SCIENTIFIC ABSTRACT VOLODUTSKAYA, Z.M. - VOLOGDIN, LV.

• Document Type: CREST
• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R001860710005-3
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• Document Creation Date: November 2, 2016
• Document Release Date: August 9, 2001
• Sequence Number: 5
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

SUXLROKOVs V.P.; VOIODUTSLLYA, Z.H. ,
, - t~i
.4~111N~,?~-r 104. ~
Xxtracting acetic acid from undistilled pyroligneous distillate. Der.i
lesokhIm. prom. 2 no.8:12-15 Ag 153. (KLU 6-7)
1. TSentralinyy nauebno-issledovatel'skiy, lesokhimicheskiy institut.
(Acetic acid) (Wood distillation)

SUKA.ROrOV* V.P.; VOWDUTSXA6YA, Z~X~
-
Utraction of Industrial furfaral from furfural oils obtained bjr
woodjMolysim, Der.1 lesokh1m. prom. 3 no.2.-10-12 Y 154. (MIRA 7:1)
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SUMAROKOV, V.P.; VOLODUTSKAYA., Z.M.
Production of high-(raalit7 methylacetate. Gidroliz. i lesokhi--,.
prom. 17 no.7:16-17 164. (14IRA 17:11)
1. NITKhIB.
CROWN EIRM-W, Sx~

SUMAROKOVY V.P.1 VOLODUTSKAYA, Z.M.
Using organic solvents,for the extraction of lov molecular
weight fatty acids Cl..;C from acid sewage wastes from the
manufacture of synthetii fatty acids and fatty alcohols.
Sbor.trud.TSNILXHI no.l4t74-84 161. (KIRA 16W
(Acids, Fatty) (Industrial wastes)

. ..... . . . . . . . . . .
V. P.0 votODUTSV, Z. 14,
2. 'USSR (W)
4. Acetic Acid
7. Concentration of acetic acid with an agent obtained from, wastes of distillation of
birch lumber. Der. i lesokhim. prom. 2, no. 2, 1953.
9. Monthl List of Russian Accessions, Library of Congress, May
1953, Unel.

VOLODUTSKATA, Z. M.
SUKLRDKOV, V- P- ; GUSAKOV, V- N- ; KMY"OV, V. A. ;
Extraction of acetic acid by wood-tar oile from vapor and ~Ls
products obtained in a vertical gas-circulating retort. Sbor.
trud. TSKILIHI no-13%46-59 159. (MIRA 13110)
(Acetic acid) (Wood-Chemistry)

SUMAROKOV, V.P.; VOLODUTSKAYA, Z.H.
Complex esterification of tall-oil acids with n-butyl alcohol.
Gidroliz, i lesokhIm. prom. 16 no.4:7-9 163. (MIRA 16:7)
le Nauchno-issledovatellskiy tekhnokhimicheskiy institut.
(Esterification) (Tall oil)

SUIAROM, V.P.; VOLODUTSKAYA, Z.M.
Effect of technology of production on the composition of black
acetic acid. Gidroliz. i lesoklAm. prom. 14 no-5:" 161.
(MIRA 16;7)
1. TSentrallnyy nauchno-iseledovatellakiy loookhimicheskiy
Inatitut,
(Acatic acid)

SUMARCKOV., V.P.; VOLODUTSKAYA, Z.F.
Complex esterification of tall oil acida with isoamyl alcohol.
Gidroliz. i lesokhim. prom. 17 no-3:11-13 164.
(MIRA 17:9)
1. NITKhIB.

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it
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Url-I!~,

---U-W-DlAj X.N., kand.tekhnsnauk; MATYIR, AsA., kand.tekhususuk; KAMWVA,
X. S. inxh.
Xffeot of cooling conditions on the structure and properties
of keramit gravelso Stroi.mat, 6 no.2sl4-16 7 160.
WA 13 t 6)
(Aggregates(Building materials))

VOIOD-fAYZVA, M.
Notes of & mother of mary children# RabotnItsa 37 no-10:29
0 159. (Childr*n-Managovent) MRA 13:2)

VOIDDTAYEVA. Hariya.
Notes of a mother of Mny children. Rabotnitsa 36 no,8:25-27 Ag
158. (Parent and child) (MIRA 11:9)

VOLODTAYIWA, 14iLriya
~ t
~V children [conclusion]. Rabotnitea
Notes of a nother of several
?. 36 no*9:21-23 S 158, (MIRA 1l.-12)
(Family)
i~,,

7111.7.
A*A.

VO/-01)
YOIM'XO, M-S-, sooluzhemyy vrech Turkmenskoy SSR; ICULIYRV, X.A.
Some data on the occurrence of ppppataci favor in children. Pediatriia
no.8:37-38 Ag 157. (MIRA 10:12)
1. Iz Ashkhabadskogo gorodskogo otdols sdravookhranentys (zav. N.A.
Yolbehin)
(PAPMAGI IBM)

TERENTIYEV, A.P.; OBTEMPERANSKAYA, S.I.; VOLODZIKO, V.Ye.; BUZWWA,
M.M.
Quantitative determination of methyl acrylate by means of
haxamethylenimine. Zhur. anal. khim. 19 no. 1:135-136 164.
(MIRA 17:5)
1.,Moskovskiy gosudarstvennyy universitet imeni Lomonosova.
AM
-77
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t - -,-- ---. t 9-IR MEN RAW.109

OBTEWAAr(SKAYA, S.I.; YOLODZIKI",__V-Ye.
Quantitative determination of alkoxy groups in carboxylic esters.
Zhur. anal.khim. IS no.12:1483-1485 D 163. (MIRA 17:4)
1. Moskovskiy gosudarstvannyy universitat iseni Lomonosova.

