2005
DOI: 10.1016/j.jvolgeores.2004.07.014
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Australia and Indonesia in collision: geochemical sources of magmatism

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Cited by 55 publications
(44 citation statements)
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“…Marini and Maury, 2005), Banda (e.g. Elburg et al, 2005;Nebel et al, 2011) and Bismarck (e.g. Holm and Richards, 2013;Woodhead et al, 2010;Cunningham et al, 2012) arcs, oblique subduction as in the northern Mariana arc (e.g.…”
Section: Death Of the Northern Assa By Terrane Collisionmentioning
confidence: 99%
“…Marini and Maury, 2005), Banda (e.g. Elburg et al, 2005;Nebel et al, 2011) and Bismarck (e.g. Holm and Richards, 2013;Woodhead et al, 2010;Cunningham et al, 2012) arcs, oblique subduction as in the northern Mariana arc (e.g.…”
Section: Death Of the Northern Assa By Terrane Collisionmentioning
confidence: 99%
“…The Banda Arc in the southeast of the study area is situated on the continental margin of the Sunda Shelf and has a particularly complex orogeny. The Banda Arc is separated into an inner volcanic arc, the subduction zone of the Australian plate, and an outer non-volcanic arc, which accreted in the Neogene to the Sunda shelf moving at the same rate as the Australian Plate (Elburg et al, 2005). The Outer Banda Arc was formed in the Permian to Quaternary ages and consists mainly of metamorphic and sedimentary rocks, with only a few igneous facies (Hall, 2002).…”
Section: Background: Geologymentioning
confidence: 99%
“…The magmatic evolution observed in active and recent arccontinent collisions on the west Pacific (e.g., Van Berger at al., 1993;Elburg and Foden, 1998;Elburg et al, 2002Elburg et al, , 2005Wang et al, 2004;Huang et al, 2006) provides important information to interpret ancient orogens as remnants of island arc-continent collision (e.g., Corriveau, 1990;Draut and Clift, 2001;Draut et al, 2002Draut et al, , 2009Brown et al, 2006;Chew et al, 2007;Gordienko et al, 2007, Van Staal et al, 2007.…”
Section: Arc-continent Collision and K-rich Magmatismmentioning
confidence: 99%
“…The enrichment of potassium and other incompatible elements in igneous rocks emplaced during arc-continent collision is interpreted as a consequence of progressive involvement of continental material (e.g., continental igneous and metamorphic rocks and passive margin sediments) (e.g., Elburg et al, 2005), melt contributions from an enriched/metasomatised sub-continental lithospheric mantle (e.g., Polvé et al, 1997;Draut et al, 2004;Wang et al, 2004), and fractional crystallization (Draut et al, 2009).…”
Section: Arc-continent Collision and K-rich Magmatismmentioning
confidence: 99%
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