SCIENTIFIC ABSTRACT GERLING, E.K. - GERLING, E.K.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R000514910004-7
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 99
• Document Creation Date: November 2, 2016
• Document Release Date: September 17, 2002
• Sequence Number: 4
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

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A%&-ILA &ITALLUAGICAL 1.11111ATURt CLASSIFICATION V.
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IW 13o . 11114 %1 Ars Anti Oil- Agr t)( tho- r4rth 3 4 - F101 tvar~.
Radium Inst., Acad. Sci. LUM

1 -0) "
A, ,. ,!' int ruji,)nj a,' A~ G.-~ m ,~, 'i,rx,, in the .`,~,Ia
P-~nlrml . ... ::. 'Wrlin, 1. 6. AariK (Co4t. n!r,.,. h* :. .,il, U. i. .,. .,.,
1):.2, .1,, Aorlowite bpeci.vnj Crom L;it.
inv,,.,it!, .''their content of' ilu, Aa,- ~.n; Tr, :1u,nE -t:tvrm-m..!. two I.Am-
%3 .. tom-.c: sl:;i,-ltaa.,%is-y ~3,0
i,). - ;( Ij year.; a, a.
j

Ago of pausft "im d libe Dow low" in IM Unit. E. K-
(~Cflw nd It. E. VLadimiruva lCompt. rend-leaJ. Sco. L'R.*~.S.
194", V 170-11k).-The age of the Kmite intrusiims and their
r9matites has been obtainod. from asimLirsidta (1) wO e9chittite (M
y the lit method. (1) from the BIUZWV%k&)'L minebas IN 3 it
trig. f R.. 11 0.1018 g.-kar g.. and Th O-OM - Per q:hTba corre.
spnnzg figures tat (11) are 0-691, -, Mi. ages an
246 x 104 and 218 x 104 years. respectively. Cwvw showing tha
He evolved " beating 11) at diffete t temp. arv reproduced. (111
retains tie -h*n heated. only 20% of Its total amount twin filer.
&fed by heating to 1200'. 11. ~. 7,

c tl
Nkrisil"Hoo of pitams o2M~ in aMwW w&Wm 1; ' N (;crhnK,
G St. Ermuhn, &nit N, V Mrau-Aaja (j Apri, ( kem Ruis
1944. 17. -Analym of gwi tontwnol m n4ural
bv i:~,wltlustiotl. hydt~gctl.~tv-", 1-otnp ,,,( Vt all't III th'! gl,~%
aiK - -h%"jU4'n! LOMIMMIIA-11 %iih 111JI1111 JIT,
AnAlyll'. et" in al:lhll,kl ANKLLM &Jljlaf4tkiq is dexi-il"A The
pTe,ence of Old . ~,f N,O - th~ p,oitity ,I
jwtw,,lmm hvlJt,,iwN,r,, pre,tit. is rrjx.rt,,f 1, .% 11

go 0 0 0 0 0 0 0 0 0 0 o 0 o 0 o o a
Is If 11 is JD
y
00 4 1 a 14

00-1 1 M I
--

NOMM OZ* OOGUM 61 miataw
ItarkAn i1 .41W. C4.. JNj.
(~f the expertairrital visethoxi Pr"
100 natural waters front Ta
ut N.0 pa 1. in Ociam
otheirs.
jla~. andicaLing that it is i,f suirf
0 a

i,,u,l,dr-irri?,I
tar
bMad
m
A 41TALLIOGICAL JIT14AItill CLAIMPICATIC"
ss
V
L it OW a it tr n 11 11
0 0 0 0 0 0 0 e 0 0 0 * 0 4
o of 0:0 0 0 0 0 0 0 0 9 0 a
mm~~

so 0 go inip see so go 0 W
17 Is A sj 1, L 11 m
T.L AA "CC Putt..

salitig F K t; lin
"
an.1 V
,
1944. 17, 3211-3.14
)
t
(c1
41

'i S R sh,- so
afeu and ,)-4 c c in

r origin.
A

see

as
zoo
XING

CIO 0
gee 0

an
0
0 so

A
c I~v
,- - , , I i ) -. i . , .
/Y
The absolute aglIcals of the earth's loololgical hIst*q
A A, Polkaylov F. K Ilerbitj I"r-t lkad Vauk
S. S R- ~,,, r-I 1940. "9-"qfq, t"IltIMI %uminary I - ~
IN-1hir 4 tho It- -'1 1% mtChi'l, jrj di,
I it,til Fl-her

