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2014 | OriginalPaper | Chapter

8. Recycling of Lead at Neoarchean Continental Margins

Author : Jaana Halla

Published in: Evolution of Archean Crust and Early Life

Publisher: Springer Netherlands

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Abstract

A time-fixed Pb-Pb model of 2.7 ± 0.1 Ga mantle-derived granitoids from different Archean cratons suggests that the Pb isotope heterogeneity of Neoarchean granitoids can be explained by sediment recycling and subduction at oceanic and continental margins consisting of different-aged crustal segments. Recycling of crustal Pb to the mantle wedge gave rise to increasingly radiogenic mantle sources for the granitoids as the accretion of oceanic island arcs (OIA) and Mesoarchean microcontinents proceeded, leading to the formation of young (< 3.2 Ga) continental margins (YCM). Materials recycling at old (> 3.2 Ga) continental margins (OCM) encompassing fragments of Paleo- and Eoarchean protocrust provided the high- or low-µ Pb isotope signatures, depending on the age and U/Pb ratio of the crustal lead sources.

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Metadata
Title
Recycling of Lead at Neoarchean Continental Margins
Author
Jaana Halla
Copyright Year
2014
Publisher
Springer Netherlands
DOI
https://doi.org/10.1007/978-94-007-7615-9_8