Diachronous Redistribution of Hf and Nd Isotopes at the Crystal Scale—Consequences for the Isotopic Evolution of a Poly-Metamorphic Crustal Terrane

Diachronous Redistribution of Hf and Nd Isotopes at the Crystal Scale—Consequences for the Isotopic Evolution of a Poly-Metamorphic Crustal Terrane

In metamorphic rocks, mineral species react over a range of pressure–temperature conditions that do not necessarily overlap. Mineral equilibration can occur at varied points along the metamorphic pressure–temperature (PT) path, and thus at different times. The sole or dominant use of zircon isotopic...

Full description

Bibliographic Details
Main Authors: Adrien Vezinet, Emilie Thomassot, Yan Luo, Chiranjeeb Sarkar, D. Graham Pearson
Format: Article
Language:English
Published: MDPI AG 2022-01-01
Series:Geosciences
Subjects:
apatite U–Pb/Sm–Nd isotopes
metamorphism
Archean Saglek
Hf–Nd decoupling
Online Access:https://www.mdpi.com/2076-3263/12/1/36

Similar Items

Similar Items