Earthquake and Volcano Deformation
|
|
- Eunice Haynes
- 5 years ago
- Views:
Transcription
1 Earthquake and Volcano Deformation Paul Segall Stanford University Draft Copy September, 2005 Last Updated Sept, 2008 COPYRIGHT NOTICE: To be published by Princeton University Press and copyrighted, c 2007 by Paul Segall. All rights reserved. No part of this book may be reproduced in any form by any electronic or mechanical means (including photocopying, recording, or information storage and retrieval) without permission in writing from the publisher. Users are not permitted to mount this file on any network servers. For more information, send to permissions@press.princeton.edu.
2 Contents 1 Deformation, Stress, and Conservation Laws Strain Strains in Curvilinear Coordinates Rotation Stress Coordinate Transformations Principal Strains and Stresses Compatibility equations Conservation Laws Equilibrium equations in curvilinear coordinates Constitutive Laws Reciprocal Theorem Dislocation Models of Strike Slip Faults Full Space Solution Half Space Solution Coseismic Faulting Interseismic Deformation Postseismic Slip Distributed Slip Application to the San Andreas and Other Strike Slip Faults Displacement at Depth Summary Dip Slip Faults and Dislocations in Three Dimensions Volterra s Formula Body Force Equivalents and Moment Tensors Screw Dislocations Two Dimensional Edge Dislocations
3 4 CONTENTS Dipping Fault Coseismic Deformation Associated with Dipping Faults Displacements and Stresses due to Edge Dislocation at Depth Dislocations in three dimensions Full Space Green s Functions Half-Space Green s Functions Point Source Solutions Finite rectangular sources Examples Distributed Slip Strain Energy Change due to Faulting Problems References Crack Models of Faults Inversion of the Integral Equation Displacement on Earth s Surface A Brief Introduction to Fracture Mechanics Non Singular Stress Distributions Comparison of Slip Distributions and Surface Displacements Boundary Element Methods Fourier Transform Methods Some Three Dimensional Crack Results Problems References Elastic Heterogeneity Long Strike-Slip Fault Bounding Two Media Strike-Slip Fault Within a Compliant Fault Zone Strike-Slip Fault Beneath a Layer Strike-Slip Within a Layer over Half-space Propagator Matrix Methods The Propagator Matrix for Antiplane Deformation Vertical Fault in a Homogeneous Half-Space Vertical Fault Within Half-Space Beneath a Layer Vertical Fault in Layer over Half-Space General solution for an arbitrary number of layers Displacements and Stresses at Depth Propagator Methods for Plane Strain Propagator Solutions in Three Dimensions
4 CONTENTS Approximate Solutions for Arbitrary Variations in Properties Variations in Shear Modulus Screw dislocation Edge dislocation Effects of Elastic Heterogeneity on Inversions Problems References Postseismic Relaxation Elastic Layer over Viscous Channel Visco-Elasticity Correspondence Principle Strike-slip Fault in an Elastic Plate overlying a Viscoelastic Half-space Stress in Plate and Half-Space Strike Slip Fault in Elastic Layer Overlying a Viscoelastic Channel Dip Slip Faulting Examples Three Dimensional Calculations Concluding Remarks References Problems Volcano Deformation Spherical Magma Chamber Center of Dilatation Volume of the uplift, magma chamber, and magma Ellipsoidal Magma Chambers Magmatic Pipes and Conduits Dikes and Sills Crack models of dikes and sills Surface Fracturing and Dike Intrusion Other Magma Chamber Geometries Viscoelastic Relaxation Around Magma Chambers Problems References Topography and Earth Curvature Scaling Considerations Implementation Considerations Center of Dilatation beneath a volcano
5 6 CONTENTS 8.4 Earth s Sphericity Summary Problems References Gravitational Effects Non-dimensional Form of Equilibrium Equations Inclusion in propagator formulation Surface Gravity Approximation Gravitational effects in viscoelastic solutions Incompressible Half-Space No Buoyancy Approximation Wang approach Comparison of Different Viscoelastic Models Relaxed Viscoelastic Response Changes in Gravity Induced by Deformation Gravity Changes and Volcano Deformation An Example Problems Poroelastic Effects Constitutive Laws Macroscopic Descriptions Micromechanical Description Field Equations Analogy to Thermoelasticity One Dimensional Deformation Step Load on the Free Surface Time varying fluid load at the free surface Dislocations in Two Dimensions Inflating Magma Chamber in a Poroelastic Half-Plane Cummulative Poroelastic Deformation in Three Dimensions Solution when pore pressure distribution is known References Exercises Fault Friction Slip Weakening Friction Velocity Weakening Friction Rate and State Friction
