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, 2013
Source 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).
openaire   +1 more source

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
openaire   +1 more source

Temporal and geochemical evolution of the Cenozoic intraplate volcanism of Zealandia

Earth-Science Reviews, 2010
Christian Timm   +2 more
exaly  

Cenozoic intraplate volcanism on New Zealand: Upwelling induced by lithospheric removal

Earth and Planetary Science Letters, 2006
Kaj Hoernle   +2 more
exaly  

SKS Splitting Measurements in NE China: New Insights Into the Wudalianchi Intraplate Volcanism and Mantle Dynamics

Journal of Geophysical Research: Solid Earth, 2020
Mingwen Lu, Jianshe Lei, Dapeng Zhao
exaly  

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