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Predictive Mineralogy

Possible unrecorded species at Kennack, Grade-Ruan, Cornwall, England, UK

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
ChalcopyriteCuFeS298.33%Ankerite (62.42 %), Hetaerolite (59.63 %), Native Copper (53.15 %), Pyrite (51.72 %), Siderite (51.43 %)
SphaleriteZnS80.74%Ankerite (53.36 %), Hetaerolite (58.72 %)
GalenaPbS69.21%Ankerite (54.09 %), Hetaerolite (70.64 %)
GoethiteFe3+O(OH)51.37%Hetaerolite (51.38 %)
HemimorphiteZn4Si2O7(OH)2 · H2O50.45%Hetaerolite (50.46 %)
MalachiteCu2(CO3)(OH)250.45%Hetaerolite (50.46 %)
CerussitePbCO349.90%Hetaerolite (62.39 %)

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
32 : Ba/Mn/Pb/Zn deposits, including metamorphic deposits

Unique: Hetaerolite
100
40 : Regional metamorphism (greenschist, amphibolite, granulite facies)11
13 : Hadean serpentinization10
38 : Ophiolites9
6 : Secondary asteroid phases4
26 : Hadean detrital minerals2
16 : Low-𝑇 aqueous alteration of Hadean subaerial lithologies (see also #23)2
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]2
31 : Thermally altered carbonate, phosphate, and iron formations2
9 : Lava/xenolith minerals (hornfels, sanidinite facies)2
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)1