燕山期以后，华南形成的构造格局为：扬子—特提斯构造域及太平洋构造域。
After the Yanshan movement, the tectonic framework formed in South China is the Yangtze Tethys structural domain and the Pacific structural domain.
第二发展阶段从燕山期以来，发展成为一条平移断裂带，属于狭义的环太平洋构造域的平移系统。
Second stage is a wrench fault system, which belongs to the Pacific Ocean cycle regime in narrow sense during the Yanshanian and Himalayan periods.
鄂尔多斯盆地地处中国沉积盆地分布的中带，兼受东滨太平洋构造域和西南特提斯-喜马拉雅构造域的影响，是我国第二大含油气盆地。
Ordos is the secondary petroliferous basin located at the middle zone of sedimentary basin in china, affected by The East Pacific tectonic process and The Southwest Tethys-Himalayas tectonic process.
鄂尔多斯盆地地处中国沉积盆地分布的中带，兼受东滨太平洋构造域和西南特提斯-喜马拉雅构造域的影响，是我国第二大含油气盆地。
Ordos is the secondary petroliferous basin located at the middle zone of sedimentary basin in china, affected by The East Pacific tectonic process and The Southwest Tethys-Himalayas tectonic process.
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