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A lithospheric velocity model for the flat slab region of Argentina from joint inversion of Rayleigh wave phase velocity dispersion and teleseismic receiver functions

机译：从瑞利波相位速度色散和Telesmic接收机功能的联合反演中阿根廷平板区域的岩性速度模型

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Jean-Baptiste Ammirati; Patricia Alvarado; Susan Beck;
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机译：Saudi Arabia下面的剪切速度结构从P和S波接收器功能的联合反演，以及瑞利波组速度色散数据
2. Shear Velocity Model of Alaska Via Joint Inversion of Rayleigh Wave Ellipticity, Phase Velocities, and Receiver Functions Across the Alaska Transportable Array [J] . Berg Elizabeth M., Lin Fan-Chi, Allam Amir, Journal of geophysical research. Solid earth: JGR . 2020,第2期

机译：Alaska剪切速度模型通过瑞利波椭圆形，相位速度，相位速度的关节反转和横跨阿拉斯加可运输阵列的接收器功能
3. Lithospheric structure of the Chinese mainland determined from joint inversion of regional and teleseismic Rayleigh-wave group velocities [J] . Mei Feng, Meijian An Journal of geophysical research. Solid earth: JGR . 2010,第B6期

机译：区域和远震瑞利波群速度联合反演确定的中国大陆岩石圈结构
4. Inversion of Rayleigh Wave Dispersion Curves Considering the Sensitivities of Phase Velocities to S-wave Velocities [C] . Xuefeng Liu, Youhua Fan International conference on environmental and engineering geophysics . 2012

机译：考虑相速度对S波速度敏感性的瑞利波频散曲线反演
5. Lithospheric structure beneath Eastern Africa from joint inversion of receiver functions and Rayleigh wave velocities. [D] . Dugda, Mulugeta Tuji. 2007

机译：由接收器功能和瑞利波速度的联合反演，东非下方的岩石圈结构。
6. Phase velocities and attentuations of shear Lamb and Rayleigh waves in plate-like tissues submerged in a fluid (L) [O] . Ivan Z. Nenadic, Matthew W. Urban, Miguel Bernal, -1

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7. Estimation of S-Wave Velocity Structure Model by Joint Inversion of Site Amplification, Receiver Function and Phase Velocity of Rayleigh Wave [O] . Hiroyuki MIURA, Atsuko MATSUO, Tatsuo KANNO, 2017

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8. Developing Regionalized Models of Lithospheric Thickness and Velocity Structure Across Eurasia and the Middle East from Jointly Inverting P-Wave and S-Wave Receiver Functions with Rayleigh Wave Group and Phase Velocities. [R] . Julia, J., Matzel, E., Nyblade, A. A., 2011

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A lithospheric velocity model for the flat slab region of Argentina from joint inversion of Rayleigh wave phase velocity dispersion and teleseismic receiver functions

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