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Stress Modeling for Upper and Lower Crust and Implications in Southeastern Tibetan Plateau

https://doi.org/10.2139/ssrn.4673834
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On the state of stress in the near-surface of the earth's crust
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The Stress Field in the Upper Crust as Determined from In Situ Measurements
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Tectonic Stress Redistribution Induced by Geothermal Gradient Difference: Numerical Modeling of Stress Around the Anninghe Seismic Gap in the Southeastern Tibetan Plateau
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GPS monitoring of temporal deformation of the Xianshuihe fault
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In situ stress state and seismic hazard in the Dayi seismic gap of the Longmenshan thrust belt
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The high-resolution community velocity model V2.0 of southwest China, constructed by joint body and surface wave tomography of data recorded at temporary dense arrays
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Evidence of crustal ‘channel flow’ in the eastern margin of Tibetan Plateau from MT measurements
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The effect of saturation on velocity in low porosity rocks
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Flow laws of multiphase rocks calculated from experimental data on the constituent phases
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Geotectonic relevance of rock-stress determinations
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The hydrofracturing stress measuring method and recent field results
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Trends in relationships between measured in-situ stresses and depth
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A theory for In Situ stresses in isotropic and transverseley isotropic rock
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Two crustal low-velocity channels beneath SE Tibet revealed by joint inversion of Rayleigh wave dispersion and receiver functions
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Stress estimation in rock: a brief history and review
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The role of fractures, effective pressure and loading on the difference between the static and dynamic Poisson's ratio and Young's modulus of Westerly granite
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Crustal ductile flow and its contribution to tectonic stress in Southwest China
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Implications of hydrostatic pore pressures and high crustal strength for the deformation of intraplate lithosphere
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The Mechanics of Earthquakes and Faulting
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Probabilistic Horizontal Stress Ratios in Rock
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Dislocation and diffusion creep of synthetic anorthite aggregates
inferredcites →https://doi.org/10.1029/2005jb003873openalex-extracted
Crustal structure beneath the eastern margin of the Tibetan Plateau and its tectonic implications
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Flow of synthetic, wet, partially molten “granite” under undrained conditions: An experimental study
inferredcites →https://doi.org/10.1029/2008jb005821openalex-extracted
Global variations of stress drop for moderate to large earthquakes
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Present‐Day Crustal Deformation of Continental China Derived From GPS and Its Tectonic Implications
inferredcites →https://doi.org/10.1029/90jb02491openalex-extracted
Flow laws of polyphase aggregates from end‐member flow laws
inferredcites →https://doi.org/10.1029/92jb00132openalex-extracted
First‐ and second‐order patterns of stress in the lithosphere: The World Stress Map Project
inferredcites →https://doi.org/10.1029/jb085ib11p06083openalex-extracted
The conference on magnitude of deviatoric stresses in the Earth's crust and uppermost mantle
inferredcites →https://doi.org/10.1029/jb085ib11p06231openalex-extracted
Some constraints on levels of shear stress in the crust from observations and theory
inferredcites →https://doi.org/10.1029/jb089ib11p09321openalex-extracted
Near‐surface in situ stress: Introduction
inferredcites →https://doi.org/10.1038/35075035openalex-extracted
Evolution of Asian monsoons and phased uplift of the Himalaya–Tibetan plateau since Late Miocene times
inferredcites →https://doi.org/10.1126/science.1155371openalex-extracted
The Geological Evolution of the Tibetan Plateau
inferredcites →https://doi.org/10.1126/science.276.5313.788openalex-extracted
Surface Deformation and Lower Crustal Flow in Eastern Tibet
inferredcites →https://doi.org/10.1130/0016-7606(1959)70[115:rofpim]2.0.co;2openalex-extracted
ROLE OF FLUID PRESSURE IN MECHANICS OF OVERTHRUST FAULTING
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Earthquake focal depths, effective elastic thickness, and the strength of the continental lithosphere
inferredcites →https://doi.org/10.1130/0091-7613(2000)28<703:tobtem>2.0.co;2openalex-extracted
Topographic ooze: Building the eastern margin of Tibet by lower crustal flow
inferredcites →https://doi.org/10.1130/g22924a.1openalex-extracted
Present-day kinematics at the India-Asia collision zone
inferredcites →https://doi.org/10.1146/annurev-earth-050212-124117openalex-extracted
Continental Lower Crust
inferredcites →https://doi.org/10.1146/annurev.earth.36.031207.124326openalex-extracted
Rheology of the Lower Crust and Upper Mantle: Evidence from Rock Mechanics, Geodesy, and Field Observations
inferredcites →https://doi.org/10.2118/38719-msopenalex-extracted
Stress Magnitudes From Logs: Effects of Tectonic Strains and Temperature
inferredcites →https://doi.org/10.2118/54653-paopenalex-extracted
Stress Magnitudes from Logs: Effects of Tectonic Strains and Temperature
inferredcites →https://doi.org/10.2747/0020-6814.44.1.39openalex-extracted
Faulting, Flow, and the Strength of the Continental Lithosphere
inferredcites →https://doi.org/10.3389/feart.2023.1153744openalex-extracted
Effect of rheological heterogeneities on the lithospheric deformation of the Tibetan Plateau and neighbouring regions
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