SCIENTIFIC ABSTRACT N.F. CHUKHONTSEV - F.V. CHUKHROV

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R000509110010-4
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: June 12, 2000
• Sequence Number: 10
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

CHUKHOIITSZIV,, ll.F.,.dotsent
SimpWied calcullp-tion of the cmis-section area and perimeter
of anchored mine workings. Ugoll 36 no.6:24--9-5 Je 161.
(MMA 24:7)
1. Novocheekasskiy politekhnichaskiy institut.
(I-Iinin- engineering)

AcC NRt AP6015579 (N) SOURCE CODE: UR/0146/66/009/002/0083/008.5
AUTHOR: Chakhontsev, V. M.
ORG: KuybyshevPol technic Institute
(Kuybyahevfjkiypolitekhnicheskiyinatitut)
TITLE: Realization of expo nential functions by means of
nonlinear semiconductor
resistors
SOURCE: IVUZ. Priborostroyeniye, v. 9, no. 2, 1966, 83-85
TOPIC TAGS: function generator, exponential function,
varistor/1U4"I'- A
SUL'~ r- XL&LI'4~
ABSTRACT* Formulas are deduced 'or designing varistor-type
exponential -function
n
generatorAhat implement relations lof this form: I - MU ,where
U is the input
voltage, I is the output current, M Is a factor of
proportionality. The I-V
characteristic of the varistor is corrected by connecting it in
series with a suitable
resistor. The new formulas permit determining the values of M
and the series
resistance. They were verified experimentally: a function
generator designedwith
n . 1. 7, 1. 6, 1. 5, and 1. 4 exhibited an error of only 10.
70/c ; a varistor manufacture
by the Tallin Radiotechnical Plant im, Kh. Pegel'm was used.
Orig. art. has:
1 figure and 11 formulas.
SUB CODE: 09 / SUBM DATE; Z7Apr65 / ORIG REF: 005
c
rd 1 / 1 UDC; 62
a

ZHEVNOVATYY, A.I.; Prinimall uchastiyet XHAZANOVA,
I.V.; KUZNECHENKOV, I.G.;
rHUKHQKTgL--V-.d,; SHENBERG, G.F.
Agitation flowshest in the leaching of alumina-bearing
calcine with
the use of hydracy~jones as main 'apparatuses for
separatin the pulp.
TSvet. met, 36 no.100-53 Ja 163. IMIRA 16:5)
(Leaching) (Alumina)

DUTKIN, G.S., inzh.;GHUKHOV, S.P., insh.
Preventing corrosion of reinforcements of electric
transmission
lines in a tropical climate. Energ. stroi. no.2:87-89
159
(MIRA 13:3)
1. Treat OArmsetll.
(Corrosion and anticorrosivea) (Electric cables)

DTJTKIN, G.S:!. CHMOV 5 P - GRIGORITIV, Yuje., red.;
IGLITS111, I.Lot
red tekhn.red.
(Equipment and regulations for the erection of 33 to
500 kv.
electric power transmission lines] Montazhnye
prisposobleniia
i ukazaniia po montazha provodov linii
slak-troperadachi 35 - 500 kv.
Kaskva, Goe.energ.izd-vo, 1960. 46 p. (KmA 14:1)
1. Armset2, trust, Moscow.
(Blectric lines)

DUTKIN, G.S.; ROSHCHIN, GRIGORIYEV-1 Yu#Ss, redq
PRILEPSMA, V.D.0 takhn. red.
(Electric inmaatore and accessories of 35 to 500 kvo
electric
power transmission lines] Isoliatory i armatura linii
elektropere-
dachi 35-500 kv. Moskva, 1959. 92 p, (MIRA 14:9)
1. Moscow. Naucbno-issledovatellskiy inatitut
elaktropronyahlennouti.
TSentrallnoyebyuro +,ekbnicheakoy informatsiis
(Electric 3ines-Overhead)

CUUKHOV,, S-4Pi,,inzh.; DUTKINp, G.S., inzh.
New supporting devices for electric transmissi~)n wires of
220 to
500 kv. Energ. strol. no.20:150-153 '61. (MIRA 15:1)
1. Trest "Armset"'.
(Electric lines--Overhead)

, CHUKHUY A. podpolkanik
Tactical and special training In en aviation maintenance unite
Tyl i onabs Bove Voor, Sil 21 no.9s2l-23 S 161.
(MM 240-12)
(Military education)

CIJUKHRAY . 1A..; 1111URAVIYE-VI A.I.p red,
[Generation of the--feake-sl Pokolenie besstrashnykh.
Mosk,7av Voenizdat., 1944-- 317 P. (MIRA 18:7)

CHUMYI V,
Universal power supply unit. Radio no.605-57 Je 164.
(MM 17:10)

-- ii- - - --- -
Nikollskiy, V. V., Zalesskaya, M. A., and Chukxaveva, 11.
1. "The dyramics of MI
changes and the al'bumen content .'In discharges
of.gonorrhea patients under the
influence of penicillin and sulfadin therapy", Sbornik
nauch. trudov (Rost. obl.
nauch.-iS31ed. akushersko-ginekol. in-t), Issue 8, 1948,
p. 88-94.
So: U-3261, 10 Anril 1953,(Latonis 'Zhurnal Inykh Statey,
No. 12, l(.!49(-

CHaHRAYEVA, N. M.
Chukhraveya, N, M, "An analysis of the causes of
stillbirths in the-,
delivery statinns of the cities of Rostov Oblast durinr
194711 (Author's
I
summary of the paper),,Sbornik nauch. trudov (Rost. obl.
nauch-kssled.
akushersko-ginekol. in-t), Issue 8, 1948, p. 213-14.
SO: U-3261, 10 April 1953 (letopis 'Zhurnal Inykh Statey,
No. 12, 1949).

CHUKREYEV, V.K.
- Phenological seasonality and winters in the northeastern
U.S.S.R.
Probl. Sev.' no.7:217-223 163. (HIRA 17;2)

VOWITSIM, Igor' VU4~7"ieh; IVANOV, Lev Andrianovich. Prinimal
UChaStiyejCHU L NEGRABOV, G.A.., dots., retsenzent;
MALAKHOV, K.M., mekbanik-nastavnik Dallnevostochnogo pa-
rokhodstva,, retsenzenti MM1WVAi-E.$.S red.; LAVWCVA, N.B.,
tekbn. red.
(Breakd own of internal combustion marine engines] Avarii sudo-
vykh dvigatelei vnutrennego sgoraniia. 14oskva, Izd-vo
q1orskoi transpart.." 1961. 240 p. (IMA 15:2)
(Marine engines--Maintenance and repair)

CHUMMI., L.A., inzh.;.KUZIaVA, T.M., inzh..
Brittle failure of-marine-,boilers elements,
Sudostroenie
27 n0.9:60-61 S 161. (MIRA 14:11)
(Boilers,, Marine-Corrosion)

CHUKHRINJ, L.A.,, inzho
Portable metallographic microocope. Energetik 10
no.3.16 Mr
162. (KM 15:2)
(Pipelines-Metallography)
(Mip~-Oscope)

Construction brigade of Hryhorii Rae!--huk.
Sill.bud.no.6:22-23
6 155. .(XrRA 9:7)
loStarshiy sootaklinik Ternopillskogo pblaunogo
upraylinnys sill-
skogo goopodaretva.
(Skala-Podol'Bkaya region--Construction industry-)

CMIMMM. D. P.
,,, - -iera-----Ov;"-?-~-~~~!~'-
Method of application of prolonged interrupted
conditioned
reflex aleep theraW. Khirurglia, Moskva noo4:12-18
Apr. 1952.
(CLML ?.2:2)
1. Docent. 2. Kiev.

(;HUKHRlrzl Inn I D.P.
- y::
Ifethod of propbylactic regisen and condit'.oned
reflex sloop
tberapy. 7alldsher & Akush., Moskva no- 5:39-44 May
1952,
(CLHL 22:3)
1. Docent. 2. Kiev.

GHtEMIMMO,
Organization and present state of.smergencyof surgical
servic~3 in
medical institutions of Ukraine. Sovet. sdravookhr. 11
no.2:17-2~
Mar~Lpr 1952.' (GLKL 22:1)
I*' Docent, Deputy Kinister of Public Health Ukrainian
SSR.

OMHRIYENKC; I D. -P,
"Rectrograde Invagination with Prolapse of the Sma-u
Intestine into the
Stomach, it Sov. Med.. 16, No.5, 1952

ONUMMIMKO.-, D.P.
Modico-prophylactic r men, conditioned reflex sleep
therapy
and ther&PY with. prolov4ged ptWsiological sleep in
the practice of
therapeutic in6titutions of Uluraine.-Klin. zed.,
Moskva 30 no-7:3-
9 July 1952. (CLML 22:4)
1. Docent. Deputy Minister of Public Health Ukraine
SSR. 2. Kiev.

