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: Calaverite, Hessite, Petzite, Tellurobismuthite | 379 |
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]
Unique: Halloysite | 100 |
6 : Secondary asteroid phases | 13 |
53 : Other minerals with taphonomic origins | 8 |
47c : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates] | 7 |
36 : Carbonatites, kimberlites, and related igneous rocks | 5 |
40 : Regional metamorphism (greenschist, amphibolite, granulite facies) | 4 |
26 : Hadean detrital minerals | 4 |
38 : Ophiolites | 3 |
22 : Hydration and low-𝑇 subsurface aqueous alteration (see also #23) | 2 |
16 : Low-𝑇 aqueous alteration of Hadean subaerial lithologies (see also #23) | 2 |
39 : High-𝑃 metamorphism (blueschist, eclogite, ultrahigh 𝑃 facies) | 2 |