1.
Structural characteristics and hydrocarbon accumulation of Kuche fold-thrust belts, Talimu Basin
塔里木盆地库车褶皱冲断带的构造特征与油气聚集
2.
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。
3.
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
4.
accumulation zone of thrust fold
逆掩断裂褶皱聚集带
5.
Deformation Feature and Genesis Simulation of Fold-and-Thrust Belts in the Southern Margin,Junggar Basin
准噶尔盆地南缘褶皱-冲断带变形特征及成因机制模拟
6.
Influence of viscosity of ductile substrate on deformational features of fold-thrust belts: insights from physical modeling
韧性基底层黏度对褶皱-冲断带变形特征的影响——来自物理模拟的启示
7.
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。
8.
folding and thrusting
褶皱和逆掩断层作用
9.
IDENTIFICATION OF CENOZOIC FOLD-THRUST STRUCTURE AND ITS DYNAMIC SETTING IN JIYANG SAG
济阳坳陷新生代褶皱—冲断构造的厘定及其动力学背景分析
10.
Fold-and-thrust structure in Yeyagou area, western Junggar,China and its implication
西准噶尔野鸭沟地区褶皱冲断构造的特征及意义
11.
Research on Rock Burst Rules and Prevention Near Fold;
褶皱附近冲击矿压规律及其控制研究
12.
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。
13.
Folding or faulting that affects a relatively large area.
褶皱或出现断层影响了相当大地区.
14.
orthotectonic Caledonides
标准构造型加里东褶皱带
15.
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。
16.
Sedimentation ceases: tilling or folding is accompanied or followed by uplift.
沉积间断，即掀斜或褶皱伴生或伴随着抬升运动。
17.
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
18.
To gather into small wrinkles or folds.
使收缩成皱褶或褶缝