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Continuity for the Repetto Formation |
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Continuity for the Repetto Formation |
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Conrey, B. L., 1967, Early Pliocene sedimentary history of the Los Angeles Basin, California: California Division of Mines and Geology Special Report 93, 63 p. |
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<DIV STYLE="text-align:Left;"><P STYLE="text-align:Justify;font-size:16ptmargin:7 0 7 0;"><SPAN><SPAN>The sandy deposits of the Repetto Formation, consisting of channel-fill deposits in suprafan facies, are distributed in the central structural trough north and east of the Palos Verdes Hills (Redin, 1991). These sandstones were sourced from the northeast, from conglomeratic mid- to upper-channelized fan deposits. Repetto sandstones grade southward from the suprafan facies into distal submarine-fan facies into offshore areas.</SPAN></SPAN></P><DIV><P><SPAN /></P></DIV></DIV> |
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See access and use constraints information. |
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| title:
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Repetto Continuity |
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["Repetto","Los Angels Basin"] |
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en-US |
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