Hf and Pb Isotopic Constraints on the Origin of a Well-Studied Suite of Icelandic Picrites.
Publikation: Konferencebidrag › Konferenceabstrakt til konference › Forskning
Standard
Hf and Pb Isotopic Constraints on the Origin of a Well-Studied Suite of Icelandic Picrites. / Niklas, Robert W.; Brandon, A.D.; Waight, Tod.
2019. Abstract fra Goldschmidt Conference.Publikation: Konferencebidrag › Konferenceabstrakt til konference › Forskning
Harvard
APA
Vancouver
Author
Bibtex
}
RIS
TY - ABST
T1 - Hf and Pb Isotopic Constraints on the Origin of a Well-Studied Suite of Icelandic Picrites.
AU - Niklas, Robert W.
AU - Brandon, A.D.
AU - Waight, Tod
PY - 2019
Y1 - 2019
N2 - The Iceland plume is one of the best geochemically studied plume in the literature. Isotopically enriched Icelandic lavas likely contained significant recycled components in their mantle source regions [1]. Although up to four endmembers have been proposed to explain the isotopic range sampled by the plume [2], principle component analysis (PCA) has shown that >99% of the variation is the result of mixing between two endmembers [3]. A suite of modern Icelandic picrites have been previously analyzed for 186-187Os, He, Nd, Sr and Tl isotopic systematics and major and trace elements [4-6]. These data show mixing between a high 3He/4He enriched component and a low 3He/4He depleted component in the picrite mantle source. Both components contained negligable subducted sediment [5]. In order to provide context for these end-members, we have determined the Hf and double-spike Pb isotopic compositions of these picrites. Measured 176Hf/177Hf, 206Pb/204Pb, 207Pb/204Pb, 208Pb/204Pb ratios varied between 0.28310-0.28336, 18.04818.967, 15.432-15.572 and 37.711-38.526, respectively. 207Pb and 208Pb values are almost uniformly negative and positive, respectively, consistent with the bulk of Icelandic lavas [2]. All lithophile element isotopic systematics show broad correlation with 187Os/188Os consistent with mixing. These correlations allow calculation of the lithophile isotopic systematics of the two mantle endmembers, which are consistent with the hybrid recycled crust-primitive mantle and depleted mantle end members proposed in [4]. This hybrid endmember shows that recycled crust is likely mixed with primordial undegassed material in the deep mantle, and that this mixture has recently been sampled by mantle plumes.
AB - The Iceland plume is one of the best geochemically studied plume in the literature. Isotopically enriched Icelandic lavas likely contained significant recycled components in their mantle source regions [1]. Although up to four endmembers have been proposed to explain the isotopic range sampled by the plume [2], principle component analysis (PCA) has shown that >99% of the variation is the result of mixing between two endmembers [3]. A suite of modern Icelandic picrites have been previously analyzed for 186-187Os, He, Nd, Sr and Tl isotopic systematics and major and trace elements [4-6]. These data show mixing between a high 3He/4He enriched component and a low 3He/4He depleted component in the picrite mantle source. Both components contained negligable subducted sediment [5]. In order to provide context for these end-members, we have determined the Hf and double-spike Pb isotopic compositions of these picrites. Measured 176Hf/177Hf, 206Pb/204Pb, 207Pb/204Pb, 208Pb/204Pb ratios varied between 0.28310-0.28336, 18.04818.967, 15.432-15.572 and 37.711-38.526, respectively. 207Pb and 208Pb values are almost uniformly negative and positive, respectively, consistent with the bulk of Icelandic lavas [2]. All lithophile element isotopic systematics show broad correlation with 187Os/188Os consistent with mixing. These correlations allow calculation of the lithophile isotopic systematics of the two mantle endmembers, which are consistent with the hybrid recycled crust-primitive mantle and depleted mantle end members proposed in [4]. This hybrid endmember shows that recycled crust is likely mixed with primordial undegassed material in the deep mantle, and that this mixture has recently been sampled by mantle plumes.
M3 - Conference abstract for conference
T2 - Goldschmidt Conference
Y2 - 18 August 2019 through 23 August 2019
ER -
ID: 321561867