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. |
Age ID | Locality Notes |
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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 | |
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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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