Add to ORKGrift zones. pared to mid-ocean ridge basalts (MORB) [1–7]. Hot involves low-volume, scattered, sporadic eruptions [12]. With rift locations determined by pre-existing zones of weakness in the lithosphere [13,14], it is improbable that Earth and Planetary Science Letters⁎Keywords: continental rift; mantle flow; anisotropy; hotspot; plume; plum-pudding 1
High-resolution uppermantle tomographic models are interpreted in terms of plate tectonics, hotspots...
Hot plumes were considered by Morgan (1971, 1972) to be basic components of a whole-mantle thermal c...
Large igneous provinces (LIPs) such as continental flood basalt (CFB) and oceanic plateau basalt (O...
When continents rift to form new ocean basins, the rifting'is sometimes accompanied by mas-sive...
Models of melting accompanying mantle upwelling predict far more melt than is observed at nonvolcani...
Oceanic volcanism can be understood in terms of decompression melting (ridges), addition of water to...
Hotspots and hotspot tracks are on, or start on, preexisting lithospheric features such as fracture ...
The Easter Microplate is bounded in the east and west by two large overlapping spreading centres cal...
Hotspots and hotspot tracks are on, or start on, preexisting lithospheric features such as fracture ...
Geophysical evidence and numerical models of mantle stirring imply the source of mid-ocean ridge bas...
International audienceThe role of the uppermost mantle strength in the pattern of lithosphere riftin...
International audienceAnalysis of major rift systems suggests that the preexisting structure of the ...
Continental flood basalt (CFB) provinces have been attributed to a variety of sources. Among these a...
copyrighted by American Geophysical UnionPersistent, long-lived, stationary sites of\ud excessive ma...
Continental flood basalt Large igneous provinces Throughout its history, the Earth has experienced g...
High-resolution uppermantle tomographic models are interpreted in terms of plate tectonics, hotspots...
Hot plumes were considered by Morgan (1971, 1972) to be basic components of a whole-mantle thermal c...
Large igneous provinces (LIPs) such as continental flood basalt (CFB) and oceanic plateau basalt (O...
When continents rift to form new ocean basins, the rifting'is sometimes accompanied by mas-sive...
Models of melting accompanying mantle upwelling predict far more melt than is observed at nonvolcani...
Oceanic volcanism can be understood in terms of decompression melting (ridges), addition of water to...
Hotspots and hotspot tracks are on, or start on, preexisting lithospheric features such as fracture ...
The Easter Microplate is bounded in the east and west by two large overlapping spreading centres cal...
Hotspots and hotspot tracks are on, or start on, preexisting lithospheric features such as fracture ...
Geophysical evidence and numerical models of mantle stirring imply the source of mid-ocean ridge bas...
International audienceThe role of the uppermost mantle strength in the pattern of lithosphere riftin...
International audienceAnalysis of major rift systems suggests that the preexisting structure of the ...
Continental flood basalt (CFB) provinces have been attributed to a variety of sources. Among these a...
copyrighted by American Geophysical UnionPersistent, long-lived, stationary sites of\ud excessive ma...
Continental flood basalt Large igneous provinces Throughout its history, the Earth has experienced g...
High-resolution uppermantle tomographic models are interpreted in terms of plate tectonics, hotspots...
Hot plumes were considered by Morgan (1971, 1972) to be basic components of a whole-mantle thermal c...
Large igneous provinces (LIPs) such as continental flood basalt (CFB) and oceanic plateau basalt (O...