化工矿产地质
化工礦產地質
화공광산지질
Geology of Chemical Minerals
2015年
3期
144-148
,共5页
磐石铜矿%水文地质特征%侵蚀基准面%充水因素%涌水量
磐石銅礦%水文地質特徵%侵蝕基準麵%充水因素%湧水量
반석동광%수문지질특정%침식기준면%충수인소%용수량
Panshi copper mine%hydrogeological feature%erosion base level%water filling factors%water yield
磐石石咀铜矿位于吉林省中南部磐石-明城背斜的东翼,区内经历了多期多阶段构造运动.矿体赋存于石咀子组大理岩、硅质条带大理岩中,岩石溶隙、溶洞较发育,地质条件复杂.从矿区水文地质特征、地下水补迳排关系、矿坑充水因素等要素入手,综合分析坑道涌水特点、涌水规律,并预测其涌水量,指导矿山水文地质工作.
磐石石咀銅礦位于吉林省中南部磐石-明城揹斜的東翼,區內經歷瞭多期多階段構造運動.礦體賦存于石咀子組大理巖、硅質條帶大理巖中,巖石溶隙、溶洞較髮育,地質條件複雜.從礦區水文地質特徵、地下水補逕排關繫、礦坑充水因素等要素入手,綜閤分析坑道湧水特點、湧水規律,併預測其湧水量,指導礦山水文地質工作.
반석석저동광위우길림성중남부반석-명성배사적동익,구내경력료다기다계단구조운동.광체부존우석저자조대리암、규질조대대리암중,암석용극、용동교발육,지질조건복잡.종광구수문지질특정、지하수보경배관계、광갱충수인소등요소입수,종합분석갱도용수특점、용수규률,병예측기용수량,지도광산수문지질공작.
The Shizui copper mine of Panshi is located at the east limb of Mingcheng anticline in Jilin province. It has undergone multi-stage tectonic movements. The ore bodies occur in marble and Siliceous bands marble of Shizuizi Formation. The solution fissure and karst cave developed well in rock, and the geological condition is complex. According to the hydrogeological feature, the groundwater recharge, flow and discharge relationship as well as mining water filling factors, we analysed the feature and the law of tunnel water gushing synthetically and predicted the water yield in order to guide the hydrogeological work.
