『Abstract
Cycles of the geosynclinal-orogenic-platformal development of
the continental crust are separated by natural phases of crustal
destruction. They are determined by pulses of degassing of the
Earth's core marked by decelerated inversions of the magnetic
field. Such pulses occur under the influence of fluid flows that
ascend from the core and loss hydrogen. Consequently, the fluids
acquire acidic properties and become aggressive to rocks of the
continental crust (H2 + 2CO = H2O
+ 0.5CO2 + 1.5C). Oceanization of the continental
crust represents the main result of its destruction accompanied
by the formation of seas and sedimentary basins largely on the
underwater margins of continents. Development of geodynamic compression
setting of the Earth's crust due to its evolution creates conditions
that impede the loss of hydrogen from ascending fluid flows. Consequently,
they acquire the ability to generate hydrocarbons (4H2
+ CO =2H2O + CH4 + C)
and produce oil and gas pools. This setting is marked by intrusions
of alkaline rocks with characteristic water-hydrocarbon inclusions
in minerals and by the development of fold-thrust and reversed
fault dislocations in depressions. The dislocations controlled
not only the fluid-related leaching of rocks, but also the distribution
of oil and gas pools within both sedimentary basins and their
basement.』
(Introduction)
Abyssal generation of hydrocarbons and their upward migration
Generation of hydrocarbons in connection with magmatism, ore accumulation,
and formation of platform depressions
Formation of oil and gas pools
Conclusions
Acknowledgments
References