Predictive Mineralogy
There are no predicted missing minerals from this locality based on our current calculations.
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 |
---|
47c : Low-π subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]
Unique: Smithsonite | 100 |
47a : Low-π subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals] | 17 |
45b : Oxidized fumarolic minerals (see also [#11]) - [Other oxidized fumarolic minerals] | 7 |
53 : Other minerals with taphonomic origins | 6 |
50 : Coal and/or oil shale minerals | 4 |
54 : Coal and other mine fire minerals (see also #51 and #56) | 4 |
47h : Low-π subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals] | 3 |
24 : Authigenic minerals in terrestrial sediments (see also #17) | 3 |
6 : Secondary asteroid phases | 3 |
31 : Thermally altered carbonate, phosphate, and iron formations | 3 |
47g : Low-π subaerial oxidative hydration, weathering (see also #16 and #23) - [Halogen-bearing surface weathering minerals] | 3 |