SCIENTIFIC ABSTRACT VARSANOFYEVA, V.A.I - VARSANYI, G.

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VAFSA1TOF'YE'v'A) V. A.., P-7:W PA 33/101797 Oct Biography "Vladimir Afanaelyevich'Obruchev (On III Eight,. Fifth Birthday AnAlversary)p" Prof V. A. Vareanoflyeva) Dr Geol Mining Solp 3 pp Offauka I ZhIsn'" No 10 Complete biography of Obruohw) vk6 to cut at the foremost Russan geologists, No to putt- cularly famillar vith the goolog d 61borlap and blo books on this oubjoot are used am tuU, VARSAIvOFIYEVA, V. A. Prof. "The Stalin Five-Year Plan and Develooment of Scientific Geolopical Tdeas 1n the USSR." Byul. Mosk. ob Fsp. Prirod., Ot~el. 'Col., 25, No-1) pp. 3-1M., 1950 Entire periodical is divided into three parts: (1) principal charges in the deUelopment of Russian geological science after the October Revolution (1917-1929); (2) developoent of geology during the period of the First and Second Five-Year Plans (1929-1937); (3) beginning of the Third Five-Year Plan, the war years, and the postwar Five Year Plans. 252T`2 .7 VARSAINOPYEVA', V. it. EJ~ptr "Aleksandr 11~kolayevich Mazarovich (1886-1950),," 3yul Mosk. ob Ispytat Prirody, Otdel geol.. 25, No-3, PP. 3-16, :1950 Mazarovich died 25 Nar 1950. He was a professor at Moscou University., Chair of Geol. FacuAt-y Pnd Chair of Historical Geoloey. Presents list of 129 urotks of IMazaro- vich, covering the period 1910-3.950., which are on peororpholq-11 stratigrnphy'., Ceol. etructures., regional geog., etc., of MSR. 253TIOl r s c,!i ---, If A"-ademik A'! i.-jjey Pot I, i 'P. 2h Catal-wi with geolo-ical litlnratiro, ey.-;eqit!onF, ani activ! ~J~e.C3. 5 9 17. 6,.,,;, .PTVI VARS"OY'YZVA. Vera Aleksandrovna, 1889- , professor (redaktor]; MIUM, V.V. r e cQt rT [In memorv of Professor Aleksandr Nikolaevich Mazarovicb] Famiati professors, Aleksandra Nikolaevicha YAzarovicha. Pbd red. V.A.Varsanoflevoi i V.V.Ken- nera. Honkva,.Ixd-vo Moskovskogo, ob-va ispytatelel prirody, 1953. 191 P. (HLRA 6:8) (VAsarovich, Alekoandr Nikolaevich. 1886-1950) (Geology) SARTCHIVA, T.G.; SOKOLISKAYA, A.N. [authors]; VARSOOIrOYEVA, V.A. [reviewer]. ------- -"Guide to Paleozoic brachiopods of the Moscow Basin.* T.G.Sarycheva, A.N, Sokollskaia. Reviewed by V.A.Varsanofleva. Biul.KOIP. Otd.geol. 28 n0-3: 74-75 '53. (KLHA 6:11) (Moscow Basin-Brachiopoda, lossil) (Brachiopoda, Fossil--Koscow Basin) (SarycheTa, T.G.) (Sokollskaia, A.N.) VAPS"OFITEU. VoAo Vladimir Afauss'evIch Obruchey. Biul.901P. Otd.gsol. 28 no.3;5-22 '53- MRA 6:12) (Obruchey, Vladimir Afanaelerich, 1863- HAVIKOVICH, A.I.; VARSAHOF'YIVA,V.A.,redaktor; DOBRONRAVOVA, A.O., redaktor; redaktor. (Contemporary, and fossil coral reefs] Bovremennre i Iskopasmys rify. Hoskva, Izd-vo Akademii nauk SSM, 1954. 169 p. (Reefs) (MMA 7-12) VIRWOFIYNVAI V. 300th anniversary of the reunion of the Ukraine with Russia. Blul.MOIP. Otd.geol. 29,no.3:1-VIII My-Je 154. WaA 7:8) (Ukraine--Geology) (Geolog7--Ukraine) VARSANOFIYUA, V.A. in , - - --l-,~' I Geomorpholog7 of vomtainous reglonE such as the Northern Urales VOP,geog, 36:160-181 1546- (MW 8:4) (Ural mo-autain.1) VARSANCIrIT11VA, Vera Alaksandrovza; KIKULINSKIT, S.R., rodaktor.- POKAMIKATA. Y.Y., takhxicheskiy rodaktor. [The Moscow Society of fiaturallsts mad its role la the development of Russian. scieucal Mookovskee *b3hCh4*tT* ispytatelal prirody i ego zwwhoxie v razvitti otechentyeassi sauki. Hooky*. Izd-vo Hoskovokego ulty., 1955. 100 Pe (ULRA 9:5) (Moscow-Biological societies--History) TARUNOYIYBVA$ V.A., prof.; SMXUTOVO BeNs, red.1 FONMWA, A*A&# takhn. red. [Programs of pedagogical institutes; geolog7 for natural science facultiesI 13rogramvq podagogi;hookikh institutov; goolneiia dlia fakulltetov estestvornaniia, Hookyal Goo, uchebno-ped~og. izd-vo X-va proov. RMR, 1955.11 P-, XUA 11009) 16 Russia (1917- R.S.P.S.R.) Glavnoye upravlerd7e vysehikh i ore,dnikh pedagogichaskikh uchebnykh zavedeuiy. (Geoloe,7--Study and teaching) USSR/ Scientists Geology Card 1/1 Pub - 45 6/18 Authors I Varsaaofleva& Ve A@ Title I Aleksey Petrovich Pavlov POriOdiCdl I Izv. AN SSSn Ser g6ogs Is 54 609 Jan-Feb 1955 Abstract 9 In comnemoration of the passing of 100 years sincs the birth of Aleksey Petrovich Pavlov (1854 - 1929) his life history a-ad work are recalled. It is claimed that Pavlov distinguished him elf as a teacher of geology, research worker and author, having been professor of' the Moscow University and member of the Aaadenw of Sciences of the USSR. He is said to have advanced the idea of the relationship between soil science and geolo&v and to have conducted extensive resea-rches cf topov-raphicel formtions outside the realm of glacial action* -Institution t Submitted S Card 1/1 Pub. 121, - 7,/39 Authors I Varsallo6evap V. A., Dr. of ;~Qol. Iiineral. Sc. T:Ulo r 150-th a:iniv~-rsai-y or the IID-,c-)w ~,'-ociet,v of Natural Sci~3ntists Periodical t Vf-zit. All 2612, 56-61, Feb 1956, Abstraot I The 150-tl~ an-iverSlirv ~,f uf the Mc.)scow Society of special meetLaes o" tric Acal". uf ~c., U.E~'F. Institution VARSANOFIYEVA, V.A. In memory of Vladlril Afanassevich Obruchey; obituar7. Biul XOIP.Otd., geol. 31 no.15:3-12 S-0 156, (KIRA 10:3) (Obruchev, Vladimir Afanaelevich, 1863-1956) VARSAYWYNA, V.A., doktor geologo-mineralogicheakikh nauk. The 150th anniversary of the Moscow Haturallstst Society. Test.AY SSSR 26 zo.206-61 7 056. (MLRA 9:6) (Moscow--Scientific societies) OUSH~U-U, Nadezhda kkolayevna VARSANWPLU"Y. A. -QtVOtf3t,fen"7y redaktor, .kWYXR. I.L.. redaktor Awl-JU.-a redal:tor (Two summers In the Arctic) Dva lets v Arktike. Hoalwa, Izd-vo Akad.nsuk SSSR, 1957. 175 P. (MIRA 10:11) (Arctic regions) VICH, A.I., dote.; VARSAJ~ prof.; SEMIKHATOV, B.N., prof*; RAVIKO TITOV, A.G.; HAKSAYET, A.V. tekhn.red. (Programs of peaagogir-al institutes; geology] Programmy pedagogiche- skikh institutov; geologiia. Mos;,va. Gos. uchabno-pedag izd-vo MIRA H-va proav. RSFSRO 1957. 21 P. 1* 1i:3) 1. Russia (1917- R.S.F.S.R.) Glavnoye upravlaniya vysshikh i arednikh pedagogicheskikh uchebnykh zavedenii. (Geology--Study and teaching) F , ~77773' Fl AUTHORi Varsanoflyeva, V. A. 5-!,-1/6 TITLEs Fqrty Years of Soviet Geology (Sorok lot sovetskoy geologii) PERIODICAL: Byulleten' Moskovskogo Obshchestva Ispytateley Prirodyt Otdal G6ologicheskiyp 1957P No'5v PP 5-54 (USSR) ABSTRAM The history of development of Soviet geology is divided by the author into 5 main periodej 1. The period of civil war, 2. Initial reconstruction of national economn 3. The first 5-year plant 4- World War II, and 5, The post-war period. After describing briefly achievements during the first 3 periods, the author passes to the period of World War II when the main efforts of the Soviet geologists were directed towards discovery of now deposits of strategic materials. During this period, now copper-polymetal deposits in the Altai, and new manganese deposits in Kazakhstan and the Saath Urals were discovered, and the tin 'jams in the Fav last was fully established. The Uralstregion was converted during the World War II into the center of