© 2018 Elsevier LtdA stress transfer modeling revealed the stress heterogeneity and its correlation with the seismicity pattern in the bifurcation zone of the Great Sumatran Fault (GSF), where the GSF is divided into two separate sub-parallel segments up to 35 km apart, i.e. Angkola and Barumun, forming a strike-slip duplex at around equator. The analysis was conducted using a seismic catalog compiled from five institutions, i.e. the Indonesian Agency for Meteorology, Climatology, and Geophysics (BMKG), United States Geological Survey USGS), Harvard and Global Centroid Moment Tensor (GCMT), International Seismological Center (ISC), and Geoforschungzentrum (GFZ) Germany, in the period of 1970–2017. Our frequency-magnitude distribution analysis indicates that this zone has a high stress regime. Especially at the tip of the bifurcation zone, in which 20° clockwise rotation of principal stress and 20% increase in stress ratio are observed from the stress inversion. Consequently, events with magnitude larger than 6.0 are concentrated in this area. In addition, our stress transfer modeling reveals the mechanism of the stress heterogeneity at the bifurcation zone and a possible interaction between segment ruptures. Two main internal structures perpendicular to the strike-slip duplex are also observed from the displacement vector. Due to its high stress concentration and its close distance to populous cities of Padang Sidempuan, Bukittinggi, Solok and Padang Panjang in western Sumatra, the tip of GSF bifurcation poses a big potential of seismic hazard. The information of the principal stress rotation and stress ratio obtained in this study can be used further to assess the potential of great ruptures and estimate the possible damage in the study area.

Bifurcation zone,Coulomb stress transfer,Great Sumatran Fault,Seismicity,Stress heterogeneity

Authors thank ITB for supporting this research through the “Riset Unggulan ITB 2017” scheme.

https://doi.org/10.1016/j.jseaes.2018.06.002