Geologic investigations of a “slip gap” in the surficial ruptures of the 1992 Landers earthquake, southern California
A 3-km-long gap in the dextral surficial rupture of the 1992 M w = 7.3 Landers earthquake occurs at the north end of a major fault stepover between the Johnson Valley and Homestead Valley faults. This gap is situated along a segment of the Landers rupture that has been modeled geophysically as havin...
Main Authors: | , |
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Format: | Journal Article |
Language: | English |
Published: |
2012
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Subjects: | |
Online Access: | https://hdl.handle.net/10356/104271 http://hdl.handle.net/10220/8491 |