Stratigraphy of El Chanate Group (Late Cretaceous) and its implications for the tectonic evolution of northwestern Sonora, Mexico
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Keywords

stratigraphy, tectonics, El Chanate Group, Late Cretaceous, Sonora, Mexico

How to Cite

Jacques-Áyala, C. (2018). Stratigraphy of El Chanate Group (Late Cretaceous) and its implications for the tectonic evolution of northwestern Sonora, Mexico. Revista Mexicana De Ciencias Geológicas, 16(2), 97–120. Retrieved from https://rmcg.geociencias.unam.mx/index.php/rmcg/article/view/1056

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Abstract

The Late Cretaceous El Chanate Group is a clastic and volcanic sequence, ranging from 700 to more tan 2,800 m in thickness, deposited in a continental basin. It disconformably overlies the Lower Cretaceous Bisbee Group and underlies the Late Cretaceous (71 Ma) Tarahumara Formation. On the basin of major upward-fining eyeles and different conglomerate composition, three stratigraphic units were identified in the Sierra El Chanate: the Pozo Duro (oldest), Anita, and Escalante (youngest) formations. El Chanate Group and its three formations are proposed herein as formal stratigraphic units… download the full paper in PDF.

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