ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
西南日本秋吉带石炭系高山(Ko-yama)灰岩群的褶皱构造
  
关键词:folded structure  Ko-yama Limestone  Carboniferous  Akiyoshi Belt
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作者单位E-mail
Noriyuki INADA Dept. Earth Sci., Okayama University sc19506@s.okayama-u.ac.jp 
Shigeyuki SUZUKI Dept. Earth Sci., Okayama University  
Keisuke ISHIDA Laboratory of Geology, Institute of SAS, Tokushima University  
Shinji YAMASHITA Dept. Earth Sci., Okayama University  
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摘要:
Folded Structure of the Carboniferous Ko-yama Limestone Group, Akiyoshi Belt, SW JAPAN
      The study area is located in Kawakami-cho, Okayama Prefecture, which is occupied by Lower Carboniferous to Middle Permian Ko-yama Limestone Group (Yokoyama et al., 1979), Permian Yoshii Group (Sano et al., 1987) and Triassic Nariwa Group (Tera-oka, 1959). The Nariwa Group unconformably covers the Paleozoic successions (Otoh, 1985). These succes-sions belong to the Akiyoshi Belt. The Ko-yama Limestone Group is composed mainly of massive limestone, with basic volcanic rocks, acidic tuff and chert. The group was dated by foraminifer and fusu-linid as Lower Carboniferous to Middle Permian (Yo-koyama et al., 1979).
Noriyuki INADA,Shigeyuki SUZUKI,Keisuke ISHIDA,Shinji YAMASHITA.2012.Folded Structure of the Carboniferous Ko-yama Limestone Group, Akiyoshi Belt, SW JAPAN[J].Acta Geoscientica Sinica,33(s1):24.
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