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1地质概况王仙岭岩体位于湖南省郴州市东南约10km处,出露面积约20km2,北大南小,大致呈倒葫芦状NNE向展布,侵入泥盆系和石炭系碳酸盐岩。晚侏罗世千里山岩体位于其东约2km处。两个岩体之间发育了一系列近平行的NE-NNE向花岗斑岩脉。王仙岭岩体云英岩化发育,在岩体与围岩接触带上主要发育大理岩化、夕卡岩化等蚀变。大型荷花坪锡多金属矿床位于王仙岭岩体
1 Geological Survey Wang Xianling rock mass is located about 10km southeast of Chenzhou City, Hunan Province. The exposed area is about 20km2. North Da Nannan is small and shows a gourd-like NNE distribution that intrudes into the Devonian and Carboniferous carbonate rocks. The Late Jurassic Chilishan Massif is located about 2km east of it. A series of near-parallel NE-NNE granitic porphyry veins were developed between two rock masses. The Wangxianling pluton is characterized by marbling, with the main development of marbleization and skarnization on the contact zone between the rock mass and the surrounding rock. Large lotus Ping tin polymetallic deposits located in Wang Xianling rock mass