'

0
! t t P 0
4 1
i1f."Hi
in ' IF Is ' 111 (1 0 0 IF 0 S
ffif HIS M 0 0 0 0 0 0 0 0 0 0 4
'R'
IL 4-A 1. A P 9
I
I'V --- I
r
M W U Sit B 11 V 0 P 4 it 41
Is
I U U 429
of '
I I " I
It
1 at
4 Natural occurrence of some liable Poditim of WON-
Missouri 11"Jon of Ursenlam V (I. KilloOn. H. 9.
1T
M
fill N. V. haranov,skays. Bull. surod. tiril . 1
I
(",file is, Aim. 1947, AW 411114(in RUw4n).- On Ill* as-
unil
1, C.11111. s-11 fill' AMIMP11-10 11141 -Is t Iss"101" offilt
I'll"llifit"I that lilt latitfucts; of allsinfalleous finalists fit 11 tis,lon 11) lilt. title extent; vith A. no. (4
I life Identical with liftiv- 1)(CAUCT'i UM1111 the Milan of slow (A' I U. X III") no.
1, ~fm- I I its l
, o"'11
!

a
strustrons; And, in jurticular, that, a"itritin to Frrmi
1
11 !
.
"l \i- A M 1:'. CU ollo. X, (A' - 2 1 x lo"I.
t"
Anderwin. and C."Aw (CA 15, 1311
1. 14
44 the fiI.
f i I ~k.. , logilAr I- ilix.,X.0,1411. where his - .00
'I'Mi. fe.111t its
ormation .4 stable Xr, the age of o4furul X. -
"'ll't .4.f.litilliegiralit414 1, '12 X 11) 11 Year
its FA, I'l hydell'.. .4 their X, eisole"I
'-is
ihs -
-f
mnlit Ilmot Chern
n, S61'su
t) J4,ILI
a
f ,
-110 is( I1.011411""l, filown 't If' I year. giving -00
i
s
i
K
p
."i'
a
t
it I Isis hillillAilly at 21111" %4f, r - I slit ~ 11), yroll, III Xjm*l.jKjtltIIj of %ith t tt I.A5 X so

3
1j-Jvt-d 'is '~' 5 1. 1,mloss IWI it]. I ~ M anal 1,fribuinarily its, I)Jitaillid by file 111, iiii-thibl. 11 the figure 11 14 1%
.
10
-
irml from chusolveil gates by mrWated flushing with 11, is I.L,, ed 1,y its,. -,t.i is it, -,,iditsit I., Crito ... fill and
0
i I
;
0, anti himling in musin. The gals evolml -luring the lscflfl~ 44 ss'ItIllillistin (C.A. 40, I~WM'J' title noths I.Vi x list .00
the otifirral %as led thnnigh active C at - IM)" to adjorts YrArs: it mranq that just J lite Xe ssAx-samulated to the
I
f X
i
"
"S 0
The heavy oble gaw4, then Ile waA collectril. V"orpti ,
f" o
s
11111letal is l(qit uvtr gfV1. 1wrioills, the
front life C Was done by puniping off at ;;6(1*; the pa MI :1:,n that of fie but bill[ Sigailialust. It the age (it
'
'
1 =go
thris 14-ol over Ca fit to absorb all chemically ac ve
it yrars, Will bir N, In the aftme
c earth ctrubt 6
X 10
. st

jw~ To siatilaic Xr, the pS was then kelit over (). X.
I liwniu!4 I, ~ubqiisjf.l the total just. of U in The ewtb
C at - U41' 1,,f 31 min. and Iturnifed off (by means a
of "I'l. find, list lite avil. of Xv imumulutrit] through

V .%let ,,*I gage used 4, j,tloq,); 10 timn rrpfttc(l punilang fi.jon something of thit or-Irt of 10' cu in.

i-ullrd its list is niiival sit o9r; of the A. to remove lite re- another willote of Xt might lie the slionlamr-

