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鄂西仁和坪向斜煤系高岭岩的矿石特征及应用前景
引用本文:陈开旭,刘明忠 刘国庆 徐德明 陈泽云.鄂西仁和坪向斜煤系高岭岩的矿石特征及应用前景[J].中国地质,2004,31(3):315-319.
作者姓名:陈开旭  刘明忠 刘国庆 徐德明 陈泽云
作者单位:1. 中国地质大学,湖北,武汉,430074;宜昌地质矿产研究所,湖北,宜昌,443003
2. 宜昌市国土资源局,湖北,宜昌,443000
3. 宜昌地质矿产研究所,湖北,宜昌,443003
基金项目:国家矿产资源补偿费矿产勘查项目资助。
摘    要:对鄂西仁和坪向斜二叠系梁山组煤系高岭岩成矿地质特征及矿石组分的研究表明,该地区高岭岩矿床属碎屑沉积型,以硬质高岭岩为主,矿层层位稳定,矿石中高岭石多呈隐晶至微晶片状结构,且纯度高(高岭石含量90%~95%),具有低Mn(<30×10-6)高Ti(>0.5%)的特点,矿石中Fe、Mg、Ca、Na、K、Mn、S、As及重金属元素Cu、Pb、Zn、Cd、Tl等有害组分含量普遍较低。综合分析认为本区高岭岩属功能化极强的优质高岭石原料,在橡胶、塑料、涂料、药用包装等领域有广阔的应用前景。

关 键 词:煤系高岭岩  矿石组分  成矿地质  仁和坪向斜
文章编号:1000-3657(2004)03-0315-05

Ore features and application prospects of kaolinitic rock in coal measures of the Renheping syncline, western Hubei
CHEN Kai-xu,LIU Ming-zhong,LIU Guo-qing,XU De-ming,CHEN Zhe-yun.Ore features and application prospects of kaolinitic rock in coal measures of the Renheping syncline, western Hubei[J].Chinese Geology,2004,31(3):315-319.
Authors:CHEN Kai-xu  LIU Ming-zhong  LIU Guo-qing  XU De-ming  CHEN Zhe-yun
Institution:CHEN Kai-xu1,2,LIU Ming-zhong3,LIU Guo-qing2,XU De-ming2,CHEN Zhe-yun3
Abstract:Abstract: Study of geological features and ore composition of kaolinitic rock in coal measures of the Permian Liangshan Formation in the Renheping syncline, western Hubei, indicates that the kaolinitic rock deposit is of clastic sedimentary type and dominated by hard kaolinitic rock, with a persistent ore horizon. Kaolinite in the ore is mostly aphanitic to microcrystalline flaky textures, has a high purity (the kaolinite content is 90% to 95%) and is characterized by low Mn (<30 ×10-6) and high Ti (>0.5%). The harmful components Fe, Mg, Ca, Na, K, Mn, S and As and heavy metals elements Cu, Pb, Zn, Cd and Tl are all lower. Integrated analysis suggests that the kaolinitic rock may serve as high-quality functional kaolinite raw material and has good prospects in the rubber, plastic, coating and medicinal package industries.
Keywords:kaolinitic rocks of coal measures  ore composition  Renheping syncline
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