Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
6442436 | Precambrian Research | 2011 | 15 Pages |
Abstract
⺠Neoproterozoic magmatism and mineralisation with emplacement age of the Dapingliang granites constrained between ca. 816 and 826 Ma. ⺠The Dapingliang granites maybe formed by partial melting of K-rich basalt of the lower crust during a period of transition from crustal compression to extension. ⺠A post-collisional granite belt derived from lower crust in the Kuluketage block was determined.
Related Topics
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Authors
Xiaofeng Cao, Xinbiao Lü, Shentai Liu, Ping Zhang, Xiang Gao, Chao Chen, Yalong Mo,