• A GEOTHERMAL MODEL OF THE LITHOSPHERE IN THE BAIKAL RIFT ZONE WITH CONSIDERATION OF ADVECTIVE HEAT AND MASS TRANSPORT BY ENDOGENOUS FLUIDS 

  Golubev V.A.; Zubkov V.S. (2006)

  The lithosphere of rift zones is characterized by high permeability. Therefore, discharge of endogenous fluids is confined to these zones. Additional heat transport related to their flux should be reflected in the joint ...
• MECHANISM OF THE APPEARANCE OF A LARGE-SCALE VORTEX IN THE TROPOSPHERE ABOVE A NONUNIFORMLY HEATED SURFACE 

  Belotserkovskii O.M.; Oparin A.M.; Mingalev I.V.; Mingalev V.S.; Mingalev O.V. (2006)

  This paper is dedicated to a numerical modeling study of the formation mechanisms of a large-scale vortex over a warm water band on the ocean surface. For this purpose, we developed a 3D model of the atmospheric circulation ...
• EVALUATION OF STANDARD GIBBS POTENTIALS FOR COPPER HYDROXOSULFATE HYDRATES FROM SOLUTIONS OF DUAL LINEAR PROGRAMMING PROBLEMS 

  Yeriomin O.V.; Vinnichenko S.V.; Yurgenson G.A. (2006)

  The study of an oxidation zone at the Udokan deposit has shown that alteration of copper sulfides (chalcopyrite, bornite, and chalcocite) under cryogenic conditions is accompanied by the formation of hydrated complex ...
• ISOTOPE AGE OF SUBVOLCANIC GRANITOID ROCKS OF THE EARLY PROTEROZOIC PANARECHKA VOLCANOTECTONIC STRUCTURE, KOLA PENINSULA 

  Skuf'in P.K.; Bayanova T.B.; Mitrofanov F.P. (2006)

  The Panarechka volcanotectonic calderalike structure (PVTS) was found in the Early Proterozoic Pechenga–Varzuga Rift Belt (fault-lineament) of the Kola region. This is an oval body (21 × 8 km in size) that extends in a NW ...
• PLATINUM- AND GOLD-BEARING RODINGITES OF THE UST'-DEP OPHIOLITE BLOCK (MIDDLE AMUR REGION) 

  Molchanov V.P.; Plyusnina L.P.; Khanchuk A.I.; Zimin S.S.; Oktyabr'skii R.A. (2006)

  The Ust’-Dep ophiolite block, a part of the Selemdzha–Zeya Belt, occupies an area of 350 km2 and incorporates apoharzburgite serpentinite massifs intruded by numerous (>60) dikes of diabases and granitoids up to 100 m thick ...

View more