The sources of phosphorus for the phosphatic rocks in the Toyoma Formation, Northeastern Japan

スポンサーリンク

概要

• 論文の詳細を見る

• The apatite in the phosphatic rocks of the Toyoma Formation is carbonate fluorapatite highly enriched in Ce and Y. The Ce and Y enrichment of the apatite suggests that the source of phosphorus is biogenic phosphate mineral debris such as fish bones, teeth and scales rather than phosphorus-bearing organic matter. The spatially and stratigraphically limited distribution of the phosphatic rocks in the formation is in accord with this view.

• 信州大学の論文
• 2005-03-30

著者

• MORIKIYO Toshiro

  Department of Geology, Shinshu University

• Matsunaga K

  Department Of Chemistry Faculty Of Engineering Science Osaka University

• Morikiyo T

  Department Of Geology Faculty Of Science Shinshu University

• MATSUNAGA Kinuko

  Department of Geology, Faculty of Science, Shinshu University

• IWAMASA Kazuo

  Department of Geology, Faculty of Science, Shinshu University

• Iwamasa Kazuo

  Department Of Geology Faculty Of Science Shinshu University

• Matsunaga Kinuko

  Department Of Geology Faculty Of Science Shinshu University

• Iwamasa K

  Department of Geology, Faculty of Science, Shinshu University

関連論文

• Finding dolomitic melnoite diatreme at Badou in the Laiwu–Zibo area, Shandong province, China
• The sources of phosphorus for the phosphatic rocks in the Toyoma Formation, Northeastern Japan
• Variations of divalent cation concentrations in pore water and the precipitation of Mg-rich authigenic mineral during early diagenesis of Toyoma Formation
• The genesis of phosphatic and carbonate rocks in the Toyoma Formation, Northeastern Japan

スポンサーリンク