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。
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.
出处
《云南地质》
2011年第2期216-219,共4页
Yunnan Geology
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
Composite Syntectic Granite
Cogenetic Collision S Type
Oversaturated Calc-Alkalic Type
Hydrothermal Filling Metacomatism
Relin Rock Body of Zhongdian
