富含流体的降温地形产生异常的前弧孔隙
Christine Chesley1, Samer Naif2, Kerry Key3
1Lamont-Doherty Earth Observatory, Columbia University, Palisades, NY, USA. chesley@ldeo.columbia.edu.
Nature
|July 8, 2021
概括
潜水作为管道,将大量的水输入前弓并改变故障机制. 这项研究将海底沉积与富含流体的损害区域联系起来,影响地震活动和板块界面应力.
科学领域:
- 地质学
- 构造学
- 海洋学
背景情况:
- 潜伏地形对巨型地震行为的影响是有争议的.
- 之前的模型表明地形改变了俯冲区结构和应力, 但直接成像是有限的.
- 了解潜水区水文和断层网络至关重要.
研究的目的:
- 调查海底沉积的地质和水文影响.
- 图像一个潜伏海底山和相关的前弧的电阻结构.
- 将潜水地形与板块界面和地震性的流体诱导变化联系起来.
主要方法:
- 获取被动和受控来源的海底电磁数据.
- 在新西兰北方的Hikurangi边缘限制电阻模型.
- 地质图像与地震和缓慢滑动事件数据的相关性.
主要成果:
- 在多孔的火山岩层中吸收大量的水 (3.2 - 4.7 倍于正常的岩层).
- 图像显示了一个富含流体的板面接口.
- 在海面上方的导电异常与重复的地震和缓慢的滑动事件相关.
结论:
- 潜入海底的岩石显著改变了上层板块的结构和物理条件.
- 海底山是水运输到地幔的主要途径.
- 降压地形调节流体过压,影响有效的正常应力和地震行为.
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