重庆市巫山县邓家铁矿水文地质特征  

The Hydrogeological and Geological Characteristics of Dengjia iron mine in Wushan County of Chongqing

作　　者：郭锐[1] 罗明伟[1] 赵涛[1] 杜春阳[1] 付恒一[1] 

机构地区：[1]河南省地质矿产勘查开发局第二地质勘查院,河南许昌461000

出　　处：《资源导刊（地球科技版）》2014年第9期33-35,38,共4页

摘　　要：通过对重庆市巫山县邓家铁矿水文地质条件的分析指出：矿区含水层对矿床未来开发的影响较轻，但矿床主要充水类型——岩溶裂隙一溶洞（暗河）则是影响矿床开采的主要因素；而断裂构造不仅是连接含水层，也是沟通岩溶水相互联系的重要媒介，也是不可忽视的重要影响因素。by geological condition analysis on Dengjia iron mine, it was stated that the aquifers in the mining area has a minor effect on the future development of mineral deposits. However, the fissure water filling deposit type-karst fissure-karst cave will cause major impact to mining of the mineral deposits. Besides, the faulted structure not only serve to connect the aquifers and also serve as an important medium connecting the karst water and has to be considered as important factor to cause the impact on future development of mineral deposits.

关 键 词：铁矿 含水层 水文地质特征 重庆巫山 

分 类 号：TD745.2[矿业工程—矿井通风与安全]