但自喜马拉雅运动以来，断褶构造活动强烈。
There the crustal structure was relatively stable, but folding and faulting have been intense since the Himalayan movement.
超晚期断褶构造发育程度控制了上扬子地台区油气藏及金属矿产资源的形成与分布。
The formation and distribution of the petroleum and metallic mineral resources in the study region were controlled by the degree of development of the latest foldfault structures.
柴达木盆地西北地区花状断褶构造和后生表褶构造分布普遍，断裂活动具明显的剪切挤压性质。
Faulting and other tectonic activities in the Northwest Qaidam Basin are widespread and characterized by shearing and compression.
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