Deformation and metamorphism of the San Dionisio pyritic ore body, Rio Tinto, Spain
At the present time massive stratiform sulphide deposits are widely regarded as having an exhalative-sedimentary origin. The applicability of this view to the Rio Tinto deposits has been tested by investigating whether or not there is evidence in the essentially pyritic San Dionisio ore body of the...
| Main Author: | |
|---|---|
| Published: |
Imperial College London
1968
|
| Subjects: | |
| Online Access: | https://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.623117 |