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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Titanite | CaTi(SiO4)O | 52.52% | Allanite-(Ce) (52.52 %) |
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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33 : Minerals deposited by hydrothermal metal-rich fluids (see also [#12])
Unique: Berthierite, Bournonite, Glaucodot, Ullmannite | 331 |
32 : Ba/Mn/Pb/Zn deposits, including metamorphic deposits
Unique: Pyrosmalite-(Mn) | 100 |
40 : Regional metamorphism (greenschist, amphibolite, granulite facies) | 28 |
31 : Thermally altered carbonate, phosphate, and iron formations | 16 |
37 : Layered igneous intrusions and related PGE minerals | 11 |
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47) | 11 |
22 : Hydration and low-𝑇 subsurface aqueous alteration (see also #23) | 7 |
6 : Secondary asteroid phases | 6 |
34 : Complex granite pegmatites | 5 |
24 : Authigenic minerals in terrestrial sediments (see also #17) | 4 |
47h : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals] | 4 |
47e : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Vanadates, chromates, manganates] | 4 |