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鲁甸地震(M_s6.5)临震预测、中期预测及中地壳流变结构

Imminent and Medium-Term Predictions for Ludian Earthquake(M_s6.5)and Rheological Structure of the Middle Crust

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【作者】 曾佐勋刘根深李献瑞贺赤诚杨学祥杨冬红

【Author】 Zeng Zuoxun;Liu Genshen;Li Xianrui;He Chicheng;Yang Xuexiang;Yang Donghong;Three Gorges Research Center for Geo-hazard,Ministry of Education,China University of Geosciences;School of Earth Sciences,China University of Geosciences;Huazhong Tectonomechanical Research Center;Institute of Geophysics & Geomatics,China University of Geosciences;College of Geo-exploration Science and Technology,Jilin University;Research Center of Palaeontology & Stratigraphy,Jilin University;Key-Lab for Evolution of Past Life and Environment in Northeast Asia,Ministry of Education,Jilin University;

【机构】 中国地质大学教育部长江三峡库区地质灾害研究中心中国地质大学地球科学学院中国地质大学华中构造力学研究中心中国地质大学地球物理与空间信息学院吉林大学地球探测科学与技术学院吉林大学古生物学与地层学研究中心吉林大学东北亚生物演化与环境教育部重点实验室

【摘要】 2014年8月3日16时30分,在云南省昭通市鲁甸县(27.1°N,103.3°E)发生Ms6.5地震,震源深度10km,死亡617人,失踪112人,受伤3 143人,受灾人口108.84万人.根据月亮赤纬角、太阳黑子极值年等周期变化及两者的叠加效应,总结出2013—2014年是云南强震高危期,具备Ms7地震的发生条件.次年,利用基础SW前兆仪的临震预测指纹法信息,制定了2014年底211号地震预测表,预测了2014年8月四川(26.18°N,105.33°E)将发生Ms5.3地震发生.2014年8月3日云南鲁甸Ms6.5地震表明:这次地震的指纹法预测时间相差1天,震中相差226km,震级误差Ms1.2.通过构造背景、地壳速度结构和震源机制研究,NW向的包谷垴-小河左旋走滑断裂是鲁甸地震的发震断裂.中下地壳低速(高导)体与包谷垴-小河断裂交接部位是流变界面能量释放的位置,即本次地震的震源位置,为板内地震三层次构造模式提供了一个新的案例.

【Abstract】 At 16:30of August 3rd,2014,an earthquake with a magnitude of Ms6.5occurred in Ludian County of Zhaotong City,Yunnan Province(27.1°N,103.3°E).The depth of the hypocenter is 10 km.Due to this disaster,617 people were died,112 people disappeared and 108 840 000 people were injured.According to the superposition effects of the moon declination angle,sunspot extreme year cycles and the two,summed up 2013—2014years is Yunnan strong earthquake periods of high risk,with the condition for the occurrence of Ms7 earthquake.The following year,forecast method based SW fingerprint informationusing the earthquake precursory instrument,developed by the end of 2014 211 earthquake prediction table,predict 2014 August Sichuan(26.18°N,105.33°E)Ms5.3earthquake will occur.The Ludian Ms6.5earthquake occurred on August 3,2014 indicates that the error of the predicted date is only 1day,the predicted epicenter is about 226 km away from the actual earthquake epicenter.Besides that the actual magnitude is Ms1.2larger than the predicted magnitude.According to the comprehensive analysis in tectonic setting,the S-wave crustal velocity structure and the focus mechanism of the Ludian earthquake,we believe that the Baogunao-Xiaohe left-lateral strike-slip fault triggered the Ludian earthquake,while the junction of the middlelow crusts low-velocity(high-conductivity)body and the Baogunao-Xiaohe fault is the location of the focus releasing the accumulated energy which practically is the epicenter.This provides a new case study of the three-level tectonic model for intraplate earthquakes.

【基金】 国家“985”创新平台建设项目子课题(地震及其次生地质灾害研究);国家自然科学基金重点项目(No.41230206);国家自然科学基金青年科学基金项目(No.41404041)
  • 【文献出处】 地球科学(中国地质大学学报) ,Earth Science(Journal of China University of Geosciences) , 编辑部邮箱 ,2014年12期
  • 【分类号】P315.7
  • 【被引频次】4
  • 【下载频次】232
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