腾冲优质高岭土矿床控矿因素及成因探讨  

A DISCUSSION ABOUT THE ORE-CONTROLLING FACTOR AND GENESIS OF TENGCHONG HIGH GRADE KAOLINITE DEPOSIT

作　　者：施玉北 

机构地区：[1]云南地质矿产勘查开发局第四地质大队

出　　处：《云南地质》1996年第3期290-298,共9页Yunnan Geology

摘　　要：本文根据腾冲优质高岭土矿床地质特征，研究了构造盆地与古地理环境、地层层位与岩性、热泉、地形地貌及风化壳等对成矿的控矿作用，提出矿床成因类型应属风化壳型叠加近代热泉蚀变的复合型。According to the geological characteristics of Tengchong high grade kaolinite deposit,the controlling functions of structural basin,paleogeographic environmeng, stratigraphic horizon,lithologic character,hot spring,geomorphologic and weathering crust,etc in metallogenesis are studied in this paper,It is put forward that the genesis of this ore deposit belongs to the composite type of weathering crust superimposed by recent hot spring alteration.

关 键 词：高岭土矿床 矿床地质特征 控矿因素 矿床成因论 

分 类 号：P619.232[天文地球—矿床学]