Late Quaternary subsidence of Santa Catalina Island, California Continental Borderland, demonstrated by seismic-reflection data and fossil assemblages from submerged marine terraces

Author:

Castillo Chris M.1,Klemperer Simon L.1,Ingle James C.1,Powell Charles L.2,Legg Mark R.3,Francis Robert D.4

Affiliation:

1. Department of Geophysics, Stanford University, Mitchell Building, 397 Panama Mall, Stanford, California 94305, USA

2. U.S. Geological Survey, Western Region Geology and Geophysics Science Center, 345 Middlefield Road, Menlo Park, California 94025, USA

3. Legg Geophysical, 16541 Gothard Street, #107, Huntington Beach, California 92647, USA

4. Department of Geological Sciences, California State University–Long Beach, 1250 Bellflower Boulevard, Long Beach, California 90840, USA

Publisher

Geological Society of America

Subject

Geology

Reference107 articles.

1. Isostatic rebound, active faulting, and potential geomorphic effects in the Lake Lahontan basin, Nevada and California;Adams,1999

2. Sediment accumulation in a modern epicontinental-shelf setting: The Yellow Sea;Alexander;Marine Geology,1991

3. Benthic foraminiferal biofacies across a high energy continental shelf, San Onofre, California [M.S. thesis];Argow,1999

4. Implications of plate tectonics for the Cenozoic tectonic evolution of western North America;Atwater;Geological Society of America Bulletin,1970

5. Dominant paralic foraminifera of southern California and the Gulf of California;Bandy;Contributions from the Cushman Foundation for Foraminiferal Research,1963

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