a scale of
1:5,000,000; explanatory notes] Tektonicheskaia karta SSSR i
sopredel'nykh stran v masshtabe 1-5,000,000; ob"iasnitelInnia
zapiska. Moskva, Gos. nauchno-tokhn. Izd-vo lit-ry po geol. i
okhrane nedr, 1957. 77 p. (MLRA 10:5)
1. Akademiya nank SSSR.
(Russia-Geology-maps)

AUTHOR: Nat,ibina,
TITLE: New Data on tne Toc ton', -s
N o vy y e d a n n y y e p o t e k t K e " Ni:) n ti,-
PERIODICAL: By u 11 e t e n I Mo s k v s k o ~r o o b s h ~-. i: s t v a F t
0 t -d e i ce 0 1, ot~-J- C h;, 3 Y F.

ABSTRACT: This article dealq with [~(.W j 'i t 'I t
belt located on the bnundnriea of 0;e oxt-.~,Ivo
tic folding area, interf,09P"t hk?tWeQr1 t'.-
berian plateau. The author :-,:,ns S r -
.- . , 1 a t 4 , j:
the marginal zone of the East As i I .
area within the lini~s of which shar-c' Y7.
depressions were formed durn; r t
represent the c~,aracteri~-.tJ- f -3~tures t h
clinal stage in the deve::-,pm,?r.,' :)f area
mation of these structures, wazi t 1% e,.
process ; a spec 4 a I 'y., e f' M,.~ , .:~ 1: :~ - --i
in the Pac,~ ~'i ~: ret, i: n %,~cmpnn! hy
magmatic a,: tivi t les
area und the uil-~ur f -;rmIc- - c-r. ho 7
of the Siberi.lin pluteLnu
Card 1/3 inten.-i and

New Data on the Tect3,~-12s of z:-e
of the foundations. Extert~~ive mater:al I I
au thor c I ea r'-,y empha 3 i2 e s t he Ma 171, ",.,1 r I c,,' P
Hercynian folding 3.ruc Lure )f thc. !Y!'.
determines the large ba-il-1- Bt
golian-Okhotsk belt. Thp.morpholuf_'c ar-I
of the Meso zoic de press i ons of thi s --i rt~a J i
form the typ-ica. g~osynclinal e
of the lar6e structural elements of 1-hle e
ozoic a6e with longitudinal rupture~j sh,"a.- 1, r. - r
nection with the distribut.~ or. of var~(ja.-, ";F,
The east part of t h e T r,-, r; z3 - BW?U41 -i r (2,,'L -a
lian-Okhotsk belt being studie~i at lna
a close c(Dnnectior vii th the orp de, o:,i
eastern strikes (as dist: ng-uis,.ed ~,y 3, SSm-
structural elements. The findings Q i''. w-
taceous granite intrusions in B~x, kl~x~ r-,-:
~rofnising prospects for findi-ig non-fer:- .; li,-. ;
in ccrinect-lon with tnese 6ranitcds, I ~;t I-.
following scientists in this artf,-,I", A,v~, F- - V
Obrucne v , A . D. Ark hangel, ; sk : y , N :3 +-,:- ~ - yY,
Card 213 A.N. Mazarovich, M.S. Natjtina, I.V

New Data on the Tec tonics G.' * ne
N.A. Korensov, A..A.
kin, L.I. Krasnyy. Y A fkvizal e-.-- aN
V V S t a r c h e ri,~ u , Y -AR 1 N
I K N i k i I'o rk-, v a , 'N . i . K, ~,- r; L - v.
Mashkin, V,V. Belot-,so-., Yc-~V. P~"."
There are . mui,s, : fl~.,-Ur-
ces .
1. Geoiogy-Mongoliri
Card 5/3

