Testing Models of the Oceanside Blind Thrust through High-Resolution Mapping and Age Control on Marine Terrace Deformation, Coastal Southern California

Erik Haaker and Dr. Tom Rockwell’s poster presentation for the Rocky Mountain (66th Annual) and Cordilleran (110th Annual) Joint Meeting, Bozeman Montana

Rocky Mountain (66th Annual) and Cordilleran (110th Annual) Joint Meeting (19–21 May 2014) Paper No. 6-7
Presentation Time: 8:00 AM-5:00 PM

TESTING MODELS OF THE OCEANSIDE BLIND THRUST THROUGH HIGH-RESOLUTION MAPPING AND AGE CONTROL ON MARINE TERRACE DEFORMATION, COASTAL SOUTHERN CALIFORNIA

HAAKER, Erik C.¹, KENNEDY, George L.², ROCKWELL, Thomas K.³, GRANT LUDWIG, Lisa⁴, ZUMBRO, Justin⁵, and FREEMAN, S. Thomas⁵,
(1) Earth Consultants International, Inc, 1642 E 4th St, Santa Ana, CA 92701, echaaker@gmail.com
(2) Brian F. Smith and Associates, Inc, 14010 Poway Rd, Poway, CA 9206
(3) Geological Sciences, San Diego State University, 5500 Campanile Dr, San Diego, CA 92182
(4) Program in Public Health, University of California, Irvine, Irvine, CA 92697
(5) GeoPentech, Inc, 525 Cabrillo Park Dr, Santa Ana, CA 92701

Marine terraces and their respective shorelines provide information on vertical tectonic motions, thereby yielding constraints on rates and styles of deformation for underlying structures, such as blind thrust faults. In coastal southern California, the Oceanside Blind Thrust (OBT) has been inferred from offshore seismic reflection data, and its intersection with the coast has been inferred to be the source of uplift of the San Joaquin Hills (SJH). The OBT is believed to be the result of a tectonically inverted Miocene detachment fault, and has been hypothesized as a late Quaternary seismic source underlying coastal San Diego and southern Orange counties. Late Quaternary motion on the OBT should deform and uplift Quaternary marine terraces. To test OBT seismic source models, we collected high-resolution GPS elevation data for the flight of Pleistocene marine terraces spanning the southern California coastal zone from northern San Diego County through the city of Newport Beach in Orange County. We mapped the terraces by geomorphically tracing out and correlating individual shoreline exposures. In addition, we compiled subsurface geotechnical borehole data that supplement our survey data where urban development has obscured or obliterated the original geomorphic relationships. From these new data, the shorelines for terraces below 140 m elevation remain at nearly constant elevation from San Diego northward through Camp Pendleton. The lowest two terraces that date to MIS 5.1 and 5.5 show minor variation in San Clemente, and then gently decrease a few meters in elevation towards the north in the vicinity of Newport Bay. These observations do not appear to support late Quaternary activity of the OBT, and raise questions about how to reconcile recent seismicity in the SJH with published models of an underlying blind thrust.

Session No. 6–Booth# 23 Sedimentary Geology, Paleoclimatology, and Paleontology (Posters) Monday, 19 May 2014: 8:00 AM-5:00 PM Montana State University Ballroom B, C, D Geological Society of America Abstracts with Programs. Vol. 46, No. 5, p.12