| 青海德尔尼硫化物矿床成因的新认识 |
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| 引用本文： | 阿延寿.青海德尔尼硫化物矿床成因的新认识[J].青海国土经略,2001(1). |
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| 作者姓名： | 阿延寿 |
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| 作者单位： | 青海省第一地质矿产勘查大队 平安 |
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| 摘 要： | 通过对青海德尔尼硫化物矿床的产出部位、成矿环境、矿石矿物的组合、主要化学元素的成份及同位素测试数据等分析研究,认为该矿床具有裂谷成矿机制的特征,成因类型应属裂谷型层控矿床。
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| 关 键 词： | 青海德尔尼 阿尼玛卿裂谷 裂谷型层控矿床 |
NEW RECOGNITION ON THE ORIGIN OF DEERNI SULFIDE DEPOSIT IN QINGHAI PROVINCE |
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| Authors: | A Yanshou Qinghai No Team of Geology and Mineral Exploration Pingan |
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| Institution: | A Yanshou Qinghai No.1 Team of Geology and Mineral Exploration,Pingan 810600 |
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| Abstract: | Through the studies of produced position, metallogenic surrounding, mineralassemblages of ore, main chemical composition, and isotopic date, et al., the author holdthat Deerni sulfide deposit is characterized by rift-type metallogenic mechanism, its genetictype should be belong to a rift-type stratabound ore deposit. |
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| Keywords: | Deerni Qinghai Anyemaqen rift rift-type stratabound ore deposit |
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