1981
DOI: 10.2113/gsecongeo.76.6.1330
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Nickel sulfide deposits in Western Australia; a review

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Cited by 41 publications
(23 citation statements)
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“…An excellent review of these nickel sulfide ores has been presented by Marston et al (1981), and the following details are summarized from their contribution. Geol., vol.…”
Section: Additional Aspects Of Greenstone Belt Metallogenymentioning
confidence: 99%
“…An excellent review of these nickel sulfide ores has been presented by Marston et al (1981), and the following details are summarized from their contribution. Geol., vol.…”
Section: Additional Aspects Of Greenstone Belt Metallogenymentioning
confidence: 99%
“…The petrogenetic affinity of the komatiites (see Nesbitt et al 1979) also does not appear to be critical (cf. Marston et al 1981). Although most important deposits are associated with aluminum-undepleted komatiites (e.g., Kambalda: Lesher et al 1981), some are associated with aluminum-depleted komatiites (e.g., Forrestania: Porter and McKay 1981;Ruth Well: Barley and Bickle 1982;E.…”
Section: Fundamental Featuresmentioning
confidence: 99%
“…Nesbitt (1971) and Naldrett and Cabri (1976) noted that some deposits contain concentrations of sulfides that are too great to have been dissolved in the overlying host units, and proposed that the sulfides were carried in suspension directly from the mantle. Under the assumption that the olivine in the host units is intratelluric, Ross and Hopkins (1975) and Marston et al (1981) suggested that immiscible sulfides and olivine crystals accumulated (in a subsurface magma chamber) prior to eruption, and that sulfides were erupted as a segregated phase.…”
Section: Introductionmentioning
confidence: 99%
“…at Kambalda (Marston et al 1981(Marston et al , p. 1354; and one deposit from Canada: Redstone (Robinson and Hutchinson 1982).…”
Section: Mineralized Rocksmentioning
confidence: 99%
“…apparently unique to the Arabian Shield. Examples of Ni deposits hosted by metasedimentary rocks outside of the Arabian Shield include the nearby presence of ultramafic flows or sills (see, for example, Marston et al 1981). In most of these deposits, Ni enrichment of sedimentary units is thought to occur by processes other than volcanic exhalation, such as metarnorphic remobilization of magmatic ore (Barrett et al 1977;Groves et al 1979).…”
Section: Introduction Anomalous Ni Concentrations In the Late Proteromentioning
confidence: 99%