SCIENTIFIC ABSTRACT GOLOVANOV, I. -

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• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R000515810012-8
• Release Decision: RIF
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• Document Creation Date: November 2, 2016
• Document Release Date: September 24, 2001
• Sequence Number: 12
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

$MTAWT, ~ I.I.
ImPrOVONIOnts for the vibration knot oatcher. Rampromi. 28 no.11:29 V 153.
(MM 6sII)
(Wood-pulp Indwtry)

of sorted vvodpap. Bm.yron. 33 no. 21 t
(XnA 33: 11)

MMWT, $.T.,; 001MANOT, I.M.
-Peculiarities of the growth of crystals of supergene galena. Dokl.
Alt Vs.SSIR ne.11:21r-24 156. (MIRA 13:6)
1. Institat geologii AN UsSSit. Predstavieno akad. AN UzSSR
A.S.Uklovskim.
(G&~ena)

BAnhuff. $.T.; OOZOVAWV. I.M.
now aduaral in the thaumette group. Dokl. AN Us.
SSR no*12M-21 157. (MMA 11:5)
1.1matilbat geolegil AN VaSSR. Predstaylena alrad. AN UzSSR A.S.
Moumdm.
Mbekistan-Thaumaelte)

ATI-J~,I'Rs: Bmdalov, 3. T. , Golovanov, 1. Y., jCV/20-121-5-36/50
Khozbatelev,
A Monticellite Skarn From Central Asia (Montichellitovyy
skarn iz Sredney Azii)
PERIODICAIt Doklady Akaaemii nauk SSSR, 1958, Vol. 121, Nr 5,
pp. B97-900 (USSR)
ABSTRACT: ;(onticellite, sperrite, and melilite have been known in Cen-
tral Asia (3rednyaya Aziya) since 1950. The former forms in
all known cases both alone and also with the complex of its
paragenetic minerals (of the two last-mentioned ones) con-
siderable acauxulations of metamorphosed minerals which are
bound to the contact zone between eruptive and carbonate
rocks. Table I shows the physical propprties of monticellite
from Gavasay (Namangan area, Uzbek - SSR = Namanganskaya
Oblast', Umbekskeye. SSR) and from Almalyk. The latter forms
small roundish grains of Otl to I mm of size, without crys-
t alline shape; the monticellite grains from Gavasay are an-
gular, of irregular shape, up to 0,1 mm of size. Table 2 shows
Card 1/3 ohemical analyses with a conversion to mineral components to-

A 11onticellite Skarn From Central Asia
Card 2/3
SOVI/20-1 21 -5-36/50
gether with comparing data from other sites. The first au-
thor took a radiogram in the Radiometric Latoratory of the
Institute of Geology of the AS, Uubek SSR (Institut
geologii Akademii nauk UzbSSR). Table 3 shows the results of
his interpretation. They confirmed the composition of the min-
*ral as monticellite from Almalyk. Moreover, sperrite is
found in the skarn from Gavasay. It forms crystals of 0,05 to
0,1 mm of size, of irregular shape, which develop at the cost
of the monticellite grains. The mineral of the melilite group
forms small angular crystals which often have an almost square
aross-aection. The formation of the monticellite-skarn is
genetically bound to the contact-zone between eruptive rocks
of middle to basic composition and to dolomites (Almalyk) or
dolomitized lime (Gavasay), Heret like elsewhere, the process
has taken place under the participation of postmagmatic solu-
tions (Ref 6). It follows from table 4 that C02-gas escaped
during the formation of monticellite skarn and that kiesel-
guhr penetrated into the solution.
There are 4 figures, 1 table, and 12 references, 10 of which
are Soviet.

