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 |
---|---|---|---|---|---|---|---|
Albite (*) | Feldspar | Na(AlSi3O8) | 0 | 8803 | |||
Ankerite (*) | None | Ca(Fe2+,Mg)(CO3)2 | 0 | 3092 | |||
Anthophyllite (*) | Amphibole | Mg2Mg5Si8O22(OH)2 | 1 | 32714 | 718 | ||
Antigorite (*) | Serpentine Clay | Mg3Si2O5(OH)4 | 0 | 708 | |||
Aragonite (*) | Aragonite | Ca(CO3) | 1 | 32714 | 3250 | ||
Arsenic (*) | Arsenic | As | 0 | 379 | |||
Arsenopyrite (*) | Arsenopyrite | FeAsS | 5 | 32712,32713,32715,32717,32718 | 9052 | ||
Augite (*) | Pyroxene | (Ca,Mg,Fe)2Si2O6 | 0 | 2060 | |||
Bismuth (*) | Arsenic | Bi | 1 | 32716 | 1966 | ||
Brochantite (*) | Brochantite | Cu4(SO4)(OH)6 | 1 | 32714 | 1633 | ||
Calaverite (*) | Melonite | AuTe2 | 1 | 32714 | 361 | ||
Calcite (*) | Calcite | Ca(CO3) | 2 | 32714,32718 | 27770 | ||
Chalcopyrite (*) | Chalcopyrite | CuFeS2 | 5 | 32712,32713,32714,32715,32716 | 27198 | ||
Chromite (*) | Spinel | Fe2+Cr2O4 | 1 | 32714 | 3902 | ||
Clinochlore (*) | Chlorite Clay | Mg5Al(AlSi3O10)(OH)8 | 0 | 1756 | |||
Clinozoisite (*) | Clinozoisite Epidote | Ca2Al3[Si2O7][SiO4]O(OH) | 0 | 1025 | |||
Covellite (*) | Covellite | CuS | 1 | 32714 | 4165 | ||
Epidote (*) | Epidote Clinozoisite | Ca2(Al2Fe3+)[Si2O7][SiO4]O(OH) | 1 | 32718 | 8173 | ||
Galena (*) | Rocksalt | PbS | 2 | 32712,32717 | 24243 | ||
Goethite (*) | Diaspore | FeO(OH) | 1 | 32715 | 7437 | ||
Gold (*) | Copper | Au | 5 | 32712,32713,32715,32716,32718 | 30554 | ||
Graphite (*) | None | C | 1 | 32718 | 2812 | ||
Hematite (*) | Corundum | Fe2O3 | 2 | 32714,32718 | 14640 | ||
Jarosite (*) | Alunite | KFe3+3(SO4)2(OH)6 | 1 | 32715 | 2228 | ||
Mackinawite (*) | None | (Fe,Ni)1+xS (x = 0-0.07) | 1 | 32714 | 451 | ||
Magnetite (*) | Spinel | Fe2+Fe3+2O4 | 1 | 32718 | 14899 | ||
Marcasite (*) | Marcasite | FeS2 | 1 | 32714 | 5674 | ||
Michenerite (*) | Ullmannite | PdBiTe | 1 | 32714 | 114 | ||
Microcline (*) | Feldspar | K(AlSi3O8) | 0 | 4924 | |||
Minnesotaite (*) | Clay Talc | Fe2+3Si4O10(OH)2 | 1 | 32718 | 61 | ||
Molybdenite (*) | Molybdenite | MoS2 | 1 | 32716 | 5800 | ||
Monazite-(Ce) (*) | Monazite | Ce(PO4) | 1 | 32718 | 945 | ||
Nickeline (*) | Nickeline | NiAs | 0 | 633 | |||
Palladium (*) | Copper | Pd | 0 | 59 | |||
Pentlandite (*) | Pentlandite | (Ni,Fe)9S8 | 1 | 32714 | 1512 | ||
Platinum (*) | Copper | Pt | 0 | 485 | |||
Pyrite (*) | Pyrite | FeS2 | 7 | 32712,32713,32714,32715,32716,32717,32718 | 39462 | ||
Pyrrhotite (*) | Nickeline | Fe7S8 | 3 | 32713,32714,32715 | 9056 | ||
Quartz (*) | Quartz | SiO2 | 6 | 32712,32713,32715,32716,32717,32718 | 61156 | ||
Silver (*) | Copper | Ag | 3 | 32712,32713,32716 | 5186 | ||
Sperrylite (*) | Pyrite | PtAs2 | 1 | 32714 | 337 | ||
Sphalerite (*) | Sphalerite | ZnS | 3 | 32712,32714,32717 | 21482 | ||
Stilpnomelane (*) | Stilpnomelane Clay | (K,Ca,Na)(Fe,Mg,Al)8(Si,Al)12(O,OH)36·nH2O | 1 | 32718 | 456 | ||
Talc (*) | Clay Talc | Mg3Si4O10(OH)2 | 1 | 32714 | 3337 | ||
Tetrahedrite-(Zn) (*) | Tetrahedrite | Cu6(Cu4Zn2)Sb4S13 | 1 | 32714 | 5317 | ||
Titanite (*) | Titanite | CaTi(SiO4)O | 0 | 4899 | |||
Tremolite (*) | Amphibole | Ca2(Mg5.0-4.5Fe2+0.0-0.5)Si8O22(OH)2 | 0 | 2562 | |||
Violarite (*) | Spinel | FeNi2S4 | 1 | 32714 | 380 | ||
Xenotime-(Y) (*) | Zircon | Y(PO4) | 1 | 32718 | 939 | ||
Zircon (*) | Zircon | Zr(SiO4) | 0 | 5251 |
Sample | Source Locality | Reference URL |
---|---|---|
All locality data graciously provided by mindat.org
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