Lacustrine tempestite and its geological significance in the Cenozoic study of the Qaidam Basin

@inproceedings{Li2014LacustrineTA,
  title={Lacustrine tempestite and its geological significance in the Cenozoic study of the Qaidam Basin},
  author={Fengjie Li and Yuchuan Yang and Junwu Li and Chengjin Yang and Tingyong Dai and Junxing Zhao and Yi Haisheng},
  year={2014}
}
Abstract During the Cenozoic a typical lacustrine tempestite deposition was developed in the Lulehe and Xichagou sections of the Qaidam Basin. The sedimentary structures of these two sections above are examined here in detail, which consist of storm erosion, storm tear, storm wave and rapid storm-generated sedimentary structures after storm processes, such as groove casts, scour structures, cutoff structures, hummocky cross-stratification (HCS), parallel bedding and graded bedding. On the basis… CONTINUE READING