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. |
Acanthite | Arsenopyrite | Chalcopyrite | Copper | Corundum | Covellite | Digenite | Marcasite | Nickeline | None |
Not in a structural group | Polybasite | Pyrite | Quartz | Rocksalt | Sphalerite | Spinel | Uytenbogaardtite |
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 | 254 | 251.4 | 0 | 2793 | |
Arsenopyrite (*) | Arsenopyrite | FeAsS | 254 | 251.4 | 0 | 9052 | |
Bornite (*) | None | Cu5FeS4 | 254 | 251.4 | 0 | 5516 | |
Boulangerite (*) | None | Pb5Sb4S11 | 254 | 251.4 | 0 | 843 | |
Cervelleite (*) | None | Ag4TeS | 254 | 251.4 | 0 | 42 | |
Chalcocite (*) | None | Cu2S | 254 | 251.4 | 0 | 5707 | |
Chalcopyrite (*) | Chalcopyrite | CuFeS2 | 254 | 251.4 | 0 | 27198 | |
Covellite (*) | Covellite | CuS | 254 | 251.4 | 0 | 4165 | |
Digenite (*) | Digenite | Cu1.8S | 254 | 251.4 | 0 | 1027 | |
Galena (*) | Rocksalt | PbS | 254 | 251.4 | 0 | 24243 | |
Gold (*) | Copper | Au | 254 | 251.4 | 0 | 30554 | |
Hematite (*) | Corundum | Fe2O3 | 254 | 251.4 | 0 | 14640 | |
Magnetite (*) | Spinel | Fe2+Fe3+2O4 | 254 | 251.4 | 0 | 14899 | |
Marcasite (*) | Marcasite | FeS2 | 254 | 251.4 | 0 | 5674 | |
Naumannite (*) | Not in a structural group | Ag2Se | 254 | 251.4 | 0 | 192 | |
Polybasite (*) | Polybasite | [Ag9CuS4][(Ag,Cu)6(Sb,As)2S7] | 254 | 251.4 | 0 | 716 | |
Pyrite (*) | Pyrite | FeS2 | 254 | 251.4 | 0 | 39462 | |
Pyrrhotite (*) | Nickeline | Fe7S8 | 254 | 251.4 | 0 | 9056 | |
Quartz (*) | Quartz | SiO2 | 254 | 251.4 | 0 | 61156 | |
Silver (*) | Copper | Ag | 254 | 251.4 | 0 | 5186 | |
Sphalerite (*) | Sphalerite | ZnS | 254 | 251.4 | 0 | 21482 | |
Stromeyerite (*) | None | CuAgS | 254 | 251.4 | 0 | 332 | |
Stützite (*) | None | Ag5-xTe3 (x = 0.24-0.36) | 254 | 251.4 | 0 | 92 | |
Uytenbogaardtite (*) | Uytenbogaardtite | Ag3AuS2 | 254 | 251.4 | 0 | 46 |
Age ID | Locality Notes |
---|---|
Giersdorf_00000732 | Uranium of the Huemul Mine is primarily found as lenticular Cu-U-V deposits hosted by the Huemul Member of the Diamante formation. Orehosting facies are grey fluvial sandstones and conglomerates filling anastomosing paleochannels incised into pink pelitic beds. |
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 | |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
RC63_350_Don_Sixto | 254 | 251.4 | 252.7±1.3 | alteration-mineralization | adularia | 240563 | Don Sixto Project (El Pantanito), Agua Escondida, Malargüe Department, Mendoza Province, Argentina | Don Sixto | Mugas Lobos and Márquez‐Zavalía | 10.1111/rge.12014 | RG63_350 | ||||||||||
Giersdorf_00000732 | 29 | 29 | 29 | The suspected source for the Uranium in the area is Permo-Triassic felsic volcanics which were leached from the source rocks in the Mesozoic and early Tertiary periods as a result of denudation. | uraninite | Yes | Uraninite | Uraninite | U | 51086 | Huemul Mine, Pampa Amarilla District, Malargüe Department, Mendoza Province, Argentina | Huemul Mine | Dahlkamp (2010) | 10.1007/2F978-3-540-78943-7 | UDW_427 | Uranium is accompanied by Cu mineralization, which predates the U mineralization. |
Sample | Source Locality | Reference URL |
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