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. |
Clay | Feldspar | Mica | None | Not in a structural group | Quartz | Rutile | Titanite | Zircon |
Albite (*) | Muscovite (*) | Orthoclase (*) | Quartz (*) | Rutile (*) |
Sillimanite (*) | Titanite (*) | Zircon (*) |
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) | 405 | 270 | 0 | 8803 | |
Muscovite (*) | Mica Clay | KAl2(Si3Al)O10(OH)2 | 405 | 270 | 0 | 17380 | |
Orthoclase (*) | Feldspar | K(AlSi3O8) | 405 | 270 | 0 | 2349 | |
Quartz (*) | Quartz | SiO2 | 405 | 270 | 0 | 61156 | |
Rutile (*) | Rutile | TiO2 | 405 | 270 | 0 | 5614 | |
Sillimanite (*) | Not in a structural group | Al2SiO5 | 405 | 270 | 0 | 1516 | |
Titanite (*) | Titanite | CaTi(SiO4)O | 405 | 270 | 0 | 4899 | |
Zircon (*) | Zircon | Zr(SiO4) | 405 | 270 | 0 | 5251 |
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 | |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
Kristen002524 | 405 | 270 | Hercynian Orogeny | Yes | Pb, Zn, Cu, Ag | 46301 | Aveiro, Portugal | Aviero District | Marques de Sá et al. (2014) | 10.1016/j.oregeorev.2014.03.001 | OGR62_54 | studied depoists correspond to veins emplaced in E-W fractures, generated late relatively to the Hercynian orogeny |
Sample | Source Locality | Reference URL |
---|---|---|
All locality data graciously provided by mindat.org
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