SCIENTIFIC ABSTRACT TATEVOSYAN, G.T. - TATEVOSYANTS, KH.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R001755110016-4
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: July 16, 2001
• Sequence Number: 16
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

TATZVOSTAK, G.T.; GASPARYAH, O.Te.
I
O.Ovwl,~"Ketbyl (sister of 5-c7anomethyl-2-furoic acid. Sint. geterotaikl.
Boad. no. 2:50-52 157. (MIRA 11:7)
(Vuroic acid)

MEHOTIN, A.L.; TATWOSYANw G.T.. . .
-
- .1
2-(2-fuTyl)-1,3,4-Mdiazo-5-thiol. Sint. gaterotsikl. noed.
no. 2:60-63 '57- (Thiols) (MIRA 11:7)

MMHOUN, A.L.; TATIVOSUN, G.T.; DIVAMN. N.M.
Investigating the field of derivatives of m1batituted acetic acids.
Report 16.10: Dialkylaminoethyl asters of r, -alkyloorcaptoethyl-
benzy1mastio acid. Izv. AS Arm. SSR Ser. khtm. neak 10 no.4t267-
276 177- (MIRA, 10:12)
1, Institut tonkoy organicheskoy khimii AN ArmSSR.
(Acetic acid)

MZHOYAN, A. L.; TATXVOSYAN, G. T.; IDMDZHTAN, S. P.
Substituted h7drazides of P-(2-=th7lln-4ol7l-3)-propiouic acid.
Izv. AN Arm. SSR Ser. khim. mauk 10 no.4:291-296 157. (KM 10:12)
1. Institut tonkoy organicheskoy khimii AN ArmSSR.
(Hydrazides) (Propionic acid)

min
I~A~
ndth
p eayj4cetir atida.
,+,rro- ROV
NO
'r-N' 11957 Kin Ru---tv d. CA. SO,
tor 'ii, d A) hcvu 4,1,1
rTw"-) z-nl 0.5 ~g ro. 11 was t,-duxcd " n If-) Lath
zt nj,&~ b: !, (in cise of d. coluratiot of tl;e
ri,tt 1&-15 ad. ad~'upL Br wla5 addi.4) and tLe mixt. he--ted
4 Lis.. k,p-, ,x-cd i-,W hviling U~O. airred,
wv:ti'-rf. dricil,
R A i
I T? 4 C, A"
wl'l It. 'Ju
:75
11'-0 added 'ifo fly and I -I Uci
To bath 15 kzii,
~lla- al Vic ppz., the Cilis Sepil , W250) i -it dil.
11"I avii 1"'0' niuated w"I'l 100 IlA. 20% N-.0it,
I'le i4--, c%td. 'vill EL'a reltov~ impuci!ir S' f~cldj-
-'Ift Hel tk' and tht- "i c~(-f wills Fr,('l
Pt.;
14
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R7S -4
f-t. Pr, 1 4
4)1 F'-
'Ail
41a ~-~M
v4iq ~g4

R", c", 4.P./mm'. do, nlog. 11-t given); Mt, Pr,
MIL-~pliel- IMIXI, 1.44ft", Lie, tu. 92.0,
671 KI ; E, 1r. W 5. 107-
`11) 11. 1, 4
Lt flu
K!'j; q j.11j, I
611, 312. i"
llwjj!~ iti t(YJ nil Ibi, ~.,i k, I cli,i W10 di.lkyl-
1:2 'it ull. af;%. C411%. ticatal 02. (in lito
-ba(h lt;-Ie hrs~ ti'vii ucatzzd 1:60, samd Nla,,CO, stJn., exid.
PhCR'R"-
with INA drkd. and distd. in racu"'Kiyc~
Iq Wei r pd. (R' P I kid, b.p.1mm. dw, rj?, and
MR KivenT Mil. Me,, a'. .5 122-/5, 1.0027, 1.490U, 68.43
HO salt, Tia. 101% InfthiUde. m, MV; 014odide. m.
fr., OX910,
P11-. lfc. fl- 73 () 147'14, O.M3. IAM'L
Me, Efu.
si 4 'j-1 ~':2 X-1 milki-ho, .11 T2* I I
E I- 4hJ3. V ef) i -1tratc, fr*
I-tjj'); rt. Su, 7i) 13. 14ielg, -~d-93
93 (lic]
Far P1iCR'!C;CQvo. iijitNEis. Pr, 9 ti, ow!6,
OMM 1-wsG, Emc. 8a-; cildcoilidt, m.
M- MR. BU 79-4. 183-5,17,
61,6,
If

-
A -
r
I vg~A~

d 1~= 1"
lei
c1 N915. 1 vri-, 10~ 3~- (eigrate, m. fr?') For
%1 73 ~4' 1:nj .4 . 0 ''"CA.
14,
ate[ ~-Ilt' Ta. '(4),-:
ci R".13 (ci!Eatt, m. SO-1. Thc follOwIng Iq1-
12R IRIT019(~1 it), '--lut, me, me, 75.2, 140/4, UjAM.G,
I.thW. 8216 (IlCi ialt. m. f--f5-; m Eg*;
ethiod~l-!, ta. 103'; (Atratc. m, 97'); Nlc~ Ut, 77VA. 151-
1,4940, 861.4~ M CI salt, m. 85% cftratn.m.
100-V); M-, Pr, 73.0. 176--J"/&, 0.9624, 1-4866, OLIFs
frpethiodide, ra- 139'; whiodLar, p, 07'; civrate, m. FZ*);
Ha, W-5. M-8 16. OMU, 1.40W, 95.04 (citmte m
IOG7). Et~ Et. 73.5, 160-2'14, 0,97W,, 1.4912, W166
r_ -3'); it, Vir, S&';, 173-V/5,0.9705,1.4004,
I(P. -r
-Pr, Pr, 91.6, 176-6'/4,
tn. RV);
o-0617" 4.4P&Rr M.95 (dirat i, m, 1170),, Pr, Bu, 78.0,
Ok -24-90, 10-5 .3S-- Ru. BLL 02.1.
'WA, 1 P-3 "i4z'tv te, 11.14).

7P T--A-
HNMHOYAN, A,L#; akaelemik-, T44TIV03YAN. G,T,; AGBALYAN, S.G.; DIVANYAN, N,K.
Research in f;he field of furan derivatives. Report Wo,16. Dokl. AN
Arm. SSR 25 no,4:207-211 157. (KIRA IltZ)
1. Inatitut tonkoy organichemkoy khimii AN ArmSSH.

