Sedimentary rock hosted copper mineralization in the Neoproterozoic Redstone Copperbelt, Northwest Territories, Canada
Physical-chemical fluid evolution, timing of fluid-migration and driving forces for fluid-flow are factors that fundamentally control the mass transport that leads to the formation of sedimentary rock hosted copper deposits. This thesis constrains these factors for Kupferschiefer-type mineralization...
| Main Author: | |
|---|---|
| Language: | English |
| Published: |
University of British Columbia
2015
|
| Online Access: | http://hdl.handle.net/2429/54237 |