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GCS_WGS_1984
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FGDC
Bureau of Economic Geology
10100 Burnet Rd. Bldg. 130
Austin
TX
78729
US
8-5
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BEG
10100 Burnet Rd. Bldg 139
Austin
Texas
78758
US
Enterprise Geodatabase Feature Class
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Repetto Continuity
<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>
Continuity for the Repetto Formation
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.
Los Angels Basin
Repetto
Repetto
Los Angels Basin
Access constraints: Restriction Code: other restrictions; Other Constraints: Access constraints: None
See access and use constraints information.
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