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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Malachite | Cu2(CO3)(OH)2 | 50.34% | Anglesite (50.35 %) |
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 | 100 |
47c : Low-π subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]
Unique: Smithsonite | 100 |
50 : Coal and/or oil shale minerals | 4 |
54 : Coal and other mine fire minerals (see also #51 and #56) | 4 |
45b : Oxidized fumarolic minerals (see also [#11]) - [Other oxidized fumarolic minerals] | 3 |
45a : Oxidized fumarolic minerals (see also [#11]) - [Sulfates, arsenates, selenates, antimonates] | 2 |
47b : Low-π subaerial oxidative hydration, weathering (see also #16 and #23) - [Sulfates and sulfites] | 2 |
47a : Low-π subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals] | 2 |
57 : Other minerals formed by human processes | 2 |
36 : Carbonatites, kimberlites, and related igneous rocks | 1 |
33 : Minerals deposited by hydrothermal metal-rich fluids (see also [#12]) | 1 |
12 : Hadean hydrothermal subsurface sulfide deposits (see also #33) | 1 |