GHUKEIRIYEKKO, D.P.
Intestinal obstruction due to ascarlasis. Ked..parazit.,
Kookwa, no.3.*
262-268 may-june 1953, (GLKL 25*.l)
1e Of the Department of ftoulty Surgery (Read -- Prof. L
Ta. Dayneka),
Vinnitea Medical Inititute.

GHU IYENKO. D.P.. dotsent.
Strangulation of intestines In openings of the mesentery,
the epiploon, and
the broad ligament; data from therapeutic institutions of
the Ukraine. Xhi-
rurgiia no.7:47-54 J1 153. (MLRA 6:9)
(Intestines--Obstructions)

comnum D.P., aoteent
Ovarian cyst and Intestinal obstruction. Akush. I gin.
no-3:49-~4
MY-Je 154. (MM 718)
1. Iz kafsdry fakulOtetakoy khirargii (zav. prof.
M.A.Zinbarovskiy)
I kafedry akuaherstva i ginakologii (zav. prof.
Ya.V.Kukoler) Dnspro-
petrovskogo meditsinskogo instituta.
(IMSTMAL OBSTRUCTION,,etiology and pathogenesis,
~ *ovarian cyst)
(OVARINS, cysts.
~compl,', intestinal.obstruct.)
(CTSTSV
*ovaries, compl., Intestinal obstruct4)

GH=IYMO. D,P., doteent (Xiyev).
*000- 1._ - -
Vestiges of the vitellins duct an a Cause of
intestinal obstruction;
according to data from Ukrainian hospitals and
clinics. Vext.khir.
74 no.2:44-49 Mr '54. MRA 7:4)
(Intestines--Obstructions) (Umbilicus)

CHUNUMM, D. P.
CHUKHRIYEW, D. P, - "Imperwability of tba intestineff
(Clinical And Exper'siental
investigation ), Dnepropetrovsk-Odessa, 1955. Chair of
General SUrPrY,
Odessa State Medical Inst imeni N. L'Pirogov; Chair of
Pharmacology and
Chair of Hospital Surgery, Dnepropetr6vsk State Medical
IRst. (Dissertation
for the degree of Doctor of Medical Sciencea).
SO. &AAh2= Le&2piel No. 46p 12 November 1955. Moscow

CHL)K0k1Y&NY,-0j
&nmwles of papers. presenUd at the XM Congre" of Surgw= of the
USSRP MaGeov., 20 - 27 jewwXy 2955" j=1U4*&
Changes in the Electric Activity of the Cerebral Cortex in Cases
of Intestinal Obstruction and a Substantiation of Methods of
Anaesthesia for
its Operative Treatment.
D. F. CHUKHRIENKO
SCURMI -4A6D13 (Offtelaa Publication) V=Iwaifted-

CHUHRIYEWC, 0 DMITRIY PAVLOVICH
CRUINUIRIYaKO, Dmitriy Favlovich (Dnepropetrovsk State Med
Inst), Academic
degree of Doctor of Medical Sciences, based on his defense,
31 October 10,55,
in the Council of the Odessa State Med Inst imeni Firogov,
of his dissertaTion
entitled: It Intestinal dbstruction (a clinical and
experimental investi.gation).11
For the Academic Degree of Doctor of Sciences.
Byulleten' Ministerstva Vysshego Ubrazovaniya SSSRp List
No.8, 14 April 1955
Dedision of higher Certification Commission Conc~rning
Academic Degrees and Titles.
JPRS 512

F.
Frcm the Russian for Dr. John F. Potter
Vestnik Akad. Med. Nauk SSSR
11 (2): 35-45; 1956
Homoplastic Transplanting of Glands of Internal
Secretion to Vascular Pedicel
by
T, E. Gnilorybov (Honorary Sci. Worker of the Ukrainian
SSR, Dnepropetrovsk)
(From tile Chair of Hospital Surgery (Head: Prof. T. E.
Gnilorybov) of the
Dnepropetrovsk Medical Institute (Dir.: D. P.
Chukhrienko, docent).)
(Article entered editorial office lo-27-55-)
Tx~.IaVdd at. rbf-- Natli'mal 11tatitutikto Gfr,
rlea~th, mary"ad
Paill trsm4l-axiou avs,119ble In

CHUXHRrn=D, D.P., -dotsent
Bffectivenses of other anesthesia in surgery of the
gastrointestinal
treat; experimental research. Khirurgiia 32
n'o.11:40-43 N '156.
(HIJU -10:3
1. Is kafedry gdopitalluoy khtrurgil, (sav. -
saalusbannyy doyatell
nauki-Prof.1jeoOntlorybov) i kafedry farmakologii (A&VO
- Prort
G.Ye*Batrak) Dnapiopetrovskogo maditBinakogo institute.
(GASUOINUSTVUL STSTEK, surg.
expers, other anesthe.)
WM,.MT*ffYL.ansoth~sta and analgesia
in experf surg. of gastrointestinal tract)

GHUKKRIYJINKO, D.P., dotoent (Dnepropetrovsk, ul.
Dzerzhinskogo d.18-a kv.28)
Methods and e??ectiveness of local nevocaine anesthesia
in surgery of
the gastrointestinal tract; experimental research [with
summary in
English. p.1581 Vest.khir. 77 no.8:18-29 Ag '56. .(KLRA
9:10)
10, Iz goopitallnoy khirurgicheskoy kliniki
rybov) 1.ka.fedry farmakologii'(sav. - prof.
petrovskogo mediteinskogo instituta.
(GASTROINUSTINAL SYSTEM,,surg.
local anesth. in dogs)
(ANESTHESIA, TOGAL, exper.
in gastrointestinal tract surg.
(saos - prof. 17eeftilo-
G.Ye..'Batrak) Dnepro-
In dogs)

USSR/Human and Animal Morphology (Normal and
Pathological). S-1
Digestive System. Digestive Tract ind GLands.
Abe Jour: Ref Zhur - Biol,,, No 19,, 195% 88329
Author Chukhriyenko;, D. P.
Inst Dnepropetrovsk Madical Institute
Title Pathologica-1.11natomy of Intestinal
Obstruction.
Orig Pub: Sb. naucbn. tr, Dneprepetr. red.
i-nt, 1957., 2.,
311-315
Abstract: A survey,, Changos in the digestive
tract are do-
U
,sc.,ibed., particularly the destructive
processes-
in the nervous apparatus of the-intestinal
wall.
etc. It is noted
manifestations of venous stasis,
that the pithonorphological, changes are loss
marked
in obs'uruction then in strangulation.
Card 1,P1_

CRUKHRIYW,O, Dmitriy Pavlovich
[Obstruction of the intestines] Neprokhodimost'
kisheahnika.
Kiyev, Goa.Med.izd-vo USSR, 1958. 428 p. (MIRI 12:2)
(INTBSTINES--OBSTRUCTIONS)

GNIIDRMV, T.Toq.: W&TIT, M.P.; POZI-ITAKOV, K. I.;
KHOlROSHXkNMW, N.Ya.;
Dmitril Averkievich Vasilanko. Nov. khir. arkh. no.2:138-139
Mr-Ap
159. (KIRA 12:7)
(VASII=, MKITRII AV= BVION, 1883-)
Q~ ,

CHUIMRIUMOv D.P.; GRINEVt M.M.
Some data on the ac#on qf muscle relaxants (ditilin,
diplacin).
Khirurgiia 35 no.9397-102 159, (MIBA 13:12)
I (MUSCLE RM,AXkMS)

CHUMMIYEMOI.-A.]P*,,;~prof*;~~,(Daepropetrovsk, u1.
&ybyeheva, d.6, kv.2)
Operative treatment of recurrent and massive forms of
recta'I pro-
lapse with the use of capron material. Yest.khir. 83
no-10'.78-83
0 '59. (KIRA 13:2)
1. Is 2-y-gospitallnoy khirurgicheskoy kliniki
(zaveduyushabiy - prof.
D.1~. Chukhriyenko) Daepropetrovskogo meditsinskogo
instituta.
(RECTUM diseases)
(NM10

AMIT&Vp A.M.., profs; BEREZOV, Ye.L., prof.; BISENKOV, N.P...
kand. med.
nauk; BRAYTSEV) V.R., prof.; DEYNBU, I.Ya.., prof.; DYSKIN,
Ye.A., kand. med, nauk KAZANSKIY, V.I., prof.; KARAVANOV,
G.G.,
prof.; LEVIN, M.M., prof.; MAKSD4MKOV, A.N.) prof.; MAYAT,
V.S.,
profs; NAPALKOVj P.N.) profs; ROZANOV, B.S.# prof.; RUSANOV,
A.A.,
prof.; RUSANOV, G.A.p kand. mod. nauk; FILATOVp A.11.., profs;
HUKHR_1ZYE~NKO D-P ~rof.; SHILOVTSEV, S.P., prof.; PETROVSKIY,
r_~
.. otv.
Bo s, pro sj otv* red.; MELIVIKOV, A.V., prof., red. toma;
SUVOROVA. T.A., dote., red.; WROWORTSEVA, K.S., red.; RULEVA,
M.S., tekhn. red,
[Multivolume ma=.al on surgery) Mnogotomnoe rukovodstvo po
khirurgii. Moskva, Medgiz. Vol.7. (Surgory of the abdominal
wall and organs of the abdominal cavity., the stomach and
intestines Khirurgiia briushnoi stenki., organov briushnoi po-
losti-zholudka i kishechnika. 196o. 746 p. (MIRA 15-3)
1. Deystvitellnyy chlen Akademii meditsinskikh nauk SSSR (for
Braytsev, Petrovskiy) Meltnikov). 2. Chlen-korress ondent
Akademii,
s
meditsinskikh nauk SSSR (for Maksimenkov) Filatov
(ABDONEN"SOMY)

