淮南矿区岩溶发育特征及其富水规律  

The karst development characteristic and the water abundance regular in Huainan mine area

作　　者：李小明[1,2] 朱丽[1] 李永军[1] 杨希培[1] 

机构地区：[1]华北科技学院,北京东燕郊101601 [2]中国矿业大学煤炭资源与安全开采国家重点实验室,北京100083

出　　处：《华北科技学院学报》2010年第1期8-11,22,共5页Journal of North China Institute of Science and Technology

基　　金："973计划"(2006CB202208);华北科技学院优秀人才科研启动基金(A08002)

摘　　要：本文在对淮南矿区奥陶系发育、分布特征分析的基础上,探讨了奥灰岩富水性规律与奥灰岩性、岩溶发育和分布及充填情况、裂隙发育情况及构造(主要为断层)之间的相关关系,初步揭示了奥灰岩的富水规律,为系统研究淮南矿区奥陶系岩溶发育规律和矿井奥灰水的防治提供了理论依据。In this paper, the dependence relation, between the water abundance regular of Ordovieian limestone and lithology , the karst development characteristic, distributing, the filling situation, the fissure development characteristic, the tectonic （ the fault is primary） ,is discussed, based on analysis to the development and distributing of 0rdovieian system in Huainan mine area. The wa- ter abundance regular of Ordovician limestone is disclosed primarily, and it provides the theory basis for studying systematically the karst development regular in Ordovician and the prevention of Ordovician karst water of mine in Huainan mine area

关 键 词：淮南矿区 奥灰岩溶 富水规律 奥灰水防治 

分 类 号：TD741[矿业工程—矿井通风与安全]