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James Hickey, Joachim Gottsmann and Rodrigo del Potro The large-scale surface uplift in the Altiplano-Puna region of Bolivia: A parametric study of source characteristics and crustal rheology using finite element analysis Geochemistry, Geophysics, Geosystems 14

Article first published online: 11 MAR 2013 | DOI: 10.1002/ggge.20057

Key Points

  • Pressurization of magma body extending from APMB causing surface uplift
  • Pressure-time function can explain temporal deformation pattern
  • Source-depth soft layer can buffer subsurface deformation

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