Chalcophile elements and sulphide ‘populations’ in the SCLM
Variability of sulphide texture and composition according to terrane age
Cobalt is elevated in sulphides in all xenoliths south of the Great Glen Fault.
Cobalt enrichment is the result of Iapetus ocean crust subduction.
Carbonate-phosphate-sulphide immiscibility suggests carbonatite metasomatism of SCLM.