Jurassic history of the central Sierra Nevada and the "Nevadan' orogeny

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Abstract

Recent mapping, combined with published age determinations indicate: the Jurassic arc was, at least in part, formed at the western edge of North America; the "Nevadan' orogeny was a protracted event that lasted at least 20 million years, with volcanism, plutonism, sedimentation and deformation occurring simultaneously, and; displacement along the Melones Fault Zone occurred late in the history of the area and resulted from oblique convergence between North America and oceanic crust to the west. -from Author

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Albino, G. V. (1992). Jurassic history of the central Sierra Nevada and the “Nevadan’’ orogeny.” Basement Tectonics 7. Proc. International Conference, Kingston, Ontario, 1987, 289–303. https://doi.org/10.1007/978-94-017-0833-3_20

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