the defense industry. Prospected iron ore resources considerably increased at that time, although the quality of iron ores is not the same throughout. There are exceptionally pure oresp as those in Card Bakal. There exist also naturally alloyed iron-chrome-nickel m Fourty Years of Soviet Geology 5-5-1/6 ores of the Khalilovo type and ores with other valuable impu- j#ties necessary for the manufacture of high-quality steels. Independent deposits of alloying elementst chromium, nickel, cobalt, eto. were also discovered. A great role in the dis- covery of now manganese deposits was played by A.Go Betekhtin and N.P. Kheraskov. The intensive prospecting of non-ferrous metals almost doubled the mining of bauxite ores in the Urals. The guiding idea in the prospecting was A.D. Arkhangellakiy's theory of sedimentary genesis of bauxite deposits. Ore depos- its of exogenous genesis in the Urals were widely studied during World War III which resulted in the establishment of a raw material base for the nickel industry. The beginning of the 5th period in the development of Soviet geology was ohar- acterized by the transformation of the Committee of Geologic Problems into the Kinistry of Geology of the USSR in 1946. The construction of numdrous hydroengineering units called for the extensive use of hydrogeology and engineering geology. Geophysical methods of prospecting, which previously were used only in petroleum geology, were improved and widely used. One of the practical results of their applioation was the discovery of very large magnetite deposits in the Turgay-lowland. The drilling of deep basic test wells acquired considerable impor- Cax:d 2/11 tance, in particular for the discovery of oil deposits. Large Fourty Years of Soviet Geology 5-5-1/6 oil deposits were found in the eastern parts of the Tartar ASSR. The finding of Siberian diamonds gave rise to tle preparatory work for the establishment of a diamond-recover- ing industry in the Yakut ASSR. The author then proceeds to outline the main development lines of the Soviet geological science during the recent 12 years. 1, Lithologyp Metallogeny and Petrography: In the science of sedimentary rocksp several main lines and research methods- have been developed in the USSR. V.P. Baturin pays most attention to petrographic-mineralogical investigations aiming at the stratigraphic classification of sedimentary rooks by terrigenous components. U.M. Strakhovq following A.D. Ar- khangeltakiyp has been atudying recent sedimentation iWavenves- and compares them with those of the past. lie tried to find the laws of sedimentation and found his thesis of periodiOity-Lnd- irreversibility of sedimentation on the Earth's history. L.V. Pustovalov advanced the conception of sedimentation processes as one whole on the basis of notions of meehanical and chemical differentiation of substance. N.S. Shatakiy proposes to study sedimentary formations as natural complexes of sediments. He has applied this conception to phosphorite- Card 3/11 bearing and manganese-bearing formations. In January 1955, Fourty Years of Soviet Geology 5-5-1/6 the Western-Siberian section of the AN USSR oGlIed a confer- enoe on sedimentary formations in Novosibirsk. V.?. Kaslov studied rock-forming organisms of the carbonaceous rooks. H.He Strakhov, G.I. Toodorovich, D.S. Sokolov, L.M. Miro- pollskiy and others continued to develop the study nf dolo- mites which was begun by B.P. Krotov. M.V. Klenova, 1.I* Gorshkova and others studied sedimentary processes and mineral formation on the bottom of contemporary seas, develo7~~ng the geology of seas into a special science. Of a partiou),ar impor- tance are complex explorations of the Soviet deep-sea expedi- tiontof the Oceanology Institute which have been carried out on*the "Vityazl" ship in the Pacific and Okhotsk Sea. In 1952, an all-union conference on sedimentary rooks and sedi- ~mentary mineral products was called in Moscow. The science on mineral products connected both with sedimentary and mag- matic rooks has been developed in contact with geochemistry. A*P& Vinogradov in the Geochemical Institute of the AS USSR develops the geochemical line of approach in studying living substances. Extensive investigations of A.G. Betekhtin on the genesis of manganese deposits are of great geochemioal significance. In 1946 S.S. Smirnov put forward a new con- Card 4/11 oeption of the "Pacific ore belt". This belt incorporates Fourty Years of Soviet Geology 5-5-1/6 the entire region of Neso- and Cenozoic folding adjacent to the Pacific. In this region of tin-gold mineralization, the base of the Soviet tin industry was established under the guidance of Smirnow himself, Yu. A* Bilibin also contributed much to the exploration of mineral depoaiis and the devel- opment of the science of metallogeny. Ore deposits in all folded zones of the USSR have been explored and studied under the guidance of great specialists, such as A.G. Betekhtinp D*S. Xorzhinakiyt K.I. Satpayev, G.D. Azhgirey, F.I. Vollfson, Ye.Ye. Zakharov and others,, The origin of some deposits has not been cleaied up thu's far, for example the Dzhezkazgan deposit, which is the largest copper deposit in the USSR, is considered'as hydrothermal by Satpayev but other investigators hold it as sedimentary. In 1956, the first all-union conference on gooohemical methods of ore deposits prospecting was balled in Moacow. A conferenoe on the types of metallogen'ic maps' took also place in koscow in 1956. Petrography of crystalline rooko developed in close contact with metallogeny. This conneotion found its expression in the first petrographic conference hold in Card 5/:Ll Moscow In 1935 which was dedicated to the problem of "Regu- Fourty Years of Soviet Geology 5-5-1/6 larities in development of magmatism in connection with mineral products". A new branch of the science of eruptive rocks, volcanology, has been developed in the USSR during the past 25 years- In 1931, A.N. Zavaritskiy began systematic study of the volcanos in the Kamchatka peninsula, where a volcanological station was established. This station system- atically observes volcanos of the Klyuchevskaya group, and since 1946 has studied volcanos on the Kuril islands. D.S. Belyankin founded another new branch of science, the "petro- graphy of technical stones" which studies artificial building materials. I section of technical and experimental petrography was established at the Institute of Geological Sciences of the AD USSR. The problem of petroleum origin needs a further investigation. The advocate of the inorganic originp W.A. Kudryavtoevt was recently supported by P.N. Kropotkin and V.B. Porfirlyev, although the organic genesis theory is shared by most of the students of this''problemio 2. Stratigraphy and Paleontology. Much work has been done by-the'All-Union Petroleum Geologic-Survey Institute on the unifivition of stratigraphic schemes and geochronologioal sub- divisions. In 1955, the JL11-Union Scientific Research Geolog- ical Institute called the all.