km Fig. 1, 1987, 1988;, 2010; Santra et al., 2013, 1933;, 1956;, ,000 m, Table Suzuki et al. 2011,, 1932
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1 Jour. Geol. Soc. Japan, Vol. 122, No. 7, p , July 2016 doi: /geosoc 巡 検 案 内 書 Tephrochronology of the Kazusa Group in southern Kanto Plain, central Japan Takehiko Suzuki 1, Masaaki Shirai 1 and Tohru Fukushima J 1 Department of Geography, Graduate School of Urban Environmental Sciences, Tokyo Metropolitan University, 1-1 Minami-osawa, Hachioji, Tokyo , Japan 2 Musashino School of Paleontology, MKJ Office, Chuo, Musashi-murayama, Tokyo , Japan Corresponding author: suzukit@tmu.ac.jp PDF J-STAGE km Keywords Early Pleistocene, tephra, petrographic properties, Kanto Plain, Sayama Hills, Tama Hills 1 25, JR JR Stop N, E, SGO Stop N, E Stop 2-c 2, 1 HU 1 2 HU 2 Stop N, E,, 1 HU 1 Stop N, E NG-YR Stop N, E -Kd18 SG-Kd18 MT The Geological Society of Japan
2 km Fig. 1, 1987, 1988;, 2010; Santra et al., 2013, 1933;, 1956;, ,000 m, Table Suzuki et al. 2011,, m Fig.. Tectonic setting of the Kanto Plain originated from a paleo-forearc basin. Forearc basin: Sugiyama 1989 and Iwata et al. 2002, Kazusa Trough: Kaizuka Triangular shows volcanic field area discussed in this study., 1994;, , 2000 Fig , 1958, m 80 m, 1974,
3 Table. Petrographic properties of representative tephras in the Sayama and Tama Hills., 2007 SGO;, 2004 SYG;, 2005, m m Fig. 2, , 1955;, 1970;, 1982;, 1984;, 1994;, 2007;, Fig , 1979;, , 2000;, 2002;, Fig. 4 HM-Kd16 GS NK NB-Kd17 SG-Kd18 MT Kd19 NG-YR YU PK YM KK TN Sr-Kmd Ob4e-Kd23A Ob4d-Kd23B Ob4c-Kd24 Ob4b 4 Ob4b-6, -5, -4, -1 Omn-SK110 22
4 346 鈴木 毅彦 白井 正明 福嶋 徹 Fig. 2. Index map of the excursion area. Produced from 5-mmesh DEM of the Geospatial Information Authority of Japan. Fig. 3. Stratigraphy of the Kazusa Group. Compiled from Takano 1994, Mitsunashi and Kikuchi 1982, Eto 1986, Tokyo Metropolitan Institute of Civil Engineering 1996, Suzuki et al and Sakai The stratigraphic relations of among the formations among of these areas are after Fujioka and Kameo 2004, and Suzuki and Murata のものに相当する これらテフラはまた銚子地域における石 多摩丘陵の上総層群の特徴の一つとして 鶴川撓曲を挟ん 灰質ナンノ化石対比基準面 9 11 の層位とその年代より 降 で北西部と中部では 堆積環境のちがいから岩相が大きく異 下年代が Ma にあると推定されている なることがあげられる 北西部では上総層群は北東方向に緩 一方 石灰質ナンノ化石による微化石層序 高野, 1994; く傾斜し 礫層 シルト層 砂層を 1 サイクルとして複数 藤岡ほか, 2003; 江藤ほか, 1987 放射年代測定 伊藤ほか, 2002 古地磁気層序 畝村ほか, 1986; 植木ほか, 2013 な のサイクルが累重するため層相変化が著しい このうち小山 どの研究も行われている 層 干潟 汽水内湾性 砂層 海浜 浅海性 からなる堆積サ 田層 連光寺層 稲城層はいずれも下位より河川性礫層 泥
