Redefinition of the Hida Gaien belt

Since the 1950s, rocks of the Hida Gaien belt have been subdivided into four units: (1) Middle to Upper Paleozoic shallow marine formations (including their metamorphosed facies of the Unazuki belt); (2) mafic to ultramafic igneous rocks including high P/T metamorphic rocks older than 300 Ma; (3) Up...

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Veröffentlicht in:Chishitsugaku zasshi 2004, Vol.110(10), pp.640-658
Hauptverfasser: Tsukada, Kazuhiro, Takeuchi, Makoto, Kojima, Satoru
Format: Artikel
Sprache:eng ; jpn
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