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Predictive Mineralogy

Possible unrecorded species at Rio delle Ossa, San Clemente, Monterenzio, Metropolitan City of Bologna, Emilia-Romagna, Italy

This table is based on statistical analysis of other localities containing similar species to the ones found at this locality.

Possible missing speciesFormulaMatch %Due to recorded presence of
ChalcopyriteCuFeS279.73%Ankerite (62.42 %), Jamborite (52.27 %), Millerite (66.43 %), Pyrite (51.72 %), Siderite (51.43 %), Vaesite (76.38 %)
SphaleriteZnS76.56%Ankerite (53.36 %), Jamborite (54.55 %), Millerite (50.48 %), Vaesite (59.06 %)
GalenaPbS63.80%Ankerite (54.09 %), Vaesite (55.91 %)
RutileTiO256.67%Brookite (56.67 %)

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 ModeScore
12 : Hadean hydrothermal subsurface sulfide deposits (see also #33)

Unique: Vaesite
100
47b : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Sulfates and sulfites]12
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]12
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)2
24 : Authigenic minerals in terrestrial sediments (see also #17)2
40 : Regional metamorphism (greenschist, amphibolite, granulite facies)1
36 : Carbonatites, kimberlites, and related igneous rocks1
38 : Ophiolites1
13 : Hadean serpentinization1
26 : Hadean detrital minerals1
34 : Complex granite pegmatites1