GIG OpenIR
Liu, Ping-Ping1; Zhou, Mei-Fu1; Ren, Zhongyuan2; Wang, Christina Yan3; Wang, Kun3
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 PublicationJOURNAL OF ASIAN EARTH SCIENCES
ISSN1367-9120
2016-09-01
Volume127Pages:211-230
DOI10.1016/j.jseaes.2016.04.026
Language英语
WOS Research AreaGeology
WOS IDWOS:000381323400014
Indexed BySCI
Citation statistics
Cited Times:21[WOS]   [WOS Record]     [Related Records in WOS]
Document Type期刊论文
Identifierhttp://ir.gig.ac.cn/handle/344008/33207
Collection中国科学院广州地球化学研究所
Corresponding AuthorLiu, Ping-Ping
Affiliation1.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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