Isobaric cooling of two regional metamorphic complexes related to igneous intrusions in southeastern Australia

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    Abstract

    Evidence of retrograde reactions in two SE Australian low-pressure regional metamorphic complexes supports the suggestion of England and Richardson that metamorphic complexes controlled largely by magmatic intrusions should cool isobarically in the early stages. This behavior contrasts with the cooling of metamorphic complexes formed during major collision-type processes, which show evidence of marked decrease in pressure.-Author

    Original languageEnglish
    Pages (from-to)76-81
    Number of pages6
    JournalGeology
    Volume10
    Issue number2
    DOIs
    Publication statusPublished - 1982

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