A proposed new approach and unified solution to old Pb paradoxes

TitleA proposed new approach and unified solution to old Pb paradoxes
Publication TypeJournal Article
Year of Publication2016
AuthorsCastillo P.R
JournalLithos
Volume252
Pagination32-40
Date Published2016/05
Type of ArticleArticle
ISBN Number0024-4937
Accession NumberWOS:000374599800003
Keywordscarbon-dioxide; continental-crust; convection; core formation; Crustal recycling; earths core; equations; evolution; isotopic composition; lead; mantle; Mantle geochemistry; Marine carbonate recycling hypothesis; ocean island basalts; OIB mantle sources; sr; System of
Abstract

One of the most remarkable features of many and, perhaps, all oceanic basalts is that their Pb isotopic ratios ((206)pb/(204)pb, Pb-207/Pb-204 and (208)pb/Pb-204) are too radiogenic to be coming from the undifferentiated mantle or bulk silicate Earth. This has created three major concerns in the behavior of U, Th and Pb in the Earth's mantle that have been termed the Pb paradoxes. These are the unexpectedly long time-integrated high U/Pb (1st paradox), long time-integrated low Th/U (2nd paradox) and constant Ce/Pb and Nb/U (3rd paradox) in the mantle sources of oceanic basalts. The origins of such unexpected ratios have been the object of intense studies that produced several highly significant, but generally individualized results during the last four decades. Detailed analysis of available data shows that the paradoxes are closely interrelated as they all pertain to the mantle and have many common characteristic features. Thus, the Pb paradoxes constitute a system of equations that must be solved all together as each solution must satisfy every equation in the system. For example, compositional data for the voluminous mid-ocean ridge basalts (MORE) show that the 1st and 2nd paradoxes exhibit a long time-integrated enrichment of U and the Th/U and Nb/Th ratios are also constant. A single solution to simultaneously explain the paradoxes in MORE is possible if recycled materials with variable enrichments in incompatible trace elements, particularly U and its daughter Pb* plus Nb, Ce, and Th are added to or mixed with the depleted upper mantle. Significantly, a similar binary mixing solution has been proposed for the Pb paradoxes in ocean island basalts. (c) 2016 Elsevier B.V. All rights reserved.

DOI10.1016/j.lithos.2016.02.015
Short TitleLithos
Student Publication: 
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