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

doi:10.1016/j.jseaes.2016.04.026

GIG OpenIR

	Liu, Ping-Ping 1; Zhou, Mei-Fu 1; Ren, Zhongyuan2 ; Wang, Christina Yan 3; Wang, Kun 3
	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
Source Publication	JOURNAL OF ASIAN EARTH SCIENCES
ISSN	1367-9120
	2016-09-01
Volume	127 Pages:211-230
DOI	10.1016/j.jseaes.2016.04.026
Language	英语
WOS Research Area	Geology
WOS ID	WOS:000381323400014
Indexed By	SCI
Citation statistics	Cited Times:21[WOS] [WOS Record] [Related Records in WOS]
Document Type	期刊论文
Identifier	http://ir.gig.ac.cn/handle/344008/33207
Collection	中国科学院广州地球化学研究所
Corresponding Author	Liu, Ping-Ping
Affiliation	1.Univ Hong Kong, Dept Earth Sci, Hong Kong, Hong Kong, Peoples R China 2.Chinese Acad Sci, Guangzhou Inst Geochem, State Key Lab Isotope Geochem, Guangzhou 510460, Guangdong, Peoples R China 3.Chinese Acad Sci, Guangzhou Inst Geochem, Key Lab Mineral & Metallogeny, Guangzhou 510460, Guangdong, Peoples R China
Recommended Citation 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.

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