Устинов Н.В., Покровская И.Е.
Верхнеюрские «черные глины» Баренцевоморского шельфа // Геологическое строение и нефтегазоносность Арктических морей России // СПб, ВНИИОкеангеология, 1994, с. 19–29Устрицкий В.И., Храмов А.Н.
Геологическая история Арктики с позиций тектоники литосферных плит // Моря Советской Арктики. Л.: Недра, 1984. С. 253–265.Хуторской М.Д., Подгорных Л.В., Ахмедзянов В.Р.
Геотермическое поле и термическая эволюция литосферы Баренцевоморского региона // Вестн. РАЕН, № 5, 2000. С. 55–77.Хуторской М.Д.
Геотермия Центрально-Азиатского складчатого пояса. М.: Изд-во РУДН, 1996. 289 с.Хуторской М.Д., Подгорных Л.В.
Объемная модель геотермического поля Баренцевоморского региона. /Докл. РАН, т. 377, № 1, 2001. С. 265–269.Цыбуля Л.А.,Левашкевич В.Г.
Тепловое поле Баренцевоморского региона. – Апатиты, 1992. 114 с.Шеридан Р.
Атлантическая континентальная окраина Северной Америки // Геология континентальных окраин. Т.2. М.: Мир, 1978. С. 82–101.Эринчик Ю.М., Мильштейн Е.Д.
Рифейский рифтогенез центральной части Восточно-Европейской платформы. С.-Пб. Изд. ВСЕГЕИ, 1995. 48 с.Bates J.L.
East coast basin // Atlas series Scotian shelf. 1991. GSC. 152 p.Crough S.T., Thompson G.A.
Numerical and approximate solution for lithospheric thickening and thinning // Earth & Planet. Sci. Lett.,1976, v.31, P. 397–402.Dziewonski A.M.
Mapping the lower mantle: Determination of lateral heterogeneity in P-velosity up to degree and order 6 // J.Geophys.Res. 1984. vol.89. P. 5929–5952.Dziewonski A.M., Anderson D.L.
Seismic tomography of the Earth`s interior // Amer. Sci. Let., 1984. vol. 72. N.5. P. 483–494.Fairhead J.D.
The structure of the lithosphere beneath the Eastern rift, East Africa, deduced from gravity studies // Tectonophysics, 1976, v.30, P. 269–298.Judge A., Jessop A.
Heat Flow North of 60 N.– In: Arctic Geophysical Review (J.F.Sweeney, ed.). Publications of the Earth Physics Branch, v.45, N 4, Ottawa, Canada, 1978, pp.25–33.Rowley D.B., Lottes A.L.
Plate-kinematic reconstructions of the North Atlantic and Arctic: late Jurassic to present // Tectonophysics. 1988. 155. P. 73–120.Seismic tomography: Theory and practice // Ed. By H.M. Iyer and K.Hirahara, L., 1993. P. 519–584.
M.D. Khutorskoy[229]
, Yu.G. Leonov[230], L.V. Podgornykh[231], A.V. Ermakov[232], V.R. Akhmedzyanov[233]. Geothermal studies of Arctic Basin – Problems and SolutionsAbstract
2D– and 3D-modeling of geothermal field along geotraverses in Western-Arctic and in Podvodniki basins carried out. These ware constructed on deep seismic profiling and drilling data. The catagenetic transformation depths of organic substance for various parts of the sedimentary basin are designed. This interval least depth is dated for Southern-Barents basin where on the prospecting data the highest hydrocarbonic potential is established. On 3D-models «the thermal dome» is dated for this area, allocated for the first time. Heat flow measurements data in the northern part of Svalbard plate near Franz-Josef Land (FJL) and Spizbergen are resulted. Measurements were carried out by new updating geothermal probe «GEOS-M». Seven heat flow measurements on «FJL» and twenty – on «Spizbergen» are received. On first of them heat flow variation from 30 up to 85 mW/m2
are connected both with trough valley Franz-Victoria tectonic activization and with structural and thermal conductivity heterogenesis inside sedimentary cover. Abnormal heat flow values (from 120 up to 519 mW/m2), measured in trough Orly (to the eastern of Spizbergen North-East Land), testify to rift zone development which completely destroyed a continental crust. These researches were carried out at financial support of the Norwegian oil management, as well as Russian Academy of Science, Earth sciences branch of the Russian Academy of Science and the Russian basic research Foundation.