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. |
Diaspore | None |
Graphite (*) | Groutite (*) |
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 |
---|---|---|---|---|---|---|---|
Graphite (*) | None | C | 2000 | 1800 | 0 | 2812 | |
Groutite (*) | Diaspore | Mn3+O(OH) | 2000 | 1800 | 0 | 72 |
Age ID | Locality Notes |
---|---|
Giersdorf_00001020 | Deposits are associated with a granitic gneiss dome and are stockwork-metasomatic deposit associated with alkaline metasomatism. The ore deposits cluster about centers of albitite bodies and are upward-branching lenses and stocks. Their thicknesses vary from 3-5 meters to tens of meters; they extend horizontally from tens to a few hundreds of meters and extend vertically for 1 km or more. |
Giersdorf_00001021 | Deposits are associated with a granitic gneiss dome and are stockwork-metasomatic deposit associated with alkaline metasomatism. The ore deposits cluster about centers of albitite bodies and are upward-branching lenses and stocks. Their thicknesses vary from 3-5 meters to tens of meters; they extend horizontally from tens to a few hundreds of meters and extend vertically for 1 km or more. |
Giersdorf_00001022 | Deposits are associated with a granitic gneiss dome and are stockwork-metasomatic deposit associated with alkaline metasomatism. The ore deposits cluster about centers of albitite bodies and are upward-branching lenses and stocks. Their thicknesses vary from 3-5 meters to tens of meters; they extend horizontally from tens to a few hundreds of meters and extend vertically for 1 km or more. |
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_00001022 | 2000 | 1800 | 2000-1800 | Yes | Brannerite, Uraninite | 271947 | Michurinske Deposit, Central Ukrainian Uranium Province, Kirovohrad Oblast, Ukraine | Michurisnk Deposit | Laverov et al. (1992) | 10.1080/00206819209465621 | IGR34_549 | Deposits formed from the late stage of early Proterozoic protoactivation which developed as a consequence of granitization (2 Ga.) and proceeded synchronously with emplacement of rapakivi granitic plutons in neighboring blocks. (1.8 Ga.) | |||||||||
Giersdorf_00001020 | 2000 | 1800 | 2000-1800 | Yes | Brannerite, Uraninite | 271956 | Severynka Deposit, Central Ukrainian Uranium Province, Kirovohrad Oblast, Ukraine | Severisnk Deposit | Laverov et al. (1992) | 10.1080/00206819209465621 | IGR34_549 | Deposits formed from the late stage of early Proterozoic protoactivation which developed as a consequence of granitization (2 Ga.) and proceeded synchronously with emplacement of rapakivi granitic plutons in neighboring blocks. (1.8 Ga.) | |||||||||
Giersdorf_00001021 | 2000 | 1800 | 2000-1800 | Yes | Brannerite, Uraninite | 271945 | Vatutinske Deposit, Central Ukrainian Uranium Province, Kirovohrad Oblast, Ukraine | Vatutinsk Deposit | Laverov et al. (1992) | 10.1080/00206819209465621 | IGR34_549 | Deposits formed from the late stage of early Proterozoic protoactivation which developed as a consequence of granitization (2 Ga.) and proceeded synchronously with emplacement of rapakivi granitic plutons in neighboring blocks. (1.8 Ga.) |
Sample | Source Locality | Reference URL |
---|---|---|
All locality data graciously provided by mindat.org
All age data...
Other copyright data...