SCIENTIFIC ABSTRACT ZHURAVLEVA, A. - ZHURAVLEVA, I.T.

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• Collection: Scientific Abstracts
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• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: July 16, 2001
• Sequence Number: 17
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

84118~
8/01 ~J61:)/030/01 0/02 5/03
BOO1 /B.o6,6:
V.j 44W Knst06 LroyaL -Lei I
AUTHORS: Vasillyevy S
Vasillyev, G. S.
Acetone
TITM Effect of Nitrogen oni%benzal-
urn
PERIODICAL; Zh al obahchey.khimii,:1960 Vol 30, 10P
pp- 3414 3416
-o;~ide with iin-
TEXT: Proceeding from the reaction of nitrogen:teti
saturated'aliphatic ketoneal one.of~.the authors~ (Ref.1) ishowed i~iti~
i
according to thestructure of the initial ketontG-additioft produdto hre
obtained which differ as to nature and properties. The nitro grodp'wile
found to be added to the leastj and the ONO group:tc- the most strongiy
hydrogenated carbon atom. When treating benzal 4c,eton6 with nitrogem
tetroxide, not only an addition to the d ouble bond ofithe,side chain.:
takes place, but also a substitution of the hydr 'ogert of'the benzene
ring in the para position. The behavior of diben,Z,'al a~e'~one toward
nitrogen tetroxide was investigated. Dibental acatoiWdissolved In ether
was treated with gaseous and liquid reagents. The nitrite of nitro -L-
Card 11.3

111911 11"W; "MID111 11119191MIN1111 11 11711.111VIVIIHIM IIHII 11111 111 HIM IHINI Iffil IT11111
84883
Effect of.11itrogen on Dibenzal Acetone, 8/079/6o/o3o/olO/025/930,
BOO1/B0'66
0 J~it]to
reaulted in tho rormol, 0111 0 and-th nL-Litte of V11
t -t)nt31q
oxyketone (II) in the latter.
CH - C CH CHC H
a H CH
6 5 6 5,
ONO NO 0
2,
H
0 N CH CH C -~CH-W= C
2 2.
CD
ONO NO 0
'By agitating with iiaters hydroxyl was'substitut0d,fortthe.0NO group, in
both products (Refs.2~and 3), to give. the correspondin:g:cryetalifne
.hydroxy-nitro-ketones. The addition.products decomposed when heated
with water or mineral aoids on the water bath for 26-3.0 houre (Rafe-:4
and 5). There are 5 references: 3 Soviet, l us, alid I :British.
Card 2/3

S
Effect of Nitrogen on Dibenzal Acetone /OW6o/lo3o/olO/025630~
BOOltpO66
ASSOCIATION: Moskovskiy institut tonkoy khimicheskoy iekhnol ogi
(Moscow Institute of Fine Chemical,Taolmol6gy)

VASIL'YEV, S.V.,L~V~LEVA., ~A.A*; KWTOMARDVA V.L.; VASJ:L',UV GIs$
Action of.mitrogen tetroxide,ou dibe4zaUcetondid Zh~r.ob.khimo,.30:
161,
KMA 134 14)
no,

~10 Wskovakly iwtltut tonkoy kbilrdebeakoy tildlnolo~jle
one
(Nitrogen oxide) (Peatadien

~wj
4N

-USY
Ys'

7 41~ 4,
'2Z /I
AUTHORS: Veller, V.N., Candidate of Technical Sci6nces and
Zhuravleva, A.A. Engineer-
TITIE: Comnarati~e investigations on Pistonz
(Sravnitellnyye'issledovaniya porshney)
PERIODICAL: Teploenergetika, 1958, r40;21 Pp, 36 - 43 (USSR),
ABSTRACT: In governor systems extensive use is made of piston
elements. Rotating and seif-centering pistons are used to
obtain high sensitivity. Comparative charaoteristics of such
pistons were obtained.'.experimentally, using the rig illustrated
in Fig.1, the principies of operation of:whLch are described.
Two hydraulic pistons are joined back-to-back by a connecting
rod, and subjected to various axial and latBral pressures. An
expression is given for the insensitivity. Three types of piston
were invest-igated: a rotating piston, the A,11-Union Thermo-
technical Institute (VTI) self-centerin-;Pl. to , and the
Central Boiler Turbine Institute (TsKTI~,
Two designs of rotating pistons were tested:, one with~screw-
thread.channels on the side walls (Fig.2A) and~one with nozzles
(Fig.2B). The nozzles were made in the form,of sloping holes*
~drilled through the head of the piston.',,At first, the~su:~face
of the piston with nozzles was made smooth but with this :
arrangement, it was not possible to start the -piston rotating
Gard

