Neotectenic Stress Field and Landslide Erosion

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Publication date
1 January 1998
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Abstract

根据水系地貌学数据研究认为黄土高原新构造应力场的主压应力方向为Ｎ５８°Ｅ，其起源于印度板块和欧亚板块的碰撞。野外调查和遥感地图分析，发现了安塞县南部的古滑坡侵蚀群，滑坡移动方向受控于新构造应力场。长武王东沟现代滑坡移动方向与新构造应力场的主压应力方向一致。滑坡侵蚀对小流域高含沙水流的形成起着重要的作

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    Institute of Soil and Water Conservation,Chinese Academy of Sciences and Ministry of Water Resources

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