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Terrace dating as an archive of the run-through of the Sanmen Gorges
引用本文:PAN Baotian,WANG Junping,GAO Hongshan,CHEN Yingying,LI Jijun,LIU Xiaofeng. Terrace dating as an archive of the run-through of the Sanmen Gorges[J]. 自然科学进展(英文版), 2005, 15(12): 1096-1103. DOI: 10.1080/10020070512331343191
作者姓名:PAN Baotian  WANG Junping  GAO Hongshan  CHEN Yingying  LI Jijun  LIU Xiaofeng
作者单位:Key Laboratory of Western China's Environmental Systems, Ministry of Education, and Department of Geography, Lanzhou University, Lanzhou 730000, China
基金项目:中国科学院资助项目,Innovation Team Project of National,教育部博士后科学基金,中国科学院资助项目
摘    要:Analysis of morphological properties in the Sanmen Gorges region of the Yellow River shows that four river terraces have been developed at the entrance to the gorges. Commonly, thick aeolian loess-paleosol sequence was deposited on the terraces, which makes it easy to date the terraces. The dating of paleomagnetic, loess-paleosol sequence matching and thermoluminescence show that terraces T2, T3 and T4 were formed 0.129 Ma, 0.625 Ma and 0.865 Ma ago, respectively. The formation of these terraces in this region indicates that the Yellow River has experienced four intensive downcutting events during the last 0.9 Ma. The Yellow River cut through the Sanmen Gorges and inpoured into the East China Sea no later than 0.865 Ma.

关 键 词:river terrace   paleomagnetic dating   Yellow River   loess.

Terrace dating as an archive of the run-through of the Sanmen Gorges
PAN Baotian,WANG Junping,GAO Hongshan,CHEN Yingying,LI Jijun,LIU Xiaofeng. Terrace dating as an archive of the run-through of the Sanmen Gorges[J]. Progress in Natural Science, 2005, 15(12): 1096-1103. DOI: 10.1080/10020070512331343191
Authors:PAN Baotian  WANG Junping  GAO Hongshan  CHEN Yingying  LI Jijun  LIU Xiaofeng
Affiliation:Key Laboratory of Western China's Environmental Systems, Ministry of Education, and Department of Geography, Lanzhou University, Lanzhou 730000, China
Abstract:Analysis of morphological properties in the Sanmen Gorges region of the Yellow River shows that four river terraces have been developed at the entrance to the gorges. Commonly, thick aeolian loess-paleosol sequence was deposited on the terraces, which makes it easy to date the terraces. The dating of paleomagnetic, loess-paleosol sequence matching and thermoluminescence show that terraces T2, T3 and T4 were formed 0. 129 Ma, 0. 625 Ma and 0. 865 Ma ago, respectively. The formation of these terraces in this region indicates that the Yellow River has experienced four intensive downcutting events during the last 0.9 Ma. The Yellow River cut through the Sanmen Gorges and inpoured into the East China Sea no later than 0. 865 Ma.
Keywords:river terrace  paleomagnetic dating  Yellow River  loess
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