5 Fig.. Correlation of tephras in the Kazusa Group. Modified from Suzuki and Murata 2011, and ages of calcareous nannofossil datum are after Sato et al
6 , 2011 Fig.. Accumulation rate of the Kazusa Group in the Tama Hills, southeast of the Musashino Upland, Boso Peninsula and Choshi area. After Suzuki and Murata 2011., 1994, 1984, 1982, 1994 Fig. 5, 1991, 2004 Stop 1 SGO 1 25, N, E Fig. 6, 128 m SGO, 2004 Fig cm 2 cm n Table 1 Suzuki et al SGO 7 km E1, HU 1,, 1994 Ob4b-1 Ob4b-1, 2011; Suzuki et al., 2011, 2014; Suzuki et al., 2016 Table Ma, 2011 Stop km Ma Suzuki et al., 2011 SYG;, 2005, Ob4b-1 Stop 2 Ob4b-1 Stop 1 1m 4.5 km 9.7 m Stop 2 Stop 3 50 cm Suzuki et al., 2016
7 地質雑 関東平野南部における上総層群のテフロクロノロジー 349 Fig. 6. Maps showing locations of stops. の様な分布と粒径が数 cm であること またホルンブレンド が存在する可能性があり 1.6 Ma 頃の同地域の火山活動の とカミングトン閃石を特徴的に含む点は 多摩丘陵から埼玉 指標になり得る 県秩父盆地 狭山丘陵にかけて分布する中期更新世のテフラ 群 例えば鈴木, 2000 や坂田ほか, 2012 など と類似する これらの給源火山はまだよく分かっていないが 粒度や斑晶 鉱物の組合せから中期更新世に爆発的噴火を繰り返していた の可能性 関東山地南西端に位置する黒富士火山 竹下, 2005 がある Ob4b-1 も同様に黒富士火山やその近傍に給源火口 Stop 2 多摩川河床 上総層群小山田層とそれに含まれる HU1 と 第 2 堀 之 内 テ フ ラ 第 1 堀之内テフラ の露頭 HU2 地形図 1 25,000 立川 位 置 N, E Stop 2-c 日野市栄町
8 Fig.. Stratigraphic columns of each the sections are shown in Fig. 2. Modified from Suzuki and Murata 2011.
9 地質雑 関東平野南部における上総層群のテフロクロノロジー 351 Fig. 8. Landform and the summit level map of the Tama Hills. Fig. 9. NG-YR and YM tephras cropped out at Stop 4 and at 420 m west of Stop 4, respectively. 2 丁目 多摩川河川敷 JR 中央線鉄橋上流 解 説 温暖期に相当する現在では 多摩川の中流から上流 1994 Stop 2-c 付近で降下軽石層である第 1 堀之内テフ Ob4b-1 が観察できる HU2 は房総半島の上 ラ HU1 域にかけては河床が下刻傾向にある このため多くの地点に 総層群黄和田層中の Kd25 に対比されており 大峰 -SK110 おいて段丘構成層の基盤となる上総層群が現河床沿いに露出 する 加住丘陵から流下する谷地川が多摩川に合流する テフラ 長橋ほか, 2000 や大峰テフラ Omn, 町田 新井, ともよばれている 同テフラは飛騨山脈の火山を給源 2003 Stop 2 付近 Fig. 6; JR 中央線鉄橋の上流約 1 km の区間 とし 中部日本から東北日本の各地で分布が確認されている では同層群中の小山田層が露出する 小山田層は礫層からな 前期更新世初頭の重要指標テフラで その噴出年代は生層 る下部 シルト層からなる中部 砂層からなる上部に区分さ 序 古地磁気層序 放射年代値などから Ma 前 Stop 2 では下部 Stop 2-a 付近 お れており 高野, 1994 が観察できる よび中部 Stop 2-b Stop 2-c 付近 後と推定されている 里口ほか, 1999; 長橋ほか, 2000; 町 関東では Kd25 の模式地である養老川 長 田 新井, 2003 Stop 2 付近の小山田層についてはテフラと足跡化石の報 をはじめ 多摩丘陵西部の小山田層中 多摩 橋ほか, 2000 東京都内地下 佐藤 丘陵南部の小柴層中 藤岡ほか, 2003 告がなされており 倉川 足跡化石発掘調査団, 2000; 多摩 Stop 2-b 付近でガ 川足跡化石調査団, 2002; 福嶋, 2009 HU2, 高野, ラス質降下火山灰層である第 2 堀之内テフラ 銚子地域の犬吠層群中 ほか, 2004; Suzuki et al., 2011 で本テフラの存在が知られている 藤岡 亀尾, 2004
