Stable H–C–O isotope and trace element geochemistry of the Cummins Range Carbonatite Complex, Kimberley region, Western Australia: implications for hydrothermal REE mineralization, carbonatite evolution and mantle source regions

Stable H–C–O isotope and trace element geochemistry of the Cummins Range Carbonatite Complex, Kimberley region, Western Australia: implications for hydrothermal REE mineralization, carbonatite evolution and mantle source regions

The Neoproterozoic Cummins Range Carbonatite Complex (CRCC) is situated in the southern Halls Creek Orogen adjacent to the Kimberley Craton in northern Western Australia. The CRCC is a composite, subvertical to vertical stock ∼2 km across with a rim of phlogopite–diopside clinopyroxenite surrounding...

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Bibliographic Details
Main Authors: Downes, P., Demeny, A., Czuppon, G., Jacques, A., Verrall, M., Sweetapple, M., Adams, D., McNaughton, Neal, Gwalani, L., Griffin, B.J.
Format: Journal Article
Published: Springer 2014
Subjects:
Carbonatite
H–C–Ostable isotopes
Phoscorite
Kimberley
Monazite-(Ce)
Clinopyroxenite
REEmineralization
Online Access:http://hdl.handle.net/20.500.11937/27278

Internet

http://hdl.handle.net/20.500.11937/27278

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