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应用地球物理  2020, Vol. 17 Issue (1): 37-53    DOI: 10.1007/s11770-020-0808-8
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喀斯特地区煤田多孔联采3D-RVSP 勘探实践:以中国五轮山为例*
胡明顺1,2,潘冬明1,周福宝2,李娟娟3,王扬州4,陈圣恩5,许永忠1
1. 资源与地球科学学院,中国矿业大学,江苏徐州 221116;
2. 煤矿瓦斯与火灾防治教育部重点实验室,中国矿业大学,江苏徐州 221116;
3. 感知矿山物联网研究中心,中国矿业大学,江苏徐州 221116;
4. 应用地球物理研究所,兖矿集团有限公司,山东兖州 273500;
5. 土木与环境工程系,美国北卡罗莱纳大学夏洛特分校,美国夏洛特 28223
Multi-hole joint acquisition of a 3D-RVSP in a karst area: Case study in the Wulunshan Coal Field, China*
Hu Ming-Shun 1,2, Pan Dong-Ming?1, Zhou Fu-Bao 2, Li Juan-Juan 3, Wang Yang-Zhou 4,Chen Shen-En 5, and Xu Yong-Zhong 1
1. School of Resource and Geosciences, China University of Mining and Technology, Xuzhou 221116, China.
2. Key Laboratory of Gas and Fire Control for Coal Mines, CUMT, Xuzhou 221116, China.
3. IoT Perception Mine Research Center, China University of Mining & Technology, Xuzhou 221116, China.
4. Institute of Applied Geophysics, Yankuang Group Company limited, Zoucheng 273500, China.
5 Department of Civil and Environmental Engineering, University of North Carolina at Charlotte, Charlotte 28223, USA.
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摘要 喀斯特地貌等复杂地表地区的常规地震勘探一直面临着激发和接收条件差的难题。RVSP(Reverse Vertical Seismic Profile)地震勘探采用井中激发、地面接收的观测方式,能够一定程度上减少复杂地表对地震波传播的影响。本文通过数值模拟和实际资料分析指出:在岩溶发育的喀斯特地貌等复杂地表地区,浅层激发的地震波受各种多次波、面波和岩溶地质体的散射干扰作用,反射地震数据品质极低,且难以通过去噪方法提高信噪比。当加大激发深度,避开浅表层复杂地质体时,能够提高反射波品质。RVSP 方法采用井中激发,正好具有上述潜在优势。根据其观测系统的特殊性,利用有效反射波与大部分干扰波存在的视速度差异进行滤波可进一步提高反射波信噪比。本研究在典型的喀斯特地貌地区开展了8 孔联采3D-RVSP 勘探研究,结果表明:在岩溶发育的复杂地表条件地区,3D-RVSP观测能够获得较高质量的反射地震资料;采用多孔联采的3D-RVSP 方式,具有数据采集效率高、改善地下覆盖均匀性的特点;获得的成像结果分辨率高,能够对细小断裂构造进行精细刻画。
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关键词喀斯特   复杂地表   地震响应   3D-RVSP   多孔联采     
Abstract: Conventional surface seismic exploration in areas with complex surfaces such as karst landforms has been faced with the problem of poor excitation and reception conditions. RVSP (reverse vertical seismic profile) seismic exploration adopts a geometry in which the sources are downhole and receivers are on the ground which can reduce the influence of complex surfaces on seismic wave propagation (to some extent). Through numerical simulations and real data analysis, it was noted that in areas with complex surfaces and large numbers of underground karst caves, seismic waves generated in shallow boreholes are easily affected by various surface and multiple waves as well as by scattering from karst bodies. Therefore, the quality of the reflected seismic data is extremely low. Also, it is difficult to improve the signal to noise ratio (SNR) with conventional noise fi ltering methods. However, when the source depth is increased, the quality of the refl ected waves can be improved. This is exactly what the RVSP method accomplishes. Besides, for the RVSP method, due to its particular geometry, the apparent velocities of the reflected waves and most interference waves are quite diff erent, which can help to fi lter most noise to further improve the SNR of the refl ected signals. In this study, a 3D-RVSP exploration study using 8-hole joint acquisition was conducted in a typical karst landform. The results show that the 3D-RVSP method can obtain higher quality seismic data for complex surface conditions that have large numbers of underground karst caves. Furthermore, multi-hole joint acquisition for 3D-RVSP has higher data collection efficiency and better uniformity of underground coverage. Therefore, in this study, 38 faults were accurately revealed and at high resolution based on the 3D-RVSP imaging results
Key wordsKarst   Complex surface   Seismic response   3D-RVSP   Multi-hole joint acquisition   
收稿日期: 2019-08-07; 出版日期: 2020-09-04
基金资助:

本研究项目由国家重点研发计划项目(编号:2017YFC0804105),江苏省自然科学基金项目 (编号:BK20160245),中央高校基本科研业务项目 (编号:2015XKMS036)和江苏省优势学科资助项目提供科研经费联合资助。

通讯作者: 潘冬明 (E-mail:pdm3816@163.com)      E-mail: pdm3816@163.com
作者简介: 胡明顺,博士,讲师,硕士生导师,SEG 和中国地球物理学会会员。2013 年12 月毕业于中国矿业大学地质资源与地质工程专业,获工学博士学位,2011.8-2013.8 国家公派美国University of North Carolina at Charlotte 联合培养博士。2014 年至今就职于中国矿业大学地球物理系,主要从事井孔地震数据采集、处理和成像理论及应用研究。E-mail: mhu3@cumt.edu.cn.
引用本文:   
. 喀斯特地区煤田多孔联采3D-RVSP 勘探实践:以中国五轮山为例*[J]. 应用地球物理, 2020, 17(1): 37-53.
. Multi-hole joint acquisition of a 3D-RVSP in a karst area: Case study in the Wulunshan Coal Field, China*[J]. APPLIED GEOPHYSICS, 2020, 17(1): 37-53.
 
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[1] 李建国,崔晓杰,黄建华,张晓璐,李彦鹏. 复杂地表变偏移距VSP角度域旅行时层析及叠前深度偏移*[J]. 应用地球物理, 2019, 16(3): 358-366.
[2] 贺芙邦, 游俊, 陈开远. 基于岩石物理分析的叠前弹性反演预测含气砂岩分布[J]. 应用地球物理, 2011, 8(3): 197-205.
[3] 岳玉波, 李振春, 张平, 周学锋, 秦宁. 复杂地表条件下高斯波束叠前深度偏移[J]. 应用地球物理, 2010, 7(2): 143-148.
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