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jrfapp: A Python Package for Joint Inversion of Apparent S-Wave Velocity and Receiver Function Time Series
Receiver function (RF) inversion is a well-established method to quantify a horizontally layered approximation of the S-wave velocity structure...
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A two-step multi-frequency receiver function inversion method for shallow crustal S-wave velocity structure and its application across the basin-mountain range belts in Northeast China
A shallow crustal velocity structure (above 10 km depth) is essential for understanding the crustal structures and deformation and assessing the...
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S-wave velocity inversion and prediction using a deep hybrid neural network
The S-wave velocity is a critical petrophysical parameter in reservoir description, prestack seismic inversion, and geomechanical analysis. However,...
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Three-dimensional S-wave velocity structure of the crust and upper mantle for the normal fault system beneath the Yinchuan Basin from joint inversion of receiver function and surface wave
A series of parallel normal faults are distributed in the Helan Mountain-Yinchuan Basin tectonic belt, where a historical M8.0 earthquake occurred....
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Examination of one-dimensional S-wave velocity structure using strong-motion data for high-seismic-intensity area during the 2018 Hokkaido Eastern Iburi earthquake
The Yufutsu Plain, a sedimentary basin surrounded by mountains, is located in the southern part of the Ishikari–Yufutsu Lowlands, Hokkaido, Japan....
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Estimating S-wave amplitude for earthquake early warning in New Zealand: Leveraging the first 3 seconds of P-Wave
This study addresses the critical question of predicting the amplitude of S-waves during earthquakes in Aotearoa New Zealand (NZ), a highly...
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Seismic Hazard Implications in and Around the Yedisu Seismic Gap (Eastern Türkiye) Based on Coulomb Stress Changes, b-Values, and S-wave Velocity
The Yedisu Seismic Gap is one of the most important seismic gaps throughout the North Anatolian Fault Zone since it has not produced destructive...
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Three-dimensional S-wave velocity structure of the upper crust in the Guangdong-Hong Kong-Macao Greater Bay Area: insights into the basins structure and genesis of hot springs
As one of the four largest bay areas with strong economic activities in the world, the Guangdong-Hong Kong-Macao Greater Bay Area (GHMGBA) is located...
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Simultaneous Estimation of P- and S-Wave Velocities by Integrated Inversion of Guided-P and Surface Wave Dispersion Curves
Compared with surface wave corresponding to the normal mode, which is widely studied, there is less research on guided-P wave corresponding to the...
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P-, S-wave velocity and VP/VS of the Colima Volcanic Complex from local earthquake tomography
The Colima Volcanic Complex (CVC), located in western Mexico, is a complex tectonic area dominated by subduction processes and the deformation and...
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Ambient noise tomography for a high-resolution 3D S-wave velocity model of the Kinki Region, Southwestern Japan, using dense seismic array data
Research interest in the Kinki region, southwestern Japan, has been aroused by the frequent occurrence of microearthquake activity that do not always...
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Clay soil porosity estimation using seismic P- and S-wave velocities along Isfahan Metro Line 2
To study how the soils, respond to an earthquake, seismic waves are frequently utilized. The purpose of this work is to build the porosity graphs...
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Deep Velocity Structure of Southeast Asia from Rayleigh Wave Group Velocities: 3D Isotropic Model of the S-Wave Velocity Distribution in the Upper Mantle
AbstractWe present the results of studying the deep velocity structure of the crust and upper mantle beneath Southeast Asia based on data from a...
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Examination of shallow and deep S-wave velocity structures from microtremor array measurements and receiver function analysis at strong-motion stations in Kathmandu basin, Nepal
The Himalayan collision zone, where the Indian Plate subducts beneath the Eurasian Plate at a low angle, has caused many devastating earthquakes. The...
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Shear wave velocity (Vs) and SPT resistance (N) correlation for the Isfahan Metro, Iran
Some soil characteristics, such as the shear wave velocity, the shear modulus, the Poisson ratio, and the porosity, affect how clay soils behave. The...
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Water Effects on Elastic S-Wave Propagation and Attenuation Across Single Clay-Rich Rock Fractures: Insights from Ultrasonic Measurements
Though previous studies have shown that the presence of water strongly influences wave responses of rock fractures, water effects on wave behaviours...
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Research on the differential coefficient least-squares optimization method of reverse time migration in acoustic-reflected S-wave imaging logging
The numerical dispersion phenomenon in the finite-difference forward modeling simulations of the wave equation significantly affects the imaging...
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Effects of pressure and fluid properties on S-wave attenuation of tight rocks based on ultrasonic experiments
The tight oil/gas reservoirs in China have showed the great exploration prospects and high production potential, with the characteristics of low...
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S-Wave Velocity Structure in the City of Oued Fodda, Northern Algeria, by Inversion of Rayleigh Wave Ellipticity
The city of Oued Fodda is located in north-central Algeria in the margins of the middle Cheliff basin. This region has suffered several destructive...
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Detailed S-wave velocity structure of sediment and crust off Sanriku, Japan by a new analysis method for distributed acoustic sensing data using a seafloor cable and seismic interferometry
The S-wave velocity ( V s) structure of sediments and the uppermost crust in the landward slope of a subduction zone are important for determining the...
