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Bulong Ni Mine, Bulong Goldfield, Kalgoorlie-Boulder Shire, Western Australia, Australiai
Regional Level Types
Bulong Ni MineMine
Bulong GoldfieldOre Field
Kalgoorlie-Boulder ShireShire
Western AustraliaState
AustraliaCountry

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Latitude & Longitude (WGS84):
30° 41' 22'' South , 121° 48' 57'' East
Latitude & Longitude (decimal):
Type:
Nearest Settlements:
PlacePopulationDistance
Stoneville2,841 (2016)20.3km
Williamstown161 (2018)32.5km
Boulder5,178 (2017)32.7km
Kalgoorlie31,107 (2014)33.2km
Mindat Locality ID:
271527
Long-form identifier:
mindat:1:2:271527:1
GUID (UUID V4):
49f84eb2-450c-47aa-bdae-639a60dff39e


Nickel was the focus of attention at Bulong in the late 1990's, with far less success than the Bulong area gold chapter. In 1998 Preston Resources purchased the Bulong nickel deposit from Resolute Resources, in a complex deal for $319 million.

The ore is a laterite nickel deposit hosted in a nontronite clay zone. The intention was to pressure acid leach the material to extract the nickel. This technology had been used in Cuba since the 1950's, but had been unavailable for use elsewhere due to political reasons until the late 1990's. Few realised the technology as it stood at the time was unsuitable for most Western Australian laterite nickel deposits. Glowing reports were produced not only by the company, but independent media, about how another nickel boom was on the horizon, like that experienced in Western Australia in the early 1970's.

The process involves the ore going through an autoclave containing superheated acid at high pressure. The ore was having none of it. Magnesium at the deposit runs at 5-6% and is viewed in the process as an impurity which requires removal. More sulphuric acid was needed than anticipated, to the point they used up all available supplies in Western Australia, and had to import more at a high cost. The technology had worked in humid wet conditions, but the dry clay instead clogged the autoclave. The gypsum in the ore coated the pipes making them un-usable. Further, the nickel grade was only 1%, whereas the mines around Kambalda run at 3%. The high use of acid corroded parts of the processing plant that wasn't clogged. Costs skyrocketed, production levels plummeted. They persisted from 1998 to 2002, at which point the mine closed and Preston went into administration.

At the same time, the process was being used at two other Western Australian nickel mines with similar results. The Cawse nickel mine closed and Centaur Mining and Exploration sank under a sea of debt. The Murrin Murrin nickel mine run by Anaconda also ran into serious trouble. The shear size of this deposit probably saved it, and after the departure of Andrew 'Twiggy' Forrest, the mess was cleaned up. Twiggy went on to form Fortescue Metals, and become an iron ore squillionaire. Even as late as 2010, BHP abandoned its Raventhorpe laterite nickel project due to cost and processing issues.

At the time of writing (2012) Bulong is still in mothballs.

The Bulong Complex is a 37 kilometre long, folded and metamorphosed acid volcanoclastic, with an extensive tightly folded ultramafic rich sill zone. The structure has two opposite plunging synforms separated by an extensive saddle. Most of the sills are altered layered olivine rich rocks, with a few sills and rare dykes of altered pyroxenitic, gabbroic, dioritic and granophyric rocks. Large magma pulses produced olivine cumulate, and thin zones of pyroxene and pyroxene-plagioclase cumulate.

The altered layers are cumulate olivine and accessory cumulus chromite, in association with varying amounts of intercumular clinopyroxene, orthopyroxene, and plagioclase. Metaserpentinites form mesh textures, parallel vein texture, primary texture preservation, fibro-lamellar intergrowths, asbestos veins associated with magnetite, and abundant non-fibrous serpentine rich veins containing minor talc, carbonate, chlorite, amphibole, magnetite, and sulphide, associated with vesicular looking patches of dark green translucent serpentine. Antigorite is the dominant species with some chrysotile in weathered serpentine veins after relict olivine.

See also geology information for the Bulong North Complex Mindat listing, which contains the northern shallow pits.

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Commodity List

This is a list of exploitable or exploited mineral commodities recorded at this locality.


