节点文献
滇西雪山河变质岩群的矿物组成与原岩特征
MINERAL ASSEMBLAGE AND CHARACTERISTICS OF THE PROTOLITHES OF XUESH ANHE METAMORPHIC GROUP IN WESTERN YUNNAN
【摘要】 滇西澜沧江深大断裂带中北段东侧出露中生代浅变质岩系———雪山河变质岩群,其主要矿物组成为石英、黑云母和白云母。通过对其岩相学特征分析评价以及原岩恢复,提出该变质岩群为区内铜(金)矿(床)点的主要矿源层,其原岩主要为沉积岩,但可能有火山凝灰物质加入。
【Abstract】 The Xueshanhe metamorphic group, belonging to the Mesozoic lower metamorphic series, and whose major minerals are quartz, biotite and muscovite, is exposed at the eastern side of the middle-northern part of the Lancangjiang fault in western Yunnan. This paper deals with the metamorphic group in detail on the lithological character and the protolithes restored. The results showed that the metamorphic group, whose protolith is chiefly sedimentary rocks but is likely to be introduced by volcanic tuffaceous material, is the primary source-bed of copper (gold) ores in this region.
【关键词】 雪山河变质岩群;
岩相学特征;
原岩;
滇西;
【Key words】 Xueshanhe metamorphic group; lithological character; protolith; western Yunnan;
【Key words】 Xueshanhe metamorphic group; lithological character; protolith; western Yunnan;
【基金】 "九·五"国家科技攻关项目(96 914 02 04 03);原中国有色金属工业总公司地质科研项目(96 D 43)
- 【文献出处】 矿物学报 ,Acta Mineralogica Sinica , 编辑部邮箱 ,2004年04期
- 【分类号】P588.34
- 【被引频次】4
- 【下载频次】130