Dynamic Modeling of the Andean Orogeny Embedded in a 3D Spherical-Shell Model of the Earth's Mantle

• Antragsteller: Professor Dr. Jonas Kley
• Fachliche Zuordnung: Paläontologie
• Förderung: Förderung von 2009 bis 2015
• Projektkennung: Deutsche Forschungsgemeinschaft (DFG) - Projektnummer 105044687

• Erstellungsjahr: 2016

Zusammenfassung der Projektergebnisse

We achieved the most important goals of the first part of our project: We developed a dynamical 3-D spherical-shell model of the thermal and chemical evolution of the Earth’s mantle and obtained the following results. The continental-crust (CC) formation is inseparably tied to thermoconvective mantle evolution. The actual rate of continental growth is NOT uniform through time. Our integrated CC-growth curve is near curves of Belousova et al. (2010) and Dhuime et al. (2012), however it shows episodicity. A cluster of our runs reproduces the observed peaks of ages of detrital zircons. The same runs arrive at the observed present-day surface heat flow and continental mass. The second part served as a numerical preparation of a second 3-D spherical shell model with prescribed plate motions and at a precondition of a regional dynamic model of Andean orogenesis. In this way, the following extensive numerical improvements of the code have been achieved: Enhancement of the code to increase global resolution and maximum number of MPI processes. Further development and integration of the Ruby test framework into the automated BuildBot tests. Implementation of a finite-element inf-sup stabilization using pressure-polynomial projections. Development and implementation of an efficient preconditioner for the variable-viscosity Stokes system. Refinement of the Pressure Correction algorithm, giving more robust convergence. Restructuring of the code to use language features of Fortran95 and Fortran2003 where possible. Integration of automated code documentation using doxygen. Integration of VTK-support and automated visualization. Significant improvements in the formulation of the free-slip boundary condition on the spherical surface.

Projektbezogene Publikationen (Auswahl)

• (2008), Mantle convection and evolution with growing continents, Journal of Geophysical Research, 113, B09,405
  Walzer, U., and R. Hendel
  (Siehe online unter https://doi.org/10.1029/2007JB005459)
• (2009), Andean Orogeny and Plate Generation, in High Performance Computing in Science and Engineering ’08, edited by W. E. Nagel, D. B. Kröner, and M. M. Resch, pp. 559–583, Springer, Berlin
  Walzer, U., R. Hendel, C. Köstler, and J. Kley
  
• (2009), Mantle dynamics - A case study, in Advances in Geocomputing, Lecture Notes in Earth Sciences, vol. 119, edited by H. Xing, pp. 139–181, Springer
  Gottschaldt, K.-D., U. Walzer, D. R. Stegman, J. R. Baumgardner, and H.-B. Mühlhaus
  
• (2009), Predictability of Rayleigh-number and continental-growth evolution of a dynamic model of the Earth’s mantle, in High Performance Computing in Science and Engineering ’07, edited by S. Wagner, M. Steinmetz, A. Bode, and M. Brehm, pp. 585–600, Springer, Berlin
  Walzer, U., and R. Hendel
  
• (2009), Unsteady evolution of the Bolivian Subandean thrust belt: the role of enhanced erosion and clastic wedge progradation, Earth and Planetary Science Letters, 281 (3), 134–146
  Uba, C. E., J. Kley, M. R. Strecker, and A. K. Schmitt
  
• (2010), Towards a dynamical model of the Mars’ evolution, in High Performance Computing in Science and Engineering Stuttgart ’09, edited by W. E. Nagel, D. B. Kröner, and M. M. Resch, pp. 485–510, Springer, Berlin
  Walzer, U., T. Burghardt, R. Hendel, and J. Kley
  
• (2011), A geodynamic model of the evolution of the Earth’s chemical mantle reservoirs, in High Performance Computing in Science and Engineering ’10, edited by W. E. Nagel, D. B. Kröner, and M. M. Resch, pp. 573–592, Springer, Berlin
  Walzer, U., and R. Hendel
  
• (2013), A Forward Model of Mantle Convection with Evolving Continents and a Model of the Andean Subduction Orogen, in High Performance Computing in Science and Engineering ’12, edited by W. E. Nagel, D. H. Kröner, and M. M. Resch, pp. 473–501, Springer, Berlin Heidelberg,
  Walzer, U., R. Hendel, C. Köstler, M. M¨ller, J. Kley, and L. Viereck-Götte
  (Siehe online unter https://doi.org/10.1007/978-3-642-33374-3_35)
• (2013), Geodynamic mantle modeling and its relation to origin and preservation of life, in High Performance of Computing in Science and Engineering. ’13, edited by W. E. Nagel, D. H. Kröner, and M. M. Resch, pp. 591– 617, Springer
  Walzer, U., and R. Hendel
  (Siehe online unter https://doi.org/10.1007/978-3-319-02165-2_42)
• (2013), Real episodic growth of continental crust or artifact of preservation? A 3-D geodynamic model, Journal of Geophysical Research, 118, 2356–2370
  Walzer, U., and R. Hendel
  (Siehe online unter https://doi.org/10.1002/jgrb.50150)