Geological Survey of Canada

Post-recrystallisation phenomena in metamorphosed stratabound sulphide ores: a comment RECENTLY, Vokes and Craig (1993) described and illustrated evidence for sequential mobilisation of sphalerite, chalcopyrite and quartz in the small Gressli deposit in central Norway during Caledonian amphibolite-f...

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Bibliographic Details
Main Authors: Cromwell Road, C. J. Stanley, A. C. Roberts, D. C. Harris
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Published: 1994
Subjects:
nagyagite
crystal structure
electron-probe microanalysis
Sacarimb
Romania
Canada
Norway
Sulitjelma
Northern Norway
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.605.2216
http://www.minersoc.org/pages/Archive-MM/Volume_58/58-392-482.pdf
Description
Summary:Post-recrystallisation phenomena in metamorphosed stratabound sulphide ores: a comment RECENTLY, Vokes and Craig (1993) described and illustrated evidence for sequential mobilisation of sphalerite, chalcopyrite and quartz in the small Gressli deposit in central Norway during Caledonian amphibolite-facies metamorphism. These authors stressed the need to study other similarly deformed and metamorphosed deposits to determine if similar textures might be present. The classic Cu-(Zn) pyritic deposits at Sulitjelma in northern Norway (Cook et al., 1990, 1993) are already well known as being excellent examples of stratiform assive sulphide deposits in which the

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