@article{fdi:010053706, title = {{A}ctive deformation along the southern end of the {T}osco-{A}breojos fault system : new insights from multibeam swath bathymetry}, author = {{M}ichaud, {F}ran{\c{c}}ois and {C}almus, {T}. and {R}atzov, {G}. and {R}oyer, {J}. {Y}. and {S}osson, {M}. and {B}igot-{C}ormier, {F}. and {B}andy, {W}. and {G}utierrez, {C}. {M}.}, editor = {}, language = {{ENG}}, abstract = {{T}he relative motion of the {P}acific plate with respect to the {N}orth {A}merica plate is partitioned between transcurrent faults located along the western margin of {B}aja {C}alifornia and transform faults and spreading ridges in the {G}ulf of {C}alifornia. {H}owever, the amount of right lateral offset along the {B}aja {C}alifornia western margin is still debated. {W}e revisited multibeam swath bathymetry data along the southern end of the {T}osco-{A}breojos fault system. {I}n this area the depths are less than 1,000 m and allow a finer gridding at 60 m cell spacing. {T}his improved resolution unveils several transcurrent right lateral faults offsetting the seafloor and canyons, which can be used as markers to quantify local offsets. {T}he seafloor of the southern end of the {T}osco-{A}breojos fault system (south of 24{A} degrees {N}) displays {NW}-{SE} elongated bathymetric highs and lows, suggesting a transtensional tectonic regime associated with the formation of pull-apart basins. {I}n such an active tectonic context, submarine canyon networks are unstable. {U}sing the deformation rate inferred from kinematic predictions and pull-apart geometry, we suggest a minimum age for the reorganization of the canyon network.}, keywords = {{T}osco-{A}breojos fault ; seafloor morphology ; submarine canyon ; plate ; boundary ; {B}aja {C}alifornia peninsula ; {M}exico}, booktitle = {}, journal = {{P}ure and {A}pplied {G}eophysics}, volume = {168}, numero = {8-9}, pages = {1363--1372}, ISSN = {0033-4553}, year = {2011}, DOI = {10.1007/s00024-010-0193-y}, URL = {https://www.documentation.ird.fr/hor/fdi:010053706}, }