Thermal and Chronological Record of Syn- to Post-Laramide Burial and Exhumation, Sierra Madre Oriental, Mexico
Published:January 01, 2001
Gary G. Gray, Robert J. Pottorf, Donald A. Yurewicz, Keith I. Mahon, David R. Pevear, Richard J. Chuchla, 2001. "Thermal and Chronological Record of Syn- to Post-Laramide Burial and Exhumation, Sierra Madre Oriental, Mexico", The Western Gulf of Mexico Basin: Tectonics,Sedimentary Basins, and Petroleum Systems, Claudio Bartolini, Richard T. Buffler, Abelardo Cantú-Chapa
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Thermal and thermochronological data from the Sierra Madre Oriental indicate that a foreland basin formed on the leading edge of the fold belt during and after the late stages of the Laramide orogeny. This basin appears to have been at least 4 km thick by 50 Ma and to have reached maximum temperatures of 165° to 170°C under 5 to 7 km of burial. In areas such as the Parras and La Popa Basins, these burial amounts are in addition to the presently preserved Upper Cretaceous-Lower Tertiary section.
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The Western Gulf of Mexico Basin: Tectonics,Sedimentary Basins, and Petroleum Systems
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