Evidence for aseismic deformation in the western transverse ranges, southern California

Implications for seismic risk assessment

Ernest M Duebendorfer, Jan Vermilye, Peter A. Geiser, Thomas L. Davis

Research output: Contribution to journalArticle

15 Citations (Scopus)

Abstract

Recent studies in southern California suggest that long-term deformation rates are far in excess of that which can be accounted for by historical seismicity, and thus, a deficit of moderate and/or large earthquakes exists in southern California. Although possible, this conclusion is not unique because aseismic deformation may have contributed to bulk regional strain. We examined Cretaceous to Pleistocene sedimentary rocks exposed in the Ventura basin along four cross-strike traverses to evaluate the possibility that aseismic deformation contributed to regional shortening. Our field and microstructural investigations suggest that aseismic deformational mechanisms, particularly pressure solution, contributed significantly to permanent shortening strain during the late Neogene and that the proposed seismic deficiency may be overestimated.

Original languageEnglish (US)
Pages (from-to)271-274
Number of pages4
JournalGeology
Volume26
Issue number3
DOIs
StatePublished - Mar 1998

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risk assessment
pressure solution
Neogene
seismicity
sedimentary rock
Pleistocene
Cretaceous
earthquake
basin
rate

ASJC Scopus subject areas

  • Geology

Cite this

Evidence for aseismic deformation in the western transverse ranges, southern California : Implications for seismic risk assessment. / Duebendorfer, Ernest M; Vermilye, Jan; Geiser, Peter A.; Davis, Thomas L.

In: Geology, Vol. 26, No. 3, 03.1998, p. 271-274.

Research output: Contribution to journalArticle

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