A Monticellite Skarn From Central Asia SJV/20-121-5-36/50
.A,9sc.(;l VI 'O.N: ',~iutltut goologii Akalemii nauk UzSSR (In!)titute of Geolog,.,,
U'v -O-zbek 33,0
PH E:3,,;",IT ZL i April 9, 1958, By D. S. Korzhinskiy, Member, Acalemy of
Soiences, USSR
SUT47T7 _~:;: kpril 5, 1958
Card 3/3

GOIDTAWV, I.M.
gavercem load u1swrals from the Vargasbinkan depoisite
7^j?#Us**tdpVq*v*uiu,ob-v& 00-139W-95 159,
(MIRA 1317)
(Alma4k region-Lo&d)

OOLOVANOT, I.M.
PUttuarite crystals from the Iurgasbinkan deposit. Zap. Toes. min. ob-va
88 no.3:333-335 '59. (xru mn)
1. InstItut Cealogii AN Usb M
(ftrgashinkat region (Mbekistan)-Plattnerite crystals)

30) SOV/20-124-2-45/71
AUTHORt Golowasov, I. M.
TITM On #L6 Occurrence of Huntite in the Kurgaahinkan Deposit
(Usl4kakays SSR) (0 nakhodke khantita v mestorozhdanii
KU4&shinkan (UsSSR))
PIRIODICALs Dokl.*dy A-katlenii nauk SSSR, 1959, Vol 124, Nr 2, PP 398-401
(US$R)
ABSTRACT: The author recalls the occurrence of huntite in the United
States (Ref 2) and its further findings (Refs 1,46). Now,
huntite was found also in the USSR in the Kurgashinkan lead-
zinc group of the Alualyk or* region (Uzbekskaya SSR) in the
form of small veins of a thickness of 1 - 3 cm in the *luvial
crust of dolomites D3 weakly peppered with serpentine. Runtite
was equally found in the T&kfon deposit (Tadzhik*AyaSSR by
chemical analyses and radiograms (made by A. D. Danilova~.
Solid. oollomorphous masses of huntite fill gaps in
Kurgashinkan. Its exterior cannot be distinguished fron ordi-
narjr magnesite and strongly reminds of normal chalk. Inspite
of low hardness (2 - 2-5) huntite is rather brittle. If it is
Card 113

SOY/20-124-2;45/71
On the Occurrence of 1juntits in the Xurgaabinkan Deposit (Uzbekskay SSR)
hit it is split into cornered oblong splinters with a flat
aboll-like surface. Since huntite is highly hy-grosoopical its
spocific weight could be determined precisely (approximately
2.65 - 2.70). The Meygen reagent does not cause any coloration.
Huntite is molten by the flame of the blowtorch; after con-
tinmed action It is covered with loose magnesium and calcium
oxide powder. Concerning the optic properties of the cuts only
an sggregatlys polarization and a strong double refraction
could lie found. Table 1 shows radiograms (taken by L. A.
Sokolova under the supervision of S. T. Badalov) of huntite
from Nurgashinkan and the United States which show great
sizilarity. Chemical analyses of huntite of different origin
arm, shown in table 2 (carried out by P. L. Prikhidlko). The
spoctru-m analysis was carried out in the laboratory of the
Trmst "Sredattsystmetrazvefts" (Trust for Central Asian Non-Ferrous
Metal Research) by the Analyst Z. M. Lopott. The heating curve
of the sample from Kurgashinkan Ng 1,a) shows 2 andothermal
effectes a maximum at 6650 "d 900 . The curve of weight change
om heating (Fig 1,b) shown a total loss of weight of 50.5%.
Card 2/3 This confirms the chemical analysis: 5MgCo 3* C&CO 3- X93 ca(co3)4

