General Setting
Information Search and Selection

Com ments

on

Geo logic

Para meters

1 Depth:

2 Permeability/Hydraulic Conductivity:

3 Formation Thickness:
4 Net Sand Thickness:
5 Percent Shale:
6 Continuity:
7 Top Seal Thickness:
8 Continuity of top seal:
9 Hydrocarbon Production:
10 Fluid Residence Time:
11 Flow Direction Elevation:

12

CO2 Solu bility Brine

 12a Temperature:
12b Pressure:
12c Salinity:
13 Rock/Water Reaction:
14 Porosity:
15 Water Chemistry:
16 Rock Mineralogy:

Repetto Formation, Los Angeles Basin

Comments on Geologic Parameters

6 Continuity:

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.

6 Map:

6 Reference:

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.