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The AAPG/Datapages Combined Publications Database
AAPG Bulletin
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The Los Angeles coastal belt is traversed by chains of low hills whose anticlinally warped land surfaces correspond to underlying petroliferous structures. The Dominguez surface, named after its exposure on one of the hills, is middle Pleistocene in age. Antecedent streams indicate uplift, but may destroy significant parts of the warped surfaces. Piracy aids the recognition of uplifts. Consequent streams bear a close relationship to underlying structure. Valley-fill, alluvial fans, and sand dunes may cover anticlinal upwarps. Faulting modifies the surface in different ways.
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