Dan property, south Yukon
Description
Massive black sphalerite occurs with pyrrhotite and magnetite in up to 3 irregular but roughly concordant layers at the contact between massive white marble and hard green and white-banded meta-tuff. The mineralization is believed to have replaced brecciated marble in the footwall of a south-dipping thrust fault which passes through the DAN prospect and extends through the Crescent Lake area 5.8 km to the east.
Resources
| Name |
Format |
Description |
Link |
| Yukon Geological Survey publication metadata |
HTML |
|
https://data.geology.gov.yk.ca/Reference/42511 |
| Original metadata (https://open.yukon.ca) |
HTML |
|
https://open.yukon.ca/information/ff70fe65-cbd6-42de-8642-ce3424e77f57 |
| Report |
PDF |
|
https://ygsftp.gov.yk.ca/publications/yeg/yeg90.pdf |