首页> 中文期刊> 《价值工程》 >芦子园铅锌矿水文地质条件与地质环境评价

芦子园铅锌矿水文地质条件与地质环境评价

         

摘要

Luziyuan lead zinc mine is one of the major breakthrough deposits of"southwest Sanjiang metallogenic belt"in recent years. The deposit type belongs to the sedimentary transformation - skarn lead-zinc deposit. Since its lead and zinc reserves were proven, hydrology works for this region were increasing and also got some achievements. In this paper, according to the hydro-geological characteristics, (GE) aquifer (Group) division, chemical characteristics of groundwater and the prediction of mine water inflow with water rich coefficient method and water hydrodynamic method in Luziyuan area, the hydro-geological conditions of mining area were elucidated, the geological environment was introduced and evaluated, then the corresponding governance measures were put forward, which provide scientific reference for safety production in mine area.%芦子园铅锌矿是“西南三江成矿带”近年取得的重大突破的矿床之一[1]。矿床类型属沉积改造-矽卡岩型铅锌矿床[2]。自探明其铅锌储量以来,对该区水文地质的工作日益增加,因此也取得了一些成果。本文通过对芦子园矿区的水文地质基本特征、含(隔)水层(组)划分、地下水化学特征以及采用富水系数法和水动力学法对矿坑涌水量进行预测来阐明矿区水文地质条件,并且对矿区地质环境进行介绍和评价,提出相应的治理完善的措施,为矿区内安全生产提供科学依据。

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