FN Archimer Export Format PT J TI Strain localization in the root of detachment faults at a melt‐starved mid‐ocean ridge: a microstructural study of abyssal peridotites from the Southwest Indian Ridge BT AF BICKERT, Manon Cannat, M. Tommasi, A. Jammes, S. Lavier, L. AS 1:1;2:1;3:2;4:3;5:4; FF 1:;2:;3:;4:;5:; C1 Marine Geosciences, Institut de Physique du Globe de Paris UMR 7154 ‐CNRS Université de Paris, France Géosciences Montpellier, CNRS & Université de Montpellier, France Department of GeographyTexas State University San Marcos Texas 78666, USA Department of Geological Sciences, Institute for GeophysicsJackson School of Geosciences, The University of Texas at Austin, United States C2 IPGP, FRANCE UNIV MONTPELLIER, FRANCE UNIV TEXAS, USA UNIV TEXAS AUSTIN, USA IF 4.48 TC 14 UR https://archimer.ifremer.fr/doc/00689/80139/83187.pdf https://archimer.ifremer.fr/doc/00689/80139/83188.pdf https://archimer.ifremer.fr/doc/00689/80139/83189.xlsx https://archimer.ifremer.fr/doc/00689/80139/83190.xls https://archimer.ifremer.fr/doc/00689/80139/83191.xlsx https://archimer.ifremer.fr/doc/00689/80139/83192.xlsx LA English DT Article CR MD 183 / SMOOTHSEAFLOOR BO Marion Dufresne AB Detachment faults that exhume mantle peridotites to the seafloor play a major role in the accommodation of plate divergence at slow‐spreading ridges. Using 99 samples of partially serpentinized peridotites dredged from a nearly amagmatic segment of the eastern part of the Southwest Indian Ridge, we characterize the deformation processes active in the root zone of detachment fault systems. The deformation is heterogeneous even at the sample scale and combines both brittle and crystal‐plastic mechanisms. Strain localization is initially controlled by strength contrasts at the grain scale between olivine and orthopyroxene and between variably oriented olivine crystals. Orthopyroxene deformation is primarily brittle (microfractures), but kink bands and dynamic recrystallization are locally observed. In contrast, olivine deforms primarily by dislocation creep with dynamic recrystallization under high deviatoric stresses (80‐270 MPa). Olivine grains poorly oriented to deform by dislocation glide display kink bands and localized microfractures. Dynamic recrystallization controlled by strain and stress concentrations produce anastomosing zones of grain size reduction (GSR). GSR zones contain limited late to post‐kinematic amphibole, suggesting the presence of small volumes of hydrous fluids. Plagioclase, when present, is post‐kinematic. This heterogeneous high‐stress deformation is observed, with variable intensity, in every sample investigated, suggesting that it was pervasively distributed in the root region of axial detachments. Abyssal peridotite samples from more magmatically robust slow mid‐ocean ridges do not show this pervasive high stress deformation microstructure, implying magma, when present, tends to localize most of the strain at the root of axial detachment systems. PY 2021 PD MAY SO Geochemistry Geophysics Geosystems SN 1525-2027 PU American Geophysical Union (AGU) VL 22 IS 5 UT 000654502900013 DI 10.1029/2020GC009434 ID 80139 ER EF