BOY/20-124-2-45/71
On the Oomrreaoe ocr Runtite iA the Xurgashinkan Deposit (Uzbekskays SSR)
(Ref 2). As a comparison values of the constants of American
hunt4to are givent which widely agree with those of huntits,
fron,Xurgashinkan. Conditions of the occurrence of huntite
indtb&te a "bypergeneous" character of its formation. It is
oonaeoted. with the circulation of the surface water through
fissures in the sluvial crust of serpentines. In this horizon
magu&slum, content is such higher than the calcium content which
influences the chemical composition of the mineral. Huntite is
suppoved to be much more widespread, however, it may have been
somatimes neglected or considered to be magnesite. B. T.
Bada,loy assisted in this work. There are I figure, 2 tables,
and 5 references.
ASSOCIATIONj Inotitut geologii Akademii nauk UsSSR (Institute of Geology,
AS Vabokskays. SSR)
PD-IMENTED: August 14, 1958, by A. G. Betekhtin, Academician
SUBRITTEDs August 14, 1958
Card 3/3

L.A.
N 4AC.
Al
ski

ill,
0014VANOV, Io )(w Ownd Gool-Min Sci -- *Mineralogy and geochemioal peculiarities
'0 1?
=.. of the polym
m
of ths,k"rpn*%I4e stalFicurza. ink,,~~osit (UESSR)."
ix= f
Tashkent, 1961 (Aaa-d Sai UzSSR. Inat of Geol). (KL. 4-61, 190)
_IU1_

S&RUKOV, G.V.; VANS, S.A.,
beterninotion of tba total carbon content of titanium
tatrachUride. TitAn i ago splavy no.5:201-204 161. (MM 15:2)
(Titanium cbloride-Analysis)
, (Carbon-Amalysis)

OM.OVAJW, 1.14.
Oleasion of the UmbpkUtsn 1kranab of the A3-1-Unio-n Mineralogical
glwisty4 lbb,geal~mburs 6 no.2z63 162. (KM 15 t4)
I. Institut geologii AN Us=.
(mmeralogy)
: f
~-i

BAXULOV, S.T.; GOLOVAROV, I.M.
......
gow"u" sinmiogicai,aw #*=tic chamoteristics or
Unite. Ilab. goa* sh=e It Aa.60-14 163. (KI RA 17 t 8)
3. Institut geologii in. Kh.M. AbdullayevaL AN UzSSR.

GOLOVA.'~'d-V, I #E,.
...... 4'...
(*~ mineml m-.tl-ter in ore _ - .. I I . ".
C"C,-.r!l 163. 1 , - ~,LA - - -, I
,-- ~ " -,,(J,

IXLONSKIY, A.S., akadenik, otv. red.; BADALOV, S.T., daktor geol.-
miz. nauk P red GO ANOV, I.M., kand. geol.-rrizier. nauk,
red.; nauk, red.;
VAIAHOV, A.A., doktor geol.-miner. nauk, red.; 01AVLO,
S.G., doktor geol.-miner. nauk, red.; A-ITAKHOV, A.N., red.
[Problems of mineralogy and geochemisiry] Vop,--osy minera-
logii i gookhInii. Tashkent, Jzd-vo Nauka, Uzbek..qg-~,
19W.. 27E p. (MIRA 17; 8)
1. Akadem4a nauk Uzbekskoy SM , Tashkent. Institut geo-
logii i geofiziki.2.Akademiya nauk Uzb.XR (for Uklonskly).

G.MOVANO,vI I T, 4111.1 bljkNBIUIWV, M*1 MMONTIDV, B.V.1 YESIMOV, B.O.
Rtsn'uth mAxieralizaticin in mapeolum magnetite okaimn in one
of the ore uw-ifestaticne in the Xurama Range. Uzb. geo. Offn
9 nc.6%1047 165. (MIRA 19t1)
1. Inatitut geologii i geofiziki imeni Abdullayeva AN Uum
Sutmitted btarob 19, 1965-

e~VOjDVAjI()V, I.M.
' - --- ......... ..... .......... - .
NaLtTojaroatt,e crystaU from the Kurgashinkan complex metal
deposit (Uzbek S.S.R.). Zap.Vses.min.ob-va 89 no.6s7O4-709
161. (MUU 15; 5)
1. trati-tat Fectl,)gii kN VzSM, Tashkent.
(Umbskintan-Jarosite)