-union conference on general Fourty Years of Soviet Geology 5-5-1/6 problems of stratigraphy and classification. In 1952, a stratigraphic commission headed by L.S. Librovich and in 1956 an interdepartmental stratigraphic committee headed by D.V. Nalivkin were established, In 1956p a conference on the uni- fication of stratigraphy in Siberia was hold in Leningradp and a conference on the Urals stratigraphy took place in Sverdlovsk. Micropaleontology in the USSR has been developed by M.N. Dampell, M.N. Subbotina, A.V. Fursenko, G.A. Dut- kevich, D*X. Rauzer-Chernousova, M.A. Xalmykova, and others. An independent important place in the USSR belongs to evolu- tionary paleontology. The main centers of this science are the Paleontological Institute of the AN USSR and the AN of the Georgian SSR. A.A. Borisyakv Yu. A. Orlov and Ye.I. Belyayeva studied the Tertiary fauna of mammals and Orlovp I.1. Yefremov and A.K. Roshdextven9kiy investigated Neoczoic reptiles. Locations of Mesozoic reptiles and Tertiary mammals- in longolia were studied during 4 years. In 1954# an all- union paleontological conference on the state and problems of the Soviet paleontology was hold in Moscow. Paleobotanics was developed by the works of A.R. Krishtofovich, N.D. Za- leaskiyj L.N. Krechetovich, I.V* Palibin, V.D. Frinads, and Card 7/11 X.F. Neyburg. A special branch of paleobotanio studying Fourty Years of Soviet Geology 5-5-1/6 spores and pollen was singled out by the works of V.P. Griahukp A~A* Lyuberq S*N* Naumova. and M.I. Heyshtadt, 3* Quaternary Geology and Geomorphology. The Quaternary geology which rose from geological sciences has been de- veloped in the USSR. An all-union conference on studying the Quaternary period was hold in Moscow in May 1957- Regional conferences took place in various citiest in 19481 in Tashkeni on loses genesis and recent tectonic movements in Central Asia; in 1952P on the lowland at the Caspian Sea, and in 1953, in Minsk and Tallin on geology and engi- neering geology of the Baltic countries and Belorussia. A special conference to discuse the problems connected with the composition of a unified stratigraphic scheme of Qua- ternary deposits wat called in Moscow in 1954 by the Insti- tute of Geological Sciences and Institute of Geography of the AN USSR. In May-June 1955 a conference on the loessen of the Ukraine was held in Kiyev, in November 1955 a confer- once on the stratigraphy of Quaternary deposits of the Baltic countries took place in Vilnyus and Kaunas$ and in May 1956 a conference on the lower border of the Anthropogen Series. A number of conference* were hold on the problems Card 6/11 of karats in 1947 in Perm, and in 1955 and 1956 in Moscow Faurty Years of Soviet Geology 5-5-1/6 One branch of karst studying, speleology lags behind in tho USSR. In 1956, an interdepartmental conference took place in Leningrad on the principles of composing legends for gener- al geoPorphological maps. P.N. Toys# performed the morpholo- gical analysis of the Carpathian mountains, L.D. Dolgushin investigated the polar region of the Urals. Ezoeptional successes during the past 15 to 20 years have been achieved by the Soviet hydrogeology, engineering geology, and congela- tion study. The world's only Institute of Congelation Study was established at the AN SSSR due to the initiative of V.A. Obruchev. 4. Tectonics. Tectonic maps of the USSR were published in 1952 on a scale of 184,000,000 and in 1956 on a scale of 135,000,000- Experimental tectonics has been studied by V.V. Belousov in the Institute of Earth's Physics of the AN USSR, where a special laboratory of tectonic physics was established in 1949. An essential achievement of Soviet tectonics is the study of vertical oscillations of the Earth's crust in the regions of geosynclines. Much material has been accumulated on structural geology. New types of disloca- tions have been discovered, in particular "abyssal break0 Card 9/11 described by A.V. Peyve for the eastern slope of the North Fourty Year3 of Sovint Geology 5-5-1/6 Urals* G.D# Axhgirsy analyzed structural forms and came to the oonoluslou on the dominating role of compressing tangential forces in the processes of mountaiu. origination. N.V. Muratov and B#A. Petrusheyskiy investigated many gooeyaclinal regions of the USSR. N.S. Shatskiy developed now ideas in the studying of plateaus assailing Stills's conaipts of "orogenic phases". He denies the universality and simultaneity of orogenio phases. However, Belousovle school opposes the concepts of Shatskiy in many respeots, Delouaoy and V* Yea Khain paid attention to so-called "wave" movements which were discovered while studying oscillating movements in geosynclines. The basic deep drilling supplied much material for solving several pro- blems such as inheritance in development of atructurest geotectonic inversion. etc. B.A. Petrushevskiy applied a combination of historlao -;struatu:_,a1 analysis with seismic methods for studying the Urals-Siberian Epy-Heraynian plateau and the Tyant-Shan'. The accumulated material makes it possible to elucidate the problem of the structure and origination of thq oceans. There are differences between the Indian and At- lhni:r6-362ceans on the one hand and the Pacific ocean on the 10/11 other'hand. It in supposed that thesa differences are due to Fourty Years of Soviet Geology the-mods of their origination. AVAILABLD Library of Congress card 11/11 5-5-1/6 CHERNOV, G.A.; VARSANOFOYIVA, V.A., red,; MOROZOVA, A., oty. za vypusk; TSIVU1tU-""I-.-q- t616A:7iic' (Tourist trips to the 'Pechora Alps"] Turistakie pokhody v "Pechorskie Allpy." Syktyvkar, Komi knizhnoe izd-vo. 1959. 147 p. WRA 13:6) (Pechora Valley-Description and travel) VARSANOFIYEVA, V-A. - Basic problems in the genesis and development of the relief of the Northern Urals. Trudy Komi fil. AN SSSR no-7:3-19 159. (MMA 13: 11) (Ural Mountains-Geology-History) VARSANOFIYEVA, V.A., prof., doktor geologo-rdneral. nauk, otv. red.; U'F!Z6Ij1L ~ Itekbn. red. [Collection of works on geology and paleontolog7) Sbornik tru- dov po geologii i paleontologii. Syktyvkar, 196o. 402 P. (mIRA 15:3) 1. Akaderdya nauk SSSR. Komi filial, Syktyvkar. (Geology) (Paleontology) SMCBEV, V.N.; UMVICH. LA. -L ; doktor geol.-miner. nank, Prof. MCK, X.M. Follow Lenin's attitude toward nature. IUn.takh. 4 no.6:2-5 Je !60* (MM 13 t 9) 1. Prezident Moskovskogo obshchestva Ispytateley prirody (for Sukachev). 2. Vitae-prezident Mo,skovskogo obahchestva ispytatelay prirody, chlen-korrespondent AN SSSR (for Zenkevich). 3- Vitae- prezIdent Moskovskogo obahchestva Ispytateley prlrod7, chlen- korrespondeat APS RSM (for "anoffyova). 4. Chlen Prexidiu- ma Soveta Moskovskogo obshch9stviriiiiii May pirody (-L'or Tanshin). 5- Uchenyy sekretarl Mo;kovskogo obahchestva ispytateley prirody (for Efron). (Natural resources) VARSANOPTINA, V.A.; BOUDAEOV) A.A.; OUSTSOV, Ya.A.; LUIGE.. 