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断层崖

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Diluvial fans and spring sinter platforms that may largely correspond with these fault scarps.

以及与各级断层崖大致对应的河流阶地、洪积扇和泉华台地。

Along the fault we may recognize at least eight fault scarps or steep fault slopes whose heights are 0.33-0.62 m, 4.3-5.2 m, 6.8-8.3 m, 10-11.8 m,~16 m, 20-28 m, 45-50 m and 65-80 m respectively, as well as river terraces, diluvial fans and spring sinter platforms that may largely correspond with these fault scarps.

沿断层至少可以识别出高度分别为0.33~0.62m、4.3~5.2m、6.8~8.3m、10~11.8m、约16m、20~28m、45~50m和65~80m的8套断层崖或断层陡坎,以及与各级断层崖大致对应的河流阶地、洪积扇和泉华台地。

The northern foot of a series of well-preserved fault scarp and triangular face.

北面的山麓还有一系列保存完好的断层崖及三角面。

A major vertical fault scarp formed during the earthquake was less than 1000 ft from the spillway .

地震时形成的一个主要的垂直断层崖,离溢洪道不到1000英尺。

Sahnto toward the eastern side of the formation of nearly 10 meters fault scarp, looking from the North China Plain, the situation is magnificent.

山土东侧的走向断层形成近10米的断层崖,从华北平原仰望,形势雄伟。

Along the Daqingshan Piedmont Fault exist typical tectonic landforms, which are fault scarp, 3 orders of piedmont terrace, 5 orders of river terrace and 3 orders of alluvial fan, all carefully dated and measured. All these landforms display the intense vertical movement of this fault.

沿大青山山前断裂发育典型的构造地貌,计有夷平面、3级山前台地、5级河流阶地和3期洪积扇,基岩断层崖和全新世断层陡坎分布广泛,标志着断裂强烈的垂直差异性升降运动和间歇性活动的特点。

As the evolution process of the drainage channels on the scarp slope is concerned,the construction of their mathematic models and the visualization methods are discussed.

断层崖上的沟谷演化过程,我们也对其数学模型的构造和可视化方法进行了探讨。

The advantages of the diffusion equation feature are gained to discuss the visual process of scarp slope, together with forcasting it's future shape.

我们初步利用扩散方程的这一特性来探讨断层崖坡面演化过程的可视化方法,同时预测其未来的形态。

Prominent fault scarps lace the newly viewed region.

显而易见的断层崖环绕着新观察到的区域。

Fault scarps developed in the alluvial fans range in height from 1 m to 25m and alternate along the strike of the fault zone from northeast-facing to southwest-facing in a left-stepping en-echelon pattern.

冲积扇中的断层陡坎高lm到25m,沿断层带走向左行雁列状断层崖呈现,向NE和SW倾。

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