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|Title:||Active parasitic folds on the Elysian Park anticline : implications for seismic hazard in central Los Angeles, California||Authors:||Oskin, Michael
Rockwell, Thomas K.
|Keywords:||DRNTU::Science::Geology::Volcanoes and earthquakes||Issue Date:||2000||Source:||Oskin, M., Sieh, K., Rockwell, T., Miller, G., Guptill, P., Curtis, M., et al. (2000). Active parasitic folds on the Elysian Park anticline: Implications for seismic hazard in central Los Angeles, California. Geological Society of America Bulletin, 112(5), 693-707.||Series/Report no.:||Geological society of America bulletin||Abstract:||We characterize the seismic hazard of the Elysian Park fault, a blind reverse fault beneath central Los Angeles, by analysis of the Elysian Park anticline, which overlies it. New shallow-subsurface geotechnical data, combined with other surficial stratigraphy and geomorphology, reveal that the Elysian Park anticline is an active 20-km-long structure. From the style and rates of deformation of parasitic folds on the southern limb of the anticline, we estimate a contraction rate of 0.6–1.1 mm/yr. This rate provides a basis for estimating a rate of contraction of the entire Elysian Park anticline, which in turn allows us to estimate a 0.8–2.2 mm/yr time-averaged rate of slip on the underlying fault. At this rate of slip, rupture of the Elysian Park fault could produce a nominal Mw 6.2 to 6.7 earthquake every 500 to 1300 yr, on average. Although this Elysian Park earthquake would recur infrequently, its size and recurrence interval may be similar to those estimated for the sources of the destructive 1971 San Fernando and 1994 Northridge earthquakes.||URI:||https://hdl.handle.net/10356/95286
|ISSN:||0016-7606||DOI:||10.1130/0016-7606(2000)112<693:APFOTE>2.0.CO;2||Rights:||© 2000 Geological Society of America.||Fulltext Permission:||none||Fulltext Availability:||No Fulltext|
|Appears in Collections:||EOS Journal Articles|
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