WebWhere both converging plates are oceanic, the margin of the older oceanic crust will be subducted because older oceanic crust is colder and therefore more dense. As the dense slab collapses into the asthenosphere, however, it also may “roll back” oceanward and cause extension in the overlying plate.This results in a process known as back-arc spreading, in … Webmodel suggests that rollback and necking occur sequentially in three phases: at first there is a modest rollback caused by the initial drag of the accumulating continent, and then …
Numerical models of Farallon plate subduction: Creating and …
Webslab, causing its forward or rearward migration with respect to the arc. Based on a compilation of upper plate absolute motion, trench absolute motion, back-arc deformation … WebSep 6, 2024 · This happened in the Pacific Northwest of the U.S. and Canada, for example, in the Cascade Volcanic Arc, which includes Mount Rainier in Washington state, according … hunter collective hair
Episodic slab rollback fosters exhumation of HP—UHP rocks
WebHere we show that in the south Tyrrhenian subduction zone, slab rollback pulls asthenospheric material much farther along the plate contact, reaching the base of the … WebDec 1, 2024 · Volumes 376–377, 1 December 2024, 105790 Research Article Slab roll-back triggered back-arc extension south of the Paleo-Asian Ocean: Insights from Devonian MORB-like diabase dykes from the Chinese Altai Wang, Yuping, Jianping Zheng, E.A. Belousova, Ming Chen, Hongkun Dai, Zhou Add to Mendeley WebNov 1, 2011 · A fast returning wedge flow of up to 20 cm/yr exists in a broad region above the slab, accommodating the differential motions between the back-lying slab and the overriding plate. Besides the different dip angles, the transition in the style of subduction at ~ 20 Ma also causes a change in slab morphology ( Fig. 3 ). hunter collection