IF
snami,ig 11, . Ill, Ila, was dristartaki spin by heatin# to:Nx)' 111 ii,tion of Th but oo dirtel expil. evidentv can Ile
alid thit-if readvisPIrd on C at - IJ)*; now, with 8-11)
11
r
A
l I'll'Idird QA Tel N. Than see
o
the
j,unst-jtI, .
-
d be r,ernoIr.A. after .1tich the
A-1hear.ol2fript..,
. ISO
lNell' %AS (04,11141 jWf I lig. urastAnite: A 39 cu. Tom. (fit 'fee
W and 71W# mm. He), Xc 0. 77 cu. mm., Xsr/A 0.02n as

Against WINKIIII in sit. Theaticrolthentinstral(loyesirs) --Joe
.
is
0
A a V ITAIL1,1161CAL Ultillift,111 ILAWICAM.

wee
11 Av s; -s-
if a
a
-"'i
s
0
0 0.0 9 0 I,
4
dad

U30'11plljuclear Fh:,-sics - UraniLm Dec A47
Neclear Physics - Xenon
"Some New Methods of Determining Absolute Geological Age of !ineral-c,ll V. G, a-lopin,
Academician; E. K. Gerling, 4 pp
"Dok Akad Nauk SSSR, Nova Ser" Vol LVIII, no 7
Describes new method of determining absolute geological age of uranixr. ~iinerals
according to ratio of xenon, included in mineral, to the uranium. Fasis of new method
is process of voluntary separati-,n of uranium which, like radioactive disintegrati6n,
must take place at a constant and unclangeable speed in ther-r-oJynimUcal conditions of
earth's crust. In order to calculate absolute geological age in years on basis of
ratio of xenon to uranitz., following formula is used:
t = i/nx 2.30 loglo Xe
L7
ax
PA 60T82

8!
'3
%)'
J
I R I
167 Now Data on the G*Ochtmlstry of Inert Air Nikle
GAS.s. V. G. Khlopin vid E, K. Qjglffilf. Radium
InStilute Arld4rrij CO FICIror.. USSH. MAY 20. 1918.
op.INP-;f2s)
A new method " forripAx for determining the age of urn
nium minerals by the ratio of xenon to uratilunt lit thent his
be" propmed and Toothed exp#rtmentallv. Converiely.
the same to rmula can tw uhd to '"finial, how a-urb xeso-
can acrumulAir In the #Arlh's r1o, during the- A-logicil
time of its existence. A calculation show., that the quantliv
Of XFr4n formed by spoolAnquils uranium in the e,rth,if
crull during the itiouloglival Wrid W It- is CM -
IderaLto and ...Is 10 &bmt 0.5% At, it. lot., Aefton con -
tent. The origin and occurrence of other noble gas,,
(krypt-. arM helium) 15 (Ifficussed with particuls, elit,
Phast" on the radioactive wid jor1rolatrysical onglif of
subterrantu helium. Title nuclear I'llactio" Of argon are
briefly discuslurd.
4
*00
0
;00
0 0
4 11*0
00
A S 4 - I L AatIALLURGIC4f. 1.111114TIM.CLAWFICATIC).If
V,
U o AV -0 As
" P 11 11 0. 'A 0 Of 9 ef PC it It It ofn A lia
so o 0 0 9 0 : 0 : 6 0 0 0 0 a : : :I* * 0 0 0 0 'D 0 * a 0 0
00 0 00 0

UMM/Ruclear Physics - Uranium, Jul 48
Decampo-yition Products of
Chemistry - Helium Group Gases
"New Mkita in the Geochemistry of Inert Gases,"
Acad V. G. Khlopin, E. K. Gerling, Radium Insf,,~
Aced Sc I usEm, 4 pp
'Dok Ak Nauk SSSR" Vol LX1, No 2
A-athars previously established accumulation of
xenon heavy isotopes In ancient uranium minerals,
and determined xenon content of uranite from
Cherns;Yra- Sralfaa deposits in Worth Karelia. (IZ Ak
3%uk SSMp Otdel EhIm Nauk, No 6, 600, 1947).
Vft 11/49T81
Gives formula expressing aze of uranium minerals in
terms of their xenonfuranium ratio emd explains Its
uses. Cryptou also accumulates in the earth's criast..
but In smaller quaiLtitiee than x3non. Suggests that
both these gases may -Iso be formed. during spon-
t^w'--u* finvion of tho-ium; however, as yet there Is
insufficient theoretical and practical data on thle
point. Stresses that underground Isotopes differ
rrCM atmospheric ones. Similarly, underground and
radioactive helium have different isotopic compo-
nitIons. Discur-ses bearing of this on Mourem's
hypothesis. Explains absence of large qaantities of
underground argon by saying that ThMAOn and Pow-
lands overestimated probability of its formation froC
potassium. Work on this point continues. Submitted
20 Jun 48.

