Fluid Redox Fingerprint of the CaCO<sub>3</sub>+Antigorite Dehydration Reaction in Subducted Metacarbonate Sediments
Antigorite dehydration is a process able to release, in comparison with other minerals, the highest amount of H<sub>2</sub>O from a subducting slab. The released fluid delivers critical elements (e.g., S, Cu, and REE) to the overlying subarc mantle, modifying the mantle source of arc mag...
| Main Authors: | , , , , |
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| 格式: | 文件 |
| 语言: | English |
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MDPI AG
2023-04-01
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| 丛编: | Geosciences |
| 主题: | |
| 在线阅读: | https://www.mdpi.com/2076-3263/13/5/130 |