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Unknown seismogenic structures lurking beneath convergent margins introduce substantial uncertainty in seismic hazard assessments. In northwestern Luzon, the Mw 7.0 Abra earthquake on 27 July 2022 highlights the seismic activity along an unmapped blind fault underneath the Cordillera Central. By integrating coseismic displacements constrained by radar satellite imagery and Global Navigation Satellite System, we image oblique coseismic slip at 11–22 km depth with peak slip of ∼1 m beneath the Philippine Fault Zone in northern Luzon. The southward propagation of coseismic slip and aftershocks terminated at a distance of 50 km from the northern end of the 1990 Luzon earthquake rupture, leaving a seismicity gap in between. Coulomb stress changes of reaching 2 bars are imparted at the shallow portions of the Vigan‐Aggao and Abra River faults, where the updated 100‐year seismic potential is increased to Mw 7.0–7.7, given the thick seismogenic layer of ∼30 km in northern Luzon. Plain Language Summary: On 27 July 2022, the Mw 7.0 Abra earthquake hit northwestern Luzon, the Philippines, killing 11 people, damaging more than 30,000 buildings, and causing US$34 million worth of damage. The earthquake occurred on a previously unrecognized deep fault with no observable surface ruptures. In this study, we collected coseismic displacements from Global Navigation Satellite System and Interferometric Synthetic Aperture Radar to investigate the source fault and coseismic slip distribution. Our model shows that the coseismic slip occurred beneath the Philippine Fault Zone in northern Luzon at a depth of 11–22 km. The coseismic slip and aftershocks propagated southward and terminated at a distance of 50 km from the northern tip of the 1990 Luzon coseismic surface rupture. This leaves a seismicity gap between latitudes 16.5°N–17°N along the Philippine Fault Zone. The mainshock‐induced stress perturbation on the nearby active faults, together with the unusually thick seismogenic layer on the northern Philippine Fault Zone, implies a high seismic hazard in Luzon. Successive crustal deformation and seismicity monitoring will provide valuable constraints for the energy budget of earthquakes across northern Luzon, where local communities are threatened by inland crustal earthquakes and megathrust events in the future. Key Points: Global Navigation Satellite System and Sentinel‐1 Aperture Radar reveal the Abra rupture on an oblique blind fault beneath northern LuzonThe coseismic rupture brought the shallow parts (5 km depth) of adjacent faults up to 2 bars closer to failureInferred slip and depth distribution of seismicity reveal the thick seismogenic layer of 30 km on the northern Philippine Fault Zone [ABSTRACT FROM AUTHOR]

We present precise deformation velocity maps for the two year period from September 2011 to July 2013 of the northern Taiwan area, Taipei, by using persistent scatterer interferometry (PSI) technique for processing 18 high resolution X-band synthetic aperture radar (SAR) images archived from COSMO-SkyMed (CSK) constellation. According to the result, the highest subsidence rates are found in Luzou and Wuku area in which the rate is about 15 mm/yr and 10 mm/yr respectively in the whole dataset. However, dramatic change from serve subsidence to uplift in surface deformation was revealed in the Taipei Basin in two different time spans: 2011/09–2012/09 and 2012/09–2013/07. This result shows good agreement with robust continuous GPS measurement and precise leveling survey data across the central Taipei Basin. Moreover, it also represents high correlation with groundwater table. From 8 well data in the Taipei basin, the storativity is roughly constant across most of the aquifer with values between 0.5 × 10 − 4 and 1.6 × 10 − 3 in Jingmei Formation and 0.8 × 10 − 4 and 1.4 × 10 − 3 in Wuku Formation. This high correlation indicated that one meter groundwater level change could induce about 9 and 16 mm surface deformation change in Luzou and Wuku area respectively, which is about eight times faster the long-term tectonic deformation rate in this area. Thus, to access the activity of the Shanchiao Fault, it is important to discriminate tectonic movement from anthropogenic or seasonal effect in the Taipei Basin to better understand the geohazards and mitigation in the Taipei metropolitan area. [ABSTRACT FROM AUTHOR]