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Buick, I. S., Cartwright, I., Williams, I. S. (1997) High-temperature Retrogression of Granulite-facies Marbles form the Reynolds Range Group, Central Australia: Phase Equilibria, Isotopic Resetting and Fluid Fluxes. Journal of Petrology, 38 (7) 877-910 doi:10.1093/petroj/38.7.877

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Reference TypeJournal (article/letter/editorial)
TitleHigh-temperature Retrogression of Granulite-facies Marbles form the Reynolds Range Group, Central Australia: Phase Equilibria, Isotopic Resetting and Fluid Fluxes
JournalJournal of Petrology
AuthorsBuick, I. S.Author
Cartwright, I.Author
Williams, I. S.Author
Year1997 (July 1)Volume38
Issue7
PublisherOxford University Press (OUP)
DOIdoi:10.1093/petroj/38.7.877Search in ResearchGate
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Mindat Ref. ID178895Long-form Identifiermindat:1:5:178895:6
GUID0
Full ReferenceBuick, I. S., Cartwright, I., Williams, I. S. (1997) High-temperature Retrogression of Granulite-facies Marbles form the Reynolds Range Group, Central Australia: Phase Equilibria, Isotopic Resetting and Fluid Fluxes. Journal of Petrology, 38 (7) 877-910 doi:10.1093/petroj/38.7.877
Plain TextBuick, I. S., Cartwright, I., Williams, I. S. (1997) High-temperature Retrogression of Granulite-facies Marbles form the Reynolds Range Group, Central Australia: Phase Equilibria, Isotopic Resetting and Fluid Fluxes. Journal of Petrology, 38 (7) 877-910 doi:10.1093/petroj/38.7.877
In(1997, July) Journal of Petrology Vol. 38 (7) Oxford University Press (OUP)

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BUICK, I. S., CARTWRIGHT, I. (1994) Significance of early scapolite in greenschist-facies marbles from the Reynolds Range Group, central Australia. Journal of the Geological Society, 151 (5) 803-812 doi:10.1144/gsjgs.151.5.0803
Cartwright, I., Buick, I.S ., Roland, M. (1997) Fluid flow in marbles at Jervois, central Australia: Oxygen isotope disequilibrium and zoning produced by decoupling of mineralogical and isotopic resetting,Ā Contributions of Mineralogy and Petrology, 128: pp.335 - 351.
BUICK, I. S., HARLEY, S. L., CARTWRIGHT, I., MATTEY, D. (1994) Stable isotopic signatures of superposed fluid events in granulite facies marbles of the Rauer Group, East Antarctica. Journal of Metamorphic Geology, 12 (3) 285-299 doi:10.1111/j.1525-1314.1994.tb00023.x
BUICK, IAN S., CARTWRIGHT, IAN (1996) Fluidā€”Rock Interaction during Low-Pressure Polymetamorphism of the Reynolds Range Group, Central Australia. Journal of Petrology, 37 (5) 1097-1124 doi:10.1093/petrology/37.5.1097
CARTWRIGHT, I., BUICK, I. S. (1994) Channelled fluid infiltration and variation in permeability in Reynolds Range marbles, Australia. Journal of the Geological Society, 151 (4) 583-586 doi:10.1144/gsjgs.151.4.0583
CARTWRIGHT, I., BUICK, I. S. (1995) Formation of wollastonite-bearing marbles during late regional metamorphic channelled fluid flow in the Upper Calcsilicate Unit of the Reynolds Range Group, central Australia. Journal of Metamorphic Geology, 13 (3) 397-417 doi:10.1111/j.1525-1314.1995.tb00228.x
WILLIAMS, I. S., BUICK, I. S., CARTWRIGHT, I. (2004) An extended episode of early Mesoproterozoic metamorphic fluid flow in the Reynolds Range, central Australia*. Journal of Metamorphic Geology, 14 (1) 29-47 doi:10.1111/j.1525-1314.1996.00029.x
Cartwright, Ian, Buick, Ian S., Maas, Roland (1997) Fluid flow in marbles at Jervois, central Australia: oxygen isotope disequilibrium and zoning produced by decoupling of mineralogical and isotopic resetting. Contributions to Mineralogy and Petrology, 128 (4) 335-351 doi:10.1007/s004100050313
Buick, Ian S., Frei, Robert, Cartwright, Ian (1999) The timing of high-temperature retrogression in the Reynolds Range, central Australia: constraints from garnet and epidote Pb-Pb dating. Contributions to Mineralogy and Petrology, 135 (2) 244-254 doi:10.1007/s004100050510
Buick, I.S., Cartwright, I. (1995) Fluidā€rock interaction during early contact metamorphism of the Reynolds Range Group, central Australia. Australian Journal of Earth Sciences, 42 (3) 301-310 doi:10.1080/08120099508728204
Cartwright, Ian, Buick, Ian S. (2000) Millimetre-scale variation in metamorphic permeability of marbles during transient fluid flow: an example from the Reynolds Range, central Australia. Contributions to Mineralogy and Petrology, 140 (2) 163-179 doi:10.1007/s004100000180
 
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