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: Freibergite Subgroup | 100 |
47a : Low-π subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals] | 11 |
47f : Low-π subaerial oxidative hydration, weathering (see also #16 and #23) - [Uranyl (UβΆβΊ) minerals] | 7 |
47c : Low-π subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates] | 7 |
53 : Other minerals with taphonomic origins | 4 |
47b : Low-π subaerial oxidative hydration, weathering (see also #16 and #23) - [Sulfates and sulfites] | 4 |
36 : Carbonatites, kimberlites, and related igneous rocks | 2 |
38 : Ophiolites | 2 |
40 : Regional metamorphism (greenschist, amphibolite, granulite facies) | 1 |
37 : Layered igneous intrusions and related PGE minerals | 1 |
7 : Ultramafic igneous rocks | 1 |