The middle Pleistocene Merced-2 and -3 sequences from Ocean Beach, San Francisco

The Merced Formation comprises a 2-km-thick shallow marine and non-marine succession that was deposited in a small transtensional basin along the San Andreas Fault during the late Pliocene to middle Pleistocene. The sediments dip between 10° and 80° to the northeast, and are locally disrupted by sma...

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Veröffentlicht in:Sedimentary geology 2002-10, Vol.153 (1), p.23-41
Hauptverfasser: Carter, R.M, Abbott, S.T, Graham, I.J, Naish, T.R, Gammon, P.R
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Sprache:eng
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