TATJIVOSYAN, G.T.;JDU=RTAN# B.P#
5-Carlioxy-2-farylacetic said, Sint, geteroteikl. ooed* no*31
4D-42 $58 (XIFA 13:3)
(Furanacetic acid)

IMZHOYAN, A.L.: TATEVOSYAN, G.T.,- TFjIIZTAN. A.G.; MMMAII, S.P.
Indole dnrlvatives. Report 116.2: 2--k-alky~-(~2'sethyl-3'indolrl)I
-stbyl-5-marcapto-1.3.4-diazole. Izv.AN WSR. Khtm.nauki
11 no.2:127-133 158. (MIRA 11:11)
1. Institut tonkoy organichaskoy khImii AN ArmSSR.
(Oxadiazole)

M=HOYAN. A.L.; TATEVOSYAN, G.T., akademik; AGRALYAN, S.G.; RUSHETYAN, A.Y.
Research in the field of derivatives of substituted acetic acids.
Dokl. AN Arm. SSR 27 no.l.-41-47 '58. (Km 11:9)
I.Insbitut tonkoy organicheskoy khimii AN ArmSSR. 2-AN ArmSSR (for
TatevDayan),
(Acetic acid)

MMHDTAN, A.Z., akademik; TATEVOSTANL AGBALTAN. S.G.
Research in the field of derivatives of substituted acetic acids.
Report No.14. Dokle AN Arm. SSR, 27 no.2:93-99 158. CGRA 11:10)
1.1notitut tonkey organichasker khimil AN Armyanskoy SSR.
LAN Arzyanskey SSR (for Mndshoyan).
(Acetic acid)

MNMHDTAN, A.L*;__,TATIVOSYAN, G.T., akademik; AGBALTAN, B.G.; BOSTANMHTAN, R.Kh,
Research in the field of substituted acetic acid derivatives.
Report No. 15: M-dimethyl-?r -dialkylaminoprop7l and tetra-
I
alky,ldiaminoisopropyl asters of dialkylphenvlacetic acids. Dokl.
AN.A-rm. SSR 27 no-3:179-185 '58- (MIRA 11:12)
l.Iristitut t,onko7 orglnichaskoy khimii AN ArmVanskoy SSR.
(Acetic acid)

XNDZHOTAN, A.L.. akademik,- AFRIXTAI, V.G.;- 'a-T-1-AMALrAN, S. G.;
MIGORTAN, X.T.; DIVANTAN, N.M.; BADALTAH, T.Ts.; WLWJTAN, N.A.
-:1 1- . . Iwestljstjon In the field of furan derivatives. Report K0.21.
. Dokf.Al Arm.SSR.27 nP-5005-'314 '513- (MIRA 12:5)
1. Institut tonkoy organichookoy khimil AN ArmSSR. 2. AN ArmSSR
(for Mwilzboyan). (Puran)
I

NEWHOUN, A.L.; TIRZYAN, A.G.; TATIVOSYAN. G.T.
I
13-Insetbrl-5-IndolecarboVIle acid* Sint. goteroteikl. mood.
no.4.-26-30 159. (MMA 13:21)
(Indolecarbo3ylic acid)

XNDZELOYN, Jk.L..; TATZVOSUM, G.T. ; UNANYAN, M.P.
'---ftuwa
IN- ( -indolyl-3-propyl)piperidins. Sint. goterotaikla moods noo4:
42-4~ 159. (MM13tll)
(Indole)

KAJWZHOTAN, A.L.; TIMZTAN, A.G.;.a W,, --G. T.
/4 -Z-jwthyl-3~-lndolyl)proplonlc acid. Sint. geterotmikl. sood.
no.4-.58-60 159. (MIRA 13:1.1) 1
(Indoloproplonio aoid)

MND7,HOrAN. A.L.. akadnmik; TAITXVGrAffi-M,,-.-,AGULTAH, S.G.; BOSTAIMZHW,
R.U.
Study of derivatives of substituted acetic acids. Rewrt No.16:
AmIno est"r" of diphenylalkylacetic acids. Dokl.Aff Arm.SSR 28
no.3.111-26 '159. (MIRA 12:7)
1 - Institut tonkoy organicheakoy khImii AN ArmSSR. 2. AN ArmSSR
(ior i4ndshoyan).
(Acetic acid)

5 (3)
AUTHOR. Tatevosyan G T SOT/74-28-8-6/6
TITLEs Alkaloids of the Ibogaine Group (Alkaloidy gruppy ibogaina)
PERIODICAL: Uspekhi khimiij 1959, Vol 28, Nr 8, pp 990-1010 (USSR)
ABSTRACT: In the present paper the author reports on the discove3.7 and
investigation of ibogaine and its analo as Alkaloids o" the
Tabernathe iboga H. Baill. (Apocynaceaef,which belongj'to the
class of the numerous and ividely disparsed natural alkaloids of
the indole series, were discovered more than half a century ago
(Refs 1, 2, 3). Research workers focussed their attention on them
only when the valuable pharmacological properties of the
principal representative of this group - ibogaine - were
discovered. In the years 1938-1940 an intensive pharmacological
and, later on, chemical investigation of these alkaloids was
started. Although investigations have not been completed by far,
it has at least been possible to establish the structure of the
moat important alkaloids of this group. They differ from the
restof alkaloids of the indole series in their peculiar
combination of the indole ccxv vd1h to bicyclic isochinuclidine
system and the nitrogenous seven-membered ring 13 individual
Card 1/4 bases have so far been separated out of the roots of the iboga

Alkaloids of the lbogaine Group
SOY/74-28-8-6/6
tree. Their main constants are shown in table 1. The structures
of the principal alkaloids of thi6 group (ibogaine, tabernantine
[tabernanthine ? translator's nots)$ ibogamine, and voakangine)
haire been more or less cleared up. There are a few individual
outstanding questions of the steiia configuration of
substituents. Definite concepts have been fixed with reZard to
th(3 structure of bases which are the products of the oxidative
transformation of principal alkaloids (iboluteine, dimethoxy
iboluteine, as well as oxyindolenine derivatives of ibogaine and
ibDgamine). Preliminary structural formulas have been suggested
far ibochine and iboxygains. Gabonine, kisantine, and kimwuline,
which were separated out only recentlyl have not yet been
investigated. They are characterized by their main constants and
some spectral data only. The similarity of the properties of
kimvuline and iboxygaine is striking. Possibly these bases are
identical (Ref 12). The majority of-studies are dealing with the
examination of the most important and most easily accessible
a2kaloia - ibogaine. Herep the formulas astabliBhed by Goutarel
and Taylor are considered in detail. Iboluteinep which was first
obtained by oxidation of ibogaine in a chloroform solution and
Card 2/4 wa.s only later separated out of the roots of the iboga tree

Alkaloids of the Ibogaine Group
SOY/74-28-8-6/6
directly, were examined thorou,,hly by Goutarel and his
collaborators (Ref 16). As to its composition (C 20H2602 N2) it
differs from ibogaine in that it contains one additional oxygen
atoja. Like ibogaine, it contains a methoxyl group*and an active
hyd:rogen atom. In the determination of its structure its
absorption spectra in the ultraviolet and infrared ra-,iges were
particularly valaable. Although it has not been possible as yet
to obtain any of the bases separated out of the roots of the iboga,
tree by complete synthesis, the structures of most alkaloids may
be regarded as established. In the past ton years Robinson
(Ref 38), Woodward (Ref 39) and others have developed hypotheses
aiming at a solution of the problems of the biogenesis of
alkaloids of the indole series. Biogenetio patternsp which were
adopted on the grounds of-these hypotheses, so far are of a very
ger.eral character. According to these hypotheses the principal
bicigenetic sources of alkaloids of the indole series are
try-ptophaneg 3v4-dioxyphenylalanine, and formaldehyde, or
equ;ivalent sub3tances. According to w4ether the condensation of
the dioxyphenylalanine with tryptophane takes place in the
Card 3/4 ot- or 13-position of the indole core, P(rindde (johimbine, reserpine,

Alkaloids of the Ibogaine Group SOY/74-28-8-6/6
a.~maline, etc) or P-indole alkaloids (strychnine# brucine,
aspidospermine, etc) are formed. These concepts of the biogenesis
of alkaloids of the ibogaine group may be confirmed and at the
B.'Me time clarified further by pbyto-physiological investigations
with amino acids containing tagged atoms, as is also the case
with other biogenetical hypotheses. There are 2 tables cnd
40 references, 2 of which are Soviet,
ASSOCIATION% Ia-t tonkoy organicheskoy khimii AN ArmSSR (Institute of Fine
Organic Chemietryt AS Armyanskaya SSR)
Card 4/4

