Fig. 4. The complete Bouguer anomaly map of the study area. Higher gravity anomalies are observed in the west region of the Dongducheon fault (DF), while lower gravity anomalies are observed on the east side. Microseismicities are concentrated mainly in the low gravity region between high gravity anomalies (HG1 and HG2).

Econ. Environ. Geol. 2022;55:633-48 https://doi.org/10.9719/EEG.2022.55.6.633

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