Deformation-enhanced recrystallization of titanite drives decoupling between U-Pb and trace elements

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Deformation-enhanced recrystallization of titanite drives decoupling between U-Pb and trace elements

Titanite is a common accessory mineral that is useful in determining both age (U-Pb isotopes) and pressure-temperature (P–T) conditions (trace-element composition: Zr, rare earth elements (REE)). However, titanite has a propensity to recrystallize during metamorphism, fluid flow, and deformation, wh...

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Bibliographic Details
Main Authors:	Gordon, S.M., Kirkland, Chris, Reddy, Steven, Blatchford, H.J., Whitney, D.L., Teyssier, C., Evans, Noreen, McDonald, B.J.
Format:	Journal Article
Language:	English
Published:	ELSEVIER 2021
Subjects:	Science & Technology Physical Sciences Geochemistry & Geophysics titanite U-Pb geochronology trace elements deformation UHP terrane petrochronology
Online Access:	http://purl.org/au-research/grants/arc/DP160104637 http://hdl.handle.net/20.500.11937/91487

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