AUTHOR: Nagibina, M.S. 11 - 5P-'! -4 /1;)
TITLE: Stratigraphic Scheme of Jurassic and Cretaceous 7eposits in
the Basin of the Upper Part of the Amur River !Skhema strati-
grafii Yurskikh i Melovykh otlozheniy basseyna verkhnelvo
techeniya r. Amura',
PERIODICAL: Izvestiya Akademii nauk SSSR, Seriya geologicheskays. 191,8,
Nr 7, pp 55-75 (USSR)
ABSTRACT: The basin of the upper part of the Amur river has been studied
since 1869, when widely spread Mesozoic deposits were first
discovered. The following geologists and paleontologists have
studied this region since 1927: A.I. Khlaponin, A.A, Leontovich,
V.D. Prinada, O.M. Kichigina, N.P. Savrasov, V.Z. Skorokhod,
P.F. Popov, B.A. Ivanov, S.S. Dobrynin, N.A. Frumel, A.T.
Arkhangellskiy, D.M. Sayapina, R.M. Tonayan, Ye.Ye. Krasnyan-
skaya, N.Ye. Slastenova, M.S. Nagibina, A.A. Kalinovskiy,
B.G. Kuznetsov, A.D. Britchenko, A,A. Kirillov, N.F. Levykin,
Ye.A. Modzalevskaya, M.N. Petrusevich, I.Srebrodol'skaya,
N.P. Kheraskov, T.N. Davydova, G.F. Krasheninnikov, `,.Ya.
Krymgollts, I.Ye. Khudyayev, Ye.V. Pavlovskiy, T.V, Luciritqkiy,
V.N. Kozerenko, A.F. Mushnikov, V.V. Onikhimovskiy,
Card 1/3 Myachina, P.T. Regunkov, 5.G. Martinson, D.D. Penninskiy,

11-59-7-1/12
Stratigraphic Fc he me of jurqssic Rn.d 77etqce-o-s 7eposiJ ts , n t-e r. of
the Upper Part of the Amjr ---',;er
V.A. Vakhrameyev, and N.A. Bolkhovitinove. All of theme
scientists studied vario,.is parts of the region. 7his Rr*,-_-I-Ie
presents t:,e recapitulation of their studies, nn! tne a-_;-or
established a new stratigrRphic s(-heme of the repiDn. Acccr~-
ing to V,7~. Skorokhod (Ref. 9~; the Mesozoic deposits -)f "he
whole ret-ion could I-e divided in two comnlexes: TRrltl7e ~-e-
posits and sweet-water continental deposits. -he mqritime de-
nosits form the following horizons: 1, fundamentAl 'bnsic'
composed of conglomerates and coarse-graine~ sandstones ~
2) inoceramic - of sandstones and sandy shists i1from 'no_eraIT.,j___
porrectus -ichw.); 3) alternating sandstones Rnd shists;
4) ~;ervillia sandstones and argillareous shists 'from ~Iervilllia
sp.); 5) Modiola and variegated sandstones (from. Modiola
By the remains of the fauna in all these horizons they were
classified as belonging to the Upner, Middle an! Lownr ..T,irassi:
period. Their overall qgnitude is ~,71C m. ~In tnese maritime
layers the sweet-water continental coal-bearin,7 depoqit~~ f-.rm
the second thick series, These deDosits were mainl.v formed by
Card 2/3 clastic sediments, representing alternating layers of s-indstone

II_C) ;--7-, 1,/I-,
t ra t i gra ph i c 'c h eme o f J u ra,; s i c n nd rre t a c e o u s ~ e p'.) q i tn i r. t h c- ~, a s i n r)
the Upper Part of the Amljr ~,iver
conglomerates, aleurolites, argillates, carbon8ceous shists
and coals, between which interlayers of acid pyrociastic rocks
and thin interlayers of felsites were found, The P.,eneral
magnitude of these layers varies from 5,2CC to 5,qcc M, ludy
points
of adjacent regions,from the geolowic and paleontolo,-ic
of view, showed that all these deposits telong to the "pper
Jurassic - Lower Cretaceous periods. The comparison of the
stratigraphic profiles of different parts of the Amur river
basin showed lRrge variety of facies and magnitudes of the
sweet-water deposits, which is directly connected -Nith the
peculiarities of the tectonic development of the lar,,e Meso-
zoic depressions of the region, There are 2 tPbles, 1 :ran,
3 diagrams, and 11 _"oviet references,
SUBMITTED: June 9, 191F~
ASSOCTATTON: ,eologicheskiy institut All %Voskva 'The -,eolloizicai in-
stitute of A") U').",R, Moscow~
Card 3/5 1- GeoloRy - USSR

