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

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

Internet

http://purl.org/au-research/grants/arc/DP160104637
http://hdl.handle.net/20.500.11937/91487

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