川西北盆地在新生代是一个典型的构造叠加区域，来自龙门山和米仓山的变形在此相互作用。
The Northwest Sichuan Basin is a typical tectonic superposition region in Cenozoic, where the deformations transferred from the Longmenshan and Micangshan affected together.
川西北盆地在新生代是一个典型的构造叠加区域，来自龙门山和米仓山的变形在此相互作用。
The Northwest Sichuan Basin is a typical tectonic superposition region in Cenozoic, where the deformations transferred from the Longmenshan and Micangshan affected together.
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