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An automated cross-correlation based event detection technique and its application to a surface passive data set

机译:基于自动互相关的事件检测技术及其在表面无源数据集中的应用

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摘要

In studies on heavy oil, shale reservoirs, tight gas and enhanced geothermal systems, the use of surface passive seismic data to monitor induced microseismicity due to the fluid flow in the subsurface is becoming more common. However, in most studies passive seismic records contain days and months of data and manually analysing the data can be expensive and inaccurate. Moreover, in the presence of noise, detecting the arrival of weak microseismic events becomes challenging. Hence, the use of an automated, accurate and computationally fast technique for event detection in passive seismic data is essential. The conventional automatic event identification algorithm computes a running-window energy ratio of the short-term average to the long-term average of the passive seismic data for each trace. We show that for the common case of a low signal-to-noise ratio in surface passive records, the conventional method is not sufficiently effective at event identification. Here, we extend the conventional algorithm by introducing a technique that is based on the cross-correlation of the energy ratios computed by the conventional method. With our technique we can measure the similarities amongst the computed energy ratios at different traces. Our approach is successful at improving the detectability of events with a low signal-to-noise ratio that are not detectable with the conventional algorithm. Also, our algorithm has the advantage to identify if an event is common to all stations (a regional event) or to a limited number of stations (a local event). We provide examples of applying our technique to synthetic data and a field surface passive data set recorded at a geothermal site.
机译:在对重油,页岩储层,致密气和增强的地热系统的研究中,由于地下流体的流动,利用地面被动地震数据来监测诱发的微地震变得越来越普遍。但是,在大多数研究中,被动地震记录包含数天和数月的数据,而手动分析数据可能既昂贵又不准确。此外,在存在噪声的情况下,检测微地震事件的到来变得具有挑战性。因此,在被动地震数据中使用自动,准确和计算快速的技术进行事件检测至关重要。常规的自动事件识别算法为每条迹线计算被动地震数据的短期平均值与长期平均值的运行窗口能量比。我们表明,对于在表面被动记录中信噪比低的常见情况,常规方法在事件识别方面不够有效。在这里,我们通过引入一种基于常规方法计算出的能量比的互相关的技术来扩展常规算法。利用我们的技术,我们可以测量不同轨迹处计算出的能量比之间的相似性。我们的方法成功地提高了具有传统算法无法检测到的低信噪比的事件的可检测性。同样,我们的算法具有识别事件是否是所有站点(区域事件)或有限数量的站点(本地事件)共有的优势。我们提供了将我们的技术应用于合成数据和地热站点记录的地表被动数据集的示例。

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