AUTHOR: Vologdin, A,_G_.r-x,o-rrespond1ng Membe-,, BOV/2o-121-4-36/54
AS USSR
TIiLE: On the Cambrian of the BsykaJL Highlands as Obtained in
the Course of Investigations of Its Organic Remnants (0
kembrii Baykal'skogo nagorlya po dannym izucheniya yego
organiGheskikh ostatkov)
PERIODICAL: Doklady Akademii nauk SSSR, 958, Vol. 121, Ur 4,
PP- 705 - 706 (USSR)
ABSTRACT: The author gives a survey on the investigation of the
deposits mentioned in the title. The results of these in.-
vestigations lead to a basic change of opinion what regards
the nature of the BaYkal highland. The present opinion of
scientists is that thick pre-Cambrian and Cambrian sediments
are found in the highland, showing a pre-Cambrian and early-
Paleozoic (salairskiy) tectogenesis. Numerous discoveries
of remains of a rich fauna of archaeocyathes (Ref 1) and
partly the rarer findings of trilobitea played an important
part in connection with the establishmnnt of an expert cpinion
an this part of East Sibiria. (Vostochnaya Sibir'), The
Card 1/3 discovery of archaeocyathes along the river Olindo (Oldynda)

On the Cambrian of the 2&AM1 Highlanda as Obtained SOV/20-121-4-36/54
In the Course of Investigations of Ito Organic Rimnantm
in the catchment area of the Vitim river and on other
places revealed the con3iderable thickness of Cambrian
sediments found In some places as well its it complicated
lithological composition. The findings were made by the
"Zabaykalzoloto" trust,N.P.Mikhno, A.K.Guseval K.A.Shakhvaratow.,,
L.I.Salop and others. Determinations were made by: IT.Ye.
Chernysheva, N.V.Pokrovskaya and I.T.Zhuravleva. The author
mentions the main results of his monograph (Ref 1); thus
the far-reaching paleogeol--aphie'al relations of Cambrian
waters in the area of the BW-VCL highland were disclosed
and a detailed.stratification of the sediments became possible.
Thanks to very detailed investigations in t-he well-known
Yangudako-Mamakanakiy district of the highland in the East
'Sibirian Cambrian several paleontological supporting zones
can be eliminated with respect to the fcllowing sequence of perio
Lower Cambria-a, Kolenekanskiy stage - no organic
remnants were found. Aldanakiy stage: with Yangudskaya formationy
containing 4 zones; Lenskiy stage with the last mentioned
mass and 5 zones; Middle Cam~~r4j_with the continuation of
Card 2/3 the Tangudskaya mass and 4 zones; the Mayskiy stage

.On, the Cambri=- of the BayloLl ' Highlands as Obtained SOY/2o-121-4-36/5,v
In the Course of Investigati'ons of Its Organic Remnants
contains the upper Yangudskaya suite. The above mentioned
,divisions are characterized by animal remains as well as
lithologically. There are 3 references, 3 of which are Soviet.
ABSOCIATION: Paloont-,logicheakiy institut Akademii nauk SSSR (Paleontolo-
gical Inatitute,AS USSR)
SIMMITTED: April 25, 1958

BYKOVERI N. A.; VOLOGDINA A. G-.,; MATIVE-M, A. K.; TITOV, N. A.,--a-nd-TAHKUV-,--r----v----
"Geology and Mineral Resources of the Western Districts of the USSR," USSR Geological
Res. Inst., Moscow and Leningrad, ig4l.
--IMMM

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VMYGOIU~ It. G.
UM/Iron Ores Apr 1947
Nineral deposits
"A New Iron Ore Deposit in the Region of the
Lower Angara," A. G. VologdIn, 4 PP
"CR Aced Sci" Vol LVI, No 1
Study of the lower course of the Angara River in
the eastern slope of the Yenisei Range and In the
basIbs'of the Rybnava and NIzhnIaya Oellanka
Rivers where thick deposits of iron ores were
discovered in the simmer of 1946,
8T86

USSR/Geology Oct 1947
Stratification
"The Age of the Metamorphic Stratum of Timan," E. A. Kalfberg,, A. G. Vologdin, 21 pp
I'Dok Akad Nauk SSSRO Vol LVIII, No 1
Lithologic properties and paleontologic characterization of metamorphic stratum of
Timan compared with cross section of same formation of Polar Urals, where Pelingichey
and Shchekurlin layers of K. A. L~vov apparently correspond to Dzhezhim and Bystrin
layers of the Timan.
PA 52T32

VOLOGDINI A. G. PA 67T88
UdOR/Wdlolhe - Algae Jan/Feb 19h8
Yadiolne - Paleontology
"Certain Algae Of the 80-CAlled W*'Tau Brooola
ftion (Khra Tau)-Kazakh 88R)i" A. 0. Vologd1n,
ftlecatol'Inat) Mad Sol USM) lab of Anolent
.Organisma, 9j pp
Xz Ak Nauk SM, Bar Blolog" No 1
Pres.ents charaot6ristlos of Bor6ldiiiphyaus, gen.nov.,
Dwoldaipbyoua borovikovij sp.nov.; Boroldaipbvcus
tek6ktaeniis, spaiov'; and U6'Problematica.' Data
obtained will be*of-us6 In 6tudies*of th6LYet Un_
evaluated paleontologioal material. Submitted
lo oot 3.946.
6'"88

UMM/06010gy Aug 48
Tectonios
Stratification
"The Cambrian Strata In Sikhote-Altn," A. 0. Vologlin,
Corr Hem "AcsA Soi UMM, Lab of Ane Org!Lni ems,,
Palsontol lusto Acad Soi USSR, 4 pp
"Dok Ak Sauk SSSR" Vol LXI, No
Lists forms of the Cambrian depositej grouping them
into tvo divisions but leaving two forms unclassifieL
24A9P34

VOL-CMIN, A. G.
U~M/Geological.Prospecting Apr/~hy/Jun 48
Coal
',*Spberoidal Formations Ymm the Pemian'Strata
44 the Tungueek. Coal' Basin," A,,04-Vologdln
.and N. A. Yeltseyeyp Aoting Hembe 4 `tp
"Upiski V-8 Mneral Obahcb" voi Luvn,, No 2
Necribes composition and possible origin of
strenge epberl~al rock fox tIone dlioovered In
~,isgion around'lover7reaches of Podkam6rknala
'Tui3gunka River. ~Aaaly
sea of'these objects shov
~-that they belchg to coal bearing strata of
,Tungueek Baqln.
114=6

L
VOLOGDIII,A.G.
Solution to the origin of stromatolites. Pr1roda 44 no.9:39-46
S 055. (KLRA 8:11)
1. Chlon-korrespondent Akademil. nauk 5SSR
(Petrology)

