Miocene and Oligocene Petroleum Reservoirs of the Santa Maria and Santa Barbara-Ventura Basins, California

This volume presents papers that have been assembled for a Core Workshop on Miocene and Oligocene Petroleum Reservoirs of the Santa Maria and Santa Barbara - Ventura Basins, California. The main emphasis of the workshop in the Miocene Monterey Formation, the most important petroleum reservoir in both the Sana Maria Basins and a very important reservoir in the Santa Barbara - Ventura Basin, particularly in the offshore. In addition to the Monterey Formation, core studies are also presented on the post-Monterey Sisquoc Formation and on pre-Monterey reservoirs including the Sespe, Alegria, and Vaqueros Formations.
Lithostratigraphy and Depositional Environments of the Vaqueros and Upper Sespe/Alegria Formations, Hondo Field, Santa Barbara Channel, California Available to Purchase
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Published:January 01, 1990
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CiteCitation
Gregory A. Miles, Catherine A. Rigsby, 1990. "Lithostratigraphy and Depositional Environments of the Vaqueros and Upper Sespe/Alegria Formations, Hondo Field, Santa Barbara Channel, California", Miocene and Oligocene Petroleum Reservoirs of the Santa Maria and Santa Barbara-Ventura Basins, California, Margaret A. Keller, Mary K. McGowen
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Abstract
The Vaqueros, Sespe, and Alegria Formations are important oil and gas reservoirs in the area of the Santa Barbara Channel. At Hondo field, which is located about 40 km west of Santa Barbara and 9 km offshore, ten exploratory wells and five development wells have been drilled into these formations. The interpretation of data obtained from these wells, including a cored section from the OCS 190-2 well, suggests that Sespe and Alegria strata in the Hondo area were deposited in a deltaic environment during the Oligocene Epoch and that Vaqueros strata formed in an inner shelf setting during a late Oligocene and early Miocene transgression. Vaqueros deposition ended abruptly when rapid subsidence and deepening related to incipient basin formation terminated shallow marine sedimentation in the area. Gradation of the Vaqueros Formation into deep-water deposits of the overlying Rincon Formation, as interpreted from well logs, occurs vertically over just a few meters.