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Pacific-type orogenic belts: linking evolution of oceans, active margins and intra-plate magmatism
2018
Episodes
Pacific-type orogens (fold belts) hosting accretionary complexes are places keeping records of the evolution of paleo-oceans, and formation and transformation of continental crust at their active convergent margins. Pacific-type orogeny induces destruction of crustal materials, their subduction to the deep mantle, generation of hydrouscarbonated plumes in the mantle transition zone (MTZ) and its related intra-plate magmatism. We propose a new approach for linking paleo-oceans, active margins
doi:10.18814/epiiugs/2018/018008
fatcat:sypdfebocfd4zfwjivucmseb44