用户名: 密码: 验证码:
Modelling fluid transport associated with mineralization and deformation in the Outokumpu Cu–Zn–Co deposit, Finland
详细信息    查看全文
文摘
Cu–Zn–Co mineralization in the Outokumpu district of eastern Finland shows evidence for structural control, metal enrichment and ore remobilisation during a Paleoproterozoic orogenic event. Our three dimensional numerical models explore deformation and fluid flow patterns within a generic architecture based on the Kylylahti deposit in the Outokumpu district. Patterns of strain localization, dilation and fluid flow associated with the serpentinites and the roof, basal and imbricate thrusts demonstrate the concepts of fluid infiltration and reworking of the Outokumpu deposits during a post-mineralisation deformation 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