Each claim states how it is known and cites its evidence.
EstablishedMineral norms from 495 pulp samples, phases identified by XRD and reflectance IR; elements by XRF, detection limits 10 ppm (Ni, Co, Cr) and 20 ppm (Mn)
Reported for this deposit
The mineral abundances the report gives were calculated as mineral norms from 495 pulp samples, after phase identification by X-ray diffraction and reflectance infrared analysis. Its elemental figures for nickel, cobalt, manganese and chromium were obtained by X-ray fluorescence, with detection limits of 10 parts per million for nickel, cobalt and chromium and 20 parts per million for manganese.
- method: As stated by the report. The details of the norm calculation are said to be in Wells and Butt (2000), which Lithoen has not retrieved, so the method is named here and not described.
- assertion basis: SOURCE_REPORTED
Evidence support: Supported by the cited evidence · one source
Evidence: Wells 2003 · Peer-reviewed
Established0.064 wt%m Cobalt
Reported for this deposit
The reserve grade for cobalt at Murrin Murrin was estimated at 0.064 weight percent as of January 2001, over 304 million tonnes at a 0.8 percent nickel cut-off. The figure is the report’s citation of the Register of Australian Mining 2001/02.
- scope: reserveGrade
- effective date: January 2001, as the report states.
- definition basis: A 0.8 percent nickel cut-off, as stated. The grade is an average over the material above that cut-off and is not a property of the deposit independent of it. No analytical method is given for the reserve estimate; the report’s XRF figures are its own sampling and are a different thing.
- source record: Register of Australian Mining 2001/02 (2001), as cited by the report at p. 3.
- assertion basis: SOURCE_REPORTED
- reporting framework: None stated. The report gives no reporting code for this reserve — no JORC classification, no competent-person sign-off — and cites the Register of Australian Mining, which Lithoen has not retrieved. A reserve grade reported without a framework cannot be compared with one reported under a code.
Evidence support: Supported by the cited evidence · one source
Evidence: Wells 2003 · Peer-reviewed
EstablishedRecognised by USGS SIR 2010–5070–H as an example of the nickel-cobalt laterite class.
How a source classifies it
Lithoen records Murrin Murrin as a deposit because the USGS nickel-cobalt laterite deposit model names and describes it as an example of that class. The USGS nickel-cobalt laterite model calls Murrin Murrin a classic clay-ore nickel-cobalt laterite deposit.
- definition basis: Named and described in the model’s treatment of example deposits.
- assertion basis: SOURCE_CLASSIFICATION
Evidence support: Supported by the cited evidence · one source
Evidence: Marsh 2013 · Primary authority
Established28°50′S, 121°54′E — Laverton 1:250 000 (SH/51-2), NE Yilgarn Craton, ~60 km E of Leonora
Reported for this deposit
Murrin Murrin lies about 60 kilometres east of Leonora in the north-eastern Yilgarn Craton of Western Australia, at 28°50′ south and 121°54′ east on the Laverton 1:250 000 map sheet. The coordinate is authored to the nearest arc-minute, which is about 1.85 kilometres on the ground, and it locates the deposit area rather than any ore body within it.
- precision note: The report writes degrees and minutes and no seconds. Lithoen stores the decimal equivalent to four places and records one arc-minute, about 1,852 m, as the accuracy. The further decimal places are conversion residue and assert nothing.
- scope: The report gives one coordinate for a deposit it elsewhere describes as two separate areas of outcrop, MM2 and MM3. The point therefore represents the deposit area and not either ore body.
- assertion basis: SOURCE_REPORTED
Evidence support: Supported by the cited evidence · one source
Evidence: Wells 2003 · Peer-reviewed
EstablishedNi in smectitic clays and chlorite, less in serpentine and Mn oxides; Co in asbolan-like Mn oxides at the smectite–ferruginous contact
Reported for this deposit
Nickel and cobalt at Murrin Murrin sit in different minerals in different parts of the profile. Nickel-cobalt mineralisation is hosted mainly in the smectite and upper saprolite zones, with nickel carried chiefly by smectitic clays and chlorite and less by serpentine and manganese oxides. Cobalt is principally associated with manganese oxides at or near the contact of the smectite and ferruginous zones. Those oxides are asbolan-like, with a cobalt to nickel ratio typically 1:1 and a cobalt to manganese ratio of 0.33.
