Mechanisms for generating elevated zircon δ18O in Archean crust: Insights from the Saglek-Hebron Complex, Canada-Reference-Cited by-同舟云学术

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Mechanisms for generating elevated zircon δ18O in Archean crust: Insights from the Saglek-Hebron Complex, Canada

Published:2023-12 Issue: Volume:624 Page:118443
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Mixon Emily E.^ORCID,Bauer Ann M.^ORCID,O'Neil Jonathan,Rizo Hanika,Blum Tyler B.^ORCID,Valley John W.,Bonamici Chloë E.^ORCID

Funder

Horizon 2020

National Science Foundation

College of Engineering, University of Wisconsin-Madison

European Research Council

Natural Sciences and Engineering Research Council of Canada

Publisher

Elsevier BV

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference78 articles.

1. Lateral growth of the continental crust through deep level subduction–accretion: a re-evaluation of central Greek Rhodope;Barr;Lithos,1999

2. Hafnium isotopes in zircons document the gradual onset of mobile-lid tectonics;Bauer;Geochem. Perspect. Lett.,2020

3. Recovering the primary geochemistry of Jack Hills zircons through quantitative estimates of chemical alteration;Bell;Geochim. Cosmochim. Acta,2016

4. Stability of zircon and its isotopic ratios in high temperature fluids: long-term (4 months) isotope exchange experiment at 850 °C and 50 MPa;Bindeman;Front. Earth Sci.,2018

5. Triple oxygen isotopes in evolving continental crust, granites, and clastic sediments;Bindeman;Rev. Mineral. Geochem.,2021

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