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138 回視聴2高評価1:18sciencepathshala123元のリリース: 2026-05-19

Accretionary prisms (wedges) form at ocean-continent convergence boundaries where the denser oceanic plate subducts beneath the continental plate; during subduction, sediments from the oceanic plate are scraped off and accumulate near the trench, creating a wedge-shaped structure characteristic of subduction zones.

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