SCIENTIFIC ABSTRACT RAVICH, M.B. - RAVICH, M.I.

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• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R001444330005-7
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: January 3, 2017
• Document Release Date: August 1, 2000
• Sequence Number: 5
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT


S/170/62/005/901/002/013
B104/BI02
AUTHORS: Khitrin, L. N., RavIch M. B., Kotova, L. L.
TITLE. Methods and results of a study of the kinetic characteristics
of combustion of powdery fuel in a flow
PERIODICAL; Inzhenerno-fizicheskiy zhurnal, v. 5, no. 1, 1962, 7-12
TEXT: Adev. ce designed for studying the combustion of powdery fuel in a
flow under isothermal conditions is described. Its main part is a
gas
vertical,electrically heated# stainless steel reaction tube of 600 mm
length and 8 mm inner diameter. :A screw conveyer transports fuel from a
bunker into the tube and at the same time air or a nitrogen oxygen
mixture is blownthrough. The mixture is heated to a certain temperature
in the tube (Maximum 7500C). The ratio between the oxygen used in the
flow during the experiment and the theoretically necessary value:amounted
to 0-035-OolO. A section of 500 mm of the reaction tube could be
investigated. Gas samples, were taken at the end of the tube. The
condi~tions for sufficient mixing of the gas flow with fuel particles~and
also :the isothermal reaction. conditions in the tube were studied in
Card:1/2

S/170/62/005/001/002i"013
Methods and results of a study of ... B104/B102
preliminary tests. Nearly isothermal burning conditions were reached with
5 9 of fuel per standard liter. The following types of fuel havebeen.
investigated- peat coke, coke of Moscow coal, anthracite and oil shale
coke residue. The activity of the fuels investigated was mainly a function
of temperature and duration of coking. The tests were limited to materials
produced by the following two methods., 1) 6-hr coking at 6000C with.
exclusion of air; 2) 6-hr coking.at 8000C with exclusion of air. The
content of 0 CO and CO was determined from gas samples. The results
2 2
show that during the reaction of oxygen with fuel complex so rption:processes~
take place, which will have to be studied more closely before the burning
processes can be calculated. There are 4 figures and 12 references.
-10 Soviet and 2 non-Soviet. The two references to English-language
publications road-as follows: Rhead T.-.E.' and 'N'heeler R. V. Journ. Chem-..
Soc.j 21, 2178, 1910; 21, 1140, 1911; 1U, 461, 1210i 1913; Lambert.
Trans. Faraday Soc.., XXXII,. part 2, 452, 1936.
ASSOCIATION: Energeticheskiy,institut im. G. M. KrzhizhanoVskogotg. Moskva
(Institute of Power Engineering imeniG. M.Krzhizhanovskiyo
Moscow)
SUBMITTED~ July 8, 1961
Card 2

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I
ATLASOV. I.P.; DEMOKIDOV. K.K.; DIBNER, V.D.; EGIAZAROY. B.Kh.-. IVANOVA,

P -I I e, / '/'~\ (~I-
J
2o-6-34/48
AUTHOR: Ravich, AI.G. , Solov'yev, D.S.,
TITLE: New Data on the Geological Structure of tho Banger Oajis in
the East Antarctic (Novyye dannyye o geolocicheskon stroyenii
oazisa Bangera v Vostochnoy Antarktide)
PERIODICALt Doklady Ikademii It 5, Nr 6 PP 11117 -1180
aitk SSSR,~ 1957, Vol- 11
(USSR)

ABSTRACTs ~In the course of the antarctic a urin e r19,
the authors
made a geological survey (1 100 000) Of the oasis and its,
environment. Thereby the characterization o f a large part of
the archaean cross section (visible thicknoss not be 1 o w12
km) of the East Antarctic is Liade possible
. The first, data of
.
the discoverer (Banger 1947) and others by Vyalov and Voronov
(1956) were'very poor..By the data won by the authors the con-
ceptions on the Pro-Cambrian of this region are fundamentally
changed. The Banger oasis, together with the i8lands to the
north situated in front of it I lies between 65 50' - 660201
3outh latitude and 100030, - 101,701 east longitude. The
archipelago iu connected with the mainland by Shakletor)ls
2
C r,I 4 shelf-glacier The rea of the 350
km
a archipelago is about.

