GIG OpenIR  > 中国科学院矿物学与成矿学重点实验室
Zhang, Long1; Sun, Wei-dong2,3,4; Chen, Ren-Xu5
Evolution of serpentinite from seafloor hydration to subduction zone metamorphism: Petrology and geochemistry of serpentinite from the ultrahigh pressure North Qaidam orogen in northern Tibet
Source PublicationLITHOS
ISSN0024-4937
2019-11-15
Volume346Pages:19
DOI10.1016/j.lithos.2019.105158
Language英语
WOS Research AreaGeochemistry & Geophysics ; Mineralogy
WOS IDWOS:000488335600016
Indexed BySCI
Citation statistics
Cited Times:7[WOS]   [WOS Record]     [Related Records in WOS]
Document Type期刊论文
Identifierhttp://ir.gig.ac.cn/handle/344008/46830
Collection中国科学院矿物学与成矿学重点实验室
Corresponding AuthorZhang, Long
Affiliation1.Chinese Acad Sci, Guangzhou Inst Geochem, CAS Key Lab Mineral & Metallogeny, Guangzhou 510640, Guangdong, Peoples R China
2.Chinese Acad Sci, Ctr Deep Sea Res, Inst Oceanol, Qingdao 266071, Shandong, Peoples R China
3.Qingdao Natl Lab Marine Sci & Technol, Lab Marine Mineral Resources, Qingdao 266237, Shandong, Peoples R China
4.Chinese Acad Sci, CAS Ctr Excellence Tibetan Plateau Earth Sci, Beijing 100101, Peoples R China
5.Univ Sci & Technol China, Sch Earth & Space Sci, CAS Key Lab Crust Mantle Mat & Environm, Hefei 230026, Anhui, Peoples R China
Recommended Citation
GB/T 7714
Zhang, Long,Sun, Wei-dong,Chen, Ren-Xu. Evolution of serpentinite from seafloor hydration to subduction zone metamorphism: Petrology and geochemistry of serpentinite from the ultrahigh pressure North Qaidam orogen in northern Tibet[J]. LITHOS,2019,346:19.
APA Zhang, Long,Sun, Wei-dong,&Chen, Ren-Xu.(2019).Evolution of serpentinite from seafloor hydration to subduction zone metamorphism: Petrology and geochemistry of serpentinite from the ultrahigh pressure North Qaidam orogen in northern Tibet.LITHOS,346,19.
MLA Zhang, Long,et al."Evolution of serpentinite from seafloor hydration to subduction zone metamorphism: Petrology and geochemistry of serpentinite from the ultrahigh pressure North Qaidam orogen in northern Tibet".LITHOS 346(2019):19.
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