摘要
燕山早期白岗岩(γi52)须在风化作用下产生强烈的高岭土化才能形成工业矿体。勐宋高岭土是由白岗岩风化形成的残坡积型砂质高岭土矿床。
Yanshan early alaskite （gamma i52） to produce kaolinitization strong weathering in order to form industrial ore bodies. Mengsong kaolin is the residual slope formed by the weathering of alaskite deposited sandy kaolin deposit.
作者
王栋
唐金礼
王聪云
陶利林
WANG Dong;TANG Jin-li;WANG Cong-yun;TAO Li-lin(Yunnan geophysical prospecting Mining Co., Ltd,Yiliang 652100 China)
出处
《世界有色金属》
2018年第4期297-298,共2页
World Nonferrous Metals