20-6-34/48
Ifew Data on t1io Gooloocal Structure of the Banger Oauifj In tfie t;nat j'intare-
tic
200 km of thouo being,occupied by the islani 1 e.
the Banger oani a- 40 km fac in 04e JOLAUW~s~lt a eMt(t[i (if
rocky volcance3 riaes out of tho glacier, utjtratud from eA,;h
0t er. by ice-clap3. Thia group foras a neg r, a u i a ('~' ()o U t
m developing right now and ia called 110bruchu,t by
k
the authors. The not high (100 - 150 M) vc,1c'kf1oez1 of the
Banger oasis are separated by narrow valleys filled by morai-
nes. The boulders predominantly come from the local ra-z~-a,
butexotic ones that chiefly consint of Rapakivi-Cranite not
seldom.occur. Only in the southwestern part of the oasis the
valleys are wide, filled by~loooeaediments and utirround-id
by flat (60 - 70 m high) hills. In them lie chains of small
lakes. The only large lake, "Fig-urnoye", more thani 210 ~~su long,
lies along a comparatively youn- thick bre-Ak. All Corn-j of
here caused by the action of vol,,a-
noes are formed in a row according to Lite j,
whereas the valleys between them run tlonC tne
tonic faults. The summer in this region lasts fror, tfia tie-
ginning of December to.the end of Februar hen ti e air ten-
ca r a ay varies between +1 an
d 2/4 per ture by d d 16 C band the blanket,

2o-6-34/48
I T~!fDa ta on the Geological Structure of the BanC;er Oasis in tne bast An-,a,rc*._-;c
of snow is absent. It is: also at other seasons that the sno,w, in
spite of very low temperaturesbelow zero, is blown away here. Due
to an extreme.d of the air, precipitations are very rare
ryness
and in summer occur hardly atall. The:region is to be considered
as "cold stone-desert". Only archaean rocks participate in its
geological structures various crystalline schists and gneisses
mostly intensively maematized, metamorphosed basic magma-rocks,
and intrusions of pyroxene-granites (-charnokites). The archaean
complex is intersected by dolerite-dikes of apparently early-
inesozoic age. Quartary sediments have alconaiderable developmenlt~
and are represented by glacial- and fluvioglacial formations. Th6~-_
tectonics of the region is extremely complicated, as the numerous..~--
faults destroyed the early plicative structures. The above-men-
tioned rocks are classified in 3 families and'a preliminary li-
thologic-mineralogical description of them is given till their
study will beconcluded. The magmatization took place in 2 stageS11:1
they are characterized by a different composition of the injec-
tion-m4terial. Pegmatite- and quartz-veins which accompany the
magmatites mostly have an intersecting character, usually in a
flat angle to the containing schists. The thickness of the veins-',...,-
Pard 3/4 is quite different, mostly it is 3 m. It: can be follovied. ove,r,,,

VAKAH, V.A.; GRAMNIM, I.S.
Concerning A.H.Daminova'g articln "More on the age of the
crystalline Rchist co lei in the Trqmir Paninsulan (Sovetakaia
FOologilft,ll no.6, 19~,87. Inform.biul.NIIG& no-11-M-80
'513. (KIRA j2:6)
(Taymir Peninsula-Schiats)

jow"m 26-

Pre - SOV/11-59-3-2/17
Late/Cambrian Deposits of the Amundsen and Sandau Mountains on
Queen Mary Land in the Eastern Antarctic
who systematically described the lamin*ar cross~sect-
:ion of the terrigenous.rock stratum and a.total~of
70 samples weretaken.-Ihecollected materialwas.
examined by the Nauchno-issledovateliskiy :Institut
geologii Arktiki (Scientific Research Institute Of
..Arctic, Geology)., The petrographic description~of
rock was handled by M G. Ravich with the assistance.
of Ye.M. Orlenko. A complete silicate analysis on
the green schist of the Sandau mountain was made by
A,Z.Shpjndjej-. The absolute age was determined at
the Laboratoriyalgeologii dokembriya All SSSR (Labo-
ratory of Geology of the Pre-Cambrian.Period, AS
USSR) under the direction of E.K..Gerling. Orographic.,"'--
ally, the Amundsen and the Sandau,mountains represent,
typical nunataks the first one being 50 m., the'other
150 m, above the ite shield of the Antarctica (Fi es,,~..
2 and 5). The absolute height of the Amund.,,en. mo,un-.
tain is 1,445 m and that of the Sandau mountain
Card 215 1,380m. Judging from,.the configuration of ice,cracks,

