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Title Transcription
オキト ドウゴ トウブ ニ ブンプ スル トキバリヤマ ルイソウ オヨビ グンルイソウ ノ ソウジョ ト コウゾウ
Title Alternative (English)
The Tokibariyama and Kori Formations in the eastem part of the Oki-Dogo Island
File
language
jpn
Author
Yamamoto, Hiroki
Komuro, Hiroaki
Murakami, Hisashi
Description
The Tokibariyama Formation of Oligocene is divided into the Uzuki Rhyolitic and Oku Andesitic Members in ascending order.These members consit mainly of rhyolitic pyroclastic rocks and andesite lavas,respectively.Some thin beds of sandstone or conglomerate are intercalated.This formation generally strikes NE~NNE and dips eastward.The Kori Formation of Miocene unconformably covering the Tokibariyama Formation consists of acidic tuff,sandstone,conglomerate and basalt lava.
These formations are cut by NNE-SSW~NE−SW and NW-SE faults and are bended due to the NESW monocline.This monocline continues to the NW-SE fault southward.Some dikes intrude concordantly with these faults.
Journal Title
島根大学地球資源環境学研究報告
Volume
14
Start Page
101
End Page
108
ISSN
13439774
Published Date
1995-12-25
NCID
AA11455176
DOI(SelfDOI)
Publisher
島根大学総合理工学部地球資源環境学教室
Publisher Aalternative
Department of Geoscience, Interdisciplinary Faculty of Science and Engineering, Shimane University
NII Type
Departmental Bulletin Paper
Format
PDF
Text Version
出版社版
OAI-PMH Set
Interdisciplinary Graduate School of Science and Engineering
Remark
12-14,16+ / 1993+
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