| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 6441037 | Lithos | 2011 | 18 Pages |
Abstract
⺠A bimodal volcanic event took place in the Early Permian, at around 295 Ma in the Eastern Tianshan Belt. ⺠The bimodal volcanic series was generated in an initial post-collisional setting. ⺠Basalts were likely derived from a lithospheric depleted mantle with partial incorporation of crustal components. ⺠Zircons from rhyolites yield varied εHf(t) values, suggesting a mixing of multiple source materials.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
Xijie Chen, Liangshu Shu, M. Santosh,