SCIENTIFIC ABSTRACT SEMIKHATOVA, S.V. - SEMIKIN, I.D.

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• Collection: Scientific Abstracts
• Document Number (FOIA) /ESDN (CREST): CIA-RDP86-00513R001547910017-6
• Release Decision: RIF
• Original Classification: S
• Document Page Count: 100
• Document Creation Date: November 2, 2016
• Document Release Date: August 9, 2001
• Sequence Number: 17
• Publication Date: December 31, 1967
• Content Type: SCIENTIFIC ABSTRACT

S7, i7rrL 29
USSR/Geology Carboniferous 11 Oct 50
"Lower and'Middle Carboniferous in the Gorlkiy
Region.," S. V. Semikhatova, All-Union Sci-Res Inst
of Natural Gases
"Dok Ak Nauk SSSR" Vol LXXIV, No 5, PP 1003-1007
New data processed in the Institute is used to
throw light upon geological history of region.
Data on Carboniferous rocks given by A. N. Petrov"'
skaya; foraminIfera detd by G. D. Kireyeeva; corals
-by T. A. Dobrolyubo~,a; and Brac4ppoda by author,
Submitted by Acad_D. V. Nalivkin 14 Aug 50.
am 172T29

1. SEMIKHATOI[A., S.V.K.
2. USSR (600)
4. Geography & Geology
V..~ -4
7. Stratigraphy and6~~g&dpi-czrl history of the Devonian and Carboniferous on the Russian
Platform. Moskva, Gostoptekhizdat, 1951
9. Monthly List of Russian Accessions, Library of Congress, February, 1953.Unclassified.

1. S?,MIKFATOVA, S.V.
2. USSR (600)
4. Moscow Basin - Geology, Stratigraphic
7. Boundary between the Bashkir and Moscow formations of middle Carbon. Dokl.
AN SSSR. 86, no. 6, 1952.
9. Mont List of Russian _ArX&Uj=, Library of Congress, Feb 1953. Unclassified.

SIMIKUTOVA, S.T., redaktar.
[Petroleum and natural gaa
part of U.S.S.R.)] Voprosy
(gyropeiskaia chast' SSSR)
geology cad geoahemistry (3kropean.
geologii i gookhimii nefti i gaza
Moskv&, Gostoptakhixdat, 1953. 382 p.
(KLRA 7:11D)

SF,MMA OVA. S.Y.
__ - ~-- ............ - - "-"
History of the middle Carboniferous period in the Russian Platform. Biul.
MOIP. Otd.geol. 28 no.4:33-52 '53. (MLRA 6:9)
(Russian Platform--Geology, Stratigraphic) (Geology, Stratigraphic-
Russian Platform)

1. IWIAY-LENKO, P.A., SE)EMATOVA, S. V.
2. USSR (6oo)
4. Don-Medveditsa Uplifts - Geology, stratigraphic
7. Deposits of the eshkirian stratum of the Middle-Garboniferous period in the
southern part of the Don-Medveditsa uplifts. Dokl. M SSSR 88 'no. 3: 1953
9. Monthl List of Russian Accessions, Library of Congress, April -1953, Uncl.
~~-L

SXMIEMO S,.*V.; NAZAIIOVA, V.A.: ROSTOVTSEVA, L.F.; N"IVKIN, D.Y., akademi1c.
I -- S-`!~"
The Turneisk and lower part of Vizeisk strata of the Orel river region in the
Dniemr-Donets deDreBBion. Dokl.AH SSSR 92 no.1:147-150 3 '53.
(MI-RA 6:8 )
1. Akademiya nauk SSSR (for Nalivkin). 2. Vsesoyaznyy naachno-issledovatell-
skiy institnt-prirodTifth gazov (for Semikhatova, Hazarova and Rostovtseva).
(Orel valley--Geolop-v, Stratigraphic) (Geology, Stratigraphic--Orel
valley)

aMIKHATOVA S.V.
Tournaisian deposits in the lower Volga Valley, Donets Basin, and
southeastern Dnieper-Donets Lowland. Trudy VNIGNI no.6:12-35 '55.
(MLRA 9: 11)
(Volga Vallay~-Geology, Stratigraphic)
(Donets Basin--Geology, Stratigraphic)
(Dnieper Lowland--Geology, Stratigraphic)

SMIKEEATMA, S.V.
Mw= atage and its significance to the Carboniferous stratigraphy
in the U.S.S.R. Biul.MOIP.Otd.geol. 30 no.5:75-104 S-0 155-
(Geology, Stratigraphic) W2A 9:1)

15-57-5-585C-
Nr
Translation from: RefLerativnyy zhurnal, Geologiya, 1957, 1 -
p 20 (USSR)
AUTHOR: Semikhatova S V.
TITLE: -Choristites of the Group Choristites mosquensis Fischer
From the Middle Carboniferous of t Don-MedveRtsa
Uplifts and Their Stratigraphic Significance (Khoristity
gruppy Choristites mosquensis Fischer v srednem karbone
Dono-filedveditskikh podnyatiy i ikh. stratigraficheskoye
znacheniye)
PERIODICAL: Tr. Vses. n.-i. geol.-razved. neft. in-ta, 1956, Nr 7,
pp 73-116.
ABSTRACT: The author describes and illustrates eight species of
brachiopods (four of these are identified approximately)
from the upper part of the Moscovian series (Podol'skiy
and ?Jyachkovo horizons) from the Archediniiko-Dontkoy rdgion
andthe village of Zhirno~e on the Medveditsa River. Mor e
Card 1/3 details are fUrnished for Choristites mosquensis, the

Choristites of the Group Choristites mosquensis (Cont.)
15-57-5-5854
varieties of which have 1) a sinus that broadens in the anterior -part
of the ventral valve, 2) a strongly beaked ventral valve, and 3)
rather thin ridges. The specific content and course of development
of Choristites mos uensis in this region are the same as in the
central part of the Russian platform. The group thrived in Podol'skoye
time and died out at the end of the Myachkovo interval. But at the
time that this group was the principal form in the Moscow basin,
other varieties were also present, whereas in the Archedin5ko-Donskoyregim
the group was not only dominant, other forms (Choristites priscu~
and C. trautscholdi) were extremely rare. The general character of
the sediments, t r thickness, and also the fossil content show
that the Carboniferous deposits of this region are of the platfo :' rm
type and should not be considered transitional to the Donets type.
However, the path of migration for the fauna through the Middle
Carboniferous connection between the Donets sea and the seas of the
central and eastern regions of the Russian platform passed through
the southern part of the Don-~,Iedveditsa uDlift zone. There is
reason to believe that at the end of Moscovian time there was a small
general uplift of the Voronezh massif, but this view needs support
Card 2/3 ~

15-57-5-5854
Choristites of the Group Choristites nos uensis (Cont.)
by further comparative lithologic and paleontologic studies in the
Carboniferous of the region of ttie Moscow basin and the Don-Medve-
ditsa uplifts. The paper has seven tables and a bibliography with
53 references.
Card 3/3 T. G. S.

SEMIMATOVA, S.V.; CHIZHGVA, V.A.
ft-~6
Stratigraphic correlation-of the Toux-nalsian P-nd the lower Vise-=
stages in the Mikhaylmsk6.ve uplift (southeastern section of the
Dnieper-Donets Lowland). Trudy VNII no.9:53-62 '56. (MLRA 10:1)
(Dnieper Lowland--4eology, Stratigraphic)
(Donets Basin--Geology, Stratigraphic)

P1STR&K, R.M.; SZKIMTOVA, S.,V.; PLSMVICH, Ye.I.; VERBYSUU, X.N.
Stratigraphy and lithology of the lover Carboniferous of White
Russia. Ixv.AX SM.Ser.gool. 21 no.4:59-?6 Ap '56. (KLU 9:8)
1. Soyuznaya geologo-polakovaya kontora Ministerstva neftyanoy pro-
myshiennosti &SSR, Moskva.
(White Russia--Geology, Stratigraphic)

SEMIKEATOVA, 181-v-.-
Stratigraphy and geological history of lower Carboniferous Kizel
horizon deposits. Biul. MOIP.Otd.geol. 31 no.15:126-127 S-0 '56.
(14LRA 10: 3)
(Geology, Stratigmphic)

SEKIKKATOYA, S.; SAZONOV, N.
Conference of the All-Union Petroleum Scientific-Research Institute
for Geological Survey on the stratigraphy of the lower part of the
lower Carboniferous. Geol.nefti 1 no.10:69-71 0 157. (MIRA 10:10)
(Geology, Stratigraphic)

S-~:, II~-.: '!,- zi I I
I I '. -~, - .- i4~, . F .
:~*3:,riti~,-n,.phic importance of the Nam-arian stage. Tr-rdly VUIGNI
nt-.8:92-137 '57. (KIRL 12:2)
(Geology, Stratigraphic)

3 "A
AUTHOR: Semikhatova, S.V. 5-6-20/42
TITLE: Some Problems in the Stratig-raphy of the Lower Part of the
Lower-Carboniferous System (Nekotoryye voprosy stratigrafii
nizhney chasti nizhnego karbona)
PBRIODICALt Byulleten' Moskovskogo Obshchestva Ispytateley Prirody. Otdel
%Zeologicheskiy, 1957, # 6, pp 133-135 (USSR)
ABSTRACTs In April 1957, the All-Union Scientific Research Geological-
Survey Petroleum Institute (VNIGNI) called a meeting dedicated
to the stratigraphic problems of the lower part of the Lower-
Carboniferous system.
The author cites the stratigraphic scheme accepted by the
meeting and proposes some correlations between the subdivision
of the European USSR of this scheme with the corresponding
formations in Western Europe, basing his suggestions on the
comparison of paleontological data.
AVAILABLEt Library of Congress
Card 1/1

