• 责任者：Liu Fang (Seismological Administration of Inner Mongolia Autonomous Region ; Hohhot 010010 ; China) ; Hu Bo
• 刊名：Seismological Research of Northeast China
• 出版年：2009
• 卷期：25(3)
• 关键词：强震 ; strong earthquakes ; 内蒙古 ; Inner Mongolia
• 页码：p.1-8
• 图表：7 illus., 1 table, 11 refs.
• 分类号：0500
• issnNo：ISSN1004-2865
• isbnNo：CN21-1108/P

The structural characteristics and the dynamic mechanism of China’s strong earthquake in the northeastern region show that NE and NW-trending fault formed the present tectonic framework in Northeast China, which controlled the northeastern regions of the geographical distribution of earthquake. The force of earthquake came from the driving of Japan Sea subduction. The 5.2 earthquake occurred between Arongqi and Elunchunqi on June 10, 2008. Analysis of the characteristics of seismic activity showed that there are the orderly migration image and orderly distribution of strong earthquakes.