GIG OpenIR  > 同位素地球化学国家重点实验室
Wang, Yu1,2; Foley, Stephen F.2
Hybridization Melting Between Continent-Derived Sediment and Depleted Peridotite in Subduction Zones
Source PublicationJOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
ISSN2169-9313
2018-05-01
Volume123Issue:5Pages:3414-3429
DOI10.1029/2018JB015507
Language英语
WOS Research AreaGeochemistry & Geophysics
WOS IDWOS:000435944700009
Indexed BySCI
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Cited Times:13[WOS]   [WOS Record]     [Related Records in WOS]
Document Type期刊论文
Identifierhttp://ir.gig.ac.cn/handle/344008/37155
Collection同位素地球化学国家重点实验室
Corresponding AuthorWang, Yu
Affiliation1.Chinese Acad Sci, Guangzhou Inst Geochem, State Key Lab Isotope Geochem, Guangzhou, Guangdong, Peoples R China
2.Macquarie Univ, Dept Earth & Planetary Sci, ARC Ctr Excellence Core Crust Fluid Syst GEMOC, Sydney, NSW, Australia
Recommended Citation
GB/T 7714
Wang, Yu,Foley, Stephen F.. Hybridization Melting Between Continent-Derived Sediment and Depleted Peridotite in Subduction Zones[J]. JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH,2018,123(5):3414-3429.
APA Wang, Yu,&Foley, Stephen F..(2018).Hybridization Melting Between Continent-Derived Sediment and Depleted Peridotite in Subduction Zones.JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH,123(5),3414-3429.
MLA Wang, Yu,et al."Hybridization Melting Between Continent-Derived Sediment and Depleted Peridotite in Subduction Zones".JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH 123.5(2018):3414-3429.
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