Timing of anatexis in the Hidaka metamorphic belt, Hokkaido, Japan

M. Owada, Yasuhito Osanai, H. Kagami

Research output: Contribution to journalArticle

12 Citations (Scopus)

Abstract

The Sr isotope compositions of pelitic granulites and S-type granitic rocks were measured, and a whole rock isochron age from these rocks is given, with a short discussion on its implication for the evolution of the granulite-facies metamorphism and the genesis of the S-type granitic magma in the Main Zone of the Hidaka metamorphic belt. -from Authors

Original languageEnglish
Pages (from-to)751-754
Number of pages4
JournalJournal - Geological Society of Japan
Volume97
Issue number9
DOIs
Publication statusPublished - Jan 1 1991
Externally publishedYes

Fingerprint

anatexis
S-type rock
Rocks
granulite facies
rock
metamorphism
magma
isotope
Isotopes
Chemical analysis

All Science Journal Classification (ASJC) codes

  • Environmental Science(all)
  • Engineering(all)
  • Earth and Planetary Sciences(all)

Cite this

Timing of anatexis in the Hidaka metamorphic belt, Hokkaido, Japan. / Owada, M.; Osanai, Yasuhito; Kagami, H.

In: Journal - Geological Society of Japan, Vol. 97, No. 9, 01.01.1991, p. 751-754.

Research output: Contribution to journalArticle

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