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Extreme mantle uplift and exhumation along a transpressive transform fault

2016; Nature Portfolio; Volume: 9; Issue: 8 Linguagem: Inglês

10.1038/ngeo2759

1752-0908

Marcia Maïa, Susanna Eleonora Sichel, A. Briais, Daniele Brunelli, Marco Ligi, N.P. Ferreira, Thomas Ferreira da Costa Campos, Bérengère Mougel, Isa Brehme, Christophe Hémond, Akihisa Motoki, Denise Silva de Moura, Carla Scalabrin, Ivo B. M. Pessanha, Eliane Alves, Arthur Ayres, Pedro Oliveira,

High-pressure geophysics and materials

Earth’s crust diverges and extends along mid-ocean ridges. Analyses of gravity and seismic data from the equatorial Atlantic show that propagation of ridge segments can compress the crust and create sufficient uplift to create small islands. Mantle exhumation at slow-spreading ridges is favoured by extensional tectonics through low-angle detachment faults1,2,3,4, and, along transforms, by transtension due to changes in ridge/transform geometry5,6. Less common, exhumation by compressive stresses has been proposed for the large-offset transforms of the equatorial Atlantic7,8. Here we show, using high-resolution bathymetry, seismic and gravity data, that the northern transform fault of the St Paul system has been controlled by compressive deformation since ∼10 million years ago. The long-lived transpression resulted from ridge overlap due to the propagation of the northern Mid-Atlantic Ridge segment into the transform domain, which induced the migration and segmentation of the transform fault creating restraining stepovers. An anticlockwise change in plate motion at ∼11 million years ago5 initially favoured extension in the left-stepping transform, triggering the formation of a transverse ridge, later uplifted through transpression, forming the St Peter and St Paul islets. Enhanced melt supply at the ridge axis due to the nearby Sierra Leone thermo chemical anomaly9 is responsible for the robust response of the northern Mid-Atlantic Ridge segment to the kinematic change. The long-lived process at the origin of the compressive stresses is directly linked to the nature of the underlying mantle and not to a change in the far-field stress regime.