| 山东昌乐新生代玄武质岩石中的刚玉及共存矿物 |
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| 引用本文： | 王萍,李国昌.山东昌乐新生代玄武质岩石中的刚玉及共存矿物[J].中国非金属矿工业导刊,1996(4). |
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| 作者姓名： | 王萍 李国昌 |
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| 作者单位： | 山东建材学院材料系!淄博，255200 |
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| 摘 要： | 昌乐方山新生代玄武质岩石中的刚玉具有明显的不同世代的结晶特征。分析与刚玉共存的各种矿物稳定存在的温度、压力范围，可以推断不同世代的刚玉结晶时的温压条件。
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| 关 键 词： | 新生代 刚玉 六方环状色带 异元熔融 原生包裹体 昌乐 |
The Corundum and Associated Minerals of Basaltic Rocks of the Cenozoic Era in Changle County,Shandong Province |
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| Wang Ping et al.The Corundum and Associated Minerals of Basaltic Rocks of the Cenozoic Era in Changle County,Shandong Province[J].China Non-Metallic Mining Industry Herald,1996(4). |
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| Authors: | Wang Ping |
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| Affiliation: | Wang Ping et al |
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| Abstract: | Corundum from basaltic rocks of the Cenozoic era has obvious crystallization characteristics in different generations in Fangshan, Changle county. Analysing the stable range of temperature and pressure of coexisting minerals with corundum is available to judge the crystallization conditions of corundum in differ ent generations. |
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| Keywords: | Cenozoic era Corundum Hexagonal color zoning Heterogenetic liquation Orignal inclosure Changle |
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