0.K.; t%RKLI14, R.L.; MUFLATOV., M.V.; F1,04YAKOVA, A.I.; PETRUSIRNSKLY, B.A.; SOKOWV) D.S.; SHVEETSOV, M.S.; LUZHIN, A.L. Nikolai Sergeavich Shatskii. Biul. MOIP. Otd,gsol, 36 no./,: 3-6 Ji-kg 161. (MIRA 14:9) (Shatakii, Nikolai Sargeavich, 1895-1960) VAHSANOPYEVAp V&A# Tectonic zimd geomorphologic development of the Ural-Timan region. Biul. MOIP, Otd.geol. 36 no.4:7-35 JI-Ag ,61.-- (MIRA 14:9) (Ural Mountain rogion-Goologyp Structwal) (Timan Ridge-Geology, Structural) CRERNOV, Georgiy Aleksandrovich; VARSMQV21M,-V..A.#.-doktor geologo- mineralogicheskikh nauk, otv.:ed.; DOLMATOV, P.S., red. izd-va; KOI;DRATIYEVA,, M.N.., tekbn. red. [Devonian sedimetits in the eastern part of the Bolshezemell- skaya tundra]Devonskie otlozheniia vostochnoi chasti Bol'she- zemel'skoi tundry. Moskva, Izd-vo Akad. nauk SSSR, 1962. 116 p. (MIRA 16:1) (Bol'shezemel'skeya tundra-Geology) BdODj 1.0., prof., doktor geol.-rdner. nauk;:~AqSAtiR F'YTTVJ"--V.A.j prof.) doktox- geol.-miner. nauk; VEELIKOVSKAYA, YeX., prof., doktor geol.-miner. nauk; GOIRDEYEV, D.I.,, prof., dok-tor eol.-miner. nauk; DOBROV, S.A., doktor pol.-ininer. nauk deceased]; KOF, ML.I., kand.tekhn.nauk~ Ldoceased]; KUM11CMA, f Ye.I., rladshiy naucbnyy sotr.; KUMIETSOV, Ye.A., prof., doktor geol.-t-iner. nauk; LEOUOV, G.P., prof., duktor geol.-r-iner. nauk; MENINEER.1 V.V., dotsent, doktor epol. -miner. nauk; NAZAREUKO, I.I., kand. sellkhoz.nauk; POBEDIMSKAYA, Ye.A., assistent; POPOV, S.P., prof., doktorgool.-miner. nauk; ScIUMOV, V.I.; S141WIOV, 11.11.1 prof., doktor geol.-miner nauk; ~11TOLIYATIIPOV, N.A.0 prof., doktor geol.-miner. nauk [deceased]; FENIKSOUA, V.V., datsent, kand.geol.-miner. nauk; SHMANOVSKIY5 I.I., prof., doktor geol.- niner. nauk; Prinimali uchastiye: BAHSAIJOV , G.P.0 prof.0 doktor geol.-miner. nauk; BOKIY, G.B.; GORSHKOV, G.P., prof., doktor geol.-miner. nauk; KUDRYAVTSEVj V.A., prof., doktor geogr. nauk; VURKOV, P.N., dotsent, kand.geol.-mi-ner. nauk; MOROZOV, S.S., prof., doktor gool.-miner. nauk; ORLOV, Yu.A., akademik; SERGEYEV, Ye.M., prof., doktor geol.-riner. nauk; TVALCHRELIDZE, A.A.; GEORGIYEVA, G.I., tekhn. red. (Continued on next card) BRODI 1.0.- (continued) Card 2. [justory of geology at Moscow University] Istoriia geologi- chenkikli nai 11c v Moskovskom unlversltete. Pod red. D.I,Gorde- eva. Moskva, Izd-vo Mosk. univ., 1962. 351 p. (mRA 15:7) 1. Moscow. Universitet. Goologicheskiy fakulitet. 2. Chlen- korrespondent Akademii nauk SSSR (for Smirnov). 3. Chlen- korrespondent Sibirskogo otdeleniya Akademii nauk SSSR (for Bokiy ). 4. DeystvitelInyy chlen Akademii nauk Gruzinskoy SSR (for Tvalchrelidze). (Moscow University) (Geology~--Study and teaching) VARSANOFIIEVA, V.A. Some problems of the stratigraphy and lithology of Carboniferous U sediments in the western slope of the Northern rals. Trudy Inat.geol. Komi fil. AN SSSR no.21n-26 162. (MIRA 15:7) (Ural Hount4ins--Geology,.BtratigreLphic) VARSANOFIYEVAt V.A. Stratigraphy of Middle Carboniferous sediments in the Malaya Pechora basin. Trudy Inst.geol.Komi fil. AN SSSR no.308-50 162. (MIRA 16:9) (Pechora Valley--Geology, Stratigraphic) I VARSANOFI M A, V.A. Nikolai Dmitrievich Zelinskii. Biul.MIP Otd.geol. 37 no,,1:130--144 Ja-F 162. MRA 15:2) (Zelinskii,, Nikolai Dmirievich, 1861-) VARSANOFIYEVA. V.A.; REYTLINGERI Ye,A, fter Devonian and Tournai sedimentii of the Malaya Pechora Valley. Biul.WIP.Otd,geol. 37 no.5136-W S-0 162. (WPA 15112) (Pechora Talley-PaleontologyStratigraphic) VARSAIIOFIYBVA, V.A. Aleksandr Aleksandrovich Chernov -1963; obiwary.Etui.101P. Otd. geol. 38 go.3.-120--122 My-je '6~.,~ (MIR-h 16:9) DEVYATOVA, E.I.; LOSEVA, E.I CHERNOV, A.A., doktor geol.-min. .; [deceased]; VARSANOPYEVA, V.A.P nauk, prof., otv. red. red.; VISKE, G.S., red. r3t-s-graDhy and palcogeograpby of the Quaternary of tho Me- ze.I.Basin]Stratigrafiia i paleogeografiia chetvertich- nogo perioaa v basseine r. Mezeni. Leningrad, Nauka, 1964. 104 P- WIRA 17:9) VARSANDFIYEVA, V.A. -.111--i- "1.- 1. .11 1 Vladlmir Afanaslevich Cbmchev and Y's role in the develormant of geological science; on the centeyy~rj of hla birth* Biul. MOIP, Otd. geol. 38 no.6al2&I46 N't 163. (MIRA 179.8) GUSLITSER, Boris lBaakovich; KANIVETS, Vyachealav Illich; WER, O.N., otv. red.; VARSANOFIYEVA. V.A., otv. red. [caves in the Pechora Valley portion of the UralB] Peshchery Pechorskogo Urala. Moskva) Naukas 1965. 132 p. (MIRA 18:11) 1AVD01") Aleksey Petrovich, akadomik[deceaged]; VARS90PIUVA, V.A., glav. red.; NENIER, V.V., otv. red.; YANSHIII, A.L..., -~ilGdemik, red.; GF-RASD*,OV, H.A., red.; DOLOOPOLOV, N.N., red.; 1,11KHAYLOV, N.F., red.; FUSHCHAROVSKIY, Yu.M.p red.; SHANTSER, Yo.V., red. [Comparative stratigraphy of the Boreal Mesozoic of Eurcipe] Sravnitellnaia stratiggraftia boreallnogo mezozoia Rvropy. Moskva, Hauka2 1965. 294 P. (""artt~ .18--n) VAIISSANOPYEV, V.D., Jnz)j.; GON(AIAHVD,11, f,F., kind. L,))ctjzi. miuk Problem of ellipt.-c condltlom in the oscillatlan-z o' -,-.,b-AlAv-1-- Taachine3. Nauch. aoob. I'D 26:106-109 165. 18.,?) NEVZOSp M.P,; VAnANOVA9 Ye.Ya.; MELINIK9 Ye.7u, t ----- ,1 4. Epidemiology of Bpt~inlc diseases in Tashkent. Zhur. mikrobiol. epid, i immun, 31 no. 5slIl-112 My 160* (MIRA 13:10) (TASHKENT-HE-PATITISt INFECTIOUS) a - _~,; MELNIK, Ye.Yu. NEVZOSY L.M.; CHICHENIB, F.I.; VARSANOVA,,--Xgt,)r Epidemiolo& of tetanus and its prevention in Uzbekistan. Trudy TashNIIVS 6:277-280 161. (MIRA 15:11) (UZBEKISTAN-TETANUC-) KHRMTS, L.B.; LEYTHAN, M.Z.; KUZIMINOVAp M.L.1 SALHINp L.V.; SLAVINA, A.M.; ZHDANOVA, L.D.; PIETNEVA, O.G.; KOYEXWp L.I.; GINZBIJRG, G.M.,- VARSANOVA, Ye.Ya.; MEWIM, YO.Yu. Studies on the epidemiological effectiveness of alcohol corpuscular and chemical aorbed typhoid and paratyphoid fever vaccines. Zhur. mi)mobiol., epid. i immun. 33 no.7: 53-59 J1 '62. (MIRA 17:1) 1. Iz Moskovskogo instituta vaktain i ayvorotok imeni Nechnikova i Tashkentskogo Instituta vaktoin i syvorotok. KHEYFETS, L.B.; SALMIN, L.V.; LEYTMANp M.Z.1 KUZ'KNOVAp M.L.; VASILIYEVA, A.V.; GALIPERIN, I.P.; SLAVINA, A.M.; ZHDANOVA, L.D. .PLETNEVA, O.G.,--VARSANOVA, Ye.Ya.; GINZBURG, G.M.; GLYAZER, N.G.; HELINIK, Comparative evaluation of typhoid fever vaecine prepared by various methods, materials from an epidemiologioal experiment in 1961. Zhur. mikriybiol., epid. i imm. 41 no. 200-76 F 164. (MIRA 17:9) 1. Moskovskiy institut vaktsin-i syvorotok imeni Mechnikova, Tashkentskiy institut vaktsin i syvorotok i Ashkhabadsk-iy institut epidemiologii, mikrobiologii i gigiyeny. VMAIIOVICH, A.D., inzh.; ZHURAVLEV, M.M., inzh. Scientific andtechnological. cooperation of the member-countries of the Organixation of the Socialist Countries for the Coopera- tions among their Railroads. Zhel.dor.tranap. 42 no.2:91-92 P '60. (KERA 13:5) (Railroads) Is- 6 0 -4 4 0 :a W-1 -01--l-I: 0 000 kC "- a 4141 1. F I la 11 u It Witte 1:141 "Olin a a is v 0 it 0 0 13 11 to a IS 0 a p a M J- it 7 0 1 sit 1- &.0 0-1 Of 9-4 T-11-4 0 Ig ' 1 go C .14,Mlj 1, puWrA .*o 00 I'm, ill'oul fou 'I.lairdit %ill IVA%r 14, Ile. 4441-lArd .0 0 pr"'" AiWatli 'lit h"41"9 Melhoall, 11,11. 1.