Biogeochemical signatures preserved in ancient siliceous sediments ; new perspectives to Triassic radiolarian bedded chert compositions
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概要
- 論文の詳細を見る
- Geochemical Society of Japanの論文
- 2006-02-01
著者
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SUZUKI Kazuhiro
Center for Chronological Research, Nagoya University
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Sugitani Kenichiro
Graduate School of Environmental Studies, Nagoya University
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Yamamoto Koshi
Graduate School Of Environmental Studies Nagoya University
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Takiguchi Toru
Graduate School Of Human Informatics Nagoya University
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Sugitani Kenichiro
Graduate School Of Environmental Studies Nagoya University
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Suzuki Kazuhiro
Center For Chronological Research Nagoya University
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Suzuki Kazuhiro
Center For Geochronological Research Nagoya University
関連論文
- Protocol and pitfalls of CHIME dating(Proceedings of the 19^ Symposium on Chronological Studies at the Nagoya University Center for Chronological Research in 2006,Part1)
- Gully erosion in Western Kenya
- Timing of the landslide-damming at Anegawa upstream, Shiga Prefecture : revealed by AMS ^C dating(Proceedings of the 19^ Symposium on Chronological Studies at the Nagoya University Center for Chronological Research in 2006,POSTER SESSION)
- Age mapping of young monazite and zircon(Proceedings of the 19^ Symposium on Chronological Studies at the Nagoya University Center for Chronological Research in 2006,POSTER SESSION)
- Database for geochemical mapping of the northeastern areas of Aichi Prefecture, central Japan ^ XRF major element data of stream sediments collected in 1994 to 2004 -
- Permo-Triassic and Early-Middle Jurassic granitoid clasts from the Jurassic conglomerates in the Mino terrane, central Japan
- CHIME ages of Mg-rich garnet-bearing gneiss clasts from the Jurassic Sawando conglomerate in the northeastern Mino terrane, central Japan
- Biogeochemical signatures preserved in ancient siliceous sediments ; new perspectives to Triassic radiolarian bedded chert compositions
- Jadeite-quartz-K-feldspar rocks in the Kamuikotan zone, Japan
- Dissolution processes of elements from subducting sediments into fluids : Evidence from the chemical composition of the Sanbagawa pelitic schists