2021
DOI: 10.3390/s21175815
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Microseismic P-Wave Travel Time Computation and 3D Localization Based on a 3D High-Order Fast Marching Method

Abstract: The travel time computation of microseismic waves in different directions (particularly, the diagonal direction) in three-dimensional space has been found to be inaccurate, which seriously affects the localization accuracy of three-dimensional microseismic sources. In order to solve this problem, this research study developed a method of calculating the P-wave travel time based on a 3D high-order fast marching method (3D_H_FMM). This study focused on designing a high-order finite-difference operator in order t… Show more

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Cited by 3 publications
(1 citation statement)
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“…Accurate earthquake location is of great significance to the study of the distribution and deep structure of seismogenic faults. In the location of microseismic events, the arrival time difference at different stations relative to the same earthquake event is picked up by the cross correlation technique to determine the source location, hence the time difference directly affects the accuracy of the location results [1][2][3][4][5][6].…”
Section: Introductionmentioning
confidence: 99%
“…Accurate earthquake location is of great significance to the study of the distribution and deep structure of seismogenic faults. In the location of microseismic events, the arrival time difference at different stations relative to the same earthquake event is picked up by the cross correlation technique to determine the source location, hence the time difference directly affects the accuracy of the location results [1][2][3][4][5][6].…”
Section: Introductionmentioning
confidence: 99%