6 CONTENTS Linearized Stability Analysis Implications for earthquake Nucleation Spring-Slider Stick Slip Cycles Non-linear stability analysis Afterslip Transient Slip Events Concluding Remarks Problems References Interseismic Deformation and Plate Boundary Cycle Models Elastic Dislocation Models Dip-slip faults Plate Motions Elastic Block Models Viscoelastic Cycle Models Viscoelastic Strike-Slip Earthquake Cycle Models Comparison to data from San Andreas Fault Viscoelastic Models with Stress Driven Deep Fault Creep Viscoelastic Cycle models For Dipping Faults Rate-State Friction Earthquake Cycle Models References Problems A Integral Transforms 495 A.1 Fourier Transforms A.2 Laplace Transforms B A Solution to the Diffusion Equation 501 C Solution of an Integral by Contour Methods 505
Overview of the PyLith Finite Element Code
Overview of the PyLith Finite Element Code www.geodynamics.org Charles Williams (GNS Science) Brad Aagaard (USGS) Matt Knepley (University of Chicago) CIG Software PyLith is a Tool for Crustal Deformation
More informationSecondary Project Proposal
Secondary Project Proposal Post-seismic deformation of Chi-chi earthquake Yunyue (Elita) Li 11:, Wednesday, June 2, 21 Li 2 Secondary project proposal Personal prospective MOTIVATION My interests for earthquake
More informationSurface changes caused by erosion and sedimentation were treated by solving: (2)
GSA DATA REPOSITORY 214279 GUY SIMPSON Model with dynamic faulting and surface processes The model used for the simulations reported in Figures 1-3 of the main text is based on two dimensional (plane strain)
More informationRheology III. Ideal materials Laboratory tests Power-law creep The strength of the lithosphere The role of micromechanical defects in power-law creep
Rheology III Ideal materials Laboratory tests Power-law creep The strength of the lithosphere The role of micromechanical defects in power-law creep Ideal materials fall into one of the following categories:
More informationThe Mechanics of Earthquakes and Faulting
The Mechanics of Earthquakes and Faulting Christopher H. Scholz Lamont-Doherty Geological Observatory and Department of Earth and Environmental Sciences, Columbia University 2nd edition CAMBRIDGE UNIVERSITY
More informationIntroduction: Advancing Simulations of Sequences of Earthquakes and Aseismic Slip (SEAS)
Introduction: Advancing Simulations of Sequences of Earthquakes and Aseismic Slip (SEAS) Brittany Erickson (Portland State University) Junle Jiang (University of California, San Diego) SCEC DR-SEAS Workshop,
More informationAnalytic and Numeric Tests of Fourier Deformation Model (Copyright 2003, Bridget R. Smith and David T. Sandwell)
Analytic and Numeric Tests of Fourier Deformation Model (Copyright 2003, Bridget R. Smith and David T. Sandwell) Although the solutions of our Fourier deformation model have been checked using computer
More informationMaterials and Methods The deformation within the process zone of a propagating fault can be modeled using an elastic approximation.
Materials and Methods The deformation within the process zone of a propagating fault can be modeled using an elastic approximation. In the process zone, stress amplitudes are poorly determined and much
More informationUsing deformation rates in Northern Cascadia to constrain time-dependent stress- and slip-rate on the megathrust
Using deformation rates in Northern Cascadia to constrain time-dependent stress- and slip-rate on the megathrust Lucile Bruhat Paul Segall Stanford University 1 50 Interseismic period for the Cascadia
More informationFRICTIONAL HEATING DURING AN EARTHQUAKE. Kyle Withers Qian Yao
FRICTIONAL HEATING DURING AN EARTHQUAKE Kyle Withers Qian Yao Temperature Change Along Fault Mode II (plain strain) crack rupturing bilaterally at a constant speed v r Idealize earthquake ruptures as shear
More informationMechanics of Earthquakes and Faulting
Mechanics of Earthquakes and Faulting 5 Sep. 2017 www.geosc.psu.edu/courses/geosc508 Work of deformation, shear and volume strain Importance of volume change and diltancy rate (rate of volume strain with
More informationTwo ways to think about the dynamics of earthquake ruptures
Two ways to think about the dynamics of earthquake ruptures (1) In terms of friction (2) In terms of fracture mechanics Scholz describes conditions for rupture propagation (i.e. instability) via energy
More information1 Introduction. 1.1 Aims. 1.2 Rock fractures
1 Introduction 1.1 Aims Rock fractures occur in a variety of geological processes and range in size from plate boundaries at the scale of hundreds of kilometres to microcracks in crystals at the scale
More informationMechanics of Earthquakes and Faulting
Mechanics of Earthquakes and Faulting www.geosc.psu.edu/courses/geosc508 Standard Solids and Fracture Fluids: Mechanical, Chemical Effects Effective Stress Dilatancy Hardening and Stability Mead, 1925
