Shear stress in fault zones

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There are currently three major competing views on the nature of earthquake fault zones. The first is that faults are (possibly segmented and heterogeneous) Euclidean zones in a continuum solid. The second focuses on granular aspects of faults and deformation fields. The third is that faults are fundamentally rough fractal objects at all relevant scales. The existing data can not distinguish un...

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ژورنال

عنوان ژورنال: Nature

سال: 1982

ISSN: 0028-0836,1476-4687

DOI: 10.1038/296708a0