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HARLEY, S. L. (1985) Garnet-Orthopyroxene Bearing Granulites from Enderby Land, Antarctica: Metamorphic Pressure Temperature-Time Evolution of the Archaean Napier Complex. Journal of Petrology, 26 (4) 819-856 doi:10.1093/petrology/26.4.819

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Reference TypeJournal (article/letter/editorial)
TitleGarnet-Orthopyroxene Bearing Granulites from Enderby Land, Antarctica: Metamorphic Pressure Temperature-Time Evolution of the Archaean Napier Complex
JournalJournal of Petrology
AuthorsHARLEY, S. L.Author
Year1985 (November 1)Volume26
Issue4
PublisherOxford University Press (OUP)
DOIdoi:10.1093/petrology/26.4.819Search in ResearchGate
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Mindat Ref. ID179713Long-form Identifiermindat:1:5:179713:2
GUID0
Full ReferenceHARLEY, S. L. (1985) Garnet-Orthopyroxene Bearing Granulites from Enderby Land, Antarctica: Metamorphic Pressure Temperature-Time Evolution of the Archaean Napier Complex. Journal of Petrology, 26 (4) 819-856 doi:10.1093/petrology/26.4.819
Plain TextHARLEY, S. L. (1985) Garnet-Orthopyroxene Bearing Granulites from Enderby Land, Antarctica: Metamorphic Pressure Temperature-Time Evolution of the Archaean Napier Complex. Journal of Petrology, 26 (4) 819-856 doi:10.1093/petrology/26.4.819
In(1985, November) Journal of Petrology Vol. 26 (4) Oxford University Press (OUP)

See Also

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HARLEY, S. L., HENSEN, B. J., SHERATON, J. W. (1990) Two-stage decompression in orthopyroxene?sillimanite granulites from Forefinger Point, Enderby Land, Antarctica: implications for the evolution of the Archaean Napier Complex. Journal of Metamorphic Geology, 8 (6) 591-613 doi:10.1111/j.1525-1314.1990.tb00490.x
ELLIS, D. J., GREEN, D. H. (1985) Garnet-forming Reactions in Mafic Granulites from Enderby Land, Antarctica--Implications for Geothermometry and Geobarometry. Journal of Petrology, 26 (3) 633-662 doi:10.1093/petrology/26.3.633
HARLEY, SIMON L. (1987) A pyroxene-bearing meta-ironstone and other pyroxene-granulites from Tonagh Island, Enderby Land, Antarctica: further evidence for very high temperature (> 980°C) Archaean regional metamorphism in the Napier Complex. Journal of Metamorphic Geology, 5 (3) 341-356 doi:10.1111/j.1525-1314.1987.tb00389.x
BRANDT, S. (2003) Ultrahigh-Temperature Metamorphism and Multistage Evolution of Garnet-Orthopyroxene Granulites from the Proterozoic Epupa Complex, NW Namibia. Journal of Petrology, 44 (6) 1121-1144 doi:10.1093/petrology/44.6.1121
HARLEY, S. L. (1988) Proterozoic Granulites from the Rauer Group, East Antarctica. I. Decompressional Pressure-Temperature Paths Deduced from Mafic and Felsic Gneisses. Journal of Petrology, 29 (5) 1059-1095 doi:10.1093/petrology/29.5.1059
SANDIFORD, MICHAEL (1985) The metamorphic evolution of granulites at Fyfe Hills; implications for Archaean crustal thickness in Enderby Land, Antarctica. Journal of Metamorphic Geology, 3 (2) 155-178 doi:10.1111/j.1525-1314.1985.tb00312.x
Harley, S. L. (1986) A sapphirine-cordierite-garnet-sillimanite granulite from Enderby Land, Antarctica: implications for FMAS petrogenetic grids in the granulite facies. Contributions to Mineralogy and Petrology, 94 (4) 452-460 doi:10.1007/bf00376338
Kelly, N.,M., Harley, S.L. (2004) Orthopyroxene–Corundum in Mg–Al-rich Granulites from the Oygarden Islands, East Antarctica. Journal of Petrology, 45(7), 1481-1512.
HARLEY, S. L. (1984) Comparison of the Garnet--Orthopyroxene Geobarometer with Recent Experimental Studies, and Applications to Natural Assemblages. Journal of Petrology, 25 (3) 697-712 doi:10.1093/petrology/25.3.697
DROOP, G. T. R., BUCHER-NURMINEN, K. (1984) Reaction Textures and Metamorphic Evolution of Sapphirine-bearing Granulites from the Gruf Complex, Italian Central Alps. Journal of Petrology, 25 (3) 766-803 doi:10.1093/petrology/25.3.766
GREW, EDWARD S., YATES, MARTIN G., SHEARER, CHARLES K., HAGERTY, JUSTIN J., SHERATON, JOHN W., SANDIFORD, MICHAEL (2006) Beryllium and Other Trace Elements in Paragneisses and Anatectic Veins of the Ultrahigh-Temperature Napier Complex, Enderby Land, East Antarctica: the Role of Sapphirine. Journal of Petrology, 47 (5) 859-882 doi:10.1093/petrology/egi098
 
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