Tight bounds on missing late veneer in early Archean peridotite from triple oxygen isotopes

Autor: Peters S.T.M.[1], Fischer M.B.[1, Pack A.[1], Szilas K.[3], Appel P.W.U.[4], Münker C.[5], Dallai L.[6], Marien C.S.[5]

Publikováno v: Peters, S T M, Fischer, M B, Pack, A, Szilas, K, Appel, P W U, Münker, C, Dallai, L & Marien, C S 2021, ' Tight bounds on missing late veneer in early Archean peridotite from triple oxygen isotopes ', Geochemical Perspectives Letters, vol. 18, pp. 27-31 . https://doi.org/10.7185/geochemlet.2120
Geochemical Perspectives Letters
18 (2021): 27–31. doi:10.7185/geochemlet.2120
info:cnr-pdr/source/autori:Peters S.T.M.[1], Fischer M.B.[1,2], Pack A.[1], Szilas K.[3], Appel P.W.U.[4], Münker C.[5], Dallai L.[6], Marien C.S.[5]/titolo:Tight bounds on missing late veneer in early Archean peridotite from triple oxygen isotopes/doi:10.7185%2Fgeochemlet.2120/rivista:Geochemical Perspectives Letters (Print)/anno:2021/pagina_da:27/pagina_a:31/intervallo_pagine:27–31/volume:18

Oxygen isotopes provide a unique possibility to study Earth's late accretion phase from a lithophile element perspective, because most carbonaceous chondrites - meteorites that likely resemble the composition of the terrestrial late veneer - have mar

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e9c09741a3a9e8f4a56a0ce3aedb5e18
https://curis.ku.dk/ws/files/280556179/GPL2120_noSI.pdf