The Upper-Kizelov Strata Near Buzuluk,-Chkalov Province.
less silicified, 'little loam material.Similar limestones,tredominant-
ly organogen-detritus containing,with 45-6eo organic relics.kmong
them foraminiferae,ostracodae,Crinoideac and ostracode splinters as
well as pieces of tubular algae.In th upper part secondary dolomi-
tes occur with numerous single corals and bits of Crinoideas; 3rd
packot,21 m thick,consiats of gray limestone of all shad es,mostly re-
cry8tallized;nuiacrous Ipats of fine-grained carbonateNleae) and lon-
tils of black flint. n the limestone a rather abundant fauna,however
with few species,as above,is reprsonted.Among the foraminiferas those
with few windings as well such wi-th a high number of windings are
predominant-4th packet,24-74 m thick, consists of limestone,at the
bottom with few intermediate layers of secondary dolomites,and thin
layers of dark-gray sid*rites and black flint.Lima is grey,prodomin-
antly containing organogen-detritua,consisting of algae-Crinoid,lae,
unevenly dolomitized in layers silicified.Dolomite is light-and dark
-grey to almost bl&ck,highly recrystallized,caleareous at the bottom,
pyritized,solid,on the top with rar* incorporations of bluish-groy
anhydride.Tho organic relics,here only appear,sporadically give evi-
dence of the secondary nature of the dolomite.Fauna of foraminiferao
has become very poor with the same arrangement of groups as in the two
following packets.Coralindeterminable owing to bad conservation.In
the overlying layer pf this packet the modification of the combination
of the foraminiferae-and brachypoda.()stracodes are Dresent in several
Card 2/4 intervals-5th packet,24 m thick;separates according'to the relief of

AJTHOR SEMIKHATOVA S.V.,RYZffOVA A.A., ROSTOVTSEVA L.F. 20-4-47/61
TITLE The Upper-Kizelov Strata Near BUZULUK,-Cbkalov Province.
(Verkhneki zelofskiye a loi bliz Buzuluka Chkalovskoy oblasti
- Russian)
PERIODICAL Doklady Akademii Nauk SSSR,1957,vol 113,Nr 4,pp 889-892 (U.S.S.R.)
ABSTRACT These strata were here disclosed for the first time. They form an
almost 2oo m thick mass which consists mainly of gritstones and in
the upper 48 m of terrigene rocks. Sea fauna is abundantly repre-
sented. The region is situated at the northern borde of the Caspian
depression.As lower limit of the mentioned strata the authoressos
take the bottom of the Rakov-mass of V.M.Pozner. The Upper Kizelov
-strata are deposited near Buzuluk in a depth of 287o m. The upper
boundary is taken in a depth of 2686 m, at a depth where the Kize-
lov-fauna is relieved by spores of the carboniferous horizon.lts
thickness is 184 m. In both boundaries there is a stratigraphical
incoincidence. At the Buzuluk cross-section these strata are sepa-
rated inb 6 pakets, 1st packet, 28 m thick, with high silification,
terrigene sediments present, fauna poor. Rock is represented by dark-
gray limestones, partially recrystallized, loamy-dolomitic at the bot-
tom, siliceous-loamy higher up, in layers pyritized. Lenticularly
black flint occurs. In the lower part-badly preserved brachypoda,so-
matimes silicified Crinoidea segme nts'Ev;rrhere gravel spicules from
Card 1/4 funei, rare ostracoda* and,Archispaeren. I packet, 38 m thick, is

The Upper-Kizelov Strata Near Buzuluku,Chkalov province. 20-4. 147161
its fauna.Lithologically not very different to the 4th packet. Lime-
stone highly recrystallized.Fine-and small-grained calcite and less
lump-shaped micro-grained carbonate serve as cement.Among the brachy-
poda the Chonetes dalmanianus,which is characteristical for the 3rd
and 4th packet, here only appears sporadically.The moat numerous are
Megachonetea zimmermanni and Pustula cf.pixidiformis.At the bottom
Spirifer-species and in an intermediate layer Cacrinella aff. and ata
as well as frequent orthothetines-relics were found.In different
depths cor&ls(5 species) and oatracodes(5 spedies) era numerous.The
6th(terrigene)packet,47-84 m thick,is composed of alternating marls,
a.rgillites,dolomites,and lime-loams, loamy limestones as well as do-
lomites and in the top contains intermediate layers of flints and si-
derites.In the anss-section argillites are predominant.In some ar.-il-
lite3 intermediate layers there are relics of corals,brachypodouses,
pelacypodae and Crinoidae in high number.Morcover single ostracodes,
fish relics,spores and pieces of vegetable tissues.In limestones there
is a similar fauna,mormover pyritized plant relicB.piecas of moss ani-
mals,trilobates,tubular algae and single badly preserved foramini'f*-
ra. capsules.According to the foraminifera and brachypodL the packets
I.-V.could be compared with the mass of Rakow and possibly with the
lower Malinov-masses of V.M.Pozner.L.p.Rostovtseva compares according
to the foraminiferae the packets II.-IV.with the IV.-V.-masses of the
Card 3/4 Pilyugin cross-section and the packets III.and IV.with the Gubakha-

The Upper-Kizelov Strata ii ear Buzuluku,Chkalov province,
packet.Tht brachypoda-complex of the V!.packet has no analogy in the
kizelov faunae so far known.According to the foraminiferae the packet
VI. ought to be classified to the kizelov horizon.V.A.Chizho,,ra ClaSS41
fies the packets III.-VI.according to the ostracodes into the upper
part of the Kiztlov horizon.The brachypoda found in the Buzuiuk cross-
section: Chonetes dalmanianus,Pustula cf.pixidiformis,Spirifer konin-
cki,Sp.Aff.attanuatus offer the possibility to classify the here des-
cribed sediments into the productus sublaevis-zone.At the same time
the entire above mention-ad fauna of brachvpoda confirms the necessity
of classifying this zone among the Wiesa and not among the Turna as
in the Donez-basin on the east sloDe of the Ural and in Western
Europe.
(3 citations from Slavic pub-lications).
ASSOCIATION Allunion-Scientific Research Institute for Geological !diner&!-Oil
Explorations.
PRESENTED BY Strakhov N.M.,Member of the Academy
SUBMITTED 22.10-1956
AVAILABLE Library of Congress
Card 4/4

L
AUTHOR :21alKHATOVA zjovq~YaJNA L.K~,DALMATSKAYA I.I~ 20-5-48/67
TITLE 'TFe_1Fc6c__o_w itaae of Middl~_, Carboniferous in the Meleke3s Depressian.
(Moskovskiy yarus Srednego karbona v Lelekesskoy vpadine -Russian)
'PERIODICAL Doklady Akademii Nauk SWR,1957,Vol 113,Nr 5,pp 1119-1122
Received 7/1957 fieveiwed 6A957
ABST?ZACT The deposits of the Moscow stage near the city of kelekess(in th%~ terri-
tory of Kuybyshev=ziamare)-Nare laid open in a depth of 1167-7d5 m, The de-
posits of the Verey horizon(44 m) are concordantly stratified on tne rocks
of the upper part of the Bashkir stage.This horizon is subvidided into 3
lithological stratified packets.Tne lowest(S m)consis-".-s of limp-stone witn
a sparse admixtures of clay and intermediate strata of aleurites and dolo-
mites.In limstone there is a lot of organogenic detritus of foraminifera,
crinolds.brachiopods,and algae.The middle packet(3o m)is a varYinR strati-
fication of clays,marls,aleurites,limestone,and rare dolomites.Clays are
predominant,with 7_270/,~aleurite-admixture,with calcareous intermediate
strata which contain fragments of crinoids,orachiopods,as well as remains
of plant tissue and lentiform intermediate strata of crusted brachiopod-
shells.The Kasn).r horizon consists of 2 stratified packets.Tne- lower one
(22 m)consists of limestone with inferior dolomites.The top packet(60 m)
consists of limestone with thin clayeyintermediate strata,its structure,
however,is on the whole similar to that on tne lower packet.Tne Fodol ho-
rizon is at the top f aintly cha-r2aterized D.,r fauna and its boundary is
traced according to electric carrotage.Compared to the Kashir horizon the
Cara 113 dolomites are here more developed than the limestone.Among limestene,alga-

