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. |
Adelite | Alunite | Apatite | Aragonite | Baryte | Bismutite | Brackebuschite | Copper | Coronadite | Corundum |
Descloizite | Diaspore | Fornacite | Malachite | Mixite | None | Not in a structural group | Quartz | Scheelite | Wurtzite |
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 |
---|---|---|---|---|---|---|---|
Baryte (*) | Baryte | Ba(SO4) | 363 | 330.8 | 0 | 11547 | |
Bayldonite (*) | None | Cu3PbO(AsO3OH)2(OH)2 | 363 | 330.8 | 0 | 172 | |
Beudantite (*) | Alunite | PbFe3+3(AsO4)(SO4)(OH)6 | 363 | 330.8 | 0 | 413 | |
Bismutite (*) | Bismutite | Bi2O2(CO3) | 363 | 330.8 | 0 | 716 | |
Cerussite (*) | Aragonite | Pb(CO3) | 363 | 330.8 | 0 | 4979 | |
Clinobisvanite (*) | None | Bi(VO4) | 363 | 330.8 | 0 | 36 | |
Copper (*) | Copper | Cu | 363 | 330.8 | 0 | 3846 | |
Cryptomelane (*) | Coronadite | K(Mn4+7Mn3+)O16 | 363 | 330.8 | 0 | 599 | |
Cuprite (*) | Not in a structural group | Cu2O | 363 | 330.8 | 0 | 2970 | |
Duftite (*) | Adelite | PbCu(AsO4)(OH) | 363 | 330.8 | 0 | 220 | |
Gartrellite (*) | None | PbCuFe3+(AsO4)2(OH)·H2O | 363 | 330.8 | 0 | 41 | |
Goethite (*) | Diaspore | FeO(OH) | 363 | 330.8 | 0 | 7437 | |
Hematite (*) | Corundum | Fe2O3 | 363 | 330.8 | 0 | 14640 | |
Heyite (*) | Brackebuschite | Pb5Fe2+2O4(VO4)2 | 363 | 330.8 | 0 | 10 | |
Iodargyrite (*) | Wurtzite | AgI | 363 | 330.8 | 0 | 180 | |
Malachite (*) | Malachite | Cu2(CO3)(OH)2 | 363 | 330.8 | 0 | 12537 | |
Mimetite (*) | Apatite | Pb5(AsO4)3Cl | 363 | 330.8 | 0 | 1107 | |
Mixite (*) | Mixite | Cu6Bi(AsO4)3(OH)6·3H2O | 363 | 330.8 | 0 | 168 | |
Molybdofornacite (*) | Fornacite | CuPb2(MoO4)(AsO4)(OH) | 363 | 330.8 | 0 | 17 | |
Mottramite (*) | Descloizite | PbCu(VO4)(OH) | 363 | 330.8 | 0 | 362 | |
Plumbogummite (*) | Alunite | PbAl3(PO4)(PO3OH)(OH)6 | 363 | 330.8 | 0 | 170 | |
Pseudomalachite (*) | None | Cu5(PO4)2(OH)4 | 363 | 330.8 | 0 | 369 | |
Pyromorphite (*) | Apatite | Pb5(PO4)3Cl | 363 | 330.8 | 0 | 1725 | |
Quartz (*) | Quartz | SiO2 | 363 | 330.8 | 0 | 61156 | |
Reichenbachite (*) | None | Cu5(PO4)2(OH)4 | 363 | 330.8 | 0 | 26 | |
Tenorite (*) | None | CuO | 363 | 330.8 | 0 | 1101 | |
Vauquelinite (*) | None | CuPb2(CrO4)(PO4)(OH) | 363 | 330.8 | 0 | 63 | |
Wulfenite (*) | Scheelite | PbMoO4 | 363 | 330.8 | 0 | 1655 |
Age ID | Locality Notes |
---|---|
Giersdorf_00000964 | The Odenwald Granitoid Complex is a Variscan I-type granitoid that formed during subduction of the Rheic ocean and the collission of Avalonia and Armorica about 365 and 330 m.y.a. |
Giersdorf_00000984 | The Böllstein Odenwald is a unit found as part of the Odenwald Granodiorite Complex and is a garnet-bearing orthogneiss |
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 | |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
Giersdorf_00000964 | 334 | 330.8 | 332.4±1.6 | U-Pb | Yes | 1850 | Odenwald, Hesse, Germany | Odenwald Granitoid Complex | Siebel et al. (2012) | 10.1007/s00710-012-0200-3 | MP105_187 | U-Pb Zircon age for the Odenwald Granitoid | |||||||||
Giersdorf_00000984 | 363 | 351 | 357±6 | Lu-Hf | Age is part of the Part I of the Variscan Orogenic Event | Yes | 1850 | Odenwald, Hesse, Germany | Böllstein Odenwald | Siebel et al. (2012) | 10.1007/s00710-012-0200-3 | MP105_187 | Age is indicative of a high-pressure facies event in the footwall of the unit |
Sample | Source Locality | Reference URL |
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