湖相重力流水道沉积特征与沉积模式:以鄂尔多斯盆地瑶曲铁路桥剖面三叠系延长组为例*
田荣恒1,2, 鲜本忠1,2, 晁储志2, 刘建平3,4,5, 张国栋6, 王俊辉1,2, 陈鹏1,2

Sedimentary characteristics and model of lacustrine gravity flow channels: a case study of the Triassic Yanchang Formation of Yaoqu railway-bridge section in Ordos Basin
Tian Rong-Heng1,2, Xian Ben-Zhong1,2, Chao Chu-Zhi2, Liu Jian-Ping3,4,5, Zhang Guo-Dong6, Wang Jun-Hui1,2, Chen Peng1,2
瑶曲铁路桥剖面洪水型水道沉积特征 A—炭屑,拍自实测露头3;B—定向排列的植物碎屑,拍自实测露头3;C—黄褐色泥砾呈低角度定向排列,拍自实测露头2-2;D—黄褐色泥砾杂乱排列,拍自实测露头2-3