3(0)
AUTHORS: Nagibina, Kref7tovni~:o,.-, V. r0
unznan Fru-Chun', Gatin~~kif, Yu. 5.
TITLE: Recent Discoveries of ial~,-ozoic F:ium~_, in tl.e Malvy KhinF--an
Mountain Range (China) (Novyye n.--khod',i f%uny v
khrebte llalyy Khingan (kitayskiy)
PERIODICAL: Dolclady Akademii nauk S)"S'R, 1950, Vol I,"), Nr 5,
PP 910 - 913
ABSTRACT: The Sovetsko-Kitaysilaya Amurskaya ekspadit~,.iya (Soviet-
Chinese-Amur Expedition has found a fauna in t~:e undifferentia-
ted volc.,.nic and sedimentary rocks in the northern part of
th4.[_1.-.y Khir.Can and th ~Ikhuri-Alinl, Thin fauna allowed
subdivi.-ion of thisquite of rocks,. The suite lies with an
angular unconform-ity on folded crystalline rocks of t~ie Upper
Arcliaic, Proterozoic, arid Lower Paleozoic. It is intruded by
igneous rock of variou.,i c ompc,)si t ion.;,, In t~ie i~,edimeiita:y
sequence, Silurian Lower and 11iddle Devonian, and i'ermian
strata could be determined, The definitely Silurian rocks
are distributed in "al in the southern p...rt of
.1 yy Khin~,,,,n and
Card 1/3 Illkhuri-Alin'. They are relate(l to t.o SiluriLn sedil-nentary

Recent Discoveries of ?aleozoic Fauna in t;e i'a_'y Kh 4 7.- :3 50
_an
Mountain Range (China)
rocks of the Sukhotinski.-/ ~_,nticlinorium on t e Ic-ft side of the
AMUr Hiver (USSR) . T~tey a:-e furt:-.er exposel L-on,, tne highwray
between the cities Of Kheykl.e and Nunltszyan. The Silurian
beds are many kilo:;ieters thick and --;.-e entirely r-imilar to
the faunally characterizad Upper Silurian rocks of t-e Nora
River discharie region (USSR). Devonian sedimer.tary rocks in
this area have been known :;ince 19.12 (Re' s At, 5), Also Vie
authors found a Devonian fauna in t:.e Kal:,-y Khin~:--in ( 19cl, ) "
The rocks lie unconfcrmably on Silu-ian 2tra-ta and outcrop in
2 areas. They are faulted ind intruded by ilranite bodies
(Erchzhan3kiy stock), Chinese ~;eolozists under t,,-,e leadership
of Chzhao Guy-san' divide the Devonian into 2 suites: a)
Nitszyukhe (1500 m thick) ;LIA h) Kholunmen (800-900 m thick).
A fauna was f3und in t;ie 1~tter suite on %Iount Vankholu and
in the vicinity of the villa,,-e of Din'Fhuy T_~e brachiopods
were identified by V~ N. Krestovnikov, t'l.e trilobites by
Z. A. Maksimova,and the pelecypoids by I, N. Kr.IFil.-)va. On
the basis of general fauna c~iar cter, ti.e lo-.,,E-r p;.rt of t~.e
Kholunmen suite may belong to the uD:)er -'.Lrt of' t.,,e Coblenzian
Card 2/3 (Lower Devonian). The for-is of t~~e Din'shuy rockci have the

