Mesozoic geology of Cape Shirreff, Livingston Island, South Shetland Islands, Antarctica
The stratigraphic succession at Cape Shirr e ff has a minimum thickness of 450 m and is mainly composed of lavas and a smaller amount of volcaniclastic breccias. Lavas are subalkaline olivine basalts and basaltic andesites which are locally well - bedded, but in most areas give a homogeneous, someti...
Main Authors: | , , , , |
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Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Universitat de Barcelona
1999
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Subjects: | |
Online Access: | http://revistes.ub.edu/index.php/ActaGeologica/article/view/5075 |