地震地貌学强调在相对地质年代域中对沉积体成像，表征了地震相的平面反射形态。
Seismic geomorphology emphasizes the imaging of sedimentary bodies in relative geologic age domain, and characterizes the plane reflection pattern of seismic facies.
地震地貌学是一种新的地震相分析与表征方法，研究的是沉积特征在沉积等时面上的地震映像。
Seismic geomorphology is a new method for seismic facies analysis and characterization, which aims at studying the seismic imaging of sedimentary characteristics on the isochronal sedimentary surface.
通过实地考察和分析，结合历史地震记载资料，对熊耳山地貌、裂谷以及崩塌遗迹的形成原因进行了初步探讨。
Through field investigation and analysis, combining with historical earthquake documents, the causes of landform, rift valley and landslip relic of Xionger mountain is studied.
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