Late-magmatic to hydrothermal processes in the Ilímaussaq intrusion, South Greenland
The 1.16 Ga old, persodic Ilímaussaq intrusion in South Greenland solidified at a depth of about 3 to 4 km, between the granitic basement and the sandstones and pillow-bearing basalts of the Eriksfjord Formation. The intrusion consists of alkali granite, syenites, and agpaitic nepheline syenites, wh...
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Format: | Doctoral or Postdoctoral Thesis |
Language: | English |
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Universität Tübingen
2008
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Online Access: | http://hdl.handle.net/10900/49137 http://nbn-resolving.de/urn:nbn:de:bsz:21-opus-32580 |