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 |
---|
33 : Minerals deposited by hydrothermal metal-rich fluids (see also [#12])
Unique: Hessite | 100 |
47c : Low-π subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates] | 5 |
53 : Other minerals with taphonomic origins | 5 |
47a : Low-π subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals] | 4 |
47h : Low-π subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals] | 3 |
40 : Regional metamorphism (greenschist, amphibolite, granulite facies) | 2 |
16 : Low-π aqueous alteration of Hadean subaerial lithologies (see also #23) | 2 |
31 : Thermally altered carbonate, phosphate, and iron formations | 2 |
36 : Carbonatites, kimberlites, and related igneous rocks | 2 |
45b : Oxidized fumarolic minerals (see also [#11]) - [Other oxidized fumarolic minerals] | 2 |
57 : Other minerals formed by human processes | 2 |