CIIUKHUYEEKO, D.P#, prof. (Dbepropetrovok)
Use of Oapron tissue in surgical trmtment of uterine prolapoe,
.36 no,5174-78 8-0 160.
Akush.i gin. . ~(MIRA 13M)
(UTERUS.-SURGERY)- (NYMN)

CHEHRIMIKO,D.P., professor
Nephropexy with the aid of capron, Vestakhir. no~6010-13.1
161. (MIRA 15:1)
1. Iz-2-y gospitallnoy khirurgicheakoy kliniki (zave -
prof.
D.P. ClAukhriyenko) Dnepropetrovskogo meditsinskogo
institute..,
(KIDNEYS--SURGERY) '(VYLON)

CHUKHRIYENKO, D.P., prof. (Dnepropetrovsk, ul.
Kuybyaheva, d.6, kv.2)
"I
,
Characteristics of the properties of lavsan as
alloplastic material.
Vest. khir. 89 no.10:53-64 0 162.
(MIRA 17:10)
1. Iz 2ry gospitallnoy khirurgicheskoy kliniki (zav. -
prof. D.P.
Chukhriyenko) Dnepropetrovskogo meditsinskogo Instituta.

CHUKHRIYENKO, D.P. (Dnepropetro-trAp ul.
Kuybysheva, d.6. kv.2.)
Gomplicated pulmonary opts and their treatment.
Ckudn. khir.
5 no.3.-49-53 My-je'63 (MA 17:1)
1. Iz kafedry gospitallnoy khirurgii No.Z (zav, -
profe DePs
Chukhriyanko) Dnepropetrovskogo meditainskogo
instituta.

-1
0 ~:~`, - . I- - , _.; I .- -j- ~ - , ~ 1 1. ,
- , - I
,=~;MM ~- -~ ~,~ 4:-- 11- -11
1 1-1 . . . . . . . . . . - - .,- . . , " -
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11
. P ---- r .

CHUKHROVj, F.V.
--~
Conference on Clay Research in Stockholm. Vast. AN WSH 33
no.12t58-61 D 163. (MIRA 17 11)
1. Chlen-korrespondent AN SSSR.

1 6 1 to it Le U id is a U
a-OL-1
04
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11-41-19 A4
at.$% .040
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90111101
Mks In COMM
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S.S. S&' Ch(. 140, 331-M; CAM. Zm&. It". 1.
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Barite occum on
the Kertch peninsula in concretions

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in fismium and cavitift in

4
tacks. mm the Cementation of the ace particles. and on fouil

anknall and plant fraginentit. 11 occurs must frequently

with
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plained as due
to the gtfttcf look radius in comparison

with othff blvalent
clemots (straller hydmte vof.) to~

gether with the mg. character
of the Mn cWloW. The

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colloidal jipt. of RAW, rapitily Changes into the tricts.
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found In variousaggreptes and com-tetions of Kertcb orm.

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that which has seod. from dil. "mucasions. Nt. G. M.
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go
**A

.00

00
00

mmowwto (too Ab-halm.
-
11
h S
S
S
R
N
k
d
X
Ak
l

.00
*0

o.
.
d%
.
.
.
.
Sas
o
.
Trbdv Ind. Go
,
,
33
C

"Oo

. A.
Mixerd.-GOMPI. SO. No. J. 45048); cf.
,

0

3147I.-Th nilveral oms isolatc.1 ftook sitatifud div #1c-
, e

-91111
:0

posits of the Carbonaccous perM. ItIstomed from molits.

.00
*
0

cont1j. sulfate of Iron and sulfuric acid (ptwucts of
S
Joffe
J

2

.
.
wrathcring) -

x9o
0e

=*a

Go*

:

z
0
U

:10

-.i AIU.SLA M(TALLW~OCAL LIMAU41 CLAWFICATION
151
U Is xv. 14 is P S 10 rW 0 0 9 -1 0 M 0 Al 0
it CF 64 It a111 U Ktta
It or 4311n1 !14 do
09 090010a 0.0 0 -a 0 0000 00 0 O's : 0 00 0 & 0 04 w0 0 0 a 0
0 0a 06 4
0 ago, 00 0 * 9 0 0 00,0 6-0 0 0 0 0 0 0 * 0 0 00004

'A, A It Q 2 F a 2 A a L 1 )0!1231 MU Idis IOU x p a 81 0 6)
a
-L-A M. Ax w B
A)
0`611CIltli AWJ 061, l6fift
0
0 1
:
00
.00
da a ustafite In are depWts Gi KAUklma.
lei. 1% R. S-V. 22, -00
clwrt~poading to -00
0o
(C... ),.SO.(Cu, 11b)tOH),, has bmu found in the Kazakh-
%taulateppe region (Whezkaigan. Azhim und Derkar) -00
gulf u.South Altai (Nfanka).
Sp Gv-~rim Avers moo
0 j
=0 0
c0 0
=06
go 0
00 z
go 4D
00 g
fmoo
0 0
11100 0
ttoo
too
A 0 - I A 0111A LURGICAL LITINATI1111 CLks%wIcAT$cv$ Vz- b
- - -~- - - - , - --.- -7---
-I -vice.) It-a., off too
I I Cv( C.1 IS I
b U is AV 10 LSJ; ', `V - 1 4 0 1 1 1 ke 0
0, at it x cg It 2 K U ts it 01 w A I An L S a 04 a M N I W j
Aj a 2 j I
0 0 *10 0 00000000 0 0 .6 o0 Is g 0 0 0 0 0 400 0

MIIIIIW_, Fo V*
. "HGnwWr=fttO frOm thO UsPawkiy Mire in Kazakhstan," Dokl.
AN SMJ
23, No.2.. 1939

CHUKHROV, Fedor Vasillyevich
Ore Deposits in the Dzhezkazgan-Ulutau Rayon
in Kazakhstan,
Moscow-ijeningrad, 1944D

~A
r It
I, L L 11-M-1 . , ).A ~ V- ~f ~, It -A. -1--,L-AA Pf CA M s
tit A4(j !W, !,*U(OV
:-so
The mlawska of. phytmorpboses and f Iosail-bones, -460
l-:--V-XhuVhrov. 1,.dy 1. 1. Gool. Nauk. Mad. Nauk !
S. S. S. R. 1VU.-JO, Momeral'-6mkkim. Sep. 'Nil. 2. 1-1,4
(in Lnglish, 18-19)(1940).-Unritic phytolnorplIUS4.4
16 conig.04AKI lia0aii4l:LI.91%5()Ian(iphmj)hatctyi)v.,
cont g.;QJ.W,V PA and 48.67o CaO are dewritwil anti tile
Illocir of formation is discussed. The photiphates are of
so 4,
the viviallite group, alit) kurskite. Vo dr(Inite ruirwrals
44 tile bmil ImIl" could he isouled. X-ray twly-s
Italle, hOWCVCr, .111-)WU tile PhOSPILMS ttl he 11tillIMAY
apatitc. T. S. joile
no 6
go
so
of
Go-'
'!Joe
go
coo
go*
;,so
use
t:oo
00,
A S a S L A mfTALLL-CGK&k WERAT1.611! CLASUPICATICK 7 ties
0 Igoe
10 10
t1U11.) 441 Oll ~11
00
-T
&V 43 it, OF 0 (e to It OR #1 K a it Ir K a' if it (4 40 111 1
is An I I I ha 0 k 9 1 if k 0 a a 1 isle
41 so 004 0 so 0 000000 IN9 0 0 0 Of 0 0 000 0 W
9000010 00 46 0 0 000000 0 0-0 0 0 &0-0 -0 0-0 0 go* 0001

1! 1 it It 16 IJ~ is rt x , v " a a n 4 if a N V. I ~ 0 v w b 0
w 41
il
a .1 0 cif!*

