| 福建岭头坪铅锌金银多金属矿地质特征及远景分析 |
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| 引用本文： | 沈中兴.福建岭头坪铅锌金银多金属矿地质特征及远景分析[J].福建地质,2005,24(3):147-153. |
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| 作者姓名： | 沈中兴 |
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| 作者单位： | 福建省闽东南地质大队,泉州,362011 |
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| 摘 要： | 岭头坪铅锌金银多金属矿产于南园组第二、三段中酸-酸性火山碎屑岩的夹层中,矿体呈似层状,受断裂构造及层间破碎带控制.成矿与中生代火山活动紧密相关,可能为中低温火山热液矿床.从成矿地质条件和金土壤异常分析,岭头坪矿区的周围及南、东侧以及石笋歧一带有很好的找矿前景.
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| 关 键 词： | 铅锌金银多金属矿 地质特征 远景分析 岭头坪 |
| 收稿时间： | 2004-07-01 |
| 修稿时间： | 2004年7月1日 |
Geologic Characteristics and Long-term Perspectives Analysis of the Lingtouping Lead-zinc-gold-silvet Polymetallic Ores in Fujian Province |
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| Shen Zhongxing.Geologic Characteristics and Long-term Perspectives Analysis of the Lingtouping Lead-zinc-gold-silvet Polymetallic Ores in Fujian Province[J].Geology of Fujian,2005,24(3):147-153. |
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| Authors: | Shen Zhongxing |
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| Institution: | Southeastern Fujian Geologic Party, Quanzhou , 362011 |
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| Abstract: | The Lingtouping lead-zinc-gold-silver polymetallic ores are discovered in the interlayers of intermediate-acidic volcaniclastic rock of the No. 2 and No. 3 members of Nanyuan Formation. The orebodies exists as quasi-stratiform and are controlled by the faulted structure and interbedding fractured zone. It is inferred that the ore-forming process has a close relation with the Mesozoic volcanic activity and it is a mesothermal and epithermal volcanic hydrothermal deposit. Based on the ore-forming geological conditions and soil-anomaly analysis, it is considered that the neighbourhood, southern and eastern sides of the Lingtouping minefield is a good orefinding target. |
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| Keywords: | lead-zinc-gold-silver polymetallic ores geologic characteristics long-term perspectives analysis Lingtouping |
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