S07111-59-3-2117
Lalt;e/Carabrian Deposits of the Amundsen and Sandau Mountains-on
queen 1.1"lary Land-in the Eastern Antarctic
the Sandau mountain is circumflown from SW by. an ice
stream heading NVI. This ice stream,is located,app Irox i-
-5 km from the mountain,summit-0 An analogous:.~:~._
mately 1,
stream circumflows the Amundsen mountain from the S,
and SE. This- ice stream is about 2 km away 'from the
Amundsen mountain peak. A-petrographic sItudy of these.,:,-
2 mountains disclosed that the metamorphic rock could'.
be classified into 5 principal groups: 1) meta=~phic:'~
converted into epidotic-chlorite slates'
with quartz-epidotic and chloritic veins; 2) meta-
morphic quartz conglomerates; 3) various metamorphicI'~%,:',',,.,,
quartz-feldspathic and quartz sandstones in-place.s. I
resembling quartzites; 4) metamorphic aleurolites:
and argillites; 5).sericitic slatds*-. These 56roups
are fully dealt withi The authors conclude that
comparing the metamorphic terrigenous.mountains.rundei?'
discussion for composition, geological-' status 'and '':I'-,
character of metamorphism with rock series in-Siberia,
Card 3/5 it may be assumed that the most probable' time of their

SOV/i I P",
IJ
Late/Cambrian Deposits of the Amundsen and Sandau
-'ucen Mary Land in the Eastern Antarctic
formation was the lato Prc-C--nbrian nclriad. Th.~;
slates of the Sandau mountain may be identiGal i.-.
the green slate formation on the Tarmyr
number of regions in EasternSiberia, o n t; h
Peninsula.and in Kareliya. In all these regdo~*,;;,
green slate formation is considered to
the Proterozoic period. The same holds truo for tlii,
green slate deposited in the Sandau mountain. P,,3-
mitic sediments are prevalent inthe composition r)
terrigenous deposits, whereas psephitic aleuropelit.-T-o'
ments are'less developed., Judging from the 1-it"11,Q-1
logical peculiarities-of metamorphic terrigenous roc-th,
the elastic material was deposited by water
and partly by wind under conditions of a littnr~11-
continental environment. There are 4 phot Lla-'.;phZil U..
map,, 2 sketches and 2 references, 1 of which S'o v _i
Card 4/5' and 1 English.

