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野鸡尾多金属矿区位于湖南郴州市东南约26km,只p东经113°05′——113°11′,北纬25°42′—25°47′,西与著名的柿竹园钨多金属矿床相邻。计有铅锌、锡、钨、铋、铜等矿带,一起划作野鸡尾岩体型锡多金属矿床。 区内出露的地层主要有泥盆系中上统的跳马涧组碎屑岩(D_(2t))、棋梓桥组(D_(2q))、余田桥组(D_(3s))、锡矿山组(D_(3x))碳酸岩和震旦系下统浅变质石英砂岩及板岩。碳酸岩从早到晚变纯,强度降低。矿区位于岩性不同的碳酸岩与砂岩或板岩接触带。棋梓桥组灰岩因泥质含
Pheasant polymetallic mine is located in the southeast of Chenzhou, Hunan, about 26km, only p longitude 113 ° 05 ’- 113 ° 11’, latitude 25 ° 42’-25 ° 47 ’, west and the famous Shizhuyuan tungsten polymetallic deposit phase adjacent. There are lead, zinc, tin, tungsten, bismuth, copper and other mineral belts, together designated as wild cockroach body type tin polymetallic deposits. The strata exposed in the area are mainly the middle Devonian clastic rocks (D 2t), Cheziziqiao Formation (D_ (2q)), Yudaqiao Formation (D_ (3s)), tin (D_ (3x)) carbonate rocks and the Sinian epithermal metamorphic quartz sandstone and slate. Carbonates are pure from morning to night, reducing their strength. The mine is located on the zone of contact between carbonate and sandstone or slate with different lithologies. Chezi Zi bridge group of limestone due to muddy