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 | |||
Altaite (*) | Rocksalt | PbTe | 0 | 489 | |||
Anglesite (*) | Baryte | Pb(SO4) | 0 | 2734 | |||
Anhydrite (*) | Not in a structural group | Ca(SO4) | 0 | 1588 | |||
Aragonite (*) | Aragonite | Ca(CO3) | 0 | 3250 | |||
Arsenopyrite (*) | Arsenopyrite | FeAsS | 0 | 9052 | |||
Barrerite (*) | Stilbite | Na2(Si7Al2)O18·6H2O | 0 | 23 | |||
Baryte (*) | Baryte | Ba(SO4) | 0 | 11547 | |||
Beidellite (*) | Clay Smectite-vermiculite | (Na,Ca)0.3Al2(Si,Al)4O10(OH)2·nH2O | 0 | 85 | |||
Bismuthinite (*) | Stibnite | Bi2S3 | 0 | 1935 | |||
Brushite (*) | Gypsum | Ca(PO3OH)·2H2O | 0 | 104 | |||
Calcite (*) | Calcite | Ca(CO3) | 0 | 27770 | |||
Cerussite (*) | Aragonite | Pb(CO3) | 0 | 4979 | |||
Chalcocite (*) | None | Cu2S | 0 | 5707 | |||
Chalcopyrite (*) | Chalcopyrite | CuFeS2 | 0 | 27198 | |||
Chlorargyrite (*) | Rocksalt | AgCl | 0 | 1382 | |||
Chrysocolla (*) | Allophane | (Cu2-xAlx)H2-xSi2O5(OH)4·nH2O | 0 | 3531 | |||
Cinnabar (*) | None | HgS | 0 | 2600 | |||
Clausthalite (*) | Rocksalt | PbSe | 0 | 281 | |||
Covellite (*) | Covellite | CuS | 0 | 4165 | |||
Epsomite (*) | Epsomite | Mg(SO4)·7H2O | 0 | 484 | |||
Fluorite (*) | Fluorite | CaF2 | 0 | 9617 | |||
Galena (*) | Rocksalt | PbS | 0 | 24243 | |||
Gold (*) | Copper | Au | 0 | 30554 | |||
Gypsum (*) | Gypsum | Ca(SO4)·2H2O | 0 | 6890 | |||
Hessite (*) | None | Ag2Te | 0 | 804 | |||
Hexahydrite (*) | Hexahydrite | Mg(SO4)·6H2O | 0 | 251 | |||
Hodrušite (*) | None | Cu8Bi12S22 | 0 | 28 | |||
Jalpaite (*) | Jalpaite | Ag3CuS2 | 0 | 116 | |||
Kaolinite (*) | Clay Kaolinite | Al2Si2O5(OH)4 | 0 | 5591 | |||
Laumontite (*) | Not in a structural group | CaAl2Si4O12·4H2O | 0 | 1271 | |||
Lenaite (*) | Chalcopyrite | AgFeS2 | 0 | 8 | |||
Malachite (*) | Malachite | Cu2(CO3)(OH)2 | 0 | 12537 | |||
Marcasite (*) | Marcasite | FeS2 | 0 | 5674 | |||
Matildite (*) | None | AgBiS2 | 0 | 252 | |||
Montmorillonite (*) | Clay Smectite-vermiculite | (Na,Ca)0.3(Al,Mg)2Si4O10(OH)2·nH2O | 0 | 1508 | |||
Mordenite (*) | Mordenite | (Na2,Ca,K2)4(Al8Si40)O96·28H2O | 0 | 405 | |||
Muscovite (*) | Mica Clay | KAl2(Si3Al)O10(OH)2 | 0 | 17380 | |||
Opal (*) | Amorphous | SiO2·nH2O | 0 | 2994 | |||
Pearceite (*) | Polybasite | [Ag9CuS4][(Ag,Cu)6(As,Sb)2S7] | 0 | 249 | |||
Polybasite (*) | Polybasite | [Ag9CuS4][(Ag,Cu)6(Sb,As)2S7] | 0 | 716 | |||
Proustite (*) | None | Ag3AsS3 | 0 | 733 | |||
Pyrargyrite (*) | None | Ag3SbS3 | 0 | 1425 | |||
Pyrite (*) | Pyrite | FeS2 | 0 | 39462 | |||
Quartz (*) | Quartz | SiO2 | 0 | 61156 | |||
Salammoniac (*) | None | (NH4)Cl | 0 | 105 | |||
Sassolite (*) | None | B(OH)3 | 0 | 31 | |||
Scolecite (*) | Natrolite | Ca(Si3Al2)O10·3H2O | 0 | 390 | |||
Silver (*) | Copper | Ag | 0 | 5186 | |||
Sphalerite (*) | Sphalerite | ZnS | 0 | 21482 | |||
Stephanite (*) | None | Ag5SbS4 | 0 | 586 | |||
Sternbergite (*) | Cubanite | AgFe2S3 | 0 | 62 | |||
Tellurobismuthite (*) | Tetradymite | Bi2Te3 | 0 | 276 | |||
Tetradymite (*) | Tetradymite | Bi2Te2S | 0 | 510 | |||
Tetrahedrite-(Zn) (*) | Tetrahedrite | Cu6(Cu4Zn2)Sb4S13 | 0 | 5317 | |||
Xanthoconite (*) | Xanthoconite | Ag3AsS3 | 0 | 89 |
Sample | Source Locality | Reference URL |
---|---|---|
All locality data graciously provided by mindat.org
All age data...
Other copyright data...