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P-wave transmission across fractures with nonlinear deformational behaviour

https://doi.org/10.1002/nag.515
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What this work says

Outgoing claims: the papers this work cites, builds on, or argues with.

inferredcites →https://doi.org/10.1007/978-3-0348-8179-1_12openalex-snapshot
Modelling Seismic Waves Around Underground Openings in Fractured Rock
inferredcites →https://doi.org/10.1007/pl00001253openalex-snapshot
Modelling Seismic Waves Around Underground Openings in Fractured Rock
inferredcites →https://doi.org/10.1007/s006030170023openalex-snapshot
Transmission of Elastic P-waves across Single Fractures with a Nonlinear Normal Deformational Behavior
inferredcites →https://doi.org/10.1016/0148-9062(76)90566-0openalex-snapshot
Methods of geological engineering in discontinuous rocks.
inferredcites →https://doi.org/10.1016/0148-9062(83)90595-8openalex-snapshot
Fundamentals of rock joint deformation
inferredcites →https://doi.org/10.1016/0148-9062(85)93227-9openalex-snapshot
Strength, deformation and conductivity coupling of rock joints
inferredcites →https://doi.org/10.1016/0148-9062(91)92362-3openalex-snapshot
Transmission of seismic waves across single natural fractures
inferredcites →https://doi.org/10.1016/0148-9062(93)92914-copenalex-snapshot
Seismic wave propagation across multiple fractures
inferredcites →https://doi.org/10.1016/0148-9062(94)90625-4openalex-snapshot
Introduction to elastic wave propagation
inferredcites →https://doi.org/10.1016/0886-7798(96)00054-5openalex-snapshot
Construction and utilization of rock caverns in Singapore Part A: The Bukit Timah granite bedrock resource
inferredcites →https://doi.org/10.1016/s0148-9062(96)00022-8openalex-snapshot
The seismic response of fractures and the interrelations among fracture properties
inferredcites →https://doi.org/10.1016/s1365-1609(00)00013-7openalex-snapshot
Effects of multiple parallel fractures on apparent attenuation of stress waves in rock masses
inferredcites →https://doi.org/10.1016/s1365-1609(00)00037-xopenalex-snapshot
Oscillation elimination in the Hopkinson bar apparatus and resultant complete dynamic stress–strain curves for rocks
inferredcites →https://doi.org/10.1029/95jb02846openalex-snapshot
Fracture interface waves
inferredcites →https://doi.org/10.1029/jb095ib06p08617openalex-snapshot
Transmission of seismic waves across single natural fractures
inferredcites →https://doi.org/10.1029/jb095ib07p11345openalex-snapshot
Anisotropy in seismic velocities and amplitudes from multiple parallel fractures
inferredcites →https://doi.org/10.1061/(asce)0733-9399(2006)132:6(641)openalex-snapshot
Normal Transmission of S-Wave Across Parallel Fractures with Coulomb Slip Behavior
inferredcites →https://doi.org/10.1061/(asce)0899-1561(2002)14:3(262)openalex-snapshot
Testing and Response of Large Diameter Brittle Materials Subjected to High Strain Rate
inferredcites →https://doi.org/10.1115/1.3424152openalex-snapshot
An Approximate Method of Analysis of the Transmission of Elastic Waves Through a Frictional Boundary
inferredcites →https://doi.org/10.1121/1.385077openalex-snapshot
Elastic wave behavior across linear slip interfaces
inferredcites →https://doi.org/10.1121/1.428292openalex-snapshot
Stop-pass behavior of acoustic waves in a 1D fractured system
inferredcites →https://doi.org/10.1190/1.1442685openalex-snapshot
A calculus for finely layered anisotropic media
inferredcites →https://doi.org/10.1190/1.1443748openalex-snapshot
Seismic anisotropy of fractured rock
inferredcites →https://doi.org/10.1520/gtj10246jopenalex-snapshot
Measurements of Coupled Normal Deformation, Permeability, and Heat Transfer in Rock Joints Using a Triaxial Test Facility
inferredcites →https://doi.org/10.1785/bssa0680040987openalex-snapshot
The effects of boundary friction on the propagation of elastic waves

What points at this work

Incoming claims: where this work appears in other papers’ reference lists and arguments.