Recent Discoveries of F'aleoz~,,-ic F.-a- ir t-.e Kh--~n -,-n
Mountain Range (China)
ASSOCIATICN:
PRESENTED
SUBMITTED
citaracter of 1 ~,!r!lQ Co'rlt~nz-m st:i P. Tle hi,:,.,.er h~)rizons
Ai
of thir -,ta,.e and yet the lo%,ier- h~)ri7ons of the Eifelian
st-.ge Do,ioni-.n) be rec~)wnined t'.: f )!Xsil
remains (Fi,-: 1). T..e Ili tsz~,ti"'.-w -,i:ite is Clelinnian
by the auth:)rs, rofess,)r Yii'v Tszy in ' ~hz:-..%n collecte~l f ossils
on the Kheykhe-Niinlfs~yanl hiKhway in t,.o ,Louth in 11)5~~; he
identified them as i1er-.iun-CztrbGniferoi!.; Sedimentary rocks
with Permian f.,-o:na1rh:iracteriqt4cs were only foun(l in t.~e
vicinity of h~ount Diguan'nhanl ~Cetitshin-y gyrebenl). They
I (iJentified by L L, Khul-
are 300 m thick, -lere i3elec.veods
fin) were 'ound. The cormian be:l~ lie ~iscorden'lly on folded
Middle Pa.'eozoic and ol,ler The,f -~re luciistrine arid
narine, depn~-,ited in I c,11 barins. Th;,re :tre 2 fi,-,ir,,:3 -.tnd
5 references, ~ of which are -S v'et.
Geologichepkiy institut Ak~,demii nauk S35R (Geo.,)~-,ic Institi~te
Acade-7.y of Sciencos USSR)
AuFust 2, 19r8, by N- S. Sh!-,tskiy,
July 4, 1958
Card 3/3

T I Lp, 'IC
U,-,per
P: - i:

PERIODICA:,: Izvest.1-:,ri 11 ... 1 -1*"-, 3-,3SR,
Ni-
9 5
I 1B
T Tne a-ut~-C-, L, dc, 1-
. u n s c f
P r i amtu- y t3 c c i f i f e i
or, o f
~.uF,e ef. f uE~ive n c, f 3 r,,::

The rut-.or cites V.-;, ae-
.~C 4
0
e 5 r, s i c
ava an i no
a'on e- e -j-,- 11 V
and bLi~;ic eff--,.k.-~icn- c: r,:
"d z- yl e -%f on e ;,n,
izu cc ~,I (i ...
-T, v -:~ 1 . "J a C;

U,--per Crera~~eu*-:
Nora an~,-'.
hyr i- t e z- c' i j, r. -7 3 r-
~inoi er, L; i~-ran- P, Th,
i n t o V V . 0 n i k L r o v 1r: i c) n n,,:
b nd i nfz wi- h ~l t e r; 1 1, i C-
1 y I A
I d e f ICU LE I I r
of Burdind,--t
lie C 1-1 Li
fUSlVe.-, Lfi the c:~7.posi~i--r~ t i e n
A.7.
Isc, no*ed by A.K. Ar--,en'-:ev.
was Kh'auonin,
.
L
piex
-
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-

-
A. Leonzovi -r i riad,3 -,-; - I ) ~.,
--Ai an(i V.D, 1 lie
A
-, h e
;
n
.
I Fa! -ner
3f che Am!.j a:, ld
ul,per
C, 1 c -an, o Gr~ n c- r mu t C, r~ S 7 ID r r
Z '--o -
h yf.
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C a nll

UPP(-,r
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2-~ nd
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k2
::ble
S U-BIM .7 T T E D
~Iard 4/4

N&GIBINA, H.S.; MSTOVNIKOV, Y.N.
Diagram of the Paleozoic stratigraphy of the vicinity of
Zeya. Izv.vys.ucheb.zav.; geol.i razv. 2 n0-11:3-19
N '59. OGRA 13: 6)
1. Geologichaskiy institut AN SSSR.
(Zeya-Geology. Stratigraphic)

