Geologic evidence for late Quaternary repetitive surface faulting on the Isurugi fault along the northwestern margin of the Tonami Plain, north-central Japan-Reference-Cited by-同舟云学术

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Geologic evidence for late Quaternary repetitive surface faulting on the Isurugi fault along the northwestern margin of the Tonami Plain, north-central Japan

Published:2015-06 Issue:2 Volume:24 Page:188-204
ISSN:1038-4871
Container-title:Island Arc
language:en
Short-container-title:Island Arc

Author:

Maruyama Tadashi¹,Saito Masaru²

Affiliation:

1. Research Institute of Earthquake and Volcano Geology; National Institute of Advanced Industrial Science and Technology (AIST); Central 7 1-1-1 Higashi Tsukuba Ibaraki 305-8567 Japan

2. Dia Consultants Company Limited; 2-272-3 Yoshino Kita-ku Saitama 331-0811 Japan

Publisher

Wiley

Subject

Geology

Reference44 articles.

1. Style and episodicity of late Quaternary activity on the Pisa-Grandview Fault Zone, Central Otago, New Zealand;Beanland;New Zealand Journal of Geology and Geophysics,1989

2. Development of the radiocarbon program OxCal;Bronk Ramsey;Radiocarbon,2001

3. Bayesian analysis of radiocarbon dates;Bronk Ramsey;Radiocarbon,2009

4. Transpressional rupture of an unmapped fault during the 2010 Haiti earthquake;Calais;Nature Geoscience,2010

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