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Events: Details

2014 CIG Mantle and Lithospheric Dynamics Workshop, Joint with the Canadian Geophysical Union

Presentation Guidelines

Abstracts

Download the complete meeting programme including abstracts [pdf].

List of Posters

By first author and Title

MONDAY, MAY 5: ADVANCING THE STATE OF THE ART IN COMPUTATIONAL MODELING OF MANTLE AND LITHOSPHERE DYNAMICS

Arrial, P-A. University of California, Davis On the sensitivity of 3D thermal convection codes to numerical discretization: A model intercomparison

Butler, S.L

University of Saskatchewan

Mantle Convection Modelling Using Comsol Multiphysics

Huettig, C.

German Aerospace Center (DLR) Berlin,

Proper velocity interpolation for viscosity-carrying particles

May, D. A.

Institute of Geophysics, ETH Zurich

An Efficient Implementation of a Q2 − P1 Finite Element Discretisation and Preconditioner for Variable Viscosity Stokes Problems

Qin, C.

University of Colorado at Boulder

A perturbation method and its application: elastic tidal response of a laterally heterogeneous planet

TUESDAY, MAY 6: NEW INSIGHTS FROM MANTLE CONVECTION MODELING:  EXPLORING MANTLE DYNAMICS FROM THE LITHOSPHERE TO THE BASE OF THE MANTLE

 

Arredondo, K.

University of California, Davis

Dynamic Linkages Between the Transition Zone & Surface Plate Motion in 2D Models of Subduction

Conrad, C.P.

Univ. of Hawaii at Manoa

Dynamic Topography and Sea Level above Stable Antipodal Mantle Upwellings

Heron, P.J.

University of Toronto

Influences on the positioning of mantle plumes following supercontinent formation

Hu, J.

University of Illinois at Urbana Champaign

Investigating Mechanisms of South American Flat Subduction

Li, M.

Arizona State University

Three dimensional morphology and dynamics of ultra-low velocity zones

Liu, X.

University of Colorado, Boulder,

Influence of Chemical Piles on Convective Structure and the Geoid from 3D Spherical Mantle Convection Models

Maguire, R.

University of Michigan, Ann Arbor

Modeling laboratory plumes with numerical techniques: validation, verification and the determination of specific heat


Nakagawa, T.

Japan Agency for Marine- Earth Science and Technology

Deep mantle structures and CMB heat flux derived from surface plate motions

O’Farrell, K.A.

University of Toronto

Thermal structure in large lower mantle viscosity convection models

Plesa, A.

German Aerospace Center (DLR) Berlin

The role of non-Newtonian rheology on the thermal evolution of stagnant-lid bodies

Rosas, J.

University of Alberta, Edmonton

Three-Dimensional Thermal Structure of the Central America Subduction Zone

Trim, S.J.

University of Toronto

Effect of continental lithosphere and deep mantle compositional heterogeneities on the surface mobility of terrestrial planets

Volk, K.E.

University of Michigan, Ann Arbor

Generating 3D Models for the Alaska-Aleutian Subduction System

Weller, M. B.

Rice University

Tectonic Bi-Stability and Internal Heating Scaling in Terrestrial Planets

Zhou, Q.

University of Illinois at Urbana-Champaign

Oceanic asthenosphere subduction and intraplate volcanism

WEDNESDAY, MAY 7: GEODYNAMICS OF LITHOSPHERE EVOLUTION:  NUMERICAL MODELS AND OBSERVATIONAL CONSTRAINTS

 

Adam, C.

Virginia Tech

Seafloor subsidence and mantle dynamics

Ahamed, S.

University of Memphis

Incorporating elastic and plastic work rates into energy balance for long-term tectonic modeling

Currie, C.

University of Alberta

Gravitational removal of magmatic arc roots in Cordilleran orogens

Feng, L.

University of Memphis

Evolution of multiple décollements in a thrust system: A numerical approach

Green, A.M.

University of Utah

Interpretation of EarthScope Magnetotelluric Data for the Northwestern United States

Holt, A.F.

University of Southern California

Mantle flow and overriding plate stress state in 3-D models of thermo-mechanical subduction

Liu, S.

University of Alberta

Farallon Plate subduction dynamics and the Laramide orogeny: Numerical models of flat subduction

Miller, M.S.

University of Southern California

Lithospheric structure of northwest Africa: Insights into the tectonic history and influence of mantle flow on large-scale deformation

Wang, H.

University of Alberta

What Resists Orogenic Shortening: Topography or Mantle Lithosphere?

Wu, G.

University of Texas at Austin

The origin of core complexes in the US Cordillera and the Aegean


Guidelines for Oral Presentations

  • Stay within your allotted time, which includes three (3) minutes for discussion and changeover to the next speaker. 
  • The presentation must cover material from your submitted abstract 
  • Ensure that your ideas are logically organized and your points are clear 
  • Speak slowly and clearly. Word choice should be simple: use active words and short sentences 
  • Speak toward the audience.  
  • Load your presentation before your session begins 
  • Refer to the following style guide for tips on how to prepare your slides:  http://www.projectionnet.com/Styleguide/presentationstyleguide.aspx 

Supported Presentation Formats 

  • PowerPoint 2011 or earlier version 
  • PDF Reader: Adobe Acrobat 
  • Video Playback: Windows Media Player, QuickTime 

Guidelines for Poster Presentations

  • Materials for hanging your poster (push pins or velcro tape) will be provided 
  • Each presenter is provided with a 1.22 m high by 2.44 m wide (4‐foot by 8‐foot) poster board.  Poster boards have a 2.5 cm (1‐inch) frame; ensure that your poster is smaller than 1.22x2.44 m. 
  • The presentation must cover material from your submitted abstract 
  • Place the title of your paper prominently at the top of the poster 
  • Include authors’ names and contact information prominently on your poster 
  • Prepare diagrams or charts so that they are legible at a distance of 2 meters. 
  • Paragraph and figure captions should be at least in a 24‐point font (0.9 cm height) and headers at least in a 36‐point font (1.2 cm height).  
  • Organize the presentation so it is clear, orderly, and self‐explanatory 
  • Group similar ideas and avoid cluttering your poster with too much text. Label different elements as I, II, III; or 1, 2, 3; or A, B, C to make it easier for viewing. 
  • Include the background of your research followed by results and conclusions.  
  • Please do not laminate your poster to ensure that it can be recycled 


Adapted from the AGU guidelines.

See the CGU website for the latest information.

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