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 |
DOI | 10.1016/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
浏览0
下载0
收藏0
其他版本
除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。