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. |
Andalusite | Arsenopyrite | Beryl | Chalcopyrite | Clay | Clinozoisite | Copper | Corundum | Epidote | Fluorite |
Marcasite | Mica | None | Not in a structural group | Pyrite | Quartz | Rocksalt | Rutile | Spinel | Staurolite |
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 |
---|---|---|---|---|---|---|---|
Anatase (*) | Not in a structural group | TiO2 | 2 | 56476,56481 | 2162 | ||
Andalusite (*) | Andalusite | Al2SiO5 | 2 | 56476,56481 | 1310 | ||
Arsenopyrite (*) | Arsenopyrite | FeAsS | 1 | 56476 | 9052 | ||
Beryl (*) | Beryl | Be3Al2Si6O18 | 290 | 210 | 1 | 56477 | 4286 |
Cassiterite (*) | Rutile | SnO2 | 2 | 56476,56481 | 5171 | ||
Chalcopyrite (*) | Chalcopyrite | CuFeS2 | 290 | 210 | 0 | 27198 | |
Corundum (*) | Corundum | Al2O3 | 2 | 56476,56481 | 1797 | ||
Epidote (*) | Epidote Clinozoisite | Ca2(Al2Fe3+)[Si2O7][SiO4]O(OH) | 2 | 56476,56481 | 8173 | ||
Galena (*) | Rocksalt | PbS | 230 | 210 | 1 | 56479 | 24243 |
Gold (*) | Copper | Au | 290 | 210 | 1 | 56477 | 30554 |
Graphite (*) | None | C | 290 | 210 | 1 | 56478 | 2812 |
Ilmenite (*) | Corundum | Fe2+Ti4+O3 | 3 | 56476,56480,56481 | 5433 | ||
Kyanite (*) | Not in a structural group | Al2OSiO4 | 2 | 56476,56481 | 1507 | ||
Magnetite (*) | Spinel | Fe2+Fe3+2O4 | 2 | 56476,56481 | 14899 | ||
Marcasite (*) | Marcasite | FeS2 | 290 | 210 | 1 | 56479 | 5674 |
Muscovite (*) | Mica Clay | KAl2(Si3Al)O10(OH)2 | 290 | 210 | 1 | 56477 | 17380 |
Pyrite (*) | Pyrite | FeS2 | 290 | 210 | 3 | 56476,56479,56481 | 39462 |
Quartz (*) | Quartz | SiO2 | 290 | 210 | 2 | 56477,56480 | 61156 |
Rutile (*) | Rutile | TiO2 | 2 | 56476,56481 | 5614 | ||
Staurolite (*) | Staurolite | Fe2+2Al9Si4O23(OH) | 2 | 56476,56481 | 978 | ||
Uraninite (*) | Fluorite | UO2 | 290 | 270 | 1 | 56479 | 2718 |
Zircon (*) | Zircon | Zr(SiO4) | 2 | 56476,56481 | 5251 |
Age ID | Locality Notes |
---|---|
Giersdorf_00000661 | The Penaran Mine is located in the Guérande mining district and is part of the Armorican Massif. It has produced 470 tons of Uranium metal. |
Giersdorf_00000661a | The Penaran Mine is located in the Guérande mining district and is part of the Armorican Massif. It has produced 470 tons of Uranium metal. |
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_00000661 | 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 | 292955 | Pen Ar Ran, Piriac-sur-Mer, Loire-Atlantique, Pays De La Loire, France | Penaran 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_00000661a | 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 | 292955 | Pen Ar Ran, Piriac-sur-Mer, Loire-Atlantique, Pays De La Loire, France | Penaran 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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