Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
6444562 | Journal of Asian Earth Sciences | 2013 | 20 Pages |
Abstract
From 513 to 420Â Ma, the Qimantagh basement mainly underwent the northward subduction of the Qimantagh Ocean. In the Permian (290-257Â Ma), due to the northward subduction of the Paleo-Tethyan Ocean, the Qimantagh area was characterized by an active continental margin setting, developing a continental magmatic arc.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geology
Authors
Wei Li, Franz Neubauer, Yongjiang Liu, Johann Genser, Shoumai Ren, Guoqing Han, Chenyue Liang,