Acknowledgement
This work was supported by the Korea Institute of Energy Technology Evaluation and Planning (KETEP) and the Ministry of Trade, Industry & Energy (MOTIE) of the Republic of Korea (No. 20212010200020). This research was also supported by the Basic Research Project grants (GP2020-003; Geological survey in the Korean Peninsula and publication of the geological maps) from the Korea Institute of Geoscience and Mineral Resources (KIGAM) funded by the Ministry of Science, Information, Communication and Technology (ICT), and Future Planning, Korea. We appreciate two anonymous reviewers for their constructive comments, which improved the manuscript.
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