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Reaction between basaltic melt and orthopyroxene at 3.0–4.5 ​GPa: Implications for the evolution of ocean island basalts in the mantle
Chunjuan Zang; Mingliang Wang; Hongfeng Tang; Hanqi He
2021
Source PublicationGeoscience Frontiers
Volume12Issue:2Pages:907-919
Abstract

 

 

DOI10.1016/j.gsf.2020.05.023
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Indexed BySCI
Language英语
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Cited Times:2[WOS]   [WOS Record]     [Related Records in WOS]
Document Type期刊论文
Identifierhttp://ir.gyig.ac.cn/handle/42920512-1/12443
Collection地球内部物质高温高压实验室
地球深部物质与流体作用地球化学研究室
Affiliation1.School of Resource and Civil Engineering, Suzhou University, Suzhou 234000, Anhui, China
2.Key Laboratory of Mine Water Resource Utilization, Education Department of Anhui Province, Suzhou 234000, China
3.School of Earth and Environment, Anhui University of Science and Technology, Huainan 232001, Anhui, China
4.Key Laboratory for High Temperature & High Pressure Study of the Earth’s Interior, Institute of Geochemistry, Chinese Academy of Science, Guiyang 550002, China
Recommended Citation
GB/T 7714
Chunjuan Zang,Mingliang Wang,Hongfeng Tang,等. Reaction between basaltic melt and orthopyroxene at 3.0–4.5 ​GPa: Implications for the evolution of ocean island basalts in the mantle[J]. Geoscience Frontiers,2021,12(2):907-919.
APA Chunjuan Zang,Mingliang Wang,Hongfeng Tang,&Hanqi He.(2021).Reaction between basaltic melt and orthopyroxene at 3.0–4.5 ​GPa: Implications for the evolution of ocean island basalts in the mantle.Geoscience Frontiers,12(2),907-919.
MLA Chunjuan Zang,et al."Reaction between basaltic melt and orthopyroxene at 3.0–4.5 ​GPa: Implications for the evolution of ocean island basalts in the mantle".Geoscience Frontiers 12.2(2021):907-919.
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