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PLANETARY MAGMOFLUIDODYNAMIC SYSTEM, DEGASSING, BASIN GENERATION AND NAPHTIDOGENESIS ON THE EARTH

The latest data on the deep structure, deep fluid dynamics, naphtidogenesis and degassing of tectonically active belts and areas of the Earth, in particular, sedimentary and petroleum basins (SB and PB) are presented. It is shown that SB and PB are global scale formations, developed as a result of the convective process in the Earth’s mantle and the planetary magma-fluid dynamics system, which stimulates the convective process. Convection covers the coromantium shell over its entire thickness, including the D’’ layer and partially the upper liquid layer of the Earth’s core. It provides magmatism in tectonically active belts and areas, including rift systems, SB and orogens, subduction and upwelling belts in the oceans. The ascending mantle magmatism under the rift systems, SB and orogens, as an element of the planetary magma-fluid dynamics system, ensures the transport of dissolved hydrogen, carbon and other gases into the upper layers of the mantle and the crust, followed by release into the gaseous phases and the participation of hydrogen and carbon in the methane and its radicals synthesis, first at depths below the sedimentary cover, and then, penetrating into the sedimentary cover, by hydrogenating organic matter hydrogen stimulates naphthidogenesis in much larger volumes in the sedimentary cover, where there are high concentrations of dispersed organic matter. It has been shown that rifting, basin generation and orogenesis is an evolutionary series of a single diving-destructive-constructive process of continental genesis involved in a global convection, ensuring the removal of thermal heat of the Earth, degassing and polygenic naphthidogenesis.