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Predictive Mineralogy

Possible unrecorded species at Löhley, Üdersdorf, Daun, Vulkaneifel, 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
AegirineNaFe3+Si2O699.33%Barytolamprophyllite (88.89 %), Fersmanite (85.71 %), Wöhlerite (58.33 %)
EttringiteCa6Al2(SO4)3(OH)12 · 26H2O97.40%Flörkeite (83.33 %), Scottyite (66.67 %), Willhendersonite (53.33 %)
NatroliteNa2Al2Si3O10 · 2H2O96.93%Barytolamprophyllite (55.56 %), Batisite (50.00 %), Fersmanite (64.29 %), Wöhlerite (61.36 %)
DiopsideCaMgSi2O696.63%Kalsilite (52.31 %), Perovskite (52.40 %), Priderite (64.18 %), Richterite (58.62 %)
ThaumasiteCa3(SO4)[Si(OH)6](CO3) · 12H2O95.55%Flörkeite (66.67 %), Scottyite (66.67 %), Willhendersonite (60.00 %)
MicroclineK(AlSi3O8)92.42%Barytolamprophyllite (62.96 %), Fersmanite (57.14 %), Wöhlerite (52.27 %)
PectoliteNaCa2Si3O8(OH)89.41%Barytolamprophyllite (70.37 %), Fersmanite (64.29 %)
EudialyteNa15Ca6Fe3Zr3Si(Si25O73)(O,OH,H2O)3(Cl,OH)284.12%Barytolamprophyllite (55.56 %), Fersmanite (64.29 %)
Cordierite(Mg,Fe)2Al3(AlSi5O18)80.00%Schüllerite (80.00 %)
SphaleriteZnS79.58%Barytolamprophyllite (62.96 %), Cerussite (56.70 %), Chalcopyrite (50.66 %), Fersmanite (57.14 %), Galena (65.95 %), Pyrrhotite (55.40 %)
AlbiteNa(AlSi3O8)78.40%Fersmanite (50.00 %), Wöhlerite (56.82 %)
ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 177.43%Mottramite (51.11 %), Vésigniéite (53.85 %)
MuscoviteKAl2(AlSi3O10)(OH)275.90%Montmorillonite (51.11 %), Topaz (50.72 %)
Lamprophyllite(Na,Mn2+)3(Sr,Na)2(Ti,Fe3+)3(Si2O7)2O2(OH,O,F)272.59%Barytolamprophyllite (62.96 %), Batisite (50.00 %), Fersmanite (50.00 %)
ÅkermaniteCa2Mg[Si2O7]66.66%Flörkeite (66.67 %)
WollastoniteCa3(Si3O9)66.66%Scottyite (66.67 %)
KaoliniteAl2(Si2O5)(OH)456.25%Bayerite (56.25 %)
Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)51.19%Wairakite (51.19 %)
LaumontiteCaAl2Si4O12 · 4H2O51.19%Wairakite (51.19 %)
BruciteMg(OH)250.94%Hydrotalcite (50.94 %)
WalstromiteBaCa2(Si3O9)50.00%Fresnoite (50.00 %)
WulfenitePb(MoO4)40.11%Vanadinite (50.14 %)

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
35 : Ultra-alkali and agpaitic igneous rocks

Unique: Barytolamprophyllite, Fersmanite, Götzenite, Lileyite
446
32 : Ba/Mn/Pb/Zn deposits, including metamorphic deposits

Unique: Fresnoite, Scottyite
202
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]

Unique: Nordstrandite
135
47h : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals]

Unique: Batiferrite
117
7 : Ultramafic igneous rocks

Unique: Noonkanbahite
116
10 : Basalt-hosted zeolite minerals

Unique: Willhendersonite
103
8 : Mafic igneous rocks

Unique: Flörkeite
102
13 : Hadean serpentinization

Unique: Hydrotalcite
100
47e : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Vanadates, chromates, manganates]22
34 : Complex granite pegmatites17
47g : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Halogen-bearing surface weathering minerals]16
36 : Carbonatites, kimberlites, and related igneous rocks12
9 : Lava/xenolith minerals (hornfels, sanidinite facies)10
16 : Low-𝑇 aqueous alteration of Hadean subaerial lithologies (see also #23)9
50 : Coal and/or oil shale minerals8
31 : Thermally altered carbonate, phosphate, and iron formations7
51 : Pyrometamorphic minerals (see also #54 and #56)7
45a : Oxidized fumarolic minerals (see also [#11]) - [Sulfates, arsenates, selenates, antimonates]7