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| 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. |
| 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 |
|---|---|---|---|---|---|---|---|
| Andradite (*) | Garnet | Ca3Fe3+2(SiO4)3 | 419.2 | 358.9 | 0 | 1534 | |
| Antigorite (*) | Serpentine Clay | Mg3Si2O5(OH)4 | 419.2 | 358.9 | 0 | 708 | |
| Aragonite (*) | Aragonite | Ca(CO3) | 541 | 0.0117 | 0 | 3250 | |
| Awaruite (*) | Auricupride Perovskite | Ni3Fe | 419.2 | 358.9 | 0 | 166 | |
| Brucite (*) | Brucite | Mg(OH)2 | 541 | 0.0117 | 0 | 462 | |
| Chrysotile (*) | Serpentine Clay | Mg3Si2O5(OH)4 | 419.2 | 358.9 | 0 | 951 | |
| Clinochlore (*) | Chlorite Clay | Mg5Al(AlSi3O10)(OH)8 | 541 | 0.0117 | 0 | 1756 | |
| Cobaltpentlandite (*) | Pentlandite | Co9S8 | 541 | 0.0117 | 0 | 82 | |
| Covellite (*) | Covellite | CuS | 541 | 0.0117 | 0 | 4165 | |
| Digenite (*) | Digenite | Cu1.8S | 541 | 0.0117 | 0 | 1027 | |
| Diopside (*) | Pyroxene | CaMgSi2O6 | 541 | 0.0117 | 0 | 4135 | |
| Dypingite (*) | None | Mg5(CO3)4(OH)2·5H2O | 2.58 | 0.0117 | 0 | 50 | |
| Enstatite (*) | Pyroxene | Mg2Si2O6 | 541 | 0.0117 | 0 | 944 | |
| Falcondoite (*) | Sepiolite Clay | Ni4Si6O15(OH)2·6H2O | 541 | 0.0117 | 0 | 4 | |
| Gaspéite (*) | Calcite | Ni(CO3) | 541 | 0.0117 | 0 | 22 | |
| Heazlewoodite (*) | None | Ni3S2 | 419.2 | 358.9 | 0 | 205 | |
| Hellyerite (*) | None | Ni(CO3)·6H2O | 2.58 | 0.0117 | 0 | 3 | |
| Hydrohonessite (*) | Woodwardite Hydrotalcite | (Ni1-xFe3+x)(SO4)x/2(OH)2·nH2O (x < 0.5, n > 3x/2) | 541 | 0.0117 | 0 | 12 | |
| Lizardite (*) | Serpentine Clay | Mg3Si2O5(OH)4 | 541 | 0.0117 | 0 | 359 | |
| Magnesite (*) | Calcite | Mg(CO3) | 485.4 | 382.7 | 0 | 1487 | |
| Magnetite (*) | Spinel | Fe2+Fe3+2O4 | 485.4 | 382.7 | 0 | 14899 | |
| Millerite (*) | Millerite | NiS | 541 | 0.0117 | 0 | 1066 | |
| Molybdenite (*) | Molybdenite | MoS2 | 541 | 0.0117 | 0 | 5800 | |
| Népouite (*) | Serpentine Clay | Ni3Si2O5(OH)4 | 541 | 0.0117 | 0 | 66 | |
| Nullaginite (*) | Malachite | Ni2(CO3)(OH)2 | 541 | 0.0117 | 0 | 3 | |
| Otwayite (*) | None | Ni2(CO3)(OH)2·H2O | 2.58 | 0.0117 | 0 | 5 | |
| Palygorskite (*) | Palygorskite Clay | (Mg,Al)2Si4O10(OH)·4H2O | 541 | 0.0117 | 0 | 306 | |
| Pecoraite (*) | Clay Serpentine | Ni3Si2O5(OH)4 | 541 | 0.0117 | 0 | 40 | |
| Pentlandite (*) | Pentlandite | (Ni,Fe)9S8 | 541 | 0.0117 | 0 | 1512 | |
| Polydymite (*) | Spinel | Ni2+Ni3+2S4 | 541 | 0.0117 | 0 | 131 | |
| Pyrite (*) | Pyrite | FeS2 | 541 | 0.0117 | 0 | 39462 | |
| Pyroaurite (*) | Hydrotalcite | Mg6Fe3+2(CO3)(OH)16·4H2O | 541 | 0.0117 | 0 | 89 | |
| Pyrrhotite (*) | Nickeline | Fe7S8 | 541 | 0.0117 | 0 | 9056 | |
| Reevesite (*) | Hydrotalcite | Ni6Fe3+2(CO3)(OH)16·4H2O | 2.58 | 0.0117 | 0 | 48 | |
| Retgersite (*) | None | Ni(SO4)·6H2O | 541 | 0.0117 | 0 | 55 | |
| Saponite (*) | Clay Smectite-vermiculite | (Ca,Na)0.3(Mg,Fe)3(Si,Al)4O10(OH)2·4H2O | 541 | 0.0117 | 0 | 301 | |
| Stevensite (*) | Clay | (Ca,Na)xMg3-ySi4O10(OH)2 | 541 | 0.0117 | 0 | 57 | |
| Talc (*) | Clay Talc | Mg3Si4O10(OH)2 | 485.4 | 382.7 | 0 | 3337 | |
| Theophrastite (*) | Brucite | Ni(OH)2 | 2.58 | 0.0117 | 0 | 6 | |
| Violarite (*) | Spinel | FeNi2S4 | 541 | 0.0117 | 0 | 380 | |
| Zaratite (*) | Amorphous | Ni3(CO3)(OH)4·4H2O | 2.58 | 0.0117 | 0 | 56 |
| Age ID | Locality Notes |
|---|---|
| Michelle_529 | Lord Brassey Mine is known for unique nickel mineral assemblages. The Lord Brassey Mine can be divided into four unique stages of mineralization; magmatic, metamorphic, hydrothermal and supergene alteration. The magmatic stage formed minerals such as enstatite, forsterite, anorthite, augite, chromite. Little remains as this assemblage has largely been altered to form new minerals. |
