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Stable (H,O, C) and noble-gas (He and Ar) isotopic compositions from calcite and fluorite in the Speewah Dome,Kimberley Region,Western Australia: implications for the conditions of crystallization and evidence for the influence of crustal-mantle fluid mixing
Authors:Gy Czuppon  R R Ramsay  I Özgenc  A Demény  L G Gwalani  K Rogers  A Eves  L Papp  L Palcsu  M Berkesi  P J Downes
Institution:1. Institute for Geological and Geochemical Research, Research Centre for Astronomy and Earth Sciences, Hungarian Academy of Sciences, Buda?rsi út 45, Budapest, 1112, Hungary
2. C/- Trident Capital Ltd, Level 24, 44 St Georges Tce, Perth, 6000, Australia
3. Department of Geology, Tinaztepe Campus, Dokuz Eylul University, 35160 – Buca, Izmir, Turkey
4. Speewah Research Project C/- King River Copper Limited, B-26/122 Mounts Bay Road, Perth, WA, 6000, Australia
5. Centre for Exploration Targeting, ARC Centre for Core to Crust Fluid Systems, University of Western Australia, Crawley, Western Australia, 6009, Australia
6. Hertelendi Laboratory of Environmental Studies of the Institute of Nuclear Research of the Academy of Sciences, Bem tér 18/C, Debrecen, H-4026, Hungary
7. Lithosphere Fluid Research Lab, Department of Petrology and Geochemistry, Institute of Geography and Earth Sciences, E?tv?s University, Pázmány P. stny 1/C, Budapest, 1117, Hungary
8. Department of Earth and Planetary Sciences, Western Australian Museum, Locked Bag 49, Welshpool DC, WA, 6986, Australia
Abstract:
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