1.
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
2.
I find every limb is mutually shared by two adjacent folds.
我发现两个相邻褶皱共同拥有其中的一个翼。
3.
accumulation zone of thrust fold
逆掩断裂褶皱聚集带
4.
These folds are characteristic of a-type fold which are commonly found in ductile shear zones.
这些褶皱的特征表明它们属于a型褶皱，而a型褶皱通常发育在韧性剪切带中。
5.
orthotectonic Caledonides
标准构造型加里东褶皱带
6.
Some have circled rings around them that are beginning to pucker.
有时乳头周围还会出现带褶皱的圆环。
7.
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。
8.
Folding or faulting that affects a relatively large area.
褶皱或出现断层影响了相当大地区.
9.
Sederholm regarded the Svecofennide belt as an older structure truncated by a younger Varelide belt.
塞德霍尔姆认为斯维科芬褶皱带本身为一老的构造，被比较年轻的卡累利褶皱带所截断。
10.
To gather into small wrinkles or folds.
使收缩成皱褶或褶缝
11.
To make into a ruffle or frill.
使有褶弄出皱褶或饰边
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.
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
14.
Analysis of the Hechi-Yishan Fold-thrust Zone in North of Guizhong Depression
桂中坳陷北部河池—宜山褶皱—冲断带分析
15.
The Folding Time of the Eastern Sichuan Jura-type Fold Belt:Evidence from Unconformity
川东“侏罗山式”褶皱带形成时代:不整合面的证据
16.
flabby, wrinkled flesh;
松软、褶皱的肌肉；
17.
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。
18.
To arrange or let fall in loose folds
布置成褶皱状或使成褶皱状垂下.