| Michelle_530 | Lord Brassey Mine is known for unique nickel mineral assemblages. The Lord Brassey Mine can be divided into four unique stages of mineralization; magmatic, metamorphic, hydrothermal and supergene alteration. The metamorphic stage is either due to greenschist-facies burial or emplacement related metamorphism. The primary magmatic assemblage has largely transformed to serpentine, chlorite, amphibole, epidote, garnet, and minor prehnite, magnetite, talc, magnesite, opal and chalcedony. |
| Michelle_531 | Lord Brassey Mine is known for unique nickel mineral assemblages. The Lord Brassey Mine can be divided into four unique stages of mineralization; magmatic, metamorphic, hydrothermal and supergene alteration. Hydrothermal alteration occurs later in the Devonian, producing serpentinite and introducing nickel. It is thought that a Devonian granitic intrusion postdates the serpentinite, introducing calcium, talc magnesite veins and possibly molybdenite and veins of diopside. |
| Michelle_532 | Lord Brassey Mine is known for unique nickel mineral assemblages. The Lord Brassey Mine can be divided into four unique stages of mineralization; magmatic, metamorphic, hydrothermal and supergene alteration. Exposure by glaciation and the following rapid erosion allowed new supergene and alteration mineralization. |
| 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_529 | 541 | 485.4 | Cambrian | Stratigraphy | Magmatic age | Augite | 5885 | Lord Brassey Mine, Heazlewood District, Waratah-Wynyard Municipality, Tasmania, Australia | Lord Brassey Mine | Anderson et al. (2002) | MR33_321 | Age of primary mineralization of igneous host rocks. Little remains of this assemblage due to metamorphism. | |||||||||
| Michelle_530 | 485.4 | 382.7 | Pre-mid-Devonian, possibly Cambrian | Stratigraphy | Metamorphic age | Epidote, Magnesite, Magnetite, Opal, Prehnite, Talc | 5885 | Lord Brassey Mine, Heazlewood District, Waratah-Wynyard Municipality, Tasmania, Australia | Lord Brassey Mine | Anderson et al. (2002) | MR33_321 | Age of metamorphism. Age described as "Pre-mid-Devonian, possibly Cambrian." The metamorphic stage is either due to greenschist-facies burial or emplacement related metamorphism. | |||||||||
| Michelle_531 | 419.2 | 358.9 | Devonian | Stratigraphy | Hydrothermal age | Andradite, Antigorite, Awaruite, Chrysotile, Heazlewoodite | 5885 | Lord Brassey Mine, Heazlewood District, Waratah-Wynyard Municipality, Tasmania, Australia | Lord Brassey Mine | Anderson et al. (2002) | MR33_321 | Age of hydrothermal alteration. Age described as "latest stage of Devonian metamorphism." Hydrothermal alteration occurs later in the Devonian, producing serpentinite and introducing nickel. It is thought that a Devonian granitic intrusion postdates the serpentinite, introducing calcium, talc magnesite veins and possibly molybdenite and veins of diopside. | |||||||||
| Michelle_532 | 2.58 | 0.0117 | Pleistocene | Stratigraphy | Supergene and weathering age | Dypingite, Hellyerite, Otwayite, Reevesite, Theophrastite, Zaratite | 5885 | Lord Brassey Mine, Heazlewood District, Waratah-Wynyard Municipality, Tasmania, Australia | Lord Brassey Mine | Anderson et al. (2002) | MR33_321 | Age of weathering and supergene alteration. Exposure by glaciation and the following rapid erosion allowed the supergene and alteration mineralization. |
| Sample | Source Locality | Reference URL |
|---|---|---|
| R061050 | Lord Brassey Mine, Heazlewood District, Waratah-Wynyard Municipality, Tasmania, Australia | https://rruff.info/R061050 |
| R070699 | Lord Brassey Mine, Heazlewood District, Waratah-Wynyard Municipality, Tasmania, Australia | https://rruff.info/R070699 |
| R050268 | Lord Brassey Mine, Heazlewood District, Waratah-Wynyard Municipality, Tasmania, Australia | https://rruff.info/R050268 |
All locality data graciously provided by mindat.org
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