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Petrography and geochemistry of the Carboniferous–Triassic Trinity Peninsula Group, West Antarctica: implications for provenance and tectonic setting

Published online by Cambridge University Press:  29 September 2014

PAULA CASTILLO ,
JUAN PABLO LACASSIE ,
CARITA AUGUSTSSON  and
FRANCISCO HERVÉ
PAULA CASTILLO*
Affiliation:
Research School of Earth Sciences, The Australian National University, Canberra ACT 0200, Australia Departamento de Geología, Universidad de Chile, Plaza Ercilla 803, Santiago, Chile
JUAN PABLO LACASSIE
Affiliation:
Servicio Nacional de Geología y Minería, Av. Santa María 0104, Santiago, Chile
CARITA AUGUSTSSON
Affiliation:
Institut für Geologie und Paläontologie, Westfälische Wilhelms-Universität Münster Corrensstrasse 24, 48 149 Münster, Germany Institutt for Petroleumsteknologi, Universitetet i Stavanger, 4036 Stavanger, Norway
FRANCISCO HERVÉ
Affiliation:
Departamento de Geología, Universidad de Chile, Plaza Ercilla 803, Santiago, Chile Escuela de Ciencias de la Tierra, Universidad Andrés Bello, Sazié 2315, Santiago, Chile
*
†Author for correspondence: paula.castillo@anu.edu.au
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Abstract

The Carboniferous-Triassic Trinity Peninsula Group is a metasedimentary sequence that crops out widely in the northern Antarctic Peninsula. These are some of the most extensive outcrops in the area and hold the key to evaluating the connections of the Antarctic Peninsula in Gondwana; however, they are still poorly understood. Here we present our provenance study of the Trinity Peninsula Group using petrographic and geochemical approaches in combination with cathodoluminescence of detrital quartz in order to constrain its source characteristics and tectonic setting. Using differences in modal composition and quartz cathodoluminescence characteristics, we define three petrofacies derived from the progressive uplift and erosion of a volcano-plutonic continental arc, which exposed the plutonic-metamorphic roots. As indicated by major and trace elements, the source is felsic with a composition ranging from tonalitic to granodioritic. The relatively unweathered condition of the source area points to a dry and cold climate at the time of deposition, but this does not necessarily mean that it was glaciated. Deposition of the sediments occurred within an active continental margin, relatively close to the source area, probably along the south Patagonia–Antarctic Peninsula sector of Gondwana. Strong chronological, petrological and chemical similarities with the sediments of the Duque the York Complex in Patagonia suggest that they were derived from the same source.

Keywords

cathodoluminescencedetrital quartzPalaeozoicGondwanaAntarctic Peninsula
Type
Original Articles
Information
Geological Magazine , Volume 152 , Issue 4 , July 2015 , pp. 575 - 588
Copyright
Copyright © Cambridge University Press 2014 

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