Geochemistry Constraints of Mesozoic–Cenozoic Calc-Alkaline Magmatism in the South Shetland Arc, Antarctica
Journal of South American Earth Sciences 18 (2005) 407–425 www.elsevier.com/locate/jsames Geochemistry constraints of Mesozoic–Cenozoic calc-alkaline magmatism in the South Shetland arc, Antarctica A. Machadoa,*, E.F. Limaa, F. Chemale Jr.a, D. Moratab, O. Oteizab, D.P.M. Almeidac, A.M.G. Figueiredod, F.M. Alexandrea, J.L. Urrutiab aInstitute of Geosciences, Federal University of Rio Grande do Sul, Isotope Geology Laboratory, Av. Bento Gonc¸alves, 9500, Campus do Vale, Agronomia, 91501-970 Porto Alegre, RS, Brazil bDepartment of Geology, University of Chile, Casilla 13518, Correo 21, Santiago, Chile cDepartment of Geology, Unisinos University, Av. Unisinos, 9500 Sa˜o Leopoldo, RS, Brazil dInstitute of Energetic and Nuclear Research (IPEN) Nacional Commission of Nuclear Energy, Radiochemistry Division, University of Sa˜o Paulo-USP, Post Box 11049, 01000 Sa˜o Paulo, SP, Brazil Received 1 July 2003; accepted 1 November 2004 Abstract Geochemical data from basalts, basaltic andesites, and andesites of the Mesozoic–Cenozoic (143–44 Ma) from Livingston, Greenwich, Robert, King George, and Ardley Islands of the South Shetland archipelago, Antarctica, are presented. The rocks have variable SiO2 of approximately 46–61 wt%, Al2O3 of 15–26 wt%, and total alkali (K2OCNa2O) of 2–6 wt%. Most samples have low Mg#, Cr, and Ni, which indicates that they have undergone significant fractional crystallization from mantle-derived melts. The presence of olivine cumulatic in the samples from Livingston and Robert Islands explains some high MgO, Ni, and Cr values, whereas low Rb, Zr, and Nb values could be related to undifferentiated magmas. N-MORB-normalized trace element patterns show that South Shetland Islands volcanic rocks have a geochemical pattern similar to that found for other island arcs, with enrichment in LILE relative to HFSE and in LREE relative to HREE.
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