TICJS Chronicle. The 711t Session of tLa Camatestan far %he
D%t6rWZ4sttQ4 Or it* A114016te Age of Sootogical Pareatlone
(at %h. Oldol.Aiy. d.ologo-doodroticb-aikh -U LS 3322
(Departaost of Goological-eAveraph%c6l 3ateacos AS 9311).
May Is - Zz. 1959. Masao.)
P3210DICALt - 363 USSR)
rockhtzlya, 1959, Ir 60 Vp 367
Awn"a..; ,
12w O%h "gultar total= of %oW 'Comalsotom an the Dotors'Lax%tan
of the Aboolat- AA- of 0-ala&-ical ftrwo*1=0 was WA 1A X.-
from My to 9. May 22. 1959 as the 14~11tut j#*kh1x1l I Ads.
ILtLokeekof khtalL to. 1. 1. Ttraal.koco (Institute of Ga.-
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St
ry an' Analytical Chemistry Los&& T. 1. T.r-J.k1Y).
t.
or 4 of .Laing report. ... 4.14 as .44
:
I* tho seat Important part-f the'asss. n1A& or. tob.
%be ale% za%oractioaal. laeoloateal Coheres*. The
folloolaff reports as-awswarms4k
A. W. Polk"ovi 2. 9. UIrElLin - Prabitas of in. alk.olus. Ad. Of
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card 9/4
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Croup* *7 ol the r7clas of the .74ra n4-ffi-
U.1T'4bqal.t6 age.
4. w. Twer&4o.. A. 1. and
K:
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S. Z. -711.11 k.
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I To. 3tarik. 4~1.-Lrylo'. 0. The
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Per
a. To. trylo'l 'flaa age of %he razits of the V-6tr.l.-
--l-4aW had %he ea0loy"r.7, Of ttAo argon sotho4L for
Ty"
6
metaxorphouo and oodia.4tary rocas, 2~
0 ""hr'ay fornstions of &as
UkA..'r" 1, , "*A
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card 214 L. xr..w And X. . P.1-vas Ab#*Ia%. ~ag. at %a-ah.tlo
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Abooluz. go at tft.'gTaxit. tatrualoss of
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?be -search vark of 0 .,6.r at utai.%arts.
U4xD#'VS=. " 'IYAJ. site 4"asad C-t attention,
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the woop"11.41st'. research watt 4"ri.4 out by the -street-
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r A& D.W%L"ItOa or t29. "44-44f act-Rat a of the 4a-
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reeks so. 41.0--44 JLA-15-3=~21 Prove& is . r.ror% two
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.
AUTHORS: Starik, I. Te., Corresponding Member SOV/20-126-1-39/62,
AS USSR,,Ravieh,-M. G_,, Krylov, A. Ya.,
Silin, Yu. ~I.
TITLE: On the Absolute Age of the Rocks of the East-Antarctic Platform''',
(Ob absolyutnom vozraste porod Vostochno-Antarkticheikoy plat-..
form
y
PERIODICAL: Doklady Akademii nauk SSSR, 1959P Vol 12 6t Hr 1, pp 14 6
(USSR)
ABSTRACT: in the present paper the-first determination results ofthe
rocks mentioned in the, -Litle, mainly of Precambrian age I a"e
~7
discussed. For this PlIrP63e the collection of.the Sovetskaya:
antarkticheakdyalekspeditsiya (Soviet Antarctic Expedition)
1956-58 was used. It was collected during the prospecting of
coastal strip of almost 5000 km length (Refajg2). The invest-
i6ated region has the structure of a 3-stage platea-a-which.is-,1-
in many a respect analogous to the other Gcidvinskiye pl~atfortmp.,
All three.3tages are characterized in short. No Mesozoic.so-di-
'
:
11.1
1:
ments have hitherto been found in the.region of the mentioned
plateau..Conozoic sediments are only represented~by covers: f
Card 1/4 basic effusives among wbidh, leucite basalts predominate..The,_

Onthe Absolute Age of the Rocks of the East-Lntarctlc SOY/20-126-1-39/62
Platform
first 40 determinations of the absolute age by means of the::''i
argon method made more precise ideas possible.concernin'g the,,,`~.:
structure.of the aforesaid plateau. Several results were~sur-_
prising and their geological interpretation meets wli.th~,sarivua
dif"ficulties (Table 1). The highostage i. a. 1020-1270 nil
lion years . were obtained at first for the oases. Langeneset,,_
Grivaon, Bangor, and Obruchev, i. e. for leucocratic granites:~,
and pegmatites. The age of the weakly migmatitic (Banaer~ oasis,
andother regions of the crystalline basement) ro-.ks.fluctuates
between 949 and 1050 million years. So-called poly-Migmatites
which are 700-730 million years old occur at the same'time:at-
several placesi especially in the Barger oasis. Thus two mic=a_
titization staCes-can be separated: a) an earlier, one which'-,.
occurred more than 1000 -million years ago, and b) a late" bne
more than '00 million years aeo.. Thus the migmati.-za. on.of
the oldest masses of the eastern Antarctic belongsAo,,the Pro-
terozoic. A packet of gneisses in the region of the Eirlsvort
bay:and the Villson elevation is for the time being theonly
1425-
exception. Weakly migmatitized,biotite-gneiss'es are here
Card 2/4 485 million years old. This agrees almost with the age of the

solute Age of -the, Rocks of the Eaet-Intarct 126-1-39/6211~~
On the Ab
Platform
here occurring-porphyroblas tic:(;raniteo. The age of the green.
la
chint3 and n1ca phyllites (middle 0.4ge of the !p tdaii).11110__
tuates betiveen 400 and 500 milliwyears, Thiu corrasponds t~
Sinisian and Lover Cambriani The Rapakivi granites in the I Px-~Zl_
on L e
treme east of the irvestigated regi has approx.-mately 'h
t recent granitoids are the subalkslin44 bio
same age, The mos
tite-hornblende varieties. They are CaledGnian, w�th-. 3,n age Uf'.
305-315 million yearz. Thaags~of-the gabbro-dolerite fromia
stratiform intrus~o" within the Bikon (Beakon) series'(170
million years old.) agrees x-ather well with the geological po..
se of Telrtli-~
Lower Triassic). The same holds in the ca
y
ary leucite-granite (mountain Gauss) which is approxiria.tei
20 million years old. The age determinations:of the mezit!' 4d-
~n
rocks confirm on the whole the authors' assumption corcerning
the 3-stage structure of the plateau. The, bid 11.e.rling constar.+
xk 7 6.02010- 11 year- 1 WhIch is much,used In the USSR,,Was ~1.xsIed
for the determination. The data are only temporary and prcl-ably
,card 3/4

