上扬子地台区长期接受地台型沉积，地壳构造较稳定。但自喜马拉雅运动以来，断褶构造活动强烈。按上扬子地台区超晚期断褶构造发育程度，可划分为５个构造区。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。应用超晚期断褶构造分区的观点，可预测上扬子地台区金属矿产资源及含油气远景。 Upward platform area to accept long-term deposition, the crustal structure is more stable. However, since the Himalayan movement, the fold-forming activity has been strong. According to the superdeveloped fold-tectonic development in the upper Yangtze platform, it can be divided into five tectonic zones. The development of ultra-late fold-fault tectonics controls the formation and distribution of oil and gas resources and metallogenic resources in the Upper Yangtze platform area. Applying the view of ultra-late fold-forming tectonic zoning can predict the metallogenic resources and hydrocarbon-bearing vista in the Upper Yangtze platform area.