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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Cassiterite | SnO2 | 61.83% | Stannite (61.84 %) |
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]) | 50 |
37 : Layered igneous intrusions and related PGE minerals | 45 |
47a : Low-π subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals] | 38 |
31 : Thermally altered carbonate, phosphate, and iron formations | 29 |
40 : Regional metamorphism (greenschist, amphibolite, granulite facies) | 23 |
47d : Low-π subaerial oxidative hydration, weathering (see also #16 and #23) - [Arsenates, antimonates, selenates, bismuthinates] | 20 |
53 : Other minerals with taphonomic origins | 13 |
47c : Low-π subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates] | 12 |
12 : Hadean hydrothermal subsurface sulfide deposits (see also #33) | 12 |
50 : Coal and/or oil shale minerals | 12 |