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| 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. |
| Autunite | Clay | Copper | Diaspore | Feldspar | Fluorite | Mica | None | Not in a structural group | Phosphuranylite |
| Quartz |
| Anatase (*) | Annite (*) | Autunite (*) | Fluorite (*) | Goethite (*) |
| Gold (*) | Muscovite (*) | Orthoclase (*) | Phurcalite (*) | Quartz (*) |
| Torbernite (*) | Uraninite (*) | Uranophane-α (*) |
| 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 | 293 | 260 | 0 | 2162 | |
| Annite (*) | Mica Clay | KFe2+3(AlSi3O10)(OH)2 | 293 | 260 | 0 | 356 | |
| Autunite (*) | Autunite | Ca(UO2)2(PO4)2·10-12H2O | 293 | 260 | 0 | 1272 | |
| Fluorite (*) | Fluorite | CaF2 | 293 | 260 | 0 | 9617 | |
| Goethite (*) | Diaspore | FeO(OH) | 293 | 260 | 0 | 7437 | |
| Gold (*) | Copper | Au | 293 | 260 | 0 | 30554 | |
| Muscovite (*) | Mica Clay | KAl2(Si3Al)O10(OH)2 | 293 | 260 | 0 | 17380 | |
| Orthoclase (*) | Feldspar | K(AlSi3O8) | 293 | 260 | 0 | 2349 | |
| Phurcalite (*) | Phosphuranylite | Ca2(UO2)3O2(PO4)2·7H2O | 293 | 260 | 0 | 20 | |
| Quartz (*) | Quartz | SiO2 | 293 | 260 | 0 | 61156 | |
| Torbernite (*) | None | Cu(UO2)2(PO4)2·12H2O | 293 | 260 | 0 | 1059 | |
| Uraninite (*) | Fluorite | UO2 | 293 | 260 | 0 | 2718 | |
| Uranophane-α (*) | None | Ca(UO2)2(SiO3OH)2·5H2O | 293 | 260 | 0 | 890 |
| 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 | |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Lucy_040a | 281 | 279 | 280 ± 1 | Rb-Sr | Preferred Age determined in study | E 38425, E 38426, E 38427, E 38429, E 38430, E 420 | Yes | 1620 | Devon, England, UK | Dartmoor Granite | Darbyshire et al. (1985) | 10.1144/gsjgs.142.6.1159 | JGSL142_1159 | ||||||||
| Lucy_040b | 280 | 280 | 280 | Rb-Sr | Preliminary examindation yields age of Dartmoor as the second episode of Hercynian Magmatism. | Yes | 1620 | Devon, England, UK | Dartmoor Granite | Darbyshire et al. (1985) | 10.1144/gsjgs.142.6.1159 | JGSL142_1159 | Statistically acceptable whole rock and/or mineral isochrons were obtained for each of the granites studies and a preliminary inspection of the tata may suggst several episodes of of Hercynian magmatism in SW England. The first, c.. 290 generated the Carnmenellis, Bodmin and St Austell granites and was succeeded some 10 Ma by the Dartmoor grantie, and finally the intrusion of the Land's End granite at 270 Ma. The emplacement of the porphyry dyke and the main phase of mineralization, would then be closely associated with the second and third magmatic episodes. However more detailed examintation of the data and comparison with other work reveals certain major discrepencies in the hypothesis. | ||||||||
| Lucy_040c | 288 | 274 | 281 ± 7 | K-Ar | Previous age stated for the Dartmoor Granite | Yes | 1620 | Devon, England, UK | Dartmoor Granite | Darbyshire et al. (1985) | 10.1144/gsjgs.142.6.1159 | JGSL142_1159 | In complete aggreement with the plateau ages of the 282 Ma for the Coombestone Tor and Gidleigh Tor. | ||||||||
| Lucy_046 | 281 | 279 | 280 ± 1 | Rb-Sr | Age granite intruded | E 38431, E38432, E 38433, E38435, E 38436 | 1521 | Merrivale Quarry, Whitchurch, West Devon, Devon, England, UK | Merrivale Quarry | Darbyshire et al. (1985) | 10.1144/gsjgs.142.6.1159 | JGSL142_1159 | |||||||||
| Lucy_199 | 270 | 260 | 265 ± 5 | K-Ar | Previous stated isotopic age | biotite | 1521 | Merrivale Quarry, Whitchurch, West Devon, Devon, England, UK | Merrivale Quarry | Miller et al (1964) | 10.1002/gj.3350040109 | GJ4_105 | Isotopic ages on the granites and associated rocks of South-West England, data of previous workers (in m.yrs) | ||||||||
| Lucy_200 | 293 | 277 | 285 ± 8 | Rb-Sr | Previous stated isotopic age | biotite | 1521 | Merrivale Quarry, Whitchurch, West Devon, Devon, England, UK | Merrivale Quarry | Miller et al (1964) | 10.1002/gj.3350040109 | GJ4_105 | Isotopic ages on the granites and associated rocks of South-West England, data of previous workers (in m.yrs) |
| Sample | Source Locality | Reference URL |
|---|---|---|
All locality data graciously provided by mindat.org
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