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The AAPG/Datapages Combined Publications Database

AAPG Special Volumes

Abstract


Pub. Id: A134 (1990)

First Page: 681

Last Page: 708

Book Title: M 51: Interior Cratonic Basins

Article/Chapter: The Parana Basin, Brazil: Chapter 33: Part II. Selected Analog Interior Cratonic Basins: Analog Basins

Subject Group: Basin or Areal Analysis or Evaluation

Spec. Pub. Type: Memoir

Pub. Year: 1990

Author(s): Pedro Victor Zalan, Sven Wolff, Marco Antonio M. Astolfi, Ines Santos Vieira, Joao Claudio J. Concelcao, Valeria T. Appi, Eugenio V. S. Neto, Jose R. Cerqueira, Airton Marques

Abstract:

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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