SCIENTIFIC ABSTRACT SERDYUCHENKO, D.P. - SERDYUK, A.S.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R001548010008-4
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: July 13, 2001
• Sequence Number: 8
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

bepultite from Northern Cauctutus. I, .. .. .
V41ady A kad. Xa uk S 8.8 R. 69.
lite ("gurnyi pukls** inerrwhaton j i. c-mium tit ~thv114 -1 ~- v -
Iteill ill ite, licar MALI Ri%vr. .41,11 %1 Ill I'l. -1talu'll 0 111,
'llawture of Ille prilmay bj~w I...k. Vt1ill't. lilt '.10.
chatertloov. uad cluartz ire frewit.m. "fl- .1111
ctiNtaIN 44 r'Wk aw %tcul- 4)f J111601%,l, 'tillit.
ttill, --il-wit-ItA , t~m- I b. -I
th... fit. ,, "huh a '-0
I tIA1411. ill VIIARA&IMAIC OVinslk, 111.11'Atmic lilt l'id-ilmill
Of the C~aboiwe by the lilk-M, "'Ill, I Ill KC-1,11
tit the fibrous sepiolile i, ~illjiur it# that Of diry-til-4,
ill "inctacollaithil" form-. Co'hirle"; 21, - It
Nl*' olitical (haraelcr ling ; ill,- film-f, mv nit wiil pat,ilfrl
to-'; -i - . - 1 -140. I'lit-dicin analv~i,iAt,rJe-
duclioiloic.ict), ;11111.4 low FrPict"altill if "'"; 0
corr~l,ontls to the fornitiLi I 'p t,# i il 11-t i *
xll,O. The koinorphou, tepl.tcemvilg ,( :f by 2
Ali- is typicul for lite Wpiolil-pilygor'k-ite -ra-
ite mitil. AIX), i, ma more ela,tic 'W . 1-11'.
viorvu, 41'eir (IiAill't cl.diallmill'. CITv. t. m I.-,"
1 '1111 1.. .'j, I., X'ul'
II'M. 3:141 tit :441' (groliti, 11A)m.- -
,tiluli~nt lilt)), The mai-4ph,gs, h-mim pi-lit,i,
.ith lilt exothrmlicramt tit ") if C..cch
i, adolixeil, the reaction i, ob-rv"j ill 775 t" hill, The
x-ray pjttm~ 5how allivit, INOO' mid it,,-
"ith. The gen"m of the Cauc.&,Lin ~.-pihte ill tit,-
1;vt, raicks is lypically mclj~oinatic. W. Fitd

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liteviou'ly lalt 1.v F"ll'. ~.Illlv %It$
hivalent emmil. Mll' X~llvrallv C%, red,
Fc by fir ill it, mlorilli; pmcr' bitt tile
tnetricanil v,isof tlti% viri.litle --vurTeni-v Atm%- ilitly th,
0 mraricrWic af-rption of Fe ' ' ' ilwili- *%lilt 1, m
tile "tIl't hind. 11- 11'. indlivilev mi tile vi'tld.
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mill'Til'. I'lle v 1.,v di.'gtim if 111i
VjkULtyA %iritfille 1, idelltii-JI Vlilt tll,it if i[IdAll,itc
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pit.,110 to the Al- Ill,- t-m
Itimll andalumle M-'g thr- 0I I I.,
'Itrill. allalym, ,I tile yAuti)." widilic give, Sio':U'A.".
Hill 0,33, AIP# 1;ep, II'W' I'S 0 11AU, N1111 I
NIKU 11.21. Cal 1.111, 11,11 - 1.31". S. trt-millm-11,1, se
to I th. -vtw '*~imlie,e-. in- tile inul,r t
"viridite-isteerveil G-f an Fe hydri-licite,w( (lie clalm it, zo

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-7~rhe--ffmwjte-magnetite
Aue to Aisqomi.- at.
solid. Sabis. 1, (if
end
Ilmenite and magnetite (titanomagbitite)
during 2 min
,
pbases. Along certain - zones in; the maxactite them is
ev*uct of martitintion. Mafie