-- ----------
f

~U=/Geology Paleontology
Card 1/1 Pub. 22.1- 50/62
-Authors I 'Vologdih, A. G. Memb, Corresp.,of Acad. So. USSR
Title io f-the Sibe an
About conophytons of the Proto'rozo and Cambrian eras o ri
platf orm
Periodict!l I-Dok, All SSSR 102/30 609 611~ May 211,1955
---Abstract ----' I~--Paleontological data-are.prerented on-conophytons (algee-seawoeds) presur-,-
ably from the Proterozoic and Cambrian eras iihich were discovered in some
places.of the Siberian platform. One USSR reforence (1937 and 1938). Draw-
ings; illustrations.
Institution Acad. of Sc., 'UMI, Fale ontological Inst.
Submitt,ed February 4) 1955

USM/ Geology -Paleontology
Card. 1A Pub 22 -.38/46
Authorm Vologdinp A. G.9 Haab. Correa. Acad. of $0.0 USSR
ra in northern Asia
Title i Annular bottomless archeocyatus of~Cambrian e
pariwic, al I Dok. All SSM 103A,, i4l-143, Jul 1. 1955
.--,--Abstract 71 Paleotolotical data-. are given--on the ring shaped-bottomless-Cambrian-era--
traces which were discovered in Northern Asia.- Ten
ferences: 2 Australian 1 Canadianp 1 Eng., 1 Germ.., and 5 USM
e
r
(1865-1954). Drawings.
institution Acad. of So., USSR,~ Paleont. Inst.
-K '17
'7Z

, vOLOGDT4,__A,.a,.; KORLE, K. B.
Somp species of ancient Cyanophytq and their blocenosps. Dckl,.
AN SSSR 164 no.21429-432 S 165. (141RA 18s9)
1. Chlen-korrespondent AN SSSR (for Vologdin).

VOLOODIN. Aleksandr~_grA&pr1yevich; SKULEYKIL, P.A., red.
[The problem of fertilizers and "coal fortilizeran]
Problema udobrenil i ugletuki. Moskvat Znanie, 1965.
70 p. Marodnyi univorsitet: Sel'skokhozialstvennyi fa-
lulltet,, no.9) (MRA l8t9)
1. Chlon-korrespondent Ali' SSSR (for Vologd1n).

VOIDGDINO AOGO
Corplax-septal Archaeocyathidae of the Upper Yx)nok aeries of the
Cambrian of the Western Sayan Mountains. Dokl. AN SSSR 159
no.2057-360 N 164. (MIRA l7sl2)
1. Faleontologicheakiy institut AN SSSR; chlen-korrespondent
AN SSSR.

Find bf h1gan remalni In the Murandava nerlen of the Proterozoic
of the KhIngan Mountains (Far Fast). Dokl. AN SSSR 164 no.31
677-6so s 65. (MIRA 18s9)
1. Paleontologicheskly Inatitut AN SSSR, Chlon-korrespondent
AN SSSSR.

VOID(IDINY A.G.
Find of Upper Slnian alga in the rocka of the Udokan Izr.,ja cf
Chita Province. Dokl. All 5"'!Sh 160 no.2:446-449 Ja 165-
(111111A 18:2)
1. Paleontoloiicheskily inititut All SSSII; chlen-korrespondent
All SSSR.
L, Jmm

V-OLOGDIN, A.G. ,
Discovery of the remains of ionr hu;ye carapace anirmls in the
Karagasskaya serles of the Eastern Saynn Moun*Aln3. Dokl. AN
SSSR 161 no.6sl426-1430 Ap 165. (MIRA 18:5)
1. Paleontologichoskiy institut AN SSM; chlon-korrespandent AN
SSSR (for Vologdin).

SUBBOTINP S.I.; BALABUSHEVICH, I.A.;,VOLOGDIN, A.G.; YJIYLOV, 1.14.
Book reviews. Sov. geIol. 7 no.lltl4P-154 N 164. OGRA 1W)
V

VC, i 0 C!
fird of zlprlg;,..~a
339 C'
AN

the &I I~aqt
Lhb region ~r
114
N ~,4 -
2.

VOLOGDINj A.G,j DROZDOVA, R.A.
Fossil blue-green algaot in the I&U Pro-Cambrian sediments of*
the Par East& Doklo AN WSR 159 no.3t576-578 N 164
(MIRA 18il)
16 Paleantologicheak inatitut AN SSSR. 2. Ohlon-korrespondent
AN WSR (for VologdIal,

VOLOGDM~ A.G.
Cribricyathoal a now class of Archaecyathi. Dokl. ;Ji 53-SR
157 no.6:1391-1394 Ag 164. (141 RA 17: 9)
1. Paleontologichaskly institut All SSSR. Chlen-korreepondont
AN SMR,

V0WGDINj,_A1ekkpa,ndr rjgoZ!.XQy4ch; IORDMISKIY, A.D.p red.izd-va;
Ryr&
At YV , tekhn. red.
(Earth and life; evolution of environment and life on
earth) Zemlia i zhiznl; evoliutsiia sredy i zhizni na
Zemle. Moskvap Izd-vo AN SSMp 1963. 172 Pe
(MIRA 16:12)
(Life-Origin) (Paleobiology)

VOLOGDIN, A.G.
Stromatolitds ani phototropism. Dokl. All SM 151 no.3-.683-686
,Tl 163. (K[RA 16:9)
1. MeontologichesIdy institut AN SSSR; chleri-korrespondent
AN SSM.
(Stromatolites) (Phototropism)

VCLOGDINj,,A,Gt_,
Late Middle Cambrian Archaeocyathidae of the Anga River basin
platform). DAL AN SSSR 151 no.4t946-949 Ag 163.
(MIRA 16:8)
1. Chlen4arrespondent AN SSSR.
(Amga VaUey-Archaec)cyathidae)
SIN I I
OWNIN -"4

VOLOGDINq A.G.
Living legend. Priroda 51 no.12 CL03-104 D 162. (KMA l5t12
10 Cblen-korrespondent AN SSSR,
(Imoda Island-Lizards)
I