G
04. On 4~be disintep-ration of PotnQulwi bv K.-cartiarp.
949) 'Har.-Apr. (In Ruf, niAn I
K, Gerling ind
The existence of 20K-cnptnre in rn4ioactlve 19 K4n trans[(jrmlri~ the
-latter Into A I Which is to be expected necording fo ti-a rulen
gi ven by Sis, 16 hysica Z, 467(1?37)), ~qs Leen confirmed' ty Ble~aer
,RAP)o..jP
no
and.Gabriel (Heiv. Phvsf- ta 67(1947)) by thp x-rav method.
The present authors foun'd another conNi-mition of the exiatence of
this proccnn by ann* Y,,.)In g, wl.th a m.,min-spectrosoope, thk~- Iflotopic
-ug,11min. Resultg
content of nrgon c c. luded In notf I
are ~Ivag of measur6ments mde on from U.,- Soltka--nsk dep~sltq,
200 x 1.0 years old T~.e water
solution of thn minernl by ti,.4m ~ri;~cesol.vely w-parated by
Sorptlon on copper oxlde~ 6111--c-c"11 ml A, t""loW.-nY argon Tomained frep,
and its content wis found to be 0.507 cm--' 1.,-, 1)0C0 g XCI. M.
spectrographlord invesligntion .9Y-wed thrit, wl-or~-"ns'ln !--Ar A36
accouhts for 0.30% of the totnl amount of argori, In sylvlte cqly,,
A40 - 1z.-prev, eat-, - Th oroforo; flr Is, n,)-t the solirm? of A""

I ~ I W It - - - - -
m ,it, 1m, ir i-1 -i -
_111~_e 0-0 a a to
I I A 5 a I 1 4 n 'I 'I M is is lot V a pit" MTN IF U u a is V a P 4; .1 0 it it of!*
A L 1-1-1 _1_k _L A 11 F it 1
0*4
g: 1824 Determination of the Decay Constant id the K -CAp -
tart In V. L. L Getting, N. E. Titor. and G. M.
R. 68. 553
Efroollo, Dokl&dy Akad, Nauk S. S. 3 .6
(194OXiA Rusiain). (See Also NSA i-119~ 1.00
From the k'" and redWactive A" contents in a ,YMI1 "t
0 known geologic $40. the authors 111veskiya Akad. NAUk. Old.
KhInt Nauk. Mo. 3 (1049)) determined the drvay --IAnt 4 *0
0 A! the transformation of e into A* by K-c4pture, the %AIUO
0: A found was 30 times smaller than the constAnt 1.9 - 10-0
year-' determined by Biruler and Gabriel Met, Phy, Aru lie
20, 67(1047)) from a study of x-rays omltt~j by K salts in off
1. 4 new series of analyses in# present aqttw)rm u-i. 1-Id-
the same sylvito (age 200 % lif yeArol. A carnAlliti- ~-( the zoo
"me deposit, two noploollnea 1350 - 1e and 280 - 10' v~Ar 0.
As*#
and a very old microcline 0.100 - 10' years), In order to
Cog
It" the A Atoms from the crystal laillros, lht ijijnrrjl~
were either dissolved or molteil. By takinj Into account 1hr see
small quantities of A" freed along with A . the mrin value Gig
for the X-dK&y Constant of Ka was found to be fS I - I I? -
10- year-'. This should be the constant sought it - ap.
proclAble leakage of A from the minerals limit place durtrit
:i the grologle time. A discussion of this question. which I,
that on Me brat of diffusion of A Atoms through crystal 141.
tices. Involves considwr4tions on the known values of the zoo
heat of diffusion of Mr. an the relative size (d A and Ht Voll
Atoms, and on the temperature of melting used In the pr" - tie
'c -n mus
ent work. As a result. the leakage in quetilk I hAyr
tie
seldom raverded IN.
r
A11,11 4 -ltALLLV(,KAL tiff--,
weii
04. jot MIJIL11(pe MI&IJI (w
11*41
U SLT~Q Is;; or it It 41 K KLO
0 0 0 0 0 We 0 0 0 0 0 a 0 0