( toot -00 00 all luill-isid 1mve Jecis it) sumpic wiling. US 1., livinjitithi. pa", lad"lrl* C11 drici-4410211"a of IWWSMT Suffill *A .00 Vir,.Ant 1"I't'lAr 431 "JAlio-h6s; to) dc4crimi"Ant of tho 'Illitit, pi-jil, 131 00 Om 01 1.9th 116.4414a&; Of W4:wd 10) vull"N.; in) j,"WOV., 0 t ill, Ill Ile ll,,,,righ I~prr ln-11mr.% 1-0 It-.411111; lit) suiJaho d4 Semitic a so &0 01--or fit ... I.-fil linvil, "I'llid )to inallitilrol'.'I IS111% in lasit-44ij Wermillb. While Mandardia.loel .I the 9040 1919. In file first 1,1,rr t owri ..f isullu,ity 6 emzr;,J oia In c1low "lopevaoSt ah it- * 0 Sit -11 Deptartment for the #'wfwr todustry of IW Mindy'rit a J. .111.1 N111% /or Milk tiWasirirs, thr Pwpff h4rortirrh JjWjj&jIr oled so lit, rilairrial. $1411-11110 Wolf ~"'j 11w, Imper CA111'. the Ituartaria" I)I/Ilee Mpill'.1, ~'( Alruila lu life Stork MW ramah-S low .1 so R 'A"rk.A ,I-, .10ti'l %- Ij..j JornalitilitiW lAnd PUhlithing Lit life -A,udArAlF- as* ts 41a Abe bAbU uf mill rilimitittex it is Wiled IWO Soo will he cart" out %u that It w0l. Is, too 0 I fort. JUM SU IlklihIMOV311111ir IOUSO"IUM for lialifily 64 VtWddbM 111 4PUr &W1111W 16114"lly. IWO. T OR It it I it Lt to 41 s 0 Is is 41 0 6 0 0 * 0 ip~o 0 0 0 0 0 0 0 0 0 0 KOVACS, J.tKOVACS, B.:SZARA 1, L.:VAYSMI, D. Antihistaminic propertips of plant tumors, 11serletes orvostad. 4 no. 4:272-275 Aug 1952. (CLKL 23:5) 1. Pharmacentics Institute of Szeged Medical University and Or- ganic Chemistry Institute of Budapest Lorand Notvos University. XCUTYAS, Firooka, dr.,; VARSARYI, Donee. dr..; FBIUM, Zoltan, dr. Comparative study of mass seroreaction in oyphilis. Borg7ogy. vener. szemle 8 no-5:139-141 Selpt 54. 1. Az Orstagoe Bor- es Nomikortani Intezat koslemenye (Igaigato: Foldvari Yerene dr. egretemi tanar) (SYPHILIS, diagnosis serodiag., routine mass exAm.) PEKM, Zoltan, dr.; VARSANTI, Donee, dr.; KONMS. Pirooka, dr. Zxperiences with dried and preserved blood serum in seradiagnosis of syphilis. Or7. hatil. 95 no.49:1354-1358 5 Dee 54. 1. Az Orazagoe Bor-lemikortani Inteset (igasgato: Foldvari Parana, dr, egyat, tanar) Szerologial Oastalyanak (yezeto: Fakete Zoltan dr.) kozlemenye. (SYPHILIS, diag. serodiag., dried serum reaction) ........... -?NMI -Zoltan -dr--- -VARSARYI Denes_,_ TES, Bodog..dr. dir VMR, ,ompar,Lt ive serological investigations with cardiolipin of omestic production. Ory. hatil. 96 no*.29:79D-794 17 Ju4 55. 1. Az Orazagoo Bor- Memikortani Inteset en a Budapesti OrvostudomaiWi Vaeteml Bor-es Nemikortani, Klinika (igazgato: Foldvari Ferenc-Ar. egyatemi tanar) kozlemerye. (CARDIOLIPIN, comparieon with other methode) YARSANYI, Danes,; ULLM41111, Agnes. Uperiments on the preparation of cardiolipin and lecithin for serological purposes in Hungary. Kiserletes orvostud. 8 no-3: 255-254 May 36 IV _~W,~Femik. -In Z *OB Budapesti Orvoet. Ia. 1.,'Prez . P O~vosi Ve&tani Intezele. (CARDIOLIPIU, prep. of for serol. purposes in Hungary, method (Run)) (LECITHIN, prep. of same) VARSANYI, Degnes'-Dr.; FWR7AN, Edet Dr. 7- Antiqvcotic effects of pentachlorophenol. 3orgyogy. vener. azemle 12 no.1-2:3_5-42 Feb-A-or 58. 1. Az Orazagoa Bor-Nemikortani Intez (Igazgato: Foldvari Perenc dr. ep,yetemi tanar) kozlemenye. (PM.NJOIS "ntachloronhenol & sodium salt, antinVeotic eff. & Tox. (Hun)) (CHIA)RIUM same) (YU14GI, eff. of drags on pentAchloro--)henol & sodium salt, antimycotic eff. (Hun)) ASZODI, Zoltan, dr.; VARSAITYI, Den6a, dr. Examination of aspecific serum positivit7 and distribution of serum proteins inepidemic hepatit1b. Orv.hetil. 100 no.30: 1790-1794 D 150. 1. Az Orazagoo Bor-Nemikortani Intezet (Igazgnto: Foldvari Ferenc dr. egyetemi tanar) ea az Orvostovabbkepso Inteoet (negb. igazgato: Barsony Jeno dr.) IV. belooztalyanak (foorvos; Aszodi Zoltan dr.) kozlemeWe. (BLOOD PROTEINS) (MRATITIS, INMTIOUS immunol.) LIEBBER, Erno. dr.; FLORIAR, Ede, dr.;.VARSANYI. Donee, dr. I.-..,-------.-- - ---------- Studies on the occurrence and prevention of industrial mycoses of the feet. Orv.hetil._101 no.47:1665-i67o 2o ul6o. 1. Orazagoo Bor-lemikortani Intezet. (FOOT die) (RINGWORM statist) (OCCUPATIONAL DISRASES statist) VIRSAIUI .-Deno&--- -.- . A simple apparatus for changing samples in flax-ephotometric studies. Kioerletes orvostud. 13 no.3:329-331 Je 161. 1. Orozagoo Bor. Nomikortani Intozet, Budapest. (PHOTOMETRI equip & supply) MASSZI Jozs0f; VARSANYI, Denes Study on the relation between catalase and amino acids. Kiserl. orvostud. 13 no.6:561-568 D 161. 1. Budapesti Orvostudomanyi Egyetem Bor- es Nemikortani Klinikaja es Orazagos Bor- es Nemikortani Intezet. (CATALASE chem) (AMINO ACIDS chem) RAN Istvan; VARSANYI, Denes Spectrophotometric microdetermination of papaverine de- compositior products. Magy kem folVoir 68 no.3:115-120 Mr 162. 1. Budapesti Orvostudomanyi Egyetem Gyogyszereazeti lntezete es Orszagos Bor- es Vemikortani Intezet 1P .-HUNGARY/Optics Optical Metiaods of Analysis. Instruments. K-7 Abs Jour Referat Zhur - Mika) No 5) 1957) 13091 Author Bardoez Arpad, Varsanyi Ferenc Inst Magyar Tudomaxyos Akad. Kozponti Fizikai Kutato Intezete, Budapest, HunjAry Title Spectrographic Analysis of Platino-Rhodium Alloys. Orig Pub Magyar kem. folyoirat, 1954, 6o, No lo, 292-296 Abstract A procedure ie, described for a quantitative spectrographic analysis of thin platino-rhodium wires, containing up to 5% rhodium. The analysis was made with molten specimens, with excitation of a condensed spark and electronic con- trol at a voltage of 1000 volta between the horizontal car- bon electrodes (one stationary and the other comprising a system of roteting rods, periodically immersed in the inves- tigated liquid. melts or in standard solutions). The Card 1/2 - ~ .: ~-. ---- -- -- ~ - - __z ... - -. - ~ . I - .1 . - .- . . ~ I I 77 t1todlum allo ul~ Atj,-A lioll ATIMTried out by the ex6faticm of v 116. con g fa%ttn&r-. -,he ends tA the IJIM; jjpacs )n a rotatWg brizO n tf . t . I . . . dip on ttlo~ 6114ft - Livia lu w4Q.1 ~qiU, i~ prepd. over tbe ran~g~ 1-25 f, th, the V ii s It 9 3-108,13 sp-zotrA line pair buinir usLA- The Owigtr 3, .8 R11 Imc c~~fl I)., u., ~! f, 01, ",lift, 'I'lle likean drVia- mm f I tb~ fo,nw, J-1, !71 th, I'l, ;.I:i I ~~Q 4- 23S3. witi; Ume-re=Ived 2 -it-T ;_rlrmr-- 1z SIT I I r-~q t Vq, -T h L-vr tuckground ftum I-age gr--k s-j-c desc-ibtd&nAillUSt11ted. It includes ar-electron Ally eantira!lec] spaez: w4lcc 9Lr-d a concale Mirror, the movemeent of wlzir-h Is syudrallm w,curat-4y with tb-- initiation of the separate $park discharges. The spectrum is detected photr- efttrkauy or photempwcally- The jA-An-g-- of the prococ,3re in Spectrochttilical awylis a" indicated by photOL-pbs -4 deasi curv" fQC the gDark tpoctrum of an Alloy of A) M1 per czat. Cu. By coating rre dde of the wirrar with At and W Other vftiv black -7t 14h., Omil-1- 4 by tha spark be-wt--n 29 and 54 nuczcsow- is used. t.bxm increasing the zatio of line to background dan,~ity. W. 13AJEER '4 el The g1rudwe of the 4c*mpltx*s fomt4 by cabaltow gl6kd C With ab$WUI~ OrpAIC golVenIS, (IreMle, %*ArS&ljyi (Vniv.. sirg"], flung- Aaa Con, N-Pja: '(1m.. d Phys. J. 117, 7--diWilRin Ench,lil. 41m, vW1.1c light 411- %Mption to Auhyd, COPCII In NIVOIL P1011, 111011, fluOll. - or AmOlf Awl p"Wine wa% examd. fly the Kbnig.Martrn~ (InJuIxtum phoi.mictet. A wirs I,( exptt. wj% cmducted in a Into. W FMIJ ill-01APPY1 V~ And pytridine. ivntg, U,15 t.) xt'llf" pyliliur. Thr villedmentally oht.dn"I 'Stine. Skin VAIU~~ for 4 .01vvra luixt. writc. 