越南东北部Cat Ba岛泥盆系-石炭系过渡层的初探
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引用本文:Toshifumi KOMATSU,Reishi TAKASHIMA,TA Hoa PHUONG,Tran Huyen DANG,Duc Phong NGUYEN,Huu Hung NGUYEN,Satoru KATO,Kento HIRATA,Takumi MAEKAWA.2012.越南东北部Cat Ba岛泥盆系-石炭系过渡层的初探[J].地球学报,33(s1):38.
DOI:10.3975/cagsb.2012.s1.19
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作者单位
Toshifumi KOMATSU Graduate School of Science and Technology, Kumamoto University 
Reishi TAKASHIMA The Center for Academic Resources and Archives Tohoku University Museum, Tohoku University 
TA Hoa PHUONG College of Sciences, Vietnam National University 
Tran Huyen DANG Vietnam Institute of Geosciences and Mineral Resources (VIGMR) 
Duc Phong NGUYEN Vietnam Institute of Geosciences and Mineral Resources (VIGMR) 
Huu Hung NGUYEN Vietnam National Museum of Nature (VNMN) 
Satoru KATO Graduate School of Science and Technology, Kumamoto University 
Kento HIRATA Graduate School of Science and Technology, Kumamoto University 
Takumi MAEKAWA Graduate School of Science and Technology, Kumamoto University 
中文摘要:The Pho Han Formation is exposed on southern Cat Ba Island, Hai Phong Province in northeastern Vietnam, and intercalates the Devonian and Carbonif-erous (D-C) boundary (Ta and Doan, 2007; Komatsu et al., 2012). The D-C boundary section consists mainly of limestone beds, numbered from 1 to 167, interca-lated with alternating black organic-rich shales. The limestone yields abundant brachiopods, crinoid-stems and conodonts. Preliminary investigations on strati-graphy (conodont biostratigraphy and δ13C) and sedi-mentology of beds 113-133 were undertaken in this study.
中文关键词:D-C boundary  Conodont  δ13C  Cat Ba Island  Vietnam
 
Devonian to Carboniferous Transitional Beds on Cat Ba Island, Northeastern Vietnam–A Preliminary Assessment
Abstract:The Pho Han Formation is exposed on southern Cat Ba Island, Hai Phong Province in northeastern Vietnam, and intercalates the Devonian and Carbonif-erous (D-C) boundary (Ta and Doan, 2007; Komatsu et al., 2012). The D-C boundary section consists mainly of limestone beds, numbered from 1 to 167, interca-lated with alternating black organic-rich shales. The limestone yields abundant brachiopods, crinoid-stems and conodonts. Preliminary investigations on strati-graphy (conodont biostratigraphy and δ13C) and sedi-mentology of beds 113-133 were undertaken in this study.
keywords:D-C boundary  Conodont  δ13C  Cat Ba Island  Vietnam
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