PPT-Shear-wave splitting measurements for Asia

Meeting slides for Nov 1 2012 Pay attention to N measurements Only give N to ones with very clear XKS signal on the original R first seismogram on the first window and second window when doing 4c but definitely no XKS energy on the original T second seismogram on the windows . Seismology- lecture 5. Barbara Romanowicz, UC Berkeley. CIDER2012, KITP. Seismological tools. Seismic tomography: surface waves, overtones. Volumetric distribution of heterogeneity. “smooth” structure – depth resolution ~50 km. Seismic velocities – P & S. Relationship to elastic moduli. Seismic anisotropy. . -- directional variation in seismic velocity. Seismic Attenuation – 1/. Q. p. & 1/Q. s. . -- What is seismic attenuation?. Base Isolators. These pads separate, or isolate, a building from it’s foundation and prevent some of an earthquake’s energy from entering the building.. Base Isolators. Japan testing base isolators . Ward et al. 2013. From ANT dispersion to . shear-wave velocity models. Ward et al. 2013. From ANT dispersion to . shear-wave velocity models. From ANT dispersion to . shear-wave velocity models. Minimize the misfit between observed and predicted dispersion data. Shear velocity of olivine. Data from . Kumazawa. & Anderson. [1969]. Seismic Anisotropy . Anisotropy of . Polycrystaline. Rocks. Twin Sisters . Dunite. Babuska. , 1972. Deformation and fabric in mantle rocks. Viscosity is a quantitative measure of a fluid’s resistance to flow.. Dynamic (or Absolute) Viscosity. :. The dynamic viscosity(. η. ) of a fluid is a measure of the resistance it offers to relative shearing motion.. N. Dyaur, R. Stewart, and L. Huang. Houston. May 16, 2013. 1. Introduction & motivation. Why physical modeling?. AGL physical modeling system. Scaled models of resource interest. laser-etched glass. April 28, 2011. Taeseo. Ku. Civil & Environmental Engineering. EAS 4480. Introduction. 1. Shear wave velocity (V. s. ). Second fastest wave & Directional and . polarized. Most fundamental wave to geotechnical engineering. x b2030152025301234z mmc203015202530x mmz mma15202530Fig 3 Shear wave speed maps of the breast inclusion phantom using a U-CUSE b F-CUSE and c M-CUSE All shear wave speed maps used the same color scal Wave Ratios and MeasurementsLength of Wave 2Length of Wave 3Length of Wave 4Length of Wave 1Length of Wave 5eSignal Part 2 Applying Technical Analy 7. Waves in a cubic . crystal. HW for next Tuesday: Chapter 3 10,13; Chapter 4 1,3,5. Stress – Cubic Crystal. Find Young’s modulus (Y = X. x. /. e. xx. ) and . Poission’s. . ratio: ( . d. w. /w)/(. Cha . Young-. cheol. Korean Consul General. Contents. ∆ Brief Introduction on Korea . ∆ Korean Wave. . - current status. . - reasons of popularity. . - future . ∆ Turkish Wave?. * remarks. Seismology- lecture 5. Barbara Romanowicz, UC Berkeley. CIDER2012, KITP. Seismological tools. Seismic tomography: surface waves, overtones. Volumetric distribution of heterogeneity. “smooth” structure – depth resolution ~50 km. Introduction:. The . present tectonics of Iran has resulted from the continental convergence of the Arabian and Eurasian plates. Our study . area (Fig.1). ,. comprises . a part of this collision zone and consists of an assemblage of distinct lithospheric .