Evidence Hub

Subsurface fault geometries in inland Hokkaido from geometric clustering of dense hypocenter distributions

Mpuang AP, Shiina T, Sawaki Y, Tagami A, Uchide T

2026

Abstract

Abstract The oblique subduction of the Pacific plate beneath Hokkaido, northernmost Japan, drives the collision between the Kuril forearc and the NE Japan arc. This collision has generated some deep and damaging inland crustal earthquakes. However, most of the seismic activity occurs at blind faults with unknown geometries. To understand the orientations and extent of these faults and their implications on the seismotectonics of inland Hokkaido, we analyzed dense crustal seismicity in inland Hokkaido to determine hidden planar fault geometries. First, we applied a deep-learning model to pick seismic P and S phases. The detected phases were associated using PyOcto and located using NonLinLoc tools. The hypocenter locations within the inland crust were relocated using tomoDD and a three-dimensional seismic velocity model. Finally, we reconstructed intricate fault geometries based on hierarchical clustering of the dense hypocenter distributions and their normal vectors. A total of 184 rectangular fault segments were successfully reconstructed in the whole inland Hokkaido region, with dominant depths in the upper crust between 6 km and 12 km. Deep faults below 20 km were found exclusively within the Hidaka collision zone in southern Hokkaido. Our results reveal that the inland Hokkaido region is dominated by high-angle faults with dip angles larger than 60°. In central Hokkaido from north to south, the faults form north-south lineaments consistent with gravity anomalies and…

Read the paper

Related studies

Go deeper in Evidence Hub

Evidence Hub adds a study data sheet (design, sample size, evidence level, key numbers), an AI summary and a chat grounded in the paper's text.

Open this study Sign up free