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. |
Atacamite | Chalcopyrite | Gypsum | None | Quartz | Zippeite |
Atacamite (*) | Chalcopyrite (*) | Gypsum (*) | Natrozippeite (*) | 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 |
---|---|---|---|---|---|---|---|
Atacamite (*) | Atacamite | Cu2Cl(OH)3 | 270 | 100 | 0 | 544 | |
Chalcopyrite (*) | Chalcopyrite | CuFeS2 | 270 | 100 | 0 | 27198 | |
Gypsum (*) | Gypsum | Ca(SO4)·2H2O | 270 | 100 | 0 | 6890 | |
Natrozippeite (*) | Zippeite | Na5(UO2)8(SO4)4O5(OH)3·12H2O | 270 | 100 | 0 | 41 | |
Quartz (*) | Quartz | SiO2 | 270 | 100 | 0 | 61156 |
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_081 | 270 | 100 | 270-100 | 40Ar - 39Ar | Lodes post-dating elvan intrusion and primary mineralization. | Yes | 1265 | St Just, Cornwall, England, UK | St Just | Hawkes et al. (1978 | US4_51 | Possibility of hydrothermal degassing of lode material around 210 Ma and 215 Ma which overprints a primary formation age of roughly 270 Ma. New mineral growth may have occurred close to 165 Ma with further hydrothermal activity at about 100 Ma. Adularia from veins in the Lizard Complex also provides indication |
Sample | Source Locality | Reference URL |
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