ISSN 1006-3021 CN11-3474/P
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2014年5月云南盈江MS5.6、MS6.1地震发震构造分析
  
关键词:Yingjiang earthquake  seismogenic fault  seismic intensity  Sudian fault  Tengchong block
基金项目:中国地质调查局项目(编号: 1212011120163; 12120114002101); 国家自然科学基金项目(编号: 41171009)和中央级公益性科研院所基本科研业务费项目(编号: DZLXJK201410)
作者单位E-mail
黄小龙 中国地质科学院地质力学研究所
北京大学 
tinyloong@163.com 
吴中海 中国地质科学院地质力学研究所 wzhh4488@sina.com 
赵小艳 云南省地震局  
吴坤罡 中国地质科学院地质力学研究所
中国地质大学(北京) 
 
黄小巾 首都师范大学  
杜锦锦 中国地质大学(北京)  
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摘要:
Seismogenic Structure of 2014 MS5.6 and MS6.1 Earthquakes in Yingjiang, Yunnan Province
      Two earthquakes of MS5.6 and MS6.1 occurred successively on May, 2014, in Yingjiang, Yunnan province. In order to determine their seismogenic structures and the regional active tectonic settings, the authors carried out field investigation of seismic intensity, remote sensing image interpretation, analysis of focal mechanism solutions and aftershock distribution. The results show that the macro-epicenters of two earthquakes were both located near the area of Malipo Village, Mengnong Township, Yingjiang County, but their seismogenic faults are different from each other. The former was associated with the NE-trending left-lateral strike-slip Xima-Panlongshan fault, whereas the latter occurred along the SN-trending right-lateral strike-slip Sudian fault. Historical seismicities were dominated by the earthquakes with magnitude 5~6 in the Yingjiang region, which clustered along the SN-trending fault. Under the combination effect of Sagaing fault and inner arc belt in western Yunnan, the north of Tengchong block bounded by Dayingjiang fault is mainly dominated by nearly SN-trending right-lateral strike slip faults, whereas the south is dominated by NE-trending left-lateral strike slip faults. The activity of nearly NS-tranding faults was relatively stronger in Late Quaternary.
HUANG Xiao-long,WU Zhong-hai,ZHAO Xiao-yan,WU Kun-gang,HUANG Xiao-jin,DU Jin-jin.2015.Seismogenic Structure of 2014 MS5.6 and MS6.1 Earthquakes in Yingjiang, Yunnan Province[J].Acta Geoscientica Sinica,36(6):761-770.
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