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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Beryl | Be3Al2(Si6O18) | 55.79% | Euclase (55.80 %) |
Cerussite | PbCO3 | 53.10% | Stolzite (53.11 %) |
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: Arsenic, Bournonite, Enargite | 300 |
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]
Unique: Tungstite | 114 |
47h : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals]
Unique: Stolzite | 100 |
34 : Complex granite pegmatites | 21 |
31 : Thermally altered carbonate, phosphate, and iron formations | 9 |
26 : Hadean detrital minerals | 8 |
21 : Chemically precipitated carbonate, phosphate, iron formations | 2 |
47c : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates] | 2 |
36 : Carbonatites, kimberlites, and related igneous rocks | 1 |
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47) | 1 |
49 : Oxic cellular biomineralization (see also #44) | 1 |
37 : Layered igneous intrusions and related PGE minerals | 1 |
12 : Hadean hydrothermal subsurface sulfide deposits (see also #33) | 1 |