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 Paul Tackley, Professor of Geophysics and Planetary Physics


Paul Tackley 
Mailing Address:

Department of Earth and Space Sciences
University of California, Los Angeles
595 Charles Young Drive East,
Box 951567
Los Angeles, CA 90095-1567

Office:Geology 3711
Telephone:(310) 206-9180
Fax:(310) 825-2779
E-mail:ptackley@ess.ucla.edu
Web Site:http://artemis.ess.ucla.edu/~pjt/Welcome.html
Quick Links

 Courses Taught

 

ESS 9
ESS 134
ESS 136
ESS 200A
ESS 202
ESS 286C
ESS 287

 Current Research Interest

 

I am interested in the structure, dynamics and evolution of Earth and other terrestrial bodies, particularly as related to convective processes in the mantle, and lithospheric dynamics. My approach emphasizes numerical simulation, using state-of-the-art numerical methods and high performance (massively-parallel + Beowulf) supercomputers to obtain more realistic, three-dimensional numerical models of dynamical processes than previously possible. Specific recent or ongoing projects include:

  1. Developing integrated, self-consistent models of plate tectonics and mantle convection- a long-standing problem in geodynamics. Temperature-dependent viscosity by itself leads to a rigid, immobile lithosphere ('single-plate planet')- additional rheological complexities are necessary to allow plates to form. I have developed some of the first 3-D models in which plates form in such a manner.
  2. Thermo-chemical convection, including the possibility of deep chemical layering, and the thermo-chemical evolution of Earth and other terrestrial planets. The melting associated with plate tectonics causes mantle differentiation, whereas convection causes mantle mixing, and the complex interaction between these two opposing processes is what determines the planet's evolution.
  3. Asthenospheric dynamics and the Yellowstone hotspot. Partial melting in the asthenosphere results in buoyancy sources that can drive flow and cause further melting. This could be an explanation explanation to deep mantle plumes for certain hotspots and other volcanism on Earth. Even if the heat source is a deep plume, these compositional effects will strongly modulate what happens in the melting region.
  4. Plume dynamics and plume-lithosphere interaction. Previous mantle plume models usually assume rather small viscosity contrasts and linear rheology, and are often 2-D (axisymmetric). When you allow more realistic rheology and three-dimensionality, things can be quite different, as we have been discovering!
  5. Continental collisional dynamics. A planned effort is to model the India:Asia collision.

 Education

 

B.A., 1987, Cambridge University, England
M.S., 1991, California Institute of Technology
Ph.D., 1994, California Institute of Technology

 Selected Publications

 Tackley, P.J., D.J. Stevenson, G.A. Glatzmaier, and G. Schubert, Effects of an endothermic phase-transition at 670 km depth in a spherical model of convection in the earth's mantle, Nature, 361 (6414), 699-704, 1993.
 Tackley, P.J., and D.J. Stevenson, A mechanism for spontaneous self-perpetuating volcanism on the terrestrial planets, in Flow and Creep in the Solar System: Observations, Modeling and Theory, edited by D.B. Stone and S.K. Runcorn, pp. 307-322, Kluwer, 1993.
 Tackley, P.J., Effects of strongly variable viscosity on three-dimensional compressible convection in planetary mantles, Journal of Geophysical Research., 101, 3311-3332, 1996.
 Tackley, P.J., On the ability of phase transitions and viscosity layering to induce long-wavelength heterogeneity in the mantle, Geophysical Research Lett., 23, 1985-1988, 1996.
 Tackley, P.J., Three-dimensional simulations of mantle convection with a thermochemical CMB boundary layer: D"?, in The Core-Mantle Boundary Region, edited by Gurnis.et. al., pp. 231-253, American Geophysical Union, 1998c.
 Tackley, P.J., Mantle convection and plate tectonics: Towards an integrated physical and chemical theory, Science, 288, 2002-2007, 2000
 Tackley, P.J., Self-consistent generation of tectonic plates in time-dependent, three-dimensional mantle convection simulations, part 1: Pseudoplastic yielding, Geochemistry, Geophysics, Geosystems, Volume 1, 2000.
 Tackley, P.J., Self-consistent generation of tectonic plates in time-dependent, three-dimensional mantle convection simulations, part 2: Strain weakening and asthenosphere, Geochemistry, Geophysics, Geosystems, Volume 1, 2000.
 Tackley, P.J., G. Schubert, G.A. Glatzmaier, P. Schenk, J.T. Ratcliffe and J.-P. Matas, Three-dimensional spherical simulations of mantle convection in Io, Icarus, in press, 2000.
 Full publication list at: http://artemis.ess.ucla.edu/~pjt/bibliography.html
 

 Graduate Students

 Shunxing Xie
sxie@ess.ucla.edu
http://www2.ess.ucla.edu/~sxie/sxie.html
 John Hernlund
hernlund@ess.ucla.edu

 
595 Charles Young Drive East • 3806 Geology Building • Box 951567 • Los Angeles • CA 90095-1567  
© 2000-08 Department of Earth and Space Sciences