Prolonged (>100 Ma) ultrahigh temperature metamorphism in the Napier Complex, East Antarctica: A petrochronological investigation of Earth's hottest crust
Author:
Affiliation:
1. School of Earth and Planetary Sciences Curtin University Perth WA Australia
2. Department of Earth Sciences University of Cambridge Cambridge UK
3. Department of Earth Science University of California, Santa Barbara Santa Barbara CA USA
Funder
Division of Earth Sciences
Australian Research Council
University of California, Santa Barbara
Publisher
Wiley
Subject
Geochemistry and Petrology,Geology
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1111/jmg.12430
Reference101 articles.
1. Conservation of deep crustal heat production;Alessio K. L.;Geology,2018
2. Abundances of the elements: Meteoritic and solar
3. Chemical Th–U–total Pb dating by electron microprobe analysis of monazite, xenotime and zircon from the Archean Napier Complex, East Antarctica: evidence for ultra-high-temperature metamorphism at 2400 Ma
4. First application of titanium-in-zircon thermometry to ultrahigh-temperature metamorphism
5. The sources of energy for crustal melting and the geochemistry of heat-producing elements
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