Предисловие	5
	В.Д.Каминский, В.А.Поселов, Г.П.Аветисов, В.В.Буценко, П.В.Рекант. Широкомасштабные геолого-геофизические работы ВНИОкеангеология с борта атомохода «Россия» по проблеме внешней границы континентального шельфа России в Арктике  (.pdf)	6
	В.Л.Иванов, В.Д.Каминский, В.А.Поселов, О.И.Супруненко.  Региональное геолого-геофизическое изучение арктического шельфа – ключ к наращиванию нефтегазового потенциала России (.pdf)	20
	Г.П.Аветисов.  Сейсмологические исследования НИГА–ВНИИОкеангеология в Арктике (история, достижения, перспективы)  (.pdf)	27
	А.Н.Евдокимов, А.Н.Сироткин, М.Ю.Бурнаева, Е.С.Радина.  Первые данные о кимберлитах на архипелаге Шпицберген  (.pdf)	42
	Я.В.Неизвестнов, О.И.Супруненко, О.В.Боровик, Н.Л.Колчина, Н.А.Куринный, Т.Н.Францева.  Мерзлотно-геотермические проблемы освоения нефтегазовых ресурсов Российской Арктики  (.pdf)	50
	В.И.Петрова, Г.И.Батова, А.В.Куршева.  Органо-геохимические исследования донных осадков в районах нефтедобычи (на примере шельфовой зоны о. Колгуев, Печорское море)  (.pdf)	60
	Д.Ю.Большиянов, И.А.Погодина, Е.А.Гусев, В.В.Шарин, В.В.Алексеев, В.А.Дымов, В.М.Анохин, Н.Ю.Аникина, Л.Г.Деревянко.  Новые данные по береговым линиям архипелагов Земля Франца-Иосифа, Новая Земля и Шпицберген  (.pdf)	68
	Л.Г.Деревянко, Е.А.Гусев, А.А.Крылов.  Палинологическая характеристика меловых отложений хребта Ломоносова  (.pdf)	78
	П.В.Рекант, Е.А.Гусев.  Признаки новейших тектонических движений на Лаптевоморской континентальной окраине по данным сейсмоакустического профилирования  (.pdf)	85
	В.В.Иванова, М.А.Анисимов.  Особенности криолитогенеза в лагунных отложениях острова Жохова  (.pdf)	95
	В.И.Слинченков, Ю.Г.Самойлович, В.В.Николаев, В.М.Константинов.  Строение кайнозойских отложений северной части Обской губы Карского моря по акустическим данным  (.pdf)	106
	Б.В.Беляцкий, А.В.Андроников.  Возраст верхней мантии района озера Бивер (Восточная Антарктика): Sm-Nd изотопная систематика мантийных ксенолитов  (.pdf)	118
	З.В.Пушина.  Комплексы диатомовых водорослей в позднечетвертичных донных отложениях залива Прюдс (Восточная Антарктика) и их биостратиграфическое значение  (.pdf)	139
	Г.П.Аветисов.  Имена сотрудниковНИГА-ВНИОкеангеология на картах Арктики и Антарктиды  (.pdf)	153
	В.В.Дремлюг.  Военное лихолетье  (.pdf)	167

	Preface	5
	2009
	V.D.Kaminsky, V.A.Poselov, G.P.Avetisov, V.V.Butsenko, P.V.Rekant.  Large-scale geological and geophysical investigations of VNIIOkeangeologia from the board of atomic icebreaker «Rossiya» under the problem of outer limits of Russian continental shelf in the Arctic	6
	17.04.2009 г. V.D.Kaminsky, V.A.Poselov, G.P.Avetisov, V.V.Butsenko, P.V.Rekant LARGE-SCALE GEOLOGICAL AND GEOPHYSICAL INVESTIGATIONS OF VNIOKEANGEOLOGIA FROM THE BOARD OF ATOMIC ICEBREAKER «ROSSIYA» UNDER THE PROBLEM OF OUTER LIMITS OF RUSSIAN CONTINENTAL SHELF IN THE ARCTIC Integrated geological and geophysical field works from the board of atomic icebreaker «Rossiya» were carried out in May–June 2007 in the transition zone between the Lomonosov Ridge and the adjacent shelf of the East-Siberian and the Laptev Seas. A primary goal of these investigations was the implementation of the UN Commission’s recommendations regarding the preparation of Russian claim connected with validation of outer limits of Russian continental shelf in the Arctic. Methods and results of above field works as well as main tasks of future investigations are presented in the article. Key words: The Arctic Ocean, outer limits of continental shelf, geological and geophysical investigations.
