长尺度地表剥蚀速率在根本上受控于构造作用，并且能够反映构造影响下的地貌发育过程。
Long-term surface denudation rates are in first order controlled by tectonic uplift and could reflect the geomorphical evolution under the influence of tectonics.
物质的侵蚀- 搬运- 堆积是地貌发育的主要过程。
The erosion-transport-deposit of weathering sediment is one of the important process of geomorphology development.
物质的侵蚀- 搬运- 堆积是地貌发育的主要过程。
The erosion-transport-deposit of weathering sediment is one of the important process of geomorphology development.
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