More informationEarthquake and Volcano Clustering at Mono Basin (California)
Excerpt from the Proceedings of the COMSOL Conference 2010 Paris Earthquake and Volcano Clustering at Mono Basin (California) D. La Marra *,1, A. Manconi 2,3 and M. Battaglia 1 1 Dept of Earth Sciences,
More informationSeismic and aseismic processes in elastodynamic simulations of spontaneous fault slip
Seismic and aseismic processes in elastodynamic simulations of spontaneous fault slip Most earthquake simulations study either one large seismic event with full inertial effects or long-term slip history
More informationSlow Slip and Tremor Along San Andreas fault system
Slow Slip and Tremor Along San Andreas fault system Slow slip in Upper Crust Aseismic creep, afterslip and spontaneous slow slip events on some faults in upper 15 km Mostly aseismic but accompanied by
More informationGeophysics Departmental Exam: 2004 Part 1
2004 Geophysics Departmental Exam: 2004 Part 1 This section is 90 minutes, closed book, and consists of questions designed to test your knowledge of facts and figures in the geosciences. The focus will
More informationSeparating Tectonic, Magmatic, Hydrological, and Landslide Signals in GPS Measurements near Lake Tahoe, Nevada-California
Separating Tectonic, Magmatic, Hydrological, and Landslide Signals in GPS Measurements near Lake Tahoe, Nevada-California Geoffrey Blewitt, Corné Kreemer, William C. Hammond, & Hans-Peter Plag NV Geodetic
More informationPredicted reversal and recovery of surface creep on the Hayward fault following the 1906 San Francisco earthquake
GEOPHYSICAL RESEARCH LETTERS, VOL. 35, L19305, doi:10.1029/2008gl035270, 2008 Predicted reversal and recovery of surface creep on the Hayward fault following the 1906 San Francisco earthquake D. A. Schmidt
More informationFault-Zone Properties arid Earthquake Rupture Dynamics
Fault-Zone Properties arid Earthquake Rupture Dynamics Eiichi Fukuyama National Research Institute for Earth Science,and Disaster Prevention Tsukuba, Japan i ':-> i' ' -':'.." \,' " '' L VH ELSEVIER AMSTERDAM
More informationELASTICITY AND FRACTURE MECHANICS. Vijay G. Ukadgaonker
THEORY OF ELASTICITY AND FRACTURE MECHANICS y x Vijay G. Ukadgaonker Theory of Elasticity and Fracture Mechanics VIJAY G. UKADGAONKER Former Professor Indian Institute of Technology Bombay Delhi-110092
More informationStress equilibrium in southern California from Maxwell stress function models fit to both earthquake data and a quasi-static dynamic simulation
Stress equilibrium in southern California from Maxwell stress function models fit to both earthquake data and a quasi-static dynamic simulation Peter Bird Dept. of Earth, Planetary, and Space Sciences
More informationContents. I Introduction 1. Preface. xiii
Contents Preface xiii I Introduction 1 1 Continuous matter 3 1.1 Molecules................................ 4 1.2 The continuum approximation.................... 6 1.3 Newtonian mechanics.........................
More informationMechanics of Earthquakes and Faulting
Mechanics of Earthquakes and Faulting www.geosc.psu.edu/courses/geosc508 Overview Milestones in continuum mechanics Concepts of modulus and stiffness. Stress-strain relations Elasticity Surface and body
More informationData Repository Hampel et al., page 1/5
GSA DATA REPOSITORY 2138 Data Repositor Hampel et al., page 1/5 SETUP OF THE FINITE-ELEMENT MODEL The finite-element models were created with the software ABAQUS and consist of a 1-km-thick lithosphere,
More informationBrittle Deformation. Earth Structure (2 nd Edition), 2004 W.W. Norton & Co, New York Slide show by Ben van der Pluijm
Lecture 6 Brittle Deformation Earth Structure (2 nd Edition), 2004 W.W. Norton & Co, New York Slide show by Ben van der Pluijm WW Norton, unless noted otherwise Brittle deformation EarthStructure (2 nd
More informationEstimating fault slip rates, locking distribution, elastic/viscous properites of lithosphere/asthenosphere. Kaj M. Johnson Indiana University
3D Viscoelastic Earthquake Cycle Models Estimating fault slip rates, locking distribution, elastic/viscous properites of lithosphere/asthenosphere Kaj M. Johnson Indiana University In collaboration with:
More informationSeismotectonics of intraplate oceanic regions. Thermal model Strength envelopes Plate forces Seismicity distributions
Seismotectonics of intraplate oceanic regions Thermal model Strength envelopes Plate forces Seismicity distributions Cooling of oceanic lithosphere also increases rock strength and seismic velocity. Thus
More informationFriction can increase with hold time. This happens through growth and increasing shear strength of contacts ( asperities ).