U&SR/Ruclear Phy8ics - Krypton, Radio- 21 Feb 51
genic
"Search f or Radlogenetic Krypton," E,. K. Gerling,
N.. V, Baranovs!-.aya
"Dok Ak 1-4a-,jk SSSR" Vo! LY--II, No 6, pp 825, 826
Lelpi-dolite cantg Pb isotopes t,0,77%) and heavy i=rt
gases (0.0967 cc/1,000 g) is found in deposits in the
Altay- and Kalbinsk Mountain Pange~ and amazonite
contg Rb isotopes (0."%) and 'heavy inert gases
(0-371 cc/5,000 g) is found in deposits in Kanozero
(Kan Lake) and Kislays Varaka. Both of these mIn-
cr-mls contain less than 5/10c cc of Krypton per 1,000
185T100
USSR/Nuclear Physics - Krypton, Radio.. 21 Feb 51
genic (Contd)
g. Concerning the Rb method, cf. H. E. Suess, "Phy
Rey" 73,, 1.209, 1948 and Haxel and Houtermans, "ZS
fur Phys" 124, 705, 1948. Submitted 28 Dec 50 by
Acad P. I., Lukirskiy..
185T100

7,4, ~,; ~,!K, F. J., Profs.
Veteorites
Alge of stone mateorites by the argon :-.ethod. "etearitika No. 10, 1952.
1 Unclassified.
Monthly List of Russian Accession , Library of C;origre5s, Jmu 1953.

s R
ThO
vt ly IsIt t, Mille
~t, prvviw~. ~CA till xT'pJji4j lips
Lnd Yt-fy Flifich le- rhal, fm nirlew-lic 4t[)Ilf &; thli miqlli'sh
C011111,
th.Lt tcimtvi m Alt "
of KO, v A noio. wid A91 iTIN'll.
t'Ait' Q ("C' ! ) , 10 , l; ~' 's" Io--, )c
)< Jill jild.-Ilmile 11 IT-IS 1 7 10". Ul V
(u x to'. rill, J S X

Fhvt orpe rlinen t on ffie I;plljltif)ri of the fIrrOl Method. U
11 K
C-
detfli
l1nation of I Im a
e of 111111 orals
(
3r
fl
.
-
-
-
g
q
.,jj
tj
f1rovilin N. ~. llarxininbri, arill 701:14Y
k
aiik S S.S.A. 86, Vd-3-6i (li(,
And.
wa; conipletcly doovinItmted and Or I-
clecrimpit, of 1,
rapturt comic, ol K" wa,, decl. fly 2 es-wathilly ditTerent
mclhod,4~ all littempt Could tic mmle tu apply this ri:tr
inethod tit raillouctivity to ]Qln. of Ov. tint of K mintrA
from the t-acli-oprile argoo own
viliting ic thon durloff
*
;
ged. timc. A lictits of K oflitcrit i wv; sloillell, Including
microclinc, azoazlinitc, and 1clAilillirv. The ijv of this in.
truNW5 Ivith villich the 111hor-A,; I% ?t Id %IIa; known (it
the kinils of the 114 or f1b yr-illi-I : oi Owilft a
CoMpall,M)n olf 411a ObLiloill by thi Irlion ItalhoA. willt
datit from the othertriftbo&
A method, It wai nectuary la kjio;v the A cy.40-jit and thit
K wtent. Tltn K Ontent vrat Md. by 4-rdlipty clItAl,
infAhods. Tu metowit the A coutcul. a welfilmd ;;ample at
the infrieml woo heated at 11401 In it quirts tube c-mincollif
to the menstuing rNurt of the ripp. fletatlig vua Lantlautil
until evolution of A ccatied, from which 8 co go lin. trem
required. 8olue of the minvuls melled at tIrls tmil).
Preliminary expts. showed trial A fr= the air dhi not dit-
fuse fit appreciab?e quantities throit'gh the Iiu&Az Ill-wrin
heitedtiII300". Tli,.,jtwa.-ipuririt4faiidwi~tlti!atneasafett
in (I MacLeod wrimucter, A inaun-slROMMIrk deth.
iv.m nvule, of the Wimple voinlin, of 3 -4Xm let of thit A.
.N[J.'o sp-thograitiq :ire rwo,41ii"t for the PT"111 lepid(lilt!
ayan~i.toc.iffe,aad the data ftwo the,% del tit. wu lofx"d.
GladV4 S. Mwy.

