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.
出处
《山东煤炭科技》
2010年第3期97-98,共2页
Shandong Coal Science and Technology
关键词
沂沭断裂带
新近纪
活动特征
Yi - Shu Fault neogene activity characteristic