Friction can increase with hold time. This happens through growth and increasing shear strength of contacts ( asperities ). If sliding speeds up, the average lifespan of asperities decreases This means
More informationVolcano Seismicity and Tremor. Geodetic + Seismic
Volcano Seismicity and Tremor Seismic Imaging Geodetic + Seismic Model based joint inversion Geodetic Monitoring How is magma stored in the crust? geometry, volume and physical state of crustal melts.
More informationThe Frictional Regime
The Frictional Regime Processes in Structural Geology & Tectonics Ben van der Pluijm WW Norton+Authors, unless noted otherwise 1/25/2016 10:08 AM We Discuss The Frictional Regime Processes of Brittle Deformation
More informationRHEOLOGY Principles, Measurements, and Applications. Christopher W. Macosko
RHEOLOGY Principles, Measurements, and Applications I -56081-5'79~5 1994 VCH Publishers. Inc. New York Part I. CONSTITUTIVE RELATIONS 1 1 l Elastic Solid 5 1.1 Introduction 5 1.2 The Stress Tensor 8 1.2.1
More informationMechanics of Earthquakes and Faulting
Mechanics of Earthquakes and Faulting Lectures & 3, 9/31 Aug 017 www.geosc.psu.edu/courses/geosc508 Discussion of Handin, JGR, 1969 and Chapter 1 Scholz, 00. Stress analysis and Mohr Circles Coulomb Failure
More informationGround displacement in a fault zone in the presence of asperities
BOLLETTINO DI GEOFISICA TEORICA ED APPLICATA VOL. 40, N. 2, pp. 95-110; JUNE 2000 Ground displacement in a fault zone in the presence of asperities S. SANTINI (1),A.PIOMBO (2) and M. DRAGONI (2) (1) Istituto
More informationExercise: concepts from chapter 8
Reading: Fundamentals of Structural Geology, Ch 8 1) The following exercises explore elementary concepts associated with a linear elastic material that is isotropic and homogeneous with respect to elastic
More informationDETAILS ABOUT THE TECHNIQUE. We use a global mantle convection model (Bunge et al., 1997) in conjunction with a
DETAILS ABOUT THE TECHNIQUE We use a global mantle convection model (Bunge et al., 1997) in conjunction with a global model of the lithosphere (Kong and Bird, 1995) to compute plate motions consistent
More informationSyllabus and Course Description Geophysical Geodesy Fall 2013 GPH 411/611
Syllabus and Course Description Geophysical Geodesy Fall 2013 GPH 411/611 Course Location: LME 422 Course Time: Tuesday & Thursday 12:00-1:15 Units: 3 Instructor Name: Bill Hammond Office Location: SEM
More informationSource parameters II. Stress drop determination Energy balance Seismic energy and seismic efficiency The heat flow paradox Apparent stress drop
Source parameters II Stress drop determination Energy balance Seismic energy and seismic efficiency The heat flow paradox Apparent stress drop Source parameters II: use of empirical Green function for
More information} based on composition
Learning goals: Predict types of earthquakes that will happen at different plate boundaries based on relative plate motion vector vs. strike (vector subtraction) Understand interseismic and coseismic deformation,
More informationMechanics PhD Preliminary Spring 2017
Mechanics PhD Preliminary Spring 2017 1. (10 points) Consider a body Ω that is assembled by gluing together two separate bodies along a flat interface. The normal vector to the interface is given by n
More informationElizabeth H. Hearn modified from W. Behr
Reconciling postseismic and interseismic surface deformation around strike-slip faults: Earthquake-cycle models with finite ruptures and viscous shear zones Elizabeth H. Hearn hearn.liz@gmail.com modified
More informationINGV. Giuseppe Pezzo. Istituto Nazionale di Geofisica e Vulcanologia, CNT, Roma. Sessione 1.1: Terremoti e le loro faglie
Giuseppe Pezzo Istituto Nazionale di Geofisica e Vulcanologia, CNT, Roma giuseppe.pezzo@ingv.it The study of surface deformation is one of the most important topics to improve the knowledge of the deep
More informationU.S. South America Workshop. Mechanics and Advanced Materials Research and Education. Rio de Janeiro, Brazil. August 2 6, Steven L.
