書誌事項
- タイトル別名
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- Radiolarian and fusuline fossils from oceanic rocks in the Ashio Terrane of the Kambara Massif, Niigata Prefecture, Southwest Japan
- ニイガタケン カンバラ サンチ ノ アシオタイ カイヨウセイ ガンセキ カラ ミイダサレタ ホウサンチュウ ボウスイチュウ カセキ
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Radiolarian and fusuline fossils were discovered respectively from chert and limestone blocks in the Ashio Terrane of the Kambara Massif, Southwest Japan. Radiolarians in gray bedded chert indicate an age of late Middle Permian (Capitanian) to early Late Permian (Wuchiapingian), and those in black massive chert indicate a latest Permian (Changhsingian) age. This is the first report of Late Permian oceanic rocks in the Kambara Massif. Fusulines in a piece of limestone float indicate a latest Carboniferous (Kasimovian and late Gzhelian) age. This limestone is probably the same as that reported in a previous study, broadly inferred to be Late Carboniferous to Early Permian in age. Therefore, the age of the limestone is now well constrained. These fossil data are important in reconstructing the oceanic plate stratigraphy of the Ashio Terrane of the Kambara Massif.
収録刊行物
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- 地質学雑誌
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地質学雑誌 116 (2), 118-123, 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
- 1390001206238667264
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- NII論文ID
- 130000413229
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- NII書誌ID
- AN00141768
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- ISSN
- 13499963
- 00167630
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- NDL書誌ID
- 10602435
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- 本文言語コード
- ja
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- データソース種別
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- JaLC
- NDL
- Crossref
- CiNii Articles
- KAKEN
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- 抄録ライセンスフラグ
- 使用不可
