Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
8088553 | Geothermics | 2018 | 17 Pages |
Abstract
The compilation of geologic, hydraulic and thermal data of 15 geothermal wells shows permeability variation among the lithologies with the maximum observed at the top of the hydrothermally altered granite. This higher permeability is likely due to the intense fracture density in the fault core of the fracture zone and the large porous and altered damage zone which allow connection with the reservoir.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
Jeanne Vidal, Albert Genter,