| 铜陵地区层控矽卡岩型矿床地质特征和成矿条件 |
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| 引用本文： | 夏元法.铜陵地区层控矽卡岩型矿床地质特征和成矿条件[J].矿产与地质,1999,13(6):338-342. |
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| 作者姓名： | 夏元法 |
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| 作者单位： | 铜陵有色地质勘察分公司,铜陵,244000 |
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| 摘 要： | 铜陵地区层控矽卡岩型矿床，主要分布于中石炭统黄龙组白云岩段。研究分析铜官山、冬瓜山、天马山、新桥等矿区地质特征、成矿物质和含矿流体的来源后，认为该类矿床属同生沉积—岩浆热液叠加改造成因。
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| 关 键 词： | 层控矽卡岩型 分布 地质特征 同位素 含矿流体 铜陵 |
| 文章编号： | 1001-5663(1999)06-0338-05 |
| 修稿时间： | 1999年8月27日 |
GEOLOGICAL CHARACTERISTICS AND ORE-FORMING CONDITION OF STRATABOUND SKARN - TYPE ORE DEPOSITS IN TONGLING DISTRICT |
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| Xia yuanfa.GEOLOGICAL CHARACTERISTICS AND ORE-FORMING CONDITION OF STRATABOUND SKARN - TYPE ORE DEPOSITS IN TONGLING DISTRICT[J].Mineral Resources and Geology,1999,13(6):338-342. |
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| Authors: | Xia yuanfa |
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| Abstract: | Stratabound Skarn-type Ore Deposits in Tongling district are mainly distributed in dolomite layers of Huangling Group mid-Carboniferous System.It is believed that the type of ore deposit is of origin of synchronous deposit-magmatic hydrothermal replacement,after studying regional geological features,ore-forming material and sounrce of mineral-containing fluid in Tonguanshan,Donguashan,Tianmashan and Xinqiao etc.. |
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| Keywords: | Stratabound Skarn-type Geological features Isotope Mineral_containing fluid Tongling |
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