KKDZHOUN, A.L.. akademik; UUTOSM, G.T#; AMMAN. S.G.;
Research in the field of amino others* Report No*2: Syzt-
thesis of 9-dIa1IqrlaminoethvI others of -trisub-
stituted ethyl alcohols, DokI AN Arm.SS)i 29 no.4:187-192
159. (KIRL 13:4)
1, Inutitut tonkoy organichookoV khimil AN ArmSSR. 2. AN A=SM
(for.Ifndshoyan). (Ithanol) (Amines)

KIMOIAX# A.L., akadevik, TATWO.S,W,..G,T,.,,AGMLUT, S.G.
Research an substitution products of acetic acids. Dok1.
A~r Aru.MR 29 n0-5:235-243 159. (KnA 13:6)
1,hotitut tonkoy organIcheskoy kbimil Akademli nau
Armystaskor SSR. kkademlym nauk Armyanskoy SSR, (for
Nnd2hoyan).
(Acetic &old)

1202HOTAN, A.L.,-. TERZYAH, A.G.; AKOPYAN, Zh.G.;c.-TATEVOSYAN, G.T.
Indole derivatives. Report-No.4: Dialky [~-alkyl-Y-(2-weth;rl--i-
indolyl)] propylamines. Izv.AN Arm.SSR khim.nauki 13 no.1:69-75
l6o. (MIRA 13:7)
1, Institut tonkoy organicheskny khimii AN ArmSSR.
(propylamine) (Indole)

TZRZTAS, A.G.; !U RON.- 11
MMRW---
Indole derivatives. Report No. 2 3~-D~methyl-5-aminomethylindoles.
In. All Arm. SSR Khtz. us;*i 13 no*.26:193-200 160.
(KIPA 13:10)
1* Institnt tonkoy organichaskoy khimll AN ArmSSR,
(Indole)

VlrlftXDZffAlf S-Po; TATIVOSTAN, O.To
Derivative no. ~ ort No.2: 3-Kqtho~V4,5-ePoxT-6.7-2',
a Of morp ~
31-Wolo)-N-metbylsorphinan. Izv. AN Arm. SSR Xhim. nautl 13
no.2htva-2o 16o. (MIRA 13dO)
1. lusti-tut tonkov organichookoy khimij AN ArmSSR.
(Norphimn)

'i TATYVCSYAN
TERZYANS A.G.; JXOPYAN, M.G.
Derivatives of indol. Report No.6s 2-M9tbyl-3-propyl-%5-
Iaminomethylindoles. Izv.AN AMAM.Mdm.nauld 14 no-1:71-77 161.
(MMA 15-- 5)
1. Institut tonkoy organicheakoy khlvnii AN Armyanakoy SSR.
(Indol)

TERZYAN, A.G.; SAFRAZBEKYAN, R.R.; SUKASYAN, R.S,; TATMOSYAN, G.T.
Synthesis and some pharmacological properties of cL-methyltryptar-ine
and its 5-methoxy derivatives. Izv.AN Arm.SSR. Khim.nauki 14
no.3:261-271 62.. (MIRA 14:9)
1. Institut tonkoy organicheskoy khimii AN Armyanskoy SSR.
(Indole)

UNANYAN., H.P..-. TATEVOSIANt G.T.
Derivatins if indole. Report No,?.* Sy4tbesis of tertiary
44-(indoly:L-3)-propylamines. lzv.Ali Am$M.Xhim.nauki 14
no.4:387,.391 161a (MIRA 14 10)
1. Institut tonkoy organicheskiy kbimii AN Armyanskoy SSR.
(Indole)

TERZWj A.G.; SAFRA7,BBKM., R.R.; KHAZRAKYAN, L.V.; TATEVOSYM, G.T.
CZ ----- --
DerivwUves of indole. ReWrt No,8.* Producto of rutaocarpine
reduction with litblum alumin= hydride. Izv.AN Am.SSR.rhim.
nauki 14 no-4:393-399 161. OWA 14110)
lo Inatitut tonkoy arganicheakoy khimii AN Armyanskoy SSR.
(Indole)

XKHITARYAN, A.V.; KOGODOVSKAYAO A.A.; TERZYAN, A.G.1 IATEVOSUll, G.T.
Derivatives of indole. Report No.9:OCA -Dimethyltryptamine
and its 5-methoxy derivatives. Izv.AN Am. SSR. Khim.nauki
-15 nc).'4:379-384 162. (MIRA 15:13.)
1. Institut tonkoy o~ganicheskoy 'khim4i AN Armyanskoy
SSR.
(Indole)

TERZTAN, A.G.; TATEVOSYAN,_G.T. . -
I
Derivatives of indole. Report No. 5s 5-Acetyl- CC -methyl-
tr7ptamlne. Izv.AN Arm.SSR.Khim.nauki 15 no.6t563-566 162.
(MIRA 16:2)
1. Inst:Lt#t tonkoy organicheskoy khimii AN Armyanskoy SSR.
(Tryptamine)

TERZYAN, A.G. AKOPYAN, M.G.; TATLVWYAN, G.T.
Derivatives of indole. Report Nollt P-Garbolines and their
tetrah7droxy derivatives methylated lh the pyridine ring.
Izv, AN Arm.SSR. Khim. nauki 16 noolt87-92 163 (MIRA 17:8)
1. Institut tankay organicheskoy khimii AN Armyanskoy SSR.

KHAZHAKYAN, L.V.; WMITARTAN, A.V.; GIRTvTY"Y, G.L.; TATET-3YAN, G.T.
Derivatives of indole. Report No.12: Structure of benzylide4armine
and somie of its derivatives. Tzv. AN Am.SSR.Khim' nauki 16 no*2:
181-189 163 NIRA 17:8)
1, Institut tonkoy organicheskoy khImli AN ArmSSR.

TERUO, A.G; KOGODOVSKAYA, A.A.; TATFVOSYAN, G.T.
-'--
Deriva-,ives of indole. Part 131 10-Carbomethoxy mt~eecarpine.
Izv. All Arm.SSR.Kbim.nauki 17 no, 21230-234 164.
(KRA 17s6)
I
1. InsUtut tonkoy organichaskoy khimii AN Armyanskoy SSR.
4

TATEVOSYMI, G.T.; TEIRZYAN, A.G.; EKWKDZHYAN, S.P.
Substittted hydrazides of,6 - (2-me thy 1-1, -c Rrboxy-3-quinolyl) -
propionic acid. Izv.AN Arm.SSR.Khim.nauki 17 no. 2t235-237
164. (141RA 17i6)
1. InstLtut tonkoy organicheskoy khimll AN Armyanskoy SSR.

TERZYAN, A.C.; AZNAURYAN, N.V.; TATEEVOSYAN, G.T.
Ir 'bile derivatives. Part 15-- Synthesis of c~-met~,Yl and
/-P. -dir-th7l-5-carboxytriptamlneB, Izv. AN Am.SSR, Kbim.nauki
Lcs uo*1-88-91 t65. (MRA 18- 5)
1. Institut tonkoy organicheskoy khimii AN Armyanskoy SSR.