Tne Moscow itage of Middle Garooniferous in the Yelekess 20-548/6'(
Depression.
ltmestones are enarateristic.3 stratifiec. packets: h2,,"),and 36 a-In.
lower organogenic -detritt: clayey limestone with thin dolomite-intermedia-
te strata and lentils of green clay dominate.Among the remal-ris of orGan"sim
there are up to 2o/u bryozoa-flikes,elsewhere UP to 1501'v siphonic-algae.
In Uve. second packet dolomites witn clayey in"termediate strata and rare
prints of brachlopods predominate, inclus ions of gypsum, anhydrite, ana flint
are found.The top packet is chiefly built of organigenic-detr-itic limesto-
ne with dolomite-intermediate strata in the middle part.The Myachkow ho-
rizon consists of limestone with dolomite-and clayey intermediate strata.
as in the Fodol horizon.There are three pacKets: 6,5,25,and 60 m.Also he-
re anhydrite,gypsum,and flint are to be found.The first packet consists of
organo.-detritic limestone with clayey intermediate strata,freqiaently suca
of shell-rock are up to i,5-3 cm tnick.Tne second packet consists or dolo-
mites with intermediate strata of organogenic-5plintery and sometimes oo-
lithic iimestone.Foraminif era and brachiopods -were determined. The thira
packet consists of varying stratifications of !=,estone,dUcmiteana t;1in
clayey strata of similar cnaracter as on the top.Tne tota.1 thickneas of
the deposits of tnt, koscow stage amounts in kelekess to 363 m and tnus
surpasses tnose of the rignt bank of the Volga to some extent.Accurdmg to
tne rock-types of tne single horizons and the total composition of the fau-
na the deposits of thi.5 stage In lielekess are equal to the deposits of tne
same age in thie Tataric vault and In the centrai parts of tOe ayn-
Gard 2/3 ecaysis altnougn loca-1 peculiarities are to be notices,

ETNOI, 011gerd Leonardovich; WIg
AaQVA -6j. , prof., red.; DAYEV, G.A.
vedushchiy red.; GXNNAD 6 khn. re d.
[Studies on the stratigraphy of Carboniferous deposits of the
eastern borderland of the Volga-Ural petroleum province (mountain
region of Bashkiria)] Issledovaniia po stratigrefii karbons vo-
stochnoi okrainy Uralo-Volzhekoi neftenosnoi oblasti (Gornaia
Bashkiriia). Pod red. S.V.Semikhatovoi. Leningrad. Gos.nauchno-
tekhn.izd-vo neft. i gorno-tomlivnoi lit-ry, Leningr. otd-nie,
1958. 193 P., maps. (MIPM 12:2)
(Bashkiria--Geology, Stratigraphic)

IL'INA, kand-geologo-mineralog.nauk; YELINA, L.M.;-IffZHOTA, A.A.;
BUZINOVA, V.M.; INITRIYEVA, L.Ya.;.GIMPELZVICH, S.D. 1 GALAKTIONOTA,.
N.M.; IL'INSKAYA, V;V.; SOLOVIYEVA, N.S.; X&RASXV, H.S.; BAKIROV, A.A.,
red.; VEBER, V.V., red.; DANOV, A.V., red.; DIKENSETLTN, G.Kh., red.;
MAKSIMOV, S.P., red.; POZNYSH, M.A., red.; SAIDOV, M.N., red.;
A S V , red.-, TURIUMITAUB, N.M., red.; 'OL'YANOV, A.V., red.
1W
ceased ~.N, D.S.,.red.; SMA AYEVA, Ye.V.. red.; CHIZHOV,
A.A., vedushchiy red.; YASHCHMHINSKAYA,.A.~.. tekhn.red.
(Coal deposits of the contral provinces of the Russian Platform]
Kamennougollnye otlozheniia tsentrpl,1nykh_oblqstei Rasskoi platformy..
Pod red. N.S.1111noi. Leningrad, Gos.nauchno-tekhn.izd-vo neft. i
gorno-toplivnoi lit-ry, 1958. 209 p. (MIRA 12:3)
(Russian Platform--Goal geology)

FLEROVA, O.V0, kand. geol.-mineral. nauk, red.; BAKIROV, A.At. red.; VEM,
V*Ve, red.; DAROVg AAe, 'red.; DIKETSMYN, Gn., *red.; MAKSIKOT.
S.P.- red.; POZIM, M.A., red.; SKOOT, M.N. red SSMIMTOVA,
9 - it
-Aj,,-red.; TU 'TAUB. N.M,, red.; KHALTURIN, D.S., re
SHABAIRVA, Ye.A., red.; ZARETSKAYA, A.I., vedushchiy ied.-, FIDOTOVA,
LG,# teklm. red.
[Mesozoic and Tertiary deposits
Rassian Platform] Mezozoiskie i
nykh oblastei Rasskoi platformy,
Goo. nauchno-tekhn. izd-vo neft.
291"p4
of the central provinces of the.
tretichi3ye O'tiozhaniia isentrall-
Pod red. O.V. Flerovoi. 14oskva,
i gorno-toplivnoi lit-ry, 19589'
(MDA 11:10)
1. Moscow. VsesoiuzW nauchno-iseledovatel'skly geologo-razvedoch-
nn neftyanoy institut.
(Rmssiaix Platform-Geology', Stratigraphia)

YILIPPOVA, fkgriya Filippovns, Va nd.geo 1. -minor. nauk, ARONOVA, S.M.; AFREMOVAj
H.F.; GI%IAKTIOITOVA, IT.M.; GASSANOVA, I.G.; GIKPBLEVICH, B.D., KARASET.
M,S.; LYASBEIKO, A.I.; MAYZEV. Z.L.; PATEYEV, M.A.; SOKOIDVA, L.I.;
SOLOYtYF,VA, II.S.; KUNIII, A.A..; SHISHENINA, Ye.F.; SBNEYDER, H.P.,
BAKIROV,, A.A., red.; VEBIR, V.V,, red.; DAHOV, A,V., red.; DIKEN-
SHTEYII,, G.Kh., red.; RAUIIIOV, S.P., red.; POZ14YSH, M,A., red.;
SAIDOV, M.N., red.; SIZUKUTOVA, S.V.,, red,- TUIKELITAUB, II.M., red,;
" of
ULI TANOV, It. V., AMUR 111, D.S red. ; SHA3AYEVA,
Ye,.A., red.; RAZINA, G.M., vedushchiy red.; G.101111ADIAWA, I.M., tekhn.
red.
[Dc.~vonian deposits in the central arovinces of the Russian Platform]
Devoriskie otlozheniia tsentralInykh o1blastei Rurskoi olatformy.
Pod red. M.F.Filippovoi. Lenizvrad, Gos. nauchno-teK-hn.izd-vo neft.
i gorno-toplivnoi lit-ry, 1958. 404 o. (1-11-RA 11:4)
(Russian PLatform--Geology, Stratigraphic)

-_,_,~~!~IKIIATOVA, S.V.
Stratigraphy of lower Carboniferous terrigenous formation in
the Volga-Ural area. Ge6l.nefti 2'no-3:30-35 Mr '58.
(14IRA 12:6)
1. VFJeSO".Zrjy7 naticbno-issledovatel'skiy geo logo -razvedo chwy
neftyanoy institut.
(Volga Valley--Geologr. Stratigraphic)
(Ural Mountain region--Geology, Stratigrapbic)

SEMIMTOVA, S.Y., RTZHOVA. A.A., DALMATSKAYA, I.I.
Middle Carboniferous sediments in Buzulak District, Orenburg
Province. Geol. nefti Supplement to no. 7:68-74 '56. (MIRA 1l.-8)
I. Vsesoyuznyy nauchno-issledovatellskiy geologo-razvedochrkvy
neftyanoy inBtitUt.
( Buzuluk District--Geology, Stratigraphic)

SZMIMkTOVA, S.V.; ULDIA, L.M.
Carboniferous sediments. Trudy VITIGNII no. 10:41-51 158.
(MIRA 14:5)
(Russian Platform-Geology, Stratigraphic)

SEMIKKATOVA. S.V-. _,- ~. t:1
.. I
Tournal and earlier Vis'e' time in the Russian Platform. Izv. AN
SSSR. Ser. geol. 23 no.2:12-24 F '58. (MIRA 11:5)
l.Vseso7uzn7y nauchno-issledovatellskiy geologorazvedochnyy
neftyano7 institut, Moskva.
(Russian Platform--Geology)

lk'k,, " 0 - 2 6 c
q'
AUTHORS: Semikhatova Yelina, L. M, , balaa~r3'_--ya, 1. 1.
TITLEt Deposits of the Bashkirskiy Stage in Melekess (Otlozheniya bashkirs-
kogo yarusa v Melekesse)
FERIODICAM Doklady AN SSSR, 1958, Vol. 118, Nr 2, PP. 381 - 363 (USSR)
ABSTRACT: These sediments are deposited with a stratigraphio discordance on
the rooks of the Protvinskiy horizon. The gap in the sedimentation
manifests itself here inphe development of lime-conglomerates and
in a high secondary change of the rooks in the upper part of this
m thick and lithologically
horizon. The Bashkirskiy stage is 45
subdivided in 2 horizons of lcral importance. The exact identifica-
tion of the latter may be carried out because of certain local
differences of the foraminifers. fauna. The lower horizon (probably
analogous to the Molotovskiy horizon) is 26 m thick and consists
of light-gray and white limes which are highly recrystallized and
highly silicified, and which contain flint-inclusions and clay-
-admixtures. With regard to fauna crinoid-foraminifera-limes pre.-
dominate, those contAining brachiopods and other fossils of animal
groups are more seldom represented. The foraminifers. fauna makes
assume an analogy with the Molotovskiy horizon, but the Pseudostaf-
Card 1/3 fella are too scarce for this. On the other hand the occurrence of-

