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Predictive Mineralogy

Possible unrecorded species at Tunaberg Cu-Co Ore Field, Tunaberg, Nyköping, Södermanland County, Sweden

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
PyriteFeS2100.00%Acanthite (68.82 %), Aikinite (81.56 %), Alabandite (53.72 %), Allargentum (74.36 %), Antimony (68.52 %), Arsenopyrite (79.40 %), Bismuth (65.41 %), Bismuthinite (76.49 %), Bornite (70.77 %), Boulangerite (84.31 %), Breithauptite (74.75 %), Sphalerite (75.10 %), Carrollite (69.27 %), Chalcopyrite (75.16 %), Clausthalite (73.89 %), Cobaltite (78.87 %), Cobaltpentlandite (76.24 %), Covellite (80.77 %), Cubanite (82.18 %), Dyscrasite (72.40 %), Emplectite (74.14 %), Erythrite (64.88 %), Galena (66.84 %), Gersdorffite (82.91 %), Silver (54.72 %), Greenockite (76.91 %), Gudmundite (84.19 %), Gustavite (83.72 %), Hauchecornite (67.74 %), Hedenbergite (52.35 %), Hessite (82.73 %), Joséite-B (76.00 %), Kawazulite (70.21 %), Linnaeite (84.73 %), Löllingite (66.48 %), Mackinawite (68.44 %), Matildite (85.40 %), Mawsonite (79.82 %), Meneghinite (83.06 %), Miargyrite (74.18 %), Millerite (71.66 %), Molybdenite (68.29 %), Nickeline (66.71 %), Nisbite (81.48 %), Parkerite (66.67 %), Pyroxmangite (52.41 %), Pyrrhotite (80.12 %), Safflorite (68.45 %), Stannoidite (75.00 %), Tellurium (80.17 %), Tellurobismuthite (82.99 %), Tetradymite (77.65 %), Tsumoite (76.00 %), Ullmannite (84.92 %), Uraninite (51.44 %), Wittichenite (75.62 %)
CalciteCaCO399.99%Acanthite (51.71 %), Aikinite (51.95 %), Allargentum (66.67 %), Boulangerite (52.73 %), Breithauptite (62.87 %), Clausthalite (58.61 %), Cobaltite (51.81 %), Dyscrasite (63.35 %), Emplectite (52.07 %), Erythrite (59.85 %), Gersdorffite (53.89 %), Greenockite (70.86 %), Gustavite (58.14 %), Hedenbergite (60.34 %), Kawazulite (53.19 %), Linnaeite (58.18 %), Löllingite (51.02 %), Matildite (52.70 %), Mawsonite (50.88 %), Meneghinite (51.37 %), Millerite (53.62 %), Nickeline (56.82 %), Pyroxmangite (53.01 %), Safflorite (66.31 %), Tellurobismuthite (50.15 %), Ullmannite (56.15 %), Wittichenite (55.07 %)
ChalcociteCu2S95.50%Carrollite (54.75 %), Covellite (50.30 %), Mawsonite (54.39 %), Wittichenite (56.16 %)
MalachiteCu2(CO3)(OH)289.75%Covellite (54.66 %), Emplectite (53.79 %), Erythrite (51.09 %)
RhodochrositeMnCO388.49%Alabandite (54.55 %), Pyroxmangite (74.70 %)
PyrargyriteAg3SbS387.71%Allargentum (58.97 %), Miargyrite (70.05 %)
HematiteFe2O376.96%Emplectite (52.76 %), Wittichenite (51.23 %)
RhodoniteCaMn3Mn[Si5O15]73.49%Pyroxmangite (73.49 %)
Pentlandite(NixFey)Σ9S868.11%Parkerite (68.12 %)
SkutteruditeCoAs358.28%Safflorite (58.29 %)
BournonitePbCuSbS357.37%Meneghinite (57.38 %)
SpessartineMn2+3Al2(SiO4)356.62%Pyroxmangite (56.63 %)
StibniteSb2S356.41%Antimony (56.42 %)
TephroiteMn2+2SiO454.81%Pyroxmangite (54.82 %)
StanniteCu2FeSnS453.12%Stannoidite (53.13 %)
MuscoviteKAl2(AlSi3O10)(OH)252.08%Stannoidite (52.08 %)
CassiteriteSnO251.04%Stannoidite (51.04 %)
ChromiteFe2+Cr3+2O442.66%Westerveldite (53.33 %)
BaryteBaSO440.82%Emplectite (51.03 %)

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
33 : Minerals deposited by hydrothermal metal-rich fluids (see also [#12])

Unique: Aikinite, Allargentum, Boulangerite, Clausthalite, Dyscrasite, Emplectite, etc.
2,188
12 : Hadean hydrothermal subsurface sulfide deposits (see also #33)

Unique: Gustavite
100
37 : Layered igneous intrusions and related PGE minerals46
31 : Thermally altered carbonate, phosphate, and iron formations15
6 : Secondary asteroid phases12
49 : Oxic cellular biomineralization (see also #44)11
45b : Oxidized fumarolic minerals (see also [#11]) - [Other oxidized fumarolic minerals]11
47d : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Arsenates, antimonates, selenates, bismuthinates]11
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]11
56 : Slag and smelter minerals (see also #51 and #55)11
34 : Complex granite pegmatites8
50 : Coal and/or oil shale minerals6