Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
9528431 | Marine and Petroleum Geology | 2005 | 14 Pages |
Abstract
Surface indications suggest that the structure has been active until the present day. Elevations of a bedding plane on the Shedgum plateau reveal a 0.25° dip angle, which cannot be distinguished on the surface by the human eye. The movements that occurred during the 4 million years since the Pliocene period reveal an average tilting of 0.06° per one million years.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Economic Geology
Authors
Salih Saner, Khattab Al-Hinai, Dogan Perincek,