| 1. | 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。 |
| 2. | Songpan - ganzi folded belt in sichuan province of china is a major issue to geoscientists
摘要四川松潘甘孜褶皱带一直是地球科学家关注的一个焦点。 |
| 3. | Growth strata and their application in timing deformation of foreland thrust - fold belts in the north margin of tianshan
生长地层及其在判断天山北缘前陆冲断褶皱带形成时间上的应用 |
| 4. | The most typical persian gulf basin is characterized by the superposition with these zones one after another
形成了内克拉通、前陆及褶皱带、活动大陆边缘、离散大陆边缘和内裂谷等5种盆地类型。 |
| 5. | Seen from the structure , this district belongs to the structure region of tethys - himalayas , " sanjiang " fold system , and the fracture - fold zone of lancangjiang river
从构造上看，本区属于特提斯喜-马拉雅构造域，三江褶皱系，澜沧江断裂褶皱带。 |
| 6. | Qinling fold belt is located at the junction of the north china plate and the yangtze plate , and its portion in henan province is a part of the east qinling mountains ( eqm )
摘要秦岭褶皱带位于华北板块和扬子板块结合部位，其在河南省内的部分多划为东秦岭。 |
| 7. | The cbm industrial production region lies in transition zone which is one part of a single continent in u . s . a . , but a compound continent that is made up of some small platform , landmass and fold belt in china
我国是一些小型地台、地块及其间的褶皱带镶嵌起来的复合大陆，煤层气勘探有利区位于地台内部。 |
| 8. | The changning - menglian belt , located the drape belt of three river in structure territory of tethyan - himalayan , is the one of most pivotal areas which is redounded to research and resolve the problem
昌宁?孟连构造带位于特提斯?喜马拉雅构造域三江褶皱带，是研究和解决该问题的最为关键的地区之一(刘本培等， 1993 ；崔春龙， 1999 ) 。 |
| 9. | The western hubei - eastern sichuan area is located at the junction belt between the eastern sichuan folded belt in the sichuan basin and xianexi folded belt , belong to eastern extended part , which is similar to the eastern - sichuan structure in many aspects . for example , they share a structural unit , resulting in the same sedimentary history and the same generation - reservoir - seal assembly as each other
鄂西渝东区处于四川盆地川东褶皱构造带与湘鄂西褶皱带的接合部位，属川东褶皱带东延组成部分，具有与川东相似的沉积发育史与生储盖组合；相同的构造发育史与构造形式；类似的天然气藏类型与保存条件。 |
| 10. | Through the regional background analysis in which western structures developed , it suggested that there did not exist a united and steady block to the west of ordos basin . alashan block neighboring on the north of the western margin was largely influenced by the action of qilian and tianshan - xingmeng folded belt which is respectively to the south and north of alashan block , was narrow in the steady block and was limited by the longshou mountain - zhongwei strike fracture in the south area
通过对鄂尔多斯盆地西缘构造发育的区域构造背景分析，认为在鄂尔多斯盆地之西，一直没有一个统一的稳定地块相邻，与盆地西缘北部相邻的阿拉善地块，受南北相邻的祁连褶皱带和天山兴蒙褶皱带活动的影响，较稳定地块的范围比较狭窄，其南又有龙首山-中卫走滑断裂构造带存在。 |
