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新疆可可托海伟晶岩形成机理的研究
引用本文:张恩世 ,张文淮 ,刘伟.新疆可可托海伟晶岩形成机理的研究[J].地球科学,1987(4).
作者姓名:张恩世  张文淮  刘伟
作者单位:Wuhan College of Geology,Wuhan 430074
摘    要:根据流体包裹体研究,获得了某些伟晶岩形成的物理—化学条件参数,特别是在可可托海3号伟晶岩脉中,发现了熔融、熔浆-溶液两类流体包裹体的共存。在此基础上探讨了该区伟晶岩的成岩成矿流体特征、演化过程和成因机制,并取得了新认识.

关 键 词:新疆  伟晶岩  成矿流体  熔浆-溶液

ON FORMATION MECHANISM OF KEKETUOHAI PEGMATITE,XINJIANG, CHINA
Zhang Enshi Zhang Wenhuai Liu Wei.ON FORMATION MECHANISM OF KEKETUOHAI PEGMATITE,XINJIANG, CHINA[J].Earth Science-Journal of China University of Geosciences,1987(4).
Authors:Zhang Enshi Zhang Wenhuai Liu Wei
Abstract:From the study of fluid inclusions, some data about the physicochemical conditions of pegmatite formation have been discussed. Some melt and melt-solution inclusions are found for the first time from No. 3 pegmatite vein in this district. Some principal problems about characteristics and evolution of rock-forming and ore-forming fluids and the formation mechanism of pegmatite have been studied deeply and some new knowledge of them has been suggested.
Keywords:Xinjiang  pegmatite  ore-forming fluids  melt-solution  
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