由密集的地震阵列揭示的上层地幔的局部地震变形
Asaf Inbal1, Jean Paul Ampuero2, Robert W Clayton2
1Seismological Laboratory, California Institute of Technology, Pasadena, CA 91125, USA. ainbal@gps.caltech.edu.
概括
纽波特-英格尔伍德断层 (NIF) 显示了深层地震活动延伸到地幔,与典型的大陆转变断层不同. 这种深度的地震性与地幔流体和岩层边界偏移有关.
科学领域:
- 地质学
- 地震学
- 构造学
背景情况:
- 大陆转变断层通常仅限于上层地的地震性.
- 洛杉矶盆地的纽波特-英格尔伍德断层 (NIF) 呈现出异常,地震活动延伸到上层地幔.
研究的目的:
- 在加利福尼亚州长底部的纽波特-英格尔伍德断层 (NIF) 的深度地震结构.
- 描述NIF的岩层地幔根内发生的深度地震的性质.
主要方法:
- 使用地震阵列分析绘制地震性图.
- 地震数据与地化学证据和岩层边界数据的相关性.
主要成果:
- 在一个穿透岩层地幔的局部区域确定了地震性.
- 深度地震与地质化学证据的地幔流体通道和石化层-石化层边界的尖垂直偏移有关.
- 这些深度地震显示了狭窄的尺寸分布和弱的时间集群.
结论:
- NIF具有延伸到岩层地幔的地震源.
- 深度地震的特征表明,在断层区域内,强相互作用模式转变为弱相互作用模式.
- 地幔流体和石层结构在NIF的深度地震性中起着重要作用.
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