TERMAN, A.G.; TATUCOYAN, G.T.
Synthei5l's of P-carbolines. 47zv.A!i 18
no-4:424-1.25 165. ("l.:IA
1. Institut ton~kwy organic 1,.e skoy khimil. iN j~j-,TjslR. .9,111111itted
Kirch 10, 1965*

fUSHIPLAN, L.G.,; TATUTAAN, G,T.
St'r-r-3c:Lcomeric 1y, actj,.re f, It Cert-s~ r
vnnv-,~~rs!jcris of rl.!S-4'
R Mr, m . nn-i,, 8 , n o.,, 3?9-3 P.3
IZV. 1.
( rcA 18 . I.!
1. Distlfiit tonkcrj khimii AR t,tod
.July 15~v 1964.

TATEVOSTAN,_a.,'C.;,,TERZYAN, A.G.; MELIKYAN, M.O.
Mechanism of the reaction of sulfuric acid hydrolysis of
vinyl-type chlorides. Izv. AN Arm. SSR. Xhim. nauki 18 no.3t
282-299 165. ()URA 18:11)
1. Institut tonkoy organicheskoy khimli A AroWanakoy SSR.
Submitted April 27,, 1964.

ACC NRi AP6032973 SOURCE CODE:- -UR/0426~/-6-6-/-019-/008/0636/0631
AUTHOR: Boyakhchyan, A. P.; Rashidyan, Le G&; Tatevosyan,.G, T.
ORG: Institute of FLne Organic Chemistryq All ArmSSR (Inatitut tcnkoy
organicheskoy khimii AN ArmSSR)
TITLEt Chloroheptenone reactions
SOURCEt Armyanskiy khimichaskiy zhurnal, v. 19, no. 8, 1966, 636-637
TOPIC TAGS: chloroheptenone derivative, methylclilorocrotylindole,
AB9TRACT; The reaction of 6-chloro-5-hepte.n-2-one (1) with phenylhy-
drazine hydrochloride, on boiling 'in benzend-* .solution in the presence
of sulfuric acid,.y1elded (40%) 2-methyl-3(Y-chlorocrotyl)indole (11),
mp 57-58*C. The r(aaction of I with 5-mathy Ilisatin, on boiling in the
presence of KOH in -in alcohol, yielded (71%) 2,6-dimethyl-3-(Y-chloro-
crotyl)-4-quinoline,:arboxylic acid (111), mp 124-128*C. III was de-
hydrochlorinated by boiling with.KOH in methanol to form compound IV
(mp 158-160*C):
C: 547,384+547.752+547.831

COSH
CCI
.00 C"
H
CH,cc1.r-HclizCH;r~,OCH,- lit
COiH
-CH'mCHdH,~0H0:'
CH
-7CH,,dk-CCICH3 CHS
-CHs
H' IV
501
SUBM DATE: 23ju165/ ORIG REFt 001
SUB CODE: 07
2/2

r" I
t"M
.1 S -VWYA6j_A",,,, JnZh.; V%NVEELYAN, M.G., akadernik; MELI K-AKHNAZAR YAN,
kand, tekan. nauk
lnvestigating the volatUization of fluorine during the manufacture
of opal glass. Stek. i ker. 22 no.M10-12 Ag t65. (14IRA 18:9)
1. Yerevanskiy mauchno-issledovatel'skly institut khim-ii- Gosudarstven-
nogo komiteta khimicheskoy prom:r-1,'-,nnost1 pri Gosplane SSSR.
2. Akademiya nauk Armyanskoy SSF for Manvelyan).

mwxum, K. G. I 'jWjK-AKMWAjj,.* ,Y.; KOSTAWAN, K~A--, N&WHADY.MNq
S.O.; YBUONTAX,
Melting: borosilicate, glass in vertical electric furnaces.
Stek.i ker. 17 no.2:5-9 F. 160. (MM 1316)
(Glass M=f&cture)

ICLIK-AKMZARY,W, A.; RIUSTAHBEKW, S.; TATEVUSUMp K.
Operation of molyWen= a~d graphite electrodes in an
electric glass furnace. Prom.Arm. 4 no.6:57-60 Ja 161.
(MIRA 14:8)
1. Hauaboo-issledovatellskiy institut kbbdi Sovnarkhoza
Armyanskoy SSR,
(Glass furnices) (Electrodes)

XAMLYaj M.; IIELIK-AKHNAZABYAN, A.; RUSTAMEKW, S.; KCSTANYAN, K.;
TATEVOSUNP K.
Studying the processes of bottle glass malting in electric glass
furnacen vith Lusavan perlite+s bass. Prom.Am. 5 no.3-039-42
Mr 162, OURA 15:4)
1. NIIKhimii Sovnarkhoza Armywwkoy SSR.
(Armenia-Perlite (Mineral)) (Glass manufacture)

ACC NR, AP6027260 SOURCE CODE: UR/0072/6G/000/006/0006/0009
AUTHOR: Tateirosyan, K. 11L (Engineer); Manvelyan, M. G. (Academician AN AmSSR);
Avsharova7S_._r."r1 ~~gneer)
ORG: Yerevan Scientific Research Institute of Chemistry (Yerevanskiy nauchno-issle-
!dovatellskiy institut khimii)
I I
TITIZ: Volatization of boric anhydride during the founding of glasses
SOURCE; Steklo i keramika, no. 6, 1956, 6-9
C TAGS: borate glass, glass property, nonstructural mineral product
!ABSTRACT: Volatization of boric anhydride from alkali-free glass "E" 01203 introduc-
Id either as alumina ca:-*.cined at 12000C or as clay) and from alkaline glass type ZS-5Na
iwas studied in 0-14000C and 0-45 hr of heat treatment. All glass s&nples contained ap--.
,proximately 10 wt % B203. The samples were heated to the desired temperature at 5OC/
i/min. The results are graphed and tabulated. It was found that volatization of B2,03
1from alkali-free glasses is completed at 5000C for samples prepared with calcined alu- 1;
Imina and is completed at 9000C for samples prepared with clay. It was also found that,!-
las a result of thermal treatment of alkali-free glasses, the B203 transfoins into cal-
icium and magnesium borates which are practically nonvolatile above 1000-12000C. The
!greater volatility Of 1203 in the alkaline- glasses is explained in terms of formation
UDC: 666.1.031.13:66.046.594

ACC NRs AP6027260
of alkaline borates. The relative evaporation Of B203 from alkaline-free glasses was:
2% for samples based on alumina and 6% for samples based on clay. For ZS-5Na alkaline
glass, only 2% B203 evalwrated*below 8000C but then the B203 evaporation increased
sharply to reach 10% at 14000C. Orig. art. has: 4 figures, 1 table.
SUB CODEt 07911/ SUBM D&TE: none/ ORIG REF: 012/ OTH REF: 002
Card 2/2

49-58-5-8/15
AUTHOR: Tatevosyan, L. K.
TIILE: Some Peculiarities of Deep-Level Structure of the Earth's
Crust in Azerbaydzhan from Gravimetric Data (Nekotox-yye
osobennosti. glubinnogo stroyeniya zemnoy kory v Azerbaydzhane
po dannym gravimetrii)
PERIODICAL: Izvestiya Akademii Nauk SSSR, Seriya Geofizicheskaya,
19581 Nr 5t pp 643-647 (USSR)
ABSTRACT: The deep structure of the Earth's crust has considerable
significance in the study of the crust's evolution and in
the formation of mineral beds. This structure can be invest-
igated by geophysical methods to a depth of tens of kilometres.
As an example,of the results obtainable, the author has chosen
to apply gravimetric results obtained in Azerbaydzhan. Most
of Azerbaydzhan has been surveyed gravimetrically - most of it
in detail. The basic material is that of Buge (Ref.1) rwhich
was recently revised by the All-Union Scientific Research
'Vsesoyuzny
Institute for Geophysical Methods of Prospecting 1.
nauchno-issledovatellsky institut geofizicheskikh metodov raz-
vedki) under the leadership of N. B. Sazhinayaland also data
on density.characteristies Of rocks in the region. Scientific
Card 1/10

