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Chinese Academy of Sciences Institutional Repositories Grid
Reaction between basaltic melt and orthopyroxene at 3.0–4.5 ​GPa: Implications for the evolution of ocean island basalts in the mantle

文献类型:期刊论文

作者Chunjuan Zang; Mingliang Wang; Hongfeng Tang; Hanqi He
刊名Geoscience Frontiers
出版日期2021
卷号12期号:2页码:907-919
DOI10.1016/j.gsf.2020.05.023
英文摘要

 

 

URL标识查看原文
语种英语
源URL[http://ir.gyig.ac.cn/handle/42920512-1/12443]  
专题地球化学研究所_地球内部物质高温高压实验室
作者单位1.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
推荐引用方式
GB/T 7714
Chunjuan Zang,Mingliang Wang,Hongfeng Tang,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[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.

入库方式: OAI收割

来源:地球化学研究所

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