| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 4697369 | Ore Geology Reviews | 2014 | 20 Pages |
Abstract
The most favorable setting for the development of the Jabali secondary deposit could be placed in the early Miocene (~Â 17Â Ma), when supergene weathering was favored by major uplift and exhumation resulting from the main phase of Red Sea extension. Low-temperature hydrothermal fluids may have also circulated at the same time, through the magmatically-induced geothermal activity in the area.
Keywords
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Economic Geology
Authors
N. Mondillo, M. Boni, G. Balassone, M. Joachimski, A. Mormone,