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. |
Apatite | Clay | Feldspar | Fluorite | Mica | Monazite | None | Not in a structural group | Pyrite | Quartz |
Sphalerite | Tourmaline |
Albite (*) | Bertrandite (*) | Fluorapatite (*) | Fluorite (*) | Monazite-(Ce) (*) |
Muscovite (*) | Pyrite (*) | Quartz (*) | Schorl (*) | Sphalerite (*) |
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 |
---|---|---|---|---|---|---|---|
Albite (*) | Feldspar | Na(AlSi3O8) | 294 | 276 | 1 | 119051 | 8803 |
Bertrandite (*) | Not in a structural group | Be4Si2O7(OH)2 | 294 | 276 | 1 | 119055 | 606 |
Fluorapatite (*) | Apatite | Ca5(PO4)3F | 294 | 276 | 1 | 119055 | 2740 |
Fluorite (*) | Fluorite | CaF2 | 294 | 276 | 1 | 119055 | 9617 |
Monazite-(Ce) (*) | Monazite | Ce(PO4) | 294 | 276 | 1 | 119055 | 945 |
Muscovite (*) | Mica Clay | KAl2(Si3Al)O10(OH)2 | 294 | 276 | 1 | 119051 | 17380 |
Pyrite (*) | Pyrite | FeS2 | 294 | 276 | 1 | 119055 | 39462 |
Quartz (*) | Quartz | SiO2 | 294 | 276 | 1 | 119055 | 61156 |
Schorl (*) | Tourmaline | NaFe2+3Al6(Si6O18)(BO3)3(OH)3(OH) | 294 | 276 | 1 | 119055 | 2705 |
Sphalerite (*) | Sphalerite | ZnS | 294 | 276 | 1 | 119055 | 21482 |
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_022a | 294 | 276 | 285 ± 9 | Rb-Sr data | Age granite intruded | C 1, C 1 KFeldpsar, C 1 Plag., C 1 Bio., C 1 Musc. | 260361 | Rosemanowas Quarry, Longdowns, Stithians, Cornwall, England, UK | Rosemanawas Quarry | Darbyshire et al. (1985) | 10.1144/gsjgs.142.6.1159 | JGSL142_1159 | |||||||||
Lucy_022b | 292 | 288 | 290 ± 2 | Rb-Sr data | C 1 mineral isochron appears to give a better estimate of the age of the Carnmenellis granite than the whole rock regression line. | C 1, C 1 KFeldpsar, C 1 Plag., C 1 Bio., C 1 Musc. | 260361 | Rosemanowas Quarry, Longdowns, Stithians, Cornwall, England, UK | Rosemanawas Quarry | Darbyshire et al. (1985) | 10.1144/gsjgs.142.6.1159 | JGSL142_1159 | Circuation of hydrothermal fluids thre does not appear to have caused widespread resetting. |
Sample | Source Locality | Reference URL |
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All locality data graciously provided by mindat.org
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