1887

Abstract

The lower, most subsided parts of sedimentary basins (Rifean-Vendian series), located on ancient platforms, are characterized by riftogenic origin. Within these Rifean rifts two factors are combined, playing the important role in oil-gas formation: accumulation of many kilometers thick sediments, and their intensive healing due to the increased heat flow.

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/content/papers/10.3997/2214-4609.201410240
1994-06-10
2020-04-03
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201410240
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