Correlation between a Tephra Bed from Deep (2038 m) Underground below Chiba City, and Kd48 in the Lowermost Kiwada Formation (Lower Pleistocene) on the Boso Peninsula

Author:

UTSUNOMIYA Masayuki1ORCID,MIZUNO Kiyohide1,NAYA Tomonori1ORCID,OMURA Kentaro2,NAGAI Masashi3

Affiliation:

1. Research Institute of Geology and Geoinformation, Geological Survey of Japan, AIST

2. Earthquake and Tsunami Research Division, National Research Institute for Earth Science and Disaster Resilience

3. Volcano Disaster Resilience Research Division, National Research Institute for Earth Science and Disaster Resilience

Publisher

Tokyo Geographical Society

Subject

Earth-Surface Processes,Geology,Geophysics,Geography, Planning and Development,Global and Planetary Change

Reference57 articles.

1. Asao, K. and Ito, T. (2011): Seismic reflection profile of the Kazusa-Shimosa Group across the central Boso Peninsula, Japan. Joint Annual Meeting of Japan Association of Mineralogical Sciences and The Geological Society of Japan, S3-O-4.

2. Chiba Prefecture (2004): Report of Seismic Geological Survey in Chiba Prefecture (Heisei 15 Nendo Jishin Kankei Kiso Kofukin Chibaken Chika Kozo Chosa Hokokusho).*

3. Natural History Museum and Institute, Chiba (1991): Geoscience Data: Catalog of Key Beds in the Lower Kazusa Group Version 1990 (Chigaku Shiryo Kazusa Sogun Kabu Kagisoshu).*

4. Geological Survey of Japan (1976): Distribution Map of Oil and Gas Fields in Japan (Including Offshore Areas) (2nd ed.), Map Series, Scale 1:200,000. Geological Survey of Japan.

5. Chiyonobu, S., Sato, T., Ishikawa, K. and Yamasaki, M. (2007): Uppermost Cenozoic calcareous nannofossil biostratigraphy of the hotspring wells located in the central part of Tokyo, Japan. Journal of the Geological Society of Japan, 113, 223-232.

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