3 ( 5 Y'
AUTHOR: Nagibina, 11. S. SOV/20-125-5-37/61
- --------------
TITLE: The Tectonic Scheme of Northern Manchuria (Skhema tektoniki
Severnoy Manlchzhurii)
PERIODICAL: Doklady Akademii nauk 353R, 1959, Vol 125, Nr 5; PP 1089-1092
(USSR)
ABSTRACT: The author, together with Yeh Tling-sling out geological
investigations in summer 1957 under the auspicea of tne
Sovietsko-Kitayskaya Amurskaya komplek8naya ekspeditsiya
(Soviet-Chinese Amur Multiple Purpose ExDedition) on the trend
from Blagoveshchensk over the city of Kii-n-chier. "Hergen') to
the village Argunsk in eastern Zabaykal'ye (Transbai-
kalia) across the mountain ranges Malyy (Minor) and Bol'shoy
(Major) Khingan. Various Precambrian, Lower Paleozoic and
Devonian sediments take part in the geological structure of
this very sparsely investigated region. There are sedimentary
and volcanic geosynclinal-type formations metamorphosed in
varying degrees. Relatively weakly metamorphosed Permian
sandstones and shales unconformably overlie the latter. These
are found interbedded with volcanic rocks of marine, continen-
Card 1/3 tal and lagoonal origin. The upper structural stages consist

The Tectonic Scheme of Northern Manchuria
of continental Jurassic and Cretaceous sediments in addition
to volcanic, sedimentary, coal bearing Cenozoic deposits an
well as basalt and ande8ite effusions. Intriisive fcrmations
of various ages are exceptionally widely distributed here.
The author differentiated the following large structural
elements along the main investigation route from southeast
to northwest. They are formed geologically differently and
lie one after another northwest of the gigantic Central
Manchurian Synecline. T h e n o r t h w e s t e r n
e d g e o f t h e Y ae C I f_ S '~_. m e n t i o
n e d S u n 1 y a u L y u o t u n s o y e u p
1 i f t T a y a s hu n a k i y f o 1 d
V e r k h n e ( U pp e r ) G a n1k h i n s k o y e
u p 1 1 f t . F o 1 d o f B o l's h o y ( L a r g e
K h i n g a n r ia r u n s k o y e ( A r g u n
n e a r ) u p 1 i f t. Northern Manchuria was previously
tentatively considered by Soviet (Refs 2,4') and by some
Chinese (Ref 5) geologists as a region of Hercynian folding.
This is confirmed by the nuthor. These fold structures are
strongly reworked by block folding, movements of Upper Meso-
Card 2/3 zoic a.-e. In the Cenozoic the formation -)" large, platform-

The Tectonic Scheme of Northern Manchuria SOV/20-125-cj-J71/61
type structure8, broad synecliz;_~ itructures as well a3 flat
arch uplifts of the two Xhingan Ranges occured. The faults
"lived" again in the Tertiary. New fractures formed, alontr
which effusions of andesite, basalt, etc molred. The asser-
tion3 concerning the bow-formed bends of the Paleozoic struc-
tures of this region (Refs 1,3) are no more confirmed than
the division of Northern Manchuria into a zone of early and
late Hercynian folding (Refs 1,'). Data on ore 0COLTrences
are given. There are I figure and 5 Soviet referent-ea.
ASSOCIATION: Geologicheskiy institut Akademii nauk SSSR (Geolo~_,-ical
Institute of the Academy of Sciences;',JSSR)
PRESENTED: September 30, 1958, by N. S. Shatskiy, Academician
SUBMITTED: September 27, 1958
Card 3/3

NAGIBINA, H.S.; BOLKHOVITINA. N.A.
Mesozoic stratigraphy of the upper Zeya trough. Izv.AB SSSA.Ser.
geol. 25 ao.1:28-42 Ja '60. (MIRA 13:8)
1. Geologicheakiy institut AN &ihR, Moskva.
(Zeya Valley--Geology, Stratigraphic)

