1. Southeastward increase of the late Quaternary slip-rate of the Xianshuihe fault, eastern Tibet. Geodynamic and seismic hazard implications;Bai;Earth Planet. Sci. Lett.,2018
2. Comprehensive multilevel exploration of buried active fault: an example of Yinchuan buried active fault;Chai;Seismol. Geol.,2006
3. Preliminary research on Megalake Jilantai-Fletao in the arid areas of China during the Late Quaternary;Chen;Chin. Sci. Bull.,2008
4. Preliminary study on the formation mechanism of the ‘Jilantai-Hetao’ megalake and the lake evolutionary history in Hetao region;Chen;Quat. Sci.,2008
5. The river terrace response to the connection of Hetao and Yinchuan Basin along the Gangdeer Mountain, north Ordos;Chen;Acta Sci. Nat. Univ. Sunyatseni,2014