@article{fdi:010057250,
  title = {{T}riggering of tremors and slow slip event in {G}uerrero, {M}exico, by the 2010 {M}w 8.8 {M}aule, {C}hile, earthquake},
  author = {{Z}igone, {D}. and {R}ivet, {D}. and {R}adiguet, {M}. and {C}ampillo, {M}. and {V}oisin, {C}hristophe and {C}otte, {N}. and {W}alpersdorf, {A}. and {S}hapiro, {N}. {M}. and {C}ougoulat, {G}. and {R}oux, {P}. and {K}ostoglodov, {V}. and {H}usker, {A}. and {P}ayero, {J}. {S}.},
  editor = {},
  language = {{ENG}},
  abstract = {{W}e investigate the triggering of seismic tremor and slow slip event in {G}uerrero ({M}exico) by the {F}ebruary 27, 2010 {M}aule earthquake ({M}w 8.8). {T}riggered tremors start with the arrival of {S} wave generated by the {M}aule earthquake, and keep occurring during the passing of {S}c{S}, {SS}, {L}ove and {R}ayleigh waves. {T}he {R}ayleigh wave dispersion curve footprints the high frequency energy envelope of the triggered tremor, indicating a strong modulation of the source of tremors by the passing surface wave. {T}his correlation and modulation by the passing waves is progressively lost with time over a few hours. {T}he tremor activity continues during the weeks/months after the earthquake. {GPS} time series suggest that the second sub-event of the 2009-2010 {SSE} in {G}uerrero is actually triggered by the {M}aule earthquake. {T}he southward displacement of the {GPS} stations starts coincidently with the earthquake and tremors. {T}he long duration of tremors indicate a continuing deformation process at depth, which we propose to be the second sub-event of the 2009-2010 {SSE}. {W}e show a quasi-systematic correlation between surface displacement rate measured by {GPS} and tremor activity, suggesting that the {NVT} are controlled by the variations in the slip history of the {SSE}. {T}his study shows that two types of tremors emerge: (1) {T}hose directly triggered by the passing waves and (2) those triggered by the stress variations associated with slow slip. {T}his indicates the prominent role of aseismic creep in the {M}exican subduction zone response to a large teleseismic earthquake, possibly leading to large-scale stress redistribution.},
  keywords = {},
  booktitle = {},
  journal = {{J}ournal of {G}eophysical {R}esearch.{S}olid {E}arth},
  volume = {117},
  numero = {},
  pages = {{B}09304},
  ISSN = {0148-0227},
  year = {2012},
  DOI = {10.1029/2012jb009160},
  URL = {https://www.documentation.ird.fr/hor/fdi:010057250},
}