ID 105967
Title Transcription
シコク セイブ チチブタイ トリガタヤマ オオノガハラ セッカイ ガンタイ ト シンキ イノ ヘンセイ コンプレックス ノ チシツ コウゾウ
Title Alternative
Geological structures of the Torigatayama-Onogahara limestone and the Younger Ino metamorphic complex of the Chichibu Terrain, West Shikoku
Author
Murata, Akihiro Institute of Socio-Arts and Sciences, University of Tokushima Tokushima University Educator and Researcher Directory KAKEN Search Researchers
Maekawa, Hirokazu Department of Physical Science, Graduate School of Science, Osaka Prefectural University
Keywords
Torigatayama-Onogahara limestone
geological structures
Younger Ino metamorphic complex
Kurosegawa Terrain
Chichibu Terrain
Shikoku
Content Type
Departmental Bulletin Paper
Description
Geological structures of the Torigatayama-Onogahara limestone body of the Permian accretionary complex and the Younger Ino metamorphic complex were studied in the Chichibu Terrain in West Shikoku. The Torigatayama-Onogahara limestone body consists of six limestone bodies, which occur in a convex way toward south. The limestone bodies are northward facing and form southward thrust sheet, and do not occur in the axial part of a synform. An antiform and a synform occur in the distributional area of the Younger Ino metamorphic complex. The antiform does not extend westward to the distributional area of the Yusugawa Unit of the Jurassic accretionary complex. The Permian accretionary complex and the Younger Ino metamorphic complex do not occupy the highest tectonic horizon in the Chichibu Terrain in West Shikoku.
Journal Title
徳島大学総合科学部自然科学研究 = Natural Science Research, The University of Tokushima
ISSN
09146385
NCID
AN10065859
Volume
27
Issue
4
Start Page
89
End Page
98
Sort Key
89
Published Date
2013-10
EDB ID
FullText File
language
jpn
TextVersion
Publisher
departments
Science and Technology