鹿児島県西之表市の形之山層に産する硫黄含有リンカイ石

• 富田 克利

  Institute of Earth Sciences, Faculty of Science, Kagoshima University

• 河野 元治

  Department of Environmental Sciences and Technology, Faculty of Agriculture, Kagoshima University

• 白木 康一

  Institute of Earth Sciences, Faculty of Science, Kagoshima University

• 大塚 裕之

  Institute of Earth Sciences, Faculty of Science, Kagoshima University

書誌事項

タイトル別名

• Sulfatian apatite from the Katanoyama Formation in Nishino-omote City, Kagoshima Prefecture.

抄録

Sulfatian apatite occurs as small blocks in the siltstone of the Katanoyama Formation in Nishino-omote City. It is hard and appears to be a nodule of siltstone. Mineralogical data including crystal structure for the sulfatian apatite were obtained. The occurrence of sulfatian apatite in the Katanoyama Formation suggests that the siltstone was deposited together with many mammals and fish bones, and the sulfatian apatite was probably formed by the reaction between the mammals and/or fish bones and the silt or mud due to diagenesis after sedimentation.

収録刊行物

• 岩鉱

  岩鉱 91 (1), 11-20, 1996

  一般社団法人　日本鉱物科学会

キーワード

• Sulfatian apatite
• Melanterite
• The Katanoyama Formation
• Pyrite
• Crystal structure

詳細情報

• CRID: 1390001206235201280
• NII論文ID: 130004493586
• DOI: 10.2465/ganko.91.11
• COI: 1:CAS:528:DyaK28XhsFWlsbw%3D
• ISSN: 18813275
• ISSN: 09149783
• 本文言語コード: en
• データソース種別:
  • JaLC
  • Crossref
  • CiNii Articles
• 抄録ライセンスフラグ: 使用不可