1) '25e`r pyridirte xrrAtly 41sdrml Itt"is the c.dol, valur~. 1,ArticulArPt At 11210 A A~ it Aji rrtkk.,f by cotatrof ttls Itut in an EtOlf oln. onle. ll.:1 ; joylitfille the rNinlr(ion drerra'"I 11rAr tht. nax., the rvi-fruer ,( a %elklefin"I normirtliate, tmiIxI., wring the ptobable f(mumIA CoICI-jEfoll). pv., "11114 to' w ctmitsvined- The Plot %Pill the most Stabw intermediate 11111alus 1101 In"le Owo (I 1:,e; pyfidmr. (on incorrmsing fit, pyriijuir coorn 1110 vulioui. rZifin lion cutvtv divrirgell Iv.1cmatirlilly limn the vw1rit itala, smikating thus the isfoluble r%Wflu, of A WmA, J."Ibly *I.* I,f St. third, own-mediatc. ]'his (Act excludes the povtihility of the I.w1fl-tion no, 4. Since no meaning cAll bt Qt1AChj4j In the -,wi,jencr of :.1 jistrrmedites i. a coc.,jj..Ijv,I of 4. The L',Wjjpj()jI (I" A* the exi't", #3 WAS cjfahjih",~ Ue 0 M Ifh al Well C11--fination no lortin Fintly C-AF Istit.t. lust Ainend oib 14"" was worsVi. '-- tnd (tit 16 47-51g1")), A Met ka distillatcl- 31.musim wgredknts lu tuhws 'r,, d &IILYL&M- ,OWU00~7' The thus tbc M-4 W- altm,liaw kdiW tfwWtlm" Lie awgic botaotot mm AX" Im mf" Ol a ced bl t qukkml With a ntal gra 04 tit Tbecaw.,C!'j ffimtstacmd's j&jjLyj&vxnslw It. so the PCIIAuctlm Also the 01149 1 4%. Imetion b-AC cul" ..... &tk is ne'.awy to 0 in new . Imemice of IlLyl dctivs- ,Dnlpds. must be ClIfisliwV11. lskfnww varAnyj. OSW 1. plawy rtt*M ichkvcmcnts. 1741,11"J".11-1-1 I 3Y. V X.I!:5arrTi. q,,. Ladik, J. "Utraviolat ~bsorptl.on ST:ectra of 11z;honyl-sulf me a'.,t ~-);-,rtzoiriasulforic acid; th-2 nature of th~,, 3=0 boril." p. 2'13. (licia Chtaica Academt-v) Sclentl~,M-_i hmillmkl:~-au. vol. 3' 110. 2, 19-~-)' Ixjapnstj SO: Konthly List of East 2uropean ,~c c --as ,~ ions, Vol. 2, 11o. 9# Librax7 of Con,-:,ress, Septc,:~ber 1953, Uncl Erg ik' V r-i ti 6 Distr: 4_22c(J) / Synthesis ol, organic fluorine compounds. XU. ijiLr:i._ fill n 1)1)ililjg 11,0 bath, Lnoled, rxinmd on ice, und the pitt. .tion-of fluorobeazene, - G 6T9y:0t1"Ttf_N_ 1,1.1 h Itird in tactio yieldvil a inixt. emag. 54% 11. It is 7 J~ nr nvc. Ctirvt:s of tht: litisfirption slwctrA of ~-, m;., an ---1IungqrIja AIMM.1.36., uddk M14NO, betweet, e 2600-31M A. a;e given and tit Mutil(KI, - '-flung. 7, 431-42(1955Xisi English); cf. CA. 50, 11201a; of qitant. awdy-'s try ah-lirptlui,. spcetris (Var,,,aflyi, C.A. 52, 52s'31-Phl? was nitrated by the following ineth,mN and 50, 71186i) simplified far mixts. tit products tit m,J. the PrOportkift Of FCsI44N0t Wrrnm formed detd. froui tim' wt. XIH. Derivatives of 2-fluero.-thirturethan. Gy6tv~y ultraviolet abir&ptlort spectm cagrnts' % ield. tentil. nf 010, Attila l1avikil, and L4-WO 1W. 443-9; reaction. and % p-, a., and ta=crs LqvenT. 35 Z. IINO~ of. CA. 49, GWli; 52. 3&1f~=Th: following Z-fluorddhyl: (op. gr. IAI) and 128 g. coned. 11*804.84.tr. -10% W. ll, -, urelhans, RMIC07(CIIINF, were prqxl. by adding 0.1: 40 g. HgS04.11,0, 25 IF. 80 11404. twit X j. NaN%, 004 intile CIC(VCI IINF (1) to 0.2 inult RNIJj cooled in Su ml. 71.2, 0% 90, 4, -; DiONOO, 1480, alliming tile, Inixt, to stan-I Overnight, M CrIn If I,*,, I 60.2, pode& 100. -j,~; CC4 + NjOs, 93S, coded, 72, 23, neussary. drying [lit! filtrate, All I I HqWd NA, - (8-5 9. from 25 9. PhF), rom tPlop., 78, 1_ 13, Nt0j vapor, " (41 g. from 96 g. PhIV. 1300 001vent, Rild I,% yield givC11f, -jrk h ' ' ___ crystg. 4- t ___\ 83.7; *-MeC411s, 76.1; "k 90, 10, Took reactloes -give larl AiMmixed ype Ut" b. -430% 82. J~JVCW,. -8% P~ and 10-28111o prezurnabI7 -40, 39.6; p-MC41[4, -, 13 glVe 72 an 171 - TIjr 1190% a hezine. 76% 80.0; t;0.8; P_Br I -aMMM-1somers. 1,2,4~ aCsfft, hexane, 84 Fcal'(141K from hexane, 941. AJI; ~1~;.bs 53-6% was prepti. in 0% yjdd 6?g.PhFvit 01,11sMA0 and 76g. fundiij IIN06 at pJFGff,. ht,,,e, 111-129 (ycUo# try"5), 82.3; O-Or 5tO06ln24.8!Tvykld(rws I0Ix,2,4-CICjf;(N0;Ninl0l NQU,, 30% M11, 62' (ytlloiw crrstals). 96 ,t* m-0!,- 4H", 30% Etolif Ne Virs. 0,105-40" in ultraviolet light with 51-211 $1.1, P.0SNCql1,j, 30zo MOIL, 20 C. dry KF, wid the proccss,repeated 3 times, and in 124-6`1 (yellow). 88.~; N-,64^AiV-MCthY(, 125- 79.8% Yield, w. 24% Trow 4t. M cooled and stirred with 70), 02.4; N-PG~e_x4yi, -, - X I . , * W11, W ' 0 dyl, MOB, 1060, 9.5 x, NjD4 Wet$ fix struill portions. I ( A H .5% 81.4, JAI.) added to: y-P ' Y MOH, 139" 'W.2 N 4 jr. 60% ok= at 04 witb 3 g. H,,SOA,HO a 3 F. fuming 7 6. V 150-400), 87.8.- W=1 W(d 8 S. fivitts 5;Ir' N i!~ flioroUlAtiaid1ko tned 510 Kt -,wu- A!.~�i -31 Irk 4nthes~s of 2-jIUorvdkYIUrdJ~4n' JV4Z-fiIJvfvdhnrbMIak, Me3CO .08-9-, M.4. With esttinse bloc agents (e.g. dlh%C~ propyl fluorophosphate), toxld doses of these compds. ad- ministered to animals produced no toxic symptoms. The' compd3. ire being tested as growth lahibitors for expti., A I- W-d cadcerous tumors. XY, Decomposition reactions of de-. rivativesoffluoroacetiCticid. Oyargy OlLh, Attila Pavil and C, B rw. 45i-3.-moroacetatei (1) with ;0&_9-XII.IIt9hL fluoroaceAmme whose 15% HIO 5013. Is stable. This win. treated with thloMe of lime Hofmann reaction) decotnp. compIttely. 2-Fluorooithauol' is also completely decompd. an alk. oxidation with M chlorideoflime. Blol.effectsoflandUareslaWar, XVU. ryeparation of Z-fluoroethyLimlni. Gy(kty OlAh and Attila Pav)Ath. ]bid. 481-1--See C-4. 50, 10042a. janei B. At, HUNGARY/Atomic and Molecular Physics - Statistical Physics-. Ther- D-3 modynamics Abs Jour : Ref Zhur - Fizi-ka., No 8., 1958., No 17727 under the assupption of thermdynanic equilibrium., in accor- dance with the requirement of the Gibbs-Duhen relations. The calculated values of the vapor pressure aad of the ac- tivity coefficient are given in a table and in graphs. Card 2/9 C01124UNIST CHINA / Physical Chemistry. Thermidinamics. B Thermoohemistry, Equilibria* Physico- Chemical Analysis. Abs J9.ur: Ref Zhur-Khimiya, No 24, 1958, 80650. Absti;oot: tration of each componeat in the saturated vapor. These pQncentraUqns are determinea by an optical method. Qu44tjtative analysis, based on absorption ppoc~ra, was described pro:- viously (Ref Zbar..'