Geo-Platinum 87 1988
DOI: 10.1007/978-94-009-1353-0_16
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Nickel-Copper and Precious Metal Mineralisation in the Caledonian Mafic and Ultramafic Intrusions of North-East Scotland

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“…These include: the New Rambler deposit, Wyoming (McCallum et al 1976); Rathbun Lake, Ontario (Rowell and Edgar 1986); the Bay of Islands Ophiolite Complex, Newfoundland (Lydon and Richardson 1988); the Cliff occurrence of the Unst Ophiolite, Shetland (Gunn et al 1985); Peter Lake, Saskatchewan (Hulbert et al 1988); mafic and ultramafic intrusions in Scotland (Fletcher 1988); serpentinites of the Eastern Central Alps (Burkhard et al 1988); the Donaldson West deposit, Quebec (Dillon-Leitch et al 1986); the Bou-Azzer ophiolite complex, Morocco (Fischer et al 1988); the Lac des lies Complex, Ontario (MacDonald 1988); the Bird River Sill, Manitoba ); the Niquelandia Complex, Brazil (Ferrario and Garuti 1988); the Acoje Ophiolite, the Philippines (Orberger et al 1988(Orberger et al , 1990; the Bravo Intrusion, Quebec (Barnes and Giovenazzo 1990); Blue Lake, Quebec (Beaudoin et al 1990); the Coldwell Lake Complex, Ontario (Ohnenstetter et al 1991); the Troodos Ophiolite, Cyprus (Prichard and Lord 1990); the Thetford Mines Ophiolite, Quebec (Tanguay et al 1990); the Salt Chuck intrusion, Alaska (Watkinson and Melling 1992) and the Coolac Serpentinite, Australia (Graham et al 1991). These include: the New Rambler deposit, Wyoming (McCallum et al 1976); Rathbun Lake, Ontario (Rowell and Edgar 1986); the Bay of Islands Ophiolite Complex, Newfoundland (Lydon and Richardson 1988); the Cliff occurrence of the Unst Ophiolite, Shetland (Gunn et al 1985); Peter Lake, Saskatchewan (Hulbert et al 1988); mafic and ultramafic intrusions in Scotland (Fletcher 1988); serpentinites of the Eastern Central Alps (Burkhard et al 1988); the Donaldson West deposit, Quebec (Dillon-Leitch et al 1986); the Bou-Azzer ophiolite complex, Morocco (Fischer et al 1988); the Lac des lies Complex, Ontario (MacDonald 1988); the Bird River Sill, Manitoba ); the Niquelandia Complex, Brazil (Ferrario and Garuti 1988); the Acoje Ophiolite, the Phi...…”
Section: Discussion and Geological Applicationsmentioning
confidence: 99%
“…These include: the New Rambler deposit, Wyoming (McCallum et al 1976); Rathbun Lake, Ontario (Rowell and Edgar 1986); the Bay of Islands Ophiolite Complex, Newfoundland (Lydon and Richardson 1988); the Cliff occurrence of the Unst Ophiolite, Shetland (Gunn et al 1985); Peter Lake, Saskatchewan (Hulbert et al 1988); mafic and ultramafic intrusions in Scotland (Fletcher 1988); serpentinites of the Eastern Central Alps (Burkhard et al 1988); the Donaldson West deposit, Quebec (Dillon-Leitch et al 1986); the Bou-Azzer ophiolite complex, Morocco (Fischer et al 1988); the Lac des lies Complex, Ontario (MacDonald 1988); the Bird River Sill, Manitoba ); the Niquelandia Complex, Brazil (Ferrario and Garuti 1988); the Acoje Ophiolite, the Philippines (Orberger et al 1988(Orberger et al , 1990; the Bravo Intrusion, Quebec (Barnes and Giovenazzo 1990); Blue Lake, Quebec (Beaudoin et al 1990); the Coldwell Lake Complex, Ontario (Ohnenstetter et al 1991); the Troodos Ophiolite, Cyprus (Prichard and Lord 1990); the Thetford Mines Ophiolite, Quebec (Tanguay et al 1990); the Salt Chuck intrusion, Alaska (Watkinson and Melling 1992) and the Coolac Serpentinite, Australia (Graham et al 1991). These include: the New Rambler deposit, Wyoming (McCallum et al 1976); Rathbun Lake, Ontario (Rowell and Edgar 1986); the Bay of Islands Ophiolite Complex, Newfoundland (Lydon and Richardson 1988); the Cliff occurrence of the Unst Ophiolite, Shetland (Gunn et al 1985); Peter Lake, Saskatchewan (Hulbert et al 1988); mafic and ultramafic intrusions in Scotland (Fletcher 1988); serpentinites of the Eastern Central Alps (Burkhard et al 1988); the Donaldson West deposit, Quebec (Dillon-Leitch et al 1986); the Bou-Azzer ophiolite complex, Morocco (Fischer et al 1988); the Lac des lies Complex, Ontario (MacDonald 1988); the Bird River Sill, Manitoba ); the Niquelandia Complex, Brazil (Ferrario and Garuti 1988); the Acoje Ophiolite, the Phi...…”
Section: Discussion and Geological Applicationsmentioning
confidence: 99%
“…7A, B): strong enrichment in LILE and Pb, slight enrichment in LREE with respect to HREE, and depletion of Nb and Ta (Perfit et al, 1980). The geodynamic context of the Aguablanca ore deposit, therefore, contrasts with most other Ni-Cu deposits that are closely related to rift settings (Lesher, 1997) and only rarely occur in compressive orogenic environments (e.g., the Moxie pluton: Thompson and Naldrett, 1984; the Caledonian intrusions of northeast Scotland : Fletcher, 1987; the Rana intrusion: Boyd and Mathisen, 1979). Recent geophysical studies of the southwest Iberian Peninsula (seismic reflection profile, IBERSEIS: Simancas et al, 2003) have revealed the presence of a thick, sill-like structure represented by a long high-amplitude reflective band in a midcrustal decollement.…”
Section: Genesis and Geodynamic Context Of The Aguablanca Ore Depositmentioning
confidence: 99%