1.
The Mechanism of Gas Accumulation in the Overpressured Kuqa Fold-Thrust Belt;
库车坳陷山前断褶带超压体系油气成藏机理
2.
GEOLOGICAL DEVELOPMENT OF THE CHENXIAN-HUAIJI STRUCTURAL BELT WITH SPECIAL REFERENCE TO THE TRENDING OF THE CATHAYSIAN SYSTEM
郴怀断褶带的地质发展史兼论华夏系方向构造问题
3.
5)Cale-donian fault-fold belt (Hercynian deformation) in the southeast of it ;
5）塔东南中、新元古基底的加里东断褶带（海西改建）；
4.
folding and thrusting
褶皱和逆掩断层作用
5.
accumulation zone of thrust fold
逆掩断裂褶皱聚集带
6.
Folding or faulting that affects a relatively large area.
褶皱或出现断层影响了相当大地区.
7.
From Fold to Fault-the Concept Change on Structural Forms
从褶曲到断层——构造形态认识的转变
8.
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。
9.
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。
10.
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
11.
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
12.
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。
13.
The core of the anticlinal fold, which is squeezed between faults, underwent intense crushing.
背斜褶皱的核部在断层间受到挤压，遭受到很强的破坏。
14.
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
15.
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
16.
Yanshanian Tectonic Evolution of the Chengde Basin and the Adjacent Area in the Eastern Segment of the Yanshan Fold-and-thrust Belt;
燕山褶断带东段承德盆地及邻区燕山期构造演化
17.
A Paleomagnetic Study of Early Cretaceous Strata from the Eastern Yanshan Fold-and-thrust Belt and Its Geological Implications;
燕山褶断带东段早白垩世古地磁研究及其构造意义
18.
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