Predictive Mineralogy
This table is based on statistical analysis of other localities containing similar species to the ones found at this locality.
Possible missing species | Formula | Match % | Due to recorded presence of |
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Gypsum | CaSO4 · 2H2O | 61.07% | Anhydrite (61.07 %) |
Key: Mineral matches key element mineralogy of deposit Key element(s) in mineral not listed for deposit (-20% score)
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 |
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31 : Thermally altered carbonate, phosphate, and iron formations
Unique: Magnesiohögbomite-6N6S | 110 |
47h : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals]
Unique: Wulfenite | 100 |
40 : Regional metamorphism (greenschist, amphibolite, granulite facies) | 57 |
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47) | 39 |
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals] | 30 |
47c : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates] | 29 |
34 : Complex granite pegmatites | 23 |
53 : Other minerals with taphonomic origins | 20 |
26 : Hadean detrital minerals | 20 |
35 : Ultra-alkali and agpaitic igneous rocks | 12 |
38 : Ophiolites | 10 |
24 : Authigenic minerals in terrestrial sediments (see also #17) | 9 |