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Spacing of faults at the scale of the lithosphere and localization instability: 1. Theory
Author(s) -
Montési Laurent G. J.,
Zuber Maria T.
Publication year - 2003
Publication title -
journal of geophysical research: solid earth
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/2002jb001923
Subject(s) - instability , lithosphere , brittleness , necking , geology , wavelength , shear (geology) , shear zone , geometry , seismology , tectonics , mechanics , physics , optics , materials science , petrology , composite material , mathematics
Large‐scale tectonic structures such as orogens and rifts commonly display regularly spaced faults and/or localized shear zones. To understand how fault sets organize with a characteristic spacing, we present a semianalytical instability analysis of an idealized lithosphere composed of a brittle layer over a ductile half‐space undergoing horizontal shortening or extension. The rheology of the layer is characterized by an effective stress exponent, n e . The layer is pseudoplastic if 1/ n e = 0 and forms localized structures if 1/ n e < 0. Two instabilities grow simultaneously in this model: the “buckling/necking instability” that produces broad undulations of the brittle layer as a whole, and the “localization instability” that produces a spatially periodic pattern of faulting. The latter appears only if the material in the brittle layer weakens in response to a local perturbation of strain rate, as indicated by 1/ n e < 0. Fault spacing scales with the thickness of the brittle layer and depends on the efficiency of localization. Localization is more efficient for more negative 1/ n e , leading to more widely spaced faults. The fault spacing is related to the wavelength at which different deformation modes within the layer enter a resonance that exists only if 1/ n e < 0. Depth‐dependent viscosity and the model density offset the instability wavelengths by an amount a L that we determine empirically. The wave number of the localization instability, is k j L = π( j + a L )(−1/ n e ) −1/2 / H , with H the thickness of the brittle layer, j an integer, and 1/4 < a L < 1/2 if the strength of the layer increases with depth and the strength of the substrate decreases with depth.

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