Fig. 7. Comparison of our fault system model with the classical model of the strike-slip duplex structure model. (A) Distribution of microseismicities and anticipated fault lines. (B) A classical tectonic model of the strike-slip duplex structure (Twiss and Moores, 1992). (C) Application of the classical model to our study area. It is observed that the microseismicities are distributed along the fault lines inferred by gravity analysis. Distribution of microsesmicities and consistency with the classical strike-slip duplex model support that our model of En echelon lines and strike-slip duplex structure across and along the Dongducheon Fault (DF) are reliable.

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

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