背斜的

Sloping downward in opposite directions, as in an anticline .

背斜的沿不同方向向下倾斜的，如在背斜地势中

Aran anticline northwest dumping fractured reservoir development is the most favorable position.

Aran背斜的西北倾伏端是裂缝性储层发育最有利的部位。

Occurs to the eastern Houshiding overturned anticline of Fuping complex domal uplift, Pingyang gneissic granite, a trondhjemite looks like a domal anticline in the west part and becomes two sub-anticlines overturned to south in the east part.

岩体的西部似一穹状背斜，向东逐渐转变为两个向南倒转的次级背斜，总体上为向南倒转的复式背斜的核部，其产状及其面理构造与区域构造线完全一致。

For example, the limbs of anticline you have just measured dip toward opposite direction and the dip angles are basically identical. In profile, the anticline has a vertical axial plane. This type of fold is called upright fold.

例如，你们刚才测量的那一个背斜，它的两翼向相反方向倾斜，倾角基本相等，在横剖面上，这个背斜的轴面是垂直的，这种轴面直立的褶皱叫做直立褶皱。

For example, the limb s of anticline you have just measured dip toward opposite direction and the dip angles are basically identical. In profile, the anticline has a vertical axial plane. This type of fold is called upright fold.

例如，你们刚才测量的那一个背斜，它的两翼向相反方向倾斜，倾角基本相等，在横剖面上，这个背斜的轴面是垂直的，这种轴面直立的褶皱叫做直立褶皱。

The forming mechanism of the anticlines is analyzed in terms of tectonics and sedimentology.

从构造和沉积两方面研究了沾车地区滚动背斜的形成机制。

Tectonization effects on Aran anticline exhibited as the follows: Aran anticline begin form rudiment in Ml member of URF; stronger compressive aggrandized extent of uplift in M2 member of URF; the strongest Tectonization aggrandized ultimately extent, especially in curvature of Aran anticline in later Quaternary sediment, Aran anticline finalized the design.

晚阿尔卑斯构造运动对Aran背斜地区的具体影响为：上红组M_1段沉积末，Aran背斜已经形成雏形；M_2段开始沉积到结束，构造挤压活动强度有所加大，Aran背斜隆起幅度相对有所增大；第四系以后发生了一次强烈的构造运动使Aran背斜的褶皱幅度、特别是曲度明显的加大，至此Aran背斜基本定型。

At early stage bedding fault activated, then transected strata to control formation of anticlines miniature, from late Permian to Jurassic growth faults controlled growth anticline, finally joined end to end, and merged to a common slip surface.

断裂早期以顺层滑脱为主，晚期切穿地层控制了纵弯背斜和断展背斜的雏形，二叠纪晚期-侏罗纪时期生长断裂控制了生长背斜的发育，且各断裂在深部归结为统一滑脱面，首尾相接使得背斜发育具明显的顺序性。

The major morphology of the anticline is multiple box-shaped or asymmetry inclined, mostly, and it is similar to that of fault-bend fold and fault-propagation fold.

背斜形态多为复式箱状背斜和不对称的斜歪背斜，分别与断层弯曲背斜和断层扩展背斜的几何形态一致。

Parameters of anticline, which are from seismic and geological sections of the Cizhuya propagation anticline, respectively, give the consistent depth and dip angle of detachment fault at 8.10-8.63 km and 29°-45°.

根据地震剖面的解释及地表资料整理结果，把上述演算结果应用于重庆方斗山地区的茨竹亚背斜的2个剖面中，计算出隐伏滑脱层的深度分别为8.10~8.63 km，证明茨竹亚背斜隐伏主滑脱层发育于寒武系底部。

The split between the two groups can hardly be papered over.

这两个团体间的分歧难以掩饰。

This approach not only encourages a greater number of responses, but minimizes the likelihood of stale groupthink.

这种做法不仅鼓励了更多的反应，而且减少跟风的可能性。