- assertion basis: SOURCE_REPORTED
- source verbatim: The report notes that the smectite at Murrin Murrin "is typically referred to as nontronite, but is strictly a Fe-rich dioctahedral smectite, being intermediate between … nontronite, beidellite and montmorillonite". Lithoen carries the general term smectite here rather than the species name the literature commonly uses, on the report’s own authority.
- precision note: Reported for this deposit; the ratios are attributed by the report to Wells and Butt (2000), which Lithoen has not retrieved.
Evidence support: Supported by the cited evidence · one source
Evidence: Wells 2003 · Peer-reviewed
Established1 wt%m Nickel
Reported for this deposit
The reserve grade for nickel at Murrin Murrin was estimated at 1.0 weight percent as of January 2001, over 304 million tonnes at a 0.8 percent nickel cut-off. The figure is the report’s citation of the Register of Australian Mining 2001/02.
- scope: reserveGrade
- effective date: January 2001, as the report states.
- definition basis: A 0.8 percent nickel cut-off, as stated. The grade is an average over the material above that cut-off and is not a property of the deposit independent of it. No analytical method is given for the reserve estimate; the report’s XRF figures are its own sampling and are a different thing.
- source record: Register of Australian Mining 2001/02 (2001), as cited by the report at p. 3.
- assertion basis: SOURCE_REPORTED
- reporting framework: None stated. The report gives no reporting code for this reserve — no JORC classification, no competent-person sign-off — and cites the Register of Australian Mining, which Lithoen has not retrieved. A reserve grade reported without a framework cannot be compared with one reported under a code.
Evidence support: Supported by the cited evidence · one source
Evidence: Wells 2003 · Peer-reviewed
InferredNo garnierite: an entirely serpentinised protolith, and possibly poor drainage.
How a source classifies it
Unlike many nickel-cobalt laterites there is no garnierite at Murrin Murrin. The USGS model attributes that to the parent rock being entirely serpentinised, and possibly to the relatively poor drainage of the Yilgarn craton. Cobalt occurs there in manganese oxides in the limonite zone and the upper part of the clay zone.
- precision note: The model gives these as attributions — "may be due to", "possibly" — and Lithoen carries them at that strength.
- assertion basis: SOURCE_CLASSIFICATION
Evidence support: Supported by the cited evidence · one source
Evidence: Marsh 2013 · Primary authority
Establishedsaprolite; smectite zone; ferruginous zone; calcrete
Reported for this deposit
Lateritic weathering at Murrin Murrin produced a profile of three units: saprolite at the base of weathering, overlain by a smectite zone, capped by a ferruginous zone, with calcrete interleaved with thin ferruginous hardcap developed in places at the top. Iron oxides make up only 5 to 10 percent of the minerals in the saprolite and lower smectite zones and rise sharply to 50 to 70 percent in the upper smectite and ferruginous zones.
- component: The percentages are of the mineral assemblage of each zone, not of the ore and not of any element. They come from norms calculated on 495 pulp samples, as the report’s footnote states.
- precision note: The three units are the report’s own division and it calls the division broad.
- assertion basis: SOURCE_REPORTED
Evidence support: Supported by the cited evidence · one source
Evidence: Wells 2003 · Peer-reviewed
Established304 Mt
Reported for this deposit
Ore reserves at Murrin Murrin were estimated at 304 million tonnes, at a cut-off grade of 0.8 percent nickel, as of January 2001. The figure is the report’s citation of the Register of Australian Mining 2001/02, not an estimate the report made.
- tonnage category: reportedReserve
- effective date: January 2001, as the report states.
- reporting framework: None stated. The report gives no reporting code — no JORC classification and no reserve category beyond the word "reserves" — and Lithoen supplies none. A reserve reported without a framework cannot be compared with one reported under a code.
- definition basis: A 0.8 percent nickel cut-off, as stated. The tonnage and the grades below are inseparable from that cut-off: at another cut-off they would be different numbers about the same rock.
- source record: Register of Australian Mining 2001/02 (2001), as cited by the report at p. 3. Lithoen has not retrieved the Register.
