Combined Sr, Nd, Pb and Li isotope geochemistry of alkaline lavas from northern James Ross Island (Antarctic Peninsula) and implications for back-arc magma formation

• Published in: Chemical geology Vol. 258; no. 3; pp. 207 - 218
• Main Authors: Košler, J., Magna, T., Mlčoch, B., Mixa, P., Nývlt, D., Holub, F.V.
• Format: Journal Article
• Language: English
• Published: Elsevier B.V 30-01-2009
• Subjects: Antarctic Peninsula; Back-arc magmatism; Depleted and enriched mantle; James Ross Island; Marine; Sr–Nd–Pb–Li isotopes; Antarctic Plate; PSW, Antarctica, Antarctic Peninsula; ANE, British Isles, Scotland, Shetland; PSW, Antarctic Ocean, Bransfield Strait; PSW, Antarctica, Antarctic Peninsula, James Ross I; Depleted and enriched mantle; Sr–Nd–Pb–Li isotopes; Back-arc magmatism; Antarctic Peninsula; James Ross Island
• ISSN: 0009-2541; 1872-6836
• DOI: 10.1016/j.chemgeo.2008.10.006

We present a comprehensive geochemical data set for a suite of back-arc alkaline volcanic rocks from James Ross Island Volcanic Group (JRIVG), Antarctic Peninsula. The elemental and isotopic (Sr, Nd, Pb and Li) composition of these Cenozoic basalts emplaced east of the Antarctic Peninsula is different from the compositions of the fore-arc alkaline volcanic rocks in Southern Shetlands and nearby Bransfield Strait. The variability in elemental and isotopic composition is not consistent with the JRIVG derivation from a single mantle source but rather it suggests that the magma was mainly derived from a depleted mantle with subordinate OIB-like enriched mantle component (EM II). The isotopic data are consistent with mantle melting during extension and possible roll-back of the subducted lithosphere of the Antarctic plate. Magma contamination by Triassic–Early Tertiary clastic sediments deposited in the back-arc basin was only localized and affected Li isotopic composition in two of the samples, while most of the basalts show very little variation in
δ
7Li values, as anticipated for “mantle-driven” Li isotopic composition. These variations are difficult to resolve with radiogenic isotope systematics but Li isotopes may prove sensitive in tracking complex geochemical processes acting through the oceanic crust pile, including hydrothermal leaching and seawater equilibration.