j_jzj3-2- /1:233
t4,~e
Compa ra lwrestiGation, on Pistons
b- increasing the oil pressure. To 9 t ma(%, urithout :the
p13tOn rotating showed that the degr6ci of iriseasitiVity~ is
12 - 14% over its whole travel. The pis-,;on could only be
made tc rotate after screw-thread charne].s~had been.=-de round
the wails3 to equalise the prc;ssure oil t'_he~ sides of :tLe; piston
and reduce friction
Results of tests wiih a rotating and.altationarg -piston are
.3. axial and lateral
given. in Fig With the p-;ston rotatin,,.
forces did not cause loss oi sensitivit7. The conditions
under which the piston continues to rotate. were investigated.
On the basis of the tests, a nrocedurlb wmdeveloped for
calculat-ing the torqve necessary -to rotate, the piston under
di-fferent zompressions.
:The rotatinG pistons were made withd~ep channels so that the,
torque was set up by. the oil flowing throuj-,h the cha~nnels,
which were in the f orm of twe-start threads. The results of
tests on pistons of this kind are given in irig.4 and show that
tha for~;e required to maintain rotati6n in these pis"tonis is
ass thar- in those viiUh nozzles. The , re:~ults of tests 'on
51pecinens with deep spiral grooves under different compressive
forces and with constant oil flc-,7 throug*a the grooves are
Card2/5

(;omDara4-j,.Te Investigat4onzc on
given in Fig-5. They show that althou'~;;fi Idstons with n#zles
are more resistant to compressive and axial fcrcaes,~~they
also ohould have relatively deep grooves.
Tea-"-,s wei-e made on the same installat-ita to determihe' t1he
flow of oil with the pis' ons rotatinz.~.' For exac~ple:,~,,with a
stationary piston at 32 and a pressure of 3. 09 atra. tbe
f low was 340 kg/hour; and, at 40 C and 7.05 atm. , it r, as
or
554 kg/hrr . With the piston rotating) leakage through the
Eap was reduced to 205 kb/hour at 170 Od and 202 r.p.m; to
325 kdirhour at 40 ou and 430 r.p.m. The re(laction in~ leakage
-is about 400% of the initial vahe, whatever the tem-perature of
the o-41.
The piston of the Central Boiler Turbihe Itjtitute Is illus-
trated in irig.6. A special feature pist~'on i's that the
skirt is relieved so that or-ly narrow bands of the P:'Jston wall
are in contact with the cylJrder wall. 9.he authors-thihk that.
suCh grooves can prevent asymmetrical prE.Sssure distribution in
the gap but cannot induce self-centeringr forces. The results
of tests on ti-is kind of piston are Sivert ir., Yig.?. ~.It will
be seen that lateral forces --ause considEXable loss of B'ens-i-
tivity. Sym:i1etrical distribution of oil pressure in, the -ap,
Card3/5

Comparative Investigations on Vietons
is confirmed.
The conditions necessary to obtain maximum. S-3nsitivity.in
piston-type mechanisms are discussed. It~is shown that'the
types of piston described above have certaiin defects rhich! it
is claimed, are overcome in the self-centerirj~ piston of the
All-Union Thermo-technical lnstitute. Th,is pisto-n. is then;:
illustrated in FiS.8 and described. An ever nui)-,ber of,
depressions is made around the wall of tLe ;,-i8t(jft and 6hch~is
e
conne--ted to the inner side of the wall by a drilled hole.'
Also, holes are drilled down from the pistor.head to meet an
annular groove ir. the skirt below the depiressions., The! cor.~-
sequent self-centering action of the~pistqn is eyplained.
Test results vith a piston of this kind~are Given in F1g.96
They were for a piston in which the diamet'er of. the drilled
holes from the hollovs was 1 run; it.had uprer and lov-.-er
clea--ances to the cylinder of 0.14 mm and 0,2.mm, respecti7ely.
A second series of tests was carried out:with~other specimiens
in which the.diameter of the holes was 2 ami and the cleara~nces
were U.32 mm and 0.3 umu. It will be seeh~-frojft the grap~hs that
the insensitivity of the pistons remains,:SME,.11. Testamade
with the centering holes blocked up showed F-L.InUCh 1OWer
(;ard4/5

