Abstract
Vein mineralisation with no preferred orientation, cutting lower Palaeozoic rocks, and local replacement deposits in dolomite show a zoning in tungsten-bismuth, arsenic and antimony minerals away from the adjacent late-Hercynian Costabona granite. A local reversed zoning is related to higher temperatures indicated by fluid inclusion study. Many of the minerals have not previously been reported from this area. © 1981 Springer-Verlag.
Original language | English |
---|---|
Pages (from-to) | 195-204 |
Journal | Mineralium Deposita |
Volume | 16 |
Issue number | 2 |
DOIs | |
Publication status | Published - 1 Aug 1981 |