在加拿大西部通过水力压裂激活断层
1Department of Geoscience, University of Calgary, Calgary, Alberta T1N 1N4, Canada.
概括
在加拿大西部的水力压裂操作与诱导的地震有关, 地震可能是由压力变化引发的,并且在断裂事件发生后持续数月.
科学领域:
- 地质学
- 地震学
- 石油工程
背景情况:
- 水力压裂是加拿大西部地震的主要原因.
- 在美国中西部, 排放盐水是引发地震的主要原因.
- 加拿大页岩地区的地震活动需要详细分析.
研究的目的:
- 调查加拿大页岩矿石中水力压裂与诱导地震的关系.
- 分析地震模式及其与注入数据的时空相关性.
- 了解通过液压压裂的故障激活的机制和程度.
主要方法:
- 使用基于模板的地震目录.
- 在4个月内收集了全面的注射数据.
- 分析了与水力压裂作业相关的地震性模式.
主要成果:
- 地震在水力压裂现场附近的空间和时间上紧密聚集在一起.
- 最大的诱导事件的时刻大小为3.9.
- 地震性表明压力变化可能会激活超过1公里的断层滑动.
- 由于断裂造成的断层压力导致持续数月的地震.
结论:
- 水力压裂是加拿大西部地震的重要原因.
- 诱导的地震性可以扩展到注射区之外,影响更深的地质结构.
- 了解这些地震模式对于管理与非传统石油和天然气开采有关的风险至关重要.
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