PPT-Azimuthal anisotropy layering in the Pacific upper mantle

Huaiyu Yuan 123 Scott French 4 and Barbara A Romanowicz 456 1 CCFS EPS Macquarie University Australia 2 CET University of Western Australia Australia. Layering is a simple andinexpensive propagationmethod. It produces aclone, or an exactduplicate, of the motherplant.Air Layering...the quick and easy propagation method Layering involves the formatio Transition Zone Discontinuities beneath the Contiguous United . States. Stephen . S. . Gao and Kelly . H. Liu. sgao@mst.edu. ; . http://www.mst.edu/~sgao. . Missouri . University of Science and . Technology . 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. Takafumi. . Niida. for the PHENIX Collaboration. University of Tsukuba. “Heavy Ion collisions in the LHC era” . in . Quy. . Nhon. outline. 2. Introduction of . v. n. H. igher harmonic flow (. v. . charged . pions. . W. ith respect to 3. rd. event plane . In . Au+Au. 200GeV collisions . a. t RHIC-PHENIX. Takafumi. . Niida. for the PHENIX Collaboration. JPS meeting, Mar. 2012 . outline. Introduction. 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 . The fundamental abstraction . used to . collect protocols into a unified whole . is known as a . layering model. All aspects of a communication problem can be partitioned . into pieces that work together. 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 . 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 . 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. Layering Sarah Skubel & Maria Stutzman Layering A system of vegetative clonal propagation where stems are stimulated to form adventitious roots while still attached to the parent plant How Does it Work? 78Teacher Page Preparation In ClassWrap-upExtensions Lava Layering 79 Procedurebaking soda vinegar.food coloring;playdough Key Words Materialsbaking sodameasuring cupPurpose Lava Layering 80 Res 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 .