摘要
我国水土流失严重地区 (段 )主要受控于地质构造 ,集中分布于不同的构造带、构造体系的结合部位、互相穿插交汇或复合等部位 ,特别是沿活动性深大断裂两侧更为明显突出。
Areas with heavy soil and water loss in our country are chiefly those at the mercy of their geological structure and are usually located in various structure zones, binding sites of tectonic systems, intersectant or overlapping areas, and , in particular near active rifts.
出处
《水土保持研究》
CSCD
2003年第3期105-106,共2页
Research of Soil and Water Conservation
基金
地震科学联合基金资助项目 ( 1980 89)
