Origin of the Fangmayu Chromite Deposit, Miyun, Beijing: Constraints from Electron Microprobe Analyses of Cr-Spinel
Stratiform chromite deposits in China have long been considered to form by fractional crystallization of mafic magma. However, some researchers recently proposed that some chromite deposits are also hosted in ophiolite. In this study, Cr-spinels of the dunites, wehrlites and clinopyroxenites from th...
| Main Authors: | , , , |
|---|---|
| Format: | Article |
| Language: | English |
| Published: |
Science Press, PR China
2015-09-01
|
| Series: | Yankuang ceshi |
| Subjects: | |
| Online Access: | http://www.ykcs.ac.cn/en/article/doi/10.15898/j.cnki.11-2131/td.2015.05.017 |