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Predictive Mineralogy

Possible unrecorded species at Schellkopf, Brenk, Brohltal, Ahrweiler, Rhineland-Palatinate, 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
QuartzSiO299.99%Aragonite (53.70 %), Calcite (62.43 %), Chabazite-Ca (50.66 %), Davyne (57.14 %), Fedorite (90.00 %), Fluorapatite (70.90 %), Fluorapophyllite-(K) (60.71 %), Fluorite (66.12 %), Hydrotalcite (50.00 %), Hydroxylapatite (58.93 %), Ilmenite (52.06 %), Montmorillonite (65.62 %), Thaumasite (51.69 %), Titanite (65.16 %)
MagnetiteFe2+Fe3+2O499.99%Aegirine-augite (54.11 %), Davyne (71.43 %), Hydrotalcite (60.38 %), Ilmenite (57.89 %), Leucite (56.66 %), Lizardite (66.06 %), Nepheline (53.00 %), Nosean (55.46 %), Paranatrolite (62.50 %), Pitiglianoite (57.14 %), Thaumasite (54.59 %)
NatroliteNa2Al2Si3O10 · 2H2O95.15%Gonnardite (70.92 %), Paranatrolite (66.67 %), Zeophyllite (50.00 %)
PyriteFeS294.79%Calcite (51.16 %), Hydrotalcite (51.89 %), Paranatrolite (54.17 %), Thaumasite (51.69 %)
GypsumCaSO4 · 2H2O92.44%Davyne (57.14 %), Ettringite (58.04 %), Thénardite (58.00 %)
Augite(CaxMgyFez)(Mgy1Fez1)Si2O685.99%Davyne (66.67 %), Nosean (57.98 %)
PhlogopiteKMg3(AlSi3O10)(OH)283.67%Davyne (61.90 %), Pitiglianoite (57.14 %)
WollastoniteCa3(Si3O9)81.35%Afwillite (51.06 %), Davyne (61.90 %)
AndraditeCa3Fe3+2(SiO4)380.95%Davyne (80.95 %)
HaüyneNa3Ca(Si3Al3)O12(SO4)76.19%Davyne (76.19 %)
ZirconZr(SiO4)76.19%Davyne (66.67 %), Pitiglianoite (85.71 %)
BaddeleyiteZrO275.10%Davyne (57.14 %), Pitiglianoite (85.71 %)
MicroclineK(AlSi3O8)70.00%Fedorite (70.00 %)
Chabazite-Na(Na2,K2,Ca,Sr,Mg)2[Al2Si4O12]2 · 12H2O70.00%Phillipsite-Na (70.00 %)
DiopsideCaMgSi2O666.66%Davyne (66.67 %)
ForsteriteMg2SiO461.90%Davyne (61.90 %)
HematiteFe2O358.33%Paranatrolite (58.33 %)
AnorthiteCa(Al2Si2O8)57.14%Davyne (57.14 %)
SodaliteNa4(Si3Al3)O12Cl57.14%Pitiglianoite (57.14 %)
HaliteNaCl56.28%Thénardite (56.29 %)
GalenaPbS56.00%Fedorite (70.00 %)
TobermoriteCa4Si6O17(H2O)2 · (Ca · 3H2O)55.31%Afwillite (55.32 %)
GrossularCa3Al2(SiO4)352.38%Davyne (52.38 %)
MeioniteCa4Al6Si6O24CO352.38%Davyne (52.38 %)
MuscoviteKAl2(AlSi3O10)(OH)251.10%Montmorillonite (51.11 %)
SpurriteCa5(SiO4)2(CO3)51.06%Afwillite (51.06 %)
BruciteMg(OH)250.94%Hydrotalcite (50.94 %)
Charoite(K,Sr)15-16(Ca,Na)32[Si6O11(O,OH)6]2[Si12O18(O,OH)12]2[Si17O25(O,OH)18]2(OH,F)4 · ~3H2O50.00%Fedorite (50.00 %)
PyrrhotiteFe1-xS50.00%Paranatrolite (50.00 %)
SphaleriteZnS40.00%Fedorite (50.00 %)

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
13 : Hadean serpentinization

Unique: Hydrotalcite
103
48 : Soil leaching zone minerals

Unique: Gibbsite
100
35 : Ultra-alkali and agpaitic igneous rocks50
31 : Thermally altered carbonate, phosphate, and iron formations39
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]23
9 : Lava/xenolith minerals (hornfels, sanidinite facies)22
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)20
22 : Hydration and low-𝑇 subsurface aqueous alteration (see also #23)18
51 : Pyrometamorphic minerals (see also #54 and #56)14
25 : Evaporites (prebiotic)14
26 : Hadean detrital minerals13
53 : Other minerals with taphonomic origins13