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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*
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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
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Tian Rong-Heng 1,2, Xian Ben-Zhong 1,2, Chao Chu-Zhi 2, Liu Jian-Ping 3,4,5, Zhang Guo-Dong 6, Wang Jun-Hui 1,2, Chen Peng 1,2
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瑶曲铁路桥剖面典型沉积型水道特征(实测露头2-2,位置见 图 2 或 图 3 ) A—沉积型水道剖面特征;B—沉积型水道示意图;C—沉积型水道解释模型 |
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