Please use this identifier to cite or link to this item: http://hdl.handle.net/2440/130677
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Type: Journal article
Title: Emergence of continents above sea-level influences sediment melt composition
Author: Liebmann, J.
Spencer, C.J.
Kirkland, C.L.
E. Bucholz, C.
He, X.F.
Santosh, M.
Xia, X.P.
Martin, L.
Evans, N.J.
Citation: Terra Nova, 2021; :[1]-[10]
Publisher: Wiley
Issue Date: 2021
ISSN: 0954-4879
1365-3121
Statement of
Responsibility: 
Janne Liebmann, Christopher J. Spencer, Christopher L. Kirkland, Claire E. Bucholz, Xiao-Fang He, M. Santosh, Xiaoping P. Xia, Laure Martin, Noreen J. Evans
Abstract: The Archean-Proterozoic transition heralded a number of fundamental changes on Earth, including the oxygenation of the atmosphere, a marked emergence of continents above sea-level, and an increase in δ¹⁸O of felsic magmas. The potential drivers for the latter are changes in the composition of supracrustal material or increased crustal reworking. Although the onset of subduction-induced continental collision and associated enhanced crustal recycling could produce high-δ¹⁸O felsic magmas, temporally constrained zircon δ¹⁸O reveals an increase in δ¹⁸O at ~2.35 Ga that predates the oldest widely recognized supercontinent. In this work, we use the O and Hf isotope ratios of magmatic zircon crystals in Archean and Proterozoic sediment-derived granitoids of the North China Craton to track the incorporation of supracrustal material into magmas. The results are consistent with a Paleoproterozoic increase of continental freeboard producing sedimentary reservoirs with comparatively elevated δ¹⁸O that subsequently partially melted to generate the granitoids.
Description: OnlinePubl.
Rights: © 2021 John Wiley & Sons Ltd
RMID: 1000040917
DOI: 10.1111/ter.12531
Grant ID: http://purl.org/au-research/grants/arc/LE150100013
Appears in Collections:Geology & Geophysics publications

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