I 20-2-50/6o
Deposits of the Bashkirskiy Stage in Ifelekess
differences of the fauna stand in the complexes render their assi-
milation difficult. Nevertheless the upper complex may be equated
with the upper part of the Podvercyakiy horizon (according to the
first occurrence of Aljutovella and Verella). The first occurrence
of Schubertella, here miGht be explained by its belated penetration
to this part of the viater. Thu3 only the upper half of the sedi-
ments of the Bashkirskiy sta6e is apparentlY present in the blele-
kess. There is no Cap between the Bashkirsk-iy- and Vereysl-,iy sed-i-
ments, here. The Bashkirskiy sediments at the right bank of the
Volga approximately have a similar extension in the Uljanovskiy
support bore-hole, but the thickness here decreases toward the
west to 25 m and still further. These facts reflect the existence
of apparently large elevations during the Carboniferous.
ASSOCIATIONt All-Union Scientific Research Institute for Petroleum Geology and
Prospecting ~Vsesoyuznyy nauchno-is3ledovatellskiy -eologorazve-
dochnyy neftyanoy institut)
PRESENTEDs March 14, 1957, by S. I. Mironov, Academician
SUBMITTEDs March 14, 1957
AVAILABLE: Library of Congress
Card 3/3

_5AM1KHATOYA, Sof I.Y r
,prof.; TELINA, Lyuboy' Mikhaylovrw;
N~
Antonina Alekeandrovan; BTYSMA, Tamara Vladimirovna;
DALMATSKAYA, Irina Ippolitovna; DOBROKHOTOTA, Sofiya Yasillyevna;
MIHYAYEVA, Yevgeniya Geor--iyevna; ROSTOVTSEVA, Lidiya Fedorovna;
2AIUITSKAYA, A.I., ved.red.; POLOSINA, A.S., tekhn.red.
[Studies on Carboniferous sediments of the Yolga-Ural oil-bearing
province] Materialy k izueheniiu kamennougolinykh otlozhenii
Volgo-Urallskoi neftenoonoi oblanti. Pod red. S.V.Somikhatovoi.
Moskva, Gos.nauchno-tekhn.izd-vo neft. i gorno-to-Dlivnoi lit-ry,
1959. 206 p. (MMa 13:3)
(Tolga Talley--Geology)
(Ural Mountains--Geology)

SEMIKHATOVA, S.V.
Stratigraphy of the lower part of the lower Carboniferous. Trudy
VNIGNI no.14:5-30 '59. (MIRA 12:10)
l.VaesoyuzW nauchno-icRledovatellskiy goologorazvedochny7
naft3ranoy institut (VNIGNI).
(Russian 1-Utform--Geology, Stratigraphic)

SEMEMTOYA, S.; MAKAROTA, T.; IVANOVA, Z.; FILIPPOYA, M.
Precized unified diagrams of the Faleozoic 3tratig7aaph7
of the Volga-Ural oil-bearing province, 1960. Geol.nefti
i gaza 4 no.6:52-3 of cover Je 160. (MIRA 13:7)
(Volga Valley--Geology, Stratigraphic)
(Ural Mountain region--Geology, Stratigraphic)

DAWATSKAYA, I.I.; LATSKDVA, V.Ye.; ORLOVA9 I.N.; RAUZER-GBEENOUSOVA9 D.M.;
REYTLINGM, Td.A. - SAFONqU; T-.P-j- SEMIKHATOVA, Ye.N.; CITMOVAq Ye.I.;
y 0 P
SHATSKUp N.S.9 akademik, gJAv. red.; KENNER9 V.V 9 zam glav. red.;
prof-.',' red. - toma; KATLYAREVSi4A, P.S., red. izd-
va; NOVICHKOVA# N.D., tekhn. red.
[Regional stratigrapby of-the U.S.S.R.) RegionalInala stratigrafiia
SSSR. Glav.'red. 14-.S.Shatakii. Moskva. Vol-5. (Stratigrapby of the
Middle Carbaniferoud sediments of the central and eastern parts of th's
Russian platform babed on-the studies of Foraminiferal Stratigraftia
srednekamennougollnykh otlozhenii tsentrallnoi i vostochnoi chasti Rus-
skoi platformy (nA osnove izucheniia foraminifer). Ft,2. [Volga and Koma
Valleys] Pavolzble i Prikamle. 1961. 355 P. (MIRA .14:8)
1. Vsesoyuznyy nauchno-issledovatellskiy geologorazvedochnyy neftyanoy
institut (for Dalmatska7a),_2. Institut geologicheskildi nauk AN SSSR
(for Rauzer-Chernouso-way Heytlinger). 3. TSentraltnaya nauchno-
issledovatellskaya laboratoriya Upravleniya, neftyanoy promyshlemosti
Permskogo Sovnarkhoza (for Safoncka). J+. Nizhnevolzhskiy filial Vse-
soyuznogo nauchno-isolodovatellskogo geologorazvedochnogo neftyanogo
institute (for Lat~kovaq Orlova, Chernova). 5. Rostovskiy go,-rLdarstven-
nyy universitet (for Semikhatova , Ye.N.)
(Volga Valley-Paleontology, Stratigraphic)
(Kama Valley-Paleontologyq Stratigraphia)

SEYIIHATOVA. S.Y..
Veroya horizon in the southern wing of the Moscow syneclise and the
eastern part if the Russian Platform. Dokl. AN SSSR 140 no.6:
1403-1406 0 161. (MIRA 14;11)
1. Vsesoyuznyy nauchno-issiedavatellskiy geologorazvedochnyy
neftyanoy institut. Predstavleno akademikom D.V.Nalivkinym.
(Russian Platform--Geology, Stratigraphic)

SEIMMATOVA S~11~~ CH-FZHC7uA. VcA-,~ IMIMPIAH, O.M.
StratigraL,hy and fa!,j.es of the Lower Carboniferous of the Kam --
Kine!5 Derresalion. Tniely VIIII no.34.2-71-280 162, (MIPA 141. ;t)
(K.iybyshev Stratigraphi-n)
0
(Orenburg Prav.~Lnce--Geology, Stratigraphic.)

SE2,,IKHATOVA, S.V., prof., red.; YUNGANS, S.M., ved. red.; FEDGTGVA,
G.'-j.tekh-Ln. red.
[Stratigraphic diagrams of Paleozoic sedirznts] Stratigrafiche-
skie skheqr paleozoiskikh otlozhenii; trudy. Moskva, Gostop-
tekhizdat. Vol-3. (Carboniferous system]Kamennougollnaia sistema.
Pod red. S.V.Semikhatovoi. 1962. 321 p. (MIRA 15:5)
1. Soveshchaniye po utochneniyu unifitsirovannykh stratigrafi-
cheskikh skhem poleozoya Volgo-Urallskoy neftegazonosnoy pro-
vintsii, Nioscow, 1960.
(Geology, Stratigraphic)

S&MIKHATOVA, S.V., prof., glav. red.; FILIPPOVA, M.F., red.;
MAKAROVA, T.V., red.; IVAJ[OVA, Z.P., red.; CHULKOVA,
V.V., red.; BEI(MAN, Yu.K., ved. red.; POLOSINA, A.S.,
tekhn. red.
[R solutions of the Conference on the Study of Accurate
Ulfication of Stratigraphic Scales of the Upper Proterozoic
and Paleozoic in the Volga-Ural Oil and Gas Region held in
Moscow at the All-Union Scientific Research Institute of
Petroleum. Geology and Prospecting, February 12-20, 19601
Resheniia soveshchaniia po utochneniiu.unifitsirovannykh
stratigraficheskikh skhem. verkhfiego proterozoia i paleozois.
Volgo-Urallskoi neftegazonosnoi provintsii, sostoiavshegosia
v Moskeve pri WNIGNI s 12 po 20 fev-ralia 1960 g. Moskva,
Gostoptekhizdat, 1962. 47 p. (MIRA 16:5)
1. Soveshc.ianiye po utochneniyu unifitsirovannykh stratigra-
ficheskikh skhem verkhnego proterozoya i paleozoya Volgo-
Ural'skoy neftegazonsonoy provintsii, Moscow, 1960.
(Volga-Ural--Geology, Stratigraphic)

SEMIXF-ATOVA, S. V.
Rrachiopoda from the key sections of tho Bashkix otage -11i
m~iunt'alnous %ahkiria. Trudy VNICNI no,43:180-22", 164
N,IRA 18:2)

- :z T:. Gi -. P,.~ F3, r .~ S.
b- _-. - , ~., - , . ; --- V~., .'.
Brachiopoda ir the bomdary layers of the Tournai and Visean
stages nf the -%zulith test hole no.1 ard stratuig-ra-phic
significance. Trudy VNfCZ"I no.43:124-145 !64
18.-2)

SMI,91KHATOVA, S.V.
Co,-relation of the ITIamur of Western Barope with a cross section
of the Carboniferous of the Russian Platform based on the de-
velopment of Brachiopida. B4.ul. MOIP Otd. geol. 40 no. 6:150-151
ff-D T65. (nm 19:1)
I. Submitted May 13, lc)65.