9A&O laevioh; KORDE, N.D., red.izd-%-a; SIMKINA,
VOLOGDIH, Ajakamdr r!
---~G.S., tekhn.red.
and algae from the d~tmbrian of the Baikal Upland-]
Arkheotsiaty i vodorosli kembriia Balkallskogo nagorlia, Moskvat
Izd-vo Akad. nauk SSSR. 1962. 3.15 p. 2~ plates"(kkademiia nauk
SSSR. Faleontologichoskii inatitxit. Tz4W.Y, vol. 93).
(KMA 16 3 2)
(Baikal lake region-4rchaeocyathidae)
(Baikal bake region-Alagae, Fossil)

VOLOODIN2 A.G,
Diatomlike organism for the Cambrian of the Tannu-Ma
.mountain rd*p in Tuva. Dokl. AN SSSR 1,46 no,4:909-912
0 162. (MIM 15: 11)
1. Paleontologicheqkiy institut AN SSSR, Chlon-korreepondent
AN SSSR.
(Tanau-Ola Rangp-Diatow, Fossil)

VOLOGDIN, A. G. (Moskva)
"Japan at the dawn of ages" [in Japanese) by M. Hinato, S. Ijiri,
and S. Kaneko. Reviewed by A.G. Volodgin. Priroda 51 no.8:123-
124 Ag 162. (MIRA 15:9)
1, Chlen-korrespondent AN SSSR
(Japan-Paleontology) ~Minato, M.) (Ijiri,, S.)
(Kaneko., S.)

,,. VOLOGDMS A.G. (Mookya)
The moot ancient marine animals. Priroda 51 no.10:85-86 0 162.
(MIRA 15:10)
1. Chlon-korrespondent AN SSSR.
(Archaeocyathidas)

VOLOGDINp A.
Anatomy of Archaeocyathus. Palsont. zhur. no.219-20 162.
. (MIRA 15:10)
1. Paloontologichankiy institut Akademii nauk SSSR.
(Arebasocyathidae)

'4-
?IIA
y=nnz Iyevich; KORDE, K.B., red.izd-va; LAUT,
aG.j tekhn. red.
(The most ancient algae of the U.S.S.R.]Drevneishic vodorosl-i
SSSR. Moskva, Izd-vo Izd-vo Akad.nauk SSSR, 1962. 6f5 P.
(MIRA 15:n)
(Algae, Fossil)
~-I T"
V IVI-30 W-21RUXIED141 PREIRM. ",-:11 1 1 MR-IM W%W165 FOU, Om_ DMUM-ANE"i, W W. IS-09rerVeN

New gemis of singl&-dalled krchaeocyatha with a poeudointermllum.
Dokl.All SSSR 14.5 -m-2.,-EA-W-421 Jl 162. (MIRA 1537)
1. Paleontologicheskiy M.T FAtut AN SSSR. li'Mr-m-korrespondent.
AN WSR.
(T annu- Ola !Z% a

KORDE) Kira Borisovna; VOLDqp:p,.A.Q.,, doktor gool.-minoral.nauk,
oiv.red.; MATUYZi~C6,
T.A., red.izd-va; RYLIKAI Yu.V., tekhn.red.
(Cambri" *ftw of tU o=ttO"tern Siberian Platform] iodoroall
k9mbriJa.IUgo4ostoka Sibirbkoi platformy. Iloskvap Izd-vo Akad.
nauk SSSR', 1961. 146 p. (Akademiia nauk SSSR. Paloontologicheakii
inatitut. Trudy, vol.89) (14IRA 1/,:Il)
1. Chlen-korrespondent All SSSR (for Vologdin).
(Siberian Platform-Algea,, Fossil)
I

VOLOGDJK,,~ (fbelxa)
Witnesses of polar migration. Priroda 30 no.31:102-103 N 161.
1. Chlen~--korrespondent AN SSSR.
(Chihsien region, Chin&-Stromatolites)
I
M
I

~ lz~~ -,.- - - - - - - - - -- . - I -- -
VOLOODIN , A.G.
original method. Priroda 50 no.9:89 S 161. (MM. 14:8)
1. Chlen-ko=eo ondent AN SSSRI, Moskva.
Rina-Fruit culture)

" LO! p ~01 N A -G -
Paleontologic basis for the delineation of the Sinian in Eastern
Siberia. Sov.geole 4 no.5;77-95 W 161# (MA l4t6)
1. Paleontologicheskiy institut All SM.
(Siberia, Eastern-Geologys Stratigraphic)

TOLOODINI, A.G,
Ancient,Cambrian archaeocyathid coenqves of the Oldynda Piver basin
in the Baikal Upl". Dokl. AN SSSR' 136 no.5:1180-U82 F 161.
(KMA 14: 5)
1. Paleontologichookly institut AN SGSR, chlez&-korrespondent AN SSSR.
(Oldynda Valley-Geology, Stratigraphio)

VOLOGDIII~ A.G.
Smo results of studies on Siman doposits of Ilcrth
Biul. MOIP. OTD. geol. 35 no. 3:169-170 My-Je Iff,.
(MRA 14:2)
(Chim-Geology, Stratigraphic)

VOLOGDIN, A.G.
Concerning the article of M.Kenneri ]GY.Pokrovelmia, and A.M.
Rozanov NUpper Cambrian archaeoc7Lth:Ld coral cenosis In the Tannu-
Ola Range, Tuva.' 1xv. AN SSSR. Ser. gaol. 25 no.lOsIO7-109 0 160.
(KnU 13: 10)
(Tannu-01a Range-Gorale, Ybesil)
(Kenner, V.7.) (Pokrovskaia, N.V.) (Rozanov, A.M.)

