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@@Foreland basins occllr as elongate troughs and consist of depositional regions on continental crust in front of major fold-thrust belts.A typical collisional foreland basin is bounded longitudinally by a pair of marginal sea basin.In general,during evolution of a foreland basin excess sediment is bypassed out of the mature basin and empties longitudinally into the marginal sea or remnant basins.The foreland basin west of Taiwan is presented here to characterize these distinct features.