煤炭工程 ›› 2013, Vol. 45 ›› Issue (8): 75-78.doi:

• 研究探讨 • 上一篇    下一篇

补连塔矿12406工作面浅部地层结构地质雷达探测研究

聂俊丽   

  1. 贵州大学
  • 收稿日期:2013-03-29 修回日期:2013-06-08 出版日期:2013-08-10 发布日期:2013-08-10
  • 通讯作者: 聂俊丽 E-mail:niejunli451@sohu.com

Stratification Explore on 12406 Face of Bulianta mine by GPR

  • Received:2013-03-29 Revised:2013-06-08 Online:2013-08-10 Published:2013-08-10

摘要: 利用地质雷达对浅地表地层进行精细探测的优势,对补连塔矿12406工作面进行地质雷达探测,根据雷达相将该研究区地层分为5种不同类型。结合钻孔资料划分了该工作面浅部地层的详细地层结构,得到了沿测线的沉积结构图,可为矿区生态复垦提供基础资料。探测结果表明:浅地表松散层厚度差异大;地质雷达在测线1200-1500m范围的砂层沉积区探测效果良好,有效信号可达10m,可识别粗砂、中砂、细砂分界面;存在粘土(基岩风化产物)和砾石层的区域,雷达探测深度较浅;分别与粘土和砾石层深度对应,深度均小于10m,有些仅厚几十厘米。

关键词: 地质雷达, 钻孔, 地层

Abstract: The geological strata of the 12406 face, Bulianta mine was detected by GPR that has the advantage of a fine probing for shallow surface layers. According to the radar face, the stratification of the study area is divided into five different types. Combined the borehole data with the GPR profile, sedimentary structures along the survey line was obtained, which would be basic data for mine ecological reclamation. The detection results show that: the thickness of shallow loose layer is different sharply. The GPR wave probing is deeper in all sand layers than other loose layers. GPR detection was good in survey line 1200-1500m range sand layer deposition and the effective signal was up to 10m. The interface of coarse sand, medium sand or fine sand can be identified. The GPR detection depth is shallow in clay (sandstone weathering products) and gravel area; depth, which is corresponding with the deep of clay and gravel and shallower than 10m, some only a few tens of centimeters thick.

Key words: ground penetrating radar, drilling bore hole, stratification