Occurrence of sulphides on the bornite-idaite join from Vielsalm, Stavelot Massif, Belgium
peer reviewed ; Sulphides with chemical compositions between idaite and bornite have been identified from several quartz veins crosscutting Ordovician schists in Vielsalm, Belgium. Idaite is an oxidation product of bornite, and occurs in the more oxidised parts of the quartz veins. The alteration sequence bomite --> "anomalous bornite" --> idaite is observed, associated with the growth of chalcopyrite lamellae parallel to the
Verfasser: | |
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Dokumenttyp: | journal article |
Erscheinungsdatum: | 2003 |
Verlag/Hrsg.: |
E Schweizerbartsche Verlags
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Schlagwörter: | idaite / CU3FeS4 / stannite structure / vielsalm / Stavelot Massif / Belgium / Physical / chemical / mathematical & earth Sciences / Earth sciences & physical geography / Physique / chimie / mathématiques & sciences de la terre / Sciences de la terre & géographie physique |
Sprache: | Englisch |
Permalink: | https://search.fid-benelux.de/Record/base-28941685 |
Datenquelle: | BASE; Originalkatalog |
Powered By: | BASE |
Link(s) : | https://orbi.uliege.be/handle/2268/7834 |