@article{fdi:010070835,
  title = {{G}eological record of flat slab-induced extension in the southern {P}eruvian forearc},
  author = {{N}oury, {M}. and {P}hilippon, {M}. and {B}ernet, {M}. and {P}aquette, {J}. {L}. and {S}emp{\'e}r{\'e}, {T}hierry},
  editor = {},
  language = {{ENG}},
  abstract = {{T}he long-lived {A}ndean subduction zone underwent several flat slab episodes and is therefore ideal to study the consequences of a complete cycle of slab flattening and steepening on the upper plate deformation pattern. {I}n the modern {P}eruvian forearc (15 degrees-17 degrees {S}), slab flattening caused a {P}aleogene (52-30 {M}a) landward migration of volcanic activity. {C}ombining structural geology and a source-tosink thermochronological study, we show that the flat slab period is contemporaneous with uplift accommodated by large-scale crustal extension in the forearc. {I}n this light, we argue that the study area is an ancient analog to the modern {M}exican and northern {P}eruvian forearcs located above modern flat slab segments and currently under-going widespread extension.},
  keywords = {{PEROU}},
  booktitle = {},
  journal = {{G}eology},
  volume = {45},
  numero = {8},
  pages = {723--726},
  ISSN = {0091-7613},
  year = {2017},
  DOI = {10.1130/g38990.1},
  URL = {https://www.documentation.ird.fr/hor/fdi:010070835},
}