,...b.ltt.d for the 10th Psafto Sciaom. Congmas, Honolmlo, Rowell ZI An,-
of Geology and t-lwh.
y-P. and their pcsltlun in t."
t
foms* (Sectio. M. C)
IECIM, D. A., No.cow State UnIverolty. Phy. L.1 I-,aty - "Th. 4-.-,.y
op-41i~trl. "--to of artLflol.Ll '.4 1. aoe tivity to upl- I&",.
tI..I
of tbl (3-0 VI
Cbjr of For. The :de='YtL...L(K. A.
Fr. at r1r,e romer-y'l, and f fir :on rLl.Sa"ton V.D)
.1 ..ttut. of 0.1.1'&y - *Bl.8.'U."hlcl _d
-ph.l.cic.1 ane.1yalls of reprod-lil.. -4 _.e--,w..nt of flatflob
the f0 rt 1~... n I_
Ln I,as I the , h-.t :-t~,(5-t.
,. I. 'tote-;,-!- zf -ta.1
C~X~l - --Zy .- ~ t ~, tt~ r-r.
turtna_~-Y...'1-8'e ~. 'ho"O-'i rL 0-'
Ntm'-.1Z V. IL..t.'t... r 0.e_Q'..Cj
dl.trib.-l.. of rLylnG L~ ti. P~...%~ VII.C)
h,riz- in the
T~~.M ml~ A., In.tlt,t. if G-J~a
-t--. d.p..It. ~f K--tk.' (S.- ... '11..
MMILM.-Y. P., Institute of 0,,wzLgy p!,ce3,c, ct re-t 3~1-
e-ot&tLoo to t p-t ~f thee~n the P-1fir
'x weste
t
(G.Ctl- VTI.C.J)
X.wT=-ZOXXL_D, A., Inatitit, if Eexth Phlslie -.'l C. r.. S~ -14,
'Tr" COL"" '06"ce'l Lnd`i-. L'. tt' _"J"! 'ut~ In"
or t~,o F~LflrbZ~ " (S..t!'. 11I.C.2)
I. ".' Inotit,." if Occon"__-z Ir. th,
..rtb.- ;--t of lill, ?-ifl" ~S.Ctl- III
"Thi
br-wee fr~o U~, ;~izt ~f ~t,e III.A
~o-fth,
A
(:ic n r:.
t'r
A., ~f G Ina, -d
Lz.bmrlt=ce of St-t-1 e2ments in Uw t- ft-ifl: 0-1
dep-saloo" VCI.C)
P-43S. T . NMQr',&~ :..A., ond lnstltute jor
rCaerttlc%
d_,l.sr-t of)-.. J~l the -rt~-7. -tf P_ t r, c'
'.1c- A. I~t-_ic " 0-L_'Z S,b,t=c- in
bottact -dL-t. Lz t~, --:m pe-i .r t~ P-r_~
L
le. jl~rn.ttt,, f -~h Pl~y~ica t, ai 0. -t
t
bet-e. f-'. enrt!_1 ~r
_thn
Let. I- t-ct-- ~r
-Th~
It-ey.' tveratty, P..y-- Y%,.!ty, :h- R-3
'e
h,d f,r
1""* F-IoL -or, to the -~her. 'f tn~ .,a "I
the ror--pl.6 .fthe F`~' C'.relter (3-, ~;.
4e-, 11h U,
MID' - -Il I..t.' i_4.P.
ho~_
try f lec 1. -.1
cScttm VII.A) 'r th.
!;Egn;A~ C - to
L~tlt
TZ-1 r=- a, r. ---d
F-.,tf-
e~pjl~c' savilzv, Y, tnatit- 'f to t:...
th. P_: f: (3"t t'
L'!t
X-1
L-71. C-t. rcnfL-...
.f b-
-.1eL.e-
P. A.?
on S. r1l..D.L)
sly= tt- f c
-r;=t3.'. the 'c- .." .- re-." _f L.1 t,:,
P..1 1, -_" (5,oct'-4 rI:.D.5)

-JAGIB~MA,__~.S,~- KROPOTKIN, P.N.; MAMOVA, N.G.; 60BO V6KAYA,
STREYSP N.A.~ LE
V.N.; PEM, A.V.; PAVLOVSKIY, Ye.V.
Andrei Khrisaafovich Ivanov, 18c/7-1961. Izv.AN SSSR.Ser.geol.
27 no.3:114 Mr 161. (KIRA 15:2)
(Ivanov, Andrei Khrisaneovich, 1897-1961)

