沂沭断裂带新近纪活动特征分析  

Analysis of Activity Characteristic about Yi-Shu Fault

作　　者：刘美娟[1] 

机构地区：[1]山东科技大学地质科学与工程学院,山东青岛266510

出　　处：《山东煤炭科技》2010年第3期97-98,共2页Shandong Coal Science and Technology

摘　　要：沂沭断裂带是山东境内一条重要的构造带,对山东的构造格局、沉积矿产的形成等有重要的影响,受到了国内外学者的广泛重视。本文通过对沂沭断裂带的主要构造特征,在新时期的受力状态,及一些新的构造地貌类型的分析,得出沂沭断裂带仍是一个活动的断裂。Yishu fault zone is an important tectonic zone in Shandong province, which has an essential influence on the tectonic framework, the formation of mineral deposits of Shandong province, so this fault zone receives extensive attention of scholars home and abroad. In this paper, we carry ore＂ analysis on the main tectonic feature, the force status in new period and some new type of tectonic landforms, arriving at a conclusion that Yishu fault zone is still moveable.

关 键 词：沂沭断裂带 新近纪 活动特征 

分 类 号：P548.205.2[天文地球—构造地质学]