Low total and inorganic carbon contents within the Taiwan Chelungpu fault system

MINORU IKEHARA; TETSURO HIRONO; OSAMU TADAI; MASUMI SAKAGUCHI; HIROYUKI KIKUTA; TATSURO FUKUCHI; TOSHIAKI MISHIMA; NORIHIRO NAKAMURA; KAN AOIKE; KOICHIRO FUJIMOTO; YOSHITAKA HASHIMOTO; TSUYOSHI ISHIKAWA; HISAO ITO; MASATAKA KINOSHITA; WEIREN LIN; KOJI MASUDA; TAKUO MATSUBARA; OSAMU MATSUBAYASHI; KAZUO MIZOGUCHI; MASAFUMI MURAYAMA; KENSHIRO OTSUKI; HIROKI SONE; MIKI TAKAHASHI; WATARU TANIKAWA; MASAHARU TANIMIZU; WONN SOH; SHENG-RONG SONG

doi:10.2343/geochemj.41.391

Note

Low total and inorganic carbon contents within the Taiwan Chelungpu fault system

MINORU IKEHARA, TETSURO HIRONO, OSAMU TADAI, MASUMI SAKAGUCHI, HIROYUKI KIKUTA, TATSURO FUKUCHI, TOSHIAKI MISHIMA, NORIHIRO NAKAMURA, KAN AOIKE, KOICHIRO FUJIMOTO, YOSHITAKA HASHIMOTO, TSUYOSHI ISHIKAWA, HISAO ITO, MASATAKA KINOSHITA, WEIREN LIN, KOJI MASUDA, TAKUO MATSUBARA, OSAMU MATSUBAYASHI, KAZUO MIZOGUCHI, MASAFUMI MURAYAMA, KENSHIRO OTSUKI, HIROKI SONE, MIKI TAKAHASHI, WATARU TANIKAWA, MASAHARU TANIMIZU, WONN SOH, SHENG-RONG SONG

著者情報

MINORU IKEHARA
Center for Advanced Marine Core Research, Kochi University
TETSURO HIRONO
Department of Earth and Space Science, Graduate School of Science, Osaka University
Kochi Institute for Core Sample Research, Japan Agency for Marine-Earth Science and Technology
OSAMU TADAI
Marine Works Japan Ltd.
MASUMI SAKAGUCHI
Marine Works Japan Ltd.
HIROYUKI KIKUTA
Kochi Institute for Core Sample Research, Japan Agency for Marine-Earth Science and Technology
TATSURO FUKUCHI
Department of Earth Sciences, Graduate School of Science & Engineering, Yamaguchi University
TOSHIAKI MISHIMA
Center for Advanced Marine Core Research, Kochi University
NORIHIRO NAKAMURA
Department of Geoenvironmental Science, Graduate School of Science, Tohoku University
KAN AOIKE
Center for Deep Earth Exploration, Japan Agency for Marine-Earth Science and Technology
KOICHIRO FUJIMOTO
Faculty of Education, Tokyo Gakugei University
YOSHITAKA HASHIMOTO
Department of Natural Environmental Science, Kochi University
TSUYOSHI ISHIKAWA
Kochi Institute for Core Sample Research, Japan Agency for Marine-Earth Science and Technology
HISAO ITO
Center for Deep Earth Exploration, Japan Agency for Marine-Earth Science and Technology
MASATAKA KINOSHITA
Institute for Research on Earth Evolution, Japan Agency for Marine-Earth Science and Technology
WEIREN LIN
Kochi Institute for Core Sample Research, Japan Agency for Marine-Earth Science and Technology
KOJI MASUDA
Institute for Geo-Resources and Environment, National Institute of Advanced Industrial Science and Technology
TAKUO MATSUBARA
Department of Earth Sciences, Graduate School of Science & Engineering, Yamaguchi University
OSAMU MATSUBAYASHI
Institute of Geology and Geoinformation, National Institute of Advanced Industrial Science and Technology
KAZUO MIZOGUCHI
Earthquake Research Department, National Research Institute for Earth Science and Disaster Prevention
MASAFUMI MURAYAMA
Center for Advanced Marine Core Research, Kochi University
KENSHIRO OTSUKI
Department of Geoenvironmental Science, Graduate School of Science, Tohoku University
HIROKI SONE
Department of Geophysics, School of Earth Sciences, Stanford University
MIKI TAKAHASHI
Institute for Geo-Resources and Environment, National Institute of Advanced Industrial Science and Technology
WATARU TANIKAWA
Kochi Institute for Core Sample Research, Japan Agency for Marine-Earth Science and Technology
MASAHARU TANIMIZU
Kochi Institute for Core Sample Research, Japan Agency for Marine-Earth Science and Technology
WONN SOH
Kochi Institute for Core Sample Research, Japan Agency for Marine-Earth Science and Technology
SHENG-RONG SONG
Department of Geosciences, National Taiwan University

キーワード: Chelungpu fault, Chi-Chi earthquake, total carbon content, inorganic carbon content, carbonate mineral

ジャーナルフリー

2007 年 41 巻 5 号 p. 391-396

DOI https://doi.org/10.2343/geochemj.41.391

詳細

抄録

We presented the total and inorganic carbon contents of core samples recovered from the Taiwan Chelungpu fault system, which slipped at the 1999 Chi-Chi earthquake, and reported lower contents of inorganic carbon within the black gouge zone in FZB1136 (fault zone at depth 1136 m in Hole B) and in the black-material disks in FZB1194 and FZB1243.

責任著者(Corresponding author)

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