Decoupling between Ti‐in‐zircon and Zr‐in‐rutile thermometry during ultrahigh temperature metamorphism of the Dabie Orogen, China
Author:
Affiliation:
1. School of Earth SciencesChina University of Geosciences Wuhan China
2. School of Earth SciencesEast China University of Technology Nanchang China
Funder
National Natural Science Foundation of China
Publisher
Wiley
Subject
Geology
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1002/gj.3819
Reference47 articles.
1. Geochronology and isotopic character of ultrahigh-pressure metamorphism with implications for collision of the Sino-Korean and Yangtze cratons, central China
2. First application of titanium-in-zircon thermometry to ultrahigh-temperature metamorphism
3. What can we learn from melt inclusions in migmatites and granulites?
4. Trace element systematics of granulite‐facies rutile;Chen Y.;Earth Science,2018
5. Zr-in-rutile thermometry in eclogite and vein from southwestern Tianshan, China
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1. Current applications using key mineral phases in igneous and metamorphic geology: perspectives for the future;Geological Society, London, Special Publications;2023-05-31
2. The provenance of late Cenozoic East Asian Red Clay: Tectonic-metamorphic history of potential source regions and a novel combined zircon-rutile approach;Earth-Science Reviews;2022-02
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