| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 6350084 | Palaeogeography, Palaeoclimatology, Palaeoecology | 2014 | 53 Pages |
Abstract
Based on the analysed biomarker thermal maturity indicators, it may be deduced that the Mukalla coals and carbonaceous shales in the Jiza-Qamar Basin have entered an early-mature to mature stages for hydrocarbon generation. This is also supported by vitrinite reflectance values of 0.63-0.83% Ro indicative that these sediments have reached oil window maturity.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
Mohammed Hail Hakimi, Wan Hasiah Abdullah,