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Thickness distribution of eolian deposits since 13 ka on parallel-contour slope; relationship between the erosion rate by soil creep and the slope curvature on actual slope



Thickness distribution of eolian deposits since 13 ka on parallel-contour slope; relationship between the erosion rate by soil creep and the slope curvature on actual slope



Chikei = Transactions - Japanese Geomorphological Union 20(2): 117-118




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