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~~:rdatiiius of gti~Wosltc. to'ne pmr,inembers (a
lati nd ta.~ boriptrandtlil,
lmd te7 gmup~, a
All Ll..iii~ii6 al
Y'V rm
Cajav6sitels de=Wpd ns A,
timlxt.,Of the* mob.'of
.27'4%
OV1~10H)-with 1 th isecexchauge of Cal+ for 2Na+ or.~;
or
Wrefringence indicat~,dless densn~,'
lower ?s~UnWl
jkrositis. -'TW
with; the'Almitnal"
"ematiiii. thermal,curve shows.. it, 4istina~ enq1ot6erTmW,:,.
effftt'at 1500 to 2V Ntborbbd H10);'a ibailp, 6dotheri Me
t 390' tt~'43b*, (16Ss ot'constitution HtO ~-' 011)-,'~
1k
"'At (190*~w 700'~(htt~:Mlcafi'jrp sulfate complex is d~cn.fjlpd.
'nit: X-,ray b-K :tvo-~tt-'
UroSltq~ and p
Ca
by
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1 slillce:d ill The -1,4,01111xi. svll,,:~td mijost ni:
~~J 3v~ Wit (:c', P'O in!
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jilt Cl~ rp

SPRDYUCHEITKO, D. P. i84T95
USSR/Minerals - Refractory 21 jun 51
"Chrome-Spinelides From the Malka-River Ultrabasic
Massif," D. P. Serdyuchenko, V.. A. Moleva
"Dok Alk Nauk SSSR" Vol LXXVIII, No 6, pp 1203-12C6
Describes 3 types of chromites occurring among ser-
pentines of area near the Malka River and gives
their chemi~ai composition. Submitted by Acad D- S~
Belyankin 16 Apr 51.
18~hT95

its Dryonlan st.diumitis of ', Tiousn I- V
r1 do KO. "'k t I .,--I i I 1.. '0"'.
"-mllpw h, 1.1 '11 Cl
i
., v
iv", tilt I I'mi, salmo
ly1drollit-A sit fgjavi4 I..A.. "'-d
val'itir, g-thit'.. V-:1. it ..to-ttv. Attlilit, tism,talm lill'i
,0.), 111mr1j. wof It J~ A- o)-it"I m s.,twinx
att its, ill ow'. OplwA limprillt,~
I.7?U; 1 .585 to 1.610. The is invu.
ifiriml fmin colirriv mplac"t hoorm-s- Typt.
Vill ittr %%fill a I'villi'lillaill ill 111V
-ot". "od 'holld.11mind 111111111c m0al, fillifix lilt- vat-1
um I'lle %as fiallic-if I'll, ir'vrv~m. of -,It .... I
sedill)"ll. "If 1-ts"'A i ...... . M.'s"Ir
at hi,-ul-natte ~oh- Ow Few- am- dmtinel fir,mich
41-oll.11. sul ... tarim- dialusw m1k xid lulls, AlIkab". Cat).
Slits. wed Aljtl~ ~%ci, gii-allv s,-m-,vtd bv iti,
but .. pairs .4 Fr -' I'v ... obill'A lilt Sl(s, and
w A,tot the am-ific Othnow. flo- ..r,- ppui. o.t.
Jdat'ren '11,111mi, nal's-1 ... I- .
thid. 72, -Is 7;1~ 1114S). :;nsitlat rimolitunt, m, A.-tv-1 o,
flir fratioitilm hom Molifir fit 111111VT Drvolli'lls of tilt %% .
'111.1 S. Viral, "tilt lite ("Itmilimi if g'. 111111, dil-
fill, V..'" hi4iii-kil Hplihi 1. twO

