| 铜陵狮子山矿田花树坡铜矿床地质特征及矿床成因浅析 |
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| 引用本文： | 陈帮国.铜陵狮子山矿田花树坡铜矿床地质特征及矿床成因浅析[J].矿产与地质,2001,15(4):243-246. |
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| 作者姓名： | 陈帮国 |
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| 作者单位： | 安徽铜陵有色金属公司狮子山铜矿, |
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| 摘 要： | 铜陵花树坡铜矿床生体赋存于二叠系下统栖霞组硅质层内，次要矿体赋存于孤峰组内，受层位控制，矿体围岩具有热接触变质、接触交换变质特点，受断裂构造，、岩浆岩控制明显。褶皱殂成的虚脱空间及褶皱的叠加、层间剥离等多种因纱的复合，导致了矿体的形成，成矿温度为中－高温，该矿床为层控式矽卡岩型矿床。
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| 关 键 词： | 铜矿床 地质特征 成矿条件 成因 变质作用 断裂构造 岩浆岩 |
| 文章编号： | 1001-5663(2001)04-0243-04 |
| 修稿时间： | 2001年2月19日 |
A BRIEF DISCUSSION ON GEOLOGICAL CHARACTERS AND
METALLOGENY OF HUASHUPO COPPER ORE DEPOSIT OF
SHIZHISHAN FIELD, TONGLING |
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| CHEN Bang,guo.A BRIEF DISCUSSION ON GEOLOGICAL CHARACTERS AND
METALLOGENY OF HUASHUPO COPPER ORE DEPOSIT OF
SHIZHISHAN FIELD, TONGLING[J].Mineral Resources and Geology,2001,15(4):243-246. |
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| Authors: | CHEN Bang guo |
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| Abstract: | The main orebody of Huashupo Copper Deposit in Tongling occurs in silica horizon of Qixia Group of Lower Permian System, while minor ores controlled by strata occur in Gufeng Group. The country rocks of the ores are characterized by heat contact metamorphism and metasomatism and clearly controlled by tectonic structures and magmatite. The combination of several factors including peeled fold, fold overlap and stripping in horizons led to the formation of the orebodies. The mineralzation temperature is middle to high and the deposit belongs to strata bond skarn type. |
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| Keywords: | Huashupo Copper deposit Geological character Ore forming condition Genesis |
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