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. |
Arsenic | Feldspar | Garnet | Molybdenite | None | Quartz |
Albite (*) | Bismuth (*) | Microcline (*) | Molybdenite (*) | Quartz (*) |
Spessartine (*) |
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 |
---|---|---|---|---|---|---|---|
Albite (*) | Feldspar | Na(AlSi3O8) | 383 | 359 | 0 | 8803 | |
Bismuth (*) | Arsenic | Bi | 383 | 359 | 0 | 1966 | |
Microcline (*) | Feldspar | K(AlSi3O8) | 383 | 359 | 0 | 4924 | |
Molybdenite (*) | Molybdenite | MoS2 | 383 | 359 | 0 | 5800 | |
Quartz (*) | Quartz | SiO2 | 383 | 359 | 0 | 61156 | |
Spessartine (*) | Garnet | Mn2+3Al2(SiO4)3 | 383 | 359 | 0 | 1214 |
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 |
---|---|---|
All locality data graciously provided by mindat.org
All age data...
Other copyright data...