4.7 Article

Detecting the Preparatory Phase of Induced Earthquakes at The Geysers (California) Using K-Means Clustering

期刊

出版社

AMER GEOPHYSICAL UNION
DOI: 10.1029/2023JB026429

关键词

earthquake preparatory phase; machine learning; induced earthquakes

向作者/读者索取更多资源

This paper investigates the seismic activity preceding 19 moderate earthquakes in The Geysers, Northern California, aiming to verify the existence of a preparatory phase before their occurrence. The analysis shows that there is a common preparatory phase for 11 events, and another five events have different characteristics. The duration of the preparatory process ranges between about 16 hours and four days. There is also a clear correlation between events with a preparation phase and the location of injection's wells.
The generation of strong earthquakes is a long-debated problem in seismology, and its importance is increased by the possible implications for earthquake forecasting. It is hypothesized that the earthquake generation processes are anticipated by several phenomena occurring within a nucleation region. These phenomena, also defined as preparatory processes, load stress on the fault leading it to reach a critical state. In this paper, we investigate the seismicity preceding 19 moderate (M-w >= 3.5) earthquakes at The Geysers, Northern California, aiming to verify the existence of a preparatory phase before their occurrence. We apply an unsupervised K-means clustering technique to analyze time series of physics-related features extracted from catalog information and estimated for events occurred before the mainshocks. Specifically, we study the temporal evolution of the b-value from the Gutenberg-Richter (b), the magnitude of completeness (Mc), the fractal dimension (Dc), the inter-event time (dt), and the moment rate (M-0). Our analysis shows that out of 19 moderate magnitude events considered, a common preparatory phase for 11 events is clearly identified, plus other five events for which we can guess a preparatory phase but with different characteristics from the previous ones. The latter result confirms that even within the same tectonic context different possible activation behaviors may exist. The duration of the preparatory process ranges between about 16 hr and 4 days. We observe that also for the retrieved preparatory process a decrease in b, Mc, and Dc, and an increase of M-0. Finally, we show a clear correlation between events with a preparation phase and the location of injection's wells, suggesting an important role of fluids in the preparatory process.

作者

我是这篇论文的作者
点击您的名字以认领此论文并将其添加到您的个人资料中。

评论

主要评分

4.7
评分不足

次要评分

新颖性
-
重要性
-
科学严谨性
-
评价这篇论文

推荐

暂无数据
暂无数据