	V.L.Ivanov, V.D.Kaminsky, V.A.Poselov, O.I.Suprunenko.  Regional geological and geophysical studies of the Arctic seashelf as a key to the growth of the Russia’s oil and gas potential	20
	17.04.2009 г. V.L.Ivanov, V.D.Kaminsky, V.A.Poselov, O.I.Suprunenko REGIONAL GEOLOGICAL AND GEOPHYSICAL STUDIES OF THE ARCTIC SEASHELF AS A KEY TO THE GROWTH OF THE RUSSIA’S OIL AND GAS POTENTIAL The article indicates that the regional geological and geophysical studies in discovering and establishing the basis of the Russian Arctic sea shelf hydrocarbons are of extreme importance. The studies emphasize the necessity of the future development of these works. Parallel to the traditional geographic sea shelf, a «juridical» deep-sea Arctic basin may be considered as a possible object of resource finding activities. Its belonging to the continental margin of Eurasia is proved according to the UNO Convention on the law of the sea of 1982. Keywords: regional studies, oil and gas bearing, geographic sea shelf, juridical sea shelf.
	G.P.Avetisov.  Seismological investigations of NIIGA-VNIIOkeangeologia in the Arctic: history of study, progress, prospect	27
	29.05.2009 г. G.P.Avetisov SEISMOLOGICAL INVESTIGATIONS OF NIGA-VNIOKEANGEOLOGIA IN THE ARCTIC: HISTORY OF STUDY, PROGRESS, PROSPECT Information about seismological investigations of NIIGA-VNIIOkeangeologia in the Arctic is presented in the article. Expeditionary observations were begun in 1968 and carried out in the Frantz Josef Land, New Siberian Islands, Western Yakutiya, Norilsk’s Region, and Lena’s River Delta. Some features of deep geological structure in the areas of study are discovered. Digital bank of cumulative seismological data in the Arctic is compiled. Hypocenters and focal mechanisms of earthquakes in the Arctic are studied based on compilation and analysis of all available seismological data. Some new ideas about present-day geodynamics are developed. Key words: Arctic, earthquake, data bank, focal mechanisms, geodynamics, geological structure.
	A.N.Evdokimov, A.N.Sirotkin, M.Yu.Burnaeva, E.S.Radina.  First data of the kimberlites in the archipelago Spitsbergen	42
	17.04.2009 г. A.N.Evdokimov, A.N.Sirotkin, M.Yu.Burnaeva, E.S.Radina FIRST DATA OF THE KIMBERLITES IN THE ARCHIPELAGO SPITSBERGEN For the first time the kimberlitic accessory minerals of diamond paragenesis are discovered in the Paleozoic mafite - ultramafitic Spitsbergen’s dikes. In this connection the complex of picrite Middle Paleozoic hypabyssal rocks of archipelago is referred to the pyropic subfacies of the kimberlite, the forming possible northern branch of Arkhangel’sk diamond-bearing province. The keywords: Spitsbergen, kimberlite.
	Ya.V.Neizvestnov, O.I.Suprunenko, O.V.Borovik, N.L.Kolchina, N.A.Kurinnyi, T.N.Frantceva.  Cryogenic-geothermal problems in development of petroleum resources of the Russian Arctic	50
	17.04.2009 г. Ya.V.Neizvestnov, O.I.Suprunenko, O.V.Borovik, N.L.Kolchina, N.A.Kurinyi, T.N.Frantceva CRYOGENIC-GEOTHERMAL PROBLEMS IN DEVELOPMENT OF PETROLEUM RESOURCES OF THE RUSSIAN ARCTIC Cryogenic-geothermal conditions of the petroleum provinces and basins of the Russian Arctic offshore and onshore territories against the background of the permafrost rocks degradation of the Eurasian permafrost area, started from the end of the Late Neo Pleistocene have been discussed. It was shown that the unit of permafrost rocks within hydrocarbon plays has two stage structure. Cryogenic rocks of the upper stage contain «normal» ice-cement. The cement in the lower stage admittedly is gas hydrate. Some data on gas hydrate deposits from the Mackenzie River Delta and from the shelf zone of the Beaufort Sea, which have similar environment, have been sited to support the assumption. Key words: Permafrost rocks, gas hydrate negative temperature waters (cryopegs), hydrocarbon plays.
