| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 9535752 | Journal of Asian Earth Sciences | 2005 | 11 Pages |
Abstract
The grade of diagenetic/metamorphic alteration increases from north to south in the Antalya Unit, related to the higher heat flow due to the southward deepening of the basin. Vertical diagenetic/metamorphic inversion between the Lower Paleozoic and Triassic units is related to higher the heat flux, which affected the Triassic sediments, rather than to thrust tectonics.
Keywords
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geology
Authors
Ãmer Bozkaya, Hüseyin Yalçın,