Immiscible Fe- and Si-rich silicate melts in plagioclase from the Baima mafic intrusion (SW China): Implications for the origin of bi-modal igneous suites in large igneous provinces

	Immiscible Fe- and Si-rich silicate melts in plagioclase from the Baima mafic intrusion (SW China): Implications for the origin of bi-modal igneous suites in large igneous provinces
	Liu, Ping-Ping; Zhou, Mei-Fu; Ren, Zhongyuan; Wang, Christina Yan; Wang, Kun
刊名	Journal of Asian Earth Sciences
	2016
卷号	127 页码:211-230
ISSN号	1367-9120
收录类别	SCI
语种	英语
内容类型	期刊论文
源URL	[http://ir.gig.ac.cn:8080/handle/344008/33207]
专题	中国科学院广州地球化学研究所
推荐引用方式 GB/T 7714	Liu, Ping-Ping,Zhou, Mei-Fu,Ren, Zhongyuan,et al. Immiscible Fe- and Si-rich silicate melts in plagioclase from the Baima mafic intrusion (SW China): Implications for the origin of bi-modal igneous suites in large igneous provinces[J]. Journal of Asian Earth Sciences,2016,127:211-230.
APA	Liu, Ping-Ping,Zhou, Mei-Fu,Ren, Zhongyuan,Wang, Christina Yan,&Wang, Kun.(2016).Immiscible Fe- and Si-rich silicate melts in plagioclase from the Baima mafic intrusion (SW China): Implications for the origin of bi-modal igneous suites in large igneous provinces.Journal of Asian Earth Sciences,127,211-230.
MLA	Liu, Ping-Ping,et al."Immiscible Fe- and Si-rich silicate melts in plagioclase from the Baima mafic intrusion (SW China): Implications for the origin of bi-modal igneous suites in large igneous provinces".Journal of Asian Earth Sciences 127(2016):211-230.