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Predictive Mineralogy

Possible unrecorded species at Ornans Meteorite, Ornans, Besançon, Doubs, Bourgogne-Franche-Comté, France

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
QuartzSiO299.97%Chloritoid (60.27 %), Diopside (51.68 %), Hematite (62.61 %), Magnetite (50.54 %), Margarite (54.01 %), Muscovite (80.32 %), Pyrrhotite (67.51 %), Rutile (72.22 %)
PyriteFeS299.03%Hematite (50.17 %), Muscovite (50.01 %), Pentlandite (58.72 %), Pyrrhotite (80.12 %), Rutile (52.79 %)
CalciteCaCO388.46%Diopside (54.07 %), Monticellite (74.88 %)
ChromiteFe2+Cr3+2O477.49%Awaruite (57.00 %), Iron (51.19 %), Taenite (62.40 %), Troilite (60.27 %)
ChalcopyriteCuFeS275.00%Pentlandite (73.72 %), Pyrrhotite (76.22 %)
PhlogopiteKMg3(AlSi3O10)(OH)254.18%Monticellite (54.19 %)
SphaleriteZnS44.31%Pyrrhotite (55.40 %)

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
3 : Solar nebular condensates (CAIs, AOAs, URIs)50
5 : Primary asteroid phases50
40 : Regional metamorphism (greenschist, amphibolite, granulite facies)35
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)28
6 : Secondary asteroid phases22
31 : Thermally altered carbonate, phosphate, and iron formations19
35 : Ultra-alkali and agpaitic igneous rocks17
9 : Lava/xenolith minerals (hornfels, sanidinite facies)15
39 : High-𝑃 metamorphism (blueschist, eclogite, ultrahigh 𝑃 facies)14
4 : Primary chondrule phases6