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. |
Corundum | None |
Hematite (*) |
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 |
---|---|---|---|---|---|---|---|
Hematite (*) | Corundum | Fe2O3 | 363 | 330.8 | 1 | 59332 | 14640 |
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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