| 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. |
| Aluminite | Alumohydrocalcite | Calcite | Diaspore | Gypsum | Humboldtine | Marcasite | None | Oxalate | Pyrite |
| Starkeyite | Sulphur |
| Aluminite (*) | Alumohydrocalcite (*) | Calcite (*) | Dolomite (*) | Felsőbányaite (*) |
| Goethite (*) | Gypsum (*) | Humboldtine (*) | Marcasite (*) | Mellite (*) |
| Pyrite (*) | Rozenite (*) | Sulphur (*) | Whewellite (*) |
| 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 |
|---|---|---|---|---|---|---|---|
| Aluminite (*) | Aluminite | Al2(SO4)(OH)4·7H2O | 56 | 33.9 | 0 | 78 | |
| Alumohydrocalcite (*) | Alumohydrocalcite | CaAl2(CO3)2(OH)4·4H2O | 56 | 33.9 | 0 | 46 | |
| Calcite (*) | Calcite | Ca(CO3) | 56 | 33.9 | 0 | 27770 | |
| Dolomite (*) | None | CaMg(CO3)2 | 56 | 33.9 | 0 | 9895 | |
| Felsőbányaite (*) | None | Al4(SO4)(OH)10·4H2O | 56 | 33.9 | 0 | 66 | |
| Goethite (*) | Diaspore | FeO(OH) | 56 | 33.9 | 0 | 7437 | |
| Gypsum (*) | Gypsum | Ca(SO4)·2H2O | 56 | 33.9 | 0 | 6890 | |
| Humboldtine (*) | Humboldtine Oxalate | Fe2+(C2O4)·2H2O | 56 | 33.9 | 0 | 27 | |
| Marcasite (*) | Marcasite | FeS2 | 56 | 33.9 | 0 | 5674 | |
| Mellite (*) | None | Al2C6(COO)6·16H2O | 56 | 33.9 | 0 | 11 | |
| Pyrite (*) | Pyrite | FeS2 | 56 | 33.9 | 0 | 39462 | |
| Rozenite (*) | Starkeyite | Fe2+(SO4)·4H2O | 56 | 33.9 | 0 | 293 | |
| Sulphur (*) | Sulphur | S | 56 | 33.9 | 0 | 2045 | |
| Whewellite (*) | Oxalate | Ca(C2O4)·H2O | 56 | 33.9 | 0 | 66 |
| Age ID | Locality Notes |
|---|---|
| Michelle_707 | Mellite is formed from the reaction between organic carbon rich solutions with aluminosilicates. It is found but rarely in nature, occurring as crystalline prisms or pyramids with a resinous lustre as a secondary mineral in crevices in brown coal and lignite and sometime in association with gypsum in lignitic clays in Bohemia, Thuringia and Russia. This locality is near Tatabánya, Hungary. |
| Excel ID | Max Age (Ma) | Min Age (Ma) | Age as listed in reference | Dating Method | Age Interpret | Prioritized? | Sample Source | Sample Num | Run Num | Age from other Locality | Dated Mineral | Minerals explicitely stated as having this age | Age applies to these Elements | MinDat Locality ID | Dated Locality (Max Age) | Location as listed in reference | Reference | Reference DOI | Reference ID | Age Notes | |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Michelle_707 | 56 | 33.9 | Eocene | Age of mellite | Mellite | 1983 | Csordakúti Mine, Bicske-Csordakút, Bicske-Zsámbéki Basin, Fejér, Hungary | Csordakút Bicske | Jehlicka et al. (2006) | 10.1016/j.saa.2005.10.036 | SA65_229 | Age of mellite mineralization |
All locality data graciously provided by mindat.org
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