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| DOI | 10.1038/s41467-021-21343-9 |
| Depth-dependent peridotite-melt interaction and the origin of variable silica in the cratonic mantle | |
| Emma L. Tomlinson; Balz S. Kamber | |
| 2021-02-17 | |
| 发表期刊 | Nature Communications
 |
| 出版年 | 2021 |
| 领域 | 资源环境 |
| URL | 查看原文 |
| 引用统计 | |
| 文献类型 | 期刊论文 |
| 条目标识符 | http://119.78.100.173/C666/handle/2XK7JSWQ/315665 |
| 专题 | 资源环境科学 |
| 推荐引用方式 GB/T 7714 | Emma L. Tomlinson,Balz S. Kamber. Depth-dependent peridotite-melt interaction and the origin of variable silica in the cratonic mantle[J]. Nature Communications,2021. |
| APA | Emma L. Tomlinson,&Balz S. Kamber.(2021).Depth-dependent peridotite-melt interaction and the origin of variable silica in the cratonic mantle.Nature Communications. |
| MLA | Emma L. Tomlinson,et al."Depth-dependent peridotite-melt interaction and the origin of variable silica in the cratonic mantle".Nature Communications (2021). |
| 条目包含的文件 | 条目无相关文件。 | |||||
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