Half graben inversion tectonics revealed by gravity modeling in the Mikawa Bay Region, Central Japan Ayumu Miyakawa (
[email protected] ) US Geological Survey of Japan, AIST https://orcid.org/0000-0001-8089-6406 Tomoya Abe Geological Survey of Japan, AIST Tatsuya Sumita Geological Survey of Japan, AIST Makoto Otsubo Geological Survey of Japan, AIST Research article Keywords: Gravity survey, Inversion tectonics, Mikawa Bay Region, Nishi-Mikawa Plain, Chita Peninsula, Utsumi Fault, Takahama Fault, Basement structure, Half graben, Central Japan Posted Date: May 22nd, 2020 DOI: https://doi.org/10.21203/rs.3.rs-29592/v1 License: This work is licensed under a Creative Commons Attribution 4.0 International License. Read Full License Version of Record: A version of this preprint was published on October 20th, 2020. See the published version at https://doi.org/10.1186/s40645-020-00376-6. 1 Half graben inversion tectonics revealed by gravity modeling in the Mikawa Bay 2 Region, Central Japan 3 Ayumu Miyakawa 1 4 Corresponding author 5 Email:
[email protected] 6 7 Tomoya Abe 1 8 Email:
[email protected] 9 10 Tatsuya Sumita 1 11 Email:
[email protected] 12 13 Makoto Otsubo 1 14 Email:
[email protected] 15 16 (Institutional addresses) 17 1 Geological Survey of Japan, AIST, AIST Tsukuba Central 7, 1-1-1 Higashi, Tsukuba, Ibaraki 18 Pref., 305-8567, Japan 19 20 21 Abstract 22 The Mikawa Bay Region, central Japan, is characterized by many active faults recording 23 Quaternary activity. It is, however, difficult to understand the overall tectonic character of the 24 region due to the thick sediments in this region.