GERLING, E. K., and YASHMO, M. L.
"Age and Orl:.,,in of Tectitet," 7r. la~,or. geolog~i dokembriya AN SS~~,R, No 2,
232-2h6, 151-53
The authors critically consider the numerous hypC-theses or the origin
of tectites. A13. the hypotheses of the cosnlc ortgin of tectites ecxplairi
sufficiently well their vii.~ie distribution on earth, however, they do not
convincingly Inscrfl~e the mechani.-ri governing the fornintion or "P.C.-Otes.
Deserving of attention is the hyrethetis of the formation of tectites
durirF the collision of meteorites on earth mid of the e-,' plosion, and
melting of the meteoritic -.u6stqnc,!. P~rom the hypothfiset .)f i,he
terrestrial orig4r. of tectites, the authors pick out the vii1canJc
hypothesis) ~dijch explains well the age of tectites, as deterrined by
the authors according to the potasEium-argon method and not exceeding
3-12 million years (conseqilently this hvFothP.-is explAdns the cause
for the tectites' being found in quaternary rocks.) The ratio 0 18/o16
found here in tectitess can be explained by the remelting of the sedimentary
rocks of clay corrosition. If the future demonvtrates the possibility
of the transfer of tectites by air or other wayr, to con:iderEible distancer

from the volcanoes, then the prIncipal objection apirst the, hypc't~,esiE of
the I)Vlcinjc or4-gin of tectites falls away.
RZhGeol, No 1, 1955

~-T N 4.- j I -
STARIK, I.Ye., ctvet3t7Ctinyy redaktor' SHCHLILBAKOV, U.I., Eikadsunik,
redaktoz, VINOGRADOV, A.P., akud,5mik,reda~tor; ]JAIULN07, II.I.,
professor, redaktor; q&_=9',jj., professor, redaktor; LE-
VIR, kandidat fiziko-matematicheskikh nau~. reduktor;
KRnov, A..Ta., redaktor, PEKARSKAYA, T.B.. kandidat goologo-
mineralogicheskikh nauk; MYASNIKOV, I.A., redaktcr; POLYAKOVA.,
T.V., tek-linicheskiy redaktor.
[Transactions of the first session of the Conrniut3ion on Determining
the Absolute Age of Geologic Formational Trudy -pervui sessii *~.omissii
po opredeleniiu absollutnogo vozraata geologichaskilch formatell; 12-15
aprelia lq52 g. Moskva, Izd-vo Akademli nauk SSSR, 1954, 231 P-WEA 8:1)
1. Chlen-korres-condent Akademii nauk SSSR (for StazJk). 2. Akademiya
nauk SSSR. Otdeleniye ggeologo-geograficheakikh nauk.
(Earth--Age)

GMLNG& I X
;Wzwuw-,-~
Ago relationships of granite Intrusions of the Ukraine on the bests,
of argon method dRta. Bbil.Kom.po opr,SLb6.vo%r.gaol.form. no-l'.5-8
'55 - (KLRA 9: 10)
1. Laboratoriya goologii dokombriya AN SSSR.
(Ukraine-Grnnite) (Radloargon dAting)

USSR/Phyaics of the EartI4- Origin and Structuxe of the Earth, 0-2
Abst Journall Referat Zhur - Fizika, No 12, 1956, 36318
Author: Gerling, E. K.
Institution: laboratory for Geology of the Precambrian Period, Academy of
Sciences USSR
Title; Inert Gases Found in Meteorites and Their Isotope Content
Original
Periodicali Byul. Komis. po opredeleniyu absolyut. vozrasta geol. formatsiy
AN SSSR, 1955, No 1, 57-60
Abstracti Meteorites are irradiated for a long t e by cosmic particles of
e , re c - 101 ev in the absence of any
very high ene i a a hing 1016 1
protective shiding. It is known that as a result of such irra-
diation iron meteorites accumulate large amounts of helium with
a mass 3 and 4, formed as a result of Interaction between the
cosmic particles and the material of the meteorites. An inveF.-,.
gation of the contents of other inert gases, namely neon and
argon, in 5 meteorites, and also a study of their isotopic
Card 112

