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 |
---|
47g : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Halogen-bearing surface weathering minerals]
Unique: Chlorargyrite | 100 |
33 : Minerals deposited by hydrothermal metal-rich fluids (see also [#12]) | 14 |
49 : Oxic cellular biomineralization (see also #44) | 13 |
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals] | 4 |
53 : Other minerals with taphonomic origins | 4 |
47c : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates] | 4 |
36 : Carbonatites, kimberlites, and related igneous rocks | 1 |
38 : Ophiolites | 1 |
7 : Ultramafic igneous rocks | 1 |
47h : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals] | 1 |
50 : Coal and/or oil shale minerals | 1 |