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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Bibliographic Details
Main Author: Graser, Gesa
Other Authors: Markl, Gregor (Prof. Dr.)
Format: Doctoral or Postdoctoral Thesis
Language:English
Published: Universität Tübingen 2008
Subjects:
550
Online Access:http://hdl.handle.net/10900/49137
http://nbn-resolving.de/urn:nbn:de:bsz:21-opus-32580