紀伊半島北部の中新世石仏凝灰岩部層の火砕性堆積物

• 佐藤 隆春

  大阪市立自然史博物館

• 鈴木 桂子

  神戸大学大学院理学研究科地球惑星科学専攻

• 和田 穣隆

  奈良教育大学地学教室

• 中条 武司

  大阪市立自然史博物館

書誌事項

タイトル別名

• Volcaniclastic rocks of the Miocene Sekibutsu Tuff Member in the northern Kii Peninsula, central Japan
• キイ ハントウ ホクブ ノ チュウシンセイ セキブツ ギョウカイガンブソウ ノ カサイセイ タイセキブツ

抄録

The Miocene Sekibutsu Tuff Member at Nara, central Honshu, Japan, consists mainly of pyroclastic flow deposits and reworked volcaniclastic deposits. The pyroclastic flow deposits, which could have been deposited at some distance from the source calderas, occur in the lower part of the member and are subdivided into three units based on pumice content and size (in ascending order: units L1, L2, and L3). Unit L1 consists of several layers of lapilli tuff and tuff breccia interbedded with thin layers of sandstone and mudstone. The matrix of the tuff breccia includes sand-sized mudstone clasts, and the breccia contains an irregularly lens-shaped pumice-rich zone that is several meters wide. Unit L2 consists of massive tuff with a small amount of lapilli-sized pumice. Unit L3 comprises lapilli tuff and lithofacies similar to those of unit L1. Reworked volcaniclastic deposits constitute the upper part of the member. The deposits are unconformably overlain by pyroclastic flow deposits.

収録刊行物

• 地質学雑誌

  地質学雑誌 121 (6), 173-178, 2015-06-10

  一般社団法人 日本地質学会

キーワード

• Pyroclastic-flow deposits
• reworked-volcaniclastic deposits
• Miocene
• Kii Peninsula
• The Sekibutsu Tuff Member

詳細情報

• CRID: 1390001206241482240
• NII論文ID: 130005089847
• NII書誌ID: AN00141768
• DOI: 10.5575/geosoc.2015.0017
• ISSN: 13499963
• ISSN: 00167630
• NDL書誌ID: 026604785
• Web Site: http://id.ndl.go.jp/bib/026604785
• Web Site: https://ndlsearch.ndl.go.jp/books/R000000004-I026604785
• Web Site: https://www.jstage.jst.go.jp/article/geosoc/121/6/121_2015.0017/_pdf
• 本文言語コード: ja
• データソース種別:
  • JaLC
  • NDL
  • Crossref
  • CiNii Articles
  • KAKEN
• 抄録ライセンスフラグ: 使用不可