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IDENTIFICATION OF SHEAR WAVE PROPAGATION AND INVERSION, OF NONLINEARLITY OF SOIL IN SEDIMENTARY BASIN : Analysis of weak motion and strong motion observed at a vertical array at Kuno district in the Ashigara Valley

机译：沉积盆地土壤非线性的剪切波传播和逆转的鉴定：散瞳区Kuno区垂直阵列弱运动和强运动分析

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Toshimi SATOH; Toshiaki SATO; Hiroshi KAWASE;
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年度 1993
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1. Inversion of strain-dependent nonlinear characteristics of soils using weak and strong motions observed by borehole sites in Japan [J] . Satoh T., Tatsumi Y., Fushimi M. Bulletin of the Seismological Society of America . 2001,第2期

机译：日本井场观测到的弱和强运动反演土壤应变相关的非线性特征
2. Multiple estimates of soil structure at a vertical strong motion array: Understanding uncertainties from different shear wave velocity profiles [J] . Raptakis Dimitrios, Makra Konstantia Engineering Geology . 2015,第Null期

机译：垂直强运动阵列下土壤结构的多种估计：了解不同剪切波速度剖面的不确定性
3. Shear-wave velocity profile at the Texcoco strong-motion array site, Valley of Mexico [J] . Bill Stephenson, Cinna Lomnitz Geofisica internacional . 2005,第1期

机译：墨西哥谷Texcoco强运动阵列场地的剪切波速度剖面
4. Simplified model of wave propagation by Normalized Input-Output Minimization (NIOM) and its application to strong motion records of Hiyoshi vertical array [C] . H. Kawakami, H.R. Haddadi European conference on earthquake engineering . 1998

机译：归一化输入输出最小化（NIOM）简化波传播模型及其在Hiyoshi垂直阵列强运动记录中的应用
5. Improved Shear Wave Motion Detection Using Pulse-Inversion Harmonic Imaging with a Phased Array Transducer [O] . Pengfei Song, Heng Zhao, Matthew W. Urban, -1

机译：使用相控阵换能器的脉冲反转谐波成像改进的剪切波运动检测
6. SIMULATION OF SITE AMPLIFICATION FACTORS OBTAINED FROM BOREHOLE RECORDS CONSIDERING BOTH TWO-DIMENSIONAL EFFECT AND NONLINEAR BEHAVIOR OF SOIL SEDIMENTS : Analysis of weak motion and strong motion observed at a vertical array at Kuno district in the Ashigara Valley [O] . Toshimi SATOH, Hiroshi KAWASE 1995

机译：考虑到土壤沉积物二维效应和非线性行为的钻孔记录的现场扩增因子模拟：散瞳区kuno区垂直阵列观察到弱运动和强运动的分析
7. Analysis of Near-Source Waves: Separation of Wave Types Using Strong Motion Array Recordings [R] . Darragh, R. B. 1988

机译：近源波分析：利用强运动阵列记录分离波型

IDENTIFICATION OF SHEAR WAVE PROPAGATION AND INVERSION, OF NONLINEARLITY OF SOIL IN SEDIMENTARY BASIN : Analysis of weak motion and strong motion observed at a vertical array at Kuno district in the Ashigara Valley

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