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用于多跨孔研究和跨孔地震勘探多传感器设置的三维逆时偏移成像

3D Reverse-Time Migration Imaging for Multiple Cross-Hole Research and Multiple Sensor Settings of Cross-Hole Seismic Exploration.

作者信息

Cheng Fei, Peng Daicheng, Yang Sansheng

机构信息

Hubei Key Laboratory of Marine Geological Resources, China University of Geosciences, Wuhan 430074, China.

Key Laboratory of Exploration Technologies for Oil and Gas Resource, Ministry of Education, Yangtze University, Wuhan 430100, China.

出版信息

Sensors (Basel). 2024 Jan 26;24(3):815. doi: 10.3390/s24030815.

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 responses from geological bodies in 3D space and are potentially affected by objects outside the well profiles, distorting the imaging results and geological interpretation. This paper proposes a 3D cross-hole acoustic wave reverse-time migration imaging method to capture 3D cross-hole geological structures using sensor settings in multi-cross-hole seismic research. Based on the analysis of resulting 3D cross-hole images under varying sensor settings, optimizing the observation system can aid in the cost-efficient obtainment of the 3D underground structure distribution. To verify this method's effectiveness on 3D cross-hole structure imaging, numerical simulations were conducted on four typical geological models regarding layers, local high-velocity zones, large dip angles, and faults. The results verify the model's superiority in providing more reliable and accurate 3D geological information for cross-hole seismic exploration, presenting a theoretical basis for processing and interpreting cross-hole data.

摘要

与地面地震勘探相比,二维(2D)跨孔地震计算机断层扫描(CT)成像采集方法有可能对目标区域进行最佳表征。它在石油和天然气勘探、工程地质等领域有广泛应用。限于二维孔速度剖面,该方法无法获取剖面外横向地质结构的三维(3D)信息。此外,跨孔地震勘探接收到的传感器数据构成三维空间中地质体的响应,并可能受到井剖面外物体的影响,从而使成像结果和地质解释失真。本文提出一种三维跨孔声波逆时偏移成像方法,利用多跨孔地震研究中的传感器设置来获取三维跨孔地质结构。基于对不同传感器设置下所得三维跨孔图像的分析,优化观测系统有助于经济高效地获取三维地下结构分布。为验证该方法对三维跨孔结构成像的有效性,针对层、局部高速区、大倾角和断层四种典型地质模型进行了数值模拟。结果验证了该模型在为跨孔地震勘探提供更可靠、准确的三维地质信息方面的优越性,为跨孔数据的处理和解释提供了理论依据。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/7141/10856999/e26dfe6bfc50/sensors-24-00815-g001.jpg

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