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- W1539793757 abstract "During the early Mesozoic, a continental margin magmatic arc developed along a convergent plate boundary at the western edge of North America in California and Nevada. New stratigraphic and structural data suggest that two segments of this arc, a northern segment including localities north of lat. 38 30' N., and a southern segment south of that latitude, may have been juxtaposed by large-magnitude strike-slip displacement along the MojaveSnow Lake fault. The two arc segments show major contrasts in their igneous and stratigraphic histories. Restoration of displacement on the Mojave-Snow Lake fault places the northern segment near Mineral King pendant in the southern Sierra Nevada and the western Mojave. Stratigraphic similarities between the northern arc segment and these latter areas are consistent with the reconstruction. Because of the probability that several cryptic faults may have disrupted and juxtaposed parts of the arc, the original paleogeography of the arc is highly uncertain. Nevertheless, the arc underwent several episodes of contractional and extensional deformation during Triassic and Jurassic time, and during the Early Jurassic may have been broadly extensional. Overlap relations in various segments of the arc tie together rocks of the Sonoma and Antler orogenic belts in central and western Nevada with the miogeocline by Late Triassic time. Reconstruction of the MojaveSnow Lake fault, together with other overlap relations, suggests that the Shoo Fly Complex was in close proximity to the El Paso terrane in the southern Sierra during the Triassic." @default.
- W1539793757 created "2016-06-24" @default.
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- W1539793757 date "1993-01-01" @default.
- W1539793757 modified "2023-09-23" @default.
- W1539793757 title "Triassic-Jurassic Magmatic Arc in Eastern California and Western Nevada: Arc Evolution, Cryptic Tectonic Breaks, and Significance of the Mojave-Snow Lake Fault" @default.
- W1539793757 hasPublicationYear "1993" @default.
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