Computational Modeling of Composite and Functionally Graded Materials U.S. South America Workshop Mechanics and Advanced Materials Research and Education Rio de Janeiro, Brazil August 2 6, 2002 Steven
More informationWhat we should know about mechanics of materials
What we should know about mechanics of materials 0 John Maloney Van Vliet Group / Laboratory for Material Chemomechanics Department of Materials Science and Engineering Massachusetts Institute of Technology
More informationFalk Amelung. Sang-Ho Yun. Thomas Walter. Asta Miklius. now at GFZ Potsdam. Hawaii Volcano Observatory. Stanford University
Falk Amelung RSMAS - University of Miami Thomas Walter now at GFZ Potsdam Sang-Ho Yun Stanford University Asta Miklius Hawaii Volcano Observatory Pinatubo 1991 Bautista et al., 98 Mount Pinatubo erupted
More informationPEAT SEISMOLOGY Lecture 12: Earthquake source mechanisms and radiation patterns II
PEAT8002 - SEISMOLOGY Lecture 12: Earthquake source mechanisms and radiation patterns II Nick Rawlinson Research School of Earth Sciences Australian National University Waveform modelling P-wave first-motions
More information3D Finite Element Modeling of fault-slip triggering caused by porepressure
3D Finite Element Modeling of fault-slip triggering caused by porepressure changes Arsalan Sattari and David W. Eaton Department of Geoscience, University of Calgary Suary We present a 3D model using a
More information3D Elasticity Theory
3D lasticity Theory Many structural analysis problems are analysed using the theory of elasticity in which Hooke s law is used to enforce proportionality between stress and strain at any deformation level.
More informationRotation of the Principal Stress Directions Due to Earthquake Faulting and Its Seismological Implications
Bulletin of the Seismological Society of America, Vol. 85, No. 5, pp. 1513-1517, October 1995 Rotation of the Principal Stress Directions Due to Earthquake Faulting and Its Seismological Implications by
More informationCOSSERAT THEORIES: SHELLS, RODS AND POINTS
COSSERAT THEORIES: SHELLS, RODS AND POINTS SOLID MECHANICS AND ITS APPLICATIONS Volume 79 Series Editor: G.M.L. GLADWELL Department of Civil Engineering University of Waterloo Waterloo, Ontario, Canada
More informationCan geodetic strain rate be useful in seismic hazard studies?
Can geodetic strain rate be useful in seismic hazard studies? F. Riguzzi 1, R. Devoti 1, G. Pietrantonio 1, M. Crespi 2, C. Doglioni 2, A.R. Pisani 1 Istituto Nazionale di Geofisica e Vulcanologia 2 Università
More informationA new hybrid numerical scheme for modelling elastodynamics in unbounded media with near-source heterogeneities
A new hybrid numerical scheme for modelling elastodynamics in unbounded media with near-source heterogeneities Setare Hajarolasvadi Ahmed E. Elbanna https://www.youtube.com/watch?v=bltx92tuwha MOTIVATION
More informationGeology for Engineers Rock Mechanics and Deformation of Earth Materials
89.325 Geology for Engineers Rock Mechanics and Deformation of Earth Materials Why do rocks break? Rock mechanics experiments a first order understanding. Faults and Fractures Triaxial load machine. a)
More informationGeophysical Journal International
Geophysical Journal International Geophys. J. Int. (2010) 182, 1124 1140 doi: 10.1111/j.1365-246X.2010.04678.x A unified continuum representation of post-seismic relaxation mechanisms: semi-analytic models
More informationModule 3 : Equilibrium of rods and plates Lecture 15 : Torsion of rods. The Lecture Contains: Torsion of Rods. Torsional Energy
The Lecture Contains: Torsion of Rods Torsional Energy This lecture is adopted from the following book 1. Theory of Elasticity, 3 rd edition by Landau and Lifshitz. Course of Theoretical Physics, vol-7
More informationAfterslip, slow earthquakes and aftershocks: Modeling using the rate & state friction law
