Strike-Slip Fault Terminations at Seismogenic Depths: The Structure and Kinematics of the Glacier Lakes Fault, Sierra Nevada United States
[1] Structural complexity is common at the terminations of earthquake surface ruptures; similar deformation may therefore be expected at the end zones of earthquake ruptures at depth. The 8.2 km long Glacier Lakes fault (GLF) in the Sierra Nevada is a left-lateral strike-slip fault with a maximum ob...
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Hosted by Utah State University Libraries
2008
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Online Access: | https://digitalcommons.usu.edu/geology_facpub/4 https://digitalcommons.usu.edu/cgi/viewcontent.cgi?article=1003&context=geology_facpub |