VOIDOIN, A.G.; MASMY, A.B.
A new group of fossil organisms froa the bottom part of the jUdoca
aeries of the Siberian Platform. Doid. Ali SSSR 134 no,,3:691-693
S 160. W" 13:9)
1. Phleontologichaskiy inatitut Akadomii nauk SSSR. 2. Chlen-
korrespondent, AN SSSR (for Vologdin).
(Usti-lyfjoma ~Vgion--Invertebrates, fossil)

VOU)GDIII, A.G.-
Uew data on Siberian Irchaoc7athidee. XMIADIP.M.geol. 34
no.4:173-174 Jl-kg 159. (KIRA 13:8)
(Siberia-Archeocyathidae)

A.G.
mStromatoporoides In the Soviet Union' by T.I.1kyorskil. Re-
viewed by A.G.Vologd1n. S07.9801. 2 n0-7:160-161 JI 159.
1. Akademlya nauk SSSR.
(Otromatoporoldea)

VOLOGDIN, A.G.
Ontogergr and phylogair of Archaeoc7aths. Trudv Inst.morf.zlhiv.
no.27:79-90 159. (MIRA 13:2)
1. Paleoutolo cheskiy institut AN SSSR.
rArchaeoc7athidas)
WIF
p

VOLOGDIW, A.G.
On the threshold of new discoveries. Nauka I.zhiznl 26 no.9:8,12
3 '59. (KIRA 13:1)
I.Chlen-korrespandent AN SSSR.
(China-Geological research)

VOLOGDIN, A*G
Teraiidas from Cambrian deposts of Chita i1rovince. Jokl. AN SSSR
124 no*5:1133-2236 Y 159. PURA 12.23)
1,Faleontologichaski;r institut AN SSSR. 09M M.Tr=: 4pondent AN
S.S.S.R.
(Chita--Sponges, Fossil)
PIR "W" m4 r-k-WOMMMOMMUM w 19MMIA,

3(5)917(4)
AUTHORx Vologdin, A. G, Corresponding Member SOV120-124-5-49162
TITLE: Tersiidae From Cambrian Sediments of the Chits.Oblastl
(Ters-44-4y kembriyskllkh otlozhaniy Chitinokoy oblaati)
PERIODICAL- Dokla&y Akademii nauk SSSRO '1959., Vol -12,t, I'll! 5, Pp 1133-1136
(USSR)
ABSTRAM The discovery of Cambrlan limeDtones with remains of Archaeo-
Oyathidae and algae in the region of the Gazimurskiy works
(Chita oblast' ) by 114, V. Basova in-0-4-.1duced the disclosure of
Cambrian sediments 4,r, the whole area of Zabaykallye (Trans-
baikalia) and in the upper Amu:r region Ir. 1956, 11. P. Mikhno
found very well preseri-ed Ar4~haeocyaThidae in -the region of
the Zola basir~. For this rea-aon many dew data on the inner
stru-,ture of these old marir~e anituals -,ould be obtained (Ref 1).
Since the evaluation of the entire Mikhno yield is delayed,
the author takes some new fozms which he de,-cr�bes (Tersia
retioulats, ep, n, T, curvntla, sp, r-_., T.. denslus.-ula sp, n.,
Pigs 2: 4-6), Many scientists are inclined no'. to rot-,ard the
entire group of the one-Falled taenial Arrhaeooyathidap as
Card 1/2 independent organiim6 blit as "outerowths" of thc2e

Tersiidae From Cambrian S~--dimerts -of -the Chite Oblast! 3nV120--12.1--r,--II-!,'~-2
Archaeocyathidae or. the bodi&s of which they had developed.
This completely wrong explaration is xefuted by Lumerclus
cases where terviidac were found on the calicos of dead
individuals of Archaeocyathidne (Fip, 1)6, The n-athor matntains
that his invefitigation of the t6raiidfte haa pio-ied their com-
plate independence and that it had demon-5Lrated that it is
impossible to regard them a3 o-at-growths of thooe organismg
which serve as subctratum, for the tersiidao, The found forms
indioated a connectJon of -.hla still insufficiently known
"taphocoenogin'* with '.-,he lover Part of Cambrinn of the
Sikhote-Alin' =cuntain chain, norm-weet :Ioigolia, and the
area of the Salairs~tayrs, geos)m-clinal of southern Siberia.
There ara 2 figurpL; and 3 zefeTence7,,
ASSOCIATIONi Paleontologicheekly institut Akadenii nauk SSSR (Paleonto-
logical Institut"e of the Academy of S,:Aencea, USSR)
SUBMITTED: November 7956
Card 2/2

Corrennond ing
AUTHOR :
AzAdemy of jcience3f V,;4.t
TI T1,7: The Lower Canbrian Foraminifera o1' ',Niva
(Ni7hnek-embriynk1ye foraminifo.-y nivy)
Doklady .~'.kadomil Nnuk 19513# Vol. 17.), Nr 2,
PP. 405-4C6 (U',f)71)
ABSTRkCT: The up to now nearce rests of foraminifera in c~vnbriun
oediraents we-e cumplett!J in '1957 by the d1rouvery Of trie
mentioned J*auna. The audhor d1acoverud He. residues of
inicrafauna In a specimen (if the ot,',Iecti.~n ef ar, nywo.--yatiAd-
limen (by G.N. -,ukashev, A1.1-Union Geslogicall '7n~tu--.u
Vaesoyuznyy geologicheakiy, institut). -he material
-0 , n f -'I
from the s,,uthern slope of the Tarinu la cha' , Jm 0111
valley of the Irbitey river. It is tt,ue that later ci
Ye. R~~-ytlinger Cave up her original view that thel.-
foraminifera, 'out the aut'hor sticks to th(; A'.-, rm e j -C.
because one -.f the earliest groups of pr,,)tozorins in
concerned and the simplIcity as Weil a~ the primitivity
of the shell crrreapond with iti geoloeical [q#.-. The
Card 1/2 following new systerntio categorlen are set up: ~-:rder

The Lower Cambrian F:)raminifera of Tuva 2 -.1 2 - 5 2,!6 3
ReAtlingerellld% Vologd. In tiddition to thitt 11 fal'-.111un
are set up, 6 of which are new and doijerflood 1'.i Uils
They are: Tuvaellina Vologd., Bnatrycho.-:nria Vo)r,4,P~i.,
Flexurel Vologd., Kordt-ella Vologd. (::nvifcjr!i
la
1946), (Obruchevella Reitl., 1946) , *,u k a-s-ch ti v c- "I i , V c, 1 C' C
Leb,-devuftlla Vologd. ind Reltlin,~.!ertljrj Volot:d. In all
I k
cases systematic descriptionz, are. given.
the shells of the described types.
There are 1 filKare and 3 referencr_-n, 2 of which are ~,'nvic-.
ASSOCIkTION: 11aleontologicheskly institut '.kademil nauk
(Palaeontological Tinstitutp IA-2 ur?n)
SUBMITTED: December 28, 1957
1. Foraminifera-USSR 2. Geological time--Determination
3. Paleoecology-USSR
Card 2/2

