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1)  The East China Sea and adjacent regions
东海及邻近地区
2)  East China Sea and adjacent regions
东海及邻区
3)  Central and Western Shandong and its adjacent areas
山东中西部及邻近地区
1.
Based Atkinson(1992) method,the nonelastic attenuation in Central and Western Shandong and its adjacent areas was inversed with the digital seismic wave data recorded by 10 stations in Shandong digital seismic network from June 2004 to August 2007,and the relation of Q value with frequency we got is Q(f)=382.
利用山东数字地震台网10个地震台自2004年6月至2007年8月记录的数字波形资料,采用Atkinson(1992)方法反演了山东中西部及邻近地区的非弹性衰减,得到该地区Q值与频率的关系是Q(f)=382。
4)  East China Sea and its vicinity
东海及邻近海域
5)  Shanghai and adjacent area
上海及其邻近地区
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6)  Qinghai and its neighboring region
青海及邻近区域
1.
In this paper,we use the data of Qinghai Province and its neighboring region as the research object,analyze regional geological structure,historic earthquake distribution and focal mechanism solutions,and the earthquake catalog of Qinghai and its neighboring region,divide the earthquake active cycles,and analyze energy release laws.
0级地震发生以后,未来地震趋势如何,是人们十分关心的问题,本文以青海省及邻近区域为研究对象,运用区域地质构造、历史地震分布、震源机制解及青海及邻近区域的地震目录等,进行周期划分,能量释放分析等方面研究。
补充资料：太平洋地区标准会议标准(见太平洋地区标准会议)


太平洋地区标准会议标准(见太平洋地区标准会议)
standards of PASC: see Pacific Area Standards Congress; PASC

Ta iPingyang Diqu Bioozhun Hu呼ib沁幻Zhun太平洋地区标准会议标准(s切md田心sofR巧C)见太平洋地区标准会议。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
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