Knowledge Management System Of Guangzhou Institute of Geochemistry,CAS
Xue, Shuo1,2; Li, Yuan1,2 | |
Pyrrhotite-silicate melt partitioning of rhenium and the deep rhenium cycle in subduction zones | |
Source Publication | GEOLOGY |
ISSN | 0091-7613 |
2022-02-01 | |
Volume | 50Issue:2Pages:232-237 |
DOI | 10.1130/G49374.1 |
Language | 英语 |
WOS Research Area | Geology |
WOS ID | WOS:000749744100006 |
Indexed By | SCI |
Citation statistics | |
Document Type | 期刊论文 |
Identifier | http://ir.gig.ac.cn/handle/344008/66384 |
Collection | 中国科学院广州地球化学研究所 |
Corresponding Author | Li, Yuan |
Affiliation | 1.Chinese Acad Sci, Guangzhou Inst Geochem, State Key Lab Isotope Geochem, Guangzhou 510640, Peoples R China 2.Chinese Acad Sci, Ctr Excellence Deep Earth Sci, Guangzhou 510640, Peoples R China |
Recommended Citation GB/T 7714 | Xue, Shuo,Li, Yuan. Pyrrhotite-silicate melt partitioning of rhenium and the deep rhenium cycle in subduction zones[J]. GEOLOGY,2022,50(2):232-237. |
APA | Xue, Shuo,&Li, Yuan.(2022).Pyrrhotite-silicate melt partitioning of rhenium and the deep rhenium cycle in subduction zones.GEOLOGY,50(2),232-237. |
MLA | Xue, Shuo,et al."Pyrrhotite-silicate melt partitioning of rhenium and the deep rhenium cycle in subduction zones".GEOLOGY 50.2(2022):232-237. |
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