Afterslip, slow earthquakes and aftershocks: Modeling using the rate & state friction law Agnès Helmstetter (LGIT Grenoble) and Bruce Shaw (LDE0 Columbia Univ) Days after Nias earthquake Cumulative number
More informationHomogeneous vs. realistic heterogeneous material-properties in subduction zone models: Coseismic and postseismic deformation
Homogeneous vs. realistic heterogeneous material-properties in subduction zone models: Coseismic and postseismic deformation T. Masterlark 1, C. DeMets 2, H.F. Wang 2, O. S nchez 3, and J. Stock 4 1 US
More information1. classic definition = study of deformed rocks in the upper crust
Structural Geology I. Introduction 1. classic definition = study of deformed rocks in the upper crust deformed includes translation, rotation, and strain (change of shape) All rocks are deformed in some
More informationGravitational deformation after the April 6, 2009 L Aquila Earthquake detected by Cosmo-SkyMed
Gravitational deformation after the April 6, 2009 L Aquila Earthquake detected by Cosmo-SkyMed Christian Bignami 1 ; Matteo Albano 1 ; Salvatore Barba 1 ; Mario Costantini 2 ; Fabio Malvarosa 2 ; Marco
More informationKinematics of the Southern California Fault System Constrained by GPS Measurements
Title Page Kinematics of the Southern California Fault System Constrained by GPS Measurements Brendan Meade and Bradford Hager Three basic questions Large historical earthquakes One basic question How
More informationEarthquakes and Seismotectonics Chapter 5
Earthquakes and Seismotectonics Chapter 5 What Creates Earthquakes? The term Earthquake is ambiguous: Applies to general shaking of the ground and to the source of the shaking We will talk about both,
More informationGravity Tectonics Volcanism Atmosphere Water Winds Chemistry. Planetary Surfaces
Gravity Tectonics Volcanism Atmosphere Water Winds Chemistry Planetary Surfaces Gravity & Rotation Polar flattening caused by rotation is the largest deviation from a sphere for a planet sized object (as
More informationDeformation of a layered half-space due to a very long tensile fault
Deformation of a layered half-space due to a very long tensile fault Sarva Jit Singh and Mahabir Singh Department of Mathematics, Maharshi Dayanand University, Rohtak 124 1, India. e-mail: s j singh@yahoo.com
More informationModeling the Thermal-Mechanical Behavior of Mid-Ocean Ridge Transform Faults
Excerpt from the Proceedings of the COMSOL Conference 2008 Boston Modeling the Thermal-Mechanical Behavior of Mid-Ocean Ridge Transform Faults Emily C Roland *1, Mark Behn,2 and Greg Hirth 3 1 MIT/WHOI
More informationFor an imposed stress history consisting of a rapidly applied step-function jump in
Problem 2 (20 points) MASSACHUSETTS INSTITUTE OF TECHNOLOGY DEPARTMENT OF MECHANICAL ENGINEERING CAMBRIDGE, MASSACHUSETTS 0239 2.002 MECHANICS AND MATERIALS II SOLUTION for QUIZ NO. October 5, 2003 For
More informationMechanics of Earthquakes and Faulting
Mechanics of Earthquakes and Faulting www.geosc.psu.edu/courses/geosc508 Surface and body forces Tensors, Mohr circles. Theoretical strength of materials Defects Stress concentrations Griffith failure
More informationCOPYRIGHTED MATERIAL. Index
Index A Admissible function, 163 Amplification factor, 36 Amplitude, 1, 22 Amplitude-modulated carrier, 630 Amplitude ratio, 36 Antinodes, 612 Approximate analytical methods, 647 Assumed modes method,
More informationThe Non-Linear Field Theories of Mechanics
С. Truesdell-W.Noll The Non-Linear Field Theories of Mechanics Second Edition with 28 Figures Springer-Verlag Berlin Heidelberg NewYork London Paris Tokyo Hong Kong Barcelona Budapest Contents. The Non-Linear
More informationTopics. Magma Ascent and Emplacement. Magma Generation. Magma Rise. Energy Sources. Instabilities. How does magma ascend? How do dikes form?
