Research Paper GEOSPHERE Detrital zircon record of Phanerozoic magmatism in the southern Central Andes GEOSPHERE, v. 17, no. 3 T.N. Capaldi1,*, N.R. McKenzie2, B.K. Horton1,3, C. Mackaman-Lofland1, C.L. Colleps2, and D.F. Stockli1 1Department of Geological Sciences, Jackson School of Geosciences, University of Texas at Austin, Austin, Texas 78712, USA https://doi.org/10.1130/GES02346.1 2Department of Earth Sciences, University of Hong Kong, Pokfulam Road, Hong Kong, China 3Institute for Geophysics, Jackson School of Geosciences, University of Texas at Austin, Austin, Texas 78712, USA 11 figures; 1 table; 1 set of supplemental files CORRESPONDENCE:
[email protected] ABSTRACT arc width reflects shallower slab dip. Comparisons geodynamic processes, upper-plate deformation, among slab dip calculations with time-averaged and subduction- related magmatism. CITATION: Capaldi, T.N., McKenzie, N.R., Horton, B.K., Mackaman-Lofland, C., Colleps, C.L., and Stockli, D.F., The spatial and temporal distribution of arc εHf and Th/U zircon results exhibit a clear trend of The South American plate at 28°S –33°S is com- 2021, Detrital zircon record of Phanerozoic magmatism magmatism and associated isotopic variations decreasing (enriched) magma compositions with posed of numerous north-south–trending terranes in the southern Central Andes: Geosphere, v. 17, no. 3, provide insights into the Phanerozoic history increasing arc width and decreasing slab dip. Col- of variable composition that may have induced a p. 876– 897, https://doi.org/10.1130 /GES02346.1. of the western margin of South America during lectively, these data sets demonstrate the influence spatial control on the geochemical signatures of Science Editor: Shanaka de Silva major shifts in Andean and pre-Andean plate inter- of subduction angle on the position of upper-plate subsequent Andean tectono-magmatic regimes Associate Editor: Christopher J.