Search Results - "Brown, Stuart J.A."
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Physical volcanology and geochemistry of a Late Archaean volcanic arc: Kurnalpi and Gindalbie Terranes, Eastern Goldfields Superterrane, Western Australia
Published in Precambrian research (15-02-2008)“…Late Archaean (2715–2704 Ma) calc-alkaline volcanic complexes in the Kurnalpi Terrane are identical in facies and geochemistry to modern intra-arc volcanic…”
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SHRIMP U-Pb zircon age constraints on the Late Archaean tectonostratigraphic architecture of the Eastern Goldfields Superterrane, Yilgarn Craton, Western Australia
Published in Precambrian research (15-02-2008)“…Reassessment of Late Archaean tectonostratigraphic architecture of the Eastern Goldfields Superterrane is based on 35 new SHRIMP U-Pb zircon ages of…”
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Late Archaean synorogenic basins of the Eastern Goldfields Superterrane, Yilgarn Craton, Western Australia
Published in Precambrian research (01-02-2008)“…Siliciclastic supersequences of the Kalgoorlie and Gindalbie Terranes post-date ∼2660 Ma deformation, uplift and erosion associated with the amalgamation of…”
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Late Archaean synorogenic basins of the Eastern Goldfields Superterrane, Yilgarn Craton, Western Australia
Published in Precambrian research (01-02-2008)“…The Penny Dam, Belches, Yilgangi, White Hills, Granny, Royal, Lucky, Brock and Wallaby Supersequences of the Kurnalpi Terrane crop out in synclines that are…”
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Crystallisation history and crustal inheritance in a large silicic magma system: 206Pb/ 238U ion probe dating of zircons from the 1.2 Ma Ongatiti ignimbrite, Taupo Volcanic Zone
Published in Journal of volcanology and geothermal research (01-07-2004)“…Cathodoluminescence (CL) images of more than 300 zircons from the 1.21 Ma Ongatiti ignimbrite, Taupo Volcanic Zone (TVZ), reveal rare resorbed zircon cores…”
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Crystallisation ages in coeval silicic magma bodies: 238U– 230Th disequilibrium evidence from the Rotoiti and Earthquake Flat eruption deposits, Taupo Volcanic Zone, New Zealand
Published in Earth and planetary science letters (01-02-2003)“…The timescales over which moderate to large bodies of silicic magma are generated and stored are addressed here by studies of two geographically adjacent,…”
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