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Predictive Mineralogy

Possible unrecorded species at Neubulach, Calw, Karlsruhe Region, Baden-Württemberg, 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
GalenaPbS99.99%Adamite (66.33 %), Agardite-(Ce) (77.08 %), Ankerite (54.09 %), Arseniosiderite (52.21 %), Arsenocrandallite (68.75 %), Bariopharmacosiderite (53.23 %), Bayldonite (74.37 %), Brochantite (55.97 %), Chalcophyllite (55.56 %), Chalcopyrite (51.07 %), Covellite (64.18 %), Cyanotrichite (57.08 %), Digenite (59.98 %), Emplectite (61.38 %), Ferrisymplesite (50.00 %), Langite (63.00 %), Olivenite (50.95 %), Parnauite (60.80 %), Philipsburgite (60.61 %), Pitticite (62.67 %), Pyromorphite (77.81 %), Rooseveltite (52.27 %), Spionkopite (58.14 %), Strashimirite (54.78 %), Yarrowite (51.81 %), Zincolivenite (75.61 %)
SphaleriteZnS99.99%Adamite (55.00 %), Agardite-(Ce) (62.50 %), Ankerite (53.36 %), Arsenocrandallite (56.25 %), Bayldonite (55.28 %), Brochantite (50.32 %), Chalcophyllite (54.67 %), Chalcopyrite (50.66 %), Covellite (64.68 %), Digenite (61.34 %), Emplectite (62.41 %), Ferrisymplesite (58.33 %), Langite (58.40 %), Mansfieldite (54.17 %), Parnauite (50.40 %), Philipsburgite (60.61 %), Pitticite (60.00 %), Pyromorphite (56.90 %), Rooseveltite (56.82 %), Spionkopite (67.44 %), Yarrowite (65.06 %), Zincolivenite (54.88 %)
CerussitePbCO399.99%Adamite (60.00 %), Agardite-(Ce) (62.50 %), Arsenocrandallite (62.50 %), Bayldonite (73.37 %), Cyanotrichite (50.47 %), Langite (53.94 %), Parnauite (51.20 %), Philipsburgite (63.64 %), Pyromorphite (68.61 %), Zincolivenite (58.54 %)
ArsenopyriteFeAsS99.94%Arsenocrandallite (62.50 %), Bulachite (80.00 %), Ferrisymplesite (54.17 %), Mansfieldite (66.67 %), Pitticite (66.67 %), Preisingerite (50.82 %), Rooseveltite (68.18 %)
ScoroditeFe3+AsO4 · 2H2O99.91%Arseniosiderite (57.52 %), Arsenocrandallite (62.50 %), Ferrisymplesite (62.50 %), Mansfieldite (70.83 %), Pitticite (50.67 %), Preisingerite (63.93 %), Rooseveltite (72.73 %)
MimetitePb5(AsO4)3Cl99.90%Adamite (58.67 %), Agardite-(Ce) (64.58 %), Arsenocrandallite (56.25 %), Bayldonite (71.86 %), Parnauite (51.20 %), Philipsburgite (69.70 %), Zincolivenite (65.85 %)
GypsumCaSO4 · 2H2O96.43%Arsenocrandallite (68.75 %), Bariopharmacoalumite (50.00 %), Cyanotrichite (52.36 %), Strashimirite (52.17 %)
BismuthiniteBi2S394.13%Emplectite (57.24 %), Preisingerite (62.30 %), Rooseveltite (63.64 %)
AnglesitePbSO494.03%Agardite-(Ce) (50.00 %), Arsenocrandallite (50.00 %), Bayldonite (52.26 %), Zincolivenite (50.00 %)
BismuthBi93.29%Ferrisymplesite (50.00 %), Preisingerite (60.66 %), Rooseveltite (65.91 %)
AragoniteCaCO383.59%Arsenocrandallite (56.25 %), Ferrisymplesite (62.50 %)
SmithsoniteZnCO376.82%Arsenocrandallite (50.00 %), Zincolivenite (53.66 %)
Aurichalcite(Zn,Cu)5(CO3)2(OH)675.75%Arsenocrandallite (50.00 %), Philipsburgite (51.52 %)
LavendulanNaCaCu5(AsO4)4Cl · 5H2O75.00%Arsenocrandallite (50.00 %), Bariopharmacoalumite (50.00 %)
PharmacosideriteKFe3+4(AsO4)3(OH)4 · 6-7H2O62.50%Arsenocrandallite (62.50 %)
SilverAg60.00%Agardite-(Ce) (50.00 %), Ferrisymplesite (50.00 %)
DuftitePbCu(AsO4)(OH)57.57%Philipsburgite (57.58 %)
BeudantitePbFe3(AsO4)(SO4)(OH)656.25%Arsenocrandallite (56.25 %)
HemimorphiteZn4Si2O7(OH)2 · H2O54.54%Philipsburgite (54.55 %)
LinaritePbCu(SO4)(OH)252.08%Agardite-(Ce) (52.08 %)
AutuniteCa(UO2)2(PO4)2 · 10-12H2O51.51%Torbernite (51.52 %)
LöllingiteFeAs250.00%Ferrisymplesite (50.00 %)
ParasymplesiteFe2+3(AsO4)2 · 8H2O50.00%Ferrisymplesite (50.00 %)
CarminitePbFe3+2(AsO4)2(OH)250.00%Arsenocrandallite (50.00 %)
ConnelliteCu19(SO4)(OH)32Cl4 · 3H2O50.00%Arsenocrandallite (50.00 %)
MarcasiteFeS250.00%Arsenocrandallite (50.00 %)
SulphurS850.00%Arsenocrandallite (50.00 %)
ErythriteCo3(AsO4)2 · 8H2O43.33%Ferrisymplesite (54.17 %)

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]244
47d : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Arsenates, antimonates, selenates, bismuthinates]222
33 : Minerals deposited by hydrothermal metal-rich fluids (see also [#12])

Unique: Emplectite
100
47c : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]65
47h : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals]43
46 : Near-surface hydrothermal alteration of minerals (see also #22)12
47b : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Sulfates and sulfites]12
22 : Hydration and low-𝑇 subsurface aqueous alteration (see also #23)12
50 : Coal and/or oil shale minerals11
45b : Oxidized fumarolic minerals (see also [#11]) - [Other oxidized fumarolic minerals]10
55 : Anthropogenic mine minerals9