96-58-2-?/23
Comparative Investigations on Pistons
sensitivity.
The results indicate that with self-centeri. aG pistons~ !the'
i.t~,qensitivity.is practically:zero both unde:? compress ve and
lateral forces. The total oil leakage vith self-centering
pistons is 800 litres/hour with a hcle diameter of 1 mm and
2 700 litres/hour with a hole diameter of 2.mo~ The correE-;-
ponding flow for rotating systems is 14 000 lilre8/hou'r*- 1,Thc.
insensitivity of self-centerinS pistons inc.-reases sharplyiif
the oil supply holes become choked tut evon thea the insensitivity
is less than with plain-wall6d pistons.
Somewhat modified designs of,self-centerin.6 pistons have now
been developed by, the Central Boiler Turbine Institute and
this construction is described. With self-aentering pistons,
-the centering force appears before moven,ont coitivenceo-, 1.,dth
rotating pistons, it is not generalted until they have' eo=ienced
to rotate. The ruaterial of which self-ce:nterinZ pistons are
made is of relatively little~importance.,: i
There are 9 figures and 4 Russian reference.
Unio
ASSOCIATION: Voesoyuznyy teplotekhnicheskiy institu'; (All- n
Heat Engineering-Institute)
AVAILABLE: Library of wngreas
Card 5/5 1. Pistons-Characteristics

ACC N& AT6OA87
SOURCE CODE:
AUVORs Zhuravleva, A. X. (Khartkov); SlAva, 0. K. 00iartkov),
ORGs none
TITISt Mration of rotors of a discklrum construction
SOURal lbarikov. PolitekhnichaskiY institut* Dinamika i piaichrostf mashin
~kov lzd-~ro 4~r
(Dynamics and strength of machinea)t no& 3, 1(har lkciskogo un
116-12Z
TOPIC TAGS: vibration analysis, rotor blade, turbine rotor
ABSTRACT: In a drum-like rotor,~tha-rigidity of the discs and'that:6f'tho shell,
'connecting them is of the same order of magnitude, so that the coMition. of a rigid
disc clamping (along a certain radius) is not fulfilled. Thevibriiitions of one disc,
are transmitted t1hrough the shell to other discs. A rotor ofV.iis type must be
considered as a single dynamic system with a complex spectrum ofrosonance-states.
excited by forces originated in any of the parts of the rotor, 'Iho ~-uthors devaAoped
a method for the calculation of the vibrations of this system by urirj~ adiscrota,model
of a shell consisting of massive rings without thickness connectedby massless ;rtiona
PO
of the shell. The matrix equations of such a model are obtained by-expressing the
displacements of the shell along the axes x, y, z in sphorio coordiutes. The
22
Card 1 /2

EHII I IPAR
T-r,
/
AqTHOR: Zhuravleva, F. A. 2o-4-411[51
TITLE: On the Family Faeudorthoceratidae Flowei.''et Caster (0 semeystve
Pseudorthoceratidae Flower et Cast 0935)
PERIODICAL: Doklady AN SSSR, 1957t Vol. 116, Xr4, pp-A;77-680 (USSR)
ABSTRACTt At the begin this family contained 5 lat~-,ptlaedcoic gen6ra
with straight shells. Inspite of the peculiarity of the deposits
in the inner of the siphon Flower and CaS'ter (reference 4) have
counted this family to the group Annulogiplicnata, of the subd 'ivi-
sion CXrtochoarlites. Flower has lat.er discovered a series of new
genera of,straight,Devonian nautiloideae:of the family. Flower
considers the inner siphon deposits which forta riw on the si-
phonal funnels as the most characteristic f,:.~ature of the~fam,ily
mentioned in the title. They do not thicken here, as it is the
case with the actinoceratides$ but are exte..,ided to their~neigh-
boring oonnexion rings. In the case of a:sufficient development
they formp coalescing, a kind of connected ;Jiner siphon shell.
Flower's 18 genera were subdivided into ~ subfamilies. The midd-
le Silurian genus VirMceras is by Flower considered to be the
ancestor of all families in question. The investigations of the
recent years have comploted the number of genera of the family
and changed the conceptions concerning their origin. It became ob-
vious that the family did not occur at the begin of Devonian
Card 1/2 (Flower,but much es rli er.Ac cording to Toichert and Glenister (re-

