江西沉积变质型铁矿矿床水文地质特征的研究

Study of hydrogeological characteristics of metamorphosed sedimentary type iron ore in Jiangxi

沉积-变质型(新余式)铁矿为江西最重要的铁矿类型。铁矿主要分布江西中部,西起萍乡南坑,经分宜松山、安福杨家桥,新余良山,东至弋阳县洪山,近东西向长达350km。共划分六个矿田,其中新余矿田的良山、太平山、寨口、下坊、巴丘-花桥、井头、杨家桥、松山等矿区工作程度最高。在地质勘探同时,开展了矿床水文地质、工程地质工作,为矿山开采设计提供依据和资料。为今后科学地开展矿床水文地质勘探提供资料依据。

Metamorphosed sedimentary iron deposit is the most important kind of iron deposit in Jiangxi. The iron deposits mainly distributed in the middle part of Jiangxi,the area of iron deposits is from the west-Nankeng of Pingxiang, passing through Songshan of Fenyi, Yangjiaqiao of Anfu, Liangshan of Xinyu, to the east-Hongshan of Yiyang county. The length is about 350kin based on the east-west strike. The iron deposits can depart from six ore fields, the level of exploitation in the following ore districts is the highest in the Xinyu ore field, such as Liangshan, Taipingshan, Zhaikou, Xiafang, Baqiu-Huaqiao, Jingtou, Yangjiaqiao, Songshan. Along with the geological exploration, we also carried out hydrogeological work and engineering geological work, which not only provided materials and foundation for designing and exploiting of the mines, but also provides materials for the later hydrogeological exploiting of the deposits.