TY  - JOUR
A1  - Astudillo-Sotomayor, Luis
A1  - Jara Muñoz, Julius
A1  - Melnick, Daniel
A1  - Cortés‐Aranda, Joaquín
A1  - Tassara, Andrés
A1  - Strecker, Manfred
T1  - Fast Holocene slip and localized strain along the Liquiñe-Ofqui strike-slip fault system, Chile
T2  - Scientific reports
N2  - In active tectonic settings dominated by strike-slip kinematics, slip partitioning across subparallel faults is a common feature; therefore, assessing the degree of partitioning and strain localization is paramount for seismic hazard assessments. Here, we estimate a slip rate of 18.8 +/- 2.0 mm/year over the past 9.0 +/- 0.1 ka for a single strand of the Liquirie-Ofqui Fault System, which straddles the Main Cordillera in Southern Chile. This Holocene rate accounts for similar to 82% of the trench-parallel component of oblique plate convergence and is similar to million-year estimates integrated over the entire fault system. Our results imply that strain localizes on a single fault at millennial time scale but over longer time scales strain localization is not sustained. The fast millennial slip rate in the absence of historical Mw> 6.5 earthquakes along the Liquine-Ofqui Fault System implies either a component of aseismic slip or Mw similar to 7 earthquakes involving multi-trace ruptures and > 150-year repeat times. Our results have implications for the understanding of strike-slip fault system dynamics within volcanic arcs and seismic hazard assessments.
KW  - Geodynamics
KW  - Geomorphology
KW  - Tectonics
Y1  - 2021
UR  - https://publishup.uni-potsdam.de/frontdoor/index/index/docId/64127
SN  - 2045-2322
VL  - 11
IS  - 1
PB  - Macmillan Publishers Limited, part of Springer Nature
CY  - London
ER  -