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在拉顿盆地下方的注入诱导的地下室地震性:由精致的断层架构和盆地结构制约
Ruijia Wang1, Evans A Onyango2,3, Brandon Schmandt2
1Department of Earth and Space Sciences, Southern University of Science and Technology , Shenzhen, Guangdong, People's Republic of China.
概括
人造液体注射可以在新地区引发地震. 这项研究将注入井与拉顿盆地的断层复杂性和地震活动联系起来,揭示了流体连接到更深的地下层断层.
科学领域:
- 地质物理学 地质物理学
- 地震学 地震学
- 地震科学 地震科学 地震科学
背景情况:
- 液体注射引起的地震性对低地震性地区构成风险.
- 有限的研究提供了关于地震源和地下结构的详细约束.
研究的目的:
- 改进地震源观测,限制拉顿盆地的地下结构.
- 为了研究液体注入和故障重新激活之间的关系.
主要方法:
- 利用密集的节点地震阵列来精细地转移低中心.
- 采用远距离地震接收器功能来限制盆地结构.
- 分析了基于交叉相关的低中心和焦点机制.
主要成果:
- 确定了具有明显时空模式的活跃断层段.
- 在高速注入井附近观察到故障复杂性增加.
- 绘制地图的盆地厚度和沉积物结构变化.
结论:
- 液体注入影响了拉顿盆地的断层再激活和复杂性.
- 建立了从注入深度到地下室断层的潜在流体连接.
- 为了解合地下系统中的诱导地震性提供了关键的约束.
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