On the Family Pseudorthoceratidae Flower at Caster 2o-4-41/51
ference 5) the mentioned family in assumed -.1.o1be a descendant
of an old branch9probably of the Baltoceiatidae.The,new gene ra of
the author confirm a second'time this early ori gin.The numbe r of
the family has to be designed in another~:ralr according to th'e.in-
vestigations of recent years. Also the mentioned genus Virgodera
of the middle Silurian is to be counted io this group. Spyrocer-
as,however, does scarcely belong to it.A,diagnosis of the family
and a list of the 28 genera counted by the author Ito iV(with 2
new ones) is given. They became known from the layers of the,midd-
le Ordovician till Permian.The new genera are.H) lletastromoceras
gen.nov. with the type:h1jormosum sp.nov, fzom the Llandov stagd
on-the Podkamennaya Tunguska river. The most they are related to
Stromotoceras Teichert and Glonister 2) ]~,etc
_._phi2piorthoceras
gen.nov. type:M.Helenae sp.nov. middle Ordoi,ician of the:same si-
te,Krivolutskiy horizon.Differs from all.other genera of the fa-
mily by an almost marginal siphon and by a Ileculiar transversal
sculpture.There are 2 figures and 5 references, 2 of which are
Slavic.
ASSOCIA12IOll: Pala eont o3Q:ica 1 institute All USSR (Pal eont ologich eskiy institut
FR ES E"'U ED : January 5,1957, by I.I.Shraalfgauzen,Academician AN SSSR)
SUBMITTED; December 18p 1956
AVAILABLE: Library of Congress.
Card.2/2

111rill Hil Vill IG;

III 1131311111frollill M -I'll- -- --- -

4111111 [fill III Ifliff IHlH
TT-
TRIGM, N.I.; ZHURAYLEVA, G. M.
Reaction of the organism of a newborn child to, intracutansous and
oral BCG administration.- Prob.tub.no.'4:27-33 J149 15~-Odm 8-.!0)
1. Is dispanearnogo sektorn Inuti.tuti tuborkul6ia A141 SSSR
(dir.Z.A.Lebedeva), 25-7. gorodskor bb"Vedineiii I bol"hitsy (zav.
H.A.Kruglova) :1 14-y Detskay bollniter (say. P. Ka:.
(BCG vkCCINATION,. off.
on newborn inf. Intracutansous & orpa adialli.)
(INFANTS(NNBORK)
off. of BCO vacc. intracutaneous & oraladnin.

