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. |
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 | |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
Emily000537 | 383 | 359 | late Ordovician to late Middle Devonian | stratigraphy | Yes | 26277 | Whipstick Mine (Jingera Mineral Co. Mine), Whipstick, Auckland Co., New South Wales, Australia | Whipstick Deposit | Rose G (1971) | GSNSW43_1 | Molybdenum bismuth ore bodies that bear uranium are hosted in Bega Granite which intrudes into Ordovician sediments, devonian sediments are later in age than the Bega Granite |
Sample | Source Locality | Reference URL |
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