"".1, 1 A.K.
IN"'l-leet. rtisonan,-a of soiu,: al:Lpha,-- - -i- -," -~nt,
Ziur. fiz. khir. ~8
,y~o It - I. A ~~ I's 1 11
, ~, : T, " -. - --. 2
- " P'l in:ltlt~At Imen.1

G~IOTAWV, X., knpitan-lartemant.
Radio operator@ on the cruiuar "Ordxhonikidsoll. IL-4le no.7:6 Jl
'54. (Radio operatere) (YTQ* 919)

00,WTAN01r, X.
w...m mw - - famwWwwwama
Helping editors Of Ww2TJVr*wifp*per~o Promolcoopo no,5:35 MY 157
(XLRA 10;8)
Mil amimpapers)

S/081/61/000/009/007/015
BIOI/B205
AUTHORSt Smirnova, I. N., Balezin, S. A., Golovanov,_K. N.
TITLE: Effect of organic admixtures to motor fuel on corrosion
and wear of internal-combustion engines. (Stand tests of
anticorromiye admixturets to motor fuel)
PERIODICALt fleferativnyy zhurnal. Khimiya, no. 9, 1961, 275, abstract
9M233 (9i233) ch &P.] Mosk. gos. peci. in-ta im.
60 no. 146, 127 - 146)
I. Lenin&" 1~ :
TEXT: It vas found that addition of' anticorrosive admixtures to motor
fuel leads to intensified removal of corrosive sulfur from the motor.
Reduction of the amount of aggressive agent decreases the corrosion of
surfaces in the motor. Anticorrosive admixtures inhibit the oxidation
of SO2 to SO 3but promote the formation of a protective layer on the
operating sarfaces of the motor. [Abstracter's note: Complete trans-
lationI
Card 1/1

SHIRNOU0 I.N.1 BUZIN, S.A. I WWV&NOV,_j.Nj Frinimali uchastiyet
'-I- W
M141YANOV, L.A.; TURKEVICII, I.; 0131YEV, P.I.; FYDOTOV, V.S.;
MitMILOV, YO.M.
Moot of organic additives in fuel on the corrosion and wear
of internal combustion engirkes. Ucki. zap. MGPI no.146:127-146
160. ()URA 15:4)
(Gan and oil engines.-Corrosion) (Addition reactions)

GOLOVANOV,,.L.
WId founiation. IUn.tekh, 7 no.gs29-32 S 162. OGRA 16t6)
(Soil stabilization) (Leningrad--Foundations)

GOWVANOVII-~t-... -,
lagand skbout mercury drops. IUn.tekh. 7 no.5:68-72 Ky 163.
(KMi 16:6)
(Pola.rography)

GoLlansov. L.
I -
SteLronmeto Clock. Wn.takh. 3 uo.2:31-32 7 159.
(Xink 12:1)
(Pftgua-4nitronomical clocke)
dc'.

GOWV.(,IlOV. L.
......... .... . ..
Pemilulun, the univerval h&ndymn. rUn.takh. 4 no.1:49-51
ja '6o. (MIRA 13:5)
(Pendulum)

GOIMAWr,,, ~. , ,
Busti" vith high-froquetwy currents. 1UP. takh. 3 ne.6,.36-38
jo 159~ (KERA i2t8)
tftaistiu) (Ilootria diveharges)

GOIDTANDY, r" 101*
-
3101ROUtS of automatic-control oratems. IUn. tokh. 3 no.8:2-6
Ag 159. (KMA 12:32)
(Automatic control)

G010VAIWOV, L.
.. ".1, 1 1 1; f: 11 W
*Radio reins" of a steel horse. lUn.takh. 4 no.11:62-63 N
I ", (Tractorm-Ra4io control) (MIU 13:4)

("Oloa UUQTOJ!toi-.-,"Ov T'sawso tol;Aos)
(TV-ltLTGl "WOO-U41"A VIX70)
(6: CT VEIN)
o09, 9y III-TTtgeou t -q*$-uMj *so%mV sq4 xoVtm sanova-liL
"I 101YA01100

