Zircon geochronology and Hf–O isotopes of the Nulliak supracrustal assemblage (Saglek Block–Canada): Constraints on deposition age and setting, metamorphic age and environments of zircon crystallization-Reference-Cited by-同舟云学术

Zircon geochronology and Hf–O isotopes of the Nulliak supracrustal assemblage (Saglek Block–Canada): Constraints on deposition age and setting, metamorphic age and environments of zircon crystallization

Published:2022-09 Issue: Volume:379 Page:106789
ISSN:0301-9268
Container-title:Precambrian Research
language:en
Short-container-title:Precambrian Research

Author:

Vezinet A.,Thomassot E.,Luo Y.,Pearson D.G.,Stern R.A.,Sarkar C.

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference102 articles.

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4. The Archean gneiss complex of northern labrador. 1. preliminary U-Th–Pb geochronology;Baadsgaard;Can. J. Earth Sci.,1979

5. Early Archean crustal evolution of the Jack Hills Zircon source terrane inferred from Lu–Hf, 207Pb/206Pb, and δ18O systematics of Jack Hills zircons;Bell;Geochim. Cosmochim. Acta,2011

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1. Depositional age and provenance of metasedimentary rocks from the Hengshan Complex, North China Craton: Implications for the late Neoarchean to early Paleoproterozoic tectonic setting of the Trans-North China Orogen;Precambrian Research;2024-05

2. Mechanisms for generating elevated zircon δ18O in Archean crust: Insights from the Saglek-Hebron Complex, Canada;Earth and Planetary Science Letters;2023-12