中国新生代碱性玄武岩型宝石矿床  

Cenozoic Alkaline Basaltic Gem Deposits in China

作　　者：邹天人[1] 於晓晋[2] 夏凤荣[1] 陈伟十[1] 

机构地区：[1]中国地质科学院矿床地质研究所,北京100037 [2]北京科技大学,100083

出　　处：《地质论评》1999年第S1期119-122,共4页Geological Review

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。The Cenozoic basalts are widely distributed in eastern China. Among them, 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.

关 键 词：宝石矿床 碱性玄武岩 新生代 中国东部 

分 类 号：P619.28[天文地球—矿床学]