Magma Ascent and Emplacement Reading: Encyclopedia of Volcanoes: Physical Properties of Magmas (pp. 171-190) Magma Chambers (pp. 191-206) Plumbing Systems (pp. 219-236) Magma ascent at shallow levels (pp.237-249)
More informationfriction friction a-b slow fast increases during sliding
µ increases during sliding faster sliding --> stronger fault --> slows sliding leads to stable slip: no earthquakes can start velocity-strengthening friction slow fast µ velocity-strengthening friction
More informationPhysical Science and Engineering. Course Information. Course Number: ME 100
Physical Science and Engineering Course Number: ME 100 Course Title: Course Information Basic Principles of Mechanics Academic Semester: Fall Academic Year: 2016-2017 Semester Start Date: 8/21/2016 Semester
More informationERTH 456 / GEOL 556 Volcanology. Lecture 06: Conduits
1 / 28 ERTH 456 / GEOL 556 Volcanology Lecture 06: Conduits Ronni Grapenthin rg@nmt.edu MSEC 356, x5924 hours: TR 3-4PM or appt. September 12, 2016 2 / 28 How does magma get from source to surface? What
More informationRHEOLOGY & LINEAR ELASTICITY. B Importance of fluids and fractures in deformation C Linear elasticity for homogeneous isotropic materials
GG303 Lecture 2 0 9/4/01 1 RHEOLOGY & LINEAR ELASTICITY I II Main Topics A Rheology: Macroscopic deformation behavior B Importance of fluids and fractures in deformation C Linear elasticity for homogeneous
More informationQualitative modeling of earthquakes and aseismic slip in the Tohoku-Oki area. Nadia Lapusta, Caltech Hiroyuki Noda, JAMSTEC
Qualitative modeling of earthquakes and aseismic slip in the Tohoku-Oki area Nadia Lapusta, Caltech Hiroyuki Noda, JAMSTEC Constitutive law on the fault: Rate-and-state friction at low slip rates + Potential
More informationTransition from stick-slip to stable sliding: the crucial effect of asperities
Transition from stick-slip to stable sliding: the crucial effect of asperities Strasbourg, 15 Nov. 2007 François Renard LGCA, CNRS-OSUG, University of Grenoble, France PGP, University of Oslo, Norway Collaborators:
More informationEnabling Technologies
Enabling Technologies Mechanical Modelling 1 Key Parameter Mineral System Exploration is reflected in scale-dependent translation A. Gradient in hydraulic potential B. Permeability C. Solubility sensitivity
More informationFINITE ELEMENT ANALYSIS OF COMPOSITE MATERIALS
FINITE ELEMENT ANALYSIS OF COMPOSITE MATERIALS Ever J. Barbero Department of Mechanical and Aerospace Engineering West Virginia University USA CRC Press Taylor &.Francis Group Boca Raton London New York
More informationElements of Rock Mechanics
Elements of Rock Mechanics Stress and strain Creep Constitutive equation Hooke's law Empirical relations Effects of porosity and fluids Anelasticity and viscoelasticity Reading: Shearer, 3 Stress Consider
More informationTheory of Elasticity
Theory of Elasticity Aldo Maceri Theory of Elasticity 123 Prof. Dr.-Ing. Aldo Maceri Universitá Roma Tre Departimento di Ingegneria Meccanica e Industriale Via della Vasca Navale, 79 00146 Roma Italy
More informationPhysics and Chemistry of the Earth and Terrestrial Planets
MIT OpenCourseWare http://ocw.mit.edu 12.002 Physics and Chemistry of the Earth and Terrestrial Planets Fall 2008 For information about citing these materials or our Terms of Use, visit: http://ocw.mit.edu/terms.
More informationBifurcation Analysis in Geomechanics
Bifurcation Analysis in Geomechanics I. VARDOULAKIS Department of Engineering Science National Technical University of Athens Greece and J. SULEM Centre d'enseignement et de Recherche en Mecanique des
More informationMohr's Circle and Earth Stress (The Elastic Earth)
Lect. 1 - Mohr s Circle and Earth Stress 6 Mohr's Circle and Earth Stress (The Elastic Earth) In the equations that we derived for Mohr s circle, we measured the angle, θ, as the angle between σ 1 and
More informationSupporting Information for Inferring field-scale properties of a fractured aquifer from ground surface deformation during a well test
GEOPHYSICAL RESEARCH LETTERS Supporting Information for Inferring field-scale properties of a fractured aquifer from ground surface deformation during a well test Jonathan Schuite 1, Laurent Longuevergne
More informationLecture 20: Slow Slip Events and Stress Transfer. GEOS 655 Tectonic Geodesy Jeff Freymueller
Lecture 20: Slow Slip Events and Stress Transfer GEOS 655 Tectonic Geodesy Jeff Freymueller Slow Slip Events From Kristine Larson What is a Slow Slip Event? Slip on a fault, like in an earthquake, BUT
More informationINFLUENCE OF LOCAL PERTURBATION ON REGIONAL STRESS AND ITS IMPACT ON THE DESIGN OF MAJOR UNDERGROUND STRUCTURE IN HYDROELECTRIC PROJECT
INFLUENCE OF LOCAL PERTURBATION ON REGIONAL STRESS AND ITS IMPACT ON THE DESIGN OF MAJOR UNDERGROUND STRUCTURE IN HYDROELECTRIC PROJECT *D.S. Subrahmanyam National Institute of Rock Mechanics, Bangalore
More informationEarthquake nucleation. Pablo Ampuero Caltech Seismolab
Earthquake nucleation Pablo Ampuero Caltech Seismolab How do earthquakes start? Do small and large earthquakes start differently? Predictive value of earthquake onset and foreshock sequences? Seismological
More informationWhat is the Relationship between Pressure & Volume Change in a Magma Chamber and Surface Deformation at Active Volcanoes?
