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. |
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 |
---|---|---|---|---|---|---|---|
Acanthite (*) | Acanthite | Ag2S | 0 | 2793 | |||
Albite (*) | Feldspar | Na(AlSi3O8) | 0 | 8803 | |||
Ankerite (*) | None | Ca(Fe2+,Mg)(CO3)2 | 0 | 3092 | |||
Arsenopyrite (*) | Arsenopyrite | FeAsS | 0 | 9052 | |||
Autunite (*) | Autunite | Ca(UO2)2(PO4)2·10-12H2O | 0 | 1272 | |||
Baryte (*) | Baryte | Ba(SO4) | 0 | 11547 | |||
Bornite (*) | None | Cu5FeS4 | 0 | 5516 | |||
Boulangerite (*) | None | Pb5Sb4S11 | 0 | 843 | |||
Brannerite (*) | Brannerite | UTi2O6 | 0 | 248 | |||
Braunite (*) | Braunite | Mn2+Mn3+6O8(SiO4) | 0 | 483 | |||
Calcite (*) | Calcite | Ca(CO3) | 0 | 27770 | |||
Chalcopyrite (*) | Chalcopyrite | CuFeS2 | 0 | 27198 | |||
Cinnabar (*) | None | HgS | 0 | 2600 | |||
Cobaltite (*) | Cobaltite | CoAsS | 0 | 966 | |||
Coffinite (*) | Zircon | U(SiO4)·nH2O | 0 | 566 | |||
Covellite (*) | Covellite | CuS | 0 | 4165 | |||
Cristobalite (*) | Cristobalite | SiO2 | 0 | 453 | |||
Digenite (*) | Digenite | Cu1.8S | 0 | 1027 | |||
Dolomite (*) | None | CaMg(CO3)2 | 0 | 9895 | |||
Epidote (*) | Epidote Clinozoisite | Ca2(Al2Fe3+)[Si2O7][SiO4]O(OH) | 0 | 8173 | |||
Freieslebenite (*) | None | AgPbSbS3 | 0 | 105 | |||
Galena (*) | Rocksalt | PbS | 0 | 24243 | |||
Gold (*) | Copper | Au | 0 | 30554 | |||
Graphite (*) | None | C | 0 | 2812 | |||
Gypsum (*) | Gypsum | Ca(SO4)·2H2O | 0 | 6890 | |||
Hematite (*) | Corundum | Fe2O3 | 0 | 14640 | |||
Iron (*) | Iron | Fe | 0 | 1089 | |||
Jalpaite (*) | Jalpaite | Ag3CuS2 | 0 | 116 | |||
Lepidocrocite (*) | Lepidocrocite | Fe3+O(OH) | 0 | 581 | |||
Lillianite (*) | Lillianite | Pb3-2xAgxBi2+xS6 | 0 | 128 | |||
Magnetite (*) | Spinel | Fe2+Fe3+2O4 | 0 | 14899 | |||
Marcasite (*) | Marcasite | FeS2 | 0 | 5674 | |||
Monazite-(Ce) (*) | Monazite | Ce(PO4) | 0 | 945 | |||
Mordenite (*) | Mordenite | (Na2,Ca,K2)4(Al8Si40)O96·28H2O | 0 | 405 | |||
Muscovite (*) | Mica Clay | KAl2(Si3Al)O10(OH)2 | 0 | 17380 | |||
Gersdorffite-Pa3 (*) | Pyrite | NiAsS | 0 | 767 | |||
Perroudite (*) | None | Ag4Hg5S5(I,Br)2Cl2 | 0 | 23 | |||
Prehnite (*) | Prehnite | Ca2Al(Si3Al)O10(OH)2 | 0 | 1898 | |||
Proustite (*) | None | Ag3AsS3 | 0 | 733 | |||
Pyrite (*) | Pyrite | FeS2 | 0 | 39462 | |||
Pyrrhotite (*) | Nickeline | Fe7S8 | 0 | 9056 | |||
Quartz (*) | Quartz | SiO2 | 0 | 61156 | |||
Rutile (*) | Rutile | TiO2 | 0 | 5614 | |||
Scheelite (*) | Scheelite | Ca(WO4) | 0 | 4894 | |||
Senarmontite (*) | Arsenolite | Sb2O3 | 0 | 179 | |||
Siderite (*) | Calcite | Fe(CO3) | 0 | 6417 | |||
Silver (*) | Copper | Ag | 0 | 5186 | |||
Sphalerite (*) | Sphalerite | ZnS | 0 | 21482 | |||
Stibnite (*) | Stibnite | Sb2S3 | 0 | 3418 | |||
Stützite (*) | None | Ag5-xTe3 (x = 0.24-0.36) | 0 | 92 | |||
Tetrahedrite-(Zn) (*) | Tetrahedrite | Cu6(Cu4Zn2)Sb4S13 | 0 | 5317 | |||
Thorianite (*) | Fluorite | ThO2 | 0 | 236 | |||
Thorite (*) | Zircon | Th(SiO4) | 0 | 1006 | |||
Traskite (*) | None | Ba21Ca(Fe2+,Mn,Ti)4(Ti,Fe,Mg)12(Si12O36)(Si2O7)6(O,OH)30Cl6·14H2O | 0 | 4 | |||
Tridymite (*) | Tridymite | SiO2 | 0 | 458 | |||
Valentinite (*) | None | Sb2O3 | 0 | 369 | |||
Vyacheslavite (*) | None | U4+(PO4)(OH) | 0 | 8 | |||
Xanthoconite (*) | Xanthoconite | Ag3AsS3 | 0 | 89 | |||
Xenotime-(Y) (*) | Zircon | Y(PO4) | 0 | 939 | |||
Zircon (*) | Zircon | Zr(SiO4) | 0 | 5251 |
Sample | Source Locality | Reference URL |
---|---|---|
All locality data graciously provided by mindat.org
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