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• W127965863 startingPage "431" @default.
• W127965863 abstract "We offer a kinematic solution to the “ophiolite enigma, paradox or conundrum”, which is that obducted large-slab full-sequence ophiolite complexes must have originated by organized sea-floor spreading (e.g. sheeted dyke complexes), which indicates an origin at oceanic ridges, yet have geochemical affinities that link them to arcs, especially fore-arcs. Our model is that, following the nucleation of a subduction zone on an oceanic transform/fracture zone, a stable ridge/trench/trench triple junction with a ridge separating hanging-wall plates allows the arc-parallel growth and lengthening of an ophiolite fore-arc, synchronously with the development of a rear-arc oceanic basin at the same ridge. Fore-arc boninites result from sub-ridge asthenosphere hydration by water released from the basaltic crust of the subducting plate. The thermal thickening of the fore-arc ophiolite is buffered by its position above the subducting lithosphere. If obduction onto a continental margin is to occur, it must happen within 10–15 million years. If the fore-arc ages beyond about 20 million years, the fore-arc lithosphere becomes too thick to obduct and bulldozes the continental margin with which it collides or the thin hot arc lithosphere overrides the forearc, which is subducted, onto the continental margin. The immensely-variable style of arc–continent collision is dependent on the age of the arc/fore-arc and the rifted margin when collision occurs. The mafic-protolith basal aureole is formed from oceanic crust in the subduction channel and attached to the base of the ophiolite about 5 million years after the birth of the ophiolite. It is obducted with the ophiolite and is not formed during obduction. The slip-direction in the subduction channel must be oblique towards the RTT triple junction because the oblique motion cannot be partitioned into trench-orthogonal and trench-parallel components." @default.
• W127965863 created "2016-06-24" @default.
• W127965863 creator A5006910350 @default.
• W127965863 creator A5014831343 @default.
• W127965863 date "2011-01-01" @default.
• W127965863 modified "2023-10-08" @default.
• W127965863 title "The Origin of Obducted Large-Slab Ophiolite Complexes" @default.
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• W127965863 doi "https://doi.org/10.1007/978-3-540-88558-0_15" @default.
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