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Predictive Mineralogy

Possible unrecorded species at Loben, Bad Sankt Leonhard im Lavanttal, Wolfsberg District, Carinthia, Austria

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
HematiteFe2O390.25%Lepidocrocite (55.13 %), Ranciéite (52.88 %), Romanèchite (53.91 %)
SphaleriteZnS79.99%Ankerite (53.36 %), Arsenopyrite (55.02 %), Chalcopyrite (50.66 %), Galena (65.95 %), Jamesonite (74.21 %), Marcasite (65.85 %), Pitticite (60.00 %), Plagionite (78.76 %), Pyromorphite (56.90 %), Pyrrhotite (55.40 %)
MalachiteCu2(CO3)(OH)279.11%Allophane (53.24 %), Pitticite (55.33 %)
BaryteBaSO475.93%Plagionite (50.44 %), Ranciéite (51.44 %)
RhodochrositeMnCO369.17%Kutnohorite (69.18 %)
CerussitePbCO368.60%Pyromorphite (68.61 %)
ZinkenitePb9Sb22S4253.09%Plagionite (53.10 %)
PyrolusiteMn4+O252.33%Cryptomelane (52.34 %)
BoulangeritePb5Sb4S1152.21%Plagionite (52.21 %)
DolomiteCaMg(CO3)250.17%Kutnohorite (50.18 %)

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: Plagionite
107
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]

Unique: Halloysite
104
32 : Ba/Mn/Pb/Zn deposits, including metamorphic deposits

Unique: Kutnohorite
100
40 : Regional metamorphism (greenschist, amphibolite, granulite facies)16
47e : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Vanadates, chromates, manganates]7
55 : Anthropogenic mine minerals7
47h : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals]6
50 : Coal and/or oil shale minerals6
45b : Oxidized fumarolic minerals (see also [#11]) - [Other oxidized fumarolic minerals]5
47d : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Arsenates, antimonates, selenates, bismuthinates]5
49 : Oxic cellular biomineralization (see also #44)4
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)4
47b : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Sulfates and sulfites]4