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The AAPG/Datapages Combined Publications Database
Pacific Section of AAPG
Abstract
Offshore Structure Between Santa Cruz and Santa Rosa Islands
Abstract
The offshore extension of the Santa Cruz Island, fault has been traced westward 8 km (kilometres). It has a maximum observed vertical separation of the Miocene section of 200 m (metres), decreasing westward to 15 m. The eastward offshore extension of the Santa Rosa Island fault appears to join the offshore Santa Cruz Island fault near the west shoreline of Santa Cruz Island. The vertical separation of the Miocene section is 700 m along its western part decreasing to 100-200 m toward the east. Between the two faults a small pull-apart basin, the Carrington basin (new name), has resulted from left-lateral movements on the two faults.
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