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. |
Baryte | None | Oxalate |
Baryte (*) | Whewellite (*) |
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 |
---|---|---|---|---|---|---|---|
Baryte (*) | Baryte | Ba(SO4) | 0 | 0 | 1 | 97843 | 11547 |
Whewellite (*) | Oxalate | Ca(C2O4)·H2O | 0 | 0 | 1 | 97843 | 66 |
Age ID | Locality Notes |
---|---|
Michelle_000568 | Pseudomorphs of barite (BaSO4) and Cd-rich ZnS after whewellite (CaC2O4·H2O) occur within remnants of Scots pine bark tissues in the peat layer of a poor fen located near a zinc smelter in south Poland |
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 | |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
Michelle_000568 | 0 | 0 | Recent | Age of uppermost peat layer | Baryte, Sphalerite, Whewellite | 270624 | Bagno Bruch Mire, Pyrzowice, Gmina Ożarowice, Tarnowskie Góry Co., Silesian Voivodeship, Poland | Bagno Bruch | Smieja-Król (2014) | 10.1007/s11356-014-2700-7 | ESPR21_7227 | As revealed by 210Pb dating, the uppermost peat layer (∼40 cm thick) in the fen has formed over the last 200 years, i.e., during the period of intense mining and heavy industry in Upper Silesia |
Sample | Source Locality | Reference URL |
---|---|---|
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