Mspesjujn.iron micaj, 1). 1!, ,;"0yjjEhcnku. Zapiiks
Vj,s.yus. Minfral. Objk'Aestm~017611. ;ik.-'rdsi5w minskral.)
so. 17!j,-81(1951 ); cf. &rflyucheniscs. C.A. 44. 491i.-
Phl.,ji"Pite f1mo A karn all the ilitilte,fiate contact Of see-
pentiuite with 4 younw grAllite. in Ow Aley of the river
FrT Cro.
(~') ji..Ze hou: Tals) wt IW*Wbij
Laity i4 strongly pltvo hroir; -Y ~ red-browsi: n ~ nearly
counir"Vellowi.h. Ilse (h'al, cosiff"ll.: W.-,t-Vq&,.CjWW-
Ba.*)(Al..r,Till1 Fr"' Olit, .,L4.w) (Sis-ce,
". 7
Al...Oo.u) (0If1-4jl--..j* j.1) FtOlll the ~%I%ir IOCA-litY. a
phlogispits: is licsscribetl from granile,"plite cutting through
the -"pentinite with 2V attout W. stele ch.srActer. AtrotsX
plefichrolsol; -1 ~ brourl, .1 light-re-How; -V - 1.60110 :L
11,19r-1; A - J,fA15 iz ).(Nr-,; 1.5113 ~* 0.1XV; I-, - *
Ofs,37. The rhism. ctmilm.~ Fell$
(4 Ilicstilc L A~ns].W lit grillor Imsy) SAilli4j), with
12 wt. % of this mitterill. Atid is u(trit 1111tictown -sib
inu4mvite and changed its chlorite, r1wiftic, anti rutile.
The genctsis of this biotite evidently extended over a rather
long-time period anti temp. range.' this was Indicated by
the early rMin, of plagioclase anti the final forystation of
aticrocline surrounding the biatite. 'Mrse micas of-
different ax" behave aL%o very differently after having
hern calcined at -AW; 2V is much incrva~ed. the refrac-
tive intlexel are higher. file dispersion of the axes are very
Oftnif with P < P. the I-M) content is mrssitlembly re-
-lumi.stn,illeAismllcllincrca%t4l. The-Amerhantrio(the
optical chatructerislics have been observes) by Melimel (CA.
31.4-3651)inwedtheringofbietite. neplemistroicaumles
in the biotitcz disappear at apatite and small
trains of pyrite ure included lit the mica. Thechem.conipts..
,fter deduction of thce cottraninations): M.Nao.10
(Mg.-Fe" ' 'Mrs" "' Lls*w) (Sit.nAll.sr,
114"USC 01 the presence of R'" Imssile
It" in the octahedral laren of the structure. the author
i~ of the opinion that these bissstit~ from S. Timan are -
inirrinmliatebetwertn muscovileand phlogopite. like"mal-
devite.- The defects in the surn Oil- + F- which should
be 2 are exp"cd by an exchange of the anions :X01-1) - "
()I-. W. Filet

Chlorites fro'n skams Of the Antary Basin.
4ttijitriki; mil I . S. ClarknY. Poklady.lkad. Nauk S.S.-
.5-H. SO.-MI L'f '1951).-1l3 contact-trictamullatic limc-
%ttivies and doluinites of Silurian and Cambrian age. chlorite
i% Ablind.tnt. av"Nl. with typical skarn niinefAls,,ts pyrox.
;111~1 gartict. rphlote. and yuunXcr hydruthri-mal inagne-
itcand calcite. Sometimes, the chlorite is inttTgrOWU with
phlogopite. the genetic relation of this mica to chloritc,
however, is not known; tile phase hotindities ate sharp.
Getwilly the paragellexis of chlorite "ith tuagnetit, And
calcite is youngrt thAll tile I'Volt"Ic-I(Attlet AAms. Nott-
tronite in foliAtcti aggregates is sporadically x%soctl. with the
ctilorites. Two analyses of chlovitcs show their very low
etaitent in FcO and Fet0s, while MO. AIA. an.] Si(h are
high; tile Fe is C011C.I. in tile M3~Wd. mainctitc. The min-
cral hj- -, - 1.670; a - I.W. the intettermcc "tws arc
normal, 21 Vis very small. optical ch.irucirr pt- (tilit"pt)nd-
iiigtul)tur,?tlt)titc-tvruij(tulibilitc). Thrifillcrentialthcrinal
curve shows endothcrTnic effects at 51,0-~W (strong). 7(W
(weak). W.Nf-8rj0' (rathcr strong), and at' exOtherrillc re'
action at 910 to lj;R)*. corresponding to the crystit. of forsict-
itc. The effects at 140 to 171?* which arc characteristic for
fCrTtlgillUUS ChlA)fitC3 Of stdillientary origin are entirely
absent. W. End

