摘要
利用陆地卫星像片、历史文献资料、考古发掘资料、地层钻孔和地层剖面资料,运用综合分析对比方法,揭示出全新世以来洛阳盆地水系变化具有如下基本规律:即洛河河道不断北移;伊河河道不断东延加长,河曲不断南北摆动;涧河在东周到隋唐的时期内,由于人为作用而不断改变流路.
According to landsat photos, historic data, archaeology data and layer, the multiple method was used to study Rivers Change in Luoyang Basin in Holocene. The results showed that there are some basic laws in the Rivers change：Luo River course moves towards north constantly; Yi River course is longer and longer than it before, and its band moves from south to north and then comes back constantly; Jian niver course was changed many times because of artifical action in a period of Dong Zhou to Tang Dynasty.
出处
《信阳师范学院学报（自然科学版）》
CAS
北大核心
2006年第4期490-493,共4页
Journal of Xinyang Normal University(Natural Science Edition)
基金
河南省自然科学基金资助项目(0511020500)
河南省教育厅自然科学基金资助项目(200510480006)
河南省高校青年骨干教师资助项目(2005-182)
