Add to ORKGMelts ascending from deep reservoirs and trapped beneath thick lithosphere exchange heat with and partially melt the shallow mantle as they crystallize. Basalts erupting through thick lithosphere are more likely to have experienced deep crystal fractionation and contamination than those at mature spreading centres. Geochemical data for ocean island and other hotspot magmas do not require a primitive or lower mantle source
International audienceMid-ocean ridge basalt (MORB) is the most abundant magma on Earth, and provide...
We show that there is a strong and consistent correlation between geochemical and geophysical estima...
Early studies of mid-ocean ridge discontinuities, such as transform faults and overlapping spreading...
Melts ascending from deep reservoirs and trapped beneath thick lithosphere exchange heat with and pa...
The formation of basaltic crust at mid-ocean ridges and ocean islands provides a window into the com...
The trace element concentration patterns of continental and ocean island basalts and of mid-ocean ri...
The presence in the Earth’s mantle of even small amounts of water and other volatiles has major effe...
Large igneous provinces (LIPs) such as continental flood basalt (CFB) and oceanic plateau basalt (O...
The Earth’s lithosphere can focus basaltic magmatism along pre-existing weakness zones or discontinu...
Hotspots and hotspot tracks are on, or start on, preexisting lithospheric features such as fracture ...
So-called hotspot magmas, including ocean island basalts and continental flood basalts, differ iso...
Artículo de publicación ISISeismic refraction studies of deep-crustal and upper mantle structure ben...
ocean island basalts major element chemistry lithosphere–asthenosphere boundary mantle heterogeneity...
International audienceEarth is a thermal engine that dissipates its internal heat primarily through ...
Basaltic magmatism that builds intra-plate ocean islands is often considered to be genetically assoc...
International audienceMid-ocean ridge basalt (MORB) is the most abundant magma on Earth, and provide...
We show that there is a strong and consistent correlation between geochemical and geophysical estima...
Early studies of mid-ocean ridge discontinuities, such as transform faults and overlapping spreading...
Melts ascending from deep reservoirs and trapped beneath thick lithosphere exchange heat with and pa...
The formation of basaltic crust at mid-ocean ridges and ocean islands provides a window into the com...
The trace element concentration patterns of continental and ocean island basalts and of mid-ocean ri...
The presence in the Earth’s mantle of even small amounts of water and other volatiles has major effe...
Large igneous provinces (LIPs) such as continental flood basalt (CFB) and oceanic plateau basalt (O...
The Earth’s lithosphere can focus basaltic magmatism along pre-existing weakness zones or discontinu...
Hotspots and hotspot tracks are on, or start on, preexisting lithospheric features such as fracture ...
So-called hotspot magmas, including ocean island basalts and continental flood basalts, differ iso...
Artículo de publicación ISISeismic refraction studies of deep-crustal and upper mantle structure ben...
ocean island basalts major element chemistry lithosphere–asthenosphere boundary mantle heterogeneity...
International audienceEarth is a thermal engine that dissipates its internal heat primarily through ...
Basaltic magmatism that builds intra-plate ocean islands is often considered to be genetically assoc...
International audienceMid-ocean ridge basalt (MORB) is the most abundant magma on Earth, and provide...
We show that there is a strong and consistent correlation between geochemical and geophysical estima...
Early studies of mid-ocean ridge discontinuities, such as transform faults and overlapping spreading...