Pliocene-Quaternary crustal melting in central and northern Tibet and insights into crustal flow
oleh: Qiang Wang, Chris J. Hawkesworth, Derek Wyman, Sun-Lin Chung, Fu-Yuan Wu, Xian-Hua Li, Zheng-Xiang Li, Guo-Ning Gou, Xiu-Zheng Zhang, Gong-Jian Tang, Wei Dan, Lin Ma, Yan-Hui Dong
| Format: | Article |
|---|---|
| Diterbitkan: | Nature Portfolio 2016-06-01 |
Deskripsi
The role of the low velocity-high conductivity zones (LV–HCZs) in developing the Tibetan Plateau has remained controversial. Here, Wang et al.present new geochemical and petrological data that show the LV–HCZs are sources of partial melt thus giving insight into the development of the Tibetan Plateau.