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...
Published in: | Journal of Petrology |
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Main Authors: | , , |
Format: | Text |
Language: | English |
Published: |
Oxford University Press
1997
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Subjects: | |
Online Access: | http://petrology.oxfordjournals.org/cgi/content/short/38/9/1225 https://doi.org/10.1093/petroj/38.9.1225 |