| 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. |
| Allanite | Clay | Epidote | Feldspar | Fluorite | Mica | Molybdenite | None | Pyrite | Quartz |
| Rocksalt | Scheelite | Titanite | Zircon |
| Allanite-(Ce) (*) | Anorthite (*) | Fergusonite-(Y) (*) | Ferrimolybdite (*) | Galena (*) |
| Microcline (*) | Molybdenite (*) | Molybdite (*) | Muscovite (*) | Pyrite (*) |
| Quartz (*) | Titanite (*) | Uraninite (*) | Xenotime-(Y) (*) |
| 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 |
|---|---|---|---|---|---|---|---|
| Allanite-(Ce) (*) | Allanite Epidote | CaCe(Al2Fe2+)[Si2O7][SiO4]O(OH) | 0 | 706 | |||
| Anorthite (*) | Feldspar | Ca(Al2Si2O8) | 0 | 1036 | |||
| Fergusonite-(Y) (*) | Scheelite | YNbO4 | 0 | 196 | |||
| Ferrimolybdite (*) | None | Fe3+2(Mo6+O4)3·7H2O | 0 | 345 | |||
| Galena (*) | Rocksalt | PbS | 0 | 24243 | |||
| Microcline (*) | Feldspar | K(AlSi3O8) | 0 | 4924 | |||
| Molybdenite (*) | Molybdenite | MoS2 | 0 | 5800 | |||
| Molybdite (*) | None | MoO3 | 0 | 140 | |||
| Muscovite (*) | Mica Clay | KAl2(Si3Al)O10(OH)2 | 0 | 17380 | |||
| Pyrite (*) | Pyrite | FeS2 | 0 | 39462 | |||
| Quartz (*) | Quartz | SiO2 | 0 | 61156 | |||
| Titanite (*) | Titanite | CaTi(SiO4)O | 0 | 4899 | |||
| Uraninite (*) | Fluorite | UO2 | 0 | 2718 | |||
| Xenotime-(Y) (*) | Zircon | Y(PO4) | 0 | 939 |
All locality data graciously provided by mindat.org
All age data...
Other copyright data...