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. |
Aeschynite | Amphibole | Apatite | Calcite | Chalcopyrite | Clay | Corundum | Humite | Mica | Nickeline |
None | Olivine | Pyrite | Pyroxene | Rocksalt | Rutile | Spinel | Titanite | Zirconolite |
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 |
---|---|---|---|---|---|---|---|
Aeschynite-(Ce) (*) | Aeschynite | (Ce,Ca,Fe,Th)(Ti,Nb)2(O,OH)6 | 281 | 252 | 0 | 43 | |
Calcite (*) | Calcite | Ca(CO3) | 281 | 252 | 0 | 27770 | |
Chalcopyrite (*) | Chalcopyrite | CuFeS2 | 281 | 252 | 0 | 27198 | |
Clinohumite (*) | Humite | Mg9(SiO4)4F2 | 281 | 252 | 0 | 236 | |
Diopside (*) | Pyroxene | CaMgSi2O6 | 281 | 252 | 0 | 4135 | |
Dolomite (*) | None | CaMg(CO3)2 | 281 | 252 | 0 | 9895 | |
Fluorapatite (*) | Apatite | Ca5(PO4)3F | 281 | 252 | 0 | 2740 | |
Forsterite (*) | Olivine | Mg2(SiO4) | 281 | 252 | 0 | 1188 | |
Galena (*) | Rocksalt | PbS | 281 | 252 | 0 | 24243 | |
Geikielite (*) | Corundum | MgTiO3 | 281 | 252 | 0 | 70 | |
Pargasite (*) | Amphibole | NaCa2(Mg4Al)(Si6Al2)O22(OH)2 | 281 | 252 | 0 | 313 | |
Phlogopite (*) | Mica Clay | KMg3(AlSi3O10)(OH)2 | 281 | 252 | 0 | 2273 | |
Pyrite (*) | Pyrite | FeS2 | 281 | 252 | 0 | 39462 | |
Pyrrhotite (*) | Nickeline | Fe7S8 | 281 | 252 | 0 | 9056 | |
Rutile (*) | Rutile | TiO2 | 281 | 252 | 0 | 5614 | |
Spinel (*) | Spinel | MgAl2O4 | 281 | 252 | 0 | 1934 | |
Titanite (*) | Titanite | CaTi(SiO4)O | 281 | 252 | 0 | 4899 | |
Zirconolite (*) | Zirconolite | (Ca,Y)Zr(Ti,Mg,Al)2O7 | 281 | 252 | 0 | 140 |
Age ID | Locality Notes |
---|---|
Giersdorf_00000651 | The Val Daone Conglomerate is a mid-Permian unit that runs through much of the south-central Alpine region. Some localities possess trace amounts of U and Cu. |
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_00000651 | 268 | 266 | late- to post-Kazanian | Biostratigraphy | Age is interpreted by the author as being linked to the "Mid Permian Event" which is a surge of tectonic activity that represents the final act of the Hercyanian/Variscan cycle | Yes | 24815 | Trento Province (Trentino), Trentino-Alto Adige, Italy | Trento Region | Cassinis et al. (2008) | IJG127_519 | Age of the Val Daone Conglomerate is expressed as Mid to Upper Permian, late to post Kazanian and possibly up into the lower Tatarian. The age is derived from palynological evidence as well as other paleontological sources compiled and given an estimated age. See fig. 11 | |||||||||
Giersdorf_00000652 | 276 | 273 | 276-273 | Biostratigraphy | Yes | 24815 | Trento Province (Trentino), Trentino-Alto Adige, Italy | Trento Region | Cassinis et al. (2008) | IJG127_519 | Age of the Treviogo is described as lower to middle Permian, mostly Kungarian. The age is derived from palynological evidence as well as other paleontological sources compiled and given an estimated age. See fig. 11 | ||||||||||
Giersdorf_00000653 | 281 | 277 | 281-277 | Biostratigraphy | Yes | 24815 | Trento Province (Trentino), Trentino-Alto Adige, Italy | Trento Region | Cassinis et al. (2008) | IJG127_519 | Age of the Collio Formation is described as lower Permian, mostly Artinskian. The numbers do not agree with the GSA's Arinskian age as the paper uses a different Time Scale. The age is derived from palynological evidence as well as other paleontological sources compiled and given an estimated age. See fig. 11 | ||||||||||
Giersdorf_00000654 | 266 | 252 | 266-252 | Biostratigraphy | Yes | 24815 | Trento Province (Trentino), Trentino-Alto Adige, Italy | Trento Region | Cassinis et al. (2008) | IJG127_519 | Age of the Verrucano formation is described as Upper Permian and Upper Tatarian. The age is derived from palynological evidence as well as other paleontological sources compiled and given an estimated age. See fig. 11 |
Sample | Source Locality | Reference URL |
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