Geological evolution of the Coombs-Allan Hills area, Ferrar large igneous province, Antarctica: debris avalanches, mafic pyroclastic density currents, phreatocauldrons
The Jurassic Ferrar large igneous province of Antarctica comprises igneous intrusions, flood lavas, and mafic volcaniclastic deposits (now lithified). The latter rocks are particularly diverse and well-exposed in the Coombs-Allan Hills area of South Victoria Land, where they are assigned to the Maws...
Published in: | Journal of Volcanology and Geothermal Research |
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Main Authors: | , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
2008
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Subjects: | |
Online Access: | https://espace.inrs.ca/id/eprint/1900/ https://espace.inrs.ca/id/eprint/1900/1/Ross-et-al%28geological-evolution%292008_web%5B1%5D.pdf https://doi.org/10.1016/j.jvolgeores.2005.11.011 |