10 Ob4b-1 Stop 1, 2011; Suzuki et al., 2011 Stop 2-c Ob4b-1 Ob4b-1 Ob4b-1 Stop2-c 70.0 m Stop1 128 m m m m Ob4b-1 Stop 3 1 HU , N, E Stop 3 Fig. 6 Ob4b-1 HU 1 HU 2 -SK110 Fig Ma, 2000 Stop 3 Stop 4 NG-YR 1 25, N, E Fig. 7 Stop 4 42 cm Fig. 9 NG,, 1955;, 1991 NG NG NG NG NG YM,, 2011 Fig. 4 YM Stop m 2007 Fig. 9 NG YR 2 NG NG- YR NG-YR YM Table 1 NG-YR 1991 Kd Ma, 2011 Stop 4 NG-YR 2.2 m 5 cm 1994 YU YU NG-YR Stop 4 NG-YR Fig. 7, 9 washover
11 Reinson, 1992, 2013 HCS, 2013 Stop 5 -Kd18 SG-Kd18 MT 1 25, N, E Fig. 3 Stop 5 -Kd18 SG-Kd18 MT -Kd18 SG-Kd18 30 cm 3 cm 1 cm 10 cm SiO 2 CaO wt. K 2 O 2.53 wt. Table 1 Kd18 -Kd18 SG-Kd18, 2011 Fe/Fe Mg La/Y, Fig. 1, 1991, Kd8, 2008;, 2011 MT 32 cm, 1994, 2011 Natural History Museum and Institute, Chiba, 1991, 1990 Geoscience data: Catalog of Key Beds in the Lower Part of Kazusa Group version 1990 * Natural History Museum and Institute, Chiba, 218p Endo, H., Kamishima, M., Yamazaki, T. and Takayama, T., 1991, GS-ED-1 Jour. Geol. Soc. Japan, 97, Eto, T., 1986,, 2 Sci. Rep. Yokohama Nat. Univ.
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13 Bull. Fac. General Educ. Utsunomiya Univ. Sec. 2, no. 23, 1 34 Sakata, K., Nakazawa, T. and Nakazato, H., 2012, Bull. Geol. Surv. Japan, 63, Santra, M., Steel, R., Olariu, C. and Sweet, M., 2013, Stages of sedimentary prism development on a convergent margin- Eocene Tyee Forearc Basin, Coast Range, Oregon, USA. Global and Planetary Change, 103, Satoguchi, Y., Nagahashi, Y., Kurokawa, K. and Yoshikawa, S., 1999, Earth Sci. Chikyu Kagaku, 53, Sato, M., Suzuki, T. and Nakayama, T., 2004, Jour. Geogr., 113, Sato, T., Chiyonobu, S., Hodell, D. A., 2009, Data report: Quaternary calcareous nannofossil datums and biochronology in the North Atlantic Ocean, IODP Site U Channell, J. E. T., Kanamatsu, T., Sato, T., Stein, R., Alvarez Zarikian, C. A., Malone, M. J., and the Expedition 303/306 Scientists. Proceedings of the Integrated Ocean Drilling Program, 303/306, doi: /iodp.proc Shirai1, M. and Imamura, A., 2013,, 2013 Japan Geosci. Union Meet. 2013, Abstr., HQR23 P04 Sugiyama, Y., 1989, 2 Bull. Geol. Surv. Japan, 40, Sugiyama, Y., Sangawa, A., Shimokawa, K. and Mizuno, K., 1988, 5 1 Geology of the Omaezaki District., Quadrangle Series, scale 1: 50,000 Geol. Surv. Japan, 153p Suzuki, T., 2000, Chikyu Monthly, 22, Suzuki, T., 2004, Japan Assoc. Quatern. Res., Progr. Abstr., no. 34, Suzuki, T. and Murata, M., 2008, Quatern. Res., 47, Suzuki, T. and Murata, M., 2011, Jour. Geol. Soc. Japan, 117, Suzuki, T., Murata, M., Oishi, M., Yamazaki, H., Nakayama, T., Kawashima, S. and Kawai, M., 2008, Quatern. Res., 