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A river erosion estimate on the Loess Plateau: A case study from Luohe River, a second-order tributary of the Yellow River

  • CAS - Guangzhou Institute of Geochemistry
  • CAS - Institute of Earth Environment
  • Chinese Academy of Sciences

科研成果: 期刊稿件文章同行评审

14 引用 (Scopus)

摘要

Based on fieldwork and terrace ages, which were determined using 14C, TL and paleosol stratigraphy, a general model was established for the development of the Yellow River terrace system. The ages for the terraces and valley flats of the Yellow River system are T6 - 1.67-0.85 Ma BP, T5 - 0.85-0.47 Ma BP, T4 - 0.47-0.10 Ma BP, T3 - 0.10-0.007 Ma BP, T2 - 7.0-0.7 ka BP, T 1 - 0.7-0.3 ka BP, the higher valley flat - 0.3-0.15 ka BP and the lower valley flat 0.15-0 ka BP, respectively. Each terrace or valley flat and corresponding paleo-valley represents a river erosion/deposition cycle. Using this model and selected geomorphic parameters of terraces and paleo-valleys from 10 typical cross sections of Luohe River, a tributary of the Yellow River, an attempt is made here to estimate paleo-river erosion since the Pleistocene on the Loess Plateau.

源语言英语
页(从-至)215-220
页数6
期刊Global and Planetary Change
41
3-4
DOI
出版状态已出版 - 7月 2004
已对外发布

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