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作 者:FANG LiHua WU JianPing WANG ChangZai WANG WeiLai YANG Ting
机构地区:[1]Institute of Geophysics,China Earthquake Administration
出 处:《Science China Earth Sciences》2014年第2期216-220,共5页中国科学(地球科学英文版)
基 金:supported by Key Projects in the National Science & Technology Pillar Program during the Twelfth Five-year Plan Period(Grant No.2012BAK19B01);Science and Research Program of Chinese Earthquake Industry(Grant Nos.201308013,201208009);Institute of Geophysics,China Earthquake Administration(Grant Nos.DQJB12C02,DQJB10B24)
摘 要:At 05:07 AM on June 30, 2012 (Beijing time), an Ms6.6 earthquake (hereafter referred to as Xinyuan earthquake) occurred at the junction of Xinyuan County, Ili Kazak Au tonomous Prefecture and Hejing County, Bayinguoleng Mongol Autonomous Prefecture in Xinjiang Uygur .At 05:07 AM on June 30,2012(Beijing time),an Ms6.6earthquake(hereafter referred to as Xinyuan earthquake)occurred at the junction of Xinyuan County,Ili Kazak Autonomous Prefecture and Hejing County,Bayinguoleng Mongol Autonomous Prefecture in Xinjiang Uygur Autonomous Region.The location of the main shock determined by China Earthquake Network Center is 43.4°N,84.8°E and focal depth is 7 km.By the end of 08:00 AM
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