SERDYUCFEMIKO, D P
SERDYUGHM-0, D P
KPLIDRITY, IKH KHD-ICHFFSFAYA KONSTITITTSIYA I KU.SSlFIKATSIYA (CF.LOPITES, TFEIP,
Ch--FI'ICPL STRUCTURE AND CUSSIFICATIOIT) ITSKVA, IZD-VO AFAUVII MAUK SSSR, 1953.
337 P. ILLUS., DIAGRS., TABLES. (TPUDY INSTITLITA GEOIOGICHESKM NAUK. Y-,IIWAL.NOGO-
GEOKHEI-'ICFESKAY-A SERIYA, Iry-P. 140 (110. 14)) "LITERATURP: P. 331-038)
N15
622.1
.s48

9"Magnon u-
m. pii~~Iysttc,; w1 ottiir montmorillow
mine-mls from jurassiesediments of the nortbern Caucasus.
V
%,~Faj-.7Akad.
-43
2F
f
T
M
MOT
1
-
.
W."Ike-
. C-
00-22(1953); c
A
- .
"On the basis of the rolep(Si"'in thetetrahedralcoOrdinatiou
i,gr(3UI - minerals, S. hai Eimri a classi-
ps of lay&m~structuri.

,;

fication of the miftervibi of the montmorillanitt group, in ,
r

ith 4,
which'are distiji6islied-ino~tinorill6izites.0 v.
.-'3 8 Si Ions per. formula unit; beW Ilit&, 3.8-3.6 Si.-
-
ions; saponites, With 4-6-3-4 Si ioni; and,parahulloysit
n -, . .. .
:f,
.-Mith 3-4-2.1 Si,ions V~r structural unit- lit the wemth
idkii rek-ion es-
pltr;ibasic serpentinitm mim-Af of the River M.
ped--illy in the valleys of River %I:LJka, Gedmyshkli, Ta
z.
Kol, and Rkhy-Kt)l, of. lowrr jurnssic ate, slates and claye]
'
schl cwl Scams, and
i~,tcd with:siderite,
ists Occur-iu*

j;j6bicrv&J grren-wlarcd sr-called "non-
There ar
gyps
'
conchoic U-
tronitea often H ~filiqiomiuctalic- kvz,,rs, wijh
fracture. The B dark-grew, fine scil),
-
-58?~ weakly
:tvith -y -. 1.579; - fl!~=i 1:51t,I: or -:1 558;. 2V.
..Pleochroic. The clicri. aimly:65 corrmiouds to the for-
.,4rL-:
wlitch is a Mg para-

The diffei-enti.1-thcruisl.
hall,)ysite, r lated to- s:
e

7:
curve shows eneothcrinic c(lccts:at-DO~-l50, 500-670 and.
~~810-440',and an exothermic tfiect a- 870-8
bright-greau nontroalte sl:owq',-t- strunj pleochroism, .1
*62, 2 V
I.W, p - LM2, L!, - -57 The aggregate.
Y hat opfically,
nfthisminerelisfinescal nitd,;Owelt!mentedtl
'
'
-
l
r
l
Th
h
h
re-
-
co
e c
zn.
compn.
a
aves like a ruanocryq
it be
'
Grin
S to the Ulm
~Spgnd

is ail tvi!lt it montinorillonitic
Fe Mg para]

-d
g
ggg~!,~
differentW-thermd cmirw (the "otherink,peal fsl~t t,
A dark4rv noacroilite-., but of We3.
en L pleochroism" "UTA
4 "