Petrogenesis of a Phonolite-Trachyte Succession at Mount Sidley, Marie Byrd Land, Antarctica

The 1.5 Ma evolution of the Late Pliocene (5.7 to 4.2 Ma) Mt Sidley volcano, Marie Byrd Land, is examined using major and trace elements, Sr, Nd, O and Pb isotopic data. A large (5 km × 5 km) breached caldera exposes lavas and tephras, deep within Mt Sidley, and allows its magmatic evolution to be e...

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Bibliographic Details
Published in:Journal of Petrology
Main Authors: Panter, Kurt S., Kyle, Philip R., Smellie, John L.
Format: Text
Language:English
Published: Oxford University Press 1997
Subjects:
Online Access:http://petrology.oxfordjournals.org/cgi/content/short/38/9/1225
https://doi.org/10.1093/petroj/38.9.1225