49-58-5-8/15
Some Peculiarities of Deep-Level Structure of the Earth's Crust i.--
Azerbaydzhan from Gravimetric Data.
literature gives detailed accounts of different forms of re-
ductions in the solution of geological problems (Refs.2,3).
The one! chosen is due to Bu e and assumes a constant 3density
.in the intermediate layers Naken equal to 2.3 gm/cM for
Azerbaydzhan). Gravimetric charts indicate zones of large
horizontal gradients of gravity anomaly. These appear to be
the following: the Talysh-Vandam`~'_ zone,(30-40 est), the
Nukha-Zakatall.,_-.~_ zone (25-40 est), the Kirovabad *.. zone
(25-40 est) and the Apsheron, Peninsula (25 est). The
general distribution of gravitational anomalies in zones of
increased horizontal gradient corresponds approximately to
the case of random gravitational jumps. This permits the
use of formulesderived by Iyustikh (Ref.4) and Fisher (Ref,5)
to determine the maximum depth and magnitude of the body
concerned. Referring to Fig.1, T is the distance, verti-
cally, between the top and bottom of the body, and h is
the dist~Lnce of the top of the body from the Earth's sur-
face, so that H ~ T +-h . The author takes limiting val-
ues,for the total height and the depth below the surface of
the two layers, according to the gravimetric data. The
Card 2/1(:pxcess density of the lower layer mr the upper is denoted

