@article{fdi:010093589,
  title = {{D}etecting millimetric slow slip events along the {N}orth {A}natolian fault with {GNSS}},
  author = {Özdemir, {A}. and {J}ara, {J}. and {D}ogan, {U}. and {J}olivet, {R}. and Çakir, {Z}. and {N}ocquet, {J}ean-{M}athieu and {E}rgintav, {S}. and {B}ilham, {R}.},
  editor = {},
  language = {{ENG}},
  abstract = {{A}ctive faults release part of the elastic strain energy stored in the crust via aseismic slip, either through slow slip events ({SSE}s) or steady slowly creep. {H}owever, spatial and temporal interactions between these different styles of aseismic slip have yet to be quantified especially at depth. {A}long the central section of the {N}orth {A}natolian {F}ault, we apply a {M}ultichannel {S}ingular {S}pectrum {A}nalysis ({MSSA}) on {GNSS} time series of ground motion to detect a {M}w ${{M}}_{w}$ 4.8 +/- $\pm $ 0.08 shallow {SSE} (2-5 km depth) lasting for 26 +/- $\pm $ 5 days, in agreement with local creepmeter observations. {O}ur observations confirm the recurrence of {SSE}s next to a steadily creeping section of the fault. {F}inally, we discuss how steady creep and {SSE}s interact spatially and temporally along the fault segment.},
  keywords = {{GNSS} ; geodesy ; {SSE} ; transient deformation ; {N}orth {A}natolian {F}ault ; creep ; {TURQUIE} ; {ANATOLIE}},
  booktitle = {},
  journal = {{G}eophysical {R}esearch {L}etters},
  volume = {52},
  numero = {10},
  pages = {e2024{GL}111428 [12 p.]},
  ISSN = {0094-8276},
  year = {2025},
  DOI = {10.1029/2024gl111428},
  URL = {https://www.documentation.ird.fr/hor/fdi:010093589},
}