4 A I I V V ~Y__A 1_1- AA CC W IC is I -
n

t A The elpfficeame of gentipermeable membritnes for min-

I
eral mombollentisla. F. V. chilkhrov. 7'FUJV Iffit.
-00

Gnd Na m k, A kad. N'jftr.T. ~5: Vu.,10, Atim"al.-
.00

qev~khim.
Ser. No. 2, 21-70n English, 27)(It"'Ill-After

Kiving a
couilensed revivw of the %ailiji-et of %emilivrinvable

menibmn"
,Ch. prc~_-nts data on the otiKin of veAcuhr

hr.~.olla in the Cn
det-it. f jl~,kaztn in K;,~klman.
i
l
l
I
h
h
h
l
k
l
f
i
i
d

ii c
I
ie re,u
t o
t
ie
nter-
lclA
me
at
ryvkv
la
t
t

action of alk. Inctusilicates and cupirml, 'Alts' prolml,tv

sulfate. J. S. joffe
oo

oo

00.1

i

00
-00

00
00

0
=go

-00

00
AIL.]

0

!too
-04,1

2100

2foo

C-2-

moo
Moo

00 r

go
00
;_0 40
a -4 '1 if 24 is a 3 I-V
tt n U n v! so w -A-11-
0 r, 10, " #q(3:
~

40 0 o o o 0 Ole a * 0 o 0 0 o 0 o o o o o o 0 0 0 o 0 o 0 a 0
o o a o o a 0 0
o
040900(iol*eoooooeoooe0000*0o'*oeoe*OSOO*oooGo
0 Is W
oseI

Z"NIX
ma.
M

J, 4 V blow f
A-_a a T
A 'it A.* D*DjQ& L., M 0 % W. k
ONCKM(S --D -*,of Off
Now date se s1W
A Katiddistita ore deposits. 0:
449 -F.V.Chukftrov. Comild. tend. dead. set. 1'. R. S. S. 27.
halide comixii. were limind
in de,""its of the lijelaitirt (1). tultrakasgail k1l) and
N12.111 (111) districts of Katakliqlan.
0 a!-
N) kni. southrast of the Shortantly statim of the Kara-
ganda railway; admittimmtiou twitints to tht! 'StAtilt4y -4 0
Akmolin4y dimsirt. 11 is N) kin. mst of Kar.
Kolaigs"da diori't. fit is silitatt-d 41%,ul -40
MIS kill. itouthw~m W PAVI,Rlat Citi, And is its, ill the
llayamaul.ky ill-tirivt, 11mvIt.lar trition. At -1 (lie -0
milidus a tit). of Ati-Iltaring qnam vrius wsth few suffi.le .00
xii
00 jl~ ininefals. These latter include PbS, llyrite and Cu md.
hilLs. Embolite is usually found altstied. with Ag-bearing
0 PbSentimfumite. Native All is also assocti. with the rux
Wile. and in one sample of the latirr the I content was
Zee
0.5%. At H the deposits are inainly of Cu but some por-
lions Cont in mixed llb-Cu or". lodArawite. a AR hadide
Mineral, i4. fo= at a no. of places. The otigin of thi4
mineral is assovd. with the weathering of chalowite, which
is As-tworing. In [it (lie deposit% z,e mainly Ali lu,tv-
furtallie although a few individual drii(mu 4 rontain rw An. -0
0
Thew me huOtirl are tilainly metaminlit tavvtn, oventlinx
Itirmilininity with rack layers. .00
atshchalaliytite, gairna, rhalcocitc. mvilite and many
o vto. Ag haliden ate contittint In Mitt trgion ond th-ir 0
#Vigin Is trared it) the lower Imundaty of the wrallit-fing
Iour at it drpth of aht"It I'Al its. ffilltmlitc4. julf(ty
6%fic,
War8w, ilr #11.1 crtsirgyrill.. air the Ati-mitts. mineral-,
It. V. W-11I.-tv
A 1 8 . I L A AITALIL 414KAL LIT14411,11 CLA111PICATICk tie 40
wedl
.11.0 7~
U In Av on It (Pe
't 1 1 74 Or 48
it d
0 6A 0 V 0 9 0 0 0 e 4 0 0 0
0 4lis a 0 0 0 0 0 4 0 0 0 0 0 0 0 0 0 9 * 0 0 0 0 0 0 * 0 0 * e

IA I ik k
31- A
V J,
of minerals hrov. Compt. read. afad, 1
F H. S. ~11*1-~071--,-,,WL,1140)tln~;lillgliwll); -1. 1'. .1.
J4,
0 721M.-As Wide uiijwz~ds aw must. typital of it-jimi,
00 Characterized toy muldity or Where dry C11111air Prevailed
III
the lwast. Untictswund W%Ift$ of the kVIIIIAt KAMMIM.111
00 tritJ441 i'milain C(amiderobIr chloride, with quifor
1114,11tt'h
o* And tMi4ic., Fic'm 7% %41 W* tit wlwpl.~ 44~Wlwrd f1wil III,
90 -90
i'"Inct-10 Imlict oral the mala~v. 01 C1111.4it" 'AA~ III
so eourairtril at a depth of 40 in,, (3) iodendmitir and
bttqw~ .00
mattlytite, the Ifiltri, of Which k the In'.1 euriflit,'t ...
000
AsCif at 00 m., and (4) there 12 no dclillilc 94-914MY (410119
09 vertical lines) in the disitilintion of As lialidrA, Tlii~
a, T 00
in lictud willi moly. dais fix ASCI atki AXI. Nridot goo
000 the tonal disttibuilon of As halide mincials in the h%j-vi
00 13~ genrilt sum of ure drpusits twe the ppin, of Axl aftei
that 4; 0 0
1 of Agile and AXCI Is to be regarded as a rule. 'rlic %:wk. 0
0
00-1 ditions of pptn. of Ag as halides are generally the sime
004, when passing (toni the early to the laic stages of hypct-
1000
Scoicsix. The quantity of chlivide ims as the rhi--l I'll
cipitant W As vatic% vrty little 41tuing ditypicill I,(
id
0 0
weatherlste. but uiring to the slight qkAy, of j%It hAtitlij. a
-ondifersible amt. of ASCI Is ppid. duting the carly stages.
Avets
was
00 tt 0 a
bee
A%&.SLA
Ad~ L t 4 'W 0 -1 Im a--
it it it at $t 19 a qt q it it M w ft I ok
0 0060
0 0 0 a 0 0 0 4b Goo 6000 0 **1

Sul I i I I I
W it u tj W IS It t? Is It a
is x 4D it a 41 fA a C
0

c L

I

Holloyaltes from the depDoits Berkarm and Kaistaily.

1-04111

F.V. Cliukhtov anti N.A. Koilova. G-.p(.,rnd.d-J.

0
-Yi1-t-rR'.--S.-S. 27. IOU-120910)(in EnxlkhI,--Th.-

00

Berkam
tictioidt Is al"it Al kin. s. w. of the town of

Katkaralitisk.

wdimentary rocks anti Itifts with mime v,%ttu,,ivr anti in-

tril.1vi, quatto tv .. phytirs. TIIV IttillMitifAlbul i% C1111-

.00

filled it) sand-lotiv, flouly stialc '411,11 ~V.tldj.y

00
Pyrite, SphaIrfitc, galvita, Aluartt and liarite

are found, In
111C oxillix"I jone Co. Cuptile, lintunile.
-

hilr. arurilv,
psiloinclanc, wail. calcile, ri-rvvL~ilr. inalat

00
bulloysilr,
Immur.
'

0
lit' 1131111V~Ilr h."
jaimils, allil WIllf"Itill' Will fi-IIIIII, I
F

113, Und 'Imil)%il SAVV 11111mix.
cofujwct %tructurr, Ft 1A

ged,
Also) 112ISio).31 1,0, It IN still
will d.W4 tult

.3.
disintegrate when wet, may be cut with a knife
and easily
*

coo
0
lx)ik cqxsmue to the %tin,
?read over a solid surface. I

0
t III. litilloy4lic 10-W5 Mimi,
Vinalur mid it* Vi%&-mis it'l-likV

- 00

consistency unit
lieconics luirder, WIVIS luoillelivil, Ole

powder forms it
viwous ma,-j, Tht, mineral ff,mi Kara.

gally Is similar in all
its properties to 1114( frout tier", (A.