VOLOU'D[6, A.G.
Lower Cambrian foraminiferas of Tuya. Do;cl. AN SSSR.120 no. 2:1405-
408 My 158. OuRA 11:7)
1. Ps Tent-&IogiabeBkiy institut-Alf SSSR. Chlen-korrespondent All
SSSR.'
(Tuva Autonomous Province-Foraminifers, Fossil)

VOLOODIN, A.G. ..
. ~-~ On'certain species of planktonic and benthic Archaeocyathidae.
Dokl. AN SSSR 116 no.3:493-496 S .157. (MIRA 11:2)
l.Chlon-korrespondent AN SSSR.
(Archaeocyathidas)

VOL,-)
AUT4OR: Vologdin, 1. G., Corresponding Member of the 20-4-43/52
AN USSR
TITLE: On the Onthogenesis of Archaeocyatha (0b ontogeneze,
arkheotsiat).
PERIODICALt Doklady AN SSSR, 1957, Vol- 117, Nr 4, pp. 697-700 (USSR)
ABSTRACT; Because of the vastness of the material available, the
present work cannot be expected to give a complete and full
report on the problem. The numerous attempts hitherto made to
classify the Archaeocyatha type were mostly based upon the
structure of the cup in the full-grown stage. The utilization
of ontogenetic data for the purpose of building up their
phylogeny was rendered difficult by the insufficiency of the
material available concerning skeleton morphology and by the
difficulty of obtaining amial longitudinal sections in
transparent ground sections. Furthermore, the initial part of
the cup was very small. The author had very much material at
his disposal, which made it possible to tackle the solution
of the problem in hand. Among the morphological types of
cups the author already a long time ago sorted out a group
Card 1 /5 of irregular multi-chamber skeletons) which are composed

On the Onthogeneais of Archaeocyatha 20J"3/52
of porous lamellar calcareous formation (genera
Labyrithomorpha and Sajania, fig. 1,1). Besides this
morphologically antiquated type dating back to the lower
Cambrium. and the lower Middle Cambrium, many forms having
a porous one-walled skeleton, sometimes with an interior
honeycombed tissue, can be traced (Bacatooyathus, Cambrium).
Also in later Cambrian Archaeocyatha-layers the author
discovered such types with one wall which had, however, the
rudiments of coarsely-porous bottoms (Thalassooyathus, fig-1,4).
It is from these hollow, one-walled types that the one-walled typea
with a honeycombed tissue originate, from which (by the types
with one bottom) a whole class, the tabularidae LRef. 83
originated. From the forms with a honeycombed tissue those
with double walls split off at rather an early stage, which
were either hollow or had a honeycombed tissue'in the cup.
They were sorted out by the author as an order for themselves.
By the development of irregular pin-like formations in the
skeleton and of a honeycombed tissue, the group branched off'
primitive, one-walled taenia-shaped forms. (Thersia,
Card 2/5 Thersiiden) From these the doub Ile-walled taenia-like types

20. 52
On the,Onthogenesis of Archaeocyatha 4-43/,
(Potechinocyatus, fig. 1,6) as well as all "Protopharethrides"p
and Archaeocyatha (in the new form) and others with or
without honeycombed tissue originate. From the Archaeocyatha
towards the end of the lower Cambrium "Archaesiconides"
originated by the formation of convec bottoms. The rare
"protocyclocyatheall (fig- 1,7) acquired a ringed interior wall
and the taenia. In many respects they remind one of the regular
separating walls of the "Septaideall (regular Archaecyatha).
The Protocyclocyatha were also by mistake claseed among the
latter group. The genuine septal Archaeocyatha, the Septaidea,
began with an original capsule, passed through the stage of
one-wall development, and, after acquiring skins of honeycomb-
like tissue, they develo ed regular partition walls.
(Loculocyathus, fig. 1,8~. The honeycombed tissue was lacking
in the Ajacicyathus (fig. 1,9). This group branched off from
the phylogenetic original stem at a very early stage, i.e.
about in the lower third part of the lower Cambrium, The
further development of the Loculocyathide, as regards shape,
was very varied. It is important that the Archaeocyatha,
which had double walls with partitions and bottoms, which
Card 3/5

On the Onthogenenis of Archaeoeyatha 20443/52
had formerly been olassod among the doublo-walled forms
with bottom of preceding groups, are of a quite different
origin. By the discovery of the now species
Coscinocyathella (fig. 19 11) it was possible to determine a
stuge, which pointed straight in the direction of the species
Labyrinthomorpha. A kind of the latter genus (of the Binium -
Cambrium boundary) wao probably the primogenitor of all
coacinocyathides. The species Labyrinthomorphaq however,
continued to exist independently. In the case of Lueolocyathides
and Coscinocyathides recapitulation was often weaker because
the stages reflecting the morphology of original forms were
non-existant. Some new acquisitions are due to convergence.
There are I figure and 8 references, all of which are
Slavic.
Card 4/5

Ontthe Onthogenenis of Archaeo cyatha 20-4-43/52
ASSOCIATION: Paleontological Institute A14 USSR (Paleontologicheskiy
institut Akademii nauk SSSR)
SUBMITTED: September 27, 1957
AVAILABLE: Library of Congress
Card 5/5

VOLOGDINO A.G.
On the structure of'the internal organs of Arch"oeyathidas, PokI,
AN SSSR 114 no.5:1105-1108 Je 157. Wak lotg)
1. Chlon-korrompondent AN SSSR. 2. Paleontologicheekly Instit A
SSSR.
(Archasocyatidae)

