Mineral Evolution Database
Created and maintained by the Mineral Evolution Project in partnership with RRUFF and mindat.
Mineral locality data provided by mindat.org



The Mineral Evolution database is currently under development.

The goal of this page is to present localities at which the mineral is found, and estimates of the oldest possible geologic age of the minerals at these localities.


Locality Name:
Lord Brassey Mine, Heazlewood District, Waratah-Wynyard Municipality, Tasmania, Australia

Oldest recorded age at locality: 541
Youngest recorded age at locality: 0.0117

mindat Locality ID: 5885
mindat URL: http://www.mindat.org/loc-5885.html

Tectonic Settings:

Total number of sublocalities beneath "Lord Brassey Mine, Heazlewood District, Waratah-Wynyard Municipality, Tasmania, Australia": 0
Total number of bottom-level sublocalities: 0

Latitude: 41°27'"S
Longitude: 145°17'60"E
Decimal Degree (lat, lon): -41.45,145.3

AThis mineral is Anthropogenic.
GThis mineral is directly dated.
BThis mineral is reported as having this age.
YThis mineral is using an age reported as an element mineralization period.
OThis mineral is using an age calculated from all data at the locality.
RThe age displayed for this mineral originates from a different, non-child locality.
PThe 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.

This Mineral list contains entries from this locality, including sub-localities. Minerals in bold are reported by mindat.org as occurring directly at this locality, and do not occur at any children (sublocalities) of this locality.

Elements at this locality, including sub-localities: Al C Ca Co Cu Fe H Mg Mo Na Ni O S Si 

Elements from minerals reported directly at this locality: Al C Ca Co Cu Fe H Mg Mo Na Ni O S Si 

Structural Groups for minerals in this locality: 
AmorphousAragoniteAuricuprideBruciteCalciteChloriteClayCovelliteDigeniteGarnet
HydrotalciteMalachiteMilleriteMolybdeniteNickelineNonePalygorskitePentlanditePerovskitePyrite
PyroxeneSepioliteSerpentineSmectite-vermiculiteSpinelTalcWoodwardite

41 IMA Minerals at location:
Andradite  (*)Antigorite  (*)Aragonite  (*)Awaruite  (*)Brucite  (*)
Chrysotile  (*)Clinochlore  (*)Cobaltpentlandite  (*)Covellite  (*)Digenite  (*)
Diopside  (*)Dypingite  (*)Enstatite  (*)Falcondoite  (*)Gaspéite  (*)
Heazlewoodite  (*)Hellyerite  (*)Hydrohonessite  (*)Lizardite  (*)Magnesite  (*)
Magnetite  (*)Millerite  (*)Molybdenite  (*)Népouite  (*)Nullaginite  (*)
Otwayite  (*)Palygorskite  (*)Pecoraite  (*)Pentlandite  (*)Polydymite  (*)
Pyrite  (*)Pyroaurite  (*)Pyrrhotite  (*)Reevesite  (*)Retgersite  (*)
Saponite  (*)Stevensite  (*)Talc  (*)Theophrastite  (*)Violarite  (*)
Zaratite  (*)
Mineral nameStructural GroupsIMA FormulaMax Age (Ma)Min Age (Ma)# of Sublocalities containing mineralLOCALITY IDs, not mindat ids# of localities containing mineral
Andradite  (*)GarnetCa3Fe3+2(SiO4)3419.2358.901534
Antigorite  (*)Serpentine ClayMg3Si2O5(OH)4419.2358.90708
Aragonite  (*)AragoniteCa(CO3)5410.011703250
Awaruite  (*)Auricupride PerovskiteNi3Fe419.2358.90166
Brucite  (*)BruciteMg(OH)25410.01170462
Chrysotile  (*)Serpentine ClayMg3Si2O5(OH)4419.2358.90951
Clinochlore  (*)Chlorite ClayMg5Al(AlSi3O10)(OH)85410.011701756
Cobaltpentlandite  (*)PentlanditeCo9S85410.0117082
Covellite  (*)CovelliteCuS5410.011704165
Digenite  (*)DigeniteCu1.8S5410.011701027
Diopside  (*)PyroxeneCaMgSi2O65410.011704135
Dypingite  (*)NoneMg5(CO3)4(OH)2·5H2O2.580.0117050
Enstatite  (*)PyroxeneMg2Si2O65410.01170944
Falcondoite  (*)Sepiolite ClayNi4Si6O15(OH)2·6H2O5410.011704
Gaspéite  (*)CalciteNi(CO3)5410.0117022
Heazlewoodite  (*)NoneNi3S2419.2358.90205
Hellyerite  (*)NoneNi(CO3)·6H2O2.580.011703
Hydrohonessite  (*)Woodwardite Hydrotalcite(Ni1-xFe3+x)(SO4)x/2(OH)2·nH2O (x < 0.5, n > 3x/2)5410.0117012
Lizardite  (*)Serpentine ClayMg3Si2O5(OH)45410.01170359
Magnesite  (*)CalciteMg(CO3)485.4382.701487
Magnetite  (*)SpinelFe2+Fe3+2O4485.4382.7014899
Millerite  (*)MilleriteNiS5410.011701066
Molybdenite  (*)MolybdeniteMoS25410.011705800
Népouite  (*)Serpentine ClayNi3Si2O5(OH)45410.0117066
Nullaginite  (*)MalachiteNi2(CO3)(OH)25410.011703
Otwayite  (*)NoneNi2(CO3)(OH)2·H2O2.580.011705
Palygorskite  (*)Palygorskite Clay(Mg,Al)2Si4O10(OH)·4H2O5410.01170306
Pecoraite  (*)Clay SerpentineNi3Si2O5(OH)45410.0117040
Pentlandite  (*)Pentlandite(Ni,Fe)9S85410.011701512
Polydymite  (*)SpinelNi2+Ni3+2S45410.01170131
Pyrite  (*)PyriteFeS25410.0117039462
Pyroaurite  (*)HydrotalciteMg6Fe3+2(CO3)(OH)16·4H2O5410.0117089
Pyrrhotite  (*)NickelineFe7S85410.011709056
Reevesite  (*)HydrotalciteNi6Fe3+2(CO3)(OH)16·4H2O2.580.0117048
Retgersite  (*)NoneNi(SO4)·6H2O5410.0117055
Saponite  (*)Clay Smectite-vermiculite(Ca,Na)0.3(Mg,Fe)3(Si,Al)4O10(OH)2·4H2O5410.01170301
Stevensite  (*)Clay(Ca,Na)xMg3-ySi4O10(OH)25410.0117057
Talc  (*)Clay TalcMg3Si4O10(OH)2485.4382.703337
Theophrastite  (*)BruciteNi(OH)22.580.011706
Violarite  (*)SpinelFeNi2S45410.01170380
Zaratite  (*)AmorphousNi3(CO3)(OH)4·4H2O2.580.0117056



