| 河南水洞岭块状硫化物型铜锌矿床特征及成矿模式探讨 |
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| 引用本文： | 张文博,左娅,杨贺杰,王宏勋.河南水洞岭块状硫化物型铜锌矿床特征及成矿模式探讨[J].科技信息,2011(33):I0002-I0004. |
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| 作者姓名： | 张文博 左娅 杨贺杰 王宏勋 |
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| 作者单位： | 河南省地质矿产局第三地质大队,河南郑州450016 |
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| 摘 要： | 水洞岭矿床属秦岭一大别山碰撞带东秦岭构造亚带，该矿床产于早古生界二郎坪群酸性火山岩内，并受水洞岭复向斜东北翼控制。矿体赋存在石英角斑凝灰岩中，呈似层状、透镜状产出，与地层产状一致。通过对矿床地质特征，进一步总结其成矿机制，建立水洞岭块状硫化物型铜锌矿床的成矿模式。
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| 关 键 词： | 块状硫化物 铜锌矿床 控矿因素 富集规律 成矿模式 水洞岭 河南 |
Characteristics and the Metallogenic Model of the Shuidongling Massive Sulfide Type Cu-Zn Deposit in Henan |
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| ZHANG Wen-bo,ZUO Ya,YANG He-jie,WANG Hong-xun.Characteristics and the Metallogenic Model of the Shuidongling Massive Sulfide Type Cu-Zn Deposit in Henan[J].Science,2011(33):I0002-I0004. |
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| Authors: | ZHANG Wen-bo ZUO Ya YANG He-jie WANG Hong-xun |
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| Institution: | (No.3 Geological Brigade of Henan Provincial Non-- ferrous Metals Geological and Mineral Resources Bureau, Zhengzhou Henan, 450016,China) |
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| Abstract: | Shuidongling deposit is tectonically located in Qinling-Dabie orogenic belt, in the East Qinling Mountains tectonic subbeh. The deposit is occurred in the early Paleozoic Edangping group acidic volcanic rocks, and controlled by the northeast wing of the Shuidongling compound syneline. The orebodies of the deposit occurred in quartz keratophyric tuff with their occurrence being stratiform--like state and lens, which is accordance with the strata occurrence. According to ore geology, establish a metallogenic model of the massive sulfide type copper smelting ridge bed of. |
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| Keywords: | Massive sulfide Cu--Zn deposit Ore-controlling factor Regularity of mineralization Metallogenic model Shuidongling |
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