7 - -T-,'L' ,TO`",e. ,;.
"The -S-1--l-dly of Fusulini:Is a-ii the St-rati=arhy of the C--rborftif---cus 1-:os-s of -Ur-
1-11 - 41---
a~gion of tho Doxi-Iedvedit5a a-i sloe ations ,' Dz)L-. A:11, 52, No. 06, 1946. 1,.-br., :-'Ostov-
on-Don State Univ. ira. V. Al.j. ,.' lotov, -Jnl~6-.
10

15- 57-2-1278
Translation from: Referativnyy zhurnal, Geologiya, 1957, Nr 2,
p 11 (USSR)
AUTHORS: _,~..~hatova, Ye. N., Lazareva, Ye. P., Chelmokayeva,
S. S.
TITLE: New Data on the Strati.graphy of the Lower Tertiary
Deposits in the Stalingrad Volga District (Novyye
dannyye k stratigrafii nizhnetretichnykh otlozheniy
Stalingradskogo Povolzhlya)
PERIODICAL: Uch. zap. Rostovsk.-na-Donu un-ta, 1954, Vol 23, Nr 5,
pp 93-97
ABSTRACT: Bibliographic entry
Card 1/1

DAIMATSKAYA, I.I.; LATSETA, V.Yd.; ORLOVAq I.W.; RAUZER-CBERNOUSOVA, D.M.;
REYTLINGER-9 Te.A.; SAFON07A'I' T.1I-."J"SDfIKHATOVA., Ye.N.; CEERROVA9 Ye.l.;
.9 ~
SHATSKIY 9 N. S. 9 akadeinik , glav. red -9~ -.V---za"-m glav. red.
J)
SE14IKHATOVA9 S.V.9 prof-.',-red.-toma; KATLYAREVSi4i, P.S.v red. izd-
va; NOVICHKOVA2 N.D.9 tekhn. red.
[Regional stratigrapby of"tba U.S.S.R.] Regionaltnaia stratigrafiia
SSSR. Glav. red. N'.S.Shatakii. Moskva. Vol,5. (Stratigraphy of the
Middle Carboniferous i*diments of tho central and eastern parts of the
Russian platform babed on the studies of Foraminifera] Stratigrafiia
arednekamemougollnykh otlozhenii tsentrallnoi i vostochnoi ebasti Rus-
skoi platformy (na, osnove izucheniia foraminifer). Ft.2. (Volga and Koma
Valleys] Povoloble i Prikamle. 1961. 355 P. (MIRA 34:8)
1. Vsesoyuznyy muchno-issledovatel'skiy geologorazvedochnyy neftyanoy
institut, (for DaImataka7a)-,'2,, Inatitut, geologicheskikh nauk AN SSSR
(for Rauzer-Chernousova, Reytlinger). 3. TSentralInaya iauchno-
issledovatellskaya laboratoriya Upravleniya. neftyancy promyshlennosti
Permskogo Sovnarkhoza (for Safonc(7a). 4. Nizbnevolzhskiy filial Vse.-
soyuznogo naucbno-iselodovat6lskogo geologorazvedocbnogo.lieftyanogo
instituta (for'Lats'kovap Orlaval.Chernova). 5. Rostovskiy gosudarstven-
nyy universitet (for Semilchatova , Ye.N.)
(Volga Valley~Paleontologyy Stratigraphic)
(Kama Va-lley-Paleontologyq Stratigraphic)

GOLIDFARB, Emil' Mikhaylovich; KRAVTSOV, Aleksandr Feodoelyevich; RADCHIM0,
Irina Ivanovna; ROZ3NGART, Yuriy Iosifovich;
ZaALlovich-;r TAYTS, Hoy Yurlyevich, prof., doktor tek-hn. nank, red.;
CHUMACHENKO, T., vedushchiy red.; BESPYATOV, R., tekhn. red.
[Calculat-ions for heating furnaces] Raschety nagrevatelinykh pechei.
Pod red. N.IU. Taitsa. Kiev, Gos. izd-vo tekhn. lit-ry USSR, 1958
421 p. (MIRA 11:8)
(Furnaces, Heating)

__-
Technical indices of 6pen-hearth furnace performancee Izve v7s,
ucheb; zavo; chern. met,. no.12:139-145 '60a (MIRA:~4.-J)
k
L, Dnepropetrovski7 metallurgicheskiy ~nstit-Rt.
(Open-hearth furnacps)

-D
PHASE I BOOK EXPWITATION Mr/5556
Moscov. Institut stali.
Novoye v teorii i praktike proizvodntva martenovskoy stall (71ev (Developments]
in the Theory and Practice of Open-Ifearth Stee ng) Yoscow, Retallurgizdat,
1961. 439 P. (Series: Trudy Mezhvuzovskogo nauchnogo eoveahchaniya)
2,150 copies printed.
Sponsoring Agency: Ministerstvo Vyaohcfp, i arednego spetsiallnogo obrazovaniya
RSF-jR. Ynskovskiy institut stali imani 1. V. Stalina.
Eds.: 'M. A. Glinkov, Professor, Doctor of Technical Sciences, V. V. Kondakov,
Professor, Doctor of Technical Sciences, V, A. Kudrih, Docent, Candidate of
Technical Sciences, G. N. Oyks, Professor, Doctor of Technical Sciences,
and V. 1. Yavoyskiy, Professor, Doctor of Technical Sciences; Ed.: Ye. A.
Borko; Ed. of Publishing House: N. D. Gromov, Tech. Ed.: A. I. Karasev.
YJRPOSE: This collection of articles in intended for members of scientific
institutions, faculty members of schools of higher education, engineers
concerned with metELUurg-lcal processes and physical chendstry, and students
specializing in these fields.
Card 1/14

Hew (Developments] in the Theory (Cont.) SOV/5556
COVERAGE: The collection contains papers reviewing the development of open-
staff
hearth steelmaking theory and practice. The papers, vritten by
members of schools of higher education, scientific research institutes,
and main laboratories of metallurgical plants, were presented and discassed
at the Scientific Conference of Schools of Higher Education. The following
topics are considered: the kinetics and mechanism of carbon wddation; the
process of slag formation in open-hearth furnaces using in the charge either
ore-lime briquets or composite flux (the product of calcining the mixture of
lime with bauxite); the behWior of hydrogen in the open-hearth bath; metal
desulfurization processes; the control of the open-hearth thermal melting
regime and its automation; heat-engineering problems in large-capacity
furnaces; uerodynamic properties of fuel gases and their flow'in the furnace
combiuition chamber; and the improvement of high-alloy steel quality through
the utilization of vacuum and natural gases. The following persons took
par'. in the discussion of the papers at the.Conference: S.I. Filippov,
V.A. Kudrin, M.A. Glinkov, BP. Ham, V.I. Yavoyakiy, G.N. Oyks and Ye.
V. Chelishchev (Moscow Steel Institute)j Ye. A. Kazachkov. an& A. S.
Kharitonov (Zhdanov Metallurgical Institute)j H.S. Mikhaylets(Institute of
Chemical Metallurgy of the Siberian Branch of the Academy of Sciences USSR);
A.I. Stroganov. and D. Ya. Povolot kiy (Chelyabinsk Polytechnic Inatitute);
P.V. Umrikhin Ural Polytechnic In:titute); I.I. Fomin (the Mollcow "Serp i
itut-)
molot" Metallurgical Plant); V.A. Yukley (Central Asian Polytechnic Inst
Card 2/14

New [Develop=nts3 in the Theory (Cont.) SO11/5556
and H.I. Beylinov (Night School of the Dneprodzerzhinsk Metallurgica Institate
References follow some of the articles. There are 268 references, mostly Sarlet.
TABU OF COYMM:
Foreword 5
Yavoyakly, V. 1. [Moskovskiy institut sts3i - Mosoxr Steel Institute].
Principal Trends in the Development of Scientific Research in Steel
Manu:facturing 7
Filippov, S. 1. [Ptofessor, Doctor of Technical Sciences,.Moscow Steel
Institute]. Regularity Patterns of the Kinetics of.Garbon Oxidation 15
in Metals With Low Carbcn Content
EV. I. Antonenko participated in the experimentaj
levin, S. L. (Professor, Doctor of Technical Sciences, Dnepropetrovski-y
metallurgicheakiy institut Dnepropetrovsk Yetallurgital Institute].
Card- 3!14

Nev (DLvelopmnts] in the Them (Cont.) SOV/5556
Grigorlyev, V.P. (Engineer], and Te, V, Abrosimov [Mocov Steel Tnstitate';.
Effect of the Chemical Co =_aition of the Charge an& Slag on the Dephos-
pborization Process in an Oxygen-Blawn Bath 305
Svinolobov, N.P. (Engineer], and I.D. SemIkLn (Professor],
(Dnepropetrovsk M-Aallursical Insff'EW_;-0BTAining a Luminous Flv=
in Open-Hearth Furnaces Pired With Natural Gas 315
Ol,orvkovo N.T. [Professor, Doctor of Technical Sciences, Noscov Steel
Institute]. Electromagnetic (ruductivel Stirring of VztaI in Melting
Furnaces 324
Semnenko, I.I. (Engineer, Metallurgicbeskly kiambinat im. Serove.
MetaUurgieal Combine imeni Serov). Combustion of Hlgh4ulfur
Content Mazaut Gasified in the Open-Hearth Fort in Making High-
QuaUty Steel 330
Discussion of Papers 332
Card 11/ 14

