Mesozoic Zijinshan magmatism occurred in two periods and can be further divided into three magmatic events.
Ore-bearing magmas are characterized by higher ƒO2 than the barren magmas.
Both barren and mineralized magmas have no adakitic affinities.
The changes of the tectonic setting may result in the different sources for the magmatic and mineralization event.
© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号 地址:北京市海淀区学院路29号 邮编:100083 电话:办公室:(+86 10)66554848;文献借阅、咨询服务、科技查新:66554700 |