基于综合物探技术的高丽营地裂缝活动特征及成因分析

刘岩; 葛志广; 商晓旭; 林忠伟; 张博媛; 逯朋雷

doi:10.20265/j.cnki.issn.1007-2993.2025-0018

基于综合物探技术的高丽营地裂缝活动特征及成因分析

doi: 10.20265/j.cnki.issn.1007-2993.2025-0018

1.
中兵勘察设计研究院有限公司，北京　100053
2.
中材地质工程勘查研究院有限公司，北京　100102

详细信息

作者简介:
刘　岩，男，1986年生，大学本科，工程师，主要从事岩土工程勘察、地质灾害危险性评估与勘查等方面工作。E-mail：33062017@qq.com

中图分类号: P631
计量
- 文章访问数: 19
- HTML全文浏览量: 4
- PDF下载量: 3
- 被引次数: 0
出版历程
- 收稿日期: 2025-01-11
- 修回日期: 2025-04-17
- 录用日期: 2025-04-18
- 刊出日期: 2025-08-08

Activity characteristics and cause analysis of Gaoliying ground fissures based on comprehensive geophysical exploration technology

1.
China Ordnance Industry Survey and Geotechnical Institute Co., Ltd., Beijing 100053, China
2.
CNBM Geological Engineering Exploration Academy Co., Ltd., Beijing 100102, China

摘要

摘要: 通过高密度电法、面波法对北京市顺义区高丽营镇某地裂缝进行综合地球物理勘探，结合槽探揭露验证，综合分析地裂缝发育特征及其成因。研究结果显示该区域地下20 m以内存在电阻率及横波波速异常，表明存在地裂缝。经过探槽验证，揭露F₁、F₂两条断层位于高丽营断裂带北西侧，与主断裂带距离约4 km，与黄庄—高丽营断裂高丽营段特征一致，推断地裂缝为黄庄—高丽营断裂的最新活动所产生，为构造成因和地面沉降成因引起的复合型地裂缝。
- 高密度电法 /
- 瑞雷波法 /
- 地裂缝 /
- 黄庄—高丽营断裂
Abstract: Comprehensive geophysical exploration was conducted on ground fissures in Gaoliying, Shunyi District, Beijing using high-density electrical method and surface wave method. Combined with trenching construction, the development characteristics and causes of the ground fissures were analyzed comprehensively. The research results show that there are anomalies in resistivity and shear wave velocity within 20 meters underground in the area, indicating the presence of ground fissures. After trench exploration verification, it was revealed that the F₁ and F₂ faults are located on the northwest side of the Gaoliying fault zone, about 4 km away from the main fault zone, consistent with the characteristics of the Gaoliying section of the Huangzhuang-Gaoliying fault. It is inferred that the ground fissures are the latest activity of the Huangzhuang-Gaoliying fault and are a composite type of ground fissures caused by structural and ground subsidence factors.
- high density electrical method /
- Rayleigh wave method /
- ground fissure /
- Huangzhuang-Gaoliying fault

HTML全文

图 1 研究区地裂缝发育情况

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图 2 高密度电法测线布置图

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图 3 面波测线布置图

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图 4 L₁线高密度电法反演剖面图

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图 5 L₂线高密度电法反演剖面图

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图 6 D₁线面波反演剖面图

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图 7 D₂线面波反演剖面图

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图 8 探槽北东壁F₁断层

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图 9 探槽南西壁F₂断层

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