9
S0: Monthly,List of Russian Accessions, Library of Congress, 195J, Uncl.

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109

USSR/Cultivatecl Plaarnts - Commercial. Oil-Bearing. Supr- M-5
Bearing.
Abs Jour : Ref 2hur - Biol., No 20, 1958, 91760
Author : Semikhnenko, P.G.
Inst : All-Union Scientific Research Institute of Oil and
Essential Oil Dearing Crops.
Title : Working Between the Rows of Sunflower Sowings.
Orig Pub : V, sb.: Kratkiy otchet o nauchno-issled. rabote.Vses. ff.-i.
in-ta maslichn. i efiromaslichn. kulltur za 1956 g. Kras-
nodar, "Sov. Kuban'", 1957, 244-249.
Abstract : No abstract.
Card 1/1
USSR/Cultivated Flal,ts - Comiercial. Oil-Dearin,,
.~. Su,,_-Lr-Deari:.-,.m
Abs Jour Ref Z::ur Diol., No !8, 1958, 82442
0 Aut?ior Sez:d_k!-,i,e:1ko, P.G.
7
~_~st iM-U:dio7i Scientific Research L,stit_,.te of Oil-Beari:.G
1
_-.d Esse:itial Oil-Boari..-.c CitItures.
Title Methods of Lntercroppi:~r_ Su:,.flowers
Ori~, Pub Byal. nal ~chno ilfform. Vses. n.-i. in-t maslichn.
i efiroz-,aslic'.-Il. Kul'tur, 1957, No 3, 21-23
Abstract Deep c-'Ativation (12-10' centiiieLers) does not prod-.7ce an
i-crea-se L., tll-ie yieid since it leads to -, severe desic-
cation of the soil. Shallow cultivatio-a (6-10 ce:_itiI-_ie-
ters) can be carried o~_,.t witli the s-mallest protective zo--
:1e (8-10 ce:2tiLieters) without a considerable iiij~,.-.ry cto
the root systera. It sec-Lires tie u_,_c1erc.tti_in- of VLe weeds
a: d
.1 - creation of a loose upper layer Vaich protects the
Card 1/1 soil from excessive evaporation.
- 91 -

SEMIRMTEITKO, P.G., kand. sellskokhozyaystvennykh nauk.
Unexploited possibilities for increasing sunflower yield. Zemledelie,
6 no.3:48-54 Mr '58- (mm ii:4)
(Sunflowers)

V
SUDLCHMO, Y.G., kand. oellsko~11ozyaystvennykh nauk; DROGALIN, P.V., Imnd.
sel'skokhozyaystvennykh nauk; SBMIKHNMO. P G,.,-..k=d. sel'sko-
khozyaystvennykh nauk; IGHAT YET. 13.K., kand. sellskokhozyaystven-
nykh.
Iet's avoid a routine application of cultivation practices.
Zemledelie 6 no.5:50-56 My 158. (MIRA 11:6)
(Krasnodarsk Territory-Wheat) (Tillage)

SEMIUM11KO, Pavel kand.sellskokhoz.nouk; KLYUCHNIKOV, A.I..
kand.selinkokhoz.nauk; TOKARMY, T.M., kand.sellskokhoz.nauk;
TAGOBKINA, V.P.; PITKRSKATA, A.M.; ANTONOVA, H.M., red.; IOWA,
V.M., takhn,red.
[Sunflower cultivation] Kulltura podsolnechnika. Moskva, Goo.
izd-vo sellkhoz.lit-ry, 1960. 275 p. (MIRA 13:10)
(Sunflowers)

,;~ SEMIKHNENKOJ* P.G.'-.-kand.seliskookhozyaystvennykh nauk; KAHENNOBRODSKAYA, v.p.
Methods for improving the productive qualities of sunflower seeds.
Agrobiologiia no-4:525-531 Jl-Ag 162. (MW 15:9)
1. Vaesoyuznyy nauchno-issledovatellskiy institut maslichnykh i
efiromaslichnykh kulttur, Krasnodar.
(SUNFLOWER SEEID)

I
SEmIaN-v~NKO, F.,S.y kp-nd.sel'sko-Imoz. nauk, 7:111-~"Y---V,
Sunflower under irrigation. Zemledelie 26 no. 4:73-74
Ap 164. (MIRA 17:5)
1. Vsesoyuznyv naitchno-issledovateliskiy institut rnaslichnyk-h
ykh Irull ter.
i efiromaslichrr

SEMMENK09- P.G., kand. sel'skokh. nauk
Harvest the grain and till the field simultaneously. Zemledelie 26
no.7tig-24 JI 164. (MIRA 18:7)
1. Vsesoyuznyy nauchno-issledovatellskiy institut masluchnykh i
efiromaslichnykh kulitur.

SEMIKHNEENKO, P.G., karid. sell'skokhoz. nauk-,. FODO:',YANSKFIY YU.M.
.L 11 i -.0
Harvesting luime for sunfladers. Zemledel-e 27 no.]S."' 18 Ag 165
(MIRA lg,,Il)
1. Veesoyuznyy nauchno-i-5sledovateltskiy institut maslichnykh i
efiromaslichnykh kulltur.

SEMIKIN, A.T.
.... . .l--------".-,-".---
Diagnosis of a dissecting aortic aneusysm and its rupture. Zdrav.
Belor. 5 no.2-.59-60 F 15~. OGRA 12:7)
1. Iz teraDevtiche'skogo otdeleniya respublikanskoy bollnitsy (glavnyy
vrach V.I. Khimakova, konsulltant - prof. A.D. Adenskiy)
(AORTIC ANEURYSMS)

Atypical forms of myocardial infaret. Zdrav.Belor. 4 uo.3-.
59-6o mr '58. (MIRA 13:7)
1. Iz terapevticheskogo otdeleniya respnb~likanskoy bollnitsy
Lechsanupravleniya (glavnyy vrach V.I. Xhimakova, konsul'tant -
prof. A.D. Adenskiy).
(BMT--INFAROTION)

T -ATO e -00 0 0 4 0 44 0
6

o
0 0 0 0 0 0 0 a a 61
~Ojo 0 0 a 000 s
o 0
7
L L -1 1. -It- J A L. a M. PQ A I IIf I LI -1., 1 1. A& NCC W
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9
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ZT-rudy vesesoyuzhogo soveshchaniya rpartenovtsev
7 Proceedincs of all-Union Con-
sultatim 6f the Open-Hearth Operators, ONT1,1936.

SD,IIKE.', I.D.
"Design of an Open-Hearth Furnace in the Light of Present-Day Stakhanovite
Procedures". The Theory Eind Practice of Metallw~a No 1, 1936.

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0 Devices for ibe FAmorW of W PMueft of Combadion from
00 Open-Elurth FurnaosiL 1. Sentikitt and L. Segau. (Sud. W3M,
00 No.5, ).W-Ii). (In RUIGMUTI.-Tho an t hors t I iscusa t fie t-haracter.
ixtirx (T the methods us"I to provide the draught neiessary for the
so
removal of the products of combustion from open-heafth furnaces.
*0 The ortlinarv ahimnc~v. the indirect- and direct-acting form 141raught A =*O
00 thip avul I he7direct-acting forml-draught flee combinvil with a boiler 00
10 lltilitk- the WaMl4--he4t, of the games am discunsvil. 'nip latter is
96 Zoo
Rachfurnave --O0
00 should be provUled with two such boiler equipments. one being in
00 rx-Arrve. Mnallv a scheme is suggested for the centralixation of the
goo
draught m "ystem of a number of open-hearth furnaves whi(b could
thus be vonibined with a central waste-heat, boiler Plant. zoo
zoo
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*0 A 1. St-inikin. (Still. 1939, No. 9. pp. 15-19). (In Humian). I.Arge

*0 --,%-ju-0it-y'PW-350 ton) fornar" are capable of lirtiducing up to
IOLK) tons of stivel fit 8 fir. For this it iA tiecessitrv to incream the
09 a
at:;
licat supply (luring the charging period to W-6) Willion cal. per hr.
ising fortId dr'Lft at a satirt, of ioo-m mitt. or water. Utillsa-

tion of t it, I vat of tho ticie g= for strAm mising is pimtsiblo. The
I I
furikitee shituld Ixi mado gam-tight ky A steel shelf. Um And air
uplakes ItIld sitlKwketa nud rt-jenerators should littv(- individual
-
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enerators should be
e
oc eta and re
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II
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A.
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ti, x The Author discusam more particularly, and with some
'7ell at
reference to exrrimental dAtA Anil worKS extIorienve, the design
of the Imth Ittic tho volume of tht, furnace. tnethods of supporting
tho furnact, structure, Ix)rt design, Plag litwkets, n-gettorator",

0 0 reversing val,ed and dues.
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USSR/Enaln
1W
t
J~Iwa
Furnaces
Dec 1947
"New Construction for Hearth of Blast Furnace,"
Prof 1. D. Semikin, Dnepropetrovsk Metal Inst; I. G.
Polovchenko, Engr, Dneprodzerzhinsk Night Inst, 8 pp
'Stall" No 12
Authors discuss new construction for hearths of
blast furnaces. Hearth has heavy bronze base under
the hearth block. Cooling -plates are arranged under
the hearth block. Claim that with this arrangement
stability of hearth is increased, service period.of
hearth block and foundations is lengthened, and
operating period of the furnace increases.
57T29

--saim"", I.D. - -- --
42319. SEMIKIii, I.D.-Dinamika Fakela evobodnoy strui Nauch. trudy (DneprODetr. metallurg.
in-t im Stalina), VYP 14, 1948, B 3-18-Bibliogr: 11 nazv.
SO: Letopie'Zhurnal'nykh Statey, Vol. 47, 1948.

