Reservoir Characterization of a Fan-Shaped Turbidite Complex in an Active-Margin Basin, Miocene Stevens Sandstone, Yowlumne Field, San Joaquin Basin, California
Michael S. Clark, Rick K. Prather, John D. Melvin
Abstract
Michael S. Clark, Rick K. Prather, John D. Melvin
Abstract
Yowlumne is a giant oil field, in the San Joaquin basin of Califomia, that has produced over 16.7 million m³ (105 million bbl) of oil from Upper Miocene, deep-water sandstones known as the "Stevens" (Figure 1). These sandstones, which represent clastic facies of organic-rich shales in the Monterey Formation (Figure 2), are some of the most prolific reservoirs in the basin and have contributed about 15% of over 1.9 billion m³ (12 billion bbl) of oil produced here since 1864. An integrated reservoir analysis enabled cost-effective exploitation of the distal margin of a layered, low-permeability, fan-shaped turbidite complex contained within the Yowlumne Stevens.
A significance statement is not available in the OpenAlex record.
A contribution statement is not available in the OpenAlex record.
Method details are not available in the OpenAlex metadata.
Findings are not separately available in the OpenAlex metadata.
Limitations are not available in the OpenAlex metadata.
Application details are not available in the OpenAlex metadata.
Yowlumne is a giant oil field, in the San Joaquin basin of Califomia, that has produced over 16.7 million m³ (105 million bbl) of oil from Upper Miocene, deep-water sandstones known as the "Stevens" (Figure 1). These sandstones, which represent clastic facies of organic-rich shales in the Monterey Formation (Figure 2), are some of the most prolific reservoirs in the basin and have contributed about 15% of over 1.9 billion m³ (12 billion bbl) of oil produced here since 1864. An integrated reservoir analysis enabled cost-effective exploitation of the distal margin of a layered, low-permeability, fan-shaped turbidite complex contained within the Yowlumne Stevens.
Key concepts: Turbidite, Geology, San Joaquin, Structural basin, Facies, Clastic rock, Paleontology, Passive margin