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 | Feldspar | Kaolinite | Lepidocrocite | Meta-autunite | Mica | None | Olivine | Pyrite |
Quartz | Rutile | Tourmaline |
Albite (*) | Autunite (*) | Kaolinite (*) | Lepidocrocite (*) | Meta-autunite (*) |
Microcline (*) | Muscovite (*) | Orthoclase (*) | Pyrite (*) | Pyrolusite (*) |
Quartz (*) | Schorl (*) | Torbernite (*) | Triphylite (*) |
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) | 0 | 8803 | |||
Autunite (*) | Autunite | Ca(UO2)2(PO4)2·10-12H2O | 0 | 1272 | |||
Kaolinite (*) | Clay Kaolinite | Al2Si2O5(OH)4 | 0 | 5591 | |||
Lepidocrocite (*) | Lepidocrocite | Fe3+O(OH) | 0 | 581 | |||
Meta-autunite (*) | Meta-autunite | Ca(UO2)2(PO4)2·6H2O | 0 | 388 | |||
Microcline (*) | Feldspar | K(AlSi3O8) | 0 | 4924 | |||
Muscovite (*) | Mica Clay | KAl2(Si3Al)O10(OH)2 | 0 | 17380 | |||
Orthoclase (*) | Feldspar | K(AlSi3O8) | 0 | 2349 | |||
Pyrite (*) | Pyrite | FeS2 | 0 | 39462 | |||
Pyrolusite (*) | Rutile | MnO2 | 0 | 3106 | |||
Quartz (*) | Quartz | SiO2 | 0 | 61156 | |||
Schorl (*) | Tourmaline | NaFe2+3Al6(Si6O18)(BO3)3(OH)3(OH) | 0 | 2705 | |||
Torbernite (*) | None | Cu(UO2)2(PO4)2·12H2O | 0 | 1059 | |||
Triphylite (*) | Olivine | LiFe2+(PO4) | 0 | 313 |
Sample | Source Locality | Reference URL |
---|---|---|
All locality data graciously provided by mindat.org
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