lll*.#!Iziiiluuiiitiiii3puiiiiiuijrriiiiii will 11111 milli
Jim - - - -- - - ---- - - - --- -- - - - - -- . - ----

~~~28676
S/020/6,1 /1,~0/002/021/62:'3
D1 30/t! 10
AUTHORS: Shigorin, D. 11. Smirnova' V Io
Grdcheva, Ye. F-t a-ad Shostakovskiy, Mi F, ~Corroipon~lng
Member AS USSR
TITLE: Epr spectra of V-irradiatIed acetylene and its derivative-81
PER'IODICAL: Akademiya nauk SSSR. Doklady, v-, 140,~.~ho. 12 1961, 1
4 2 2:
TEXT To determine the relationship betwemthe str,uct-ire' of the initial
molecules and the etructure of the resulting radical, the.authors d~6diid
the epr spectra of y-irradiated acetylene, mothyl ado tyleno
deutero acetylene, ethyl- and butyl,acetyl'no, an well as h
enyl- -and
methyl-phenyl acetylene at 770K. The.compounds we're i::-rddiated in.
special-gla2a ampuls giving no'epr,spectrum with the u;zierl dose of Y~radia-
tion. Before. the tests, the ampule were evaouated;' to I 6-~ mn H6.: Iri!a-
diation waa conducted with Co60. A superheterodyne! railibopectroscope i
was used for taking the epr speQtra. The magnetic ~~:~field' was calibrated
ft.. )2z
with the epr spectra of the pyroxylamine disulfoni~,~I:onl NO(SO
Card I

Rom
26676
3/0 1/140/002/021
'10
BI 3
Epr spectra of 1-irradiated ... 01~1
chloroform. Copper chloride monocrystals were usedIfor ie,tarmining-,the
concentration of the radicals-obtained. The relati4e'~';error ~when
determining the yield of radicals was v2 Test ro'su I ts' are given;in
0%-
Tables 1 arcl 2. The spectrum of doutero methyl acetyler.e ~obtained from
heavy water- wrid Li-methyl acetylenide duggentsan i4te:.,aation of the,
unpaired electron in the radical with the:protons of;ithe! CD.and CH2.
rOUDS. The aymmietric triplet of methyl-phenyl acetyler,e may be 1
9
explained by: (1) the interaction of the unpaired electron:with thl!
protons of the methylene group in the radical G5 C~C~-6H,, ~oi (2) by the
fact that this spectrum has to be ascribed to the ra6ic'Ell,o-f the phehyl
ring -ONC-P. A comparison with the spectra of benzene and methyl-I
phenyl acetylone with benzene indicates' that axplioatiori. (1 is appl~cabIN
An intensive e~r spectrum of C H is only obtained by high-lose irradia-:
2 2
tion, which suggests a considerable redistribution of: energy in the,
system. This is even more distinct with phenyl acetylene which gives no
epr spectra with high-dose irradiation either. The~red-Jstribution of the
energy absorbed may be explained by the-formation of.'aomplexes between the
the ampul walis
molecules T; facl, polymeric compounds were found on
Card 2/5,

ACCESSION NR: 076/64/038/003,10742/0745
-040334W

AUTHORS: Smirnovaq V.I.; Zhuravlevi G.S.~; Yanova Shigor~
no
D.Ne
TITLE: Electron paramagnetic resonance study of the flti~ucture and
behavior of radicals formed on ~C,,fi - #and 'photoly~ic. irradi-
ation of acetaldehyde and formaldehyde
'
*
~
1
-SOURCE; Zhurnal fizicheskoy.khimiij.-v.
-745
A no# 3
964p
, 742
didalp cetalde
TOPIC TAGS.-electrop paramagnetic resonancel fred ra -a
J*de formaldehyde,,beta irradiationp 'gamma irradLationt:ultravioletl
irradiation
ABSTRACT: The structure and behavior of free radicals formed upon 1,
~ 1:
and ultraviolet 1 irradiation of acotald4hyde!
on A - and
~ and
up
'
irradiation..of formalde)i were-studied by the,;electron.para--
yde
magnotic-resonance (EPR) me
' thod. The studied comp6uni-.Is~were conden-~
sod from the
gaseous phase into special ampules and wore.irradiated
I at -190C. Upon irradiation of acetaldehyde with A-ray dosen of 3.
I milliqn rads4 a singlet is obtained# which is attributed to the
Pard
3

ACCESSION.NR: AP4033409

-breakage
of the C-C bond and formation of CH And ~4H() radica
.
63 i'
where CH radicals rapidly recombine but CH radical has~a locaized,
*
P
