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 |
---|
32 : Ba/Mn/Pb/Zn deposits, including metamorphic deposits
Unique: Hausmannite | 101 |
47c : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]
Unique: Smithsonite | 100 |
45b : Oxidized fumarolic minerals (see also [#11]) - [Other oxidized fumarolic minerals] | 5 |
47h : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals] | 5 |
47e : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Vanadates, chromates, manganates] | 4 |
47g : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Halogen-bearing surface weathering minerals] | 4 |
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals] | 2 |
50 : Coal and/or oil shale minerals | 2 |
54 : Coal and other mine fire minerals (see also #51 and #56) | 2 |
24 : Authigenic minerals in terrestrial sediments (see also #17) | 1 |
22 : Hydration and low-𝑇 subsurface aqueous alteration (see also #23) | 1 |
36 : Carbonatites, kimberlites, and related igneous rocks | 1 |