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Predictive Mineralogy

Possible unrecorded species at Aschaffenburg District, Lower Franconia, Bavaria, 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
SilverAg99.87%Algodonite (54.55 %), Arsenolamprite (57.14 %), Domeykite (55.56 %), Duranusite (50.00 %), Koutekite (57.14 %), Metauranospinite (70.59 %), Pharmacolite (54.31 %), Skutterudite (50.92 %)
ScoroditeFe3+AsO4 路 2H2O98.68%Arseniosiderite (57.52 %), Ferrarisite (60.00 %), Pharmacosiderite (61.99 %), Pitticite (50.67 %), Yukonite (58.82 %)
AnglesitePbSO494.09%Ramsbeckite (82.89 %), Serpierite (65.51 %)
LinaritePbCu(SO4)(OH)292.89%Ramsbeckite (81.58 %), Serpierite (61.45 %)
DigeniteCu9S592.69%Idaite (53.46 %), Spionkopite (62.79 %), Yarrowite (57.83 %)
PicropharmacoliteCa4Mg(AsO4)2(HAsO4)2 路 11H2O90.51%Ferrarisite (80.00 %), Pharmacolite (52.59 %)
LangiteCu4(SO4)(OH)6 路 2H2O88.45%Posnjakite (60.11 %), Ramsbeckite (71.05 %)
Monazite-(Ce)Ce(PO4)79.72%Bergslagite (55.56 %), Chernovite-(Y) (54.39 %)
Safflorite(Co,Ni,Fe)As278.03%Ferrarisite (53.33 %), Metauranospinite (52.94 %)
SainfelditeCa5(AsO4)2(AsO3OH)2 路 4H2O73.33%Ferrarisite (73.33 %)
Schulenbergite(Cu,Zn)7(SO4)2(OH)10 路 3H2O72.36%Ramsbeckite (72.37 %)
HydrozinciteZn5(CO3)2(OH)669.73%Ramsbeckite (69.74 %)
SmithsoniteZnCO368.42%Ramsbeckite (68.42 %)
StibniteSb2S366.66%Duranusite (66.67 %)
Gu茅riniteCa6(HAsO4)3(AsO4)2 路 10.5H2O66.66%Ferrarisite (66.67 %)
Aurichalcite(Zn,Cu)5(CO3)2(OH)665.78%Ramsbeckite (65.79 %)
RauenthaliteCa3(AsO4)2 路 10H2O60.00%Ferrarisite (60.00 %)
HemimorphiteZn4Si2O7(OH)2 路 H2O59.21%Ramsbeckite (59.21 %)
AcanthiteAg2S58.82%Metauranospinite (58.82 %)
AnalcimeNa(AlSi2O6) 路 H2O56.37%Natrolite (56.38 %)
MolybdeniteMoS255.99%Powellite (55.99 %)
HaidingeriteCaHAsO4 路 H2O53.33%Ferrarisite (53.33 %)
H枚rnesiteMg3(AsO4)2 路 8H2O53.33%Ferrarisite (53.33 %)
WeiliteCa(HAsO4)53.33%Ferrarisite (53.33 %)
SarkiniteMn2+2(AsO4)(OH)52.38%Brandtite (52.38 %)
AnnabergiteNi3(AsO4)2 路 8H2O42.66%Ferrarisite (53.33 %)

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: Algodonite, Arsenic, Cuprobismutite, Domeykite, Duranusite, Emplectite, etc.
849
47a : Low-饾憞 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]277
32 : Ba/Mn/Pb/Zn deposits, including metamorphic deposits

Unique: Hausmannite, Kutnohorite
219
47d : Low-饾憞 subaerial oxidative hydration, weathering (see also #16 and #23) - [Arsenates, antimonates, selenates, bismuthinates]187
34 : Complex granite pegmatites

Unique: Rhabdophane-(Nd)
143
12 : Hadean hydrothermal subsurface sulfide deposits (see also #33)

Unique: Jordisite
100
47f : Low-饾憞 subaerial oxidative hydration, weathering (see also #16 and #23) - [Uranyl (U鈦垛伜) minerals]57
26 : Hadean detrital minerals49
47c : Low-饾憞 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]49
40 : Regional metamorphism (greenschist, amphibolite, granulite facies)39
47h : Low-饾憞 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals]35
53 : Other minerals with taphonomic origins33
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)33
35 : Ultra-alkali and agpaitic igneous rocks27