Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
9534281 | Earth-Science Reviews | 2005 | 10 Pages |
Abstract
The turtleback surfaces have been considered unique to the Death Valley region, although detachment surfaces, rollover folds, and other extensional structures have been well observed in other extended terranes of the world. The presence of a turtleback fault surface in western Anatolia, Turkey, suggests that the turtleback faults may be common structural features of highly extended terranes.
Keywords
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geology
Authors
Ibrahim Ãemen, Okan Tekeli, Gűrol SeyitoÄlu, Veysel Isik,