The effect of energy feedbacks on continental strength

Klaus Regenauer-Lieb, R.F. Weinberg, G. Rosenbaum

    Research output: Contribution to journalArticle

    114 Citations (Scopus)

    Abstract

    The classical strength profile of continents(1,2) is derived from a quasi-static view of their rheological response to stress-one that does not consider dynamic interactions between brittle and ductile layers. Such interactions result in complexities of failure in the brittle-ductile transition and the need to couple energy to understand strain localization. Here we investigate continental deformation by solving the fully coupled energy, momentum and continuum equations. We show that this approach produces unexpected feedback processes, leading to a significantly weaker dynamic strength evolution. In our model, stress localization focused on the brittle-ductile transition leads to the spontaneous development of mid-crustal detachment faults immediately above the strongest crustal layer. We also find that an additional decoupling layer forms between the lower crust and mantle. Our results explain the development of decoupling layers that are observed to accommodate hundreds of kilometres of horizontal motions during continental deformation.
    Original languageEnglish
    Pages (from-to)67-70
    JournalNature
    Volume442
    DOIs
    Publication statusPublished - 2006

    Cite this

    Regenauer-Lieb, K., Weinberg, R. F., & Rosenbaum, G. (2006). The effect of energy feedbacks on continental strength. Nature, 442, 67-70. https://doi.org/10.1038/nature04868