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. |
Calcite | Chalcopyrite | None | Pyrite | Quartz | Rocksalt | Sphalerite |
Chalcopyrite (*) | Dolomite (*) | Galena (*) | Pyrite (*) | Quartz (*) |
Siderite (*) | Sphalerite (*) |
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 |
---|---|---|---|---|---|---|---|
Chalcopyrite (*) | Chalcopyrite | CuFeS2 | 405 | 270 | 0 | 27198 | |
Dolomite (*) | None | CaMg(CO3)2 | 405 | 270 | 0 | 9895 | |
Galena (*) | Rocksalt | PbS | 405 | 270 | 0 | 24243 | |
Pyrite (*) | Pyrite | FeS2 | 405 | 270 | 0 | 39462 | |
Quartz (*) | Quartz | SiO2 | 405 | 270 | 0 | 61156 | |
Siderite (*) | Calcite | Fe(CO3) | 405 | 270 | 0 | 6417 | |
Sphalerite (*) | Sphalerite | ZnS | 405 | 270 | 0 | 21482 |
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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