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:

β“˜ Antigorite
Formula: Mg3(Si2O5)(OH)4
β“˜ 'Chlorite Group'
β“˜ Chromite
Formula: Fe2+Cr3+2O4
β“˜ Chrysotile
Formula: Mg3(Si2O5)(OH)4
β“˜ 'Clinopyroxene Subgroup'
β“˜ 'Fayalite-Forsterite Series'
β“˜ Gypsum
Formula: CaSO4 · 2H2O
β“˜ Nontronite
Formula: Na0.3Fe2((Si,Al)4O10)(OH)2 · nH2O
β“˜ Opal
Formula: SiO2 · nH2O
β“˜ Opal var. Common Opal
Formula: SiO2 · nH2O
β“˜ 'Opalite'
β“˜ 'Orthopyroxene Subgroup'
β“˜ 'Plagioclase'
Formula: (Na,Ca)[(Si,Al)AlSi2]O8
β“˜ Quartz
Formula: SiO2
β“˜ Talc
Formula: Mg3Si4O10(OH)2

List of minerals arranged by Strunz 10th Edition classification

Group 4 - Oxides and Hydroxides
β“˜Chromite4.BB.05Fe2+Cr3+2O4
β“˜Quartz4.DA.05SiO2
β“˜Opal4.DA.10SiO2 Β· nH2O
β“˜var. Common Opal4.DA.10SiO2 Β· nH2O
Group 7 - Sulphates, Chromates, Molybdates and Tungstates
β“˜Gypsum7.CD.40CaSO4 Β· 2H2O
Group 9 - Silicates
β“˜Chrysotile9..Mg3(Si2O5)(OH)4
β“˜Talc9.EC.05Mg3Si4O10(OH)2
β“˜Nontronite9.EC.40Na0.3Fe2((Si,Al)4O10)(OH)2 Β· nH2O
β“˜Antigorite9.ED.15Mg3(Si2O5)(OH)4
Unclassified
β“˜'Chlorite Group'-
β“˜'Opalite'-
β“˜'Clinopyroxene Subgroup'-
β“˜'Fayalite-Forsterite Series'-
β“˜'Plagioclase'-(Na,Ca)[(Si,Al)AlSi2]O8
β“˜'Orthopyroxene Subgroup'-

List of minerals for each chemical element

HHydrogen
Hβ“˜ AntigoriteMg3(Si2O5)(OH)4
Hβ“˜ ChrysotileMg3(Si2O5)(OH)4
Hβ“˜ GypsumCaSO4 · 2H2O
Hβ“˜ NontroniteNa0.3Fe2((Si,Al)4O10)(OH)2 · nH2O
Hβ“˜ OpalSiO2 · nH2O
Hβ“˜ TalcMg3Si4O10(OH)2
Hβ“˜ Opal var. Common OpalSiO2 · nH2O
OOxygen
Oβ“˜ AntigoriteMg3(Si2O5)(OH)4
Oβ“˜ ChrysotileMg3(Si2O5)(OH)4
Oβ“˜ ChromiteFe2+Cr23+O4
Oβ“˜ GypsumCaSO4 · 2H2O
Oβ“˜ NontroniteNa0.3Fe2((Si,Al)4O10)(OH)2 · nH2O
Oβ“˜ OpalSiO2 · nH2O
Oβ“˜ QuartzSiO2
Oβ“˜ TalcMg3Si4O10(OH)2
Oβ“˜ Opal var. Common OpalSiO2 · nH2O
Oβ“˜ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
NaSodium
Naβ“˜ NontroniteNa0.3Fe2((Si,Al)4O10)(OH)2 · nH2O
Naβ“˜ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
MgMagnesium
Mgβ“˜ AntigoriteMg3(Si2O5)(OH)4
Mgβ“˜ ChrysotileMg3(Si2O5)(OH)4
Mgβ“˜ TalcMg3Si4O10(OH)2
AlAluminium
Alβ“˜ NontroniteNa0.3Fe2((Si,Al)4O10)(OH)2 · nH2O
Alβ“˜ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
SiSilicon
Siβ“˜ AntigoriteMg3(Si2O5)(OH)4
Siβ“˜ ChrysotileMg3(Si2O5)(OH)4
Siβ“˜ NontroniteNa0.3Fe2((Si,Al)4O10)(OH)2 · nH2O
Siβ“˜ OpalSiO2 · nH2O
Siβ“˜ QuartzSiO2
Siβ“˜ TalcMg3Si4O10(OH)2
Siβ“˜ Opal var. Common OpalSiO2 · nH2O
Siβ“˜ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
SSulfur
Sβ“˜ GypsumCaSO4 · 2H2O
CaCalcium
Caβ“˜ GypsumCaSO4 · 2H2O
Caβ“˜ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
CrChromium
Crβ“˜ ChromiteFe2+Cr23+O4
FeIron
Feβ“˜ ChromiteFe2+Cr23+O4
Feβ“˜ NontroniteNa0.3Fe2((Si,Al)4O10)(OH)2 · nH2O

Other Regions, Features and Areas containing this locality

Australia
Australian PlateTectonic Plate

This page contains all mineral locality references listed on mindat.org. This does not claim to be a complete list. If you know of more minerals from this site, please register so you can add to our database. This locality information is for reference purposes only. You should never attempt to visit any sites listed in mindat.org without first ensuring that you have the permission of the land and/or mineral rights holders for access and that you are aware of all safety precautions necessary.

References

 
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