Geological Society of America Special Paper 338 1999 Since Bramlette (1946): The Miocene Monterey Formation of California revisited Richard J. Behl Department of Geological Sciences, California State University, Long Beach, California 90840-3902; e-mail:
[email protected]. INTRODUCTION eries in the Monterey Formation following the first sale of Fed- eral Outer Continental Shelf leases in the Santa Barbara Chan- For more than a century the Miocene Monterey Formation nel in 1966. A tremendous amount of this work was published has fascinated geologists with its uniquely siliceous composi- in a series of American Association of Petroleum Geologists tion, complex diagenesis, and importance as both source and (AAPG) and Society of Economic Paleontologists and Mineral- reservoir of oil in California. The Monterey’s extensive and ogists (SEPM; now the Society for Sedimentary Geology) spe- excellent outcrops, exposed at different stages of alteration, cial publications and symposium volumes in the 1980s and have served as laboratories for countless studies of silica, clay, 1990s (Isaacs, 1981a; Garrison and Douglas, 1981; Williams carbonate, phosphate, organic matter, and petroleum. Bram- and Graham, 1982; Isaacs and Garrison, 1983; Garrison et al., lette’s U.S. Geological Survey Professional Paper 212 (1946) 1984; Surdam, 1984; Casey and Barron, 1986; Dunham and served as the foundation for all of these studies and provided Blake, 1987; Schwalbach and Bohacs, 1992; Hornafius, 1994a; the detailed sedimentology, stratigraphy, and petrology to give Eichhubl, 1998) that coincided with the upturn in industry inter- them context and meaning. For the most part, Bramlette had it est in the petroleum potential of the offshore Monterey (Isaacs, right, and an explosion of new research since the 1970s 1984; Crain et al., 1985).