00
-- M%m
F40tival Of WOrIA TGcbn0lOAY- Mu-tekh. 5 no.9:49-51 3 160.
(Eno-Addbitions) (Teehnolog7) (NIU 13: 10)

I op;wuw X1.11, -
RgIt tocibmlogy la the hands of yo=g toohnicians. IUn.takh. 6
00.33.4 Mr ~62. (MM 15:4)
(Ommahoslovakia.-ftonjwre (Comnist youth))

GOLOVANOV, L.
N,v
Otestivenmes of the roung people; All-Russian Exhibition of the
Work of Young Photographers. Sov.foto 22 no.9:25 S 162.
(MUU 1518)
(Photography-Exhibitions)

GOLOVAINOV, L.
Oftope-valker" automobile, lUn.takh. 7 n0.103-34 Ja 163.
(Automobiles) (Gyroscope) (KIRA 16:5)

I -~~,4
-; il
OOLOVA PYs ~4,,
,, t- " .1 0
lkop*rt JVr= the high-&I#I;ude Tian Shan station for cosmic ra
rwiurO. XtJn. takh. 7 na.8:33--38 Ag 163. (KMA 16 tJg

GOWVANCIV, L.
In thot plivatalt of the OBlue EtLrd." IUn.takh. 8 no.11:66-67 N
f6l. (MIRA l61l2)

ACC UR: AP7011366 SOURCE CODES UR/0309/66/000/010/0020/0022
AUTHORI GoloVAnov* L. (M"Ir**r)
ORG,t none
TITV's LightAing In tht onvelops of a tuba
SOVIC&I NaudlMo-tekhilcheskiye Obahchestva SSSR# no. 10j, 19669 20-22 am 24
Topic T=9 4:614 catliiod'ie tub*,, electronic equipment
Sim CODE3 09
ABSVACTr The article doals w1M cold-cathode tabos. There is a brier
disou3sion of ~ho wo*l~~.$ono by L%Y WRABLEV in studying g*s-dischargn proport,,js
and in improvift , the old-cathode tubn. The result was the appearance of the
XIM-90 and ot~e'r' tuba6 ~in the USSR, By now over four hundred metinods and
*ircuits have 1~oun dev#lopod at institutes of the Academy of Sciences USSR
fQr usins colO~,caitbodel'"Wbas in electronic equipment. About one-fourth of tho
~YPO4 of M435 raaofflotilb~oqapetent in the Soviet Union now usas cold~cathDdw
tubosir. The insitr~aqent~#Wdng industrr is in the series production of many types
of complex iftst~unents j0d devices using such tubes. The idvantages of cold-
cathode tubes tooludes ~'scMsignaIJAC, interchangeability without Witching
devices, reliabWty, U~i*orsalltys The simpliftoation of oold-cathode tuba
cirmUts has mWe possi~lu tbA miniaturization of such tubes. The frequency
card 1/2
........ . ....... - - - - --------------

VUMMD, AA,; MMMAIM. XULAW, S.A.; LTUIMOV, A.L.; MUM-
ND~ %.A.;i SAM, I.A.; !NDMV, ye-V.
[ToW ormas sections of Or- -meson interaction with protons at
bi#b energ*,sol Polzqe senbeniia yZalnodeistviia Or -mem0mv a
pjr~tonamj pri vysMlrb arArgiiakho Dubnai, ObNedinermyi institut
inderMMi im"ovaulij, 1961* n Pe (MIRA 14til)
(mmums) (protmu)

