Antarctic Science 33(4), 373–401 (2021) © The Author(s), 2021. Published by Cambridge University Press. This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted re-use, distribution, and reproduction in any medium, provided the original work is properly cited. doi:10.1017/S0954102021000213 Lithostratigraphy, age and distribution of Eocene volcanic sequences on eastern King George Island, South Shetland Islands, Antarctica JOHN L. SMELLIE 1, RICHARD J. HUNT2, WILLIAM C. MCINTOSH 3 and RICHARD P. ESSER3,4 1School of Geography, Geology & the Environment, University of Leicester, Leicester, LE1 7RH, UK 2School of Earth Sciences, University of Leeds, Woodhouse Lane, Leeds, LS2 9JT, UK 3New Mexico Bureau of Geology and Mineral Resources, New Mexico Tech, Socorro, NM 87801, USA 4Now at: Energy and Geosciences Institute, University of Utah, Salt Lake City, UT 84108, USA
[email protected] Abstract: New mapping and dating of volcanic outcrops on the east coast of Admiralty Bay, King George Island, has demonstrated that Eocene volcanic sequences are dominant and also crop out extensively elsewhere, particularly on the eastern part of the island. The sequences can be divided into at least three formations (Hennequin, Cape Vauréal and Carruthers Cliff) together with Eocene strata at Warkocz and near Lions Rump that are currently unassigned stratigraphically. New and recently published 40Ar/39Ar ages indicate that all of the formations are Early Eocene in age, mainly Ypresian, extending to Lutetian and possibly even Priabonian time in more easterly outcrops. Compositional contrasts exist between the groups (calc-alkaline vs tholeiitic).