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Wave equation based microseismic source location and velocity inversion

机译:基于波动方程的微震源位置和速度反演

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The microseismic event locations and velocity information can be used to infer the stress field and guide hydraulic fracturing process, as well as to image the subsurface structures. How to get accurate micro seismic event locations and velocity model is the principal problem in reservoir monitoring. For most location methods, the velocity model has significant relation with the accuracy of the location results. The velocity obtained from log data is usually too rough to be used for location directly. It is necessary to discuss how to combine the location and velocity inversion. Among the main techniques for locating microseismic events, time reversal imaging (TRI) based on wave equation avoids traveltime picking and offers high-resolution locations. Frequency dependent wave equation traveltime inversion (FWT) is an inversion method that can invert velocity model with source uncertainty at certain frequency band. Thus we combine TRI with FWT to produce improved event locations and velocity model. In the proposed approach, the location and model information are interactively used and updated. Through the proposed workflow, the inverted model is better resolved and the event locations are more accurate. We test this method on synthetic borehole data and filed data of a hydraulic fracturing experiment. The results verify the effectiveness of the method and prove it has potential for real-time microseismic monitoring. (C) 2016 Elsevier B.V. All rights reserved.
机译:微地震事件的位置和速度信息可用于推断应力场并指导水力压裂过程,以及对地下结构成像。如何获得准确的微震事件位置和速度模型是储层监测的主要问题。对于大多数定位方法而言,速度模型与定位结果的准确性有着显着的关系。从测井数据获得的速度通常太粗糙,无法直接用于定位。有必要讨论如何结合位置和速度反演。在定位微地震事件的主要技术中,基于波动方程的时间反转成像(TRI)避免了行程时间的选择,并提供了高分辨率的位置。频率相关的波动方程行进时间反演(FWT)是一种反演方法,可以在一定频带下以速度不确定性反演速度模型。因此,我们将TRI与FWT相结合以产生改进的事件位置和速度模型。在所提出的方法中,位置和模型信息被交互地使用和更新。通过提出的工作流程,可以更好地解析倒置模型,并更准确地确定事件位置。我们在合成钻孔数据和水力压裂实验的现场数据中测试了该方法。结果验证了该方法的有效性,并证明了其对实时微震监测的潜力。 (C)2016 Elsevier B.V.保留所有权利。

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