3(5) SOV/2o-128-1 -,j !/56
AUTHOR: Ravich, Y. G.
TITLE - A Short Information7on the Geologic Structure of the East~ern
Mountains in Queen Maud's Land, East Antarctica
PERIODICAL: Doklady Akademii nauk SSSR, 1959, Vol 128, Nr.1,
pp 152 155 (USSR)
ABSTRAM In February 1959 a group of collaborators tit the Institu
geologii Arktiki (Institute of the Geology of Antarctic

investig e
ated the eastern part of the mountains of Qu en
0
IMaud's Land between 9 2511 and 1803'
71 eastern longitude an
..
71 - 720'southprn Istitude in an extension of,133o km as,
as the oasis Shirmakher at the point of contact between~:Ia'nd'
ice and.shelf Ice. The present paper is based upon the material.
I ly various
collected by L. V. Klimov and D. S. Solov1yev, Main,
gneisses and crystalline schists of the granulite 'nega live
facies of the.regional metamorphism takepart in the 8e ollesi-
cal fort.ation of.,the mountains investigated. All these'.'rocks
are assured to belong to early pre-Cambrian on the strergt'-.hl~.
of-Bast'~
of the similarity of thebetter Investigated regions

Card 1/3 ,
,
Antarctic where crystalline schists and gneisses form the:..

A Short Infor.-_,at ion on tFe Geclo8ii~ Str_cturc of ti-le B ~Dv2 a -3
Eastern 11,11ountai_.ns in :~ueeri Maud's Land, East. 'Antarctica
crystallire foundation of the East,Antarctio plateau, At
some places massifs of.porrhyritic granitoids as well as,
veins of various fine-grained graritoids art, disce~vf_xed -C h i d; h.
a re
apparertly youn,3er th3n gn~,isses. Sporadical dolerite dikee,
occur as well. hrraticound s0inters of porphyritlo grarl~--_
toids and their voin facits a3 well as gneissea and crjys t i Ill, ine'
schists predomiinate among the numcrc~,as mornine-like --jaster.,.:
narj deposits. Crystalline schisvs and gneisses can be dil-:~,,,,
vided into at least 5 esPecially widely distributed groups:
1).Crystalline pyroxene-schists, and plagiognelases 2) garnk-
biotite, rare garnet sillir-anite-biotite gneisses granu
lit~,s with pyroxcre sr garnet 4) airphibiolites
cslciphyrer~, and diopside rocks. The rock species giver.',2
a re
described, as well as the rules gcverninC~, the geoloegical
structure of the region investigated, Rich graphite inseti....,
in calciphyres and in single,pegmatite veins are for, the~~t*..Lle
being the only finds. There arei however, indications that-
4 J;
IWI S C 0
vite-,phlogopite-, iron ore- and~,boron-conta r ng
mineral depo its will be found. The low degreei of trans f OL r=s
S1
Card:2/3 tion of the rocks in migmatite seems to be extre f -e
ziely o r a 0

. . . , rw~ujvld,~~qK,~--, 431-ifm- X - - -1 ---- ---
-:,~

R
I
AUCII, M.G., doktor geol.-mluer.nattk; KRYLOV, A.Ta., nauchny-I sotrudnik

RAVICH, M.G., doktor geol.-mineral.nauk; KRYWV, A.Ta., nauchnyy Botrudnik

KRYLOV, A.Ta ; SILIN, Yu-I'; ATRASHW
STARIK, I.Ye.;-ILTICH, I IOK, L.Ya.:

