Continental rift to back-arc basin: Jurassic-Cretaceous stratigraphical and structural evolution of the Larsen Basin, Antarctic Peninsula
The Larsen Basin developed in Jurassic times as a result of continental rifting during the early stages of Gondwana break‐up. Lower‐?Upper Jurassic non‐marine sedimentary and volcanic rocks constitute a syn‐rift megasequence recording initial largely amagmatic extension and subsequent widespread ext...
Published in: | Journal of the Geological Society |
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Format: | Article in Journal/Newspaper |
Language: | unknown |
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Geological Society of London
2000
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Online Access: | http://nora.nerc.ac.uk/id/eprint/20573/ https://doi.org/10.1144/jgs.157.2.417 |