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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![]() | |
2021 | |
Source Publication | Geoscience Frontiers
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Volume | 12Issue:2Pages:907-919 |
Abstract |
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DOI | 10.1016/j.gsf.2020.05.023 |
URL | 查看原文 |
Indexed By | SCI |
Language | 英语 |
Citation statistics | |
Document Type | 期刊论文 |
Identifier | http://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 |
Affiliation | 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 |
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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