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. |
Amphibole | Atacamite | Clay | Diaspore | Gypsum | Malachite | Mica | None | Oxalate | Quartz |
Rocksalt | Spinel | Talc | Taranakite |
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 |
---|---|---|---|---|---|---|---|
Anthophyllite (*) | Amphibole | Mg2Mg5Si8O22(OH)2 | 1 | 17985 | 718 | ||
Atacamite (*) | Atacamite | Cu2Cl(OH)3 | 0 | 0 | 1 | 17984 | 544 |
Birnessite (*) | None | (Na,Ca,K)0.6(Mn4+,Mn3+)2O4·1.5H2O | 2500 | 0 | 1 | 17984 | 178 |
Dolomite (*) | None | CaMg(CO3)2 | 2500 | 541 | 1 | 17984 | 9895 |
Goethite (*) | Diaspore | FeO(OH) | 2500 | 0 | 1 | 17984 | 7437 |
Gypsum (*) | Gypsum | Ca(SO4)·2H2O | 0 | 0 | 1 | 17984 | 6890 |
Halite (*) | Rocksalt | NaCl | 2500 | 0 | 1 | 17984 | 1398 |
Magnetite (*) | Spinel | Fe2+Fe3+2O4 | 1 | 17985 | 14899 | ||
Malachite (*) | Malachite | Cu2(CO3)(OH)2 | 2500 | 0 | 1 | 17984 | 12537 |
Muscovite (*) | Mica Clay | KAl2(Si3Al)O10(OH)2 | 1 | 17985 | 17380 | ||
Quartz (*) | Quartz | SiO2 | 2500 | 0 | 2 | 17984,17985 | 61156 |
Sampleite (*) | None | NaCaCu5(PO4)4Cl·5H2O | 0 | 0 | 1 | 17984 | 40 |
Talc (*) | Clay Talc | Mg3Si4O10(OH)2 | 1 | 17985 | 3337 | ||
Taranakite (*) | Taranakite | K3Al5(PO3OH)6(PO4)2·18H2O | 2500 | 0 | 1 | 17984 | 57 |
Todorokite (*) | None | (Na,Ca,K,Ba,Sr)1-x(Mn,Mg,Al)6O12·3-4H2O | 2500 | 0 | 1 | 17984 | 433 |
Weddellite (*) | Oxalate | Ca(C2O4)·2H2O | 0 | 0 | 1 | 17984 | 32 |
Age ID | Locality Notes |
---|---|
Michelle_826 | Unique mineralization derived from the alteration of copper sulphides in contact with guano deposits.The country rock is a partially silicified Proterozoic dolomite intruded by dolerite dykes. A small chalcopyrite vein found in the cave wall by R. Adams of Electrolytic Zinc Co. of Australia has been altered by phosphatic solutions from the avian and chiropterean guano deposits, resulting in crusts of atacamite with weddellite and minor sampleite coating the cliff face near the tunnel entrances. |
Michelle_827 | Country rock is a partially silicified Proterozoic dolomite intruded by dolerite dykes. A small chalcopyrite vein found in the cave wall by R. Adams of Electrolytic Zinc Co. of Australia has been altered by phosphatic solutions from the avian and chiropterean guano deposits, resulting in crusts of atacamite with weddellite and minor sampleite coating the cliff face near the tunnel entrances. |
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_826 | 0 | 0 | Recent | Age of surface mineralization | high | Atacamite, Gypsum, Sampleite, Weddellite | 134855 | Jingemia Cave, Moora Shire, Western Australia, Australia | Jingemia Cave | Bridge et al. (1978) | 10.1180/minmag.1978.042.323.07 | MM42_369 | Unique surface mineralization derived from the alteration of copper sulphides in contact with guano deposits. | ||||||||
Michelle_827 | 2500 | 541 | Proterozoic | Age of country rock | Dolomite | 134855 | Jingemia Cave, Moora Shire, Western Australia, Australia | Jingemia Cave | Bridge et al. (1978) | 10.1180/minmag.1978.042.323.07 | MM42_369 | Country rock is a partially silicified Proterozoic dolomite intruded by dolerite dykes. |
Sample | Source Locality | Reference URL |
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