Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
8911650 | Lithos | 2018 | 90 Pages |
Abstract
In combination with regional geological studies, our geochemical and geochronological results suggest that the late Permian Xiaochangdu and Late Triassic Kagong arc-like granitoids represent a section of a Permo-Triassic magmatic arc that was associated with the eastward subduction of the Paleo-Tethys oceanic slab beneath the Northern Qiangtang-Changdu terrane. Combined with other geological evidence, the ~263-232â¯Ma arc-like granitoids clearly indicate that final closure of the Paleo-Tethys ocean have not occurred until the end of the Triassic.
Related Topics
Physical Sciences and Engineering
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Geochemistry and Petrology
Authors
Xinyu Wang, Shifeng Wang, Chao Wang, Wenkun Tang,