Paleostress history estimated from preferred orientation of microcracks in the Tanzawa tonalite body, central Japan and its relationship to the Honshu arc-Izu arc collision

Author:

Sato Takatsune1,Takagi Hideo2

Affiliation:

1. Department of Earth Sciences and Environmental and Resources Engineering, Graduate School of Science and Engineering, Waseda University

2. Department of Earth Sciences, Faculty of Education and Integrated Arts and Sciences, Waseda University

Publisher

The Geological Society of Japan

Subject

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

Reference58 articles.

1. Aoike, K., 2001, Geology of the Tanzawa, Misaka and Koma Districts, Central Japan-Tectonic Evolution of the Izu Collision Zone-. Ph.D.thesis, Dept. Earth and Planet. Sci., Grad. Sch. Sci., Univ. of Tokyo. 114p.

2. 天野一男(Amano, K.), 1986, 多重衝突帯としての南部フォッサマグナ.月刊地球(Chikyu, Monthly), 8, 581-585.

3. Amano, K., 1991, Multiple collision tectonics of the South Fossa Magna in Central Japan. Modern Geology, 15, 315-329.

4. 天野一男・立川孝志・横山健治・横田千秋(Amano, K., Tachikawa, T., K., Yokoyama, K. and Yokota, C.), 1984, 神縄断層周辺の応力場.日本地質学会第91年学術大会講演要旨(91st Ann. Meet. Geol. Soc. Japan, Abst.), 528.

5. 有馬 眞・青池 寛・川手新一(Arima, M., Aoike, K. and Kawate, S.), 1999, 丹沢山地の構造発達史, 神奈川博調査研報(Res. Rep. Kanagawa Pref. Mus. Nat. Hist.), 3, 57-77.

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