	V.I.Petrova, G.I.Batova, A.V.Kursheva.  Organo-geochemical study of the bottom sediments in oil producing areas (by the example of the Kolguev island shelf zone, Pechora Sea)	60
	25.05.2009 г. V.I.Petrova, G.I.Batova, A.V.Kursheva ORGANO-GEOCHEMICAL STUDY OF THE BOTTOM SEDIMENTS IN OIL PRODUCING AREAS (BY THE EXAMPLE OF THE KOLGUEV ISLAND SHELF ZONE, PECHORA SEA) The structure and content of the basic parameters of organic matter of sediments from Kolguev island shelf zone were studied. In general, the data obtained corresponds to the geochemical background of the coastal-shelf facies of the Arctic shelf. The content and distribution of PAHs indicate the leading role of pyrogenic sources in the formation of the hydrocarbon group. Anthropogenic influence at the moment is small and local. The keywords: Organic matter (OM), hydrocarbons (HC), total organic carbon (TOC), carbonate carbon (Ccarb), polycyclic aromatic hydrocarbons (PAH), high pressure liquid chromatography (HPLC).
	D.Yu.Bolshiyanov, I.A.Pogodina, E.A.Gusev, V.V.Sharin, V.V.Alekseev, V.A.Dymov, V.A.Anohin, N.Yu.Anikina, L.G.Derevyanko.  New data on the coastlines of archipelagos Franz Josef Land, Novaya Zemlya and Spitsbergen	68
	14.05.2009 г. D.Yu.Bolshiyanov, I.A.Pogodina, E.A.Gusev, V.V.Sharin, V.V.Aleksev, V.A.Dymov, V.A.Anohin, N.Yu.Anikina, L.G.Derevyanko NEW DATA ON THE COASTLINES OF ARCHIPELAGOS FRANZ JOSEF LAND, NOVAYA ZEMLYA AND SPITSBERGEN A few marine terraces were reported at Spitsbergen (Svalbard, Grumant), France Joseph Land, and Novaya Zemplya archipelagos, which appear to correspond to ancient shorelines. Radiocarbon and U-Th dates evidence for Neopleistocene to Early Holocene age of these terraces, and their altitude above modern sea level ranges from 5 to 60 m. Analysis of foraminifers, spores, and pollen suggests mild, relatively warm and shallow-water marine environment. Keywords: Spitsbergen (Svalbard, Grumant), France Joseph Land, and Novaya Zemplya, Radiocarbon and U-Th dates, analysis of foraminifers, spores, and pollen suggests mild.
	L.G.Derevyanko, Е.А.Gusev, А.А.Krylov.  Palyonological characteristics of cretaceous rocks from Lomonosov ridge	78
	13.01.09 L.G.Derevyanko, Е.А.Gusev, А.А.Krylov PALYNOLOGICAL CHARACTERISTICS OF CRETACEOUS ROCKS FROM LOMONOSOV RIDGE We studied spores and pollen from the rocks sampled at Lomonosov Ridge in the framework of International Ocean Drilling Project (IODP-302) in 2004. Spore and pollen complexes of Lomonosov Ridge were compared to those of Maastrichtian - Danian age described in Siberia and Russian Far East. Keywords: Lomonosov Ridge, Upper Cretaceous, spore and pollen.
	P.V.Rekant, E.A.Gusev.  The seismic-acoustic evidences of the recent tectonics on the Laptev Sea continental margin .... 85	85
	17.04.09 P.V.Rekant, E.A.Gusev THE SEISMIC-ACOUSTIC EVIDENCES OF THE RECENT TECTONICS ON THE LAPTEV SEA CONTINENTAL MARGIN New evidence confirming recent tectonic movements at the Laptevs Sea continental margin was obtained by interpretation of high resolution seismic data. This evidence includes both direct and indirect manifestations. Direct ones are observed modern faults, indirect, fluid discharge zones thought to originate from these. Despite the wide occurrence of faults in the lower part of the sedimentary cover, only some of them penetrate the Quaternary sequence, as is seen at seismoacoustic profiles. Key words: Laptevs Sea, neotectonics, high resolution seismic, gas seepage.
	V.V.Ivanova, M.A.Anisimov.  Character of cryolithogenesis in lagoonal deposits at Zhokhov Island	95
	17.04.09 V.V.Ivanova, M.A.Anisimov CHARACTER OF CRYOLITHOGENESIS IN LAGOONAL DEPOSITS AT ZHOKHOV ISLAND The base of this article are the results of studies of lagoonal deposits at Zhokhov Island. This study was conducted and supported by the Russian-American archeological project "Zhokhov-2000". Features of lithofacial and chemical-mineralogical composition of frozen lagoonal deposits at Zhokhov Island are discussed in this report. Physicochemical and mechanical processes in frozen deposits have been considered, features of authigenic minerals formation and mechanism of forming of frozen deposits, features of their composition and properties have been established. Keywords: Submarine cryolithogenesis, macro and microstructure properties, granulomineralogical analysis, luminescence.
