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  3. 退积 - 维基百科，自由的百科全书
退积 - 维基百科，自由的百科全书
维基百科，自由的百科全书

退积（英語：retrogradation）是指河流三角洲前緣的位置隨時間向陸地方向移動。 當進入三角洲的沉積物的供應量小於沉積空間的增加、例如海平面上升或盆地下降，就會造成退积[1]

參考文獻

  1. ^ Gary Nichols, Sedimentology & Stratigraphy, Wiley-Blackwell, Malden, MA (1999), ISBN 0-632-03578-1
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