| 福建武夷山山口银多金属矿床地质特征及成因分析 |
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| 引用本文： | 王文兵.福建武夷山山口银多金属矿床地质特征及成因分析[J].福建地质,2010,29(2):96-100. |
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| 作者姓名： | 王文兵 |
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| 作者单位： | 福建省地质调查研究院,福州,350013 |
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| 摘 要： | 武夷山山口银多金属矿位于武夷成矿带光泽—宁化铜多金属成矿亚带东北部和浦城—宁德北西向钼多金属成矿带交汇处,矿体贮存于中生代焦坑组中,为沉积改造型矿床,主成矿期为晚三叠世。
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| 关 键 词： | 银多金属矿床 地质特征 沉积改造型 武夷山山口 |
Geological feature of the Shankou Silver polymetallic ore deposit in Wuyishan City, Fujian Province |
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| Wang wenbing.Geological feature of the Shankou Silver polymetallic ore deposit in Wuyishan City, Fujian Province[J].Geology of Fujian,2010,29(2):96-100. |
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| Authors: | Wang wenbing |
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| Institution: | Wang wenbing (Fujian Institute of Geology Survey and Research, Fuzhou, 350003) |
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| Abstract: | The Shankou Silver polymetallic ore deposit located at the Wuyishan mineralization belt＇s gloss-The Ninghua copper polymetallic mineralizes northeast the Asian belt with Pucheng- North Ningde west to molybdenum polymetallic mineralization belt intersection point. The ore body tax has Mesozoic Era Jiao Kengzu in the stratum. For deposition transformation ore deposit. Controls the ore the north east to the fault zone is many phase of active products. The main metallogenic period is the late three pack of worlds. The Shankou area and peripheral further prospects the potential to be big. |
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| Keywords: | Silver ore deposit Geological feature Deposition transformation Wuyishan City |
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