Oceanside and thirtymile bank blind thrust: Implications for earthquake hazards in coastal Southern California

Geology

Volumn 28, Issue 10, 2000, Pages 891-894

  Rivero, C ^a   Shaw, J H ^a   Mueller, K ^a  

^a HARVARD UNIVERSITY   (United States)

Author keywords

Blind thrusts; Earthquakes; InnerCalifornia borderland; Oceanside; Strike slip faults; Tectonic reactivation

Indexed keywords

OFFSHORE OIL WELL PRODUCTION; STRIKE-SLIP FAULTS;

BLIND THRUSTS; EARTHQUAKE HAZARD; INNERCALIFORNIA BORDERLAND; INTERNATIONAL BORDER; METROPOLITAN AREA; OCEANSIDE; SOUTHERN CALIFORNIA; TECTONIC REACTIVATION;

EARTHQUAKES;

EARTHQUAKE; SEISMIC HAZARD; STRIKE-SLIP FAULT; TECTONICS; THRUST;

CALIFORNIA; UNITED STATES;

EID: 84874983809     PISSN: 00917613     EISSN: None     Source Type: Journal    
DOI: 10.1130/0091-7613(2000)028<0891:OATBBT>2.3.CO;2     Document Type: Article

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5. Across section of the Los Angeles area: Seismically active fold and thrust belt, the 1987 Whittier Narrows earthquake, and earthquake hazard
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19. Microplate capture, rotation of the Western Transverse Ranges, and initiation of the San Andreas transform as a low-angle fault system
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26. Miocene collapse of the California continental margin
27. The magnitude 6.7 Northridge, California, earthquake of 17 January 1994
28. New empirical relationships among the magnitude, rupture length, rupture width, rupture area, and surface displacement