机译:从基模和高模Scholte-Rayleigh波的环境噪声相关性分析出发,东太平洋上升年轻岩石圈的结构
Department of Earth and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA 02139, USA,Institute of Geophysics and Planetary Physics, Scripps Institute of Oceanography, University of California, San Diego, La jolla, CA 92093, USA;
Department of Earth and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA 02139, USA;
Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA;
Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA;
Department of Earth and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, MA 02139, USA;
east pacific rise; lithosphere; oceanic uppermost mantle; low-velocity zone; ambient noise; fundamental- and higher-mode scholte-rayleigh waves;
机译:基频共振控制的基模和高模瑞利波传播的环境噪声互相关观测
机译:浅周期环境噪声瑞利波速率结构的浅剪切波速度结构从伊朗东北地区的波束形成和互相关技术
机译:通过研究东太平洋南部上升西翼的局部板内地震,研究海洋岩石圈的各向异性:剪切波分裂和波形模拟
机译:东北太平洋低频环境噪声水平的趋势
机译:来自环境噪声断层扫描的东亚岩石圈结构
机译:从环境噪声相关性看与苏门答腊大地震有关的表面波速度的时空变化
机译:基本谐振治理的基本噪声横相关观察的环境噪声横相关观察
机译:东太平洋上升的年轻上地壳结构在9度30分左右N.(新可用性信息的重新报告)