Predictive Mineralogy
This table is based on statistical analysis of other localities containing similar species to the ones found at this locality.
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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47h : Low-π subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals]
Unique: Wulfenite | 101 |
33 : Minerals deposited by hydrothermal metal-rich fluids (see also [#12])
Unique: Freibergite Subgroup | 100 |
45b : Oxidized fumarolic minerals (see also [#11]) - [Other oxidized fumarolic minerals] | 2 |
47c : Low-π subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates] | 2 |
57 : Other minerals formed by human processes | 2 |
45a : Oxidized fumarolic minerals (see also [#11]) - [Sulfates, arsenates, selenates, antimonates] | 1 |
47a : Low-π subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals] | 1 |
47d : Low-π subaerial oxidative hydration, weathering (see also #16 and #23) - [Arsenates, antimonates, selenates, bismuthinates] | 1 |
47g : Low-π subaerial oxidative hydration, weathering (see also #16 and #23) - [Halogen-bearing surface weathering minerals] | 1 |
37 : Layered igneous intrusions and related PGE minerals | 1 |
36 : Carbonatites, kimberlites, and related igneous rocks | 1 |
12 : Hadean hydrothermal subsurface sulfide deposits (see also #33) | 1 |