| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 5468926 | Applied Clay Science | 2017 | 13 Pages |
Abstract
It is envisaged that this temperature limit may be indicative for external orogenic settings at normal to slightly hyperthermal heat flow. This will help to a better understanding of correlating organic matter versus clay mineral indices to determine geothermal settings for basic research and exploration.
Keywords
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
Josef Mullis, Rafael Ferreiro Mählmann, Monika Wolf,