• TECTONIC SETTING AND GEODYNAMIC NATURE OF THE SAINT ANNA TROUGH (NORTHERN BARENTS-KARA CONTINENTAL MARGIN) 

  Shipilov E.V.; Matishov G.A. (2006)

  he present paper is based on the geotectonic interpretation of marine geological–geographical data with consideration of publications devoted to paleomagnetic investigations and isotope datings of rocks from the adjacent ...
• POSSIBILITY OF MAPPING PHYSIOGRAPHIC ZONES BY THERMAL SURVEY FROM SPACE 

  Gornyy V.I.; Kritsuk S.G. (2006)

  Physiographic zones of the Earth are “major units of the geographic (landscape) sphere, which give way to each other in a regular and definite order depending mainly on the ratio of heat and moisture”. The rise in the ...
• NATURE OF SPECIFIC GEOCHEMICAL FEATURES OF OIL 

  Marakushev A.A.; Marakushev S.A. (2006)

  Oil and especially the related associated bitumen, in particular, are characterized by high metal contents with a predominance of V, Ni, and Zn that make up a specific “oil” assemblage. Based on the prevalence of one of ...
• INCLUSIONS OF ZIRCON-BASED SOLID SOLUTIONS IN DIAMONDS 

  Silaev V.I.; Petrovsky V.A.; Sukharev A.E.; Filippov V.N. (2006)

  We studied micropolycrystalline diamonds from modern and Neogene–Quaternary alluvial placers found in the main diamondiferous areas of Brazil (Minas Gerais, Bahia, and Mato Grosso). The polycrystalline inclusions were found ...
• IMBRICATE THRUST STRUCTURE OF THE NORTHWESTERN CAUCASUS 

  Popkov V.I. (2006)

  Many geologists suggest a determinative role of folding in the formation of the Northwestern Caucasus structure. Mapped or drilled thrusts are considered minor structures complicating steep fold limbs. Moreover, they are ...

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