VOL 0C_h41_A1,
AUTHOR: Vologdin, A. G. , Corresponding Membcr All USSR 20-3-,9/46
------------
TITLE: -
On Certain Bptcits ~)f Planktonic and Benth ic Archaeocy2thidae
(0 neskollkikh vidakh planktonnykii i benticheskikh arkheotsiat)
PERIODICAL: Doklady AN SSSR, 1957, Vol. 116, Nr 3, PP. 493-1!96 (USSR)
ABSTRACT: There are frequently found very strange forms amongst the abun-
dant material of skeleton morphology from the Kambrium of the
USSR. The author diocovered a large quantity of sinall calcerous
formations which he first considered to be larvae or early stagen
of the same Archaeocyathidae and which he called "Spaerion" or
"Fietulall respectively, In several places of Sibotria greater
formations were discovered which were sometimes isometric, at
times somewhat prolongated, but always without symptoms of a se-
ttled life. Originally they were called "Dolium-stage", which, as
was presumed, preceded the settled stage in the case of some
Coscinocytites. This was not confirmed. Such and similar fossils
must be oGnsidered now as remainders of independently existing
Archaeocythidae. After having passed through a larva stage they
developed a very lightly built skeleton and did not settle on 'he
bottom, but lead a plankton-life. Their residues fell down to
the ground only after death. Planctonic Archaeocythid&~. Repres-
.
.
..
I
'
Card 1/3 t
h
iu life.
e.-ntativea of various orders c
ould apparent
1y ltad

On Certqin Species of Planktonic and Benthic Archaeocyathidae. 20-3-3,%!1.6
First there wa3 no connection or relation foand with the ber-thic-
forms. they are cla:;sified accordine to thi following criteriors:
a) isometric structute of the skeldbn without traces of attach -
inent to the "substrate", b) Porosity and plate-shape of the ele-
ments of the skeleton, c) Integrity of the outer shell uhich
consisted of skeleton- elements and a soft coat of tissue
(voith Flimnaerzellen), d) syvaiietric axes of the skeleton, provid-
ed they suffered no ulterior deformation. Cliss �21)taAdea. Fami-
Ij TabulocZathidae Vologd.p 1956. "-he skeleton consisting of each
two wall- and bottom- pieces. Genus Szecyathas Vologd.Gen.nov.
T,ype: Sz.cylindricus Vologd.sp.nov. distribution. Ivarovskiy-re-
gion, Altai, Lower Kambrium. Sz. irreguliris Vologd.sp.nov,
same distribution. Sz. (speci7s__Uz~~1;0,fl n) spinov. Distribution:
Sanashtykgol river, West Sayanen, middlt Kambrium. Genus Lu-
cyathus Vologd. gen. nov. skeleton druni-or egg-shaped. Ty-pe
L.elegans Vologdin sp. nov. Dictribution: Lebed river, Altai nl~d
Sanashtykgol river, West Sayanen, middle Kambriura, Benthoo-Ar-
chaeocyathidae, Glass Septaidea (a Arqh&52w!ha nezalaria Vologd.,
1937), family Leegath Vologd.faua.nov. Genus Lteclathus Vologd.
gen.nov. Types Archaeocykt~p_yavorskii Vologd. 1936, Lower Kati-
brium of Kusnetsk-Alatau. Fitmily Cosciliocyathellidae Zhuravl.1956
Card 2/3 genus Tannalacyathue Vologd.gen.nov. type: T. Multi ex from the

On Certain Species of Planktonic and Benthic Archieocyathidaa. 20 -3-39,~ 46
river Big-Shangan (Bollsho7 Shingan) in the system of the river
Elegest, Republic of Tuva. Age. Presumady lower layer of middle
Cambrium. All new systematic categories quoted are fully descri-
bed. There are 5 figures (fig. 2& -table after P-484), 4 referen-
ces, 3 of which are Slavic.
ASSOCIATION: Paleontological Institute of AN USSR (Paleontologicheskiy institut
Akademii nauk OSSR)
PRESENTED:
SUBMITTED; October 2, 1956
AVAILABLEs Library of Congress
Card 3/3

0 C_
') //~~ 4 6- 20-5-53/60
~v!~110R VOLOGLI11 A.G.,Corresponding, :eimber of the Academy.
TITL,I-' On the Structuro of the Internal Organ of Archacocyathluea.
(K stroyeniyu vnatrt.-nego or~~ana arkhootsiat -Russian)
W
PLRIODICAL Doklady Akademii'Nauk SSSR,1957,Vol 111jjNr 5,pp 1105-1100(U.S.S..a.)
ABSTIUCT The author first described the nature of skeletons of this group on
the material of Archaeocyathus lizicatones of the lower part of !.he
!Liddle Cambrian from the northern slope of the Xuznetsk Ala-Tau.
Among the specimens of usual conservation state he succeeded in
finding one with preserved soft parta9probably a consequence of ra-
pid calcination and burying at the bottom of the water basin.Besi-
des other nart3 and organs described in detail,remainiag structures
of soft tissues were preserved in the central cavity where, as it
turned out,an internal"'o"r'gan that had to fulfill metabolism fundt-
ions existed.The remarkable opeolmen was determined by the author as
Archaeocyathus demboi Vol. (Ajacicyathus accordin.- to the new no-
menclature). He succeeded in atu6ying this find on only one single
cross sectioiT of the cup. In a study of a collection of Archaeocy-
athus limestones from Trans -Baykalie (11azimur works,Zola river ba-
sin) the author succeeded in discovering quite a lot of Archaeocya-
thus remains with partially preserved soft parts in form of vari-
ous systematic positions.One of those deserves to be described in-
dividually:class Septaidea, order Loculocyathida, family Leecyathi-
dae,species Leecyathus Vologdin,1957,type of species:Archaeocyalhus
Card 1/2 yavor;kii Vol.,1931,from the lower Tersi riveT,Lower Cambrian of~ the

20-5-53/60
Cn Lhe Structure of the, Internal Organ of Archaeocya-
thidea.
Kuznetsk Ala-Tau.

