此外，还对测区内地质构造、地形地貌条件以及地层岩性进行了简要的介绍。
In addition, the characteristics of tectonics and topography of study area as well as the relevant rock mass properties are presented.
施甸境内复杂多变的地貌地形和立体气候，为各种丰富的自然资源提供了得天独厚的条件。
The complicated topographic features and varied weather bless the Shidian region with advantageous conditions of rich natural resources.
结果表明，该滑坡受地形地貌和物质结构条件控制，受人为工程切坡和降雨诱发而形成的。
It shows that the landslide is controlled by landform and material-texture conditions, and induced by engineering excavation and precipitation.
认为表生富集型氧化锰矿床的形成主要受原生含锰层、地质构造、地形地貌、顶盖层厚度、岩性、气候及水文地质等条件所制约。
Formation of the oxidized Mn deposit is controled by the primary Mn ore layer, tectonics, geomorphology, thickness and lithology of the cover rock, climate and hydrogeological condition.
复杂的地形地貌和地质条件下特高拱坝的强度与稳定分析是目前拱坝设计和分析中的重要研究课题。
The strength and stability analysis of Super-high arch DAMS built in conditions of complex topography and geology is an important subject in arch dam design and research.
通过分析发现，影响该区崩滑形成的因素有区域地质构造、地层岩性、地形地貌及气象水文条件。
The influence factors of collapse-slide are regional tectonic, stratum lithologic, geomorphic, meteorological and hydrographic characteristics of Changbai Mountain.
针对石膏山水库坝型的选择，分析了地形地貌和坝型地质条件，选择了混凝土重力拱坝方案。
In the light of the selection of dam type of Shigaoshan Reservoir, this paper analyzes the topography, geomorphology and the dam type geology, and selects the plan of concrete gravity-arch dam.
河流砂金矿的形成受物源、地形地貌、第四系、水动力等条件的控制。
The formation of fluvial Au placer deposits is controlled by the factors of material sources, morphology, topography, Quaternary stratigraphy and hydrodynamics.
东沙是江苏岸外辐射沙脊群中的第二大沙洲，具有独特的地形地貌和水动力条件，对它进行稳定性研究为揭示整个辐射沙洲及其邻近岸滩的动态演变都非常有益。
So the stability study of the Dongsha sandbank is very helpful to the analysis of the stability of the whole radial submarine sand ridges system and the neighboring tidal flat.
东沙是江苏岸外辐射沙脊群中的第二大沙洲，具有独特的地形地貌和水动力条件，对它进行稳定性研究为揭示整个辐射沙洲及其邻近岸滩的动态演变都非常有益。
So the stability study of the Dongsha sandbank is very helpful to the analysis of the stability of the whole radial submarine sand ridges system and the neighboring tidal flat.
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