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The Qianhe River flows between the Liupanshan Orogen and the Ordos Block, with the river valley controlled by the southern margin fault of the Ordos Block. Five asymmetrical terraces exist on the banks of the Qianhe River, which correspond to the five terraces of the Wei River. Each terrace is composed of alluvial deposits at the bottom beneath loess deposits, which are characterized by alternating...
The Wei River Basin is located between the Qinling Orogenic Belt and the Ordos Block. It is an important seismic belt and part of the Silk Road in China. The development of the basin is the result of interaction between the Qinling Orogenic Belt and the Ordos Block. Based on the geomorphic features, sedimentary characteristics, and geophysical detection data, combined with the tectonic movement of...
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