Why are diamonds preserved in UHP metamorphic complexes? Experimental evidence for the effect of pressure on diamond graphitization Read more about Why are diamonds preserved in UHP metamorphic complexes? Experimental evidence for the effect of pressure on diamond graphitization
Kyanite-bearing migmatites in the central Adirondack Mountains: determining a P-T-t path and its implications on conceptual models Read more about Kyanite-bearing migmatites in the central Adirondack Mountains: determining a P-T-t path and its implications on conceptual models
Kyanite-bearing migmatites in the central Adirondack Mountains: Implications for late- to post-orogenic metamorphism and melting in a collisional orogen Read more about Kyanite-bearing migmatites in the central Adirondack Mountains: Implications for late- to post-orogenic metamorphism and melting in a collisional orogen
Kyanite-bearing migmatites at Ledge Mountain, Adirondack Highlands Read more about Kyanite-bearing migmatites at Ledge Mountain, Adirondack Highlands
Kyanite-bearing migmatites at Ledge Mountain, Adirondack Highlands Read more about Kyanite-bearing migmatites at Ledge Mountain, Adirondack Highlands
Evidence for ultrahigh-temperature (UHT) metamorphism in the Adirondack Highlands Read more about Evidence for ultrahigh-temperature (UHT) metamorphism in the Adirondack Highlands
Determining the petrotectonic evolution of Ledge Mountain migmatites with phase equilibria modeling and melt reintegration: Adirondack Highlands, New York Read more about Determining the petrotectonic evolution of Ledge Mountain migmatites with phase equilibria modeling and melt reintegration: Adirondack Highlands, New York
Kyanite-Bearing Migmatites at Ledge Mountain, Adirondack Highlands Read more about Kyanite-Bearing Migmatites at Ledge Mountain, Adirondack Highlands
Ultrahigh-temperature granulite-facies metamorphism and exhumation of deep crust in a migmatite dome during late- to post- orogenic collapse and extension in the central Adirondack Highlands (New York, USA) Read more about Ultrahigh-temperature granulite-facies metamorphism and exhumation of deep crust in a migmatite dome during late- to post- orogenic collapse and extension in the central Adirondack Highlands (New York, USA)
Microfacies of the Cotham Marble: A tubestone carbonate microbialite from the Upper Triassic, Southwestern United Kingdom. Read more about Microfacies of the Cotham Marble: A tubestone carbonate microbialite from the Upper Triassic, Southwestern United Kingdom.