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该矿床原是一个航测异常点,经多年工作,现已成为一个工业矿床。本文从水文地球化学角度,对矿床形成,谈几点认识。一、地质概况矿床位于褶皱隆起带西侧,一个向斜南东翼。出露地层有:震旦系、寒武系和石炭系。地层产状:倾向240—320°、倾角10°±(图1)。矿床主要在震旦系灯影组中段(Zbdn~2)的硅质页岩夹硅质白云岩中,也是矿区第二含水层。
The deposit was originally an abnormal point of aerial survey. After many years of work, it has now become an industrial deposit. This article from the hydrogeochemistry point of view, the formation of the deposit, talk about some understanding. First, the geological overview Deposits located in the western fold fold uplift, a southwest wing of the syncline. Exposed strata are: Sinian, Cambrian and Carboniferous. Stratigraphy: inclination 240-320 °, inclination 10 ° ± (Figure 1). The deposit is mainly in siliceous shale intercalated siliceous dolomite in the middle part of Sinian Dengying Formation (Zbdn ~ 2), which is also the second aquifer in the mining area.