与日本西南部的沉降相关的非火山深震
1National Research Institute for Earth Science and Disaster Prevention, Tenno-dai 3-1, Tsukuba, Ibaraki, 305-0006, Japan. obara@bosai.go.jp
概括
在日本非火山地区发生的深度震动位于菲律宾海板块沿线.
科学领域:
- 地质物理学 地质物理学
- 地震学 地震学
背景情况:
- 深度震动是发生在地球地深处的地震事件.
- 了解震产生机制对于地震危险评估至关重要.
研究的目的:
- 在日本西南部非火山地区识别和定位深度,长期震动.
- 为了研究震分布与菲律宾海底板块之间的关系.
主要方法:
- 地震数据分析用于检测和定位深度震动.
- 地理物理地图绘制了潜水板的几何和深度.
主要成果:
- 在菲律宾海板块的600公里范围内发现了深度长期震动.
- 地震发生在平均深度为30公里的地方,在莫霍罗维奇断层附近.
- 个别的震动持续了几个星期.
结论:
- 震动的空间分布表明与潜水板有联系.
- 板块内的脱水过程产生的液体生成是这些深度震的潜在原因.
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