	V.I.Slinchenkov, J.G.Samoilovich, V.V.Nikolaev, V.M.Konstantinov.  Cainozoe deposits structure of a northen part of Ob Gulf (Kara Sea) accoding to the results of acoustic profiling survey	106
	14.05.09 V.I.Slinchenkov, J.G.Samoilovich, V.V.Nikolaev, V.M.Konstantinov CAINOZOE DEPOSITS STRUCTURE OF A NORTHERN PART OF OB GULF (KARA SEA) ACCODING TO THE RESULTS OF ACOUSTIC PROFILING SURVEY Acoustic profiling survey took place at 2005-2007 as a part of geoecological researches. Upper layers of bottom sediments were described. Intercoupling between geological and reflecting borders was established and proved. Morphological features of a bottom surface and their connection with contemporary exogenous processes were established. Areas of a possible permafrost rocks were defined so as there depth. Keywords: Gulf of Ob, ultrasonic profiling, border, bottom sediment, sediments section, profile, gas-saturated rock, frozen ground.
	B.V.Beliatsky, A.V.Andronikov.  Sm-Nd Isotopic Age Estimations for Mantle Xenoliths from the Beaver Lake Area (East Antarctica)	118
	03.06.09 B.V.Beliatsky, A.V.Andronikov SM-ND ISOTOPIC AGE ESTIMATIONS FOR MANTLE XENOLITHS FROM THE BEAVER LAKE AREA (EAST ANTARCTICA) Using Sm-Nd isotope data on mantle xenoliths and mineral separates thereof from the East Antarctic Jetty Peninsula area, authors try to estimate the timing of various events affected lithospheric mantle beneath the northern Prince Charles Mountains and probable evolution way of the mantle reservoir. Sm-Nd TDM model ages for the studied xenoliths suggest that the first differentiation of the mantle reservoir took place ca. 4.2 Ga, and thence upper mantle developed as depleted residual reservoir till ca. 2.5 Ga (isochron age 2438±200 Ma) when thermal erosion and mantle depletion changed Sm/Nd ratio of the rocks. During the subsequent period of time, probably till the generation of the Proterozoic mobile belt ca. 2.0 Ga, the regime of stable platform could predominate in the region. The upper mantle was more „conservative“, and stable conditions therein existed till ca 1.1 Ga when the collision between the Indian and East Antarctic Shields occurred. This event was recorded in Sm-Nd isochron ages of the xenoliths from the very beginning of the collision (1140±150 Ma) through the intermediate and probably the most severe stages of the collision (1090±120 Ma) till postcollisional deformation, folding and granulite metamorphism (925±82 Ma). That was probably accompanied or immediately followed by general enrichment of the upper mantle horizons as a result of the influence of submerging slab of oceanic lithosphere. The time of ca 0.9 Ga is considered to be the timing of the total enrichment and complete separation of the xenoliths source from the depleted mantle reservoir. Younger tectonothermal events such as related to Panafrican Orogeny were also reflected in partial resetting of the isotopic systems but at lesser extent. Keywords: upper mantle, isotopes, xenoliths; model age; isochron age; East Antarctic.
	Z.V.Pushina.  Diatom assemblages in the Late Quaternary sediments of the Prydz Bay (East Antarctica) and their biostratigraphical significance	139
	14.01.09 Z.V.Pushina DIATOM ASSEMBLAGES IN THE LATE QUATERNARY SEDIMENTS OF THE PRYDZ BAY (EAST ANTARCTICA) AND THEIR BIOSTRATIGRAPHICAL SIGNIFICANCE Results of the diatom distribution in sediment cores from the Prydz Bay (East Antarctica) are described. Ecostratigraphical approach to subdivision of Holocene sediments on three diatom zones, which were formed during early, middle and late Holocene was developed. Keywords: Prydz Bay, diatoms, Holocene.
	G.P.Avetisov.  Names of NIIGA-VNIIOkeangeologia employees on the maps of Arctic and Antarctica	153
	27.05.09
	V.V.Dremlyug.  Troubled years of war	167
	14.01.09