| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 5780097 | Earth and Planetary Science Letters | 2017 | 9 Pages |
Abstract
- The δ26Mg variation in OIBs is twice as large as that in the peridotitic mantle.
- Alkaline basalt has lighter Mg isotopes than tholeiite.
- Melting degree and source composition contribute to OIBs' Mg isotopic variation.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth and Planetary Sciences (General)
Authors
Yuan Zhong, Li-Hui Chen, Xiao-Jun Wang, Guo-Liang Zhang, Lie-Wen Xie, Gang Zeng,