Kanto Syntaxis: when did it begin to grow?

Author:

Hoshi Hiroyuki1

Affiliation:

1. Department of Earth Sciences, Aichi University of Education

Publisher

The Geological Society of Japan

Subject

General Earth and Planetary Sciences,General Engineering,General Environmental Science

Reference118 articles.

1. Akimoto, K., Hattori, M. and Oda, M., 2002, Late Cenozoic paleobathymetry and paleogeography in the South Fossa Magna and Enshunada regions, Japan, based on planktic and benthic foraminifera. Mar. Geol., 187, 89-118.

2. Amano, K., 1991, Multiple collision tectonics of the south Fossa Magna in central Japan. Modern Geol., 15, 315-329.

3. 天野一男・高橋治之・立川孝志・横山健治・横田千秋・菊池 純(Amano, K., Takahashi, H., Tachikawa, T., Yokoyama, K., Yokota, C. and Kikuchi, J.), 1986, 足柄層群の地質:伊豆微小大陸の衝突テクトニクス(Geology of Ashigara Group: collision tectonics of Izu micro-continent with Eurasian plate). 中川久夫・小高民夫・高柳洋吉編, 北村 信教授退官記念地質学論文集(Essay in Geology: Professor Nobu Kitamura Commemorative Volume), 北村 信教授退官記念事業会(Professor Nobu Kitamura Taikan Kinenjigyokai), 7-29.

4. 青池 寛(Aoike, K.), 1999, 伊豆衝突帯の構造発達(Tectonic evolution of the Izu collision zone). 神奈川県博調研報, 自然科学(Res. Rep. Kanagawa Pref. Mus., Nat. Hist.), 9, 113-151.

5. Arai, R. and Iwasaki, T., 2014, Crustal structure in the northwestern part of the Izu collision zone in central Japan. Earth Planets Space, 66, 21, doi: 10.1186/1880-5981-66-21.

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