!Kh1m~ , 19561 26034). '44 introduction of this rerationship is applijo%ble tq Benzene-Benzeap Chlorlde system at W." T4e p x and log j -log x curves were thds coAr" . structed in which X=mol fraction, The resuW obtained with the aid 9f statistical me~ho'd c~r- respond to true thermo4yi;amic equilibri4a pnd follow the Gibbs-Dunham equation. Car,d 2/2 16 1960) 110.151 jABSTRACT : in thr, spegtrurm of II has an ovorhigh fracluoncy 1cont'd (1.2C0 en-1), supposedly because of the inter- action of AG and PT-i. '21-Us in-~L-Ieraction is im- peded in III, v4iich is expressed by ra decrease of the frequency of the investigated band ICO norrial values. In the ultraviolet spectrum of 1, a great ntvber of aboor-ption bands In the ran.oe of 35,000411,000 cm-1, partly sharp and pDrtly diffuse, are ob3orved. The sharn bands CAIM "15 13-8 :COUPITRY 1CATT-ORY iARS. Jam. RZKh:Lm. go. 1 AU-1VOR IUST. TITLE !ORIG. PUB. : MUDITRY B CAV-TiORY t ABS. JOUR* : RZKhim,,, No, 1 1960,, No, 151 AUTHOR IFST. TITLE IORIG. PUB. ABSTRACT diffuseness of the bands of AG is attributed cont'd to the superimposition of the frequ encies of torsional vibrations W1 of AG in relation to the ring. In the spectrum of II, both "eries are sharp (bands of G-0 tray3itions of AG and PiTo at 36,359 and 38.,090 cm- , respectivoly), since in this case the superimposition of the frequencies (A)l does not take placo because of froo rotation. ',his fact also points to the GARD: 415 B-9 COUNIRY B CATSGCRY ABS. JCUR. RZKhim.0 No, 1 196o, m4 151 AMFOR INST. TITLE CRIG, FUB. ABSTRACT absence of the effect of lVperoonjugaidon between oont'd PIT and the C112-group.-- V. Aleksanyan l ,CARD: 515 Some Structural P afw=tLe Odnes, studled an ~E~-vibratlwtal - I&OX the bads of thefr=1A and cl& (Tech Univ Budapest, Hung.). cliectirs. Gy. Var-Anj S. Holl POW.Sw Edylech. Z. 211-21! German .- a ra ed spectra (a the range 2S_15 p were presented for phenyl azide (1). b=A azide in),:, and 2J,&-tribromobentyl azide (M) as liquidi. and ultra- k vlolet va?" spectra In the mage 2470-2M A. weft pre- seated f0 I and U. AssIguments were made for most of the -9 for the absorption bands. In general, inhated frequencle three axides were similar with some lower values for 11 and.. M bemuse of their JaW rasu. Bands fair the atide group appeared for 1, 11, aud M, rmp., at 2115, 2115, 2108 for the asym. valence vibration, 1294. 1256, 1250 for the sym. vaience vibration (Lieber, el al., CA $1, 12Wf), 897, 875, -formation vibration. and 670, 677, 857 for the RNrN de 682 cm.-I, a poisible azide vibration. Ile higher wave noo. for I Indicated a higher electron d. between the two outer N atom, a rcsult of conjugation of the aside group with the ring. ne ultraviolet spectrum of I consisted of a system of sharp bands due to the ir dectrms of the ring.: with the 0-0 transition band st 36.359 cm.-', and a dif. fuse band system, due to die azide group, with its 0-0 band At25,Mcm.-1 Therefore conjugation was weak. Inn': the band systems were further apart, the bands of the azide~ ou -0 transition; r p were sharper than the ring bands, the 0 g of the ring appeared at 38,M cm. and that of the sxi& p occurs at 35,199 cm.-I It was concluded that' grou hyperconjugation was absent. The -1 effect of the azide group was less than that of Cl since the 0-0 Nuid of ben 0-1~1~chlzc appeated at 37.110 cm.~ (Ham=er and Matsen.- CA 42, 8640b). Mary Lvik4F-- Country : Hungary B-1+ Catogory : ftsical Chemiatri - Molecule. Chemical Band. Abs. Jour. : 11aferat Zhur-Xhimiya, No 6, 1959 18216 Author : Schay, G.; V~~an~ij Gy.; Dullien, F. Institut. : Hungarian Academ-y-ar'sSi~nces Title Investigation of Raman Spectra of Papha-Furyl and Xlpba-Benzofuryl Ketaximes. OriG Pub, Acta chim. Acad. scient. hung.t 19581 15, No 31 273-284 AbBtract Raman spectra were obtained of the solutions of stereoisimers of methyl-alpha-furyl ketox.'me (I&MF 740 and 1040), ethyl-alpha-furyl ketoxime (II; 7.'j and ? ), phenyl- alpha-furyl ketoxime (111; 149 and 1640), methyl-alpha-(5- methyl-furyl) ketoxime (IV; 83 and 1100)9 methyl-alpha- benzofuryl ketoxime (VI 151+ and 161o) and phenyl-alpha- benzofuryl ketoxime (V ; 11+5 and 15603, in pyridine and in benzene. In all instances stretching line frequency differs in spectra of C=N stereoisomers. To isomers having high values of 1.) G:~N (I, HP 740-9 111 780; 1119 149*1 IV, 1100i V, 1610; VI2 1450) is attributed a syn-configuration of the ketoxime group, The basis for this assumption is the fact 10ard: 1/2 Country : Hungary B-4 Catogory= : Physical Chemistry - Molecule. Chemical Bond. Abo, Joure : Pteferat zhur-KhImiya, No 6. 1959 18216 Autiior Institilte TItlc OrIS. Pub. : Abstract : that in syn-isomers2 in contradistinction to anti-isomers, the hydroxyl of the ketoxime group facing the furan- (or coumarone-) ring2 forms2 through the unshared pair of electrons of tne oxygen atomq a weak hydrogen bond with the hydrogen atom of the furan ring* This decreases the, participation of the oxygen atom in the conjugation with the turan (coumarone) ring, through the ketoxime groupq and must result in an increase ofV C=N- -- V. Aleksanyan. Card: 2/2 . VAMANYI, GY.; CSUROS, Z.; DSAK, GY. R-ximi nations by catalysts. XXIX- Catalyzed anmerization of with boron trifluoride. 11. Anomerization in chloroform. p. 389. Magyar Tudomanyos Akademia. Kemiai Tudomanyok Osztalya. KOZLEEMOYE1. Budapest, Eungary, Vol. 10, No. 3, 10,58. Monthly List of Fast Suropean Accessions (EEAI) LC.. Vol. 8) No. 7, July 1959 UNCL ' F 2 ) ( /1 c , j 4E3d j Distru sli of the ptAr OLOWIL-D- Anal :i7 Wil-1,11 , y Id 00110-criortfluoro pe 4 ~~4 ~1571. 13. 1w. blo,J-4 J mule , 347-375, 9 fip., 14 tnWI, A detailed Investigatiull Of V ar 11 ra ill tile Ile ittlectril 0 -tta Volve Shmved that t Ictl! sjl~cc tric vibratiolls I. e tile1 nic of trall-Sitioll, of totally syll, to tile silkillarity ) ue ImAoluillate. 1wrluitted kind, according to tileI V ctl!cs I .- c file tll( of cillor alld fIllorille these ) Iii0ter , ed to 0 n l . o pu I g Xpeetio bCl%aVc as if tllc~ 41)ectrjllll 0 f P.cbloro- uce tile t t V i i a t%8 or nary. o.11, f g5 It! structlint as t1lat, of Sillip ;r t i e ,e b1 I me Ims t rolmin j tile frecIllca- I Ill tile majority of caw lr , aIlIfItIc"ce of f dj,vrt.:ksetj as l i li- v vs o of X!tellite I)MILIvacco e fW1111101del 'Iteil fr()IIj t1leir k1j al , (: C m-'er Ijawk were allying the str( Utell. nt tv,IIPcrat r diff e e IlIcamirk-41 (it two tells-Ity rfli,10 of q (c jwj%%,evI1 tile ill 0111141 ll u il d l . o X cl allie Cttn alld tile -it and forbiddell parts of tile S thu 1wriniLit pe %v:ls estabUled. ili ti c g clulme 'e "toll"' l6tributina is, tj AV 13 T 00 Go StT ea3- Cal zv 3;,t;,Ojjq vslnw ,tTl - , -~3j, F - . - es S..4 ojsa~-~ ._1140 aw, e amIs TOT tyke M. rwAl. D~, gT (I 'Cie N, &0 Vao Oa d 1 t -1 G 0 v or, - % q'i tTaot,-011 vi ty~OT tjot GODS . a Nix T):o vo-0- L~a "505 SV1 ~.G Irb 145:2 OT _0tTOS00,9 110 Z1 8,%j $12 w, O-r O~ Vyjaa T05 tyle OCV'A~~ .1. ~. -, aTe ~,SO T arld. t,,res x1odaT 0 ala OT t9 . 'ate Ta .(3%, . t ~O 11, 1,8- 0To %:,) OT CuastT J~m, ^OeTTAcl f t r 8,as T OT t v4 it 0,11 _,T .,,1e T Q ..10-, OSSI 9 ss~lre OT ja a C,,,Ceat.~-a 'PTe Oil TT 'e'loaat, tts tyLo "'T EfflGARY/Analytic Chemistry. General ftics. Abe Jour; Ref Zhur-Plmlyap No 22, -1958, 73673, Author : Gy 'Vargamd. Inst :A6awflo'Miences of Hungary. Title :Analytical Use of the Ultraviolet Absorption Spectra of Saturated Vapor Mixtures. Orig Pub: Ac*,& chim. Acadi scient. hung., 1958., 14, No 3-4, 391 -406 - Abstract: It is shovn that the ultraviolet spectra of vapors of aromatic and some other uwatursted coupounds are very convenient to analytic utilization, in consequence of their great variety. At the use of the ojectrograyh slit narroved to a 20th to 25tb part of the usual width, not the absolute extinct- ion values, but the differences between extinction Card 1/3 EfflGARY/Analytic Chemistry- General Topics. E Abs Jour: RefeZhur-Kbimiya) No 22.. 