USSR/Physics of the Earth - Origin and Structure of the Earth, 0-2
AbBt Journal: Referat Zhur - Fizika, No 12, 1956, 306318
Abstract: composition, has led to the conclusion that the Is*topic compoei-
tion of neon and argon in meteorites differs sharply from the
isotopic contents of these gases in air. The presence of neou
isotopes with masses 20, 21, and 22 and of argon isotopes with
masses 36 and 38 in meteorit,-B is caused by deep splitting reac-
tions, produced by cosmic particles of Mgh energy.
Card 2/2

GMING, I.L
---,.FAM "W.R
Discovery of inert gasesin meteorites and thmir isotorrAc compositloa.
Biul.Kompo opr.&bs.vosr.geol.fom. no.1:61-63 '55. (MLRA 9: 10)
1. Laboratoriye. geologil dokembriya AIT SSSR.
(Genes, Rare) (Meteorites)

GERLING, F#.K.; RIF') K.G.
Forms of argon occurrence in meteorites. Mot-toritika, n0-13:15-18 155.
(Argon) (Meteorites) (MLRA 9:2)

UMI/Astronoav Argon method
Card 1/1 Pub, 22 - 10/49
Authors I Gerling, E. K., and Rike K. Go
Title I Determining the age of stony meteoriten by t1se er8c,n metbod
Dok- AN SSSR 10113, 453-455o Nor 21, 1955
AbOtr`40t I Results of determining the age of 18 atonny vateori-tais by the aigon
method are presented. Five references, 3 Mal 8b! 2 gnalish (1551-
1954). Tables
Institution i Academy of So., USM# The Laboratory of Pra-Umbrian Geology
Presented by : Academician A. Go Betekhtin, December 20, 1954

---- --- ---
-I T

(matoarites)

GFIRLING, R.K.,.profassor-, BARANOVSKATA, N.V.
...... . ;. ~, ~
Abundance of xenon and krypton in meteorites. Meteorltiks no.14:113-
117 '56, (HIJU 10: 1)
(Metaoritse) (Xenon) (Krypton)

GERING, E.K.
Occurrence of noble Cases in meteorites, and their isotopic composition.
Dokl.All SSSR 107 ne.4:559-561 Av. 156. (MLRA 9:7)
I.Laboratoriy-a geologii doketibriya Akademii nwik SSSR. Prodstavleno
akademikom A.A.Polkanovym.
(Gasas, Rare-Isotopoo) (Meteorites)

STARIK, I.Ye,, ot79t5tvenny-y red. SHf--T, R B A YOV D I., d.,-
BARANOV, V.I., prof., red.; 5HATHlY, N.S., akndnmik, red.;
POLKANOV, A.A. , akndemik, red. ; V1110frRUADOV, A.P., akademik, red.
AFAIIASIYEV, G.D., red.; GERLIFG, E.K. prof., red.; PSKARSKAYA,
T.B., kand.geol.-min.nauk'.- red.; TUGARINOV, A,I., red,-,
CIMMYNTSKV, VJ., red.; POLYAKOVA, T.V., tekhn,red.
[Proceedings of the fourth ;cession of the Commisnion for the
Determinntion of the Absolute Age of Geological Formations,
May 12-14, 1956] Trudy chetvertoi sesaii Komissil Do opredelenibi
absoliutnotro vozrnsta geoloricheakikh formntsii; 1"-14 MRiA 1955 g.
Mosirva, 19~?. 297 p. (MIRA 11:1)
1. Akademiya nauk SSSR. Komisslya no opredelenivu nbsolyutnogo
vozrasta geclopicheskikh formataiy. 2. Chlen-korrespondent
Ali SSSR (for Stari)c, Afannslyev).
(Geology, Stratigraphic)

~WRTTNG1 F, ~, 1.
Ger3ing.. E. ~., Zhirov, K. K. - The Age of the Akch-~jt-.Iu Rare Xeta2 Intrusion
According to Data Obtained by the Helium Method for Monazites.
The Sixth Session of the Committee for Determining the, Absolute Age of
Geologic Formations at the Department of Geologic-Geographical Sciences
(CGGN) of the USSR Acndpmy of Sciences at Sverdlovsk in Mav 19,57.

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