| 冀东某地原生红刚玉矿床地质特征 |
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| 引用本文： | 王宝德,王礼胜,陈秀玉.冀东某地原生红刚玉矿床地质特征[J].华北地质矿产杂志,1999(2). |
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| 作者姓名： | 王宝德 王礼胜 陈秀玉 |
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| 作者单位： | 石家庄经济学院 |
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| 摘 要： | 冀东某地原生刚玉矿床具有埋藏浅，刚玉个体大、微红至暗红色、半透明至不透明等特点，经人工改善可生产低档红宝石。本文主要介绍该矿床的刚玉形态特征、物理性质、晶体结构、包裹体特征及矿床形成的地质条件。研究认为，本矿床应属深熔型混合岩化作用成因，即“混合岩型”刚玉矿床。
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| 关 键 词： | 冀东某地 刚玉矿床 地质特征 |
The Geological Characteristics of the Primary Corundum Deposit in Eastern Hebei |
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| Authors: | WANG Baode WANG Lisheng CHEN Xiuyu |
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| Abstract: | The primary corundum deposit in eastern Hebei is near the ground surface. The corundum is megacrysts, pink or dark red color, semi-transparence to opaque. They can be improved into lower grade ruby. This paper describes the morphological characteristics, physical property, crystal structrue, inclusions and genesis of the deposit. It is considered that the deposit is an anatectic migmatite corundum deposit. |
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| Keywords: | Eastern Hebei Corundum deposit Geological characteristics |
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