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作 者:商宇航 刘春雨[2] 邰振华 刘世明 杜添添 Shang Yuhang;Liu Chunyu;Tai Zhenhua;Liu Shiming;Du Tiantian(School of Mining Engineering,Heilongjiang University of Science&Technology,Harbin 150022,China;Geophysical Prospecting&Surveying Team,Heilongjiang Bureau of Coal Geological Exploration,Harbin 150001,China)
机构地区:[1]黑龙江科技大学矿业工程学院,哈尔滨150022 [2]黑龙江省煤田地质物测队,哈尔滨150001
出 处:《黑龙江科技大学学报》2020年第1期16-21,共6页Journal of Heilongjiang University of Science And Technology
基 金:国家自然科学基金项目(51604100);哈尔滨市应用技术研究与开发项目(2017RAQXJ054)
摘 要:为探明杨涧煤矿3^#、8^#煤层采空区、富水区、采空积水区的赋存情况,依据岩层电性特征、放射性特征、区域地质、煤层发育等地质-地球物理资料,实施瞬变电磁法和同位素测氡法对测区进行综合勘探。研究表明,通过获得3^#、8^#煤层各测线的视电阻率拟断面图、顺煤层等值线图及氡气浓度分布平面图,可推断3^#、8^#煤层中7处采空区、10处富水区、3处采空积水区的位置。This paper intends to determine the occurrence of mined area,water-rich area,and mined-out water accumulation area of No.3 and 8 coal seam in Yangjing coal mine.The study involves performing the comprehensive exploration of the survey by applying transient electromagnetic method and isotopic radon measurement and using geophysical-geological data such as electrical characteristics,radioactive characteristics,regional geology,and coal seam development;and processing the observed data appropriately and thereby obtaining the apparent resistivity pseudo-sections,contour maps along the coal seam and the radon concentration contours of the survey lines on No.3 and 8 coal seams.The study ultimately deduces the positions of 7 mined-out areas,10 water-rich areas,and 3 mined-out water accumulation areas in above two coal seams.
关 键 词:瞬变电磁法 同位素测氡法 采空区 富水区 采空积水区
分 类 号:P631.3[天文地球—地质矿产勘探]
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