松辽盆地的现今东部边界是构造侵蚀边界。
Today the boundary of Songliao basin is structure erodent borderline.
根据野外调查和实际测量资料，研究了黄土高原构造侵蚀期和期内造成的侵蚀。
According to the material of field investigation and survey, tectonic erosion periods and their erosion are studied.
地质构造作用力向上抬升地壳，侵蚀再将地壳撕得支离破碎，山脉从此形成，同时也产生了分形图案。
Mountains are the result of tectonic forces pushing the crust upward and erosion tearing some of that crust down. The resulting pattern is a fractal.
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