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

Rhyodacite 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, in

Bibliographic Details
Published in:Australian Journal of Earth Sciences
Main Authors: Peucat, J-J, Capdevila, R, Fanning, Christopher, Menot, R P, Pecora, L, Testut, L
Format: Article in Journal/Newspaper
Language:unknown
Published: Blackwell Publishing Ltd
Subjects:
Online Access:http://hdl.handle.net/1885/94241
https://doi.org/10.1046/j.1440-0952.2002.00956.x
https://openresearch-repository.anu.edu.au/bitstream/1885/94241/5/MigratedxPub23777_2002.pdf.jpg
https://openresearch-repository.anu.edu.au/bitstream/1885/94241/7/01_Peucat_1.60_Ga_felsic_volcanic_blocks_2002.pdf.jpg
Description
Summary:Rhyodacite 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, in