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Holocene beach deposits for assessing coastal uplift of the northeastern Boso Peninsula, Pacific coast of Japan

Published online by Cambridge University Press:  20 January 2017

Toru Tamura*
Affiliation:
Geological Survey of Japan, AIST, Tsukuba, Japan Department of Geography, The University of Sheffield, UK
Fumitoshi Murakami
Affiliation:
Geological Survey of Japan, AIST, Tsukuba, Japan
Kazuaki Watanabe
Affiliation:
Geological Survey of Japan, AIST, Tsukuba, Japan
*
*Corresponding author. Geological Survey of Japan, AIST, 1-1-1 Higashi, Tsukuba, Ibaraki 305-8567, Japan. Department of Geography, The University of Sheffield, Winter Street, Sheffield S10 2TN, United Kingdom. E-mail: [email protected] (T. Tamura).

Abstract

This paper presents a case study that assessed spatial variations in the tectonic uplift rates of beach deposits in the relict Kujukuri strand plain, situated on the northeastern coast of the Boso Peninsula, eastern Japan. The southern Boso Peninsula is tilted downward to the northeast due to plate subduction along the Sagami Trough. However, the cause of the northeastern coast uplift creating the relict strand plain is unclear, due to the absence of a Holocene raised marine terrace sequence. Elevations and ages of beach deposits were collected from drilled cores and ground-penetrating radar profiles along three shore-normal sections in the southern Kujukuri strand plain. From this, alongshore variations in the relative sea level since the mid-Holocene could be seen. These corresponded to north-to-northeast downward tilting at a rate of 0.4 m/ka for an interval 10 km and are concordant with the longer term tilting of the last interglacial marine terrace surrounding the plain. Although it is difficult to assess shore-normal variations of uplift based on the present dataset, the recognized tilting apparently continues to the tilting of the southern Boso Peninsula, implying the Sagami Trough probably affects the uplift of the Kujukuri coast.