electron-and consequently it:does not pobsevs; nuclear
unpaire
magnetic moment. At do ses of 40,to 100 million.ra.dgii tripleV
2 additional less intense lines-is observed,and ii attribut'd
a
to the supposition of the singlet and quartet 4btainvd; at do s e;s I of
3 million rads. The line width was A H -
47 .0 oersted. , Upon increase
,
of the temperature from -130 to -120C the singlet dis,ap pears and
the quartet becomes symmetrical. It was assumed that t he quartet
appears upon the breakage of C-H bond with the formation.of CH3 a 0
radicals or upon the breqkage of the C-0 bond in tho polymaric chain;
with the formation of O-C -0 radical. '.The quenching temperature
3
_
of the juartet was -105.~~o 50C. On A -irradiation of formaldehyde
At doses of 7 million radsthe doublet tormed is relatod,to the for
mation of -0-CH-0- type radical. At doses of 70 million rads the'
'
spectrum appears as an assymetrical line with-shouldeit-a:which m
ay be
"X ..composite of two.different spectra of the -0-CH-0- jdoublet) and
Carj 2/ 3
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i ACCESSION NR* AP4030367.
It
catalyst and repreci itate'd (111) 4: D-c.elec r 641 i:ohductivity
P
a tudied in air -or- at- 3-x'l0-21-!mm 1H& for pellet, i;aiuples as
-,functi of ambient temoerat ur
an e (20-276C) and pri'aliL-Minary heat-
treatment temperature (200-300C).~ The temperature dbpendence
of electrical conductivity of 1 shown, An, Fig.,, 11 ii6f enclosure j~
indicates that at about 120C (inflection) andlabo4e the: el'actricali
nature of the alymer changes probably ing.to~t'he etim'Lnatio'
p -ow
boundivater., Of all the-samplas, ponhaat-tr~at~dlj showed the!, I
highest:cond 10_.~7 m_1 1:his"
co
uctivity at -20C ohtr x c nducti.vity
d
r d to 10-14 ohm-,I,x cW-' ,and:activatiom-ene gy rose
oppe n ~i wLth~hei
I treatment,tempe.raturo incre.ases,to 36bC4,:1VoUh eat.-btreat4d II anA, 111-
showed poorer conductivity, than I, evidently, owfnz'~ to ithe, presence'!
of impuritiesS Room temperature dagassing of nonheat-Itreated * M_i,
ples:produced a partially irreversiblel,ris*e in re'sisti4ity by ai
factor of 1.2,-3.0 owing to the elimination of fralle lwa~tars Thdisig Ia
of the thermoelectric power. for,all the samples itt'diait-od. t
ype
-The magnetic susceptibilit lthell
conductivity., y was poiltivis4or all I
GAMPIGS1 its Volvo 100.4 with rising Ambient
temperatures, X-ray 'ihalysis indicates that or4axi., to tits, joelyple!r
,.-!;#rd2

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1
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,
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the course of the: timperature changae, %,
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oxwoelectiIi-, p, '., 4~er
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15:11957-3-2679
Translation from: Referativnyy zhurnal,, Geol6piY 1957o Nr 31
p 23 (USSR)
AUTHOR:
TITLE: Archaeocyathids of the Siberian Platform .5. Id:Th ir Vilu
n e
in the Cambrian Stratigraphy,of Siberia (Arkheotgiaty Sibirskoy
platf ormy i ikh znacheniye dlya stratigrafil kemibriya Sibir,
PERIODICAL: V ab Vopr. geologii Azii. Vol 1, Moscow., Izd-~vo AN
SSSR,, 1954.. pp 484-494
ABSTRACT: Inthe lowerpart of.the variegated~~series of the ~Aldan.
stage along the Lena River., the'.genera that:;predominate are
Ajacicyathus, Nochoroicyathusq Archaeopyathus, and -- especially
characteristic -- the primitiveo.single-wallwa.A~rchaeocyAihid',
Archaeolynthus. CosainocZathus and Dictyobyathiis'are fourid very
rarely. Upward-in the section Archaeolynthas Es encountered less
frequently, but Coscinocyathus Becomes more~labtindant. Claruscim-
thus, Dictyocyathus, and Ajacioyathu3 are common. The;
Card 1/3

Archaeocyathide of the (Cdnt.) 15-1957-3-2679
