摘要
热释汞在独山锑矿区的找矿试验表明,凡有矿(化)的地段均有各相态汞异常显示,异常峰值基本能与矿(化)体对应,平面上异常形态能反映矿(化)体产出特征,剖面上异常发育状况可作为判断别近矿、远矿以及剥蚀程度的标志。该方法成本低,找矿效果显著。
The experiment of exploring mineral in Dushan stlbimn area showed that in all mineralized areas,there is an ＂abnormal sign of differently stated mercury,The abnormal sununt value roughly corresponds to the mineraaized matter.The features of mineralized matter formed are illustrated in plane and abnomally developed state in section can be a mark to judge where the mineral locates and its state,close or remote or denuded.The method costs low but produces remarkable efficiency in exploring the mineral.
出处
《遵义师范学院学报》
2007年第3期59-61,共3页
Journal of Zunyi Normal University
关键词
热释汞
相态汞
剥蚀程度
releasing mercury
by heating
stated mercury
denudation extent.
作者简介
李赞，男，贵州大方人，贵州省有色地勘局三总队地质工程师。
