1.
orthotectonic Caledonides
标准构造型加里东褶皱带
2.
A COMPARISON BETWEEN THE AUTOCHTHONOUS AND PARAUTOCHTHONOUS TRANSFORMATION TYPE GRANITOIDS IN EAST QINLING AND SOUTH CHINA CALEDONIAN FOLDBELTS
东秦岭与华南加里东褶皱带原地-准原地改造型花岗岩特征
3.
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
4.
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
5.
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。
6.
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。
7.
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
8.
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。
9.
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
10.
LOWER PALEOZOIC OMISSION ZONE IN JIANGNAN UPLIFT──A SIGN OF CALEDONIAN FORELAND FOLD THRUST BELT
江南隆起上的下古生界缺失带──华南加里东前陆褶冲带的标志
11.
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。
12.
Antarctica can be divided into 2 big structural units, ie East antarctica shield and West Antarctica Mesozoic Cenozoic fold belt.
南极洲主要可分为东南极地盾及西南极中新生代褶皱带两大构造单元。
13.
Granites at the middle Variscian period are the largest scale magma activities on the Caledonia foldbelt inthe west Tianshan mountain.
海西中期花岗岩是西天山加里东褶皱带内规模最大的一次岩浆活动。
14.
Characteristics of Caledonian folds in the northern segment of the Yangtze platform:Evidence from unconformity
扬子东南缘北段加里东期的褶皱特征——来自不整合关系的证据
15.
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。
16.
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
17.
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
18.
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。