Type
Research Article
Copyright
University of Washington

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References

Bristow, C.S., and Pucillo, K. Quantifying rates of coastal progradation from sediment volume using GPR and OSL: the Holocene fill of Guichen Bay, south-east South Australia. Sedimentology 53, (2006). 769788.Google Scholar
Chappell, J., Ota, Y., and Berryman, K.R. Late Quaternary coseismic uplift history of Huon Peninsula, Papua New Guinea. Quatern. Sci. Rev. 15, (1996). 722.Google Scholar
Clifton, H.E. A reexamination of facies models for clastic shorelines. Posamentier, H.W., Walker, R.G. Facies models revisited. 84, (2006). SEPM Special Publication, 293337.Google Scholar
Jol, H.M., Smith, D.G., and Meyers, R.A. Digital ground penetrating radar (GPR): a new geophysical tool for coastal barrier research (examples from the Atlantic, Gulf and Pacific Coasts, U.S.A.). J. Coast. Res. 12, (1996). 960968.Google Scholar
Kaizuka, S. Tectonic setting and the Quaternary crustal movements in Kanto district. Kakimi, T., and Suzuki, Y. Earthquakes and crustal deformation in the Kanto District. (1974). Tokyo, Lattice Publication. 99118.Google Scholar
Kaizuka, S. Quaternary crustal movements in Kanto, Japan. Chigaku Zasshi 96, (1987). 223240. (in Japanese with English abstract) Google Scholar
Kumaki, Y. Holocene marine terraces and their deformations in the coastal area of southern Kanto, Japan. Geogr. Rev. Jpn 58B, (1985). 4960.CrossRefGoogle Scholar
Lambeck, K., Antonioli, F., Purcell, A., and Silenzi, S. Sea-level change along the Italian coast for the past 10, 000 yr. Quatern. Sci. Rev. 23, (2004). 15671598.Google Scholar
Land Survey Department The change of elevation of land caused by the great earthquake of September 1st, 1923. 1, (1926). Bulletin of the Earthquake Research Institute, University of Tokyo, 6568. (in Japanese) Google Scholar
Masuda, F., Fujiwara, O., Sakai, T., and Araya, T. Relative sea-level changes and co-seismic uplifts over six millennia, preserved in beach deposits of the Kujukuri strand plain, Pacific coast of the Boso Peninsula, Japan. Chigaku Zasshi 110, (2001). 650664. (in Japanese with English abstract) Google Scholar
Matsuda, T., Ota, Y., Ando, M., and Yonekura, N. Geological study for the 1703 Genroku earthquake. Kakimi, T., and Suzuki, Y. Earthquakes and crustal deformation in the Kanto District. (1974). Tokyo, Lattice Publication. 175192.Google Scholar
Matsuda, T., Ota, Y., Ando, M., and Yonekura, N. Fault mechanism and recurrence time of major earthquakes in southern Kanto district, Japan, as deduced from coastal terrace data. Geol. Soc. Am. Bull. 89, (1978). 16101618.2.0.CO;2>CrossRefGoogle Scholar
Moriwaki, H. The landform evolution of the Kujukuri coastal plain, central Japan. Daiyonki Kenkyu 18, (1979). 116. (in Japanese with English abstract) Google Scholar
Nakada, M., Yonekura, N., and Lambeck, K. Late Pleistocene and Holocene sea-level changes in Japan: implications for tectonic histories and mantle rheology. Palaeogeogr. Palaeoclimatol. Palaeoecol. 85, (1991). 107122.Google Scholar
Nakata, T., Koba, M., Imaizumi, T., Jo, W.R., Matumoto, H., and Suganuma, T. Holocene marine terraces and seismic crustal movements in the southern part of Boso Peninsula, Kanto, Japan. Geogr. Rev. Jpn 53, (1980). 2944.Google Scholar
Nielsen, L., and Clemmensen, L.B. Sea-level markers identified in ground-penetrating radar data collected across a modern beach ridge system in a microtidal regime. Terra Nova 21, (2009). 474479.Google Scholar
Ota, Y., and Yamaguchi, M. Holocene coastal uplift in the western Pacific Rimin the context of late Quaternary uplift. Quatern. Int. 120, (2004). 105117.CrossRefGoogle Scholar
Reynolds, J.M. An Introduction to Applied and Environmental Geophysics. (1997). Chichester, U.K., Wiley-VCH. 806 pGoogle Scholar
Rodriguez, A.B., and Meyer, C.T. Sea-level variation during the Holocene deduced from the morphologic and stratigraphic evolution Morgan Peninsula, Alabama, U.S.A. J. Sed. Res. 76, (2006). 257269.Google Scholar
Rohling, E.J., Grant, K., Hemleben, Ch., Siddall, M., Hoogakker, B.A.A., Bolshaw, M., and Kucera, M. High rates of sea-level rise during the last interglacial period. Nat. Geosci. 1, (2008). 3842.Google Scholar
Sato, H., Okuno, J., Katoh, S., Nakada, M., Maeda, Y., and Kobayashi, F. Holocene crustal movement along the coast of western Kobe and the 1995 Kobe Earthquake, Japan. Quatern. Sci. Rev. 22, (2003). 891897.CrossRefGoogle Scholar
Sato, H., Okuno, J., and Katoh, S. Evaluation of Holocene crustal movement in the Ako Plain, western Japan. Holocene 16, (2006). 533542.Google Scholar
Shishikura, M. Coseismic vertical displacement in the Boso Peninsula during the 1703 Genroku Kanto Earthquake, deduced from emerged shoreline topography. Rekishi Jishin 16, (2000). 113122. (in Japanese) Google Scholar
Shishikura, M. Crustal movements in the Boso Peninsula from the analysis of height distribution of the highest Holocene paleo-shoreline. Annual Report on Active Fault and Paleoearthquake Researches 1. (2001). Active Fault Research Center, AIST, 273285. (in Japanese with English abstract) Google Scholar
Shishikura, M., and Miyauchi, T. Holocene geomorphic development related to seismotectonics in coastal lowlands of the Boso Peninsula, Central Japan. Quaternary Research (Japan) 40, (2001). 235242. (in Japanese with English abstract) Google Scholar
Smith, D.G., Meyers, R.A., and Jol, H.M. Sedimentology of upper-mesotidal (3.7 m) Holocene barrier, Willapa Bay, SW Washington, U.S.A. J. Sed. Res. 69, (1999). 12901296.Google Scholar
Stuiver, M., and Reimer, P.J. Extended 14C database and revised CALIB radiocarbon calibration program. Radiocarbon 35, (1993). 215230.Google Scholar
Sugimura, A., and Naruse, Y. Changes in sea level, seismic upheavals, and terraces in the southern Kanto region, Japan (I). Japanese Journal of Geology and Geography 24, (1954). 101113.Google Scholar
Sugimura, A., and Naruse, Y. Changes in sea level, seismic upheavals, and terraces in the southern Kanto region, Japan (II). Japanese Journal of Geology and Geography 26, (1955). 165176.Google Scholar
Sunamura, T., and Horikawa, K. Sediment budget in Kujukuri coastal area, Japan. Coastal Sediments ’77. Amer. Soc. Civil Eng. (1977). 475487.Google Scholar
Tamura, T., Masuda, F., Sakai, T., and Fujiwara, O. Temporal development of prograding beach–shoreface deposits: the Holocene of Kujukuri coastal plain, eastern Japan. Mar. Geol. 198, (2003). 191207.Google Scholar
Tamura, T., Nanayama, F., Saito, Y., Murakami, F., Nakashima, R., and Watanabe, K. Intra-shoreface erosion in response to rapid sea-level fall: depositional record of a tectonically uplifted strand plain, Pacific coast of Japan. Sedimentology 54, (2007). 11491162.CrossRefGoogle Scholar
Tamura, T., Murakami, F., Nanayama, F., Watanabe, K., and Saito, Y. Ground-penetrating radar profiles of Holocene raised-beach deposits in the Kujukuri strand plain, Pacific coast of eastern Japan. Mar. Geol. 248, (2008). 1127.Google Scholar
Uda, T. Comparative study on long-term shoreline evolution during the past 6000 years and recent short-term beach changes on the Kujukuri coast. Transaction 10, (1989). Japanese Geomorphological Union, 343355. (in Japanese with English abstract) Google Scholar