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:

Glen Canyon Group, Sevier Basin and Kaiparowitz Bench

Comments on Geologic Parameters

6 Continuity:

General sand-body continuity maps of the Navajo Sandstone throughout Utah were presented by Stanley and others (1971) and Kocurek and Dott (1983). These maps are schematic and do not display sand-body pinch-outs where the Navajo Sandstone intertongues with the Carmel Formation top seal.

6 Map:

 

6 Reference:

Kocurek, G., and Dott, R. H., Jr., 1983, Jurassic paleogeography of the central and southern Rocky Mountains region, in Reynolds, M. W., and Dolly, E. D., eds., Mesozoic paleogeography of the West-Central United States: Rocky Mountain paleogeography symposium: Denver, Rocky Mountain Section, Society of Economic Paleontologists and Mineralogists, v. 2, p. 101–116.

Stanley, K. O., Jordan, W. M., and Dott, R. H., Jr., 1971, New hypothesis of early Jurassic paleogeography and sediment dispersal for western United States: American Association of Petroleum Geologists Bulletin, v. 55, no. 1, p. 10–19.