1.
We call it overturned fold because the bedding sequence of one limb is overturned due to folding.
这种类型的褶皱构造叫做倒转褶皱，因为褶皱其中一翼的岩层层序已随褶皱作用发生倒转。
2.
If both limbs of overturned fold have same dip angle, we call this special overturned fold isoclinal fold.
如果倒转褶皱构造的两翼倾角相等，则可称这种特殊类型的倒转褶皱为等斜褶皱。
3.
The compact fold structure area, anticline and. syncline in North Guizhou are often in opposite arrangement.
贵州北部紧密褶皱构造区,背斜、斜常呈相间排列。
4.
Structural Style and Thrust Breakthrough Model of Fold in Southeast Guizhou
黔东南地区褶皱构造样式及其断层突破模式
5.
The rock foundation bent under the horizontal compressive stress. It is called fold. The regional or local stress direction can be analyzed according to the fold structure.
岩层受到水平挤压应力，发生弯曲称作褶皱。通常依据褶皱构造可分析区域或局部应力方向。
6.
Now let's walk along the highway and look for other different types of folds.
现在我们沿着公路前行，沿途寻找其它不同类型的褶皱构造。
7.
Sichuan Xuanhan Baili Canyons Areas Fold Structure Characteristic and Geological Landscape Research;
四川宣汉百里峡地区褶皱构造特征及地质景观研究
8.
Fold Structure's Control Funtion on the Karst Stephen Development--taking the Weining region in Guizhou as an example
褶皱构造对岩溶泉发育的控制作用——以贵州威宁地区为例
9.
Today we are going to walk along this highway and observe some geological structures, folds in particular.
今天我们将沿着这条公路观察一些地质构造现象，尤其是观察褶皱构造。
10.
Folds are undulations or waves in the rocks of the earth. They are best displayed by layered rocks, such as sedimentary and volcanic rocks.
褶皱构造就是地球中岩石的波状起伏。它们在沉积岩和火山岩这些层状岩石中发育最好，
11.
orthotectonic Caledonides
标准构造型加里东褶皱带
12.
Salt tectonic evolution and hydrocarbon accumulation of Kuqa foreland fold belt, Tarim Basin, NW China.
库车前陆褶皱-冲断带前缘大型盐推覆构造。
13.
This sediment will then probably be formed into a folded and imbricated structure.
然后这些沉积物可能形成褶皱和叠瓦构造。
14.
THE REGIONAL TECTONIC EVOLUTION OF TARIM BASIN AND ADJACENT FOLD BELTS
塔里木盆地与相邻褶皱带的区域构造演化
15.
Research of Garment-Tuck Technique Base on 3D-Mesh;
基于三维网格构造的服装褶皱生成技术研究
16.
Yanshanian Superposed Structural Characteristics of West Margin of Foreland Fold Belt of South Dabashan
燕山期南大巴山前陆褶皱带西缘叠加构造特征
17.
Strong foliation, stretching lineation, a-type folds, sheath folds and mylonite, these structural characteristics only reflect macroscopic evidence.
强烈的片理、拉伸线理、a型褶皱、鞘褶皱以及糜棱岩，这些构造特征仅仅反映出宏观的证据。
18.
In profile, the syncline is asymmetrical and called inclined fold.
在横剖面上，这个向斜构造看起来是不对称的，这种褶皱称为倾斜褶皱。