ACTA Scientiarum Naturalium Universitatis Pekinensis
比较而言, 采用本文提出的走时残差计算方法可以有效地提高目标函数在水平方向及垂向上的收敛性, 从而得到更加准确的震源定位结果。
致谢 感谢中国石油化工集团公司石油工程地球物理有限公司胜利分公司于静主任和冯刚经理提供实际监测资料。
参考文献[1] 王健, 曾晓献, 李振峰, 等. 基于走时拟合的微震
192‒197源定位及拾震器布阵研究. 吉林大学学报: 信息科学版, 2012, 30(2):
800‒807 [2] 尹陈, 刘鸿, 李亚林, 等. 微地震监测定位精度分析. 地球物理学进展, 2013, 28(2): [3] 张娜玲. 基于微地震监测的油井压裂裂缝成像算法研究[D]. 长春: 吉林大学, 2010 [4] Zimmer U, Bland H, Jing D, et al. Accuracy of microseismic event locations recorded with single and
1519‒ distributed downhole sensor arrays // SEG Technical Program Expanded Abstracts. Tulsa, 2009: 1523 [5] 海宝权. 微地震定位方法研究[D]. 北京: 中国地质大学(北京), 2014 [6] Eisner L, Duncan P M, Heigl W M, et al. Uncertainties
648‒655 in passive seismic monitoring. The Leading Edge, 2009, 28(6):
41‒46 [7] Maxwell S. Microseismic location uncertainty. CSEG Recorder, 2009, 34(4):
[8] Jansky J, Plicka V, Eisner L. Feasibility of jointly locating microseismic events with data from surface 35‒71 and downhole receivers. First Break, 2013, 31(7): [9] 王连飞. 基于遗传算法的油井压裂微震震源点的定位技术研究[D]. 长春: 吉林大学, 2012 [10] 孙英杰. 微地震震源反演方法研究[D]. 青岛: 中国石油大学(华东), 2008 [11] 董蕊静. 水力压裂井间微地震震源定位方法研究[D]. 西安: 长安大学, 2013 [12] Prugger A F, Gendzwill D J. Microearthquake location: a nonlinear approach that makes use of a
375‒377 simplex stepping procedure. Bulletin of the Seismological Society of America, 1995, 85(1): [13] Glenn D N, Vidale J E. Eaethquake location by 3-D
395‒410 finite-difference travel times. Bulletin of the Seismological Society of America, 1990, 80(2): [14] Jansky J, Plicka V, Eisner L. Feasibility of joint 1D velocity model and event location inversion by the
229‒234 neighbourhood algorithm. Geophysical Prospecting, 2010, 58(2): [15] Jones G A, Kendall J M, Bastow I D, et al. Locating
34‒49 microseismic events using borehole data. Geophysical Prospecting, 2014, 62(1): [16] Eisner L, Hulsey B J, Duncan P, et al. Comparison of
809‒820 surface and borehole locations of induced seismicity. Geophysical Prospecting, 2010, 58(5):