Geological occurrence and morphological feature of submarine mud volcanoes: A brief review

Author:

Kioka Arata1

Affiliation:

1. Institut für Geologie, Fakultät für Geo- und Atmosphärenwissenschaften, Leopold-Franzens-Universität Innsbruck

Publisher

The Geological Society of Japan

Subject

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

Reference116 articles.

1. Amante, C. and Eakins, B. W., 2009, ETOPO1 1 Arc-Minute Global Relief Model: Procedures, data sources and analysis. NOAA Technical Memorandum NESDIS NGDC-24, National Geophysical Data Center, NOAA, doi: 10.7289/V5C8276M.

2. 浅田美穂, 2017, 熊野海盆泥火山における活動拘条件を探る.日本地球惑星科学連合2017年大会予稿集, SGL34-P04. [Asada, M., 2017, Why and where submarine mud volcanoes existing? A case study of the Kumano Basin, Nankai Trough subduction zone. Japan Geosci. Union Meet. 2017, Abstr., SGL34-P04.]

3. 浅田美穂, 2020, 「泥火山」定義, 概念, 成因, および最近の研究動向.地質雑, 126, 3-16. [Asada, M., 2020, Definition, concept, occurrence, and recent developments in the study of mud volcanoes. J. Geol. Soc. Japan, 126, 3-16.](本特集号)

4. 浅田美穂・木村俊則・野口拓郎・Moore G. F., 2016, 熊野海盆外縁隆起帯における泥火山活動報告.日本地球惑星科学連合2016年大会予稿集, SGL40-P01. [Asada, M., Kimura, T., Noguchi, T. and Moore, G. F., 2016, Mud volcano activity confirmed at the Kumano Basin Edge Fault Zone. Japan Geosci. Union Meet. 2016, Abstr., SGL40-P01.]

5. Ashi, J. and Taira, A., 1992, Structure of the Nankai accretionary prism as revealed from IZANAGI sidescan imagery and multichannel seismic reflection profiling. Isl. Arc, 1, 104-115.

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