摘要
<正>Objective The tectonic response of the Ordos Basin to Indosinian movement mainly occurred in the southwestern part of the basin due to the Late Triassic collisional Qinling orogeny to the south.The orogeny resulted in intense uplift and exhumation of the southwestern section of the Ordos
引文
Liu Chiyang,Zhao Hongge,Zhao Junfeng,Wang Jianqiang Zhang Dongdong and Yang Minghui,2008.Temporo-spatial coordinates of evolution of the Ordos Basin and its mineralization responses.Acta Geologica Sinica(English Edition),82(6):1229-1243.