地质雷达在活动断裂探测中的应用与进展

张迪; 李家存; 吴中海; 任丽丽

地质雷达在活动断裂探测中的应用与进展

1.
河南工程学院土木工程学院, 郑州 451191
2.
首都师范大学资源环境与旅游学院, 北京 100048
3.
中国地质科学院地质力学研究所, 北京 100081

基金项目:

中国地质调查局地质调查工作项目“长江经济带活动构造与区域地壳稳定性调查” 121201104000150010

煤化工资源综合利用与污染治理河南省工程实验室开放基金资助项目 502002-B01

详细信息

作者简介:
张迪(1987-), 男, 博士, 讲师, 主要从事激光和探地雷达相互结合应用研究。E-mail:zhangdi1987228@163.com

通讯作者:
李家存(1974-), 男, 博士, 副教授, 主要从事遥感技术应用与研究。E-mail:lijiacun@163.com

中图分类号: P546;P627
计量
- 文章访问数: 228
- HTML全文浏览量: 112
- PDF下载量: 24
- 被引次数: 0
出版历程
- 收稿日期: 2016-04-13
- 刊出日期: 2016-09-01

APPLICATION AND PROGRESS OF GROUND PENETRATING RADAR IN ACTIVE FAULT DETECTION

1.
College of Civil Engineering, Henan Institute of Engineering, Zhengzhou 451159, China
2.
College of Resource Environment and Tourism, Capital Normal University, Beijing 100048, China
3.
Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China

摘要

摘要: 结合国内外最新研究成果，对地质雷达技术在活动断裂探测中的应用进行了系统分析和总结，重点对地质雷达在城市活断层探测、古地震探测和断层识别方法的研究现状进行了阐述，并结合理塘活动断裂的应用实例进行评述。最后，提出了地质雷达探测活动断裂现存的问题，对该技术探测活动断裂的发展方向和应用前景进行了展望。
- 地质雷达 /
- 活动断裂 /
- 城市活断层 /
- 古地震 /
- 图像解译
Abstract: Combining with the recent research at home and abroad, the application of Ground Penetrating Radar in active fault detection was summed up and concluded. Three aspects on the application of GPR in active fault detection were put forward and reviewed:the application of GPR in urban active fault, the application of GPR in paleoearthquake and the interpretation of fault in the GPR profile, and an example of the method was illustrated to demonstrate the effectiveness of GPR method in Litang active. Finally, the existing problems of the application of GPR in active fault detection was put forward, and the direction of development and the prospect of this technology were also denoted.
- Ground Penetrating Radar /
- active fault /
- urban active fault /
- paleoearthquake /
- data interpretation

HTML全文

图 1 地质雷达工作原理示意图

Figure 1. The principle of ground penetrating radar

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图 2 收发共置天线对反射测量方式及雷达图像

Figure 2. The common-offset reflection survey and GPR profile

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图 3 宽角测量方式

Figure 3. The wide-angle reflection survey

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图 4 透射探测的方式及成像剖面示意图

Figure 4. Illustration of a transillumination multioffer gather

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图 5 Uemachi断裂二维剖面图^[22]

Figure 5. The 2D profiles of the Uemachi fault

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图 6 Christchurch city浅层地表二维雷达图像^[26]

Figure 6. The profiles of GPR in Christchurch city

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图 7 Sandhwal Village地区处理后频率为200 MHz的2D和3D地质雷达图像^[34]

Figure 7. Processed 2D and 3D GPR profiles collected using 200 MHz antenna across the HF2 scarp at Sandhwal Village

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图 8 研究区位置和地貌概况

Figure 8. Location and geomorphologic environment

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图 9 地质雷达断裂区的二维解译图像

Figure 9. The interpreted of GPR profiles (Heni)

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图 10 三维雷达图像显示

Figure 10. The 3D GPR profile

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