-90

f
Gza 5 :;.1 As Uisk
Ala.1LA .11ALLLINKAL LITERATLAt CLA$SIFKATIOP,
_8
- .10.,
a
A _ ; I. A(:.)
I) ft 91 t? it Of G( It It It U K tt It It (q KID It
00
Clog
IQ.. 4)~ Inv
It I
-s--v
I j14 .00.
i

001 '-00
0
o OWIVII (twu tho dopwts of central -00
fill
06
0 and N. A. Kodomm. Ompt. rtxd. amd. rci. V. R. S.
8:"1(1940)(in Entl6h).-Ocni. analyscs of jao-
R*
sit":s, front various deposits were made anti the fcsult.4 1-0
0 Ical vansple Is: NaP
0 tabulated. The Compn- of Ilp _0
5.10; KO 1.10; HaO &0 U.15: MAO 0.00; PbO -0
00 ().01;; CuO MIX); FelO. 492); A1.0s 0.03; M110.
10 itakcs; 804 32,56; I'M 0.27: AsIO. OAM; 110~ 0.18;
0
SM 0.4d; 110' 10.40; IfP- O.W; in-AA. relidue -
Among the jaroslics studied, Na vatictici predonfinaic
over X varieties., A .If. Kr;i.ljlw
ve 0
MIALLIjKKAL LITINAIVII
Al ~li
At$.
rw 0
k 0 0
t It It R I
t
0 0
g 00 0 a as
U 00
0 e goo

it u it 14 Is m sp x it v 41 41 o nto
I 1 .0-10. 1,11 All (X W u I & d I
I ji,tif
71
SOA 919fol -
A 50*dle md eyssolikWis Itain Katilkhatan 1i V
Chukhriv C pt r*d eaJ
41V Mi-915).
Supicrite j5(CuZn.Ca)O,2S(h.(IIIirOJ wits I'munt avwd. ~-Oo
with linaffle, lifuclumilite. Syllusill. L-villAte,
milifil-.4,11
Ogg lie anti heinhoutilliltv Ili tho Akclta#vt Jvl..it ittim-I
35 kin, mt of the Mointy statlimi ott the Kat:igan-14 tail.
way. Undirr the tnicturwillte *rnimite tvm4tv is ilk~lniet
pletwitroliou, light girro folliming the vloopikut, mul
newly colollrum Iti:
'Zil:2,licular to lite thutgation. The
O-Z Inctitin Is stra It respect to vlongulim told h-iiv - roe
age planes. 111"llitalb-11 J~., optic 111to lics., optic tingle
1.61%). and 0 - 1.644 were animis the pirtnx-ri" 00
dittil. Cyanctrichite (4CuO.AIOs.SA)..IW) wim slis.
mvi,ml Ili lite Beikars depni%it Al, kill. -,f the
90-3 If)wll 14 Karl"naliusk, inut in lite Priezov,ky drlx~o lo.
zoo
00. valr4l in lite uplivir roul- 64 tile Il"r,n,VA.6 Rivur,
Pn,l- Zoo
stfillen4y region, I(o,'t Coldoll 1,111111dy
.4
a
lvtR4Ttj4t CLAWFICATION
Aim-SLA m[lALk1;Pn.KAL L
5u V1 AT No is
It it it K,
009 004 0 0 00 0 0 000 00 0 0 0 0 a
000000100000000000.00oosooeoeeooooooooooo,oGooI
W goe,
age
!zoo
pfeiiii
boo
C-Z
0
-1400
-;,-0
0 0 0 0 0 0 0 41 0 o 0 0 f o 0 o 0 0 0 Z so
,

Migratilm of gold lath* oaldationwane.,. F V Chtik-
fava. 1-k.84. Nauk S.N.N. .. %;r ..,.r7ar
11. 26. - 141.1luillier'l 4111WIK~lw midliti'm W .%It
call 1* ofrielvrd ooly in %olli'le lyp, S-411. ..I
Au its such duposits isinducuml by frer Br,awl 11. Nh~l
A-UnWICIC SUper9VILe nligrAtiOll takes plact in the mi-Wi.111
roar formed under contlif ions of a hot sirid climat, - Ppm.
of Au is mostly due to (effous sullide antl SAh lil,ef.st'-d
I'v
ox4fittion of S. loule YAJus. of Ali may lw (otoml praelt.
ealiv ill the first staxe of orr wrallivring.

If
eal 1, IA Lli-I I I
A IL it
00 A

w"thering of wituranlitte in the 'ieptiaits III centrial

Kasakh9t-. com rrxd. amd. xcl.

lit -t twet"tiv. fisicly
INV-Ott, $lilt holli'l , lit

blitAn' vVIIIII'll III 1111he
eatthy in.tam-% til

lot AnAl IIIII Otlilfs life 114 111rd w6
Ilw IN chrm.

AvAtYx'%U(ttL%hAttift,iiiiiieftonI the

t
;
hims Ow
~Iulr del-it 114. ?kltlo Xjkj. C.,J)

,!
I 11~ IJ, F'() ltr'(),
311.11111, A144 1. O."A'

sit)#
'

'Mll
le-lil% ti) IIIV 11"ItIWOOn Of lilt' WIlIffAIWIC I-Ittill'.

&fill (twittalltut a( WLN. which entri., lilt.. kNilloidal
.,III.

v.ill Iw v'1111plefely

-4. lit 11.0. Wrathrillis rfftvts
lit Karakh,lan air Ir-
00 a

JIMIt"11114'"I th,111 fit IIIIJI6111
01114tru. `AhrIr fir.IVV 13111-

At bwsjt~ Itunt-
flivOtcuLititill iti,miml Ille

I'Lick%kild 111VOIRI l4vach fix
I'thilarv wdrphik i. It'll

S!-

VIIIIII-1v mil'LlOlliv lilt. althimsh pirm-lit lit I",-
I

.4tAitu"filtAl Illpativet flill
-;T
Is to it is 0 it to w
0 0 0 0 0 0 0 0 0 4
0 0 0 0 0 0 a 0 0 0 0-8 a 0 0 a a 0 0
-7* 0
-00
too
goo
gee
too
too
too
Poo
It
!A vt i % 1 14 4 1$ 1 1 V M it 3 0 1
~; 14
0:4 0 6 6 0 : 0 0 0 0 0 0 : 0 4 0
6!0 a 0 0 0 0 0 0 9 0 0 0 0 0

F. ve
A 52T69
)dt: -
'Quarts,
Biamth
"Self-Jormlt* Blaimth in Akchatau Ores," F. V.,
Chukbrov,,
"Upiski Veer-osely Mineralo Obshcheat" Series 2.,
Part, LXXT No
Dieduesea,:aftni%ftigk--of~.aelfforming-bimmth, one of the~:-
forms of b1ftmt)f found in the Akchatau deposits,
locate& in 1kragwAinskly Oblast,* razakh S.9R'* Depos-'
its are Imed.,-wIth quartz-veins. Bis;-
ocate& In. bnly me' part,' the western section,
Mth 1 1
In veins No 152 and 1.53 at a depth of 30 meters.

CEEKfhtIOV,-E,V. and ANOSOV, F. Ya.
t'Vanadates in oxidation zone of deposits in Central
Kazakhstan", ZaPlaki Veesoyuznopo
I h
M
ineralogic eskoRo Obshchestva Series 2, 1948.
SO: -44-30814s 4 Aug 1954-

CHUEMOV 2 F. V. PA 29/,,19T88 I

Gold
V. Chulthrov aArticle, 'The,_Migra~tlon
of Gold~ in/
Oxidation Zones," V. Kreytisr,; 1 p
z Ak Nauk-SMp Ser Geol" Iro6
Chukhrov and Kreyter disagree with the
Current
thesis of the.solution of gold by
ohlorini,
,'obtained during the' -interaction of
acid vater'conz
CbI6rIdes,- on manganese ~ dioxide.
Conclude
-that In.oxIdatIon zoves of dome
de))oslts, gold
tea in true, not colloidj solutions. kaong
60149T39j

cilimmov, F. V. PA 69T4,;

CHUMIROV, Fedor Vasillyevich
"The Eastern Kounradskiy IJeposit as an Example of the
Molybdenum Quartz
Formation of Central Kazakhstan," Sovetskaya Geolopiya,
1948, No. 31.

so added"
M- F. Ya. A=wjd
. milwal. 061kh"fin
wetv
,Ce::'K:LI&de%crIbed from dW~ leeloadW--ij
Koss t tallo are given an tille dqpodb 41 &1*.
ITIt-0 OuVolvid Koiliskiplyt, anti 14"Ill thtly in &,it.
w-f-flMl P4 AtIllf4h W NILI'Allon rott"Rift VW%%,
'46W.4,41, *#I loillwy '"Val all it mito at wonlit
qp"Jelly
.114111C(f to oliKillitph hira ot 4 highly %xinit4ato
cia".
The Primary nAwledic anti galena pit tsaa&4 to areft
site. locionsorphlir. sialthoonite, chalcedony. "Memo,
a 1
and descialzitc. Analym of the Utter . km
that of Gul'shad contains 2-22% AAA be" I
V^. Toe Miami Is characteristically I M
MCK'Ahe Wei
~ anti Havisaffe, Won"fivelesin
after 611116o ;; p"W"Lipliltv, atoll It
PWAMW
IhA" wulffillip. %JwAY% (Wilinall feeb.
Tbr ORMe in tnW of dewtoidto
TOUnIxor tholat vanadinit 4
t. The deseldialte ofiiNMr!:uC*M7t.*W"04Q%r
TW autbore tiotrelfors assum eitened V lowas, sold a
filled" of v final dftmktm by niet; a bed.
whowsk ftoinsivv, 111111") "Im
40"M fto Otawl (&W. " =J9
(Schwellaus. C.A. 40.
blate with o.51
clay ar
An [Aveattotion on t content at about 43 rocks from
tin Lollital Kastakhato" tiet"MRS Showed that the "up-
tkv* twelle Stv VvI V OVW ill V, oliff 0.11 Ift, or,
%1,174 ~Xllvhl
at lift kft 61"Ilt, 11111kil'i
%jilo W, P. 111141h,old'o -141-4 OZ;), Alt'l
earticatialad fituritut" "I sullaks"ity AlW
odur contain trl,,, a# V. silkma ftchists had c Y saii,
howeytir. showed 0.073% V*Oe-
agents, X F4pe. yanishavskil's,
This ream= resalt is in agreentent with
obver-initim (cf. C.A. 30. 41--P) that the -try rocks
a at of Suklaunu.1 cont-Lin O-Ofr-% V*O~;
of the Pb-Z, 0. Utharo think MO. it,
11"Ir are ty;Acal C041 Schists. Tt
tchi t4 tlw ctAyith wedinwo(s. o
vote cd Il" low libo, v CIA to 11"r hrfvT
"IttiIIIIISSIC ourichawnt by &CULAIIIII "'Otr or (arguing
bma 0, at jar accumulAflut V enotigh I
the va-A. Pria-w" 80
to in the oiiiiation tone Of Hitel
Ow". by a ppin.- PfC.C!".

