Response of detrital zircon and monazite, and their U-Pb isotopic systems, to regional metamorphism and host-rock partial melting, Cooma Complex, southeastern Australia
Progressive Early Silurian low-pressure greenschist to granulite facies regional metamorphism of Ordovician flysch at Cooma, southeastern Australia, had different effects on detrital zircon and monazite and their U-Pb isotopic systems. Monazite began to dissolve at lower amphibolite facies, virtually disappearing by upper amphibolite facies, above which it began to regrow, becoming most coarsely grained in migmatite leucosome and the anatectic Cooma Granodlorite. Detrital monazite U-Pb ages...[Show more]
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|Source:||Australian Journal of Earth Sciences|
|01_Williams_Response_of_detrital_zircon_2001.pdf||1.46 MB||Adobe PDF||Request a copy|
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