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 |
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