概括
高压实验显示,在受水化地幔岩石中,反矿的分解会释放出大量的水. 这种水可以触发部分融化,在潜水带中形成性性 magma.
科学领域:
- 地质地质地质地质地质地
- 矿物物理 矿物物理
- 石化学 石化学是一门学科.
背景情况:
- 俯冲区是构造板块相互作用的关键地质设置.
- 水在地幔形动力学和岩生成中的作用是研究的一个关键领域.
研究的目的:
- 在高压和高温条件下研究抗岩的稳定性和分解.
- 在模拟的潜水环境中量化抗戈脱水释放的水量.
- 评估这次释放的水对岩起源在俯冲区的影响.
主要方法:
- 使用受控温度和压力进行高压实验性岩石学.
- 矿物质稳定性和相变的分析.
- 在抗戈里特分解过程中释放的水含量的计算.
主要成果:
- 在2GPa时,抗石保持稳定,最高可达720°C,在3GPa时可达690°C,在5GPa时可达620°C.
- 反岩的分解释放出大量的H2O (重量为13%),远远超过海洋地的变化.
- 这种释放的水在最佳位置上升,并诱导覆盖着的地幔中部分融化.
结论:
- 抗岩脱水是潜水区的主要水源.
- 这一过程促进了在100-130公里的深度产生性性岩.
- 这些发现增强了我们对深水循环及其对弧形火山运动的影响的理解.
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