Confirmation of the Permian/Triassic boundary in deep-sea sedimentary rocks : earliest Triassic conodonts from black carbonaceous claystone of the Ubara section in the Tamba Belt, Southwest Japan
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概要
- 論文の詳細を見る
We found earliest Triassic (Griesbachian) conodont, Hindeodus parvus, from the basal part of the black carbonaceous claystone of the Ubara Permian/Triassic boundary section in the Tamba Belt. We also obtained Late Permian (Changxingian) conodonts from the underlying gray siliceous claystone as already reported from other P/T boundary sections. The lithologic boundary between the gray siliceous claystone and the black carbonaceous claystone is confirmed to be the Permian/Triassic boundary in deep-sea sedimentary rocks.
- 日本地質学会の論文
- 1999-12-15
著者
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Tada Ryuji
Geological Institute Graduate School Of Science University Of Tokyo
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Tada R
Univ. Tokyo Tokyo Jpn
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Tada Ryuji
Geological Institute Graduate School Of Science The University Of Tokyo.
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Kato Takuya
Geological Institute Graduate School Of Science University Of Tokyo
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Yamakita Satoshi
Department of Earth Sciences, Faculty of Education and Culture, Miyazaki University
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Kadota Naoki
Graduate School of Education, Miyazaki University
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Ogihara Shigenori
Geological Institute, Graduate School of Science, University of Tokyo
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Tajika Eiichi
Geological Institute, Graduate School of Science, University of Tokyo
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Hamada Yoshitaka
Geological Institute, Graduate School of Science, University of Tokyo
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Ogihara Shigenori
Geological Institute Graduate School Of Science University Of Tokyo
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Kadota Naoki
Graduate School Of Education Miyazaki University
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Tajika Eiichi
Geological Institute School Of Science University Of Tokyo
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Hamada Yoshitaka
Geological Institute Graduate School Of Science University Of Tokyo
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Yamakita Satoshi
Department Of Earth Sciences Faculty Of Education And Culture Miyazaki University
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Yamakita Satoshi
Department of Earth Science, Faculty of Education and Culture, Miyazaki University
関連論文
- Confirmation of the Permian/Triassic boundary in deep-sea sedimentary rocks : earliest Triassic conodonts from black carbonaceous claystone of the Ubara section in the Tamba Belt, Southwest Japan
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