PPT-1 27- 750 Texture , Microstructure & Anisotropy

AD Tony Rollett S R Wilson Rodrigues vectors unit Quaternions Last revised 2 nd Jan 2015 Briefly describe rotationsorientations Introduce RodriguesFrank vectors Introduce . Iron–carbon Alloys. Introduction. Several of the various microstructures that may be produced in steel alloys and their relationships to the iron–iron carbon phase diagram are now discussed, and it is shown that the microstructure that develops depends on both the carbon content and heat treatment.. 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 . Pankaj Jain . I.I.T. Kanpur. Introduction. Universe is assumed to be homogeneous and isotropic at large distance scales. No preferred position or direction . . A.D. . Rollett. Vectors, Matrices, . Rotations. , . Axis Transformations. Most of the material in these slides originated in lecture notes by Prof. Brent Adams (. now emeritus . at BYU). . Last revised: 9 Nov. ‘11. 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 . Kishalay De (Caltech / . I. ISc. ). Yashwant. Gupta (NCRA-TIFR. ), . Prateek. Sharma (. IISc. ). Science at Low Frequencies 2016. Microstructure emission. Cordes. et al. 1990. Milli. -period timescale (often quasi-periodic) intensity fluctuation in sub-pulse emission.. Texture and its Effect on Anisotropic Properties. Tony (A.D.) Rollett, Carnegie Mellon Univ. .. Last revised. : . 12. th. . Jan. 2014. 2. Microstructure-Properties Relationships. Microstructure. Properties. Fast axis direction with respect to NA APM. Layered upper mantle. Continuous lines: % Fo (Mg) from. Griffin et al. 2004. Grey: Fo%93. black: Fo%92. LAB and MLD in the craton. Laying shown in both fast axis directions . Huaiyu . Yuan. 1,2,3. . , Scott . French. 4. and. . Barbara A. . Romanowicz. 4,5,6. 1. . CCFS, EPS, Macquarie . University, . Australia. 2. . CET, University . of Western Australia, . Australia. 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). 1 . , P.Krkotic. 2. , J. O’Callaghan. 3. , F. Perez. 2. , M. Pont. 2. , X. Granados. 1 . , S. Calatroni. 4. , M. Taborelli. 4 . and T. Puig. 1. 1 . Institut. de . Ciència. de Materials de Barcelona, CSIC, . 2 nd LEM3 - Labex DAMAS Metz, October 13 - 15, 2015 Understanding microstructure formation F rank Mue cklich * , ** (m uecke@matsci.uni - sb.de ) * Saarland University , Chair Functional Materials 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.