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. |
Clinozoisite | Epidote | None | Quartz |
Epidote (*) | Quartz (*) |
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 |
---|---|---|---|---|---|---|---|
Epidote (*) | Epidote Clinozoisite | Ca2(Al2Fe3+)[Si2O7][SiO4]O(OH) | 2480 | 2450 | 0 | 8173 | |
Quartz (*) | Quartz | SiO2 | 2480 | 2450 | 0 | 61156 |
Age ID | Locality Notes |
---|---|
Giersdorf_00000222 | Model derived primarily from studies conducted in the Mount Tom Price mine but with supplemental information acquired from the Channar and Mount Whaleback |
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 | |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
Giersdorf_00000222 | 2480 | 2450 | 2480-2450 | Felsic and Mafic ages are indistinguishable through current dating techniques, suggesting bimodal volcanic activity in the area | Yes | 17597 | Mount Tom Price Mine, Tom Price, Ashburton Shire, Western Australia, Australia | Mount Tom Price Mine | Taylor et. al (2001) | 0361-0128/01/3161/837-37 | EG96_837 | BIF overlying the Brockman BIF, part of the Hamersley group, ages of the felsic and mafic units in this stratigraphy are indistinguishable from each other, suggesting a contemporaneous formation time. |
Sample | Source Locality | Reference URL |
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