I NAGIBINA, H.S.; MOLZMOVA9 T.V.
Structural position of Mesozoic granites In the Mougolo-4ftotak
zone and the adjacent regions of the Stinavoy Range. DokI. AN
SSSR 136 no,2s424-427 16L (101 '14:1)
9
1. Predstayleno, akademikom H.S. Shatakim.
(Asia-Granite) (Geology, Structural)

-NAGIBINA, MarinaL Sergeyevna; FLORENSOV, N.A., otv.red.; PEYVE, A.V., glaV-
nyy red.; MARKOV, M.S., red.; MFWIFI~, V.V., red.; TIMOFEYEV, F.P.,
red; ARSENIYEV, A.A., red.izd-va; RYLIIIA , Yu.V., tekhn.red. A
[Tectonics and igneous activity of the Mongolian-Okhotsk belt.]
Tektonika i magmatizm Mongolo-Okhotskogo poiasa. Moskva, 1963.
463 p. (Akademiia nauk SSSR. Geologiche:ikii institut. Trudy, no.
79). (ICPLA 17*-2)
1. Chleny-korrespondenty AN SSSR (for Florensov, Peyve).

DZEVANSKIY, Yu.K.; DODIN, A.L.; YONIKUV, A.Z.; KRASNYY, L.I.;
!"AITIKOVSKIY, V.K.; !,'OSHKIN, V.N.; LYATSKIY, V.B.;
NIKOLISKAYA, I.P.; SALCP, L.I.; SALUT4, S.A.; RABK1771
M.I.; RAVICH, M.G.; POSPELOV, A.G.; 'NIKOLAYEV, A.A.;
IL'IN, A.V.; BUZIKOV, I.P.; MASLENNIKOV, V.A.; NEYELOV,
A.N.; NIFITINA, L.P.; NIKOLAYEV, V.A.[decensed); OBRUCHEV,
S.V.; SAVELIYEV, A.A. ; SEDC.VA, I.S.; SUDOVIK(jV, N.G.;
KHILITOVA, V.Ya.; NAGIBINA, SHEYNMANN, Yu.M.;
KT!ZNhTSOV , V.A.; k-11NMOV, YTJ.A.; BDRUKAYEV, R.A.;
LYAPICHEVI G.F.; NALIWIN, D.V.,, glav. red.; VERESHCRAGIN,
V.N., zam. glav. red.; ~ENNER, V.V., zam. glav. red.;
OVECHKIN, N.K., zam. glav. red.[deceased]; SOKOLOV, B.S.,
red.; SHANTSER, Ye.V., red.; MODZALEVSKAYA, Ye.A., red.;
C HUGAYEVA , M. N. , red. ; G RESSGEYM., V. A. , red. ; K-'-LLFi , B. M.
red.; KIPARISCVA, *.D., red.; KOROBKOV, M.A., red.;
KRA9NOVY I.I., red.; T.Ya., red.; LIBROVICH,
S., red.; LIKHAREV, B.K., red.; LUPPCV, N.P., red.;
NIKIFOROVA, 0.1., red.; POLKANOV, A.A., red.fdecensed);
RENGAIRTEN, V.P., red.; STEPANOV, D.L., red.;
CHERNYSHEVA, N.Ye.; red.; SHATSKIY, N.S., red.[deceased];
ZBERZIN, A.G., red.; S1'IiU1(1VA, Z.A., red.izd-va; GUROVA,
O.A., tekhn. red.
(Stratigraphy of the U.S.S.R. in rourteen volumes. Lower
Pre-Cambrian] Stratigrafiia SSSR v chetymadtsRti to-nakh.
nwimu Dakembrii. moskva, Gas. nauchno-tekhn itd-vc lit-ry po geologil
_ .. . - - --..& _? +I,. TIV--M .4Q6n-

NAGIBINA, M.S.
Study of the geology of Siberia during the post-Obruchev per'-c-sc.
Och. po ist. geol. znan. no.12:116-123 163. (MIRA 16t1O)

NAGIBINA., M.S.
Concerning IU.A. Kosygln and 1.7. Luchinskii's article "BaBic
systems and types of tectonic sti-acture -)f the Mesozoic and
Cenozoic continent of Asia." izv. All S,-;SR. Ser. geol. 28
no.11:99-100 N163. (MIRA 17--))

NAGIBINA, M. S.
Structural position of Upper Mesozoic and Cenozoic granitoids
in the Sikhote-Alin' Mesozoic folding. Izv AN SSSR Ser geol
29 no. 5:3-8 My 164. (MIRA 17-5)
1. Geologicheskiy institut AN SSSR, Moskva.

