Geosynclinal process on an example of hercynian geosyncline of Donbas
© V.V. Gordienko, O.V. Usenko, 2000
The main geological events of Hercynian history of the Donbas geosyncline: changes of the velocity of sediment accumulation, composition and depths of magma sources, geothermal gradient at inversion period have been analyzed. They were compared to those suggested by an advection - polymorphous hypothesis. <<back |
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