Constraining Basin Geometry and Fault Kinematics on the Santo Tomás Segment of the Agua Blanca Fault Through a Combined Geophysical and Structural Study
The Agua Blanca fault is a major transverse structure of northern Baja California, extending more than 120km east from the Punta Banda ridge near the city of Ensenada to the San Matais Pass in central Baja. Through much of its eastern extent slip on this fault appears to be pure strike slip, however...
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Scholar Commons
2010
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Online Access: | https://scholarcommons.usf.edu/etd/1779 https://scholarcommons.usf.edu/cgi/viewcontent.cgi?article=2778&context=etd |