Geological Literature Search (GEOLIS) (Geological Survey of Japan / AIST)

Deformation in the North Fossa Magna and Omine Terrane, and tilting uplif of the Hida Mountain Ranges resulted from contraction tectonics (S1-O-4)(abs.)

Authors=HARAYAMA Satoru

Journal/Book_names=Abstracts, the 122nd Annual Meeting of the Geological Society of Japan

volume=122

pages=3-3

Publish_year=2015

Publish_Country=JPN

Publisher=Geological Society of Japan

Language_of_Text=JA

ISSN=13483935

DOI=10.14863/geosocabst.2015.0_004

ID=201550004

@id=https://gbank.gsj.jp/ld/resource/geolis/201550004