| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 6441072 | Lithos | 2011 | 13 Pages |
Abstract
⺠Lack of Ir depletion in volcanic rocks from SE China suggests more oxidized SCLM. ⺠Magmas underwent olivine, chromite and/or Fe-Pt alloys fractionation. ⺠There were small amounts of sulfide segregated during magmatic evolution. ⺠Pt depletion derived from fractionation of an Fe-Pt alloy/a Pt-depleted mantle source.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
Alexandra Yang Yang, Tai-Ping Zhao, Liang Qi, Sheng-Hong Yang, Mei-Fu Zhou,