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Predictive Mineralogy

Possible unrecorded species at Glücksrad Mine, Oberschulenberg, Clausthal-Zellerfeld, Goslar District, Lower Saxony, Germany

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
ArsenopyriteFeAsS99.60%Bournonite (55.79 %), Ianbruceite (57.14 %), Parasymplesite (55.32 %), Philipsbornite (58.06 %), Scorodite (74.10 %), Segnitite (57.06 %)
LeadhillitePb4(CO3)2(SO4)(OH)298.95%Chenite (58.70 %), Elyite (51.61 %), Lanarkite (63.48 %), Mattheddleite (69.44 %), Susannite (53.04 %)
DolomiteCaMg(CO3)298.55%Barysilite (61.54 %), Brianyoungite (52.69 %), Ianbruceite (57.14 %), Köttigite (56.52 %), Richelsdorfite (57.35 %)
DigeniteCu9S584.30%Spionkopite (62.79 %), Yarrowite (57.83 %)
VarisciteAlPO4 · 2H2O82.14%Metavariscite (82.14 %)
MagnetiteFe2+Fe3+2O481.71%Barysilite (53.85 %), Hydrotalcite (60.38 %)
BaryteBaSO479.99%Agardite-(Ce) (62.50 %), Arsentsumebite (68.29 %), Barysilite (69.23 %), Bayldonite (55.28 %), Beaverite-(Cu) (55.09 %), Brianyoungite (50.54 %), Chenite (52.17 %), Duftite (57.09 %), Dundasite (58.56 %), Ianbruceite (57.14 %), Köttigite (60.87 %), Ktenasite (56.52 %), Namuwite (50.68 %), Ramsbeckite (50.00 %), Richelsdorfite (63.24 %), Theisite (57.97 %), Zincolivenite (57.32 %)
BeudantitePbFe3(AsO4)(SO4)(OH)676.39%Arsentsumebite (51.22 %), Philipsbornite (51.61 %)
FluoriteCaF262.50%Agardite-(Ce) (62.50 %)
HausmanniteMn2+Mn3+2O461.53%Barysilite (61.54 %)
LeadPb61.53%Barysilite (61.54 %)
PyrochroiteMn(OH)261.53%Barysilite (61.54 %)
RhodoniteCaMn3Mn[Si5O15]61.53%Barysilite (61.54 %)
JacobsiteMn2+Fe3+2O453.84%Barysilite (53.85 %)
RichteriteNa(NaCa)Mg5(Si8O22)(OH)253.84%Barysilite (53.85 %)
SpessartineMn2+3Al2(SiO4)353.84%Barysilite (53.85 %)
TephroiteMn2+2SiO453.84%Barysilite (53.85 %)
CrandalliteCaAl3(PO4)(PO3OH)(OH)653.57%Metavariscite (53.57 %)
SideriteFeCO352.08%Agardite-(Ce) (52.08 %)
BruciteMg(OH)250.94%Hydrotalcite (50.94 %)
ScheeliteCa(WO4)43.07%Barysilite (53.85 %)

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
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]348
47c : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]

Unique: Smithsonite
231
47d : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Arsenates, antimonates, selenates, bismuthinates]224
47b : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Sulfates and sulfites]109
33 : Minerals deposited by hydrothermal metal-rich fluids (see also [#12])

Unique: Bournonite
106
48 : Soil leaching zone minerals

Unique: Gibbsite
100
13 : Hadean serpentinization

Unique: Hydrotalcite
100
47h : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals]42
50 : Coal and/or oil shale minerals35
55 : Anthropogenic mine minerals34
54 : Coal and other mine fire minerals (see also #51 and #56)31
56 : Slag and smelter minerals (see also #51 and #55)30
45b : Oxidized fumarolic minerals (see also [#11]) - [Other oxidized fumarolic minerals]18
32 : Ba/Mn/Pb/Zn deposits, including metamorphic deposits17