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.
出处
《云南地质》
1996年第3期290-298,共9页
Yunnan Geology
