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 |
47h : Low-π subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals] | 2 |
45b : Oxidized fumarolic minerals (see also [#11]) - [Other oxidized fumarolic 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 |
38 : Ophiolites | 1 |
7 : Ultramafic igneous rocks | 1 |
37 : Layered igneous intrusions and related PGE minerals | 1 |
12 : Hadean hydrothermal subsurface sulfide deposits (see also #33) | 1 |
40 : Regional metamorphism (greenschist, amphibolite, granulite facies) | 1 |