沉积与特提斯地质2016，Vol.36Issue(1)：23-29,7.
云南会泽大黑山铝土矿地球化学特征及其物源分析
Geochemistry and provenance analysis of the Daheishan bauxite deposit in Huize, Yunnan
摘要
Abstract
The Daheishan bauxite deposit in Huize, Yunnan resides in the basal part of the Upper Permian Xuanwei Formation underlain by the Emeishan basalts. The bauxite ores from the Daheishan deposit display micritic, oolitic and granular textures, and densely massive, stratified and stratoid structures. There are both negative correlations between Al2O3 and Fe2O3 , and Al2O3 and SiO2 and good correlations between TiO2 and Zr, Hf, Nb and Ta, Zr and Hf, Nb and Ta. The bauxite and basalt samples in this study exhibit similar normalized distribution patterns. The ore-forming matter may be derived from the underlying Emeishan basalts, as indicated by LogNi and LogCr diagram.关键词
铝土矿/地球化学/成矿物质来源/会泽大黑山Key words
bauxite/geochemistry/provenance/Daheishan in Huize分类
天文与地球科学引用本文复制引用
王正江,郭婷婷,俞赛赢,程琰勋,张春波,张宇栋..云南会泽大黑山铝土矿地球化学特征及其物源分析[J].沉积与特提斯地质,2016,36(1):23-29,7.基金项目
西南华南重点地区地质矿产调查评价项目(12120113072100) （12120113072100）