- assertion basis: SOURCE_REPORTED
Evidence support: Supported by the cited evidence · one source
Evidence: Wells 2003 · Peer-reviewed
EstablishedLateritic weathering of serpentinised komatiitic peridotite, Archaean Norseman-Wiluna greenstone belt; two outcrop areas MM2 and MM3
Reported for this deposit
Murrin Murrin formed by lateritic weathering of serpentinised peridotite — a komatiitic olivine cumulate — within the Archaean Norseman-Wiluna greenstone belt. Regional folding and NNE-striking, westerly dipping faults, offshoots of the Keith-Kilkenny fault, confine the ultramafic rocks to a NNE-striking sequence, and that deformation has left two areas of outcropping serpentinised peridotite: Murrin Murrin North, MM2, and Murrin Murrin South, MM3.
- assertion basis: SOURCE_REPORTED
- precision note: Reported for this deposit by a study of this deposit. The protolith and the structural setting are attributed by the report to Monti and Fazakerley (1996), which Lithoen has not retrieved.
Evidence support: Supported by the cited evidence · one source
Evidence: Wells 2003 · Peer-reviewed
ObservedMM2 profile locally influenced by faulting and shearing; MM3 not structurally controlled
Observed at this deposit
Structural control at Murrin Murrin is reported for one of its two deposits and explicitly denied for the other. The report states that profile development at MM2 is influenced locally by faulting and shearing, whereas that at MM3 is not structurally controlled. The distinction is the report’s own and is stated in those terms.
- assertion basis: SUBJECT_OBSERVED
- scope: The control is over the development of the weathering profile. The report does not say that faults localised the nickel, and no such statement is made here.
- precision note: Reported as observed at these two deposits by a study of them. It is not inherited from a laterite deposit model, and the report’s negative statement about MM3 is as much a finding as its positive one about MM2.
Evidence support: Supported by the cited evidence · one source
Evidence: Wells 2003 · Peer-reviewed
EstablishedMM2 (Murrin Murrin North) on Al-rich ortho- and meso-cumulates; MM3 (Murrin Murrin South) on Al-poor adcumulate
Reported for this deposit
Murrin Murrin is two deposits, not one. The report distinguishes Murrin Murrin North (MM2) from Murrin Murrin South (MM3) throughout, and reports different regolith mineralogy in each, which it attributes to a difference in the parent rock: MM2 formed on comparatively aluminium-rich ortho- and meso-cumulates and MM3 on an aluminium-poor adcumulate. Lithoen’s Murrin Murrin record did not come from a compilation row at all: it entered the corpus from the USGS nickel-cobalt laterite deposit model, which names Murrin Murrin as an example of the class and describes it as a single deposit.
- assertion basis: SOURCE_REPORTED
- precision note: The cumulate distinction is attributed by the report to Hill and others (1996) and the mineralogical difference to Wells and Butt (2000). Neither has been retrieved.
Evidence support: Supported by the cited evidence · one source
Evidence: Wells 2003 · Peer-reviewed
InferredTertiary and Mesozoic weathering events indicated by palaeomagnetic dating of ferruginised saprolite at MM2
Interpretation for this deposit
Palaeomagnetic dating of ferruginised saprolite at MM2 indicates both Tertiary and Mesozoic weathering events. No numerical age, no uncertainty and no published study accompany this: the report attributes it to a written communication of January 2000. Lithoen records it as an era-level statement resting on unpublished correspondence, and it should not be read as a determination that anyone can check.
- method: Palaeomagnetic dating, as stated. No laboratory, no sample count, no pole positions and no numerical result are given, and Lithoen supplies none.
- assertion basis: SUBJECT_INTERPRETED
- scope: Two named eras, not an age. "Tertiary and Mesozoic" spans roughly 250 to 2.6 million years ago; the statement is that weathering happened in both, not that it happened throughout.
- precision note: A written communication from B. Pillans, CRC LEME / ANU, January 2000, cited by the report. It is not a published determination and there is nothing to retrieve.
- precision note: Recorded as SUBJECT_INTERPRETED rather than SUBJECT_MEASURED. Palaeomagnetic poles are measured; geological eras are read off them. What this claim carries is what the dating was taken to indicate, and no measured value appears in the report at all.
Evidence support: Supported by the cited evidence · one source
Evidence: Wells 2003 · Peer-reviewed