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Crustal-Scale Cross-Section of the U.S. Cordillera, California and Beyond, Its Tectonic Significance, and Speculations on the Andean Orogeny
2002
International Geology Review
A cross-section across northern California from the San Andreas fault to central Nevada exhibits both major east-and west-vergent structures. East-vergent structures include crustal wedging and fault-propagation folds in the Coast Ranges, emplacement of the Great Valley ophiolitic basement over Sierran basement rocks, early east-vergent structures in the latter, displacement along the eastern margin of the Sierra Nevada batholith, and thrust faults in western Nevada. West-vergent structures
doi:10.2747/0020-6814.44.6.479
fatcat:dz6npl3wrjgcrgy7b7xuoapkfq