- 更多网络例句与小起伏地形相关的网络例句 [注：此内容来源于网络，仅供参考]
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As Tibetan Plateau is affected by tectonic activity and climate, many geomorphologic units emerge, such as rugged summits which are formed by obduction, extensive basins with high altitude and low relief, as well as basin-range system made up of linear range and intermountain basin.
青藏高原受不同体制的构造作用控制及气候影响，既发育由逆冲推覆作用形成的高峻山峰，也发育地形起伏小、海拔高度大的宽阔的盆地高原，还发育特征的由线状山脉与山间盆地组成的盆山系统。
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However, the sparsity of the observational points used in the refraction method due to the restrictions imposed by the surface hypsography of the area-- one point per kilometre-- makes it possible only to give relatively accurate data for base rock velocities, but not for morphologic structure configurations.
但是，小折射方法受地表的地形起伏因素影响比较大，且观测密度也不够，每公里只有一个点，所以在该区只能较准确地给出基岩的速度信息，而无法准确地获得基岩的形态起伏数据。
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However, owing to the much restricted hypsography of the surface for the refraction method and the insufficient surveying points --only one observational point a kilometre, we can only provide relatively true velocities of the base rock, but cannot obtain the accurate data of the morphologic-structural configuration.
但是，小折射方法受地表的地形起伏因素影响比较大，且观测密度也不够，每公里只有一个点，所以在该区只能较准确地给出基岩的速度信息，而无法准确地获得基岩的形态起伏数据。
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In the case of the side-glance angle of beam is zero or small,an algorithm has been developed to determine the latitude and longitude of an arbitrary pixel in an air-borne strip mode SAR image without consideration of the hypsography.
在不考虑地形起伏的情况下，从机载合成孔径雷达数据采集几何关系和成像原理的角度，针对正侧视和小斜视情况提出了计算机载SAR图像像素点经纬度的一种准确而实用的方法，给出了从雷达图像上的像素点计算其经纬度的详细过程，并结合某实际机载SAR成像参数对影响定位精度的因素包括高度测量误差，航向角、俯仰角、横滚角误差和多普勒中心、多普勒调频率误差进行了详细的分析。
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If the tectonic uplift is not considered, the relief of Dabie orogen will reach at least 3km in Late-Cretaceous. As to the value of the relief reduction factor in Dabie orogen at 90Ma, the largest value appeared in northeast region, followed consecutively by the core and southeast Tanlu fault zone, with the smalleast value appeared in northwest and southwest region. The results reflect the strong uplift difference between core and North Huaiyang flank in Dabie orogen during doming extension period. Relief in the core region and southeast Tanlu fault zone is higher than those in the peripheral regions, northwest and southwest flanks are more stable than other regions.
如果不考虑构造抬升，大别造山带在晚白垩世地形起伏至少可达3km.90Ma时大别造山带地形起伏变化率在空间上呈现如下特征：东北区块最大，热窿核部其次，东南郯庐断裂区块再次，西北、西南区块最小，反映大别造山带热窿伸展期，核部与北淮阳翼之间强烈差异隆升，核部地形和东南郯庐断裂区块起伏高于周边地区，西北、西南两个翼部比其他地区稳定。
- 更多网络解释与小起伏地形相关的网络解释 [注：此内容来源于网络，仅供参考]
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underexposure：曝光不足;照射不足
underexcitation 欠励磁 | underexposure 曝光不足;照射不足 | underfeature 小起伏地形
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underfeed：下部进料
underfeature 小起伏地形 | underfeed 下部进料 | underfilm corrosion 膜下腐蚀
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underfeature：小起伏地形
underexposure 曝光不足;照射不足 | underfeature 小起伏地形 | underfeed 下部进料