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Predictive Mineralogy

Possible unrecorded species at Cygnet district, Huon-Channel region, Huon Valley municipality, Tasmania, Australia

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
MicroclineK(AlSi3O8)98.24%Eudialyte (51.16 %), Lamprophyllite (62.92 %), Manganoeudialyte (50.00 %), Mosandrite-(Ce) (59.38 %), Wöhlerite (52.27 %)
Arfvedsonite[Na][Na2][Fe2+4Fe3+]Si8O22(OH)280.62%Manganoeudialyte (60.00 %), Mosandrite-(Ce) (51.56 %)
LorenzeniteNa2Ti2(Si2O6)O370.00%Manganoeudialyte (70.00 %)
Kentbrooksite(Na,REE)15(Ca,REE)6(Mn2+,Fe2+)3Zr3Nb[Si25O74]F2 · 2H2O70.00%Manganoeudialyte (70.00 %)
VilliaumiteNaF60.00%Manganoeudialyte (60.00 %)
MalachiteCu2(CO3)(OH)254.65%Covellite (54.66 %)
ChalcociteCu2S50.30%Covellite (50.30 %)
CatapleiiteNa2Zr(Si3O9) · 2H2O50.00%Manganoeudialyte (50.00 %)
ElpiditeNa2ZrSi6O15 · 3H2O50.00%Manganoeudialyte (50.00 %)
Loparite-(Ce)(Na,REE)2Ti2O650.00%Manganoeudialyte (50.00 %)
Rinkite-(Ce)(Ca3Ce)Na(NaCa)Ti(Si2O7)2(OF)F248.00%Manganoeudialyte (60.00 %)

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
35 : Ultra-alkali and agpaitic igneous rocks

Unique: Lamprophyllite, Manganoeudialyte, Mosandrite-(Ce), Vishnevite
417
36 : Carbonatites, kimberlites, and related igneous rocks

Unique: Fluorstrophite
110
10 : Basalt-hosted zeolite minerals

Unique: Stellerite
100
40 : Regional metamorphism (greenschist, amphibolite, granulite facies)25
31 : Thermally altered carbonate, phosphate, and iron formations24
34 : Complex granite pegmatites19
47c : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]18
9 : Lava/xenolith minerals (hornfels, sanidinite facies)14
17 : Marine authigenic Hadean minerals (see also #24)12
47d : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Arsenates, antimonates, selenates, bismuthinates]12
6 : Secondary asteroid phases8
45a : Oxidized fumarolic minerals (see also [#11]) - [Sulfates, arsenates, selenates, antimonates]8
16 : Low-𝑇 aqueous alteration of Hadean subaerial lithologies (see also #23)7