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 |
---|
Diopside | CaMgSi2O6 | 52.96% | Vesuvianite (52.97 %) |
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 |
---|
47h : Low-π subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals]
Unique: Wulfenite | 100 |
47a : Low-π subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals] | 22 |
31 : Thermally altered carbonate, phosphate, and iron formations | 17 |
47e : Low-π subaerial oxidative hydration, weathering (see also #16 and #23) - [Vanadates, chromates, manganates] | 13 |
40 : Regional metamorphism (greenschist, amphibolite, granulite facies) | 12 |
53 : Other minerals with taphonomic origins | 9 |
47c : Low-π subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates] | 9 |
34 : Complex granite pegmatites | 5 |
26 : Hadean detrital minerals | 4 |
45b : Oxidized fumarolic minerals (see also [#11]) - [Other oxidized fumarolic minerals] | 3 |
8 : Mafic igneous rocks | 2 |