佐賀県東松浦半島産ゴンナルダイト

  • 上野 禎一
    Department of Earth Sciences, Fukuoka University of Education
  • 小田 長年
    Department of Earth Sciences, Fukuoka University of Education
  • 鞭 政共
    Department of Earth Sciences, Fukuoka University of Education

書誌事項

タイトル別名
  • Gonnardite from Higashi-Matsuura Peninsula, Saga Prefecture, Japan.

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説明

Gonnardites found in the altered hydrothermal veins or druses in the Higashi-Matsuura basaltic rocks have cell parameters a=13.45 Å, b=13.42 Å and c=6.67 Å ; the chemical composition determined by Electron probe micro-analyser, (Na, Ca, K)3, 62(Al, Si)10.05O20•5.47 H2O. By heating at 350°C for one hour, the mineral turned to amorphous state and by heating at 900°C for one hour, it changed to nepheline, with cell parameters a=9.978 Å and c=8.365 Å (hexagonal system) and chemical composition determined by Electron probe micro-analyser K0.02Na4.45(Ca, Mg, Al)1.18[Si9.09Al6.91O32]. The DTA curve shows a large sharp endothermic peak at 345°C and an exsothermic peak at 940°C. The former is due to the dehydration of structural water and the latter to the formation of nepheline. The infra-red absorption spectrum shows absorption bands at 3600, 3400, 1640 and 1000 cm-1.

収録刊行物

詳細情報 詳細情報について

  • CRID
    1390001206217123712
  • NII論文ID
    130003728454
  • DOI
    10.2465/ganko1941.77.78
  • ISSN
    18830765
    00214825
  • 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

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