Houston Geological Society Bulletin

Abstract

Houston Geological Society Bulletin, Volume 13, No. 6, February 1971. Pages 3-3.

Abstract: Geology of the Ventura Basin, California as an Approach to Offshore Exploration

By

James M. Cole

Exploratory approaches used in the Ventura Basin can serve as a model for exploration of other offshore areas. In preparation for the 1968 Ventura Basin Federal offshore lease sale, a totally integrated exploration program was required, consisting of stratigraphic tests, modern geophysical surveys for purposes other than, but including structural mapping, paleontologic studies, onshore surface geologic mapping, and ocean-floor geologic mapping and sampling by divers and diving submersibles.

The Ventura Basin, two-thirds of which is offshore, is an east-west trending synclinal trough containing 40,000-50,000 feet of principally Tertiary marine clastic rocks. Structurally, it is characterized by major east-west thrust faults and tightly folded anticlinal trends. Although anticlinal accumulations provide the largest part of the Ventura Basin petroleum, significant reserves occur in a wide variety of traps, including stratigraphic, fault and unconformity. Pliocene turbidite sandstone is the principal reservoir in the eastern part of the basin, and has yielded approximately 1 billion bbls. of oil from onshore fields. Miocene, Oligocene, and Eocene marine to nonmarine clastic rocks are objectives to the west.

On February 6, 1969, industry bid what was at the time a record high $1.3 billion and spent$603 million for 383,341 acres; 50 percent of the acreage was in water deeper than 600 feet. Currently, deepwater drilling and producing technology is advancing rapidly as evaluation is underway.

Two separate areas in which Humble bought acreage and subsequently drilled wildcats are discussed in detail. One area resulted in a major oil discovery and the other, where Humble paid \$45 million for the lease, is considered a failure. Actual maps and cross-sections that were used prior to the sale are compared with current maps that reflect changes resulting from drilling; in essence, a before and after series of geologic maps are presented along with the "methodology" what was used in the geologic interpretations.

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