Late Carboniferous brachiopod Plicatiferina from Nishiamada, Fukui Prefecture, central Japan, and its tectonic implications
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- Tazawa Jun-ichi
- Department of Geology, Faculty of Science, Niigata University
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- Anso Junko
- Fukui City Museum of Natural History
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- Umeda Miyuki
- Fukui City Museum of Natural History
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- Kurihara Toshiyuki
- Graduate School of Science and Technology, Niigata University
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抄録
A new occurrence of the Late Carboniferous productoid brachiopod species, Plicatiferina borealica Kalashnikov, is described from a sequence of alternating metamorphosed limestone and subordinate metamorphosed felsic tuff, mudstone and sandstone at Nishiamada, Fukui Prefecture, central Japan. Plicatiferina is a typical Boreal-type genus, distributed in the Upper Carboniferous and lowest Permian of Arctic Canada, Arctic Russia, and the northern and southern Urals. The fossilbearing sequence at Nishiamada is assigned to the Late Carboniferous (Kasimovian?), and is correlated with the Unazuki metamorphic rocks of the Hida Belt, central Japan. The occurrence of a Boreal-type brachiopod at Nishiamada suggests that the original calcareous and volcaniclastic sediments of the Unazuki metamorphic rocks were deposited in a shallow sea on and around the eastern North China (Sino-Korea) during the Late Carboniferous.
収録刊行物
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- 地質学雑誌
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地質学雑誌 116 (1), 51-54, 2010
一般社団法人 日本地質学会
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詳細情報 詳細情報について
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- CRID
- 1390282681214067328
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- NII論文ID
- 130000254081
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- NII書誌ID
- AN00141768
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- ISSN
- 13499963
- 00167630
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- HANDLE
- 10191/26522
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- NDL書誌ID
- 10572306
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- 本文言語コード
- en
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- データソース種別
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- JaLC
- IRDB
- NDL
- Crossref
- CiNii Articles
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- 抄録ライセンスフラグ
- 使用不可