RT Journal Article
T1 Zonación estructural en una zona de cizalla en serpentinitas (Falla de Peña Parda, peridotitas de Ronda)
T1 Structural zoning in a serpentinite-bearing shear zone (Peña Parda Fault, Ronda peridotites)
A1 Esteban, José Julián
A1 Cuevas, Julia
A1 Tubía, José María
AB 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 similarstrain gradients. Deformation is partitioned into distributed deformation expressed by foliated serpentinitesand S-C structures and localized deformation expressed by R and P shear planes at lower and upperportions, respectively, of each domain. Such a structural zoning suggests that stable shear creep alternateswith intermittent seismogenic events during the fault activity
YR 2008
FD 2008
LK http://hdl.handle.net/10272/8204
UL http://hdl.handle.net/10272/8204
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 29 may 2026