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云南哀牢山和新疆可可托海伟晶岩矿物中熔融包裹体电子探针研究

李兆麟1, 张文兰2, 李文1 2, 翟伟1, 石贵勇1,   

  1. 1. 中山大学地球科学系,广州,510275;2. 南京大学金属成矿作用国家重点 实验室, 江苏 南京, 210093
  • 收稿日期:2000-12-20 修回日期:2000-12-20 出版日期:2000-12-20 发布日期:2000-12-20

Electronic Microprobe Study on the Melt Inclusions in Pegmatite Minerals from Ailaoshan and Keketuohai Pegmatite Deposits

LI Zhao-Lin1;2, ZHANG Wen-1an2, LI Wen1;2, ZHAI Wei1, SHI Gui-yong1   

  1. 1. Department of Earth Sciences, Zhongshan University, Guangzhou 510275; 2. State Key Laboratory for Mineral Deposits Research, Nanjing University, Nanjing 210093
  • Received:2000-12-20 Revised:2000-12-20 Online:2000-12-20 Published:2000-12-20

摘要: 运用电子探针测定了云南哀牢山伟晶岩和新疆可可 托海伟晶岩矿物中熔融包裹体及流体-熔融包裹体子矿物成分。据73个包裹体中120个测 点分 析结果,鉴定出锌尖晶石、刚玉、磷灰石、磁铁矿、白云母、黑云母、钾长石、钠长石、绿 柱石和石英等10种 子矿物,并确定矿物组合27个。其中锌尖晶石、刚玉在两地区伟晶岩熔融包裹体中属首次发 现,磷灰石成分属首次测定。两地伟晶岩矿物的熔融及流体-熔融包裹体中子 矿 物成分及矿物组合各异,包裹体中子矿物与主矿物的化学成分存在一定演化规律,可作为了 解伟晶岩浆结晶分异作用、元素演化规律的依据。研究表明,伟晶岩存在局部岩浆分异作 用,岩浆具不混溶性及非均匀性。此成果对了解伟晶岩物质成分、形成机制及成因研究具重 要意义。对岩浆岩、地幔岩及陨石研究也有一定启迪。

Abstract: The compositions of daughter minerals in melt an d fluid-melt inclusions in minerals from Ailaoshan pegmatite, Yunnan Provinc e and Keketuohai pegmatite, Xinjiang Autonomous Region were analyzed by electron ic microprobe. 120 analytical points from 73 inclusions we re analyzed. 10 daughter minerals (including zinc-spinel, corundum, apatite, ma gnetite, muscovite, biotite, microcline, albite, quartz and alumo silicate glass) and 27 minera l assemblages were identified. Zinc-spinel and corundum were identified for the first time in these regions. The analytical results indicate that the daughter mineral compositions and mineral assemblages in melt and fluid-melt incl usions vary with different types of pegmatites. The evolution patterns in compositions of daughter minerals and host minerals could be used as a basis to search for the evolution patterns of chemical elements during pegmatite cr ystallization. The existence of local magmatic differentiation, immiscibility an d heterogeneity was proved for the pegmatite magmas. The results of this study are significant in understanding the compositions, forming mechanism s and origins of pegmatites. It would a lso inspire further studies on magmatites, pyrolites and meteorites.