前弧地震带:一个阻断下沉巨型地震破裂的流体通道
Rintaroh Suzuki1, Naoki Uchida1,2, Weiqiang Zhu3
1Graduate School of Science, Tohoku University, Sendai, Japan.
概括
在日本前方的地震中, 机器学习确定了与流体供应相关的地震带, 潜在地限制了巨大的冲击裂, 并预测了浅层地震.
科学领域:
- 地球科学
- 地震学
- 地质学
背景情况:
- 海洋板块释放的流体向地球表面迁移.
- 这些迁移流体可以影响前弧区域的构造断层和地震活动.
研究的目的:
- 使用地震数据检测和定位日本东北部的地震.
- 调查流体迁移与前弧地震性之间的关系.
- 了解预弧地震对大冲击破裂和地震预测的影响.
主要方法:
- 使用机器学习算法进行地震检测和定位.
- 分析了日本东北部海底地震网络的数据.
- 检查了从沉积板到海底的垂直地震分布.
主要成果:
- 确定了一个独特的地震性模式,称为"前弧地震带",从沉降板块延伸到海底附近.
- 这个地震带与底层板块的流体供应相关联.
- 观察到高地震性区域延伸到内陆,与已知的缓慢滑动事件和历史地震边界保持一致.
结论:
- 预弧的地震性受流层的流体迁移的影响.
- 预弧地震带可能在限制巨型冲击破裂区域中发挥作用.
- 这些发现支持该地区包括东京大都会内的浅层破坏性地震的可能性.
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