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Find link is a tool written by Edward Betts .
searching for Ridge push 11 found (33 total)
alternate case: ridge push
Inversion (geology)
(619 words)
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breakup unconformities caused by the transition from rift-phase tension to ridge push compression. Local inversion in strike-slip rhombohedral pull-aparts as
Gorda Ridge
(922 words)
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each section has its own spreading rate, caused by the slab-pull and ridge -push of the surrounding tectonic plates. The northern segment is the narrowest
Earth's crust
(1,645 words)
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underlying mantle yields basaltic magmas and new ocean crust forms. This "ridge push " is one of the driving forces of plate tectonics, and it is constantly
Grenville orogeny
(2,738 words)
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oceanic plate was taking place. Slab pull and far-field drivers such as ridge push were aiding in closing the distance between the island arc and the continent
Sedimentary basin
(4,615 words)
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such as rifting (which is associated with divergent plate boundaries) or ridge -push or trench-pull (associated with convergent boundaries), the effect is
Carolina terrane
(1,466 words)
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Carolina-Avalonia-Gander terranes and Gondwana. The combination of slab rollback and ridge -push moved the Carolina-Avalonia-Gander terranes north across the Iapetus Ocean
Ultra-high-pressure metamorphism
(3,643 words)
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positive buoyancy of the continental slab—in opposition principally to ridge push —can then drive exhumation of the subducting crust at a rate and mode determined
Dharwar Craton
(3,536 words)
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the melting of the thickened oceanic arc crust. In 3350 Ma, due to the ridge push from the oceanic spreading centres (mid-oceanic ridges), some oceanic
Seismic anisotropy
(5,684 words)
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by mantle convection or from above by the plates, i.e. slab pull and ridge push . The favored methods for detecting seismic anisotropy are shear wave splitting
Tectonics on icy moons
(2,366 words)
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subducting plate provides the spreading force for mid-ocean ridges. “Ridge push ” is comparatively weak in Earth's plate tectonics. Extensional features
Magmatism along strike-slip faults
(4,846 words)
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driven by Harry Hess’s sea floor spreading model subduction slab-pull and ridge -push mechanism, however some areas of the ridge will spread at different rates