1-cecyathus mikhnoi Vol.sp.nov. fro
m the Zola river baoir..Accord-
ine to.the structure of the septa the form belongs to Leecyathuc,
but the structure of the intervals,thc noptal and the iitterval
coefficients do not allow identification with L.yavorakii T11 ore 1*,~,re
it is cla5sed anion-:- a new opeciev.The diar7nosio of s-,erie:3 !~hail
bc eupplemientod by tho raro presence of cuticlea of veoicular tif,-
sue In the internal cavitiou of thr. cup.The structure of the nanal
a,ystem reminds us of that of a later Archaeocyattiuat;;cmato3,11rinx
dichotomica Liagk. from the Upper Silurian in the Ural.The here des-
cribed forn apparently is able to propagate by a larval ata~;e as
well as by buda.Age; Torgashin horizon.Accompanyin- types are eriv-
merated.
(2 fig-, 4 Slavic references).
ASSOCIATION Paleontological Institute of the Academy of Science3of the U.S.S.A.
PRES-112111TED BY
SM-NITTED 23.4-1957
AVA 1 TA 3 LE Library of Cor.-ress.
Card 2/2

"'JowaDIN, A.G.
Oldest representatives of Archaeocyath& fron the eastern
slope of the Yenisey Mountain Ridge. DokI. AN SSSR 110 no.
6:1085-1088 C 156. (MLRA 10:2)
1. Chlon-korrespondent Akademii nauk SSSR. Palsontologichookiy
institut Aimdemli nauk SSSR.
(Yentsey Ridge-Arebasocyathids,e)

TOLOGDINo A.G.
------ WO-ONWMW---
Stratigraphic significance of Archo4acyath&. Dokl.AN SM 111 no.l:
185-187 N-D 156. (KLM lo: 2)
1. Chien-korrespondent Akademil nauk SM. 2. Palsontolop,4cheskiy
institut Akademii nauk 5 = .
(Archaeocyathidas)

TOLOODIN, A.G.
Classification Of the Archasocyathidae. Dokl.AN SM ill no.4:"7-
880 D 136. (MM 10:2)
1. Chlon-korrompoodent Akademit nauk S=. 2. Paleontologicheakiy
institut Akademil nauk SM.
(Archasocrathid")

VCLOGD1N, Aleksandr Gri&E!yevich; FAYNBOIN, I.B., red.; ATROSHCIDMO,
-----------
EPaleontology and search for mineral resources] Faleontologiia
i poiski poleznykh iskopsemykh. Moskva, Izd-vo *Znanie.* 1960.
27 P. (Veasoiuznoe obshchestvo po rasprostraneniiu Voliticbookikh
i nauchnykh zaanii. Ser.9, Fizika i khimiia, no.11).
(MIRA 13:7)
1. Chlen-korrespondent Akademil nauk MR (for Vologd1n).
(Paleontology, Stratigraphic) CProspecting)

Now method of protecting propeller shafts by rubber sleeves.
Sudostroenis 26 no.8:5CL51 Ag 16o. NEU 130.10)
(Shafting-Corrosion) (Rubber coatings)
Nov.

ACC NR. AN7006816 -'-----'-sOURCE,
AUTHOR: -Www- D.v.
ORG: none
TITLE: NovIca "water bus" (hydrofoil]
SObRCE: Lenir-radslcaya pravdi, no. i10, 16 Feb 67j p. 41 cOl- 1-4
0
TOPIC TAGS: inland watoxvay transportation, hydrofoil, ship
~BSTLRACT:
Soon, new hydrofoils of the Nevka-type will be replacing the Volga water
taxis" operating in Yalta, Sochi, Sukhumi, and other ports. Designed in Lenin-1
grad under chief designer D. V. Vologdin, the Nevka has both open and closed
passenger sections. This hydrofoil is intended for use in the coastal areas
of seas and in rivers and lakes, The hull will be able to rise 80-100 cm
above the water, thus making it possible to operate in a sea state of 2-3.
It will carry 14 passengers and will reach a speed of 30 knots with its
250-hp diesel engine. Instead of an inclined propeller shaft, the shafts.
will be equipped with angular reduction gearings.
[NC)
$UB CODE: 13/ SUBM DATE:"- none/ ATD PRESS: 5116
4/
A UDC: none

VOLOGDIN I
V#2ding in the assombly-of 2arge-panel apartment houo9e. Ha
Otroi. Roe. no.9:6-7 S 161. (MM 14-'10)
1. Nachallnik evarachnoy laboratorii treats. No,103 Glavnogo
Ioeningradekogo uprayleniya po zhiUahchnomu i grazhdanskomu
atroitalletvu,
(Concrete reinforcement-Welding)
(Precast concrete construction)

BENUA, F.F., kand.tekhn.nauk; VOLOGDIN, I.V., inzh.; KATIRR, A.I., kand.takhn.
nauk
Investigating the effect of vibration on the cr7stallization
process and structure of built-up weld metal in the submerged
arc process. Svar. process. Svar-proizv. no.5:1-5 My 158.
(MIRA 11*6)
l.laningradakiy institut inzhenerov vodno o transporta.
(Electric welding) (Solidification5 (Vibration)

VOLOGDINJ, I.V., lnzh.; I,IIFTAKIIOV,, R.Sh., inzh.
Reslatance volding in tho production of comtruction elemonta.
Svar. proizv, no.10:29-31 0 163. (MIRA 16tl:L)
1. Treat No*103 Glamnogo Leningradskogo upravleniya po zhilishchnomu
i grazhdanskomu stroitellstvu.

137-58-1-ZO60
Translation from: Referativnyy zhurnal, Metallurgiya, 1958, Nr 1, p 279 (USSR)
AUTHOR: Vologdin, 1. V.
TITLE: Resolving Power of Gamma Analy sis of Welded Butt Joints
(Razreshayushchaya sposobnost' gammagrafirovaniya svarnykh
stykovykh soyedineniy)
PERIODICAL: Tr. Leningr. korablestroit. in-ta, 1956, Nr 19, pp 79-90
ABSTRACT: Data on gamma analysis of welded buttjoints are generalized
and the sensitivity threshhold for discovery of minimal defects
in welds is revealed. Experimental investigations have estab-
lished the fact that cracks open to >0. I mrn may be discovered
by the ordinary type of gamma-ray radiography (source C0601
focal length 500 mm, thickness of metal 5-60 mm).. The con-
clusion is drawn that gamma-ray radiography cannot be employed
as a universal method of inspection -of butt welds, and that it
should be combined with ult-?,asonic and magnetic inspection-
V.G.
1. Welded jointa-Gamea analysis
Car4 1/1