3
S/056/62/042/003/011/049
B104/BI02
AUTHORSt Voyonko A. S. , &Lglovanov, L. B Xulakov, B. A.,
Lyubimov A. L.P RamINOW UFA., Sevin, I. I., Smirnov,YeV.',;-
TITLEt Total *--p interaction cross sections at high energies
PERIODICALs Zhurnal ekeperimentallnoy i tooreticheakoy fiziki, v. 42,
no. 3, 1962, 715 - 720
t(R-1 P) was determined for proton momenta of 3.4, 3.9, 4-9, 7-09
TEXT s cr
and 9.2 Bev/o. The experimental arrongement is shown in Fig. 1. The
total interaotion or"s section decreased between 3-5 and 7 Bev/0. lleas-~
uresents at higher energies have not clearly shown whether the decrease
of dt(R-, p) is only oharecteristio of the range investigated, or the b a
havior is an asymptotic one (Table). A comparison with other results has*:'~.':~.-~-'
shoin that at(%+# p) and Crt(I-y p) are equal in the range of 4-5 Bev
0 o 2
within the accuracy attained. Assuming that a /a - (ImIj/ImA the
2 t!
if Y Y
charge exchange is estimated with the aid of relation
Card.
lo -

5/056/62/042/003/011/049
Total 9--p interaction cross.., B104/B102
4,tX lin A0, /)/'2-) [at (A-. p) - a, (a*, p)J
'40
0 0
a 0.012 and 0.003, respectively. Aq'and A are the amplitudes of the
+
charge exchange processes (Rop-lol nq x p n) and of the elastic
scattering under the angle 00, and are the total charge exchange
cross section and the elastic scattering cross section. The two values o
were obtained at-~,;45.5 millibarn with crt( R P) - Crt(x+' P)
aillibarn, and 0
t at(x+, p) w 2 millibarn, respectively. The
data of other authors (G. von D*rdel at al., Phys. Rev. Lett., 127,
1961) are in good agreement with the results obtained here. I. Ya. Pomer-A
anchuk and Lo B. Okunl are mentioned. There are 2 f igures, I table, and
Soviet. The four moot recent refe 4~
17 references: 11 Soviet and 6 non,
encen to English-language publications read as follows s V. N. Gribovt
Ilual. Phys., 22,. 249, 19611 G. von Dardel at al., Phys. Rev. Lett., 5.~ -1 Z~
333, 19601 A.7. Voyeliko at al., Pros. of the 1960 Ann. Intern. Conf, on
High Energy Ph;rsics at Rochester, Univ. of Rocheaterl iq6op ps 443; 'j, I,
V. B. Barashenk0tv at al., Ifuclo PhYs-P j1p 522, 1960.
Card.2/3.

5/056/62/042/003/011/04~~l.-.,*.
Tot4l R'-p interaction croon... B104/BiO2
ASSOCUTIONt Ob"yedinennyy institut yadernykh i9sledovaniy (Joint
Institute of Nuclear Research)
101
S U101 ITTED iOctober 10, 1961
Fig. 1. Experimental Fig. 1 .4,
arrangement. 4'~: J
Legends (T) target In the
SPI-Mc q,
prot-on-synchrotron; 0,~-7
ML-Mfour-pole lem
M
M-57 (SP-57)) magn,:1Zt'(SIS
~ 4a ii
S SC)
;;in"'Ri.ttoln counteraj
concrete; (2) lead.
Table
Table. Measurement -results.
legends (i) momenta of x mesons, Bev/01
(2) at( millibarn; (3) muon admixturo
in the beam,
Card 3/3
1 4 .2
3,9 .30,0:LO,51:8 0,2
4,0 29,6*0,6 1 3 2,:,
7,0 27 8:k0, 8
0.2 -14A,

., QgWyMIN-0 l~ H.J, kand.takhn:nauk
, , -A.G~-CWOvanovo M.
Nov varlotIme of plastic ftaterl-als. Mauka i z;,ittia 11 n0.10:
21-23 0 161. (MIRA 15:1)
(Plastics)

.PCLOYANqy M.G. [Irolovanov, M H )I BMSO=ESXIY, V,.V.[Bor-."uh1ieIw*kyi,
T. XtI1WMXO, 'I*e:A: Kus"mankot
Use