ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
柯树背岩体的副矿物特征及地质意义
  
关键词:Keshubei rock mass  structural state of orthoclase  petrological characteristics  characteristics of accessory minerals  zircon groups
基金项目:国家杰出青年基金(49625304)和科技部攀登计划预选项目(95-预-39),南京大学内生金属矿床成矿机制研究国家重点实验室开放基金,华侨大学博士科研起动资金
作者单位
胡恭任 中国科学院地球化学研究所贵州贵阳550002华侨大学环境科学与工程系福建泉州3620ll南京大学内生金属矿床成矿机制研究国家重点实验室江苏南京210093 
刘丛强 中国科学院地球化学研究所贵州贵阳550002 
陈培荣 南京大学内生金属矿床成矿机制研究国家重点实验室江苏南京210093 
于瑞莲 华侨大学环境科学与工程系福建泉州3620ll 
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摘要:
Characteristics and Geological Significance of the Accessory Minerals from the Keshubei Granitic Body
      In this paper,mineralogical,petrological and accessory mineral characteristics of the Keshubei rock mass,as well as features of zircon groups have been studied in detail.The result shows that the western part of the rock mass differs obviously from the eastern part of the rock mass in mineral compositions,rock types,accessory minerals and zircon groups.The eastern part of the rock mass is similar to the Zhaibei rock mass,being regarded as granite of the syntectic series,whereas the western part of the rock mass is regarded as granite of the reformation series.This opinion has great guiding significance in looking for U and Au mineral deposits in this region.
HU Gong-ren,LIU Cong-qiang,CHEN Pei-rong,YU Rui-lian.2003.Characteristics and Geological Significance of the Accessory Minerals from the Keshubei Granitic Body[J].Acta Geoscientica Sinica,24(3):231-236.
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