49-58-5-8/15
Some Peculiarities of Deep-Level Structure of the Earth's Crust in
Azerbaydzhan from Gravimetric Data.
by Acr(;> 0) . Consider a layer of thic!mess dz at a
depth z 4 The effect of this on the vertical component
of the force at P(~, Ili 0) is:
A g = k b Or 2 z dx U dz 2]
~~~ P +- (X-V +- (Y 3/2
The maximum effect at P is obtained from a layer defined
by the planes z = h and z =--H :
6L gma. =-- 2WAcr (H - h)
If Agmax ,-,Ag the observed maximum anomaly then Eq.(2)
results. The author differentiates Eq.(l) and substitutes
X1 =X - t I Y' =-y - T11 , giving Eq.(3). The greatest
positive value is obtained if all elements are included for
which the integration is positive. With a positive xI ,
a stepped structure is obtained which is defined by x' - 0,
Card 3/10

49-58-5-8/15
Some Peculia-rities of Deep-Level Structure of the Earth's Crust in
Azerbaydzhan from Gravimetric Data.
y stretches to +- CO and the height is equal to H - h
Integrating Eq.(37 for the first horizontal derivatives of
the vertical gravitational anomaly gives Eq.(4). E.N.Lustig
(Ref.4) gives the formula (5) for the depth of the anomalous
body below the surface. A. G. Salikhov wrote this in the
form Eq.(6), where Ag is the difference between the maximum
and ininimum values of the gravity anomaly; g' is the maximmn
value of the first horizontal derivatives of the anomaly; Aa
is the difference in density of the masses and k is the
gravitational constant. It should be noticed that Eq.(6)
give!3 the upper limit to the possible depth below the surface
of the top point of the body. Hence, it is important to know
the geological and seismological data relevant to the problem
so aa to control the result obtained. To determine the de.)th
of the body, a region is taken where the intensity of the
anomalous field variation is known sufficiently accurately.
The profiles are ex-bended perpendicular to the isolines and
continued in both directions so that they intersect tile
greatest and smallest values of the gravitational anomaly.
The difference of these two values gives j4g . The magni-
Card 4/,Vde of g' can be determined, firstly, by Stirling's

49-58-5-8/15
Some Peculiarities of Deep-Tievel Structure of the Earth's CruBt in
Azerba,vdzhan from Gravimetric Data.
formula and secondly, by division of the difference of
gravitational anomaly values in a given interval. Several
profiles were used to determine gI by both methods and as
the results were found to be the same, the latter method was
chose.-a.as being the Bimpler. For convenience the denominator
of E.I.(6) was calculated for various values of gI and put
in ta:ale. To determine Aa it is necessary to consider what
minerals exist in the region, what densities they have, if
the density boundaries are well-defined and at what strati-
graphical level they are situated. A. 0. Martirosovi and
E. 0. Prozorovich have produced reports on the density cross-
sections in relation to the stratigraphy, etc., for almost all
regioas of Azerbaydzhan. These show that there are Tertiary
types of deposit in Azerbaydzhan - clay, marl and sandstone
and its co4glomerates, with average densities of 2.2 2.3 and
2.37 13m/cm2, giving an approximate average of 2.3. 6udden
changes of density do not seem to occur in these deposits -
as 1. 0. TsimmelIzon, V. I. Rudelev and D. L. Tereshko have
noticed. Rocks like limestone are of high density - in the
Card 5/10

49-58-5-8/15
Some Peculiarities of DeeD-Level Structure of the Earth's Crust in
Azerbaydzhan from Gravimeiric Data.
Terter and Karkarchay region - 2.61 gm/cm.? 3and in the Shcunkhor-
Kirovabad-Agdamsk-*. regions ^.,2.5-2.7 93n/cm . The author calls
these the 'volcanic complex' as opposed to the 'granite com-
plex'. B. K. Balavadze (Ref.6) determined 3the density of
the granites in the Caucasus as 2.65 gm/cm . Thus the first
type of' density b9undary is that 3between rocks of average
density 2.3 gm/cm2 and 2 6 gm/cm . The granite complex lics
on the basalt layer (Ref:7), the density of the latter being
2.85-2..9 gm/cm2 (G. A. Gamburtsev-' and P. S. Veytsman, Ref.8).
Thus there is a second type of density boundary here. (The
third type occurs between thebasalt layer and the under-
lying layer at the Mohbrovitie discontinuity). To determine
the depth of these boundaries 46 profiles were used. From
Eqs.(6.) and (2) the required depth can be determined. The
resUlt13 indicate that in the area of increased gradients on
the Api3heronski7 peninsular, the upper boundary, h - 8 km
the lower, H -12 km. In the South-West part of Talysh the
upper boundary lies at 4.5 km and the lower at 10 km. To
the East of Talysh (towards the Kurinsk-*.7- depression) the
depth Increases - 9.5 km for the upper and 20.6 for the
Card 6/lc~ower '3oundary. In the Nukha region, the upper limit of the

49-58-5-8/15
Some Peculiarities of Deep-Level structure of the Earth's Crust in
Azerbaydzhan from Gravimetric Data.
anomaly is at 3-3.5 km (connected, obviously, with the Nukha-
Zakataly gravitational maximum), whilet from Gookchaya to
Yem-lakh-Agdzhabedam. the lower boundary is again at some depth
(17-19 km). 1. 0. TsimmelIzon, working on thele.vlakh-
Agdzha:be-dam;.----,- minimum, showed that the maximum effect was
placed at 8000 m. and that regional fields depended on a deep-
lying factor, which the author places between upper and lower
limits of 8 km and 18 km. The fullest interpretation could
be given data obtained on the profile of Talysh-Apsheron
penlnwula- (Fig.2) which has a very clearly defined anomaly.
Generally speaking, the change of Ag corresponds to a
dipping of the disturbing surface in the directiom from
Talysh to the peninsula. Along the profile the anomaly
changes by 250 mgl. The first density boundary can be de-
termined,by the fact that it lies between the Tertiary de-
posits and the chalk, and that the chalk boundary can be
determined from geological data (at a depth of 2.4-2.6 km)
(Ref.9). Palaeological data (Ref.10) can also be used -
giving near the peninsula a depth of 9 km. This data
Card 7/1b

49-58-5-8/15
Some Peculiarities of Deep-Level Structure of the Earth's Crust i..:
Azerbaydzhan from Gravimetric Data.
enables the first dividin6 surface to be drawn the equival-
ent anomaly being 80 mg1 (curve Ag, in Fig.25. This
curve, however, does not fully explain the measurements.
Another, secondBurface can be drawn. This has a minimum
depth below the surface of 4.5 km below Talysh dropping in
two steps towards the East. This surface gives a gravitat-
ional anomaly of 208 mgl (curve agjj in Fig.2). Since
this surface is too deep for the first density boundary, it
must represent the basalt layer boundary. The total effect
of the two surfaces together is 288 mgl, whereas th,_ observed
results give 250 mgl. Although part of this is explicable
as errors in the theory, some of it is probably due to va-ria-
lion in the depth of the Mohorovitfi6 discontinuity. In the
foothills of Talysh, there is (according to D. L. Tereshko)
an intense, positive magnetic anomaly and there also appears
a gravitational maximum - thus showing the presence of a bed
of considerable density and high magnetic susceptibility at
no grE)at depth. On the other hand the Apsheron_'.... Sravi-
tational minimum coincides with a low) negative magnetic
Card 8/1&nomaly indicating light sedimentary strata.

49-58-5-8/15
Some Peculiarities of Deep-L-evel Structure of the Earth's Crust in
Azerbaydzhan from Gravimetric Data.
ConcIUSions
