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 |
---|
53 : Other minerals with taphonomic origins | 50 |
47a : Low-π subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals] | 50 |
47c : Low-π subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates] | 50 |
39 : High-π metamorphism (blueschist, eclogite, ultrahigh π facies) | 4 |
40 : Regional metamorphism (greenschist, amphibolite, granulite facies) | 4 |
31 : Thermally altered carbonate, phosphate, and iron formations | 4 |
43 : Shear-induced minerals (including mylonite/slickensides) | 3 |
22 : Hydration and low-π subsurface aqueous alteration (see also #23) | 3 |
16 : Low-π aqueous alteration of Hadean subaerial lithologies (see also #23) | 3 |
49 : Oxic cellular biomineralization (see also #44) | 3 |