摘要
利用钻孔彩色电视系统观测了大量钻孔内部原生裂隙以及采动岩体裂隙的分布及其发育特点.研究得出原生裂隙场具有绝大多数发育横向微裂隙,裂隙被充填物所充填以及部分发育纵向裂隙,较破碎的特点;采动岩体裂隙则具有发育纵横交错的相交裂缝,以高角度纵向裂缝为主,且随着离煤层顶板距离减小,并逐步向破碎型裂缝发展的特点.
Fissure distributing and development characteristic in hole were detected by use of borehole television. The results show that the original fissure field has characteristics such as the horizontal development of microcracks, fissures were fill with filling material, as well as part of the development of vertical cracks, broken. The rock fissures has characteristics such as the intersection cracks in high-angle vertical, and along with reducement of the distance from the roof, gradually development to the broken cracks.
出处
《煤炭学报》
EI
CAS
CSCD
北大核心
2008年第11期1216-1219,共4页
Journal of China Coal Society
基金
国家重点基础研究发展计划(973)基金资助项目(2005CB221503)
关键词
采动岩体
裂隙场
可视化探测
钻孔电视
rock mass
fissure field
visual exploration
borehole television