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 | 51.09% | Erythrite (51.09 %) |
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: Polybasite, Proustite, Pyrargyrite, Stephanite | 399 |
47g : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Halogen-bearing surface weathering minerals]
Unique: Chlorargyrite | 100 |
47d : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Arsenates, antimonates, selenates, bismuthinates] | 24 |
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals] | 24 |
49 : Oxic cellular biomineralization (see also #44) | 12 |
45b : Oxidized fumarolic minerals (see also [#11]) - [Other oxidized fumarolic minerals] | 5 |
47c : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates] | 5 |
47h : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals] | 2 |
57 : Other minerals formed by human processes | 2 |
36 : Carbonatites, kimberlites, and related igneous rocks | 1 |
38 : Ophiolites | 1 |
7 : Ultramafic igneous rocks | 1 |