1958, 73673. values of neighboring points, which are also pro- portional to the concentrations., are observed. Two neighboring points are chosen thus that the extinction value of one component should changeo in jumps, and that that of other components should change only insignificantly or even in the oppo- site direction. The raoult-Dalton, law can be used for the conversion of the vapor composition obtained in the result of the analysis into the composition of the liquid in the case of ideal mixtures - She described method was applied to a similtaneoug de- termination of the following substances dissolved in a saturated hydrocarbon: naphtbaline isome s, tetraline, c-resol, fluoranitrobenzene, chlorofluoro- Card 2/3 HMARY/Analytic Chemistry. General Topics. E Abs Jour: Ref Zhur-Mwdva~ NO,22, 1958, 73673. wA brcmofIu6r6denWe,, an Veilla's of immers of chlorofluorobemene) beftete, flUotobenzene and bro=benzone (6-coupondt mii6es). Card : 3/3 HUNGARY/Physical Chemistry - Molecule. Chemical Bond. Abs Jour : Ref Zhur Khimiya, No 19, 1959, 67o28 Author : Varsanyi, Gy Inst : HtuiGariaa AcaderW of Sciences Title : The Near Ultraviolet Absorption Spectra of 1,3- and 1,4-Deuterofluorabenzene Orig Pub Acta chira. Acad. Scient, hu"G-, 1958, 15, No 2~ 115- 138 D Abstract The author has added a few corxients to Wollmii's (J. Chen. Phys., 1946, 14, 123) ideas concerninG the near ultraviolet band-systea of fluirobenzene (I); and the vapor absorption spectrum of 1,4- and 1,3-deuterofluo- robenzenes is disavssed in detail. It was established that iii lieu of the d,)Ltble value for the frequency if the fundamental oscillation of I~ 1220 cn-1, measured Card 1/3 MIGARY/Physical Chemist-.-y - Molecule. Chemical Bond. D Abs Jour Ref Zhur IG-Amiya, No 19, 1959, 67o28 in the excited state, as well as in lieu of the 0-2 transition of the b, oscillation, a 0-1 transition of the other two a oscillations is more probable. The -ids of L,~- and 1,3 0-0 ba. -douterofluorobeiizenes ire lo- cated at 37,850 or 37,854 cm-1, and iii the case of I the 0-0 band is located at 37,819 cm-1. It was established that fundamental oscillations of frequency 1022 cm-1 ap- pear in I and in 1,341-otirobenzene, and.oscillatiois ci frequency 802 cm-l appear in 1,4-fluorobenzene in mre intensive series. La both deuteriizi-containii-G isomers an excited frequency was identified near 2200 cm-1 1,,-. 1. The frequency of this oscillation in dihaloGenbenzeiies is near 1200 cm-1. Tbe oscillati,in structure of Vie spectum of 1,4- and 1,3-deuterobluoribenzenes proved that the ft-idamental oscillations having the frequencies 1008 and 808 cip-1 are triGonometrically symmetric about the carbon skeleton. In this scheme, carbon atom Card 2/3 5 V IN e\s j, p of arommHe wid63.1looled on 1,v tiuii with th-3 ring thott.wh tho nrOu groul- vr the, bu , lli 414 ,11ittifir *britildn anS electron vibration . , ff-m., litmJ iynients vurn-spomlim: it) till, U10.1f, w),1. "j -V I 14. , - Ek r m A 114 i, A, 11 oil I., J, H f lillellyl itild bell-tyl RX1.1-n lippeal y r1ln!nivnl Eliging-cril; 1W. kii I rrwinlet of thnolo, I r,::I! 10,18, M-2'21,1 fig-,4., 3 tAl"l. 6,0 1: 1 'y'Al"m of t1;O Our, ii folu'll lit ic p1wityl Tbr, itirnmA simarn, of- phunyl, 1,enzyl awl 2, 4. it trl. , Z;d( it . - OnTi. at 3,41CO CM 1)ellZyl nZitin. It (Olk-4 Olat 1millill XljJYyl 41,kft,A*, will tilt) ultra V10101. mjwrtna m tho I a. Ole (Af(cL tif colijitgation nf tho 4ziflo tiroup (;it ths riog ix llullr~ illiti;4yi. On4 bermyl nzido4 Were studicd with llso fu!- ljetltz~,p, Ifint c-l' -liturinn wid liminino vJ:-orcag thet 3 vibreLlion mpectrilm of plimiyl w,jd,~ Ili group haa no vottiiigating effool. im ill(, O)rAtatilm ."ry sifniiiir In 114a A1140m or rno"ohalolol"ZOW.1 .1 vlOnk ollfrgy fur tbu ri:wr I oven lim; iit 110i lit- Ill Ill it latiril (legri'm of fil,;( I olumv-, Ccl6,w,khiq1 Ll not I'lolloill"fl-d ill the, V011o 0 lit of I dogrovii 13f rM.Pdom Ill) ilyumm,,11 I,, of [11101) 1 410 1' Lic-orOwl o4 provul Iii, tlii~ i6jimir. liir~ lbi-. Imml. vilirntimi of Ow oidda radif-di ittid tilt, tion of tho bi-.rtl ~ymtf-m, will by Ow fv,t Ollit ..- iwil ti;!, Otill-r' tt wo. Ou regarilml nm di-Formition Ohratiom. A Vowl c%coption of' ow! ?ihl lit iof-~ -- t 14) tu 0 t! I!!; Ifirt. of-MiAl ring fretitwitt-lim efut al&o Ito found in tho j4lx:rti-,t mtirjus cumbimi iiiii)- tritit t1wir owi~ vibrati,m irjri,(;1iwi~4, I.wf bpiiAA-j9k1 tribromobonzyl a4de, ~oivclvvr, in tho lititus, FlIrthPL11101" tim bund siy-dem tit t'.0 fljjjjj gr(;.,1,71, 3rjjfjl i-tinil , luld At a iilvlo or lou iodurorl vniam Thom in it motio. eampArtAm ill% alipluillo t1pillo fl-ctill"Imil ~4, k 4liftl I lit t lit, ~jw,! t 01114" douredpl~ of 00 mlita rrollulmoles froin, phorwyl AxidD ill- trum of plimlyl UZ1114 lint Intillrd tho ILA hilt inmird illo Alit jlk~ lliil,thl. tilts differt)nvo. for tho so-called oym. violt.,t I*- tiomn 20 A which indi--ilwh thitt hvium-wil,qvitio" Illet I,[,- 'Wild, Vililrailoll Imillig thO ' 8014iflit, 114ANVE-11k of tilt, nlethyll-110 grolill mx.:th it.4 uffvrt luthor tilt! "1110 W4141 aziikll~ Thia vibrettlan mtky ho conaldorud am Ifit, .117.ille group 111,111 tosvilid illp lit'll. lmi& vibrittion ttt tho Lwo torminal nitrage-lit atomill, thu-st i;ho bond order between them - is incrowled in phunyi "wo q 1 Diartrr lor 0 ew)- lWO). IM. W)" v Inngftation of die W4 1272, 'lai EUTI ke 14 1701 W), I. G~(w), 1481 V. Admo, 14 %) 149~- t. m 1624 m P k2 STE-1 15723tes S. lam !3 i.- 1546. I vii. H UO(in EWE ). 1u J. , frequencits Iz cm.-I v.-m found, far P.43-Methyl-2- 411 ad 480 9), e.s. 11*5*(M), 1590(m T fuiryl,kctozlmc (m. W) Ln b-caxne 11~ a YrLdice (11). MoIt p I s S72 sh Hail Mit(w); lWe st i . . xii-amthayt-22-If 4 U O ,n a uryl ketoxime (m ty-t-hyt-2- 125,5(s)- 1607(cs.). IWes.), z 448( y1 ketaxime (m. 78*) in I and U. crai-ethyl-24uryl ketor. ea.), tu , 4 03h I I(W); 610(cg.j. MIA(a (m. 73') in I and U, sy*-methyt-&-cthyl-MuryJ ISGO -4.). 1446(m). 104- 1 1 (w IL-CN r" 1607 7 1447 x IW 1) ) ( ' - . j; , ~ ketoxi= (m. UWL"v W 1 - .. ~-- .--- . -.-- 71 It. (RrfitdJ:---- t yAtwmv vy Ug "M aca awl- J-- an Outs)i -4 soty*d Uma (e;V. hi -v -14 4 ke (M. 1612) in, =ti= Mwer&. (In),.tqpdcmte. (s) Mal& 0.*.) curtmelyj 'Mau. - gthyl-2-b f! lm. 1611 In 11 , y"2-beawmi Ixtoxisne (cm. 154 k 11, cyr-phcmA._* !.tt V, Om the bub of diffactm In CN frequencies be-f - s P. tween pahv of 6omem od 24aryl and 2-bemtofuryl comod ! - 1rn WjI ketoxime (m. 143 ~n H, and arV-PviCM*2- ) .1 benzefiLryl ketaxime M. 156*) In U: 1 5* 8). 1 m it it" comfuded #Jut In m dafts. theO atom -A the OH gm--i, of the arf 16M I to 1-mediatdy adia"at to the ortho H , I 1370(w) 1429(w)- I % if the rims, A wmk H band is fmmcd !,4 the d,p~ 4 A77 J 4__Uon with the Is reduced. H. W. A=k,!r QILL