first and rare., representative of the genus .1fthmophyllum is
noted* In the upper 'variegated series, along the Lena and Bo-
toma Rivers, Ethmophyllum and,Thalamoonthus are much m .ore-abun-
dant, and a new genus occurs, Lenor-yathusl!~C,I;!truscyathus, and.
Archaeocyathus are the dominan7t -forms in he Kutorginov",and
Charako-Keteminakiy yarusy (horizons) aloni-the.Sinyaya River
at the mouth of the Peleduy. In the YelaW beds,, which foam
the uppermost layers of the Lov~er Cambrian in the 'Siberian
platform.along.the Lena, Botoma, and Alega Rivers., there occur
Archaeocyathus, [A. denius (Volgd.)] and ni~merou& species of
Ethmophyllum LE. abakanen5is 0 ogdo E r.andiperforatum
0 g Iff. heterovallum (VologdlJ".' 91"Ne -archaeocya-
thids found in this horizEn-had been recogn*iz(!d:earlier In the
Obruchevskiy and Sknashtyklollskiy.horizons of' souther 31berla.
Archaeocyathids are not encountered above thit horizon in;;the
Cambrian rocks of the Siberian platform. :Up till now, all the
archaeocyathids which have been found in rockam, In Siberia',have
been confined to Lower Cambrian deposits. This paper gives a.
Card 2/3

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lultmol I 1111141911EMIllimmull 1111 D31 12 HINK 151111. . '. ,

11111111 1111111i1 I IN I Lila

9X-It- -0~41 X_L-_1!V
AUTHOR: None given -5-3-15/37
TITLE; Chronicle of the Paleontological Sec.tion (Kh roj,,.ika: pal eonto.0:1,
logicheskoy sektsii)
PERIODICAL: Byulleten' Moskovskogo Obshchestva Ispytateley Piirody, Otdo'l
162 (USSA),
Geologicheskiy, 1957, N0.3, pp:161-
m
ABSTRACT: The following reports were delivered at a deting of the Palo-
ontological Section, Moscow Society of Naturalikstst from 8
February to 29 March 1957t ' I.T.,Zhuravleva:on "i.rcheocyathl,
Their Development and StratTgraphro ignlTroancell; Yu.V.
Teslenko on the "Age of Fossil Flora of the~~,Villdge Aleksan-'
drovka and the Town of Amvrosiyevka"*, A.A. GriE:elis on "Strati-
graphy of JurassieSediments of the Lithuanian SSR by Fora-.
miniferall; I.G. Sazonova on "New Genus in the Fandly Acone-,
ceratidae from Aptian Sediments of the Russian Plateau"t
Ye.V. Pomina on the "Problem of Association~of the.Upper- and
Lower-Tula Complexes of Foraminifera with Varicas.Carbom-
acec~s Facies of the Tula Horizon of the Mo8co% Coal Basin"t
and Ye..,K.' Shutskaya on "Stratigraphy of the Paleocene and,
Eocene of the Crimea".
AVAILABLE: Library of Congress
Card 1/1

I U.

AUTHORj -5;;3-z-29/37-
urayleva 1eT*
TIT LIS meat and Stratigraphic Signift
~can,64 (ArkIii6tudeit j-ikh::razvitiyfi i sir'atlg'rafichesk6.~G

zna6heni Y-
ye

PERIODICAM bb6hchekt
Byullst9a
!:XOikovxkogo: 7a Isp J?Arodki-~.q e1
r ale
.
-Geologidhes It', 1 5 o -1
k 9- 9 79 It ~3 9PP'114 75:101:1SO
ABSTRLCTs arahoo4athi 000 UVIng In the Siber,"
The author studied
.
plattau making use of the: - available -sit'! 4tl a; hio dait; and
:P 6r P
data of the ontogenesisq'He 6utlined~the'hlhtory Of axoboo-
oyathi development during the Aldan inff:Ltfiia,sjpo0hs of; the
Lower Cambrian periodo In the liddli~ Caiobk 430*riod no~:
authentic aroheboyathi.wers discovere&, 'TWhaterial tnvfjs--
tigated *1 shown- the ooinoidence of
and geographic peaks of archeocyathl.st tAidind of ifis' Ald aw
and the beginning.of thellLena, epoch# 1he eerily~Cazbrisn Sige.
of the 0bruchav,formationg proved already by~'trilobitiisj is
oonfirzed also' by the p"sent data onj~areheiooyathi* !;!be
author advanoes ~a, hyp9thesis -that -the ~loviei 0 Vrian'too %M
-
a' I d - on
tca In view oflits:
can b cons a n n ey dent sys
.Card 1/2 duration-,of p~tjpA;t 3010001000 years ~ancl peouliar palsonto-

-3(0)
,
uOv
,
IMORSi Zhuravleva L
T4
Re int L N Kh ~:V; i
TITLEt Now Data Oonoo= ths strst~ffrl~phy! Ll)i 6i~ OiAr f th
