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阳春盆地是在印支期复向斜基础上发育而成的小型断陷盆地,是粤西乃至广东省重要的有色金属成矿区之一,目前盆地周边已发现矿床(点)50余处,矿化元素为铜铁铅锌钨锡等(蔡明海,2001;赵海杰,2012;郑伟,2013)。锡山矿床位于阳春复式向斜的西南端,矿区地处广东省阳春市马水镇辖区内,位于阳春市204°方向,直距14.75 km处,矿区中心点地理坐标为东经111°38′15″,北纬22°07′50″,岩体周围地层为石炭系下统的
The Yangchun basin is a small faulted basin developed on the Indosinian syncline and is one of the important non-ferrous metal mineralization areas in western Guangdong and Guangdong Province. At present, more than 50 deposits (spots) have been found in the periphery of the basin. The chemical elements are copper, iron, lead, zinc, tungsten and tin (Cai Minghai, 2001; Zhao Haijie, 2012; Zheng Wei, 2013). The Xishan deposit is located in the southwestern end of the Yangchun double syncline. The mining area is located in Ma Shui Town, Yangchun City, Guangdong Province. It is located at the direction of 204 ° in Yangchun with a straight-line distance of 14.75 km. The geographical coordinates of the mining center are 111 ° 38’15 “ , Latitude 22o 07’50 ”, the strata around the rock mass are under the Carboniferous