DZEVANSKIY, Yu.K.; DODIN, A.L.; FONIKOV, A.Z.; KRASHYY, L.I.;
"Wl'K0VSKIY, V.K.; ?.'OSFKIN, MI.; LYATSKIY, V.B.;
'IKOLISKAYA, I.P SALO?, L.1 SAZUZJ, S.A.; RAMIS,
A~
M.1 lj~~VICH~ M.G.; POSPELDV, A.G.; NIKOLAYEV, A.A.;
ILI iN,A. V. ; _BUZIKOVt I. P. ; MASLENNIKOV, V. A. ; NEYELOV,
MI.; NIFITINAVL.P.; NIKOLAYEV, V.A.[deceased); OBRUCHEV,
S.V.; SAVELIYEV A.A.; SEDOVA, I.S.; SUDOVIKOV, N.G.;
KHILITOVA, V.Ya NAGIRINA, M.S.; SHEYM-1ANN, Yu.14.;
KlJZNETSOV V.A.; KIJ.ZNETSOV, YU.A.; BORUKAYEV, R.A.;
LYAPICHEVI G.F.; NALIVKIN, D.V., glav. red.; VERESHCRAGIN
V.11., zam. glav. red.; WNNER, V.V., zam. glav. red.;
OVECHKIN, N.K., zam. glav. red.[decessed]; SOKOIDV, B.S.p
red.; SHANTSER, Ye.v., red.; MQDZALEVSKAYA, Ye.A., red.;
p
CHUGAYEVA, M.N., red.; GRDSSGEYM, V.A., red.; KELLEd,B.M.,
red.; KIPARISSOVA, L.D., red.; KDRDBKOVg M.A , red.;
KRASNOV' I.I., red.; KRYI-IGGLITS, T.Ya., red:; LIBROVICH,
1'.S., red.; LIKHAREV B.K., red.; LUPPOV, N P., red.;
~NIKIFORDVA, 0.1., red.; POLKANOV, A A. red:(deceft'sed];
RENGARTENA, V.P... red.; STEPANOV, D.L,pred.;
CHERNYSHEVA, N.Ye.;,red.,- SHATSKIY, N.S., red.fdeceaaed];
EBERZIN,,A.G., red.; Sf'IFJlOVA) Z.A.p red.izd-va; GUROVA,
O.A., tekhn. red.
[Stratigraphy of the U.S.S.R. in fourteen voltunes. Lower
Pre-Cambrian] Stratigraflia SSSR v chetynindtsa ti ~ to-MAkh.,
Nizhidi Dokiibrii Moskva Nguchn~~tokhh ltd-4~ ~lit_ry'po'goologii
okhrone nedre: Pt*' 1,~ (Asiatic pait of the USSR~ 19630' '396P.

RAVICH, M.G.; ELP-AVI, L.V.; SOILOV111V, D.S.; Jukt,(x
geol.-mineral. nauk, red.
[Pre-Cambrian of eastern Antarctica.) Vokembril Vostochncl Antarktidy.
Moskva, Nedra, 1965 469 p. (Leningrad. Nauclino-issledovatellskii
institut geologli Arktiki. Trudy, vol. 138)
(MIRA IS: 5),

