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- W1558715525 abstract "The Simmler Formation (Oligocene (?)-lower Miocene) of the southern Cuyama Valley area in Santa Barbara and Ventura counties, California, is a nonmarine sequence overlying pre-Oligocene sedimentary and igneous rocks, and underlying the Vaqueros Formation. The Simmler is exposed in a narrow, folded strip along the northern side of the Ozena fault. The eight members, herein informally designated A through H, represent three distinct phases of deposition. Time I, represented by members A and B and parts of members C, D and F, was a time of fluvial in-filling of the area. Northwestward prograding alluvial-fan/wadi-stream/sabkha deposits, derived from a granitic/metamorphic source terrane southeast of the basin, dominated, while less important, northward-prograding, low-sinuosity meandering streams were derived from a sedimentary source terrane south of the basin. Time II, represented by member E, and parts of C, D and F, was also a time of fluvial in-filling, but during this period, northward prograding streams from a sedimentary source area south of the Ozena fault dominated over those from the granitic/metamorphic terrane to the southeast. Rocks of time III, represented by members G and H, indicate that a perennial river, presumably flowing through the Cuyama Badlands area, swept around the west end of the Blue Rock uplift to deposit a river-dominated delta in which subaqueous delta channels of member G interfingered with interdistributary bay deposits of member H." @default.
- W1558715525 created "2016-06-24" @default.
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- W1558715525 date "1982-01-01" @default.
- W1558715525 modified "2023-09-27" @default.
- W1558715525 title "Depositional Environments of the Simmler Formation in Southern Cuyama Valley, Santa Barbara and Ventura Counties, California" @default.
- W1558715525 hasPublicationYear "1982" @default.
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