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The new coats blouse gracefully above the hip line.
新外套在臀围线上优美地打着褶皱。
The dress designer was adept at draping and cutting the fabric without using a pattern.
这个服装设计师善于不用图样就裁剪布料及打褶皱。
The folds of her evening gown hang gracefully.
她的晚礼服的褶皱优美地飘垂着。
Baiyinchagan depression is part of downwarping faulted rift basin developed on XingmengHercynian multicycle and collision fold basement in late Mesozoic.
白音查干凹陷为兴蒙海西期多旋回、软碰撞褶皱基底上晚中生代发育起来的断-坳型裂谷盆地的次级构造单元。
Close up, the workmanship that went into each ripple and shadowy layer of tulle was inimitably precious, yet somehow the designers successfully dodged the hazard of veering into overdone froufrou.
走进看看这些华服吧，每一个褶皱、每一片薄纱上的装饰物都以一无二的手工缝制而成，而你更无法想象设计师又是如何巧妙地避免了这些装饰物相互摩擦而发出过度的声响。
Whether it is white, red, light sierozem or brown, pulled tightly, and there is no trace of infant fold, some extend to the big leg, but the ride will be full of the fullness of the curve appears.
不论是白的，红的，淡灰的，还是土褐色，拉得紧紧的，没有一丝儿褶皱，有些延伸到大腿部，更将那脚儿的丰满的曲线显得丰满了。
These are compression folds, like wrinkles on a fruit rind that's dried out.
这些是挤压后产生的褶皱，就像是干瘪果皮上的皱纹。
Tears leaked out of the crinkled corners of Hagrid's beetle-black eyes.
泪水从海格乌黑的眼睛褶皱里流了下来。
We have absolutely no evidence of that neck frill that came out of Dilophosaurus.
那种从脖子弹出来的褶皱，我们压根没找到过任何证据。
That's the nictitating membrane and this little fold is the remnant.
那是瞬膜，这个小褶皱是残余的。
Wrinkles are those folds or lines on your clothes.
皱纹就是衣服上的褶皱或线条。
TWO. Reduce Wrinkles Without an Iron. Travel.
不用熨斗减少衣物褶皱。旅行类。
Until he saw those twitches around her eyes.
他也看见了她双眼之间的褶皱。
Use the hard shape of the case to offer protection from creasing.
选择保护力更强的硬壳箱子来避免折痕和褶皱。
There are several other vestigial structures like the plica semilunaris in the human body.
人体中还有其它的退化结构，例如半月形褶皱。
In particular, farmers use a complex of 15 species known collectively as Brachionus plicatilis.
农民们特别使用的是一种由15个物种组成的复合体，统称为褶皱臂尾虫。
褶皱是层状岩石受力后形成的波状弯曲。绝大多数的层状岩石是由堆积在盆地、海岸的平坦水平成层的沉积物形成，如隆升出露地面，形成水平岩层。
褶皱有两种基本类型：
Folds are classified by their size, fold shape, tightness, and dip of the axial plane.
Finally, folds can have, but don't necessarily have a fold axis. A fold axis, “is the closest approximation to a straight line that when moved parallel to itself, generates the form of the fold.” (Davis and Reynolds, 1996 after Donath and Parker, 1964; Ramsay 1967). A fold that can be generated by a fold axis is called a cylindrical fold. This term has been broadened to include near-cylindrical folds. Often, the fold axis is the same as the hinge line.
Folds that maintain uniform layer thickness are classed as concentric folds. Those that do not are called similar folds. Similar folds tend to display thinning of the limbs and thickening of the hinge zone. Concentric folds are caused by warping from active buckling of the layers, whereas similar folds usually form by some form of shear flow where the layers are not mechanically active. Ramsay has proposed a classification scheme for folds that often is used to describe folds in profile based upon curvature of the inner and outer lines of a fold, and the behavior of dip isogons. that is, lines connecting points of equal dip:
Folds appear on all scales, in all rock types, at all levels in the crust and arise from a variety of causes.
Many folds are directly related to faults, associate with their propagation, displacement and the accommodation of strains between neighbouring faults.
Fault bend folds are caused by displacement along a non-planar fault. In non-vertical faults, the hanging-wall deforms to accommodate the mismatch across the fault as displacement progresses. Fault bend folds occur in both extensional and thrust faulting. In extension, listric faults form rollover anticlines in their hanging walls. In thrusting, ramp anticlines are formed whenever a thrust fault cuts up section from one detachment level to another. Displacement over this higher-angle ramp generates the folding.
Recently deposited sediments are normally mechanically weak and prone to remobilisation before they become lithified, leading to folding. To distinguish them from folds of tectonic origin, such structures are called synsedimentary (formed during sedimentation).
Dewatering:Rapid dewatering of sandy sediments, possibly triggered by seismic activity, can cause convolute bedding.
Folding of rocks must balance the deformation of layers with the conservation of volume in a rock mass. This occurs by several mechanisms.
Flexural slip allows folding by creating layer-parallel slip between the layers of the folded strata, which, altogether, result in deformation. A good analogy is bending a phone book, where volume preservation is accommodated by slip between the pages of the book.
The fold formed by the compression of competent rock beds is called "flexure fold".
Typically, folding is thought to occur by simple buckling of a planar surface and its confining volume. The volume change is accommodated by layer parallel shortening the volume, which grows in thickness. Folding under this mechanism is typically of the similar fold style, as thinned limbs are shortened horizontally and thickened hinges do so vertically.
The rheology of the layers being folded determines characteristic features of the folds that are measured in the field. Rocks that deform more easily form many short-wavelength, high-amplitude folds. Rocks that do not deform as easily form long-wavelength, low-amplitude folds.