Estimates of large magnitude Late Cambrian earthquakes from seismogenic soft-sediment deformation structures: Central Rocky Mountains
Author:
Affiliation:
1. Department of Geology; Colorado College; Colorado Springs Colorado 80903 USA
2. Key Laboratory of Economic Stratigraphy and Palaeogeography; Nanjing Institute of Geology and Palaeontology; Chinese Academy of Sciences; Nanjing 210008 China
Funder
National Science Foundation
National Natural Science Foundation of China
Publisher
Wiley
Subject
Stratigraphy,Geology
Link
http://onlinelibrary.wiley.com/wol1/doi/10.1111/sed.12154/fullpdf
Reference87 articles.
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2. Earthquake magnitude-frequency, epicentral distance, and soft-sediment deformation in sedimentary basins;Allen;Sed. Geol.,1986
3. Timing, style, and significance of Cambrian through Laramide brittle reactivation along the Proterozoic Homestake shear zone, Colorado mineral belt;Allen;Rocky Mt. Geol.,2004
4. A multi-kilometer pseudotachylyte system as an exhumed record of earthquake rupture geometry at hypocentral depths (Colorado, USA);Allen;Tectonophysics,2005
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