ineroas co"er I=jFs'b,/"XWw 5'0
MetaiiOgripby
"Wedmontite -- A Copp'er-Bearing Mineral of
the 14ont-:
am I I I onite' Group"" F.'V. Chukl=ov,
Active Mem, Acad,
Rd Sci USSR, F. Ya. Anosov., 5 pp *
*Upiski v-s Mineral Obshch" No .1
I*scribes cupriferous clay mineral from
well-known
Dzbezkazgan copper deposits in steppes of
Kazak6
SM, found in-upper part of oxidation zone
of Zlat-
owt.regiqn. Heating curves, petrological
analysis,
chendcal analysis, bopding of copper,
calcium, and
mogneiium, and cbaracte-i-istic variation
of weakly
a4s6rbed water in dependence upon relative
humidity
157T72
USM/Minerals Cop.per Jan/Feb/mar 50
(Contd)
&U indicate that this. cupriferous clay
mineral ie-
longs to the montmorillonite group. Very
high CIDP-
per contem in this #neral permits separate
class:L-
f-,Lcation as "medmontIte" or
"cuproiuontmorillonite,."
157T72~'~

CHUKHROV, F. V.
USSR/Geo"' fes 03m:ror'111YAtion~ N0VADec:'.$6
"The Possible Role of Aerosols, Hydrosols, and
Hydrogels in Magmatogenetic Ore Foimations,"
"Iz-Ak NaukSSSH, Ser Geoln No 6, pp, 45-61
The role of colloids in formation of magmatogene-
ti"c. deposits. Develops new concepts involving
both colloidal and true soln in processes of mag-
miatogenetic ore formation, without analyzing
opposite concepts of many other investigators on
ore'formation.
177%W
177T38

nlift In the St"" WN at Katakhatsm. --P. V,
bukhruy. Dv"y Ak". Nalth S.S.S.R. 71.-,Brrz--
h "k
mineralogical and thtsmal-chein. analysis %If
ocW rvences of the rare Cu mineral chlite, 6CAU.-
: h7
I-A.311#0. which is amocd. with dibydrite.
chrysocolla.
asuritc, malubitc, sometimes with quarts in Cu ove
de-
posits, especially those of Dzbnkugan Altyntrube.-
t
Uspenskoe. Koktaodshariss, and Samovibtt in the
Kazakh-
stan suippe. The stalactitic aggregates show a
distluc!ly
radW and spheroidal habit. their color is green or
grecalsh
black. 'ne optical properties are: -y - I ~~; # - I
M7;
a - IM5; 2V -45'. Pleochroinn -1 - yellowish
green; is - p - light-green. ne x-y disavxIIs
of efflits, of Kasakhotan and dihyMto froca
Madaorudyansk
(Una) are prectically identical, although dWte
coomins 3.
dibWte 2 mob. H#0. The colloidal nature of eldite.
distinguishes this mineral how dihydrite. The P In
both
minerals In derived in the Kazakhstan omurrences
from
ad*-cut sediments (1knestours or seadstou", with
0.08 to
0.12% PA), or ham Porphyries. Anenic Is Identified W
allte KoIrtaodthatim. W. Eitel

ranWoot ad juadto In dw oxidatfors zone. i-
chug voklatly A#44. NOINk S.S.S.R. 72,
lpff-11-
,-Ttw jarosites site much m(Nr
frequentlyot-f-urf ing
tnintfals of lk oxidation tone of printary
pyritr, I,Y1YI--
fife. and nourvolte ores than was pmvmqly
U%%1mW4I
Ch. studird may of such minciallaittim of
oft, lit Ilk-
oclus.. the absence of nabebite. azurite,
and similar
mWerals It; the oxiciation tones wish
junwite Is twily untler.
mood. Liononke poeudomorphs tiler pyrite
art, p4rtirtt-
larly chatuteristic In (he om de lit. with
curlxnwt~
Minerals, of "14 quartz. The 2."N". mlio
in tljr jar,,-
*Itts depends an life alkali Content of
The cirrulalins-111,-
In The oxidatim &ove which are derived
from t1w visillive
aw(hrr nwits of the primary ores. Their
ft-Walmr, huli-
rate thEIVI"C the &Mail COVICTIt (d the
.101`0111tflt, tM. '14L
juroshe is, e.j.. dahvd Irven beratophyf
Ic tacks, tUxtw,,
and :011ts, Ulfthiffte was obalwd in 2-m,
ikplh its
the It a depoks of Clul'ohad wbkb it
rharuritrirrif by a
jasporw N4 J*MW1q-;;;W Movistow. Notmany.
the jorcaftes are older than liamnite and
Ft 9%hh~; is
youtterr jeffoofte k sometlaors, but
always suixtrillmar,
4w*rved In limovite It the oulfide prinury
orrq ore -Avrt-t-.
Tbt elboatk conditions fat the (ormatim of
jarcstite ao-
very dbtbd in the I:wmkmstan Steppes (cf.
Kbitarov Und
UWAvvsbp. C.A. SS, JW. The recent
fortnotion of
kolvalsevatervisalactknoont; thetaberalwas
'361t; ease ppfd. from FeMmtg. sales,
whirb were
fjOllfrol lby surface wafrr tolrobling I't
fh~ 11CIP-41-1
re'et'vOirs- In dbtlaCtiOn I'Mal afacumite
anti AvCI
(cl-rarr )., jatoolte is Prefelably Ppfd.
lit low frill
,,, Mh C.Ii! to, f!,#. In 11w to" n(
vienjill ke Al I 'rulr~
millel, %%,. Filet

"'Mirretite &lid tcoro4ite from the KmIdn" ate"Q.
Chukhrot. Trudy ;ffmer4kj. uuw, Akad.,Nauk
=ld Gut'shakl ~~ in ~m~i4er~e kt-mms. Em dcum agv~e-
gate
of eclussite and phugrnite; the phosphate mizaaal ir,
yellow or bmwnissh yellow, in som2all cr-,-st. a,,gregates, Intel
C, -1%.
Klo-n with quartz The mineral contains Br a.0 X 10
Theocrtim-nce i Oul'thad sh-s a mmz Krr-i-di rniTretfte,
atvx-d. with beudanotc; .,ornettrues ~.t!)Atvvlup~j crY2--
tak w ith i 1016 1. ; I I I I !11. The gentsis is typicaf-
for the o:.idation zone of pri-n&ry pbs and aT-im-'P-'T1tC o'es.
tcor,Aitc i, only ob4~-ved in Gul' aJ tLe bf5trict
h
%la~-zaT'evsk-S--inmr,v~k Nliiie). Rlt7t CTYStaLS tile
furmi ! iiA-':, f 120 1. f 1! 1 Hardncss is 3 5; ~haracteristfc
;s the assr-m. ~jth'heudanrite in intira~te intcrjrcrFth1
T~t chein. aiLilysis gibes the formula Fr!-O,.AsX4.4HO.
W~ 1370el

CO
Ifem rAzakkdan. F. V. Chukbmr. Zap
ijki Vitjoyms. Ifixtipal,
Objk)mjTf8-tVftr-Vw.-"oUmr
ininkral) 80. 1&9-3(1951).-Tht tutneral w"
found in the
Pb-Zn are deposit*tjf Knylcspe (Jupiter
Mine, Kat- hstan
steppe). as reniform aggregates on veinlet I
h
mWood. with chakedony and quartz. m Is py%na
green or dark gree . Prown the deposits of
Malya-Tam
(Aktuodensk, W. Siberia). conichalcite is
observed in para-
geneals with atacamite, malachite, and
chalcopyrite: the
cbem. anal i corresponds to the famula
2CaO.-,)CuO.
Eitel

GHUKHFOV~ F. V.
USM/GeoPhYsica.- Oxidation Mar/Apr 52-~~-
I'Concerning the Ancient Age of the OxIdation Zone
of Deposits in the Steppe Portion of Kazakhstan)"
F.-V. Chukhroy
z Ak Nauk SSSR,, Ser Geol" go 2, pp 102-110
Considers subject problem and also comparative data,.
on the deposits in other regions of the USSR and
abroad. Concludes that ancient oxidation zones are
widespread and are encountered in various parts of
the globe; in a n=ber of cases they were form-ad
under cotditions essentially different from present
conditions.
213T80
ltf~ 4-7 0. 1 0 '43~)

of 111.11achite in (hi-oAdation rono. 11. V
,

11f,tv Afi-r rlo?
7

NFIff(Ir "Fit! a

-;--The- NPIACq

f
h
k
it
V
h
l
f
f
t

rom
azity
x
eit
s ci
ter
atgun,
e (
o
lawd pvIti
umorp

Kouumdt ctc.), brochavite, thfite, atacaml!e, and cuprip!

