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Title: Late Neogene-Quaternary left slip on N-striking faults, SE Nevada-SW Utah area: An event distinct from Miocene WSW-directed major extension

Conference · · Geological Society of America, Abstracts with Programs; (United States)
OSTI ID:5437408
 [1]
  1. CICESE, San Diego, CA (United States)

Much strike-slip faulting, on [approximately]NW-striking dextral and [approximately]NE-striking sinistral faults, was synchronous with large-magnitude extension in the Great Basin (e.g., Wernicke and others 1988, GSA Bulletin). However, in the SE Nevada area major Miocene extension ([approximately]100 km WSW extension) was followed by sinistral slip on several [approximately]N-striking faults. These faults have moderate to steep dips, cut all structures that intersect them, control range-scale topography, are typically >10 km long, and some cut Pliocene-Quaternary deposits. These data conflict with the idea that the N-striking sinistral faults were coeval with Miocene-Recent normal faulting that produced only minor extension in the SE Nevada area ([approximately]10%; Anderson and Barnhard, ref. above). However, they are consistent with seismic (Bohannon and others in press, GSA Bulletin) and numerous geologic studies documenting large-magnitude Miocene extension, and also suggest a Pliocene-Recent episode of sinistral slip on N-trending faults coeval with slowed Pliocene-Recent extension.

OSTI ID:
5437408
Report Number(s):
CONF-9305259-; CODEN: GAAPBC
Journal Information:
Geological Society of America, Abstracts with Programs; (United States), Vol. 25:5; Conference: 89. annual meeting of the Cordilleran Section and the 46th annual meeting of the Rocky Mountain Section of the Geological Society of America (GSA), Reno, NV (United States), 19-21 May 1993; ISSN 0016-7592
Country of Publication:
United States
Language:
English

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