Predictive Mineralogy
Possible unrecorded species at Radlberger Alp, LeΓnig, Kleblach-Lind, Spittal an der Drau District, Carinthia, Austria
This table is based on statistical analysis of other localities containing similar species to the ones found at this locality.
Possible missing species | Formula | Match % | Due to recorded presence of |
---|---|---|---|
Quartz | SiO2 | 99.99% | Antimony (74.33 %), Arsenopyrite (80.07 %), Berthierite (81.82 %), Chalcopyrite (67.26 %), Chalcostibite (83.98 %), Pyrite (67.27 %), Rutile (72.22 %), Stibnite (74.07 %), Ullmannite (81.56 %), Valentinite (73.67 %) |
Calcite | CaCO3 | 92.18% | Chalcostibite (63.11 %), Ullmannite (56.15 %), Valentinite (51.69 %) |
Sphalerite | ZnS | 79.93% | Antimony (62.23 %), Arsenopyrite (55.02 %), Berthierite (62.65 %), Chalcopyrite (50.66 %), Chalcostibite (70.87 %), Ullmannite (81.84 %), Valentinite (52.42 %) |
Galena | PbS | 79.39% | Antimony (54.72 %), Arsenopyrite (53.61 %), Chalcopyrite (51.07 %), Chalcostibite (59.71 %), Ullmannite (81.84 %) |
Pyrrhotite | Fe1-xS | 59.49% | Ullmannite (59.50 %) |
Key: Mineral matches key element mineralogy of deposit Key element(s) in mineral not listed for deposit (-20% score)
Predicting paragenetic modes of deposit
Green indicates almost certain match based on minerals unique to a certain deposit type. Yellow indicates a possibly poor match, but should not be entirely discounted. Scores > 100 indicate strong confidence.