Mretypical; the inverse pscudorn orphs, e.g. of p)wmarphite,

:
calamine, cerusslEe, brochantitc, chlite after nialachiw

ut nre.
Chalcedony 6 u~u2lly younger than mah-Ititc.

und the iatne is valid
for chryvicolla, cyuno-r-chice, and ~ul-

fenite. while psilGfftelwe,
mid, awl Cu-id 1
1ampadite)

1
Im often c C. ca'!)'y n2alachile of
7>r"

typkal repl:icememnt arigm,
and mzl--c~nt,- icii is ~dzd~

frcra saIns. -~hi~~h is ~-iallv uf
lxjcryqt~al radiaJ-c-=I~r

typ':~

We~thCrLng

frec Cu vAlfiec orta sh,jw
malacnite in m ~tHy ii-ate of

weqtlming~ and no lea hing a-dy "I Cu Ul
01C ourcmi-S i-
observed. 1l, yond that, climetic fat:t,,,s inilu~' ~ t4c

weathering
process; nie depth to whi~:h the cr',Ana,,iwion

of the ircs extendi
into the 1cwrr 13 cvi,~-t:y I

5
j"

um -if, iin
OdWA!"m momm-TR vptel~y -,an
e-C, Ld nordiern CAtife, the Cu caibanate minembs am, rare,
-and suif, tes (e,C., antle-ritc) prevail in the oxidation zones
Atio the concn. in CO, In the circuliting waters plays an
important role in the mass-action rcladons for the formation
of malachite and azurite. The replacement of early-
i4ttrite by malachite is a typical hydrolpis traction in the
highly dd. weathering soins. Among the direct TePlaCc-
meats of'sulfi&3 by malachite tho-e after chalcopyrite,
tennantite, etc. are particularly characteristic (from the
'Altai, and Ural); further those after smitbsonite, Ca amn-
ate minerals, limanite, libethenite, jarosite, and atacamite
(athsite) are also characteristic. W. ~. ~l

I of th&,steppa Of-MuAhstar- CMI]Mroy,
Pelfpf. i AflUrral., A kad, Waittl6r.. ff. 7. R3=p
-rite de
S S (1053); cf. 0.A. 47. (17' 404,-The chmiges of the'p~
pi-its 4 M*Mtift, blrtv~a, etc, b,, oxklatlou slAid rt=tIo4s
with neir surftcr a4u*txts s,,law. ~rc typtcally developed iu
tile following sones:- The tiriazary sul6de nrea sure demn-
6! i;~owtd t6ten to sulfatl~cxfrle arrz. frolu which a
'.14tilb-L" Wou Is derived !a the Upper parti of tile exuatiou
r
tune, intcruhed,tvith Ft WTOWS-",Allo -.WfKc tht~
are Lvvil Okanged to pure 11monitc3l " the uppefinq3t lrea0l-
cring Li,er. Uader tht. conditlows of the wo-it arld dhnat,.
of thr, XazzUlstan steppe, cowpai-able to that of IN. Chile
the effects of weatheriag are observed in the deposics ot
AlUpatvtsa; the mineral sequente ubove the solfides Is
the following (from the bottom to (lie top): szontoltioUte,
hajoviclafte, romerite, coquimbitc, q%ien5zcddtc. ferrina-
trite. metavq1tine; coplapte, pw-Outlerite, und jarosite.
'111 e %, tile rutio
For tile four last-u4lned millrral:l tile. ch.
(010-WO i- from 1:3 to 3A. In the foz horizons,
mudomcrphs art frequent of malachite after nintite.
ochanifte, and cerusAtc; chry3c-colla.;,It~,r I'mathitt.
0

T.
77-1,
Hmouite afttr hyd,olictratite' :14 tim Immixt :16,alL, m-j -
of th-! oudwirti Uril dzp4At.
1,umc,,:Atcty c,vvrc~! by ull ~ nil :4;,
co%ditil,as Lrc !t: the Itepi,e I.v,
lavdi in whkh flo ll:vudamn burr h,it d, Ln,wil wat~xK
ale StrAq'ittilt, e.g. !P K(Alt. "., 11110,OlQ~Vt. --tc. Ab tudwit
chry4occuLliA Is tyjjl~mil for Wn Delitzktutta ard qqr,advr, I
vaALt. chlitr, o", chalreAciii f,lr Mtya -Da. ks.!'y
and Samembet: vit-allates fur ;CyLyl-4pe Alit, (',uj'jjijd.
M! of thase have i& vrry muouth hu--fj~-x rgh;af. Tbc i4c',
it espcetally in-MPLed alut~g cupilLitici in Me oxi-IdLIm
zones. Chbj;*tcj, (;.g. atit.-mi'll-c ca to-a 11 b's T!,L
-~4R]IgC (It SPAZLIClit.: tt. 1, , 11.
mr,A Ill AkdrJIAI. Za bytIntmiltv. i ci, "Umviv. ki -. abvnt,
as am AI-L-utg. s0sacs, be"ust At' 4 ~ rmi Cis I , or~~
etsuva Ill the Tectind wutcr E',!TL;. W. Ifl(A

CHUKHROV, F.V.; SHUBWKOV, 0.14., doktor
geologo-mineralogicheakikh
'-' aktor; SHABLUN, T.N., redaktor; ZXESMVA, Te.V.,
takhnicbeekly redaktor
(Colloids In the earth's crast] Kolloidy V 2emuoi
kore. Moskva,
Izd-vo Akademii nauk SSSR, 1955. 670 P. (MLRA 8:11)
(Colloids)

11~ I 1...;/ 1,.~ ~ V.
C~ /--~ (, /"~,! -- dRu, ~OV,F.V.
'r-1---..,i~~,,,,~x,-.%-,-~-,-"'.-.-i~-:-
Some aspects of colloidal mineralogy. Izv.Aff SSSR.
Ser.geol.20
no.4;3-10 Jl-Ag'55. (9LRA 8:10)
(Mineralogy)

DOLGCPOLOV, X.N.; SHCHARBA OT, D.I., akademik,
otvetstvenny7 redaktor;
BELOV, N.Y.,.'akademik. redaktor; VORCBIYBYo O.A.,
redaktor; OEM-OL.-
LJ4,. re'daktor; KUN. N.P., redaktor isdatel'Btva;
ASTAF'YZVA,-I7X7.",'*'I*
tekhnicheskiy redaktor-
[Pro'blems in geochemistry and mineralogy) Voprosy
geokhimil I...
mineralogii. Ko*Ta. 1956. 174 p. (HLBA 9:7)
1. Chlen-korrespondent AN SSSR (for Chulchrov). 2.
Akademiya nauk
SSSi. Otdeleni7e geologo-geografIcti6skikh nauk.
(Geochesintry) (Mineralogy)-

15-57-4-4590
Translation from: Referativnyy zhurnal, Geologiya, 1957, Nr 4,
p 84 (USSR)
AUTHORS: Chukhrov, P. V., Yermilova, L. P.
TITLE: New Data on the Kerchenites (Novyye dannyye o kercheni-
takh)
PERIODICAL: V sb: Vopr. geokhimii i mineralogii. Moscow, 1956,
pp 158-175.
ABSTRACT: A study has been made, using various methods of
investigation, on the Kerch' and Taman' Fe phosphates
in order to refine the existing concepts concerning
their nature. From chemical, optical, X-ray, and
thermal analyses of vivianite the authors conclude
that oxidation, during the process of vivianite for-
mation, leads to the accumulation of phosphates of
ferric oxide derived from material which initially forms
solid solutions of ferrous oxide in phosphates (gamma
kerchenite, beta kerchenite, and alpha kerchenite),
Card 1/3 after which it becomes dominant or enters completely

