A | This mineral is Anthropogenic. |
G | This mineral is directly dated. |
B | This mineral is reported as having this age. |
Y | This mineral is using an age reported as an element mineralization period. |
O | This mineral is using an age calculated from all data at the locality. |
R | The age displayed for this mineral originates from a different, non-child locality. |
P | The age displayed for this mineral is the range of ages for this mineral at all of this locality's children. |
This mineral's age has not yet been recorded. |
Amorphous | Autunite | Coronadite | Corundum | Diaspore | Dufrénite | Fluorite | Gypsum | Leucophosphite | Marcasite |
None | Phosphuranylite | Pyrite | Quartz | Wardite | Zircon |
Mineral name | Structural Groups | IMA Formula | Max Age (Ma) | Min Age (Ma) | # of Sublocalities containing mineral | LOCALITY IDs, not mindat ids | # of localities containing mineral |
---|---|---|---|---|---|---|---|
Autunite (*) | Autunite | Ca(UO2)2(PO4)2·10-12H2O | 290 | 270 | 0 | 1272 | |
Bornite (*) | None | Cu5FeS4 | 290 | 210 | 0 | 5516 | |
Cacoxenite (*) | None | Fe3+24AlO6(PO4)17(OH)12·75H2O | 290 | 210 | 0 | 280 | |
Chalcocite (*) | None | Cu2S | 290 | 210 | 0 | 5707 | |
Churchite-(Y) (*) | Gypsum | Y(PO4)·2H2O | 290 | 210 | 0 | 70 | |
Coffinite (*) | Zircon | U(SiO4)·nH2O | 290 | 270 | 0 | 566 | |
Cryptomelane (*) | Coronadite | K(Mn4+7Mn3+)O16 | 290 | 210 | 0 | 599 | |
Cyrilovite (*) | Wardite | NaFe3+3(PO4)2(OH)4·2H2O | 290 | 210 | 0 | 60 | |
Fluorite (*) | Fluorite | CaF2 | 290 | 210 | 0 | 9617 | |
Goethite (*) | Diaspore | FeO(OH) | 290 | 210 | 0 | 7437 | |
Gypsum (*) | Gypsum | Ca(SO4)·2H2O | 290 | 210 | 0 | 6890 | |
Hematite (*) | Corundum | Fe2O3 | 290 | 210 | 0 | 14640 | |
Leucophosphite (*) | Leucophosphite | KFe3+2(PO4)2(OH)·2H2O | 290 | 210 | 0 | 110 | |
Marcasite (*) | Marcasite | FeS2 | 290 | 210 | 0 | 5674 | |
Metatorbernite (*) | None | Cu(UO2)2(PO4)2·8H2O | 290 | 270 | 0 | 443 | |
Metauranocircite-I (*) | None | Ba(UO2)2(PO4)2·6H2O | 290 | 270 | 0 | 38 | |
Natrodufrénite (*) | Dufrénite | NaFe2+Fe3+5(PO4)4(OH)6·2H2O | 290 | 210 | 0 | 46 | |
Opal (*) | Amorphous | SiO2·nH2O | 290 | 210 | 0 | 2994 | |
Phosphuranylite (*) | Phosphuranylite | KCa(H3O)3(UO2)7(PO4)4O4·8H2O | 290 | 270 | 0 | 182 | |
Pyrite (*) | Pyrite | FeS2 | 290 | 210 | 0 | 39462 | |
Quartz (*) | Quartz | SiO2 | 290 | 210 | 0 | 61156 | |
Sabugalite (*) | None | HAl(UO2)4(PO4)4·16H2O | 290 | 270 | 0 | 87 | |
Saléeite (*) | None | Mg(UO2)2(PO4)2(H2O)10 | 290 | 270 | 0 | 95 | |
Studtite (*) | None | (UO2)(O2)(H2O)2·2H2O | 290 | 270 | 0 | 25 | |
Torbernite (*) | None | Cu(UO2)2(PO4)2·12H2O | 290 | 270 | 0 | 1059 | |
Uraninite (*) | Fluorite | UO2 | 290 | 270 | 0 | 2718 | |
Uranophane-α (*) | None | Ca(UO2)2(SiO3OH)2·5H2O | 290 | 270 | 0 | 890 |
Age ID | Locality Notes |
---|---|
Giersdorf_00000657 | The La Commanderie Mine locality is found within the Mortagne mining district. The mine is responsible for the production of 3300 tons of Uranium metal. It is part of the Armorican Massif. The Mortagne district is also associated with the Deux-Sèvres area, all part of the Armorican Massif |
Giersdorf_00000657a | The La Commanderie Mine locality is found within the Mortagne mining district. The mine is responsible for the production of 3300 tons of Uranium metal. It is part of the Armorican Massif. The Mortagne district is also associated with the Deux-Sèvres area, all part of the Armorican Massif |
Excel ID | Max Age (Ma) | Min Age (Ma) | Age as listed in reference | Dating Method | Age Interpret | Prioritized? | Sample Source | Sample Num | Run Num | Age from other Locality | Dated Mineral | Minerals explicitely stated as having this age | Age applies to these Elements | MinDat Locality ID | Dated Locality (Max Age) | Location as listed in reference | Reference | Reference DOI | Reference ID | Age Notes | |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
Giersdorf_00000657 | 290 | 270 | 290-270 | U-Pb | The age of mineralization being post-cooling of the 300-340 Ma granite bodies restricts the formation of the Uranium minerals to being genetically derived. | U | 32248 | La Commanderie Mine, Le Temple, Deux-Sèvres, Nouvelle-Aquitaine, France | La Commanderie Mine | Chauris et al. (1994) | PMGFRA_243 | Age of the uranium mineralization in the Armorican Massif is associated with Hercynian peraluminous granites. From pg. 262: "The precise chronology of these mineralizations is not well established. The uranium veins appear to be the oldest (290-270 Ma by U/Pb dating) but underwent late remobilization processes." | |||||||||
Giersdorf_00000657a | 230 | 210 | 230-210 | K-Ar | The age of mineralization being post-cooling of the 300-340 Ma granite bodies restricts the formation of the Uranium minerals to being genetically derived. | Pb, Zn | 32248 | La Commanderie Mine, Le Temple, Deux-Sèvres, Nouvelle-Aquitaine, France | La Commanderie Mine | Chauris et al. (1994) | PMGFRA_243 | from pg 262: "The lead-zinc veins (230-210 Ma, K-Ar dating) seem to be the youngest and the antimony veins are of intermediate age" |
Sample | Source Locality | Reference URL |
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