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

David H. Elliot | Zendy; C. Mark Fanning | Zendy; Samuel B. Mukasa | Zendy; Ian Millar | Zendy

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

Author(s) -

David H. Elliot,

C. Mark Fanning,

Samuel B. Mukasa,

Ian Millar

Publication year - 2019

Publication title -

geosphere

Language(s) - English

Resource type - Journals

SCImago Journal Rank - 1.879

H-Index - 58

ISSN - 1553-040X

DOI - 10.1130/ges02011.1

Subject(s) - geology , zircon , permian , gondwana , igneous rock , geochemistry , large igneous province , pluton , carboniferous , paleozoic , paleontology , geochronology , magmatism , structural basin , tectonics

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

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