Seismological Characterization of Northern Hikurangi Margin Slow Slip Regions Associated With Normal Faults, Seamounts, and Seeps

At the northern Hikurangi margin, Aotearoa New Zealand, slow slip events (SSEs) recur every 6–24 months to ∼ ${\sim} $ 30 km depth. Although shallow SSEs (0–10 km) are well‐studied offshore, the deeper portion (10–30 km) remains poorly understood, limiting insight into SSE initiation. Here we investigate this deeper region and examine relationships between newly resolved SSEs and seismicity. Using time‐dependent inversions, we resolve two small SSEs ( MW ${M}_{W}$ 6.2 and 6.4), including one that extends from 15 to 30 km depth. Using data from a dense onshore seismograph network deployed directly above this deeper portion from December 2017 to October 2018, we construct a catalog of 3,071 high‐quality earthquakes with hypocentral uncertainties ≤ ${\le} $ 5 km, located using a 3‐D velocity model and a new 1‐D model. Earthquake magnitudes range from −0.84 to 4.40, with a completeness magnitude of 1.7 and a b‐value of 1.06. Focal mechanisms reveal numerous normal‐faulting earthquakes, including some within the slab mantle. Vertically‐aligned seismicity and normal‐faulting earthquakes outline pathways linking the slab mantle to surface seeps of mantle‐derived fluids. We infer that normal faults form due to slab bending and localized uplift of subducting seamounts, which roughen the plate interface, damage the upper plate, and promote fluid migration. Landward of ∼ ${\sim} $ 100 km from the trench, both surface seeps and normal‐faulting mechanisms cease, coinciding with the downdip limit of shallow SSEs. Together, these results suggest that the Hikurangi margin's rough subducting plate interface exerts strong control on forearc dewatering and SSE genesis.