霍邱金安铁矿水文地质条件初步研究  

Preliminary Study on Hydrological Conditions of Jin'an Iron Ore Deposit of Huoqiu County

作　　者：谭绿贵[1] 张广胜[1] 王本伟[2] 汪万芬[1] 刘忠[1] 

机构地区：[1]皖西学院资源环境与旅游管理学院 [2]六安市国土资源局

出　　处：《皖西学院学报》2012年第5期49-54,共6页Journal of West Anhui University

基　　金：安徽省高校省级自然科学研究重点项目(KJ2012A281);安徽省人文地理学重点学科资助项目

摘　　要：霍邱铁矿田地处淮河流域中上游冲积平原Ⅱ级阶地地貌单元,系华东地区第一大铁矿床。金安铁矿位于霍邱铁矿田的中部,行政区划隶属于六安市霍邱县范桥乡,是一个水文地质条件较为复杂的沉积变质型铁矿床。依据矿床含水层剖面可划分为新生水、古壳水和基含水。矿区西高东低,地下水径流方向应为自矿床西向东流动。矿床地下水补给来源,特别是新生水的补给来源主要应为入渗到含水层的大气降水。金安铁矿地下水的径流途径主要有:(1)地表水体侧向渗入;(2)塌陷裂隙渗入;(3)断层破碎带进入;(4)可通过矿井排水孔或勘探时未封闭的钻孔直接进入地下含水层。矿床地下水的排泄则主要是矿井抽水,其次是位于矿区南部的泉水出露。Huoqiu iron ore field which is locaded in the Ⅱ terrace unit of the alluvial plain in upper and middle reaches ot Huaihe river basin is the largest iron deposit in east China. Jin＇an iron deposit is a sedimentary-metamgrphic type deposit whom hydrogeological conditions are complicated, which is situated the central section of Huoqiu ore field, its administrative division belong to Fanqiao township of Huoqiu county in Lu＇an city. The aquifer profile can be divided into Xinsheng water, Guqiao water and Jiyan water, according to the characteristics of ore deposit. The runoff flow direction of groundwater of the deposit is from west to east because of mining area of west high east end. The recharge source of the deposit groundwater is mainly atmospheric precipitation which is infiltration into the aquifer stratum. The flow path of runoff of groundwater in Jin＇an iron deposit mainly includes that the surface waters laterally infiltrates, groundwater infiltrating collapse fissure, broken fault zone in, and so on. The groundwater discharge of the deposit mainly may be mine pumping, secondly, the exposed spring which is locaded in the southern area of mining.

关 键 词：水文地质条件 矿床地下水 金安铁矿床 安徽省 

分 类 号：P641.6[天文地球—地质矿产勘探]