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Hydrothermal influence of heavy oil in the presence of minerals of carbonate rock was carried out modeling hydrothermal effects involving mineral compounds of carbonate rocks. Depending
Conversion of heavy crude oil with carbonate rock in the medium of water superheated steam carried out by modeling hydrothermal effects involving mineral compounds of carbonate rocks. Depending
Mixed-Layer clay minerals as indicator of diagenesis processes in oil bearing rocs. The welldeveloped method for studying mixed layer phases is fitting, in which the parameters of theoretical basal
Influence of Hydrothermal and Pyrolysis Processes on the Transformation of Organic Matter of Dense Low-Permeability Rocks from Domanic Formations of the Romashkino Oil FieldThe model experiments regarding the conversion of organic matters from carbonate rock samples
Физико-химические параметры формирования ультрамафитов из офиолитов Кузнецкого АлатауPhysical and chemical parameters of formation of ultramafic rocks from Kuznetsky Alatau ophiolites
Reservoir rocks of viscous oil in Ufa terrigenous complex (example of the ivanovo deposit) properties. The authors used methods of mathematical statistics and made maps of reservoir parameters
Research of array geodynamics in the interface of cleaning and preparatory works efficiency. At the site of conjugation of workings, deformations in rocks serve as a source of local
Geoenvironmental parameters of the tourist ecological route (On the example of the karadag natural reserve) along the ecological route. Along it the main rocks, relief, vegetation, projective covering and its
Prospects of the method of stepwise crushing as a source of information on the fluid phase of rocks and minerals is exemplified here by the results of the investigation of mantle rocks and minerals from various geologic
PALEOGEODYNAMICS OF MAGMATIC AND METAMORPHIC PROCESSES OF FORMATION OF ULTRAMAFIC ROCKS OF CHAGAN-UZUN MASSIF (OPHIOLITES OF GORNY ALTAI) metamorphic parameters of transformation of harzburgites (5.1-1.9 kbar, 820-700 °С) and clinopyroxenites (2
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