@article{PAR00001801,
  title = {{H}ow does the {N}azca {R}idge subduction influence the modern {A}mazonian foreland basin?},
  author = {{E}spurt, {N}icolas and {B}aby, {P}atrice and {B}russet, {S}t{\'e}phane and {R}oddaz, {M}. and {H}ermoza, {W}. and {R}egard, {V}. and {A}ntoine, {P}. {O}. and {S}alas {G}ismondi, {R}. and {B}olanos, {R}.},
  editor = {},
  language = {{ENG}},
  abstract = {{T}he subduction of an aseismic ridge has important consequences on the dynamics of the overriding upper plate. {I}n the central {A}ndes, the {N}azca {R}idge subduction imprint can be tracked on the eastern side of the {A}ndes. {T}he {F}itzcarrald arch is the long-wavelength topography response of the {N}azca {R}idge flat subduction, 750 km inboard of the trench. {T}his uplift is responsible for the atypical three-dimensional shape of the {A}mazonian forelland basin. {T}he {F}itzearrald arch uplift is no older than {P}liocene as constrained by the study of {N}eogene sediments and geomorphic markers, according to the kinematics of the {N}azca {R}idge subduction.},
  keywords = {{N}azca {R}idge ; {A}mazonian foreland basin ; {N}eogene ; flat subduction ; {F}itzcarrald arch},
  booktitle = {},
  journal = {{G}eology},
  volume = {35},
  numero = {6},
  pages = {515--518},
  ISSN = {0091-7613},
  year = {2007},
  DOI = {10.1130/{G}23237{A}.1},
  URL = {https://www.documentation.ird.fr/hor/{PAR}00001801},
}