PDF-Orthorhombic anisotropy: A physical model study Scott P. Cheadle, R. J

ABSTRACT An industrial laminate has been shown to possess anisotropy when used as a medium for the propagation of elastic waves The material Phenolic CE is composed of INTRODUCTION Shearwave sp. 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. vs. GZK . …. … heavy composition . vs. anisotropies. Martin Lemoine. Institut d’Astrophysique de Paris. CNRS, Université Pierre & Marie Curie. M. . Lemoine & E. Waxman, . arXiv:0907.1354. nments (outdoor environments and virtual environments). In Experiment 1 it was found that depth extents of up to 7 m are indeed perceptually compressed relative to frontal extents in an outdoor enviro Shear alignment of olivine crystals. Shear wave splitting. c. a. Olivine Anisotropy: Basic (A-type). [1 0 0] (. a. -axis) parallel to flow direction. (0 1 0) plane parallel to flow plane. Horizontal flow . 18 Anisotropy of Magnetic SusceptibilityIn rocks with well developed tectonic fabrics, the principal magnetic susceptibility directions are closely related to orientation of structural features (e.g. of the . Moment Tensor. :. M. ij . = M. ji. Now assume the earthquake is a pure double couple, that means there is . no net volume. change, which means . trace must be 0. .. M11 + M22 + M33 = 0. That means independent elements can be represented by 5 independent parameters: . Katherine McCaffrey. PhD Candidate, Fox-Kemper Research Group. Department of Atmospheric and Oceanic Sciences. Cooperative Institute for Research in Environmental Sciences. 1. Thank you to my advisor and collaborators:. of . the Earth's inner core. Arwen Deuss. Utrecht University. Why the Earth’s core …?. Solidification heat is. engine for mantle . convection. Thermal and chemical. core convection . drives magnetic . Jason Howard, Natalie . Holzwarth. Acknowledgements . Zach Hood. WFU . Deac. HPC Cluster . NSF grant DMR-1507942 . Outline. Motivation. Background of material. Low temperature phase structure search. Fascinating region due to. rich tectonic history and. abundant data from TA . Isotropic Vs. Fast Craton and its Boundary . wrt. . the western US. Fast . Vs. 100-200 km under Great Plains. Slow Ridges (<100 km). . . 602-513-0028 . 11/02/2017 . ACHIEVING A Healthy future . . . for our CHILDREN, OUR SCHOOLS,. . . OUR HEALTH SYSTEM & OUR STATE . A . Win-Win. Agenda. nments outdoor environments and virtual environments In Experiment 1 it was found that depth extents of up to 7 m are indeed perceptually compressed relative to frontal extents in an outdoor environme Katherine McCaffrey. PhD Candidate, Fox-Kemper Research Group. Department of Atmospheric and Oceanic Sciences. Cooperative Institute for Research in Environmental Sciences. 1. Thank you to my advisor and collaborators:. From Mays, 2011, Ground and Surface Water Hydrology. Effective conductivity . that represents aggregate effect of flow through a layered system. Effective conductivity is . different. parallel to than perpendicular to the layers.