Cobalt and precious metals in sulphides of peridotite xenoliths and inferences concerning their distribution according to geodynamic environment: A case study from the Scottish lithospheric mantle
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文摘

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.

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