Highly Siderophile Elements and Coupled Fe-Os Isotope Signatures in the Temagami Iron Formation, Canada: Possible Signatures of Neoarchean Seawater Chemistry and Earth's Oxygenation History-Reference-Cited by-同舟云学术

Highly Siderophile Elements and Coupled Fe-Os Isotope Signatures in the Temagami Iron Formation, Canada: Possible Signatures of Neoarchean Seawater Chemistry and Earth's Oxygenation History

Published:2021-08-01 Issue:8 Volume:21 Page:924-939
ISSN:1531-1074
Container-title:Astrobiology
language:en
Short-container-title:Astrobiology

Author:

Schulz Toni¹²^ORCID,Viehmann Sebastian³,Hezel Dominik C.²,Koeberl Christian¹,Bau Michael⁴

Affiliation:

1. Department of Lithospheric Research, University of Vienna, Vienna, Austria.

2. Institute for Geology und Mineralogy, University of Cologne, Cologne, Germany.

3. Department of Geology, University of Vienna, Vienna, Austria.

4. Department of Physics and Earth Sciences, Jacobs University Bremen, Bremen, Germany.

Publisher

Mary Ann Liebert Inc

Subject

Space and Planetary Science,Agricultural and Biological Sciences (miscellaneous)

Link

https://www.liebertpub.com/doi/pdf/10.1089/ast.2020.2311

Reference120 articles.

1. A Whiff of Oxygen Before the Great Oxidation Event?

2. Metal Stable Isotopes in Paleoceanography

3. Distribution of high field strength elements (Y, Zr, REE, Hf, Ta, Th, U) in adjacent magnetite and chert bands and in reference standards FeR-3 and FeR-4 from the Temagami iron-formation, Canada, and the redox level of the Neoarchean ocean

4. Distribution of yttrium and rare-earth elements in the Penge and Kuruman iron-formations, Transvaal Supergroup, South Africa

5. Rare earth element systematics of the chemically precipitated component in early precambrian iron formations and the evolution of the terrestrial atmosphere-hydrosphere-lithosphere system

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