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. |
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_083a | 220 | 210 | 220-210 | Early Hydrothermal events related to Lizard Plutons | adularia | 295239 | Lizard Complex, Cornwall, England, UK | Lizard Complex | Hawkes et al. (1978 | US4_51 | Adularia from veins in the Lizard Complex also provides indication of hydrothermal events around 210-220 Ma and 160-170 Ma | ||||||||||
Lucy_083b | 170 | 160 | 170-160 | Late Hydrothermal events related to Lizard Plutons | adularia | 295239 | Lizard Complex, Cornwall, England, UK | Lizard Complex | Hawkes et al. (1978 | US4_51 | Adularia from veins in the Lizard Complex also provides indication of hydrothermal events around 210-220 Ma and 160-170 Ma |
Sample | Source Locality | Reference URL |
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