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Predictive Mineralogy

Possible unrecorded species at Tal y Fan, Caerhun, Conwy, Wales, 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
PyriteFeS298.35%Actinolite (62.14 %), Epidote (56.37 %), Ferro-hornblende (52.70 %), Muscovite (50.01 %), Stilpnomelane (57.88 %)
MagnetiteFe2+Fe3+2O496.30%Actinolite (53.38 %), Ferro-hornblende (64.86 %), Kaersutite (51.56 %), Tschermakite (53.41 %)
CalciteCaCO395.97%Actinolite (55.10 %), Epidote (51.60 %), Prehnite (61.24 %), Titanite (52.17 %)
Augite(CaxMgyFez)(Mgy1Fez1)Si2O655.62%Kaersutite (55.63 %)
HematiteFe2O350.96%Stilpnomelane (50.96 %)
ChalcopyriteCuFeS241.80%Actinolite (52.26 %)

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
40 : Regional metamorphism (greenschist, amphibolite, granulite facies)50
39 : High-𝑃 metamorphism (blueschist, eclogite, ultrahigh 𝑃 facies)37
8 : Mafic igneous rocks29
31 : Thermally altered carbonate, phosphate, and iron formations26
7 : Ultramafic igneous rocks16
16 : Low-𝑇 aqueous alteration of Hadean subaerial lithologies (see also #23)16
37 : Layered igneous intrusions and related PGE minerals14
6 : Secondary asteroid phases12
21 : Chemically precipitated carbonate, phosphate, iron formations12
32 : Ba/Mn/Pb/Zn deposits, including metamorphic deposits12