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机译:通过远震波形分析和InSAR确定安第斯山脉中部地壳地震的深度和震源机制
Office of New Reactors, U.S. Nuclear Regulatory Commission, Mail Stop 7 F3, Washington, DC 20555-0001, USA;
Department of Earth and Atmospheric Sciences, Cornell University, Ithaca, New York, USA,Department of Earth and Atmospheric Sciences, Cornell University, Snee Hall, Ithaca, NY 14853, USA;
Department of Earth and Atmospheric Sciences, Cornell University, Ithaca, New York, USA,Department of Earth and Atmospheric Sciences, Cornell University, Snee Hall, Ithaca, NY 14853, USA;
Department of Earth and Atmospheric Sciences, Cornell University, Ithaca, New York, USA,Department of Earth and Atmospheric Sciences, Cornell University, Snee Hall, Ithaca, NY 14853, USA;
Department of Earth and Atmospheric Sciences, Cornell University, Ithaca, New York, USA,Department of Earth and Atmospheric Sciences, Cornell University, Snee Hall, Ithaca, NY 14853, USA;
机译:利用远震P波形确定中亚地震震源深度和震源时间函数
机译:利用远震波形模拟估算喜马拉雅-藏族地区地震的震源深度
机译:利用远震波形模拟估算喜马拉雅-藏族地区地震的震源深度
机译:中南部安第斯山脉普纳高原内陆地壳形变力学的InSAR观测
机译:中深度地震,平板应力状态和安第斯山脉中北部北部的上地幔结构。
机译:勘误表:海啸产生的磁场可能会限制地震的震源机制
机译:中央和中央地区地区地区的深度和焦点机制,从Telesismic波形分析和Insar确定