| 中国新生代碱性玄武岩型宝石矿床 |
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| 引用本文： | 邹天人,於晓晋,夏凤荣,陈伟十.中国新生代碱性玄武岩型宝石矿床[J].地质论评,1999,45(7):119-122. |
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| 作者姓名： | 邹天人 於晓晋 夏凤荣 陈伟十 |
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| 作者单位： | 中国地质科学院矿床地质研究所,北京,100037；北京科技大学，100083；中国地质科学院矿床地质研究所,北京,100037 |
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| 摘 要： | 中国东部分布着大量的新生代玄武岩，其中第三纪的中新世和上新世的碱性玄武岩是蓝宝石、红宝石、红色锆石、橄榄石、镁铝榴石、月光石和辉石类宝石的寄主岩石，已在其内发现了多种宝石的原生矿床和矿化点。今后应重视碱性玄武岩型宝石矿床的研究和找矿评价工作。
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| 关 键 词： | 宝石矿床 碱性玄武岩 新生代 中国东部 |
Alkaline Basaltic Gem Deposits of the Cenozoic Era In China |
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| Zou Tianren,Yu Xiaojin,Xia Fengrong and Chen Weishi.Alkaline Basaltic Gem Deposits of the Cenozoic Era In China[J].Geological Review,1999,45(7):119-122. |
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| Authors: | Zou Tianren Yu Xiaojin Xia Fengrong and Chen Weishi |
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| Institution: | Institute of Mineral Deposits, Chinese Academy of Geological Sciences, Beijing, 100037 |
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| Abstract: | The Cenozoic basalts are widely distributed in eastern China. Among the m, the Miocene and Pliocene alkaline basalts are the host rocks of ruby, sapphire, red zircon, olivine, pyrope, moonstone and pyroxene gem. So far varied primary gem deposits and mineral occurrences have been found in the alkaline basalts. Henceforth,a great attention should be devoted to the research, prospecting and assessment of the alkaline basaltic gem deposits. |
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| Keywords: | gem diposit alkaline basalt Cenozoic eastern China |
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