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滇西镇康芦子园矿床是保山—镇康地块上近年来新发现的超大型铅锌多金属矿床。野外地质调查发现,蔷薇辉石呈团块状、脉状出现于距地表近200m处,往深部数量增多,结晶颗粒变粗。铅锌矿与蔷薇辉石在空间上关系密切,蔷薇辉石越发育矿石品位愈高、厚度愈大。已有研究在成矿物质和成矿流体来源方面的认识存在分歧,矿床成因争议较大[1-2],从而影响成矿模式的建立和确定未来找矿方向。本文就对该矿床的成因具有重要指示意义的蔷薇辉石进行了专门报道,将对认识矿床成因和指导矿区深
The Zhenkang Luziyuan deposit in western Yunnan is a very large Pb-Zn polymetallic deposit newly discovered in recent years in Baoshan-Zhenkang block. Field geological survey found that the Rhodonite was clumped, veins appeared in the nearly 200m from the surface, to the deeper the number increased, the coarse grains. Lead-zinc ore and pyroxenes are closely related in space, Rhodopius more development of ore grade higher, the greater the thickness. There are differences in the understanding of the source of ore-forming materials and ore-forming fluids, and the controversy of the genesis of the orebodies has been widely discussed [1-2], thus affecting the establishment of metallogenic model and determining the prospecting direction in the future. This article made a special report on the Rhodonite, which is an important indicator of the genesis of the deposit, and will be of great significance for understanding the genesis of the deposit and guiding the depth of the mine