下盘

In structural geology the relative movement of the banging wait and footwall is a major factor to classify various faults .

在构造地质学中，断层上盘和下盘的相对位移运动特征是划分各种类型断层的一个主要因素。

Then the block in the southern side of this fault is the hanging wall and the block in the northern side of this fault is the footwall.

那么，位于这条断层南侧的岩层是上盘，位于这条断层北侧的岩层则是下盘。

Then the block in the southern side of this fault is the hang ing wall and the block in the northern side of this fault is the footwall.

那么，位于这条断层南侧的岩层是上盘，位于这条断层北侧的岩层则是下盘。

Then the block in the southern side of this fault is the hang in g wall and the block in the northern side of this fault is the footwall.

那么，位于这条断层南侧的岩层是上盘，位于这条断层北侧的岩层则是下盘。

But to the region of nappe structure, by the reason of rising reverse fault top wall, so we just can calculate the fault geometry under the footwall breakpoint.

而对于逆断层因其上盘的上升过程，使得推算的断层只能获取下盘断点以下的构造形态。

So the fault on the cliff is a reverse fault because the red rock layer in the hang in g wall has moved up relative to that in the footwall.

这样看来，发育在悬崖上岩层中的那条断层就是一逆断层了，因为上盘的红色岩层相对于下盘的红色岩层发生了沿断层面向上位移的运动。

So the fault on the cliff is a reverse fault because the red rock layer in the hang ing wall has moved up relative to that in the footwall.

这样看来，发育在悬崖上岩层中的那条断层就是一逆断层了，因为上盘的红色岩层相对于下盘的红色岩层发生了沿断层面向上位移的运动。

The model is used to analyze the displacement and deformation of the roof while the entry of the hanging wall is being driven after the coal seam of the footwall has been exploited.

通过相似材料模拟试验，建立平面应力模型，分析研究断层下盘煤层开采后，在其上盘煤层中开掘巷道，巷道顶板的位移和巷道变形特征。

In the foreland basement-involved structures, although the considerable relief bewteen the hanging wall and footwall may exist, the cover strata probably keep continuous.

在有基底参与的冲断构造带中，尽管上盘与下盘有较大的构造高差，但盖层完全可能是连续的。

On the hanging wall of the nappe,isoclinal folds are developed with the axial planes inclined to the north in association with imbricated thrusts dipping to the south. In the foot wall,there exist rather wide ductile shear zones. Also,a set of structural windows and klippen are distributed along the zone . The distance of the dislpacement is estimated at about more than 20km.

推覆构造上盘变质岩中同斜倒转褶皱发育，轴面向北倾倒，伴有一组向南倾斜的叠瓦式冲断面；下盘见有较宽的韧性剪切带；还发现有一系列飞来峰与构造窗沿推覆构造带分布，推测推覆距离在20km以上。

On the other hand, the more important thing is because the urban housing is a kind of heterogeneity products.

另一方面，更重要的是由于城市住房是一种异质性产品。

Climate histogram is the fall that collects place measure calm value, cent serves as cross axle for a few equal interval, the area that the frequency that the value appears according to place is accumulated and becomes will be determined inside each interval, discharge the graph that rise with post, also be called histogram.

气候直方图是将所收集的降水量测定值，分为几个相等的区间作为横轴，并将各区间内所测定值依所出现的次数累积而成的面积，用柱子排起来的图形，也叫做柱状图。