Hf- and O-isotope data from detrital and granitoid zircons reveal characteristics of the Permian–Triassic magmatic belt along the Antarctic sector of Gondwana

Abstract

David H. Elliot1, C. Mark Fanning2, Samuel B. Mukasa3, and Ian L. Millar4 1School of Earth Sciences and Byrd Polar and Climate Research Center, Ohio State University, Columbus, Ohio 43210, USA 2Research School of Earth Sciences, Australian National University, Canberra, ACT 0200, Australia 3College of Science and Engineering, University of Minnesota, Minneapolis, Minnesota 55455, USA 4British Geological Survey, Keyworth, Nottingham NG12 5GG, UK