1.60 Ga felsic volcanic blocks in the moraines of the Terre Adélie Craton, Antarctica: comparisons with the Gawler Range Volcanics, South Australia

Peucat, J-JCapdevila, RFanning, ChristopherMenot, R PPecora, LTestut, L2015-12-130812-0099http://hdl.handle.net/1885/94241Rhyodacite and rhyolite blocks found in numerous moraines on the Terre Adélie Craton in Antarctica are samples of a high-temperature high-K calc-alkaline to alkali-calcic igneous suite emplaced at ca 1.60 Ga. They comprise lavas and pyroclastic rocks, inKeywords: geochemistry; geochronology; moraine; petrography; Precambrian; stratigraphic correlation; volcanic rock; Antarctica; Australia Antarctica; Felsic volcanics; Gawler Range Volcanics; Geochemistry; Geochronology; Moraines; Rodinia; South Australia; Terre Adélie Craton1.60 Ga felsic volcanic blocks in the moraines of the Terre Adélie Craton, Antarctica: comparisons with the Gawler Range Volcanics, South Australia200210.1046/j.1440-0952.2002.00956.x2024-03-10