Origin of the Fangmayu Chromite Deposit, Miyun, Beijing: Constraints from Electron Microprobe Analyses of Cr-Spinel

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...

Full beskrivning

Bibliografiska uppgifter
Huvudupphovsmän: LI Li-xing, ZHU Ming-yu, FANG Tong-ming, LI Hou-min
Materialtyp: Artikel
Språk:English
Publicerad: Science Press, PR China 2015-09-01
Serie:Yankuang ceshi
Ämnen:
fangmayu
chromite deposit
cr-spinel
ultramafic rocks
alaskan-type intrusion
electron microprobe
Länkar:http://www.ykcs.ac.cn/en/article/doi/10.15898/j.cnki.11-2131/td.2015.05.017

Internet

http://www.ykcs.ac.cn/en/article/doi/10.15898/j.cnki.11-2131/td.2015.05.017

Liknande verk