1T -In Azerbaydzhan as in other synclinal regions, there are
three *oasic densiVy boundaries:3between the mesozoic (2.6 g/
cm3) and th5 cenozoic (2.3 9/cm ) with a density difference
9f 0.3 9/9m , between the so-called Igranitq complex'
(2.6 g/cm ) and the bagalt layer (2 .9 gm/cm2) also with a
difference of 9.3 g/cm~', and between thq basalt layer and 3
the Moharovieic discontinuity (3.3 9/cm') a a = 0.4 g/cm
2) Maximum gravitational anomaly in the Talysh region occurs
where bhere is a dense granite complex with little sedimen-
tary rock and the basalt layer is only 4.5-5 km below the
surface. 3) The Apsheron~_#**., minimum is a result of a deep
depression of the dense crystalline rocks and the presence
of sedimentary rocks. 4 The observed curve of Ag (along
the profile Talysh-Apsheron.-,.:_.-I,: peninsula) gives a method
of determining the depth of the basalt layer surface.
Card 9/10

L~9-56-5-8115
Some Peculiarities of Deep-Level Structure of the Earth's Crust in
Azerbaydzhan from Gravimetric. Data.
5) The effect of the Mohorovieic" discontinuity, although
apparent is only secondary compared with the layers above
it. Th;~e are 2 figures and 10 references, 9 of which are
Soviet and 1 English.
ASSOCIATION: Moskovskiy gosudarstvennyy universitet im. M. V.
Lomonosova (Moscow State University, im. M. V. Lomonosov)
SUBMITTED: JulY 5, 1957.
1. Geophysical prospecting--USSR 2. Gravity--Measurement
Card 10/10

- -- --- - -- -
TATIVOSYAN, L.K.
Use of detailed gravimetric surveying in studyIng the structure
of deep-seated parts of the earth's crust in Armenia. Dokl. AN
Arm. SSr 26 no.4:~29-234 158. (KIRA 11:5)
l.Geologichaskiy fakulltet Moskovskogo gosudarstvannogo universiteta.
Predetavleno A.A* Gabriyelyanom.
(Armenia--Geology, Structural)
(Gravity)

POPOV, I.V., Icand.okon.nuuk; RASKHODCHIKOV. V.I.; TATMOSTAll, L.K.,
In2h. -7- __ __ ---I--
Rarleif of power englneerln4g ln the Germn Deamratic R,07mblic.
Rnorgokhoz.za rub. no.1:1-5 is-? 160. (14IRL 13:5)
(Germarq, Eaot--Power eDgineeriug)
v

TATEVOSYAN,, L.K.
Petroleum industry and petroleum refining in the German Federal
Republic. Khimo i tekh. topl. i masel 6 no. 5:66-71 My 16-1.
(MIRA 14: 5)
(Germany,, West-Petroleum industry)

S/169/62/000/009/002/120
D228/D307
AUTHORs Tate*;r
TITLE: Some.features of the abyssal crustal structure in the
Caucadus region.according to graviL,;etric data
PERIODICAL: Referativnyy zhurnal, Geofizika# no. 9, 1962t 7, ab-
stract 9A23 (Izv-. AN ArmSSR, Geol i geogr, n., 14,
no. 5, 1961, 31-42 ('Summary in Ar;.))
TEXT: An attempt is made to relate gravity.aromalies to the depth
structure and tectonic zones of the Caucasus. The Bouguer reduc-
tion gravity map was )averaged according to the Method of Tikhanov-
Bulanzhe (Boulanger? in order to eliminate local anomalies. The
Mohorovicio surface's depth was calculated from T'suboils methbd,
.the mean depth being taken as'equal to 50 km, and the density of
.the crust and suberustal matter as 2.9 and 3.3 g/cm3 respectively.
It is noted that the depths found coincide well with the data of
seismology and deep seismic sounding. A map of the effective crus-
--tal thicknesses is given. It is pointed out -that the depths ob-
Card 1/2

S/169/62,/000/009/002/120
Some features of the D228/D30-1
tained for'the Hohorovicic surface have to be corrected in section as
where light sedimentary or acid volcanic rocks are widely deve'lopedf
and in regions, where basic intrusions have been emplaced. The
author notes that the peculiarities of the crust's structure are
in accordaAce with the tectonics of the Caucasus. Z-Abstiacter's
notes Complete traneilation._,7
Card 2/2

hTEVOSTANt L.K.
Poosibility of introducing the metric
in Great Britain# Standartizataiia 25
.(Great Britain-Metrio
eyotem of measures and-%Wghta
zo#3s59-61 Nj~*.(KIRA U:3)
eyetem)

TATEVOSY&N,- L.K.
Basie-sti-n-dardization organizations in Poland. Standartizatsila
25 no.ICI:59-60 0 161. , (MIRA 14:9)
W61and-Standardization)

TATIKVOSYAN, L.K.
Developmfmt of the oil indust~ in the Genman Namocrati-- ReVAIL:.
Khim. i -tekb. topl. i masel 7 no.10t68-70 00&2 (FIIRA hlt?)

ARSKIY, A.K.; GALIPERIN, V.M., red.; TATEVOSYAP, L.K., red.;
BORUNOV, N.I., tekhn. red.
[Natural gas and power engineering in the U.S.A.) Pri-
rodnyi gaz v energetiXe SShA. Moskva, Gosenergoizdat, 1963.
207 p. (MIRA 17:1)

TATEVOSYANO L.K.
Petroleum ind"tr7 Of the Hungarian People's Republic. rhim.
i tekb. topl. i maBel 8 no.4:69-71 Ap 163. (MM 16t6)
(Hungary~Petroleum industry)

j
'J'APAFOS"i'All, N, -.; E.K.
!'()Lh 1,11 lt 0 1 A
Gaw,re bo.o.,,:ks w-ith nitritod slirfeens. 1%n. tokh. nr,.1:2? ja '~,5.
(MIRA 18W

USS21 Electronics - R&dio equipment
Card 1/1 Pub. 89 - 12/,z0
Authors t Filichkin, G., and Tatevosyan, S&
Title I Exchange.of experience (radio sets)
0ekodidaV---t- ladio~-3,- page- 21,-_ Mar- 1955
Abstract- - U account is -given of steps taken by a. user- (if the "Baltikall- radio
receiver to improve the quality of.the sound. It io also related
------- _--howsvccess -was- attained-in-rgduoing-interfert!nc -e__ in the "Rekord",
."ARZ11vand "Moskvichl' -receiving sets.
Institution-V
Submitted

27716. TATEVOSYANO' S. YA. --Zaahchita sinkhronnykh roishin ot v7padenlyn iz
sinkhronnoy raboty. -- v og1t S. V Tstsvoopn. Doklody (Aked nauk am. MR),
T. Xo No. 4, 1949, S. :157-59.- Rezy=e Ila Am. Yez. KOTLYAPMO, N. F.
Iooledovaniya magnitnoy sistwy kombinirovannykh role postoyannogo tpla/- Sm. 27871
TYRIN~ V. L. Raschet chisla priborov na stantsiyakh avtomaticheskoy dallney
ovyazi i metody uvelielieniya ispollzovaniya avtomatizirovaimykh kanalov - SM. 27878.
SO: Letopial Zhurnallnykh Statey, Vol 37, 1949

.I--TITMOSTAN, B.Ta.
bok"Aww'"O
Prereating synchronous motors from falling out of stop. Dokl.
AN Arm.SSR 10 no.4:157-159 149. (MM 9: 10)
l.LabDratorlyn elektrotekhniki AkAdemil nauk Armynnskoy SSR,
Yerew.w. Predstavleno A.G.losiftyanom.
(Blectric motors, Alternating current)

1rPaMVOSYAN,- arid YOTiJG!;44j ~- -.j
"Problem of the Effect of Chemical Contamination on the Electrical Character-1--tIcs-
of Certain T~Tjcs of Suzpension Insulators," p 41g.
I
High Voltage Techni- ue Muncov, Gooenargolzdet, 1W, 664pp
(Series. ITS
NO. 195)
ThIs collection of articlos eumo up the principal results of Investigations
end studies izede by Prof. A. A. Gorev, Dr. Tech. Bal., and his staff in the
field of h1dh voltage phenomena and tacbniquab at LPI (lauLngrad Polyt4Wh In3t.)
It was at this instutute that Prof. Govev completed his higher scientific
education ani then taught and carried an his investigations in the field
until hia death in 1953. In 1956, by decree of Min of Higher Education,
the HIgh-Voltage lab. at LPI was named after A. A Gorev.

TATEVOSTAIT, S.Ta..: TOROSYAN, A.S.
, "
net o-.! accumulated dirt on thm electric chnracterintice of
certaln onapmn-sinn Insulatnre. Trudy LPI no.195:419-424 158.
(14IRA 11:10)
(Mactric insulators and insulation)

TATIVOSUN. S.Ta., inzhener.
- --I
r-
SWkcn,er voltages of insulators and rod gaps at high altitudes.
IlektrLchestvo no.1:86-88 Ja '56. (XLHA 9:3)
(Blectric insulators and insulation)

TAT9VO3YAN, S. Ya.
TATEVOSUN, S. Ya. - *The Effect of Reduced Air Density on the Volt-
Second Charact,.-risties of Porcelain Insulators.0 Min Higher Education
USSR. Leningrad Polytechnic Inst imeni H. 1. Kalinin. (Dissertation
for the Degree of Candidate of Technical Sciences.)
SO: KniZhno-va letopis', No. 4. Moscow. 1956

KIRZOUN, S.A.; - -- TILL.-M., - AKLUADTAN. TS.A.
