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Constraining of Focal Mechanisms of Induced Seismicity Using Borehole Logging Information

机译:使用钻孔测井信息约束诱导地震性的焦虑机制

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Monitoring of microseismicity is essential for successful hydraulic stimulation in Enhanced/Engineered geothermal development. Hypocenter locations of the microseismic events are indicators of fractures whose permeability has been enhanced by shear slip. In addition to the locations of microseismic events, knowledge about the geometry of the fracture network is also important for better understanding of the fractured reservoir, flow, and design of the heat extraction system since fracture geometry is directly correlated to permeability. Focal mechanisms contain first order information about the fracture network. However, due to the small number of monitoring stations in geothermal microseismic monitoring, it is often difficult to constrain the focal mechanisms of microseismicity from first motion information. We propose a novel method to overcome this limitation and estimate focal mechanism by including borehole logging information such as in-situ stress and information about existing fractures. We estimate the range of fault planes which can have shear slip in a given stress state and increase of pore pressure. By referring to that range, we eliminate candidate of focal mechanisms which are consistent with first motion information but not consistent with in-situ stress. As another approach, we use existing fracture information from borehole logging. We establish a statistical model of existing fractures and calculate the likelihood of shear slip from all candidate focal mechanisms. By referring to this model, we can reject less unlikely focal mechanisms and chose more likely ones. Thus, we can constrain the focal mechanisms considering not only seismological information but also other geophysical information. We apply our method to field data from Basel, Switzerland and examine the performance and the feasibility of our method by comparing with the well constrained focal mechanisms of larger events determined using data from a regional network.
机译:对微震性的监测对于增强/工程地热发育中的成功液压刺激至关重要。微震事件的低缩进位置是骨折的指示剂,其透露性通过剪切滑动增强。除了微震事件的位置之外,关于骨折网络的几何形状的知识对于更好地理解裂缝储存系统的更好理解,由于断裂几何形状与渗透率直接相关,因此对于更好地理解散热储存系统的裂缝储存器,流量和设计也很重要。焦点机制包含有关裂缝网络的第一订单信息。然而,由于地热微震监测中的少量监测站,通常难以从第一运动信息限制微震性的焦震机制。我们提出了一种新颖的方法来克服这种限制和估计焦点机制,包括钻孔测井信息,例如原位应力和关于现有骨折的信息。我们估计在给定的应力状态下可以具有剪切滑动的故障平面范围和孔隙压力的增加。通过参考该范围,我们消除了与第一运动信息一致但不与原位应力一致的焦点机制的候选者。作为另一种方法,我们使用来自钻孔测井的现有骨折信息。我们建立了现有骨折的统计模型,并计算了所有候选焦点机制的剪切滑动的可能性。通过参考该模型,我们可以拒绝不太可能的焦点机制,并选择更有可能的机制。因此,我们可以限制焦点机制,考虑到地震信息而且也是其他地球物理信息。我们将方法应用于来自巴塞尔,瑞士的现场数据,并通过与使用来自区域网络中的数据确定的较大事件的良好限制的焦点机制来研究我们的方法的性能和可行性。

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