A Layered Velocity Location Method for Microseismic Sources in Regional Rock Mass
A positioning method and area division technology, applied in the field of geotechnical engineering, can solve problems such as the limitation of seismic source positioning accuracy
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[0066] In this embodiment, the size of the rock mass area of the microseismic source to be tested is 200m × 200m × 200m, and the positioning steps of the microseismic source are as follows:
[0067] ①According to the rock mass wave velocity in the rock mass area of the microseismic source to be tested recorded in the geological exploration data, the above rock mass area is divided into three wave velocity layers, the rock mass wave velocity in the same wave velocity layer is equal and the interface of each wave velocity layer In order to be parallel to each other, each wave velocity layer is recorded as the first wave velocity layer 1-1, the second wave velocity layer 1-2, and the third wave velocity layer 1-3 from the upper side to the lower side in the direction perpendicular to the wave velocity layer. The wave velocity of the rock mass in each layer is denoted as V 1 ,V 2 ,V 3 Set up a three-dimensional Cartesian coordinate system with the O point in the rock mass re...
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