沉降碳削弱了前弧地幔在温暖的沉降区
Ryosuke Oyanagi1,2, Atsushi Okamoto3
1School of Engineering and Science, Kokushikan University, Tokyo, 154-8515, Japan. oyanagir@kokushikan.ac.jp.
Nature communications
|August 26, 2024
概括
沉降碳转化了地幔形矿物质,在温暖的沉降区域中创造了富含和碳酸盐的区域. 这种矿物质变化可能会影响地震行为和震动活动.
科学领域:
- 地质化学 地质化学
- 矿物物理 矿物物理
- 构造学 构造学 构造学 构造学
背景情况:
- 沉浮的海洋板块将大量的碳转移到地球地幔中.
- 流体的碳动员改变了地幔石矿物学和机械性能.
研究的目的:
- 研究前弧地幔中下沉矿物质组合变化的研究.
- 碳含量流体和地幔岩石之间的模型相互作用.
主要方法:
- 多组件流体岩石相互作用的热力学建模.
- 分析矿物质组合变化与潜水区深度的分析.
主要成果:
- 富含碳的水性流体是在温暖的俯冲区 (如南开) 中产生的.
- 矿物质组合从丰富的蛇形转变为富含塔尔克+碳酸盐的矿物质组合,其深度越来越大.
- 这种过渡是由于水性碳透而发生的.
结论:
- 水性碳透影响了前弧地幔矿物学.
- 观测到的矿物过渡可能会影响地震产物 - 无地震边界深度.
- 这一过程可能会影响偶发震和滑动的下沉程度.
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