Formation of the basin is closely relative to the development of the South Dabashan-Dahongshan Orogenic Belt.
盆地的形成与南大巴山—大洪山造山带的发育密切相关。
For Kala Kunlun and Tarim, two kinds of rock associations, passive continental marginal basin and collision orogenic belt, are developed corresponding to each cycle.
对应每一旋回，喀喇昆仑地层区和塔里木地层区发育有被动大陆边缘盆地和碰撞造山两种类型的岩石组合。
Beihuaiyang basin and range structural belt is an important part of Dabie orogenic belt.
北淮阳盆岭构造带是大别造山带的重要组成部分。
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