کد مقاله کد نشریه سال انتشار مقاله انگلیسی نسخه تمام متن
4741769 1641533 2012 29 صفحه PDF دانلود رایگان
عنوان انگلیسی مقاله ISI
Mechanisms for the generation of plate tectonics by two-phase grain-damage and pinning
موضوعات مرتبط
مهندسی و علوم پایه علوم زمین و سیارات فیزیک زمین (ژئو فیزیک)
پیش نمایش صفحه اول مقاله
Mechanisms for the generation of plate tectonics by two-phase grain-damage and pinning
چکیده انگلیسی

Weakening and shear localization in the lithosphere are essential ingredients for understanding how and whether plate tectonics is generated from mantle convection on terrestrial planets. We present a new theoretical model for the mechanism of lithospheric weakening and shear-localization and hence plate generation through damage, grain evolution and Zener pinning in two-phase (polycrystalline) lithospheric rocks. Grain size evolves through the competition of coarsening, which drives grain growth, with damage, which drives grain reduction. However, in a two-phase medium the interface between phases induces Zener pinning, which impedes grain growth and facilitates damage. The size of the pinning surfaces is given by the roughness of the interface, and damage to the interface causes smaller pinning surfaces, which in turn drive down the grain-size, forcing the rheology into the grain-size-dependent diffusion creep regime. This process allows damage and rheological weakening to co-exist, which is normally considered impossible in single phase assemblages. Moreover pinning greatly inhibits grain-growth and shear-zone healing, which is much faster in single phase materials. Hence, the resulting shear-localization is rapid (less than 1 Myr), but the healing time for a dormant weak zone is very slow (greater than 100 Myrs); these effects therefore permit rapidly forming and long-lived plate boundaries. The model therefore provides a key ingredient and predictive theory for the generation of plate tectonics on Earth and other planets.


► Grain-damage and Zener pinning can combine to allow lithospheric localization.
► Damage to pinning bodies shrinks grains, forcing the rheology into diffusion creep.
► Damage and weakening thus co-exist to allow for a rapid localization feedback.
► Pinning also slows healing of weak zones with recovery much longer than 100 Myrs.
► The mechanism therefore permits rapidly forming and long-lived plate boundaries.

ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Physics of the Earth and Planetary Interiors - Volumes 202–203, August 2012, Pages 27–55
نویسندگان
, ,