NAGIBINAY M.S.; MIKUNOV, V.F.
Morphology of Mesozoic structures in the southern part of the
Chullman trough. Izv. AN SSSR. Ser. geol. 29 no.11:25-35 N '64.
(MIRA 17:12)
1. Geologicheakiy institut AN SSSR) Moskva.

NAGIBINA, M.S.; POTAPOV, Yu.1.
Tectonics of the Tugura-Nimelena Trough (wes%-rn c,.:*, -7-, 'J-p
region of the Sea of Okhotsk), Trudy GIN no.119. ~Q li-c"
-P.P'.

PA-75T69
NAGIBRIAP N. I.
a
l
A;pr 19W
Urfa
0 Ifffeau
p~p
N. ys. yarygin MA 1. 1. laglb
*Atabrln pAlftr Oblasts Uzbek 80, ii 19
Babest ItsOd"i lop
lbdltdlne IrO
a &0" of atabrin a" collent macinal
Mmapeat cutro] atabrIn &Me*
meow for a reelstame to
systm OAA buUds Up IMOM&I
nsrvMs of atebriubrIng about & can-
It,SOU. Z~M dolef r*gmlt in save"
altion Of U&Mloation =a Oftm
79269

N i, 1
1 -1 1"'k" IN. I.
"Proz,lam of the 'Ptilil-D.
~y ar.-d ?atho~,enesls of :)evere Ca.9f.-a of Eur.)Pean
Typhus Recurrens," Klin. Mod., 26, oo. 6, 1-Ad. L~abkerit hay~)ri
nosol., Bulchar -Llast, 'jzbek 6oR, -lz)4U-.

TI

T. D.
?4br. Inzt. ur,,Tanlc Gne.n'ztry, -ept. ~,i-.em 5cl., Jca!1. -ci.,
"Acetylene Derivatives; -On tKe Isomerization of Tertiary V1nylet,'q1:,yl-
c5rbinol3," Iz. Ak. Nauk 666H, jtdel, r,.him. Nauk, No. 3, 11J40;
"'r-le Derivatives of -cetylene: XXXIII Conversion of' i)1,vinylketo:,es.
Addition of Iydro,7,an 1-hlor"L.-le Lo aeta, Beta-i)iaetliyl~il,/i,,iylkotor-ies,"
ibid. , No. 3, 1943;
"Die:,Ic 'pithesis on tile daS'LS of' Vinylothirty1caruinols," i~,,Id., jio. 1,
1946;
"Dienic byrithesIs based on Divinyl notones, it Ibid.;

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NAGIBINA, I.D.! YASFNKOVA, L.S.; "AS'KC), L.V.; ALIKI-11"'ROVA, -
T
Isoprene and acrylonit'rile ~-Opol)'Lre7s- Kau-'r. I .7~-
no.12z4 D '63. 01-CfA I
IL. Inst--'.ut organi,:~heskoy AN SSSF.

',ii, t. 1 , Li i A I T . D.
C hemi s t ry.
"Rcetylene 'Jerlvutives: XVIII hlec.Iarilsm of tlie 1,dditlon of Jrganic "cils
.1
to Acetylenic ~,arblnols, "Iz. Ak. ilauk `65ri, Ot-Ael. Khim. Nauk, No. 2, 1941

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T. D.
"The Derivatives of Actylene. Part 44. -ianic 6ynthesls nase.-I on
Dlvinyl !I-etones," 1 5, D., Institute of 6r~-Ilanlc ~;tieml~try, Acariemy of
6clences of the USSR.

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