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. |
Feldspar | Garnet | None | Quartz |
Almandine (*) | Orthoclase (*) | Quartz (*) |
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 |
---|---|---|---|---|---|---|---|
Almandine (*) | Garnet | Fe2+3Al2(SiO4)3 | 290 | 210 | 0 | 2353 | |
Orthoclase (*) | Feldspar | K(AlSi3O8) | 290 | 210 | 0 | 2349 | |
Quartz (*) | Quartz | SiO2 | 290 | 210 | 0 | 61156 |
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. | Yes | 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. | Yes | 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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