伊通地堑是一个主体在海西期褶皱基底上发育起来的第三纪含油气走滑断陷盆地。
The Yitong Graben is a Tertiary petroliferous strike-slip fault basin developed on the Hercynian fold basement.
二连盆地是在海面褶皱基底上发育起来的中新生代断陷湖盆群，共发育大小不等的50个凹陷。
Erlian basin, a cluster of rift lake basins in the Mesozoic and Cenozoic eras developed on the base of the Hercynian fold belt, consists of 50 sags in different scale.
海拉尔盆地是在华力西褶皱基底上形成的中生代断陷盆地。
Hailar basin is a fault-depressed basin formed on Variscan folded basement.
因此，江南隆起带褶皱基底这一宏观变形强烈、微观变形甚弱的现象属于低温下准塑性变形结果。
The phenomenon of high macroscopic deformation and low microcosmic deformation of the folded basement in the Jiangnan uplift is attributed to the quasi-plastic deformation at low temperatures.
晚白垩纪后，构造变形表现为一系列重新活动的基底断裂和新生断裂，褶皱构造简单。
After late Cretaceous, structural deformation shows a series of movable basement fault again and new's fault. The fold structure is very simple.
基底冲断隆起带与川北类前陆盆地平缓褶皱带，在调节两侧造山带构造平衡时表现出明显的差异性。
Due to basement rock rigidity, basement thrustuplift zone and northern Sichuan paraforeland zone have marked disparity in the process of adjusting structural balance.
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.
该带不仅是一个地理界线，而且是一个由基底断裂带控制的前第三系雁列褶皱带和第三系构造转换带。
It serves not only as a geographic boundary but also as pre-tertiary en-echelon drapes and a Cenozoic tectonic conversion zone controlled by the basement fault zone.
吐哈盆地是具有双层基底的叠合盆地，被4个华力西期褶皱带围限。
Turpan-hami basin, which is surrounded with 4 Variscides, is an overlay basin with a bilamellar basement.
吐哈盆地是具有双层基底的叠合盆地，被4个华力西期褶皱带围限。
Turpan-hami basin, which is surrounded with 4 Variscides, is an overlay basin with a bilamellar basement.
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