Looping P-T paths and high-T, low-P middle crustal metamorphism: Proterozoic evolution of the southwestern United States

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Department of Geosciences, University of Massachusetts, Amherst, MA 01003, United States ^{[1
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Geology | / 12卷 / 1119-1122期

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[21] The Mangaroon Orogeny: Synchronous c. 1.7 Ga magmatism and low-P, high-T metamorphism in the West Australian Craton
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[22] Palaeoproterozoic high-T, low-P metamorphism and dehydration melting in metapelites from the Mopunga Range, Arunta Inlier, central Australia
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[23] Problems with inferring P-T-t paths in low-P granulite facies rocks
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[27] The Ryoke metamorphic belt (Japan): An excellent example of low-P/high-T metamorphic belt
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[28] DECOMPRESSION REACTIONS AND P-T CONDITIONS IN HIGH-GRADE ROCKS, NORTHERN LABRADOR - P-T-T PATHS FROM INDIVIDUAL-SAMPLES AND IMPLICATIONS FOR EARLY PROTEROZOIC TECTONIC EVOLUTION
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