构造地貌能反映断裂的结构变形特征和断层的活动强度。例如断层陡坎的高度、长度和坡度以及断层陡坎的连续程度。
Tectonic topography can reflect the structural deformation feature and active strength of faults, such as the height, length and gradient of a fault scarp as well as its continuity.
本文从地质构造、岩石结构、地貌、湖底形态及室内沉积物分析资料几个方面论证了喀纳斯湖的成因。
This article proves the genesis of Kanasi lake from the respects of geologic structure, landforms, formation of lake bottom and analysis material of sediments in laboratory.
本文应用地质构造、岩性特征、地貌成因及海面升降变化等资料，综合分析了“石老人”的形成及其岩体结构类型。
The formation and the texture of "Shilaoren" rock column have been analysed in geological structure, feature of rock, geomorphic origin and eustatic change in this paper.
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