Spatiotemporal patterns of distributed slip in southern Owens Valley indicated by deformation of late Pleistocene shorelines, eastern California
Author:
Affiliation:
1. Desert Research Institute, 2215 Raggio Parkway, Reno, Nevada 89512, USA
2. U.S. Geological Survey, University of California White Mountain Research Station, Bishop, California 93514, USA
Abstract
Publisher
Geological Society of America
Subject
Geology
Link
https://pubs.geoscienceworld.org/gsa/gsabulletin/article-pdf/132/7-8/1681/5077130/1681.pdf
Reference158 articles.
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2. Isostatic rebound, active faulting, and potential geomorphic effects in the Lake Lahontan basin, Nevada and California;Adams,1999
3. Refining the southern extent of the 1872 Owens Valley earthquake rupture through paleoseismic investigations in the Haiwee Area, southeastern California;Amos;Bulletin of the Seismological Society of America,2013
4. Chronology of tectonic, geomorphic, and volcanic interactions and the tempo of fault slip near Little Lake, California;Amos,2013
5. Late Quaternary slip rates for faults of the central Walker Lane (Nevada, USA): Spatiotemporal strain release in a strike-slip fault system;Angster;Geosphere,2019
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2. Paleoseismic evolution of the central section of the Serteng Shan fault at the northern Ordos Block (North China) since the Late Pleistocene;International Geology Review;2023-02-20
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