摘要
通过对天等把荷锰矿地质构造、赋矿层位、矿体特征、矿石特征等论述，认为把荷锰矿属于沉积―氧化型矿床，除了正常海相沉积，矿区的地层、岩性、沉积―构造环境、气候和地貌等条件均对成矿有一定的影响，分析此类锰矿床的地质特征以及成因，对寻找类似锰矿床具有一定的指导意义。
Abstract
Based on geological structure,ore-bearing horizon and characteristics of orebodies and ores of Bahe manganese deposit in Tiandeng,it is believed that Bahe manganese deposit is a sedimentary oxidation depos-it.Beside the normal marine sediments,conditions like stratigraphy,lithology,sedimentary-tectonic envi-ronment,climate and topography of the mining area have effects on mineralization.It is of great guiding sig-nificance in searching for similar manganese deposits to analyze the geological characteristics and genesis of this manganese deposit.
NETL
NSTL
维普
万方数据