47, Suzuki, T., Nakajima, E., Kawashima, S., Kawai, M. and Nakayama, T., 2016, Identification of three Early Pleistocene tephras in and around the west part of the Musashino Upland, Tokyo, Northeast Japan. Geogr. Rep. Tokyo Metr. Univ., 51, Suzuki, T., Obara, M., Aoki, T., Murata, M., Kawashima, S., Kawai, M., Nakayama, T., and Tokizane, K Identification of Lower Pleistocene tephras under Tokyo and reconstruction of Quaternary crustal movements, Kanto Tectonic Basin, central Japan. Quatern. Intern., 246, doi: /j.quaint Suzuki, Y., Kodama, K., Mitsunashi, T., Oka, S., Urabe, A., Endo, T., Horiguchi. M., Eto, T., Kikuchi. T., Yamauchi, S., Nakajima, T., Tokuhashi, S., Nirei, H., Hara, Y., Nakayama, T., Nasu, N., Kagami, H., Kimura, M. and Honza, E., 1995, 2 20 Geological Map of Tokyo Bay and Adjacent Areas 1: 100,000 2nd Edition, Miscellaneous Map Series, 20 Geol. Surv. Japan, 109p Shoda, K., Takegoshi, S. and Research Group for Geology of the Western Hills of the Kanto Plain, 2005,, th Ann. Meet. Geol. Soc. Japan, Abstr., 82 T Takahashi, M., Hayashi, H., Kasahara, K., Ikawa, T., Kawanaka, T. and Suda, S., 2005, Rep. Nat. Res. Inst. Earth Sci. Disaster Prev., 67, Takano, S., 1994, Jour. Geol. Soc. Japan, 100, Takano, S., 2002, Japan Assoc. Quatern. Res., Progr. Abstr., no. 32, Research Group for Fossil Footprints from the Riverbed of Tamagawa, 2002, Report of the Fossil Footprints of Stegodon Aurorae from the Riverbed of the Tama River in the Akishima City, Tokyo * Education Board in Akishima City, 15p Taura, I., Earth Science Club of Tokorozawa High School and Shoda, K., 2004, E1 58 Progr. Abstr. Excur. Guide 63th Ann. Meet. Assoc. Geol. Col. Japan, 114 Takeshita, Y., 2005, th Ann. Meet. Geol. Soc. Japan, Abstr., 154 Tokyo Metropolitan Institute of Civil Engineering, 1996, 6 Deep Underground Geological Map of Tokyo Wards * Tokyo Metropolitan Institute of Civil Engineering, 66p Ueda, F., 1933, Jour. Geol. Soc. Japan, 40, Ueki, T, Hara, H. and Ozaki, M., 2013, 5 1 Geology of the Hachioji District, Quadrangle Series, scale 1: 50,000 Geol. Surv. Japan, AIST, 137p Ueki, T and Sakai, M., 2007, 5 1 Geology of the Ome District, Quadrangle Series, scale 1: 50,000 Geol. Surv. Japan, AIST, 189p Unemura, S., Furuta, T., Koizumi, A. and Chiba, T., 1986, Japan Assoc. Quatern. Res., Progr. Abstr., no. 16, Yoshida, M. and Takahashi, M., 1991, Jour. Geol. Soc. Japan, 97, * English translation from the original written in Japanese.
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