Implications for metal and volatile cycles from the pH of subduction zone fluids

被引：0
|
作者：
Matthieu E. Galvez
James A. D. Connolly
Craig E. Manning
机构：
[1] Swiss Federal Institute of Technology,Earth Sciences Department
[2] Planetary and Space Sciences,Department of Earth
[3] University of California,undefined
来源：
Nature | 2016年 / 539卷
关键词：
D O I：
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中图分类号：
学科分类号：
摘要：
A thermodynamic model of fluid pH and its variability in Earth’s mantle and subducting crust highlights chemical feedbacks that connect deep Earth to surface processes.
引用
收藏
页码：420 / 424
页数：4
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