T, o8koa-6?, nq-i(i) wvulaw
ACC NR, A'17001653 CODE:- _U Rfii~l~/66/000/057/0028/0042
7; AUTHOR. Wtvich,.M. G. (Doctor of geomineralogical.sciencee)
~IORG: Scientific Research Institute of Arctkq~~ology (Mauchno;-iseledovateltakiy
i instituit ge'ologii Arktil 1
~~''-TITLE.- Geological structure of Antarctica
SOURCE: Sovetskaya antarkticheskaya ekspeditsiyag 1955-o Informatsionnyy,byulletents
V. 57, 1966, 28-m42
TOPIC TAGS: petrology, geology
ABSTRACT: This is, a review of Soviet geological investigations in Antarctica,,.
during,tho last ten years, accompanied by some information on foreign
arch there. A largo.fold-;-out map accompanying.the text shows
the
geological features of-the entire.continent as now known (19 forms~of
symbolization are used) 0 7he Soviet work has been exclusiveirin East-
ern Antarctica. In nine~years Soviet geolo Iists have investi ated ,31
9 -, .9
coastal sectors between 9,.and 165o E'(a distance',of moreUan'.8,000.
1m),:23 of them never before visited bygO010gi5t3o: The mostImp,ortant
of tho 'earlier uninvestigit~d ~areas are i the central Fart,'of Queen
Maud Land,.~ an area of 50,00D scpare kilometers now mappe dat 1:1,, 000,000-~
aiderby land,, an area of-50,0W square- Ore. ~map;*d at:
kilmet
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ethod3 (cf. C.A. 44, 9232c;rl4S, 4125b). - The vapor prc3-
Sure of said solns of N-Cl '. to a max. of 401 kg.j
cm. at 6W', and then falls to 0 at M* (m.p. of NaC
When enough NsSO, is addedto the NaCl, a 2nd max.
a
t a lower temp., defining a region where NarSOj Is
th tid phase.~ This'2nd max. rises and the former-
diminishes with increasingNaS0. cot*n,. Whenthteutec.,
1 CheMetry tic ruixt.'(70%, N&tSO,-30% NsCI) Is reached, the NmSO#
curve Is almost inperimposed on the curve for the vapor pres-
sure of pure water. Approx. values for 4% NarSO,' pressure
(in kj./3q. cm.), and A man.. and pres-
temp. of the Nal!
sure and temp. of the NaCl max. are, res&4,0, 401
OW :i 20, 350. 6W; 35. 160, 375, M; 50, 320:
I W
430,250, WO; 70 (eutectic), 2250 5W (n data
en for the N&,SO, max. at eutectic cati -p
..-P
"Il.grant for theternary system Is pre=ct'V-1n'-tr..11 I
n;J
for m, an(I is baml on previously published data (cf., C.,
C Im
26,- 1 5W; 29. 77701; 36, lWi 1). A tern Cutectic M, I
contains approx. 5%'N'n:SOj' 0., NOT
1, 70 HOO,
-Mld 1, Nfiller-

P., . I .

A=Lch,
j
fsowbd~ an Ts

ry 20 re PMUUIUULiltpotw
=
a
$m0, s'~
' an suffsts at hich temparstates. MA L Ra
E B I t
Sat
d P
~M
an
.
.
-A
-The sys by the method aWf,,'~nd
.48Me tem studied
, C
f
A
7
6W
t
e
P-1, curv
.
.
) at
s (c
amw up to As
-W.
9
,
'
k'W
th
th
t
f
u
i
-
emp;fw. P-vapq pressum
ll
n
ilt.
e
e
.0
first
d th
d
70-
t
I
a
d;
Tb
ncreasm 0 a max.
n
en
ecrease
c m=4
~
- w
t 400-4200
v
:
k
s ob
i
d
Thi
h
u
s
r
e
a
s
6w*.
t
gA. cm.;
posilb lty,ot keeping K and Na chlorkles and sulfates in
I ccedla tbe-crit,temp. of-H
sotn. at temps. great

the required prieutire ~'Cnxot very v oil;!
-n iaG diagrams
taine4 at 400-500! showed the c6aditions under which salts

the systern.crystd.." -::; ~ , " - ,,
'j, -o9eh 2

b
W

7, -h
KAU'.

p
:
p

N
9 ..--7uVT

KUM..
WM#3 IF -ATWjo~
54r tAk ara

d. :,:-
~ ~~ ... ..:
DkgMMiulcou
,
, - " -
-
t6nditWu for
~dms t t gmwtb4
'awtht WAS of exptl.
thsiik~~G Of SoNd NICI Wd of liquld solm, formcd from
jU of the pouMla inixts. of NaCl ind-NiOH in the prtf~i~
wic of RIO vApcf,."-":

c
h

4:
.11istencei4d 9"Itibrium BUYL of
t
the system at
lC t ON Above 00

O

-AhuLMm4 ItIUM
~ NE=
-A ~Y
). of
T;
Tau
, mudllso x -my abd thermographic stU
'
~-.Of KvM.M&qM show
. that the hotherm of only. at 100'
consists of 4 biranches -nding to tile a, . of Nar
CO
H
o
N
K
d
m
M
U
,.
ai
.
t
%, an
IC.M and t6t
,
,
O
tile 190thiim of soli. at 150* CML�6t$ Of 3 bra;!Q,- corfe~
SP-cilus; to crrstn. of NatM. KvM.X&vM. and KsM.
Existeme of Y,&M.Ns.M at temos. us to 476' is con-
- -
I
- , I -t

must be,crYsW-I.
how that KzM.Nalco
' V
solmi. and at temps. below 150%', B. MAY11114