Skip to main content
U.S. Department of Energy
Office of Scientific and Technical Information

Depositional environments of the Topanga Canyon Formation, central Santa Monica Mountains, southern California

Conference · · AAPG Bulletin (American Association of Petroleum Geologists); (United States)
OSTI ID:5171370
 [1];  [2]
  1. Emcon Associates, Camarillo, CA (United States)
  2. California State Univ., Northridge (United States)
The Topanga Canyon Formation within the central Santa Monica Mountains of southern California is a sequence of lower through middle Miocene conglomerate, sandstone, and siltstone deposits that record a lower, wave-dominated, marine, retrogradation cycle; a middle, river-dominated, marine and fluvial, progradational cycle; and an upper, river-dominated, marine, retrogradational cycle. The lower retrogradation consists of black siltstone (Encinal Member) below-wave-base shelf deposits west of Malibu Canyon, where circulation was restricted, and fossiliferous sandstone (Saddle Peak Member) shoreface deposits east of Malibu Canyon, where wave energy was moderate to high. The middle progradation is marked by an onset of river-dominated deltaic sedimentation. Nonmarine sandstone and conglomerate (Fernwood Member) upper delta-plain (channel, point-bar, crevasse-splay, marsh, and floodplain) deposits east of Malibu Canyon prograde southwestward into marine sandstone and siltstone (undifferentiated Topanga Canyon Formation) delta-front, interdistributary bay, and prodelta deposits. Both meandering and braided channels existed on the upper delta plain. Channel avulsion and lobe abandonment, followed by subsidence and a return to wave dominance, caused wave-dominated shoreface and river-dominated delta-front deposits to interfinger locally. The upper retrogradation consists of marine sandstone and siltstone (Cold Creek Member) distributary-mouth-bar, delta-front, and prodelta deposits that overlie the earlier fluvial deposits east of Malibu Canyon. Rocks of this age do not occur west of Malibu Canyon.
OSTI ID:
5171370
Report Number(s):
CONF-9103128--
Conference Information:
Journal Name: AAPG Bulletin (American Association of Petroleum Geologists); (United States) Journal Volume: 75:2
Country of Publication:
United States
Language:
English

Similar Records

Eocene marine to nonmarine (deltaic) deposits, Lower Piru Creek, Los Angeles and Ventura Counties, California
Conference · Mon Mar 31 23:00:00 EST 1986 · Am. Assoc. Pet. Geol., Bull.; (United States) · OSTI ID:6931072

Variability of deltaic sedimentation during clastic influx into a carbonate-dominated craton
Conference · Mon Dec 31 23:00:00 EST 1984 · Geol. Soc. Am., Abstr. Programs; (United States) · OSTI ID:6458481

Facies relationships in Mesa Rica Sandstone (Lower Cretaceous), Tucumcari Basin, east-central New Mexico
Conference · Fri Feb 28 23:00:00 EST 1986 · Am. Assoc. Pet. Geol., Bull.; (United States) · OSTI ID:7176040