褶皱构造带 meaning in Chinese
folded tectogene
Examples
- The kangmar region is located in the north himalayan tectonic zone , in which the stratums are a series of fold tectonic zone whose direction is approximately east - west
康马地区处于北喜马拉雅构造带。区内地层整体呈一系列近东西向的褶皱构造带，在此基础上还叠加有南北向构造。 - 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。 - According to these results combined with exploration practice , foot favorable exploration zones are selected , these are the integrated anticline traps below the tertiary gypsum halite , gypsum mudstone in kuqa foreland thrust belts , the second and the third row structural bells in southern junggar foreland thrust belt , the unconventional natural gas pools in die yanshan palaeohigh in north and south of western sichuan basin , the gentle fold structural belt in central sichuan basin and the deep depression in sichuan basin , and the cold take and nanbaxian structural belt in northern margin of qaidam basin
依据理论分析及勘探实践，优选出4个有利的勘探区带，它们是：库车前陆冲断带古近系、新近系膏盐岩、膏泥岩之下的完整背斜圈闭；准南前陆冲断带第二、第三排构造带；川西北部及南部燕山运动期古隆起、川中平缓褶皱构造带以及深坳陷内部的非常规天然气；柴北缘冷湖南八仙构造带。