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云南中甸热林岩体的成矿作用
引用本文:伍建兢,杨丽梅,吴俊.云南中甸热林岩体的成矿作用[J].云南地质,2011,30(2):216-219.
作者姓名:伍建兢  杨丽梅  吴俊
作者单位:云南省地质调查院矿产所,云南昆明,650216
摘    要:热林矿区的热林复式花岗岩体,从早至晚、边部到中部,分出4个侵入体组成的同源岩浆细粒-中粒-斑状结构演化系列。成矿作用有差异,从而形成各具特色的矿床。

关 键 词:复式闪熔花岗岩  同碰撞S型  过饱和钙碱型  热液充填交代  中甸热林岩体

ON THE METALLOGENESIS OF RELIN ROCK BODY IN ZHONGDIAN, YUNNAN
WU Jian-jing,YANG Li-mei,WU Jun.ON THE METALLOGENESIS OF RELIN ROCK BODY IN ZHONGDIAN, YUNNAN[J].Yunnan Geology,2011,30(2):216-219.
Authors:WU Jian-jing  YANG Li-mei  WU Jun
Institution:WU Jian-jing,YANG Li-mei,WU Jun(Institute of Mineral Resources,Yunnan Geological Survey,Kunming 650216)
Abstract:In the Relin orefield,the Relin composite granite body can be divided into cogenetic fine grain-medium grain-porphyritic structure evolution series composed of 4 intrusive bodies from margin to center successively from the early to the late.The metallogenesis of them is different,which form various ore deposit with speciality different one another.
Keywords:Composite Syntectic Granite  Cogenetic Collision S Type  Oversaturated Calc-Alkalic Type  Hydrothermal Filling Metacomatism  Relin Rock Body of Zhongdian  
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