Range-front fault scarps of the Sierra El Mayor, Baja California: Formed above an active low-angle normal fault?

Gary J. Axen, John M. Fletcher, Eric Cowgill, Michael Murphy, Paul Kapp, Ian MacMillan, Ernesto Ramos-Velázquez, Jorge Aranda-Gómez

Research output: Contribution to journalArticle

55 Scopus citations

Abstract

The Canada David detachment, a west-dipping low-angle normal fault, juxtaposes Pliocene and Pleistocene(?) sedimentary units over sheared bedrock in the Sierra El Mayor, Baja California. Along the west-central range front, the detachment is overlapped by Quaternary alluvial fans that are, in turn, cut by fault scarps up to 7 m high. Map relationships suggest that scarp-forming faults may sole into the detachment at very shallow depth (<200-300 m). Palinspastic restoration of a topographic profile across 15 north-striking scarps suggests that the ratio of net heave to net throw along scarp-forming faults is ~2, consistent with them soling into a low-angle (~30°) fault. These 15 scarps may have all formed in one earthquake, with rupture propagation from depth to the near-surface aided by clay gouge along the detachment. The detachment is abandoned in the footwall east of the scarps.

Original languageEnglish (US)
Pages (from-to)247-250
Number of pages4
JournalGeology
Volume27
Issue number3
DOIs
StatePublished - Mar 1999
Externally publishedYes

ASJC Scopus subject areas

  • Geology

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    Axen, G. J., Fletcher, J. M., Cowgill, E., Murphy, M., Kapp, P., MacMillan, I., Ramos-Velázquez, E., & Aranda-Gómez, J. (1999). Range-front fault scarps of the Sierra El Mayor, Baja California: Formed above an active low-angle normal fault? Geology, 27(3), 247-250. https://doi.org/10.1130/0091-7613(1999)027<0247:RFFSOT>2.3.CO;2