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The AAPG/Datapages Combined Publications Database
AAPG Special Volumes
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The Parana basin in South America is a large Ordovician-to-Cretaceous intracratonic basin filled by five major depositional sequences, predominantly siliciclastic in nature. Tectonism was generally mild, consisting of Precambrian fault zones that experienced horizontal and vertical reactivation. The presence of the largest basaltic lava flows on continenal crust and the thousands of associated intrusive diabase bodies are evidence of an unusual thermal history that resulted in the generation of hydrocarbons and the deformation of strata. Although numerous shows of oil and gas are present, commercial production of hydrocarbons has never been achieved.
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