| 西南日本秋吉带石炭系高山(Ko-yama)灰岩群的褶皱构造 |
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| 引用本文：Noriyuki INADA,Shigeyuki SUZUKI,Keisuke ISHIDA,Shinji YAMASHITA.2012.西南日本秋吉带石炭系高山(Ko-yama)灰岩群的褶皱构造[J].地球学报,33(s1):24. |
| DOI：10.3975/cagsb.2012.s1.13 |
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| 中文摘要: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). |
| 中文关键词:folded structure Ko-yama Limestone Carboniferous Akiyoshi Belt |
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| Folded Structure of the Carboniferous Ko-yama Limestone Group, Akiyoshi Belt, SW JAPAN |
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| Abstract: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). |
| keywords:folded structure Ko-yama Limestone Carboniferous Akiyoshi Belt |
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