| GPS资料反映的日本东北MW9.0地震的孕震特征 |
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| 引用本文： | 陈光齐,武艳强,江在森,刘晓霞,赵静.GPS资料反映的日本东北MW9.0地震的孕震特征[J].地球物理学报,2013,56(3):848-856. |
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| 作者姓名： | 陈光齐 武艳强 江在森 刘晓霞 赵静 |
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| 作者单位： | 1. 中国地震局地震预测重点实验室 中国地震局地震预测研究所, 北京 100036;
2. 日本九州大学, 福冈 8160000;
3. 中国地震局地质研究所地震动力学国家重点实验室, 北京 100029 |
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| 基金项目： | 地震行业专项，日本JSPS科研费(基盘研究，22310113 |
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| 摘 要： | 在对海洋板块俯冲型地震孕震模式的分阶段变形特征进行分析的基础上,结合同震位错反演结果分析了MW9.0级地震的同震变形特征,分析过程中通过精度检验讨论了该反演结果的可靠性.通过对震前和同震GPS结果的对比分析,讨论了二者的差异性.GPS应变(率)结果表明,震前日本岛应变积累主要反映了太平洋板块和菲律宾板块的俯冲作用,同震结果表现为指向震源方向拉张应变的释放,对日本岛的主要影响区域介于35°N和43°N之间.震前和同震GPS剖面结果反映的变形特征具有互补性,但量值相差上百倍.震前的GPS速度、应变率剖面和时间序列结果表明靠近日本岛东海岸一侧可能存在变形趋于极限现象.通过对此次地震可能前兆的分析表明,中长期预测方面、震前GPS时间序列的趋势性偏离、前震活动、震源区b值降低等现象在一定程度上反映了此次地震的孕震特征.
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| 关 键 词： | 孕震模式 同震位错反演 GPS应变率场 GPS剖面分析 |
| 收稿时间： | 2012-04-06 |
Characteristics of seismogenic model of MW9.0 earthquake in Tohoku, Japan reflected by GPS data |
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| CHEN Guang-Qi
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WU Yan-Qiang
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JIANG Zai-Sen
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LIU Xiao-Xia
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ZHAO Jing.Characteristics of seismogenic model of MW9.0 earthquake in Tohoku, Japan reflected by GPS data[J].Chinese Journal of Geophysics,2013,56(3):848-856. |
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| Authors: | CHEN Guang-Qi WU Yan-Qiang JIANG Zai-Sen LIU Xiao-Xia ZHAO Jing |
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| Institution: | 1. CEA Key Laboratory of Earthquake Prediction Institute of Earthquake Science, China Earthquake Administration, Beijing 100036, China;
2. Kyushu University, Fukuoka, 8160000, Japan;
3. State Key Laboratory of Earthquake Dynamics, Institute of Geology, CEA, Beijing 100029, China |
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| Abstract: | Based on the analysis of deformation characteristics in different stages of seismogenic model in oceanic plate subduction regions, we analyzed the coseismic deformation characteristics of MW9.0 earthquake using the inversion result of coseismic dislocation, whose reliability has been analyzed before used. Then, we discussed the differences between longterm and coseismic deformation from GPS data. GPS strain (rate) illustrates that the strain accumulation reflects the seduction effects of Pacific and Philippine plate before this earthquake, while the result of coseismic event reflects tension strain release whose affecting region mainly located between 35°N and 43°N. The deformation features reflected by GPS profile before earthquake and coseismic event are complementary, though the value differs by hundreds of times. GPS velocity and strain rate profile and GPS time-series results showed that the deformation had possibly reached its limit on the east coast of Japan. Through analyzing the possible precursor of this earthquake, the result including medium- and long-term forecasting, deviation to tendency background of GPS time series, pre-earthquake events and decreasing of b-value in hypocenter region, perhaps reflect the characteristics of seismogenic model in some extent. |
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| Keywords: | Seismogenic model Inversion of coseismic dislocation GPS strain rate field Analysis of GPS profile |
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