--SENfIXI-,t-, i.D.
42320. SE:4'IKj7-, I.D., STk~,IK7VTC;-:, K.C.,-Ispytaniye nevoy golovki martenovskoy
I - - 11 c
Dechi. Nauch, trudy (rinepropetr. mettllurg. in-t im. Staiina~ VVY? 141
- j
1948, s 19-27-
SO: Letopis'Zhurnal'nyl--h Statey, Vol. 47, 1948.

i. i".. . . . . n 1 -11: - .% .. . 1!, -1:7- - 'T T',T-~-C,~- 1 7 * -7- 7oWilli Y .
sa-il= 1--, - -.j -. 1. A . 7 . ;
-1 - -Y w ~ - 1, - -., - - --'-
B. L.; laTAYEV, B~ I.; KUZZE111, 'M. A.; MIIaAYLEI,,TKO, A. Ya.; NAZ.PuROV, 1. S.; PLUITIFIKOV, L. A.;
TAYS, N. U.; TROIBI S. G.
Metal-luxgiueskie Peui (Metallurgical Furnaces), 975 P., 11051.

124-57-2-1975
,ri-anstatio, fi-on, 1~xfcr,tlivnyy zhurnal. Mekhanika, 1957, NY ?-, p 71 (USSR)
AUTHOR r1h, -E. b1l,
TITLE To the Theory of the Fre,-. Jet (K teorii svobodnoy strui)
PERIODICAL Nauch tr. Dnepropetr. metallurg. in-ta, 1954, Nr 31, pp 3-15
ABSTRACT Differential equations are obtained, which determine the
propagation of ~i plane and an axisymi-netrical larnindr jet in an
infinite medium having the samr- pl~ysical properties. Formulas
for the volocity distribution over .i cross section and along the
a%is of tl-e jet are given Tt is shown that the dimensionless
velocity profiles become similar, starting frorn a certain fully
defined time criteria n. The calculations conducted on the basis
of the relationships obtained are confirmed satisfactorily by the
experimr-ntal data of ' D.Semll,.in iNauch- tr. Dnepropetr
mrt-illurg in-t;i, IQ48, NY 14,i. However, it is necessary to note
the formulas proposed by the authors coincide with the first
eapproxima,t,on of the solution obtained for similar problems
b V Pa i ~ S. T.,''MEkhanika, Sb. Perev, i obz. in. period.
lit 1950, Nr 1; Quorttrly kppl. Math., 1952.. Vol 10, Nr 2).
Card 1/1 Bibliography: 6references M, M. Benilova
I. ;-zs---Theory 2. Mlazhematics

124-57-1-689
Translation from: Referativnyy zhurnal, Mekhanika, 1957, Nr 1, p 89 (USSR.)
AUTHOR: Semikin, I.D.
TITLE: The Laws Governing the Combustion Process of a Gas in a
Torch Flame (Zakonomernosti fakel'nogo protsessa szhi-
ganiya gaza)
PERIODICAL: Nauch. tr. Dnepropetr. metallurg. in-ta, 1955, Nr 33,
pp 83-103
ABSTRACT: The velocity distribution in the various sections, the veloc-
ity variation along the axis, the gas-flow rate acress the cross
section, and the diameters of the cross section of the jet are
determine6 by means of G.N. Abramovich's equations of the
theory of the turbulent gaseous jet [ Prikladnaya gazovaya*-di-
namika (Ap~)lied Gasdynamics), Gostekhizdat, 1953) for values
of the empirical coefficient a = 0. 080 - 0. 085. A correlation of
the calculated and the experimental data establishes the effect
on the length of the flame of the inner diameter of the torch
(the nozzle diameter), the heat value of the fuel, the 02 content
of the air, and the excess air. Empirical formulas for the
Card 1 /Z flame length are compiled with and without consideration of the

124-57-1-689
The Laws Governing the Combustion (cont.)
entrance velocity of the gas and the air, and the temperature of the gas and
the air. The effect of the crowding of a flame and the angle of convergence
and distance between flamias are examined only qualitatively.
A. B. Reznyakov
1. Flames--:-Properties--Mathematica1 analysis 2. Gases--Combustion--Analysis
Card 2/2

ir ip

Wjjok- f
(to Ift I it'.0 C"
--
left'a non
W

How
room onlyamua tuna u%
e
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il~kiof
,
Jh- tIng P
ocas t
an
AM
'
c fo'-
gap or-fu
cil* 1~ayor ou~cffxwt fo b ta ti6l

_qRMTX11 .. Professor; ROZEMART, Yu.I., kandidat tekhnicheskikh nauk, dotsent;
I
GOLIDFARB, E.M., kandidat tekhnicheskikh nauk.
Haating massive bodies by radiation. Stall 16 no.3:252-256 Mr 156.
(MLRA 9:7)
l.Dnepropatrovskiy metallurgicheskiy institut.
(Haat--Radiation and absorption) (Blactrometallurgy)

137-58-6-11679
Translation frorn. Referativnyy zhurnal, Metalluroiya, 1958, Nr 6, p -05 (USSR)
AUTHORS Semikin, I.D., Averin, S.I.
TITLE. Controlling the Flame Jet in Open-hearth Furnaces (Organi-
zatsiya fakela plameni v martenovskikh pec,iakh)
PERIODICAL Tr. Donetsk. otd. Nauchno-teklin. o-va chernoy metallurgii.
1957, Nr 5, pp 39-46
ABSTRACT When a free jet moves in an infinite space, the process of
mixing consiscs of the capture of and transportation of the neces-
sary amount of air into the depth of the flame and then of inti'-
mate intermixing thereof. The flame length (FL) depends upon
the diameter of the burner, the heating value of the gas (calcu-
lation has to be in terms of heat value per unit weight), the 02
content of the air, the velocities of the gas and air flows and
the angle at which they meet. In Open-hearth furnace practice,
FL is not dependent upon the velocity of the gas, unless sup-
plernentary sources of energy are used in the form of com-
pressed air -3-ut the FL does depend upon air velocity, de-
clining as air velocity increases. The angle of contact of gas
Card t/Z and air must not be >ZOO, because although the FL diminishes

137-58-6-11679
Controlling the Flame J(--. in Open Hearth Furnaces
in this case as the result of the impact of the flows, the aerodynamics of
the flame are simultaneously impaired. Venturi ports should be modified in
the following directions 1) reduction of the dimensions of the gas port
where reserve draft is available, 2'i provision of multiple-jet burners if
coke gas is avallabte. The speed of outflow of cold coke gas should be
> 80 ai/sec. 31 delivery of compressed air in high-pressure Jets with Laval
nozzles- It was found at one of the plants in Dnepropetrovsk that delivery, of
compressed air into the tank by means of two side nozzles reduced heat
time by 30-40 min. A design has been developed of a port with an aerody-
namic tank in which the major role is played by air and not gas.
M.M~
1. Oper hearth f~,~_rnaces--Controi systems
Card 2/2

SEMIKIN, I.D., Prof.
--" -
Analytical determination of the longitudinal profile and
the dimensions of a laval nozzle. Izv. vym. ucheb. zav.;
chern. met. 2 no-3:107-111P Ur '59. (MIRA 12:7)
l.Dnepropetrovskiy* metallurgicheskiy institut. Rekomendovano
kafedroy metallurgicheskikh pechey Dnepropetrovekogo metallurgicheskbgo
instituta.
(Gas flow) (Nozzles)

S/148/601/000/012/010',/020
A161/A133
AUTHOR: Semikin, I, D.
TITEL: On the technical indices
(As a discussion)
Of Open hearth furnace operation
PERIODICAL: Izvestiya bysshikh uchebnykh zavedeniy. Chernaya metallurgiya,
no. 12, 19602 139 - 145
TEXT: The article deals with the problem of determining the output
quota for open-hearth furnaces. The present methods are criticized with
reference to the author Is own three works [Ref. 1: 1- D. Semikin. Diskus-
siya o rabote domennykh pechey na povyshennom davlenii (Discussion on Biast
Furnaces Operating on Higher Pressure), NTO ChM, Dnepropetrovsk, 1958;
Ref. 2t I. D~ Sem4.kin..Teplotekhnicheskaya_otsenka topliva (Heat-Technolo-
gical Fuel Rating), Trud
0 y Dnepropetrovskogo metallurgicheskogo instituta,
no. XXII, 1949; Ref, 3: 1., D. Semikin. Osnovnyye razmery raboohego pro-
stranstva martenovskikh pechey..(Basic Dimensions of the Effective Area of
Open.-Hearth Furnaces), Materialy k soveshchaniyu. staleplavil'shchikov v
Khar1kove, VNITO Metallurgov, May 19391 and calculations made in this field.
Card 1/4

S J'! A a `160,/000/0121/01 6.102-0
On the technical indices of open hearth.- A" !113
1-1, A. 3
The authors emphasizes that the output capacity of a furnace depends cn de-
sign as far as design results in a lower or higher heat capacity, i.e. a
furnace will give a high output if its design permits the combustion of more
fuel without ruininz- the brickwork, and the design of the head affecting the
flame in the furnace is the most, important design factor at the moment. He
does not a-ree with tile opinion of some metallurgists that low efficiency
is inherent in large furnaces. Three factors are suggested to serve as a
basis of productivity rating: I - The furnace heat capacity, M., (Meen))
with metal output per I million calories (as the electro-metallurgists use
to set the output quota by the furnace transformer capacity), though the
maximum heat capa3ity depends on the designer's understanding of its impor--
tance. The higher the maximum heat power, the higher will be the absolute
productivity, but the specific output per 1,000,000 cal will be gradually
lower, and intensely operating furnaces will have a lower specific output
index (which will not stimulate rational development). II - The furnace
char.o-e (E), for it is easily controllable. The annual furnace capacity
NouId than be determined by the number of heats (n) per year:
P = nE,
Card 2/4

