摘要
本文对沂、沭河中游地区的突出地貌特征进行了研究分析,在此基础上进而对区内的地貌演进过程和新构造运动特征提出了自己的认识。
In this paper the author, based on the analyses of several prominent geomorphologic features in the middle region of Yi and Shu Rivers, puts forward original opinions on the process of geomorphologic evolution and the characters of neotectonic movement.
出处
《山东师范大学学报（自然科学版）》
CAS
1989年第1期55-61,共7页
Journal of Shandong Normal University(Natural Science)
关键词
沂沭河中游
新构造运动
剥夷地面
middle region of Yi and Shu rivers,planation surface,river terrace,neotectonic movement
