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• W112587570 abstract "The Merced Formation consists of approximately 2,000 m of shallow marine and coastal nonmarine sediment of late Cenozoic age that accumulated in a structural trough south of the city of San Francisco. About 1,750 m of these deposits crop out in a well exposed tilted sequence in sea cliffs on the north side of the San Andreas fault. The part of the section north of the fault appears to be of Pleistocene age. Depositional facies within the Merced Formation can be identified with a high degree of confidence based on biota, sedimentary structures, and textural character. In vertical succession, the facies define alternating episodes of transgression and regression. The individual transgressive/regressive cycles almost certainly reflect the eustatic sea-level fluctuations that occurred during Pleistocene time. The general pattern of transgression and regression can be fairly well matched in much of the section to a Pleistocene sea-level curve determined from oxygen-isotope data. If eustatic fluctuations can be subtracted from the stratigraphic record, tectonic and sedimentologic influences become evident. The accumulation of such a thick succession of shallow-marine and coastal deposits implies long-term subsidence at an average rate of 1 m/103 yr. Evidence suggests that the rate of subsidence may have been greater in the section deposited prior to emplacement of the Rockland ash (at 0.4 Ma) than in the section deposited subsequent to the ash. A pronounced shift to predominantly nonmarine deposits about 290 m below the top of the section may be due in part to diminished subsidence rates. However, the fact that this change coincides with a change in provenance from local Franciscan sources to the Sacramento-San Joaquin River systems indicates that the shift to nonmarine facies more likely resulted from increased rates of sedimentation." @default.
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• W112587570 date "1988-01-01" @default.
• W112587570 modified "2023-09-27" @default.
• W112587570 title "Analysis of Eustatic, Tectonic, and Sedimentologic Influences on Transgressive and Regressive Cycles in the Upper Cenozoic Merced Formation, San Francisco, California" @default.
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• W112587570 doi "https://doi.org/10.1007/978-1-4612-3788-4_6" @default.
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