S/148/60/000/012/016/020
Or the 4echnical indices of open hearth... A161/A133
though it would depend an the heat capacity, the charge weight, the number
of work days a Year, form of charge (liquid or cold iron), steel grade, etc,
and would be possible for certain average conditions only (which is true
for any methods). Besides this, a correction factor would have to be usel,
since the annual number of heats depends on the charge volume, and 12 - 16
heats a day are possible in a 5-ton furnace, and only 3 - 4 in 500-ton fur--
nace. III - Th-e ftl;rnace hearth area (F), or, actually, the metal bath
surface area. This factor is just the index being used now, and the outpat
per 1 m2 of floor permits a comparison of furnaces of different sizes. It
would be practical in the first approximation, but it has a negative side
as well. The ).,,-earth area is not as dependably determinable as the charge
E'. and fair comparison of capacities would only be possible taking into ac-
count the real bath surface level. This is so for two reasonst 11) Designes
,o get a "hight' output index, and in-
want to conc.eal the real hearth area,+
dicate excessive furnace wall thickness in drawings. Such thick walls are
rapidly destroyed by slag (after 10 - 15 heats) in a narrow furnace, the
width and the metal surface area become normal, but the metal output is
still related to the smaller initial floor area; 2) Being of-the opinion
that. the.heat process is the faster the shallower the bath is, designers
Card 3/14

35082
S/704/61/000/002/006/006
0201/D302
AUTHORS., Semikin, I.D., Professor, Kostogryzov, V,S,, Candidate
;f-r-ec-hnical Sciences, and.Tsygankov, O.L., Engineer
TITLE, A heat radiation calorimeter
SOURM~ Ukraine. Gosudarstvennaya planvoya komissiya. Institut
avtomatiki. Avtomatizatsiya i priborostroyeniye; sbornik
nauchnykh trudov, no. 2, Kiyev, 1961, 153-164
T&~f. The authors describe a thermal radiation calorimeter based on the
principle of temperature difference produced at a neat resistance by the
thermal flux. The instrument consists basically of a hollow copper cy-
linder with a partition in its middle. The thickness of the cylinder
walls and of the partition does not exceed 0.2 nmt. The part of the cy-
linder above the partion acts as an absolutely black body and performs the
functijon of a heat collector. The lower part of the cylinder is slotted,
the slots acting as thermal resistances. The cylinder has a connection
sleeve for the wiring of a thermocouple battery. The battery is made of
copper-constant thermocouples, whose number is determined by the sensit-2-vity
Card 1/3

S/704/61/000/002/006/006
A heat radiation calorimeter ... D201/D302
of the instrument. The thermocouple battery is wound at the external
cylinder surface in such a manner that the heat resistances be placed be-
tween the thermocouple junctions (hot junctions) placed against the Sur-
face of the heat collector and the junctions placed at the water-cooled
part of the cylinder (cold junctions). The junctions are isolated from
the cylinder surface by mica wafers. Mica is also used to insulate the
thermocouples from the top. The heat collector, together with the thermo-
couples is placed in a protective envelope. A mirror-polished nickel foil
is placed between the collector and the envelope; this arrangement makes
the heat losses negligible. The whole arrangement is assembled into a
separate unit, fixed at the face of the water-cooled bloc which at its
other end has two pipes for the circulation of water and one for the wi--
ring from the thermocouple battery to a potentiometer. The experiments
have shown the linear dependence of the e.m.f. of the radiation calori-
meter on the thermal flux; the temperature of the radiating body Tr was
found to satisfy Eq. (17)
Card 2/3

3 03 8 9
S/148/62/000/004/004/006
400 Eo8l/E,435
AUTHORS: Semikin, I.D., Averin, S.I.
TITLE: Basic mechanism of a turbulent gas flame
PERIODICAL: Izvestiya vysshikh uchebnykh zavedeniy.
Chernaya metallurgiya, no.4, 1962, 140-152
TEXT: The paper is a continuation of previous work. The
similarity conditions in turbulent flow are analysed and a formula
derived for transforming from one type of flow to another. The
length of the flame is regarded as the sum of two lengt hs, the
capture length in which the gas emerging from the nozzle captures
some of the surrounding air and the transfer length in which the
combustion is completed. The forces in the flAme due to the
difference between the densities of the gases, and the
dimensionless-Euler forces arising from the differences in static
pressure are evaluated and a calculation made of the amount
of air transferred in the capture length. A fifth power equation
is obtained for the dimensionless length of the turbulent flame
and the factors determining this length are briefly discussed.
Card 1/2

S/!48/62/000/006/003/005
E081/E435
AUTHORS: Averin, S.I., Semikin, I.D.
TITLE: Combustion of single component gas mixture in a.
turbulent flame
PERIODICAL: Izvestiya %-ysshll,-,h uchebnykh zavedeniy. Chernaya:..
metallurgiya, no.6, 1962, 146-154
TEXT: In a previous work (Izv.VUZ. Chernaya metallurgiya, no.4,
1962) the present authors found the formula for flame length
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In order to calculate flame length from this formula, it is
necessary to know the mean composition and specific gravity of the
gas mixture at the end of the capture path, and equations are
quoted for (1) the weight fractions of combustible gas, of res-idual
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Combustion of a single ...
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EOWZ435
free oxygen, of the products of the reaction, of nitrogen and
of unburnt gas; (2) the specific gravity of the gas mixture and
(5) the mean temperature of the gas mixture. These formulae are
applied to calculating the composition, thermal characteristics,
specific gravity and flame length in the combustion of hydrogen
and carbon monoxide; the results are shown in tabular and
graphical form. The analysis is applicable to complex multi-
component gas mixtures and gives good agreement with experiment.
There are 6 figures.
ASSOCIATION: Dnepropetrovskiy metallurgicheskiy institut
(Dnepropetrovsk Metallurgical Institute)
SUBMITTED:
June 19, 1961
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s/148/62/0OO/OO8/oo8/oo9
E194/E435
AUTHORS: Averin, S.I., Semikin, I.D.
TITLE: The combustion of multicomponent gas mixtures in a
turbulent flame
.PERIODICAL: Izvestiya vysshikh uchebnykh za-vedeniy. Chernaya
metallurgiya, no.8, 1962, 158-i6g
TEXT: General equations are first formulated for the cofnbustion
of a mixture of two combustible gases w-ith oxygen. The
combustion of mixtures of oxides of'carbon and hydrogen is then
considered and, on the basis of previous articles by the same
authors (Izv.VUZ. Chernaya metallurgiya, nos. 4 and 6, 3-962),
a formula is derived for the ratio of the.flame length to the gas
nozzle diameter. An auxiliary graph is given to facilitate
practical calculations with the formula. The combustion of
hydrocarbons and of mixtures or several gases is then considered.
Calculations are made of flame length as function of Froude Number
for oxides of carbon, hydrogen, generator gas, natural gas, coke
oven ga's, blast furnace gas and Moscow city gas in an atmosphere of
air for subsonic rates of gas flow. The results are compared with
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The .combustion of ... E194/E435
published experimental data and agreement is good. The method
can be used to assess the influence of various factors on flame-
length. It is found that on burning mixtures of carbon oxides
with hydrogen the flame length increases with the hydrogen
content. Iflien burning mixtures of hydrogen and hydrocarbons,
and in particular with methane, the flame-length increases with
the concentration of hydrocarbons. When burning mixtures of
methane with hydrocarbons of the series CnH2n+2 the'flame-length
increases as the methane concentration is reduced and the
concentration Of CnH2n+2 hydrocarbons is increasedb There are
3 figures,
ASSOCIATION: Dnepropetrovskiy metallurgicheskiy institut
(Dnepropetrovsk Metallurgical Institute)
SUBMITTED: November 10, 1961
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s/148/62/ooo/ol2/008/008
E081/E184
AUTHORS: Averin, S.I., and Semikin, I.D.
------------------
TITLE: Length of a turbulent gas flame issuing under high
preasure from cylindrical and conical jets
PER10DICALs Izvestiya vysshikh uchebnykh zavedeniy,
Chernaya metallurgiya, no.12,,i962, 162-173
TEXT, A formula for turbulent flame length derived previously
by the present authors (Izv. vu-z. Chern. met. no.8, 1962) is
analysed and developed.with special reference to conditions o f high
gas velocity, in which changes of gas density must be taken:inta-
account, The relationship between the specific gravity and thia
velocity of the gas is established, and two.criteria, charactprising
respectively the relative gas flow and the initial gas compression,
are obtained. Calculations are carrie6out forShebelinka natural.
gas (92-35o CHIk, 4..2-10; C2H6I - 0'9"b C08, - 0633%* C4H.,
o. 46c,~ C Ml 01.3%~,NV o.41% CO), arid, curves are g ven to show
.5 2 'a
the dependence of fl -ame length on relative gas flow., The flatne
length increases continuously with increasing gas flow, but at a
decreasing rate up to a critical flow, after which the rate.
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Length of a turbulent gas flame ... Eo8l/Ei84
increases again. Smaller diameter j eta-give shorter flames with
a greater ratio of flame length to jet diameter. if the air is
pre-heated, the flame length increases more rapidly with gas.flow
than if it is not; the flame length to jet diameter ratio depends
less on jet diameter and the flame is longer. I-Jeasurements made.
with Shebelinka gas show good agreement with theory.
There~ are 6 figures.
ASSOCIATION: Dnepropetrovskiy metallurgicheskiy institut
(Dnepropetrovsk retallurgical Institute.)
SUBMITTED: September 12, 1961
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