前陆盆地是研究造山运动的关键地区之一。
大巴山前陆构造是后秦岭造山运动的陆内造山的结果。
The foreland of Daba Mountains resulted from the intracontinental orogeny of the Qingling orogenetic movements.
苏鲁的造山运动起始虽略晚于大别，但结束的更快，比大别更早进入了造山运动的后期。
The orogeny started late in Sulu, the orogeny, however, ends early. The orogeny in Sulu entered in the late period of the orogeny much earlier than that in Dabie.
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