@article{10272/8204,
year = {2008},
url = {http://hdl.handle.net/10272/8204},
abstract = {We study deformation structures in a serpentinite-bearing normal shear zone in the Ronda peridotites,
southern Spain. The fault zone displays a structural zoning composed by four domains showing similar
strain gradients. Deformation is partitioned into distributed deformation expressed by foliated serpentinites
and S-C structures and localized deformation expressed by R and P shear planes at lower and upper
portions, respectively, of each domain. Such a structural zoning suggests that stable shear creep alternates
with intermittent seismogenic events during the fault activity},
title = {Zonación estructural en una zona de cizalla en serpentinitas (Falla de Peña Parda, peridotitas de Ronda)},
title = {Structural zoning in a serpentinite-bearing shear zone (Peña Parda Fault, Ronda peridotites)},
author = {Esteban, José Julián and Cuevas, Julia and Tubía, José María},
}