The active principles and some aspects of the pharmacological
effect of plantain (Plantago major). Nauch.trudy Inst.fiziol.
AN Aru.SSR. 1:145-152 148. (MBA 9:8)
(PLUMIN) (ALULOIM--PHYSIMWICLL XffWT)

1. -
Mrzo-yane So A., Tatevos;~an, T. S. and Amirzadyan, Ts. A. "On the activating; and
certain aspects of the pharmacological action of the great plantain", Nauch. trucv-
(Akad. nauk Am. SSR,, In-t fiziolo.rrii), 12 1948, (running title: 19417)p p. 11+5-152f
(Resume in Amenian) , - Bibliog: 9 items,
SO: U-3261; 10 April 53 (Letopis 'Zhurnal Irrikh Statey No, 11, 1949)

MIRZOYAN, S.A., TATWOSYAW, T.S.
Pharvtacolog7 of poly prepprationa. Farm. i toks. 21 nc,,5128-33
S-0 158 (nna nai)
1' I~afadra farmakologii (sav. prof. 8.A. Hirzoyan) Yerevnnskogo
m:ditsinskogo institutao'
(PLANTS#
Teucrium pollumo phoroacol (Bus))

TATZVOSW, T.Sh.
;I -
~11~-*--111.-.- '11?141".-~
Fossil hail in andesites of the Ara Hills In the Armenian S.S.R.
Izv.AN Arm.SM.3st.nauki no.8:45-51 147. (KLRL 9:8)
1. Institut geologicheskikh nauk AN Aruyanskoy SM.
(Armeniaw.-Andesites)

TATIVOSWp T*;Ma.
- - -- NJ*
Pstrologr of eruptive rocks of the Krasnosellsk District in the
Armenian B.G.R. Isv,AN Ara.M.Ser.FM nauk 4 no.6:467-479 151.
(au 918)
1. Inatiltut cooladebaskikh nauk AN Arwqmokoy M.
(Irasnosellsk District (Arammia)-locks, Igneous)

VARUNTAM, L.A.; TATIVOSTAN. T.Sh., o'tvetstvenW redaktor:
TURTAN, M.A., tekhnicheakikh redaktor.
0
(Complex plagioclase twin crystals; with 68 illustrations) Kompleks-
nye dvointcl plagioklaza; s 68 figurami. Irevan, Isd-vo Akademii
nauk Armianskoi SSR, 1952. 78 p. illus. (Microfilm] (KLRA 7:10)
1. Chlon-korrespondent Akademil nauk Armyanskoy 631 (for Vardanyacts).
(791depar) (Crystallography)

TATIVOSTAII 11-Sh-b.
Patrograpiq of Tertiary effusive formations on the northern slopes of
the BargachjLt Range in the Armaxian S.S.R. Izv.AN Arm.SSR.Ser. 8
it
jw,6:47-5r N-D 035 ~ (MLRA 9: 7)
1.Yerevamilkir gesudaretvasM uaiversitet imeni T.M.Nelsteva.
(Salvard Valler-Petrology)

TA!PZ70SYAN T.Sh.
N--=..wm- w
Gabbro from the northern slope of the Bargushatskiy Range.
Naucb.trudy Itrev.un. 52:43-62 155. (KLRA 9:9)
1. Kafedru, mineralogil I petrografii.
(Bargusbatekly Rame-Gabbro)

2mm

VARDANTANTS, Levon Arsonovich;,TAMPSMp T.5-h., otv.red.; SHTIMM,
R.A., re.f.ixd-va; XAPLANTAN, N.A., takhn.red,
ETheory of Pedorov's mthod] Teoriia fedoravokogo mtoda,
Arevano Izd-vo Akad.nouk Armienekoi SSR, 1959. 191 P.
(KIRA 13:6)
(Crystallography)

TATEVOSTAN, T.Sh.
Petrography of basic and ultrabasto rocks of Aramazd, Mountain.
Izv. AN Irm. SWL Geol. i geog. nauki 13 no-3/4:19-32 160.
(MIRA 13:9)
1. Terevaaakiy gosuda stvennyy universitet.
(Aramazd Mountaimp-Pletrology)

(~TA~TZVOSY~", T~.S.
Gonditiow governing the formation of allcali eyenites in the
Bargushat Ridge (Armenian S.S.R.). Izv. Ali Arm. SSR. Geol. i
geog. aaulct 13 no. 5:15-26 160. (KIRA 13;32)
1. Yerevanskiy gosudarstvennyy universitet.
(Bargulshat Ridge--Syenites)

TATEVC23YAN, V-fi-
. , -),,t -grtnateo
", 1(~P, tjbe-3 r~f, tj:f~ I%c;:7.-
Polaen vi.'%,I.ily arid ratite of
11 n IC/0
. ~IF no ~' 9- '.. I- -
Ivr. AN Arzt. So:R,. Biol -,jjl~i 17 .- 40 WIP-4 18:8)
1, Yeremanskly gosudarstvenriyy uril _ver,-lt-9t, kafedra darvinisim I
genetild.

GITSEW, S.M,; SNIMV, N.V.; K&KAROVA, T.P.; PAMIMIN, K-Ye.;
Adoption. of a contimwus unit for the mercerization of cellu-
lose* Ihim.volok. no.3:51-55 160~ (KOU 1397)
1. Lenivgradskiy zavod takasetvennogo volokna I Vassoyusnyy
nauchno-imeledovatellak1y institut iskusetyemogo volokza.
(Leningrad-Callulose) (Hercerization)

TATEVCSYAN, Ye.Le; 14LKAROVA, T.P.; NEGS., A.I.
Method for determining the opti-im time for the Afiltration of
caustic soda with alkali cellulose. Khim.volok. no.5:31-34
161. (14IU 14: 1G)
1. LeUngradakiy filial Vsesoyuznogo nauchno-isaledovatellskogo
instit;uta iskasstvennogo volokna (for Tatevosyan, Makarova).
2. Lerdngradakiy tekstilInyy institut, imeni S.M.Kirova (for Meos).
(Filters and filtration) (Cellulose) (69dium hydroxide)

TATEVOSYAN Ye,L.; PEREFELKMp X.Ye.
Fractional composition of cellulose of various brands according
to the length of fibers. Xhim.volok A0,4130-33 162. (KERA 15:8)
1. LmAngradskiy filial Ysesoyu=ogo nauchno-isoledavateliskogo
instituta iskusotvennogo volokhna.
(cellulose)

T L.; MAKAROVA, T.P.1 190S, A.I.
ATLYOi" YO.,
9ffect of the conditions of mercerization and of cellulose
quality on filterabiLity during continuous merceri2ation.
Khim.volok. no.100-33 163. . (MIRA 16:2)
1. Leningradskiy filial VovBoyuznogo nauchno-inaledovateltakogo
Instituta iskusetvennogo-volakna (for Tatevosyan VAkarova),
2. LenLngradskiv tekBtillnyy inotitut (for MeoB~ 9 1
(Mercerization) (Cellulose) (F*tero and filtration)

SHIMKO,, I.G.; KUVIN, A.A.; VOYTSEKHOVSKATA,, U.S.; TATEMS L.;
90--X-U
K&rAWrA,, If.?.; GAYDUKOVO K.A.; (;INZBM,,
uchaot:Lys-. PMYAKOVA,, O.Y.; MZVERSMKO.. V.I,
Introdwing continuous vercerization systems in the mnufac-
turs of viscose rayon. Khim. volok. no-3:61-65 163.
(MIRA 16: 7)
2. UyevoldT kombinat (for Shimkov Kuvin., Voyteekbovskaya).
2, laningredski]r filial Vassoyuznogo nauchno-iseladamtell-
skogo instituta iskuaotvennogo vololma (for 'TaterowM"-
Makarova). 3. Klyevskiy filial Vaeooyusnogo nauohno-hwledo-
vatellskogo instituta lskusetvannogo volokna (for Gaydukov,
Polyakvva, Besvershenko). 4. Vessovusnyy nauckem-lasledovatell-
skly Imstitut inkusotvannogo volokna (for Ginzborg).
(Rayon) (Mercerization)

TATEVOSYANY Ye.L.; MAKAROVA, T.P.; KUPTSAN, N.A.; ICOSP A.!.
Effect of the conditions of the continuous basic treatment Gf
cellulose on the rate of its oxidative degradation. Khim. volok.
no.6:33-36 164. (HIPA 18:1)
1. Leningradskiy filial Vsesoyuznogo nauchno-issledovatellskogo
instituta. iskusstvennago volokna (for Tatevosyan, Makarova, Kuptsen).
2. Leningradskiy tekstilInyy institut imeni Kirova (for Meos).

11,14KIROVA, T.P.~- MF,(X,;, A~T,
Charaiterisli,:q of' alkali Cellulose prepared by t~r- continuous
e~-~~I.ol. D.,,ra, --olok. no.4?26-2,~ 165.
m
m 04TRA 18,8)
I. I-eningradskly filial Vp~esayuznogo nau-~hncj,.isz!].edovat,31'sk,'.);,rca
11'
~xs,.O.tuta ~~skusbtvennocro volokns L Leningradskly ttlkstilInyy
Im. S.M. Kirova.

POLYAK, A.B.; TATEVOSYAII, Ye.L.; KUPTSAIJ, N.A.; M OS, A.I.
Chan,ges in the conformation of cellulcf3e links occurring durl i!g
nerci~rization and Dre-riping. Khim. volok. no.408-41 164.
(KILRA 1814)
1. L3sotekhnicheskaya akademiya im. S.M.KirOVIL (for Polyak).
2. IlAningradskiy filial Vsesoyuznogo rauchno-issledovateliskogo
instituta iskusstvennogo volokna (for Tatevosyan, Kuptsan).
3. IA)ningradskiy institut tekstillnoy i legkoy promyshlonnosti im.
S.M.Kirova (for Meos).

TLTAVOSYANTS, Hh., inzh.
Container for transporting plaster board. I& stroi. Nook. 2 no.5:
22 My 159. (MM 13:1)
(Plaster board-Transportation)

TATEWSMY, A. V.
UMB/ChemIstry - lethane, 1;2-Dlha'logeno-, Apr 1948
Chemistry - Isomers, Rotational of 1,42-Dihalogeno
"Rarsearch an the Rotation Isomer of 1,2-D:Umlogenoo-
thanes by Combination Diffusion of Light," 0. L.
Arcnov, V. M. Tatevskly, A. V. Frost, Mosew State U
imehi M. V. Lommosov, Sci Res Inst Org Intermediate
Prcduots and Dyestuffs Imeni Vorosh1lov, 4 pp
"Dak Ak Naak SSSR" Vol LX, No 3
Studies constant of equilibrium of rotati(xi Isomers of
dihalogenoothanes by method of measuring JUiteensity of
lines of a spectrum formed by combined dispersion of
light of components and Including affect of tempera-
t factor. Submitted by Acad A. A. BalandIn 18 Feb
X I 77T1-0