Lyons Sandstone, Denver Basin (11)

Comments on Geologic Parameters

11 Flow Direction:

The hydraulic potential and the modeled flow regime in the underlying Fountain Formation (Lee and Bethke, 1994) show that fluids in the Fountain Formation flow along the basin's axis. As the Fountain flowpath pinches out, brine discharges upward into the Lyons, mixes with ground waters, and then migrates to the east. The potential simulated map added to the GIS data base of the Triassic-Permian unit by Belitz and Bredehoeft (1988) also shows flow movement to the east.

11 Map:

map

11 Reference:

Belitz, K., and Bredehoeft, J., 1988, Hydrodynamics of Denver Basin: explanation of subnormal fluid pressures: American Association of Petroleum Geologists Bulletin, v. 72, no. 11, p. 1334–1359.

Lee, M. L., and Bethke, C., 1994, Groundwater flow, late cementation and petroleum accumulation in the Permian Lyons Sandstone, Denver Basin: American Association of Petroleum Geologists Bulletin, v. 78, no. 2, p. 227–237.

Click here for "RI0283. Geological CO2 Sequestration Atlas of Miocene Strata, Offshore Texas State Waters"

RI0283

For a flyer on GCCC mission, activities, impact, and goals, please click here.


University of Texas at Austin

University of Texas

© 2021 Bureau of Economic Geology | Web Privacy Policy | Web Accessibility Policy