Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
8911847 | Lithos | 2017 | 61 Pages |
Abstract
Combined published works with our new geochronological, geological, geochemical and isotopic data, we propose that the CTT may have evolved from a continental arc to a syn-collisional setting during the period of ca. 307-301Â Ma. The continuing southward subduction of the Junggar oceanic slab beneath the CTT in the Late Carboniferous resulted in extensive arc-related volcanic rocks emplacement that had indirect links to the Pb-Zn mineralization (e.g., reworked/upgraded).
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
Wan-Jian Lu, Hua-Yong Chen, Li Zhang, Jin-Sheng Han, Bing Xiao, Deng-Feng Li, Wei-Feng Zhang, Cheng-Ming Wang, Lian-Dang Zhao, Hong-Jun Jiang,