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Corella prospect, Honeymoon Well complex, Lake Way Station, Wiluna Shire, Western Australia, Australiai
Regional Level Types
Corella prospectDeposit
Honeymoon Well complexComplex
Lake Way StationLake
Wiluna ShireShire
Western AustraliaState
AustraliaCountry

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Latitude & Longitude (WGS84):
26° 53' 30'' South , 120° 23' 0'' East
Latitude & Longitude (decimal):
Type:
Köppen climate type:
Nearest Settlements:
PlacePopulationDistance
Wiluna680 (2012)36.9km
Mindat Locality ID:
268143
Long-form identifier:
mindat:1:2:268143:9
GUID (UUID V4):
0


Corella is in the north-east section of Honeymoon Well, 1400 metres strike and 20-100 metres wide. It is an undeveloped nickel deposit with an estimated resource of 53.5 mt @ 0.62% Ni.

The deposit shows a wide variety of olivine adcumulate, mesocumulate, orthocumulate, and minor spinifex textured flows. The flows produce unique rocks recrystallised under high temperature metamorphic conditions, occurring as fault bounded boudins. Because of intense shearing there is a higher density and thickness of veins in this prospect compared to the others. The orthocumulate shows pseudomorphed antigorite-carbonate, minor chromite, tremolite, chlorite, and rarely kaersuititic amphibole. The more olivine rich rocks have been altered to a lizardite-brucite-stichtite assemblage. In places it has been altered to non-pseudomorphed antigorite-carbonate, and talc-carbonate assemblages.

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Mineral List


8 valid minerals.

Rock Types Recorded

Note: data is currently VERY limited. Please bear with us while we work towards adding this information!

Select Rock List Type

Alphabetical List Tree Diagram

Detailed Mineral List:

ⓘ Antigorite
Formula: Mg3(Si2O5)(OH)4
ⓘ Brucite
Formula: Mg(OH)2
ⓘ 'Chlorite Group'
ⓘ Chromite
Formula: Fe2+Cr3+2O4
ⓘ 'Fayalite-Forsterite Series'
ⓘ Kaersutite
Formula: NaCa2(Mg3AlTi4+)(Si6Al2)O22O2
ⓘ Lizardite
Formula: Mg3(Si2O5)(OH)4
ⓘ Stichtite
Formula: Mg6Cr3+2(OH)16[CO3] · 4H2O
ⓘ Talc
Formula: Mg3Si4O10(OH)2
ⓘ Tremolite
Formula: ◻Ca2Mg5(Si8O22)(OH)2

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 4 - Oxides and Hydroxides
ⓘChromite4.BB.05Fe2+Cr3+2O4
ⓘBrucite4.FE.05Mg(OH)2
Group 5 - Nitrates and Carbonates
ⓘStichtite5.DA.50Mg6Cr3+2(OH)16[CO3] · 4H2O
Group 9 - Silicates
ⓘTremolite9.DE.10◻Ca2Mg5(Si8O22)(OH)2
ⓘKaersutite9.DE.15NaCa2(Mg3AlTi4+)(Si6Al2)O22O2
ⓘTalc9.EC.05Mg3Si4O10(OH)2
ⓘAntigorite9.ED.15Mg3(Si2O5)(OH)4
ⓘLizardite9.ED.15Mg3(Si2O5)(OH)4
Unclassified
ⓘ'Chlorite Group'-
ⓘ'Fayalite-Forsterite Series'-

List of minerals for each chemical element

HHydrogen
Hⓘ AntigoriteMg3(Si2O5)(OH)4
Hⓘ BruciteMg(OH)2
Hⓘ LizarditeMg3(Si2O5)(OH)4
Hⓘ StichtiteMg6Cr23+(OH)16[CO3] · 4H2O
Hⓘ TalcMg3Si4O10(OH)2
Hⓘ Tremolite◻Ca2Mg5(Si8O22)(OH)2
CCarbon
Cⓘ StichtiteMg6Cr23+(OH)16[CO3] · 4H2O
OOxygen
Oⓘ AntigoriteMg3(Si2O5)(OH)4
Oⓘ BruciteMg(OH)2
Oⓘ ChromiteFe2+Cr23+O4
Oⓘ KaersutiteNaCa2(Mg3AlTi4+)(Si6Al2)O22O2
Oⓘ LizarditeMg3(Si2O5)(OH)4
Oⓘ StichtiteMg6Cr23+(OH)16[CO3] · 4H2O
Oⓘ TalcMg3Si4O10(OH)2
Oⓘ Tremolite◻Ca2Mg5(Si8O22)(OH)2
Oⓘ Fayalite-Forsterite Series
NaSodium
Naⓘ KaersutiteNaCa2(Mg3AlTi4+)(Si6Al2)O22O2
MgMagnesium
Mgⓘ AntigoriteMg3(Si2O5)(OH)4
Mgⓘ BruciteMg(OH)2
Mgⓘ KaersutiteNaCa2(Mg3AlTi4+)(Si6Al2)O22O2
Mgⓘ LizarditeMg3(Si2O5)(OH)4
Mgⓘ StichtiteMg6Cr23+(OH)16[CO3] · 4H2O
Mgⓘ TalcMg3Si4O10(OH)2
Mgⓘ Tremolite◻Ca2Mg5(Si8O22)(OH)2
Mgⓘ Fayalite-Forsterite Series
AlAluminium
Alⓘ KaersutiteNaCa2(Mg3AlTi4+)(Si6Al2)O22O2
SiSilicon
Siⓘ AntigoriteMg3(Si2O5)(OH)4
Siⓘ KaersutiteNaCa2(Mg3AlTi4+)(Si6Al2)O22O2
Siⓘ LizarditeMg3(Si2O5)(OH)4
Siⓘ TalcMg3Si4O10(OH)2
Siⓘ Tremolite◻Ca2Mg5(Si8O22)(OH)2
Siⓘ Fayalite-Forsterite Series
CaCalcium
Caⓘ KaersutiteNaCa2(Mg3AlTi4+)(Si6Al2)O22O2
Caⓘ Tremolite◻Ca2Mg5(Si8O22)(OH)2
TiTitanium
Tiⓘ KaersutiteNaCa2(Mg3AlTi4+)(Si6Al2)O22O2
CrChromium
Crⓘ ChromiteFe2+Cr23+O4
Crⓘ StichtiteMg6Cr23+(OH)16[CO3] · 4H2O
FeIron
Feⓘ ChromiteFe2+Cr23+O4
Feⓘ Fayalite-Forsterite Series

Other Regions, Features and Areas containing this locality

Australia
Australian PlateTectonic Plate

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