~o 0
wiiii lekaili:,~vaygli.. flrou~o nyy lit iiit
~
Ic4ibirlyi .,,Wi ih 46

PERiODICAL'i
Doklady Aka(16mii~.hauk:.SSSRo:.1956's'~:.Vo 6
ll~123,9i r, i,pp 1 ~.j 095
092

ABSTRAM
interpreting -tho profile ~t thi:' M'i
By
;
~'
(~~IC ~'Psrt of ths
liy&
Rll lhe
t
ri
fjOn W ti

-
ah-of the"JI6 tH
Lower;:,Gambri r iA-XtAAni
4rc
~4841
db o* ''a ti 11 sevelvil nb
~i t
`
i
8
41
o
d
" 4
~ 6
i
a
i
j
the limiesionee! 60htsi i
j~ Arclise
6
~ .h k I 6n
0~y .
d
bior
i
detsrmlue~j-`.2) 'there ~,! is"'ho" aajio6ll~At g bov.t.l
l thm~ diisti i6c ~~d
tlit 'Arttij~mphioail P`Q'oi!tio'n~ "of :the A isilit6 h6 60i; A aoh is
charaoterizid~b~r ailis 61 the Osilandi ~ ~ t,j~ii
. I Nbei I tO
1 .'! T~e`

gdbldgibalvutructure of the' .
~ 1
distriat;
'

lustrated'by figure 1'. Here one can is
i~wm t
o, f o~x n 'a
t ur

;Nidi9`s`pj.r'e`ad he 9,1 ar ,m soive ad gj4;~'L'hIL"&dj ~" COS4
Card 1/3 for!' the do term"ination' of- the

S67/26-1234L37/50
Now Data Concorning~the Stratigraphy of Lower Cambkjan of; 'the Karii iskaYa
TWA,
paleontological me thod becomes very: !~portaht: in thii'arlea.
An iaea of the full str4tigraphical~ o"ic t (., n t, of these~limebtones
could be gained by the 6onstruction, of twol' actual pr~M68 at
the Kiya river. The authors eeparate~~five'layers in,thesf?
ArchaeooyathenAimestones (total thi6lkncss 2300 respicti~ely
1300 m). These limestones comply with;.tlje~B z ikhekil,ho'izon
a a y r
of the Lena stage, according to the':resulto.
The upper part
of the mentioned limestones.belongs,to th6'higher.lying
Sanashtykgoliskiy.horizon, while tho1overmost part'and the
platelike limestones belong to the KAmeshkovskiy hori.zoni This
fact complies (Ref 3) with the upper: par t''of the Aldanskiy -
stage as well as with the Sinskiy, T61bcoMh skiy, and-onel part
of the'Olekminskiy horizon of the Lena Ista'ge in~the,~Iateau.
an t
The under-lying black limestones d~iscbis'lts'(at leiiit 20LOO m
thick) are connected to~the Archaeocyathen'limeston~~ by~grad-
ual transitions. Therefore, they can:only be compared with the,
Aldanskiy stage of the Lower Cambrian:!- T:iel finding of, alga of
the type Newlandia (determination by P. ;3.:Krasnope~,e~a)icannot~
Card 2/3 prove the pre-Cambridn age of the rocks containing them.,The~

.............. ... - --------- -----
3(0)
1
UTHOR:
A

huravleva, 1. T. - SOT/20-5.9 ;124-`2 52/M
TITLE:
a,
The Archaeocyathids of .,the W*JyHorikon on the Kiy liv4r*
'
(Arkhdotsiaty'~b
azaikhsk6g6~gorizonta~r.:Kii)
PERIODICAL: Doklady4kademii nauk SSSR9i:1959, V61 124' fir 1~ t~ pp,.424"427 (USSR)
ABSTRACT: Archaeocyathids' were-found~on1he Xiya-ri4er 1(i~znetskiy a
'
a monogenio calcareons-mass (thiok~aesa 2300 M7'- Ad 9)0 Th e
author
collected: these fossilst if it was possible, &~oeoiding tpi strata.
More6veri findings-made~by'D* V. Nikitinj.111,12~.--1927) T.- X. 3)6mbo~
; Al
id: (1
V
l
e
d L
ti
(1
)
1
a
l
wer
.
u
.
lized.
,an
(1945), V. S- Suvorova
957
953
On the. Kiya river an extraordinary variety of irchaeocyathids' was
.
.
found: several dozens of kinds belongin ~;to 28, enera. T
his c
omplex
V
of archaeocyathids was determined as being &n complex
between the. Kameshkovskiy'and the Sanashtykgollskiy, ioq~ as' being
Bazaikhakiy. This-was confirmed by slmultanoou~slfindings of tri-
lobites (Ref 7). A chiange of the archae66yathi ,da in.the COUTS6 of
time was- observed. The:oldest-ones (Ref.:9) reveal all characteristic'
features of,those.of the Xameal*ovskoye:~ario&i :perhaps of tho Aldan'
period; the most recent ones approacil th~, Sama6btykgol I skiy complex.
Figure I shows a scheme of distribution' of thc 28 genera which have
Card 1/2 been found. The following were described,for the first times

I 11131kill-Millivi I III Hill ~ 1 91
m
amm= ma