准噶尔盆地南缘的构造样式类型以断裂和褶皱的各种组合类型为主。
The tectonic patters of south margin of Junggar basin are composed of the composition of faults and folds mostly.
二连盆地是在海西期褶皱基底上发育起来的，为早白垩世断陷群。
Erlian basin is the Early Cretaceous rift group formed and developed on the Hecynian folded belt.
塔里木盆地库车褶皱冲断带克拉苏构造带在古近系膏盐岩之下发育克拉苏三角带。
The Kelasu triangle zone occurs under the Paleogene evaporites in Kelasu anticline zone of Kuqa thrust-and-fold belts, Tarim basin (Northwest China).
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