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.
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.
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