U-Pb isotopic behaviour of zircon during upper-amphibolite facies fluid infiltration in the Napier Complex, east Antarctica
Understanding the factors that contribute to U-Pb discordance in zircon is essential for interpreting isotopic data and for assessing the validity of concordia intercept ages. Modification caused by interaction with metamorphic fluids is often cited as a
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|Source:||Earth and Planetary Science Letters|
|01_Carson_U-Pb_isotopic_behaviour_of_2002.pdf||1.43 MB||Adobe PDF||Request a copy|
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