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The Shimokawa ophiolite was probably generated at a RTT triple junction (I-3-26 O-11)(abs.)
MIYASHITA Sumio
itemdescription
TitleThe Shimokawa ophiolite was probably generated at a RTT triple junction (I-3-26 O-11)(abs.)
AuthorsMIYASHITA Sumio
Data nameAbstracts, 29th International Geological Congress
Volume1
Page134-134
Year1992
PublisherInternational Geological Congress (IGC)
LanguageEN
GEOLIS URLhttps://darc.gsj.jp/archives/detail?cls=geolis&pkey=199204319
@idhttps://gbank.gsj.jp/ld/resource/geolis/199204319