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A Historical Review of Induced Earthquakes in Texas

机译:德克萨斯州诱发地震的历史回顾

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In Texas, earthquakes have occurred in close association with activities accompanying petroleum production since 1925. Here we develop a five-question test to categorize individual events as "tectonic," "possibly induced," "probably induced," or "almost certainly induced." In Texas, the probably induced and almost certainly induced earthquakes are broadly distributed geographically-in the Fort Worth basin of north Texas, the Haynesville Shale play area of east Texas, along the Gulf Coast in south Texas, and the Permian basin of west Texas. As the technologies applied to manage petroleum fields have evolved, induced earthquakes have been associated with different practices. In fields being driven by primary recovery prior to 1940, earthquakes occurred in fields extracting high volumes of petroleum from shallow strata. Subsequently, as field pressures decreased and secondary recovery technologies became common, earthquakes also occurred in association with water-flooding operations. Since 2008, the rate of earthquakes with magnitudes greater than 3 has increased from about 2 events/yr to 12 events/yr; much of this change is attributable to earthquakes occurring within a few kilometers of wastewater disposal wells injecting at high monthly rates. For three sequences monitored by temporary local seismograph networks, most hypocenters had focal depths at and deeper than the depth of injection and occurred along mapped faults situated within 2 km of injection sites. The record clearly demonstrates that induced earthquakes have been broadly distributed in several different geographic parts of Texas over the last 90 years.
机译:自1925年以来,得克萨斯州发生的地震与石油生产相关的活动密切相关。在这里,我们开发了一个五问测试,将个别事件分类为“构造”,“可能诱发”,“可能诱发”或“几乎确定诱发”。 ”在得克萨斯州,可能诱发和几乎确定诱发的地震在地理上分布广泛—在得克萨斯州北部的沃思堡盆地,得克萨斯州东部的海恩斯维尔页岩游乐区,得克萨斯州南部的墨西哥湾沿岸以及得克萨斯州西部的二叠纪盆地。随着用于管理油田的技术的发展,诱发地震与不同的实践相关联。在1940年以前的一次采油驱动的油田中,地震发生在从浅层地层开采大量石油的油田中。随后,随着油田压力的降低和二次采油技术的普及,与注水作业相关的地震也发生了。自2008年以来,大于3级的地震发生率从每年约2次事件增加到每年12次事件;这种变化的大部分归因于在废水处理井的数公里内发生的地震,这些地震以每月高速率注入。对于由临时局部地震仪网络监测的三个序列,大多数震源的震源深度都在注入深度以上,并且比注入深度更深,并且沿着注入点2 km以内的测绘断层发生。记录清楚地表明,在过去90年中,诱发地震已在德克萨斯州的几个不同地理区域广泛分布。

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