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 |
---|---|---|---|---|---|---|---|
Almandine (*) | Garnet | Fe2+3Al2(SiO4)3 | 363 | 330.8 | 0 | 2353 | |
Analcime (*) | Analcime | Na(AlSi2O6)·H2O | 363 | 330.8 | 0 | 1627 | |
Aragonite (*) | Aragonite | Ca(CO3) | 363 | 330.8 | 0 | 3250 | |
Arsenopyrite (*) | Arsenopyrite | FeAsS | 363 | 330.8 | 0 | 9052 | |
Baryte (*) | Baryte | Ba(SO4) | 363 | 330.8 | 0 | 11547 | |
Beryl (*) | Beryl | Be3Al2Si6O18 | 363 | 330.8 | 0 | 4286 | |
Bismuth (*) | Arsenic | Bi | 363 | 330.8 | 0 | 1966 | |
Bismuthinite (*) | Stibnite | Bi2S3 | 363 | 330.8 | 0 | 1935 | |
Bornite (*) | None | Cu5FeS4 | 363 | 330.8 | 0 | 5516 | |
Calcite (*) | Calcite | Ca(CO3) | 363 | 330.8 | 0 | 27770 | |
Chalcopyrite (*) | Chalcopyrite | CuFeS2 | 363 | 330.8 | 0 | 27198 | |
Devilline (*) | Devilline | CaCu4(SO4)2(OH)6·3H2O | 363 | 330.8 | 0 | 366 | |
Epidote (*) | Epidote Clinozoisite | Ca2(Al2Fe3+)[Si2O7][SiO4]O(OH) | 363 | 330.8 | 0 | 8173 | |
Galena (*) | Rocksalt | PbS | 363 | 330.8 | 0 | 24243 | |
Goethite (*) | Diaspore | FeO(OH) | 363 | 330.8 | 0 | 7437 | |
Gold (*) | Copper | Au | 363 | 330.8 | 0 | 30554 | |
Gypsum (*) | Gypsum | Ca(SO4)·2H2O | 363 | 330.8 | 0 | 6890 | |
Hematite (*) | Corundum | Fe2O3 | 363 | 330.8 | 0 | 14640 | |
Ilmenite (*) | Corundum | Fe2+Ti4+O3 | 363 | 330.8 | 0 | 5433 | |
Magnetite (*) | Spinel | Fe2+Fe3+2O4 | 363 | 330.8 | 0 | 14899 | |
Malachite (*) | Malachite | Cu2(CO3)(OH)2 | 363 | 330.8 | 0 | 12537 | |
Marcasite (*) | Marcasite | FeS2 | 363 | 330.8 | 0 | 5674 | |
Molybdenite (*) | Molybdenite | MoS2 | 363 | 330.8 | 0 | 5800 | |
Pharmacosiderite (*) | Pharmacosiderite | KFe3+4(AsO4)3(OH)4·6-7H2O | 363 | 330.8 | 0 | 428 | |
Prehnite (*) | Prehnite | Ca2Al(Si3Al)O10(OH)2 | 363 | 330.8 | 0 | 1898 | |
Pyrite (*) | Pyrite | FeS2 | 363 | 330.8 | 0 | 39462 | |
Pyrrhotite (*) | Nickeline | Fe7S8 | 363 | 330.8 | 0 | 9056 | |
Quartz (*) | Quartz | SiO2 | 363 | 330.8 | 0 | 61156 | |
Scheelite (*) | Scheelite | Ca(WO4) | 363 | 330.8 | 0 | 4894 | |
Scorodite (*) | None | Fe3+(AsO4)·2H2O | 363 | 330.8 | 0 | 1153 | |
Siderite (*) | Calcite | Fe(CO3) | 363 | 330.8 | 0 | 6417 | |
Sphalerite (*) | Sphalerite | ZnS | 363 | 330.8 | 0 | 21482 | |
Titanite (*) | Titanite | CaTi(SiO4)O | 363 | 330.8 | 0 | 4899 |
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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