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 |
---|---|---|---|---|---|---|---|
Acanthite (*) | Acanthite | Ag2S | 18 | 11.5 | 0 | 2793 | |
Albite (*) | Feldspar | Na(AlSi3O8) | 18 | 11.5 | 0 | 8803 | |
Anglesite (*) | Baryte | Pb(SO4) | 18 | 11.5 | 0 | 2734 | |
Ankerite (*) | None | Ca(Fe2+,Mg)(CO3)2 | 18 | 11.5 | 0 | 3092 | |
Argentopyrite (*) | Cubanite | AgFe2S3 | 18 | 11.5 | 0 | 53 | |
Arsenopyrite (*) | Arsenopyrite | FeAsS | 18 | 11.5 | 0 | 9052 | |
Calcite (*) | Calcite | Ca(CO3) | 18 | 11.5 | 0 | 27770 | |
Canfieldite (*) | Argyrodite | Ag8SnS6 | 18 | 11.5 | 0 | 91 | |
Cassiterite (*) | Rutile | SnO2 | 18 | 11.5 | 0 | 5171 | |
Cerussite (*) | Aragonite | Pb(CO3) | 18 | 11.5 | 0 | 4979 | |
Chalcopyrite (*) | Chalcopyrite | CuFeS2 | 18 | 11.5 | 0 | 27198 | |
Covellite (*) | Covellite | CuS | 18 | 11.5 | 0 | 4165 | |
Epidote (*) | Epidote Clinozoisite | Ca2(Al2Fe3+)[Si2O7][SiO4]O(OH) | 18 | 11.5 | 0 | 8173 | |
Famatinite (*) | Stannite Sphalerite | Cu3SbS4 | 18 | 11.5 | 0 | 163 | |
Galena (*) | Rocksalt | PbS | 18 | 11.5 | 0 | 24243 | |
Goethite (*) | Diaspore | FeO(OH) | 18 | 11.5 | 0 | 7437 | |
Gold (*) | Copper | Au | 18 | 11.5 | 0 | 30554 | |
Hematite (*) | Corundum | Fe2O3 | 18 | 11.5 | 0 | 14640 | |
Langisite (*) | Nickeline | CoAs | 18 | 11.5 | 0 | 4 | |
Magnetite (*) | Spinel | Fe2+Fe3+2O4 | 18 | 11.5 | 0 | 14899 | |
Muscovite (*) | Mica Clay | KAl2(Si3Al)O10(OH)2 | 18 | 11.5 | 0 | 17380 | |
Polybasite (*) | Polybasite | [Ag9CuS4][(Ag,Cu)6(Sb,As)2S7] | 18 | 11.5 | 0 | 716 | |
Proustite (*) | None | Ag3AsS3 | 18 | 11.5 | 0 | 733 | |
Pyrite (*) | Pyrite | FeS2 | 18 | 11.5 | 0 | 39462 | |
Pyrrhotite (*) | Nickeline | Fe7S8 | 18 | 11.5 | 0 | 9056 | |
Quartz (*) | Quartz | SiO2 | 18 | 11.5 | 0 | 61156 | |
Rammelsbergite (*) | Löllingite | NiAs2 | 18 | 11.5 | 0 | 233 | |
Sphalerite (*) | Sphalerite | ZnS | 18 | 11.5 | 0 | 21482 | |
Stephanite (*) | None | Ag5SbS4 | 18 | 11.5 | 0 | 586 | |
Tetrahedrite-(Zn) (*) | Tetrahedrite | Cu6(Cu4Zn2)Sb4S13 | 18 | 11.5 | 0 | 5317 | |
Xanthoconite (*) | Xanthoconite | Ag3AsS3 | 18 | 11.5 | 0 | 89 |
Age ID | Locality Notes |
---|---|
MP94_175_001 | The Apigania Bay vein system is hosted in marbles and schists of the Blueschist unit. Although the Apigania and Panormos Bay mineralizations are different by more than one feature; they share several geological, mineralogical, and geochemical attributes. These similarities suggest a common origin, but a different evolutionary phase of the same major ore event in the Tinos hydrothermal system. |
MP94_175_aureole | The Apigania Bay vein system is hosted in marbles and schists of the Blueschist unit. Although the Apigania and Panormos Bay mineralizations are different by more than one feature; they share several geological, mineralogical, and geochemical attributes. These similarities suggest a common origin, but a different evolutionary phase of the same major ore event in the Tinos hydrothermal system. |
MP94_175_rhyolitic_dykes | The Apigania Bay vein system is hosted in marbles and schists of the Blueschist unit. Although the Apigania and Panormos Bay mineralizations are different by more than one feature; they share several geological, mineralogical, and geochemical attributes. These similarities suggest a common origin, but a different evolutionary phase of the same major ore event in the Tinos hydrothermal system. |
MP94_175_Tinos_granodiorite | The Apigania Bay vein system is hosted in marbles and schists of the Blueschist unit. Although the Apigania and Panormos Bay mineralizations are different by more than one feature; they share several geological, mineralogical, and geochemical attributes. These similarities suggest a common origin, but a different evolutionary phase of the same major ore event in the Tinos hydrothermal system. |
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 | |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
MP94_175_001 | 14.1 | 13.9 | 14±0.1 | Rb-Sr | 192071 | Apigania Bay, Tinos Island, Tinos, South Aegean, Greece | Apigania Bay | Tombros et al. (2008) | 10.1007/s00710-008-0019-0 | MP94_175 | whole rock Rb–Sr isochrons from titanite and apatite | ||||||||||
MP94_175_aureole | 14 | 14 | ~14 | Rb-Sr | contact aureole formation | 192071 | Apigania Bay, Tinos Island, Tinos, South Aegean, Greece | Apigania Bay | Tombros et al. (2008) | 10.1007/s00710-008-0019-0 | MP94_175 | contact aureole formation | |||||||||
MP94_175_rhyolitic_dykes | 11.5 | 11.5 | 11.5 | K-Ar | Miocene ryolitic dikes | 192071 | Apigania Bay, Tinos Island, Tinos, South Aegean, Greece | Apigania Bay | Tombros et al. (2008) | 10.1007/s00710-008-0019-0 | MP94_175 | Miocene ryolitic dikes | |||||||||
MP94_175_Tinos_granodiorite | 18 | 15 | 18-15 | K-Ar | amphibole, biotite | 192071 | Apigania Bay, Tinos Island, Tinos, South Aegean, Greece | Apigania Bay | Tombros et al. (2008) | 10.1007/s00710-008-0019-0 | MP94_175 |
Sample | Source Locality | Reference URL |
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