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Journal ArticleDOI

Early Permian thrust faults in east-central California

TLDR
One exposed and another inferred thrust fault in the southeastern Inyo Mountains of east-central California are interpreted as Early Permian in age as mentioned in this paper, which is temporally and geographically related to a major episode of basin formation which occurred along a southeast-trending segment of the permian North American plate margin.
Abstract
One exposed and another inferred thrust fault in the southeastern Inyo Mountains of east-central California are interpreted as Early Permian in age. These faults, both apparently of local extent, are temporally and geographically related to a major episode of basin formation which occurred along a southeast-trending segment of the Permian North American plate margin. The close relationship between basin formation and thrust faulting supports a previous interpretation by us that this segment of the margin was undergoing active wrench tectonism during the Early Permian, resulting in the essentially simultaneous development of local extensional and compressional structures similar to those now forming in the California continental borderland.

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Book ChapterDOI

Early Mesozoic tectonic evolution of the western U.S. Cordillera

TL;DR: The early Mesozoic evolution of the U. S. Cordillera differs greatly from its previous history of mainly miogeoclinal sedimentation with outboard marginal-basin-island-arc mobile zones as mentioned in this paper.
Journal ArticleDOI

Paleozoic and Mesozoic Evolution of East-Central California

TL;DR: In this article, it was shown that sedimentation did not keep pace with subsidence, resulting in backstepping of a series of successive carbonate platforms throughout the early and middle Paleozoic.
Journal ArticleDOI

Triassic plutonism in southern California: Southward younging of arc initiation along a truncated continental margin

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Journal ArticleDOI

Structure and evolution of the East Sierran thrust system, east central California

TL;DR: Dunne et al. as discussed by the authors investigated the evolution of the East Sierran thrust system (ESTS), a belt of arc-parallel, northeast vergent contractional deformation, along the east side of the sierran continental margin arc.
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