SSAC-pv2007.QE522.PL1.1 What is the Relationship between Pressure & Volume Change in a Magma Chamber and Surface Deformation at Active Volcanoes? What factors control the magnitude of surface deformation?
More informationRheology of the Mantle and Plates (part 1): Deformation mechanisms and flow rules of mantle minerals
(part 1): Deformation mechanisms and flow rules of mantle minerals What is rheology? Rheology is the physical property that characterizes deformation behavior of a material (solid, fluid, etc) solid mechanics
More informationLecture 8 Viscoelasticity and Deformation
HW#5 Due 2/13 (Friday) Lab #1 Due 2/18 (Next Wednesday) For Friday Read: pg 130 168 (rest of Chpt. 4) 1 Poisson s Ratio, μ (pg. 115) Ratio of the strain in the direction perpendicular to the applied force
More informationRegional Geodesy. Shimon Wdowinski. MARGINS-RCL Workshop Lithospheric Rupture in the Gulf of California Salton Trough Region. University of Miami
MARGINS-RCL Workshop Lithospheric Rupture in the Gulf of California Salton Trough Region Regional Geodesy Shimon Wdowinski University of Miami Rowena Lohman, Kim Outerbridge, Tom Rockwell, and Gina Schmalze
More informationThe Finite Element Method for Mechonics of Solids with ANSYS Applicotions
The Finite Element Method for Mechonics of Solids with ANSYS Applicotions ELLIS H. DILL 0~~F~~~~"P Boca Raton London New Vork CRC Press is an imprint 01 the Taylor & Francis Group, an Informa business
More informationDefmod, an earthquake simulator that adaptively switches between quasi-static and dynamic states
Defmod, an earthquake simulator that adaptively switches between quasi-static and dynamic states C. Meng (cmeng@mit.edu) B. Hager ERL, MIT May 16, 2016 Reservoir production/injection induced seismicity
More information3D MODELING OF EARTHQUAKE CYCLES OF THE XIANSHUIHE FAULT, SOUTHWESTERN CHINA
3D MODELING OF EARTHQUAKE CYCLES OF THE XIANSHUIHE FAULT, SOUTHWESTERN CHINA Li Xiaofan MEE09177 Supervisor: Bunichiro Shibazaki ABSTRACT We perform 3D modeling of earthquake generation of the Xianshuihe
More informationVariations in Tremor Activity and Implications for Lower Crustal Deformation Along the Central San Andreas Fault
Variations in Tremor Activity and Implications for Lower Crustal Deformation Along the Central San Andreas Fault David R. Shelly USGS, Menlo Park Shelly and Hardebeck, GRL, 2010 Collaborators: Jeanne Hardebeck
More informationFrictional Properties on the San Andreas Fault near Parkfield, California, Inferred from Models of Afterslip following the 2004 Earthquake
Bulletin of the Seismological Society of America, Vol. 96, No. 4B, pp. S321 S338, September 2006, doi: 10.1785/0120050808 Frictional Properties on the San Andreas Fault near Parkfield, California, Inferred
More informationSeismic and flexure constraints on lithospheric rheology and their dynamic implications
Seismic and flexure constraints on lithospheric rheology and their dynamic implications Shijie Zhong Dept. of Physics, University of Colorado Boulder, Colorado, USA Acknowledgement: A. B. Watts Dept. of
More informationHeterogeneous Coulomb stress perturbation during earthquake cycles in a 3D rate-and-state fault model
Click Here for Full Article GEOPHYSICAL RESEARCH LETTERS, VOL. 35, L21306, doi:10.1029/2008gl035614, 2008 Heterogeneous Coulomb stress perturbation during earthquake cycles in a 3D rate-and-state fault
More informationFollow links Class Use and other Permissions. For more information, send to:
COPYRIGHT NOTICE: Stephen L. Campbell & Richard Haberman: Introduction to Differential Equations with Dynamical Systems is published by Princeton University Press and copyrighted, 2008, by Princeton University
More informationTime Dependence of Postseismic Creep Following Two Strike-Slip Earthquakes. Gerasimos Michalitsianos
Time Dependence of Postseismic Creep Following Two Strike-Slip Earthquakes Gerasimos Michalitsianos 9 April 011, GEOL394 Thesis Advisor: Laurent Montési 1 Table of Contents I. Introduction 4 II. Overview
More information