Locality Notes from all Ages at Locality:
Age IDLocality Notes
Michelle_529Lord 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_530Lord 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_531Lord 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_532Lord 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.


4 Ages assigned to this locality:

Excel IDMax Age (Ma)Min Age (Ma)Age as listed in referenceDating MethodAge InterpretPrioritized?Sample SourceSample NumRun NumAge from other LocalityDated MineralMinerals explicitely stated as having this ageAge applies to these ElementsMinDat Locality IDDated Locality (Max Age)Location as listed in referenceReferenceReference DOIReference IDAge Notes
Michelle_529541485.4CambrianStratigraphyMagmatic age    Augite 5885Lord Brassey Mine, Heazlewood District, Waratah-Wynyard Municipality, Tasmania, AustraliaLord Brassey MineAnderson et al. (2002) MR33_321Age of primary mineralization of igneous host rocks. Little remains of this assemblage due to metamorphism.
Michelle_530485.4382.7Pre-mid-Devonian, possibly CambrianStratigraphyMetamorphic age    Epidote, Magnesite, Magnetite, Opal, Prehnite, Talc 5885Lord Brassey Mine, Heazlewood District, Waratah-Wynyard Municipality, Tasmania, AustraliaLord Brassey MineAnderson et al. (2002) MR33_321Age 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_531419.2358.9DevonianStratigraphyHydrothermal age    Andradite, Antigorite, Awaruite, Chrysotile, Heazlewoodite 5885Lord Brassey Mine, Heazlewood District, Waratah-Wynyard Municipality, Tasmania, AustraliaLord Brassey MineAnderson et al. (2002) MR33_321Age 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_5322.580.0117PleistoceneStratigraphySupergene and weathering age    Dypingite, Hellyerite, Otwayite, Reevesite, Theophrastite, Zaratite 5885Lord Brassey Mine, Heazlewood District, Waratah-Wynyard Municipality, Tasmania, AustraliaLord Brassey MineAnderson et al. (2002) MR33_321Age of weathering and supergene alteration. Exposure by glaciation and the following rapid erosion allowed the supergene and alteration mineralization.


SampleSource LocalityReference URL
R061050Lord Brassey Mine, Heazlewood District, Waratah-Wynyard Municipality, Tasmania, Australiahttps://rruff.info/R061050
R070699Lord Brassey Mine, Heazlewood District, Waratah-Wynyard Municipality, Tasmania, Australiahttps://rruff.info/R070699
R050268Lord Brassey Mine, Heazlewood District, Waratah-Wynyard Municipality, Tasmania, Australiahttps://rruff.info/R050268


All locality data graciously provided by mindat.org

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