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Dynamic Response of Jointed Rock Mass Under Repeated Impact Disturbances and Evolution of Constitutive Model Parameters
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Study of wave attenuation across parallel fractures using propagator matrix method
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Validating the ability of the discontinuous deformation analysis method to model normal P‐wave propagation across rock fractures
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Investigation into the effect of fault properties on wave transmission
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Analytical study of ground motion caused by seismic wave propagation across faulted rock masses
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Transmission of Tensile Stress Wave Across a Nonlinear Deformable Rock Joint: A Theoretical Investigation
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Transmission of Seismic Waves With Tensile Components Across Cemented Rock Discontinuities Exhibiting Tension‐Softening Behavior
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Propagation Characteristics of Stress Wave in Rock
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Two-Characteristic Method for the Wave Propagation Through Joint
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Two-Characteristic Method for the Wave Propagation Through Complex Stratus Rock Mass
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A Split Three-Characteristic Method for Stress Wave Propagation Through Rock Mass with Double-Scale Discontinuities
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Theoretical Methods for Wave Propagation across Jointed Rock Masses
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Wave Propagation in Discontinuous Media by the Scattering Matrix Method
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Effects of a Single Open Joint on Energy Transmission Coefficients of Stress Waves with Different Waveforms
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Analytical Study for Stress Wave Interaction with Rock Joints Having Unequally Close–Open Behavior
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Stress Wave Propagation Across a Rock Mass with Two Non-parallel Joints
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Analytical Time-Domain Solution of Plane Wave Propagation Across a Viscoelastic Rock Joint
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Propagation of the Stress Wave Through the Filled Joint with Linear Viscoelastic Deformation Behavior Using Time-Domain Recursive Method
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Research on Transient Wave Propagation Across Nonlinear Joints Filled with Granular Materials
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Velocity Amplification of Seismic Waves Through Parallel Fractures Near a Free Surface in Fractured Rock: A Theoretical Study
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A Split Three-Characteristics Method for Stress Wave Propagation Through a Rock Mass with Double-Scale Discontinuities
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Effect of Nonlinear Deformational Macrojoint on Stress Wave Propagation Through a Double-Scale Discontinuous Rock Mass
inferred← citeshttps://doi.org/10.1007/s00603-021-02644-3openalex-snapshot
Dual-Mesh Three Characteristic Lines Method for Stress Wave Propagation Through a Microdefected Rock Mass with a Thin-Layer Filled Macrojoint
inferred← citeshttps://doi.org/10.1007/s00603-021-02730-6openalex-snapshot
Tensile Strength and Deformational Behavior of Stylolites and Mineral Healed Joints Subject to Dynamic Direct Tension
inferred← citeshttps://doi.org/10.1007/s00603-022-02840-9openalex-snapshot
Critical Angles of Obliquely Incident Stress Wave Through a Single Joint with Different Mediums on Both Sides
inferred← citeshttps://doi.org/10.1007/s00603-022-03004-5openalex-snapshot
Dynamic Mechanical Behaviors of Rock's Joints Quantified by Repeated Impact Loading Experiments with Digital Imagery
inferred← citeshttps://doi.org/10.1007/s00603-022-03181-3openalex-snapshot
UDEC Modelling on Dynamic Response of Rock Masses with Joint Stiffness Weakening Attributed to Particle Crushing of Granular Fillings
inferred← citeshttps://doi.org/10.1007/s00603-024-03800-1openalex-snapshot
Propagation of the Longitude Stress Wave through a Filled Fracture Considering Cyclic Loading/Unloading Behaviours
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Parametric Simulation of Stress Wave Propagation Affected by High-Temperature Damage in Rocks Using a Coupled DLSM-DDA Method
inferred← citeshttps://doi.org/10.1007/s00603-026-05499-8openalex-snapshot
Tensile Stress Wave Propagation Across Non-persistent Rock Joints and Comparison with Compressive Stress Wave: An Experimental Study
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Study of Multi-frequency Plane Stress Wave Propagation Through a Two-Dimensional Structural Interface
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Scattering of plane SH waves by a concentric semi-cylindrical discontinuity and canyon
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Dynamic Response to Seismic Waves at the Shallow Slope Supported by Bolts
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DEVELOPMENT OF A 3D NUMERICAL MODEL FOR SIMULATING A BLAST WAVE PROPAGATION SYSTEM CONSIDERING THE POSITION OF THE BLASTING HOLE AND IN-SITU DISCONTINUITIES
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Characteristics of Compressive Stress Wave Propagation Across a Nonlinear Viscoelastic Filled Rock Joint
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