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Qi, Yue1,2; Gou, Guo-Ning1,2; Wang, Qiang1,2,3; Wyman, Derek A.4; Jiang, Zi-Qi1,5; Li, Qi-Li6; Zhang, Le1
Cenozoic mantle composition evolution of southern Tibet indicated by Paleocene (similar to 64 Ma) pseudoleucite phonolitic rocks in central Lhasa terrane
Source PublicationLITHOS
Corresponding AuthorWang, Qiang(wqiang@gig.ac.cn)
ISSN0024-4937
2018-03-01
Volume302Pages:178-188
DOI10.1016/j.lithos.2017.12.021
Indexed BySCI
Language英语
WOS Research AreaGeochemistry & Geophysics ; Mineralogy
WOS IDWOS:000428497500011
Funding OrganizationKey Program of the Chinese Academy of Sciences ; National Key R & D Program of China ; National Natural Science Foundation of China ; Talent Project of Guangdong Province ; Guangzhou Institute of Geochemistry, Chinese Academy of Sciences (GIGCAS 135 Project)
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Cited Times:5[WOS]   [WOS Record]     [Related Records in WOS]
Document Type期刊论文
Identifierhttp://ir.gig.ac.cn/handle/344008/36714
Collection同位素地球化学国家重点实验室_期刊论文
Corresponding AuthorWang, Qiang
Affiliation1.Chinese Acad Sci, Guangzhou Inst Geochem, State Key Lab Isotope Geochem, Guangzhou 510640, Guangdong, Peoples R China
2.Univ Chinese Acad Sci, Beijing 10069, Peoples R China
3.CAS Ctr Excellence Tibetan Plateau Earth Sci, Beijing 10010, Peoples R China
4.Univ Sydney, Sch Geosci, Sydney, NSW 2006, Australia
5.Guilin Univ Technol, Sch Earth Sci, Guilin 541004, Peoples R China
6.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
Recommended Citation
GB/T 7714
Qi, Yue,Gou, Guo-Ning,Wang, Qiang,et al. Cenozoic mantle composition evolution of southern Tibet indicated by Paleocene (similar to 64 Ma) pseudoleucite phonolitic rocks in central Lhasa terrane[J]. LITHOS,2018,302:178-188.
APA Qi, Yue.,Gou, Guo-Ning.,Wang, Qiang.,Wyman, Derek A..,Jiang, Zi-Qi.,...&Zhang, Le.(2018).Cenozoic mantle composition evolution of southern Tibet indicated by Paleocene (similar to 64 Ma) pseudoleucite phonolitic rocks in central Lhasa terrane.LITHOS,302,178-188.
MLA Qi, Yue,et al."Cenozoic mantle composition evolution of southern Tibet indicated by Paleocene (similar to 64 Ma) pseudoleucite phonolitic rocks in central Lhasa terrane".LITHOS 302(2018):178-188.
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