Magmatic dyke systems of the South Shetland Islands volcanic arc (West Antarctica): reflections of the geodynamic history
The Antarctic Peninsula forms part of a magmatic arc at least since Jurassic times. Magmatic dykes are essential elements of such arcs and intrude along zones of instability. In contrast to other hypabyssal intrusions and the effusive products of arc activity, dykes do not only reflect the geochemic...
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Format: | Thesis |
Language: | English |
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Ludwig-Maximilians-Universität München
2005
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Online Access: | https://dx.doi.org/10.5282/edoc.3827 https://edoc.ub.uni-muenchen.de/id/eprint/3827 |