ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
日本西南部四国增生复合体中的锰矿分布
  
关键词:Manganese deposit  Accretionary complex  Shikoku  Metamorphism  Deep-sea manganese nodule/crust
基金项目:
作者单位E-mail
Masaharu NAKAGAWA Department of Natural Science, Faculty of Science, Kochi University mnakagaw@kochi-u.ac.jp 
摘要点击次数: 2335
全文下载次数: 4846
摘要:
Manganese Deposits Distributed in the Accretionary Complexes of Shikoku, Southwest Japan
      Bedded manganese ore deposits occur in many localities within the accretionary belts of the Shikoku region, SW Japan. The deposits occur mostly in bedded chert or its metamorphosed equivalent. These chert-hosted manganese deposits are considered to have been manganese nodule/crust-bearing siliceous sediments on deep-sea floor and have been converted to manganese ores by low-grade metamorphism through subduction-accretion process. The mineral assemblages of the ores reflect the metamorphic grade of the accretionary complexes. On the other hand, iron-manganese deposits and some manganese deposits occurring directly over basalt are considered to have been the hydrothermal precipitates associated with submarine volcanism.
Masaharu NAKAGAWA.2012.Manganese Deposits Distributed in the Accretionary Complexes of Shikoku, Southwest Japan[J].Acta Geoscientica Sinica,33(s1):50-54.
查看全文  查看/发表评论  下载PDF阅读器
Copyright©2008 All Rights Reserved
Sponsored by:
Address:: PostCode: Tel: E-mail: