鹿児島県高隈山地の時代未詳層群中に発達する千枚岩帯(予報)

• 河内 洋佑

  地質調査所地質部

書誌事項

タイトル別名

• On the Low Grade Regional Metamorphic Zone developed in Takakuma-yama, Osumi Peninsula, Southern Kyushu(Preliminary Report)
• 鹿児島県高隈山地の時代未詳層群中に発達する千板岩帯-予-
• カゴシマケン コウクマ サンチ ノ ジダイ ミショウ ソウグン チュウ ニ ハッタツ スル センバンガンタイ ヨ

抄録

In the so-called unknown Mesozoic formations (Shimanto-gawa complex) around Takakuma-yama, phyllitec rocks are regionally developed. They are derived mainly from the pelitic and the alternations of pelitic and psammitic rocks, and also the basic tuffaceous rocks, through intense flattening with or without differential movement. This zone of phyllites is probably the southward extension of the phyllite zone along Nobeoka-Shibisan Tectonic Line in Central Kyushu. From the modes of occurrence of the phyllites, especially from its regional extent, these are not the products of mere faulting but are thought to represent the regional metamorphism through Alpine orogenic movement in the outermost terrain of the Outer Zone of Southwestern Japan as recently suggested by N, YAMASHITA (1960). I propose the name "Takakuma-yama regional metamorphic zone" for this zone of phyllites. Among several characteristic features reckoned in this zone, intimate distributional relation of the post-kinematic granitic stocks with this zone is stressed.

収録刊行物

• 地球科学

  地球科学 1962 (58), 18-25, 1962

  地学団体研究会

詳細情報

• CRID: 1390001204266896128
• NII論文ID: 110007157010
• NII書誌ID: AN00141269
• DOI: 10.15080/agcjchikyukagaku.1962.58_18
• ISSN: 21897212
• ISSN: 03666611
• NDL書誌ID: 9103974
• Web Site: https://ndlsearch.ndl.go.jp/books/R000000004-I9103974
• 本文言語コード: ja
• データソース種別:
  • JaLC
  • NDL
  • CiNii Articles
• 抄録ライセンスフラグ: 使用不可