Predictive Mineralogy
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 |
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Dolomite | CaMg(CO3)2 | 50.17% | Kutnohorite (50.18 %) |
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.
Paragenetic Mode | Score |
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33 : Minerals deposited by hydrothermal metal-rich fluids (see also [#12])
Unique: Boulangerite, Freibergite Subgroup, Metacinnabar, Proustite, Pyrargyrite | 502 |
32 : Ba/Mn/Pb/Zn deposits, including metamorphic deposits
Unique: Kutnohorite | 100 |
40 : Regional metamorphism (greenschist, amphibolite, granulite facies) | 16 |
47h : Low-π subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals] | 14 |
47d : Low-π subaerial oxidative hydration, weathering (see also #16 and #23) - [Arsenates, antimonates, selenates, bismuthinates] | 13 |
49 : Oxic cellular biomineralization (see also #44) | 13 |
22 : Hydration and low-π subsurface aqueous alteration (see also #23) | 6 |
50 : Coal and/or oil shale minerals | 3 |
16 : Low-π aqueous alteration of Hadean subaerial lithologies (see also #23) | 2 |
54 : Coal and other mine fire minerals (see also #51 and #56) | 2 |
56 : Slag and smelter minerals (see also #51 and #55) | 2 |
37 : Layered igneous intrusions and related PGE minerals | 2 |