2024
DOI: 10.3390/s24030815
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3D Reverse-Time Migration Imaging for Multiple Cross-Hole Research and Multiple Sensor Settings of Cross-Hole Seismic Exploration

Fei Cheng,
Daicheng Peng,
Sansheng Yang

Abstract: The two-dimensional (2D) cross-hole seismic computed tomography (CT) imaging acquisition method has the potential to characterize the target zone optimally compared to surface seismic surveys. It has wide applications in oil and gas exploration, engineering geology, etc. Limited to 2D hole velocity profiling, this method cannot acquire three-dimensional (3D) information on lateral geological structures outside the profile. Additionally, the sensor data received by cross-hole seismic exploration constitute resp… Show more

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Cited by 2 publications
(2 citation statements)
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“…Tests of the rock massif were carried out using seismic methods, namely shallow refraction seismic and seismic crosshole tomography as a non-destructive method [7], and based on the value of the speed of propagation of P and S waves, the wear, fracture and width of the crack systems of the rock massif were measured. Due to its practicality, the crosshole tomography method has been widely used in many economic branches, including tunnel construction [8]. The tests were carried out in two phases:…”
Section: Figure 7 Spatial Location Of Investigation Boreholes On the ...mentioning
confidence: 99%
“…Tests of the rock massif were carried out using seismic methods, namely shallow refraction seismic and seismic crosshole tomography as a non-destructive method [7], and based on the value of the speed of propagation of P and S waves, the wear, fracture and width of the crack systems of the rock massif were measured. Due to its practicality, the crosshole tomography method has been widely used in many economic branches, including tunnel construction [8]. The tests were carried out in two phases:…”
Section: Figure 7 Spatial Location Of Investigation Boreholes On the ...mentioning
confidence: 99%
“…As a result, the utilization rate of spatial well locations remain relatively low. Furthermore, the 2D cross-well CT imaging technique can only provide information on the geological structure of the profile between the two wells, failing to capture the lateral structure information of the profile [27]. As a result, the imaging provides poor lateral continuity, hindering the evaluation of 3D geological structures.…”
Section: Introductionmentioning
confidence: 99%