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本矿床是无产阶级文化大革命中,714队在秦岭地区首次发现的大型菱铁矿、多金属矿床。三年来,在毛主席革命路线的指引下,紧密结合生产实际,深入调查研究,进行了一些科学研究工作,对矿床的矿石物质组分、含矿岩系及其岩相变化等方面取得了一定的研究成果。现就矿床成矿地质特征进行探讨,不当之处,请批评指正。一、区域地质概述
This deposit is a large siderite and polymetallic deposit first discovered by the 714 team in the Qinling Mountains during the Great Proletarian Cultural Revolution. In the past three years, under the guidance of Chairman Mao’s revolutionary line, a number of scientific research work has been carried out in close connection with actual production, in-depth investigation and research, and certain achievements have been made in the ore composition, ore-bearing rock series and lithofacies changes in the ore deposits Research results. Now on the geological characteristics of mineral deposits to explore, inappropriate, please comment on criticism. First, an overview of regional geology