摘要
本文通过对木吉材—浮图峪铁铜多金属矿田三个不同类型矿床成矿地质条件的详细研究及对成矿期构造应力场特征的分析,明确指出成矿期构造条件的差异是形成该区具有成因联系的不同类型矿床的主导控制因素。最后总结了该区的成矿规律并建立成矿模式。
Based on the detailed investigation on the mineralized geological condition of three deposits of different types, and the analysis on the character of tectonic stress field of mineralizing epoch in Mujicun-Futuyu Fe-Cu polymetallic ore-field, it is suggested that difference of tectonic setting of mineralizing epoch is the major controlling factor for forming the deposits of different types with genetic relationship in this region. Finally, the mineralized regularity is summarized, and a metallogenetic model in the region is proposed.
出处
《地球科学（中国地质大学学报）》
EI
CAS
CSCD
北大核心
1989年第5期563-572,共10页
Earth Science-Journal of China University of Geosciences
关键词
多金属矿床
成矿构造条件
成矿模式
mineralizing tectonic setting, metallogenetic model, compounding of structures, Hebei province