New Data on the Kerchenites (Cont.)
15-57-4-4590
into the formation of minerals (oxykerchenite, bosphorite).
The
phosphate of ferric oxide, having formed by the complete
oxidation
of ferrous-oxide vivianite, shows no crystalline features
even under
the electron microscope. The lines on the debyeograms of
different
kerchenites belong to vivianite, the quantity of which is
least in
oxykerchenite. Egueiite should be considered similar to
oxyker-
chenite in its formation. Tinticite is similar to
bosphorite, but
differs in having a lower content of weakly bound water. The
for-
mation of tinticite may be associated both with direct
precipitation
from solution and with crystallization of amorphous (to
X-rays)
bosphorite. Distinctive solid solutions form in the early
stages of
oxidation of vivianite. In these the solvent has a
crystalline
structure and the dissolved substance is Piporphous.
Hydrolysis during
oxidation of vivianite does not lead to tfte formation of
free iron
oxides and is not accompanied by a marked removal of P. In
sub-
sequent stages there probably occurs a gradual hydrolytic
splitting
of the amorphous ferriphosphate with removal of part of the
phos-
phoric acid from it. Picite may be considered an earlier
product of
this process, having been discovered in the Kerch' iron ores.
Card 2/3

15-57-4-4590
New Data on the Kerchenites (Cont.)
Further products of hydrolysis may be azovskite, which has
been
recognized in the iron ores of the Taman' peninsula.
Limonite, with
a variable P content, may possibly represent the final
product of
hydrolysis of ferriphosphates, obtained by complete or
almost
complete oxidation of the iron in vivianite.
Card 3/3 G. A. G.

CHUMMY, F.V.
ft- R"s
Zinciferono clays from the Akdshal deposits in
Kazakhstan. Kora
vyvet.r. no.2:107-123 156. (MLEA 9:8)
(Kazakhstan--Clay) (Xasakhotan--Zinc ores)

Rr 1%
-SHCHERRAKOV, D.I., akatlemik; SHATSKrrjW.S.. akademik;MIRCKCV,
S.I., akademik;
STRAKHOV, N.M., akademik; KORZHINSKIY, D.S., nkademik;
BLTEXHTIN,,A.G.,
akademik,- NALIVKIN, D*V*, akademik; POLKLIT, A.A., akademik;
AFANASI-
YEV, G.D.: VLASOV, K.A:; " Mai fTSKIY, O.D.; PAVLOVSKIY,Y~.V,,
professor; BARSAITOV, G P.Fprco~essor.
%, A.D.; IVAITOV, B.V.;
YABLOKOV, V.S.; ARDASHBIK(TTA, S.D.
Academician Vladimir Afanftslovich Obrucher., hero of socialist
labor;
obituary. Izv. AN SSSR. Ser.geol. 21 no.6.'5-10 J0156. (MLRA 9:10)
1. Chlon-korrespondent Akademii nauk BSBR (for Afanaalyov. Vlasay.
C.hukhrov. Levitakiy).
(Obruchev, Vladimir Afanaelyevich, 1863-1956)

md~lt~ 15 au~rvea I=E mas rormE~j bv m uatll~-Inff Imm
r-,7

CHUKHROV, F.. V.
"Clay Minerals in the Hypergenesio Zone of Sulphide Deposits."
paper distributed at the International Clay Mineralogy Congress
in Brussels, Belgium,
1 - 5 Jul 58.
Comment: B-3,116,859.

SOV-11-58-8-2/14
AUTHORSs
Chukhrov, F.V.t Moleva, V.A. and
Yermiloya, L.P.
TITLE:
New Data on Mitridatite (Novyye Dannyye o
Mitridatite)
PERIODICALs
Izvestiya Akademii nauk SSSRt Seriya
Geologicheskaya, 19581

Nr 8, pp 16-26 (USSR)
ABSTRACT:
The name
"mitridatite" was briven by P.A. Dvoychenko to a light-

green
earthy substance discovered by S.P. Popov in 1911 among

the
iron ores of the Kerch' Peninsula. Much later similar sub-

stances were described by F.V Chukhrov ind A.v. Sidorenko.

This
article is a detailed report on the results of laboratory

studies of these'substances with the application of most
modern

means of science. Following scientists took part in
these

studies; F.V. Chukhrov, V.I. Stepanov, A.V. Moleval V,S,
Ame-

lina, M.T. Yanchenko, A.A. Voronova and A.I. Tsvetkov. C.
Fron-

del (USA) also took part in discussion and propounded the
theory

that the results of the analysis of all these products
could

possibly concern different minerals. The results of all
these

researches could be summed up as follows. The mitridatite
4-9

a basic ferro-calcium phosphate in which some quantity of
(PO 4)
Card 1/2
was presumable replaced by the groups of (OH) 4'
Its formula

New Data on Mitridatite
SOV-11-58-8-2/14
is CA2FE 3- f-(P04)3 (OH)4 7 nH 20 'where on the average 'In"
equals 2. Its syngony is mono- or threeclinic. Aggregates
of the mineral are cryptocrystallic, earthy - loose or dense.
It can be decomposed by acids. Index of refraction - 1.77.
Some number of particles have colloid dimension 2nd appear
laminar under the microscope. The grenesis of the mitridatite
is connected with the alteration of oxykerschenite (addition
of calcium) or of anapaite (loss of part of calcium.). It
can '
be considered as a metacolloid, containing colloid particles.
There are 5 tables, 2 photo3~ 3 graphs and 9 references, 6
of which are Soviet and 3 non-Soviet.
SUBMITTED: July 18, 1957
ASSOCIATION: Institut Geologii rudnykh mestorozhdeniy,
petro-rafii, minera-
lo 'gii i geokhimii AN SSSR, Moskva (Institute of Geology of
Ore
Deposits, Petrography, Mineralogy and Geochemistry of 'the AS
USSR, Moscow)
1. Mitridatite--Chemical analysis
Card 2/2

15(6), 15~2)
Chukhroy SOV/30-58-12-14 ?46
AUTHORs 1_ , Corresponding Member,
A-Ow*-My of Sciences, USSR
TITLE3
International Conference on Clays (Mezhdunarodnoye

soveshchaniya po glinam)
PERIODICALt
Vestnik Akademii nauk SSSR,
1958, Nr 12, PP 59 - 60 (USSR)
ABSTRACTe
This conference was held
in Belgium from July I to 5 and

was devoted to clay types and
clayey minerals. Delegates

from the following countries attended
this oonferencet

Australia, England, Belgium, Hungary, the
Netherlands, Israel,

Spain, Italy, the USSR, the USA, France,
the German Federal

Republic, Czechoslovakia, Switzerland and
Sweden. The Soviet

delegation submitted 20 reports on the
geology, mineralogy

and the exploitation of clay types. A
oompilrAtion of these

reports with a short Engli sh- language
sumfoary was distributed

among the delegates. The majority of
the reports-mentioned

came from Western delegates. I. Barns, and
B. Harnalko

(Hungary) reported on the fluidity conditions of
aqueous

benthonite dispersions from Hungarian deposits. I. Kont

(Czechoslovakia) reported on the porosity of clayey minerals
Card 1/2
and their liquid-absorbent properties. The participants
in

International Conference on Clays SOV/30-58-12-4/46
the conference exyressed the intention to establish a sub-
committee for clay at the International Geological Congress.
-
Recommendations were made - to the International Association
of Mineralogical Societies to establish a group for clay
nomenclature.
Card 2/2

GHUKHROV, F.V. , glavnyy red.; BONWTIW-KUPLZTS"YA,
N.M., doktor
xam.glavnogo red.; BARWHOV, G.P., prof.,
red.; BILOV, N.V., akademik, red.;AW IKOVA, O.M.,
doktor
geol.r-mineral.nauk. red. Eaeceased); SHAUMN, T.N.,
rea.iza-va:
ZHLMOVA, Ye.T., tekhn.red.
-[Minerals; a handbook] KineraI7; spravochnik. Moskva.
Vol.l.
[Native elements. Intermetallic compounds. Carbides,
nitrides.
phosphides, arsenides. antimcaides. bismathides,
sulfides,
seleniaes, tellurides) Samo,roanye eleminty.
Inte'rmatallichookie
soeainaniia. Karbidy, nitrJdy, foofidy. arsenidy,
antimonidy.
vismatidy. sullfidy, seleni4y, telluridy. 1960. 616 p.
(MIRA 13:12)
1. Akademiya n6uk SSSR. Institut geologii rudnykh
mestorozhdaniy,
petrografii, mineralogii i geokhimii. 2.
Chlen-korrespondent
AN SSSR (for Chukhrov).
(I(ineralogy--Handbooko,.manuals, etc.)

CHUKHROV, F.T.; TUGARIMOV, A.I.
Tvanty'first session of the International Geological Congress
In
Copenhagen. Geokhimiia no.8:756-758 160& (KM 14:1)
(Geochemistry-Congresses)

CHUIMOV.1 F.V.
Letter to the editors Izvo vyse uchebt zavo; geol i
razv,
3 no,6:3-19 Je 160. ~M= 14:7)
(Geology)