Results 151 to 160 of about 411 (170)
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Recycling of oceanic crust and the origin of intraplate volcanism
Australian Journal of Earth Sciences, 2013Source models for intraplate volcanism (IPV) include vertical introduction of material from deep in the mantle (plume model), contamination of the shallow mantle (perisphere and continental mantle delamination models) and derivation by selective partial melting of oceanic crust recycled into the depleted mantle (SUMA/streaky mantle models).
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Intraplate Volcanism by Spontaneous Shallow Upper Mantle Melt Focusing
Intraplate volcanism signifies persistent magmatic activity within plate interiors far from active plate boundaries. However, due to limited assessment of the detailed physical conditions of the intraplate upper mantle, the fundamental mechanism behind the genesis of mantle magma remains poorly understood.Jung-Hun Song +3 more
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Temporal and geochemical evolution of the Cenozoic intraplate volcanism of Zealandia
Earth-Science Reviews, 2010Christian Timm +2 more
exaly
Cenozoic intraplate volcanism on New Zealand: Upwelling induced by lithospheric removal
Earth and Planetary Science Letters, 2006Kaj Hoernle +2 more
exaly
Intraplate volcanism in Eastern Australia and New Zealand
Journal of Structural Geology, 1992openaire +1 more source

