Geology of the B-baseline zone, Walton barium-copper-lead-zinc-silver deposit, Nova Scotia.
The Walton Ba-Cu-Pb-Zn-Ag deposit, Nova Scotia, is hosted by Visean-aged carbonate rocks of the Macumber Formation and its associated breccia. The Macumber Formation in the Walton area is divided into two units, the lower Macumber, a laminated carbonate 30-40$\sp\prime$ thick and the upper Macumber,...
| Main Author: | |
|---|---|
| Other Authors: | |
| Format: | Others |
| Published: |
University of Ottawa (Canada)
2009
|
| Subjects: | |
| Online Access: | http://hdl.handle.net/10393/10065 http://dx.doi.org/10.20381/ruor-8110 |