PDF-CWP Numerical modeling of waves incident on slip discontinuities Matthew Haney and Roel
Author : yoshiko-marsland | Published Date : 2015-01-19
For instance fractures allow a small amount of slip to occur along their surfaces during the passage of a seismic wave By slip we mean that the displacement across
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CWP Numerical modeling of waves incident on slip discontinuities Matthew Haney and Roel: Transcript
For instance fractures allow a small amount of slip to occur along their surfaces during the passage of a seismic wave By slip we mean that the displacement across the interface can be discontinuous Re64258ection and transmission of plane waves in t. rarefactions and contact discontinuities Contact discontinuities are surfaces that separate zones of different density and tem perature By definition such a surface is in pressure equilibrium and no gas flows across it When as often happens the tang Strike slip systems are relatively narrow and subvertical wrench zones along which two adjacent blocks move sideways horizontally parallel to the strike of the fault zone For example they are produced at transform plate boundaries where plates hori SimpleandRapidLaboratoryMethodforRewettingDrySoilforIncubationsR.L.HANEYANDE.B.HANEY Downloaded By: [Haney, R. L.] At: 13:03 28 June 2010 1494R.L.HaneyandE.B.HaneyWFPSwasusedasanacceptablemethodtodete Section 9.2. Key Terms. Media Boundary. Free-end Reflection. Fixed-end Reflection. Transmission. Standing Wave. Node. Antinode. Fundamental Frequency/First Harmonic. Harmonics. Overtone. Media Boundaries. 220M.Haney,R.Snieder,J.Sheiman&S.LoshBA1985CD1.22.3highlowNorthNorth600 mNorthH-sandB-faultA-faultH-sandtwo-way time (s)relativereflectivity19851992A10ST600 m600 m1 km0.5 s1992Figure1.(A)Mapofthetwo-w Strategic Plan 2014-2024. December 12, 2013. Definitions for Plan Development. . Guiding Principles:. Core, underlying attributes set by institutional history and a broad campus understanding of who we are and who we want to be.. Before the waves are made the particles are same distance apart. While waves moves through the medium the particles . compress. together, then they spread further apart (stretched areas)- . rarefaction.. A wave is any disturbance that transmits energy through matter or empty space.. Energy can be carried away from it’s source by a wave. As a wave travels, it does work on everything in it’s path. Wave. Repeating disturbance or movement. Carries energy through matter and space. Vibrations. Anything that moves in a rhythmic patter. Up and down. Back and forth. What is a Wave. All waves are produced when something vibrates. 2022-2023 Season. Russ Burleson. geaux15@hotmail.com. . 1. Agenda. Binder Check/Homework review. Mechanical Wave overview. Transverse Waves. Surface Waves. Longitudinal Waves (general). Sound Waves (Longitudinal). Get 1 full page and 1 half page of paper. Fold full sheet of paper. about 1-1.5” short of even. Insert half sheet in the middle. Staple . across . the fold. Pick up the top two pages and starting from the bottom, cut the top two . Thomas Lund. NorthWest. Research Associates. Boulder, CO. Boulder Fluids Seminar. 14 October, 2014. Outline. Introduction. What are gravity waves?. How are they similar/dissimilar to surface waves?. Energy is moving, not water. orbital motion. energy is transferred via circular motions. water (and gull) return to original position. the wave form moves forward. Motion decreases with depth. At. a depth of ½ of the wavelength, the motion is not significant.. Earthquakes-Tsunamis. Graviational. attraction-Tides. Wind waves move energy, not matter. Wind waves- Growth. Wind strength- must be moving faster than waves. Wind duration-longer creates larger waves.
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