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 |
---|
33 : Minerals deposited by hydrothermal metal-rich fluids (see also [#12])
Unique: Bournonite, Domeykite, Enargite, Polybasite | 340 |
47a : Low-π subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]
Unique: Halloysite | 135 |
47c : Low-π subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]
Unique: Smithsonite | 104 |
47h : Low-π subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals]
Unique: Wulfenite | 101 |
32 : Ba/Mn/Pb/Zn deposits, including metamorphic deposits
Unique: Johannsenite | 100 |
40 : Regional metamorphism (greenschist, amphibolite, granulite facies) | 27 |
31 : Thermally altered carbonate, phosphate, and iron formations | 24 |
47b : Low-π subaerial oxidative hydration, weathering (see also #16 and #23) - [Sulfates and sulfites] | 17 |
6 : Secondary asteroid phases | 15 |
47d : Low-π subaerial oxidative hydration, weathering (see also #16 and #23) - [Arsenates, antimonates, selenates, bismuthinates] | 13 |
45b : Oxidized fumarolic minerals (see also [#11]) - [Other oxidized fumarolic minerals] | 10 |
47e : Low-π subaerial oxidative hydration, weathering (see also #16 and #23) - [Vanadates, chromates, manganates] | 9 |
50 : Coal and/or oil shale minerals | 9 |
54 : Coal and other mine fire minerals (see also #51 and #56) | 9 |
53 : Other minerals with taphonomic origins | 9 |