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Copyright (c) 2016 Trine Dahl-Jensen, Peter H Voss, Tine B Larsen
This work is licensed under a Creative Commons Attribution 4.0 International License.
Abstract
A marked change in crustal thickness is seen at the deformation boundary between the undisturbed Archaean core in the south and reworked Archaean gneiss in the foreland of the Nagssugtoqidian orogen in West Greenland. In addition, intra-crustal boundaries can be tentatively interpreted. This is the first information on crustal structure in the area, which is known for kimberlite, carbonatite and ultramafic lamprophyre occurrences, and diamond exploration.
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Copyright (c) 2016 Trine Dahl-Jensen, Peter H Voss, Tine B Larsen
This work is licensed under a Creative Commons Attribution 4.0 International License.
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Editors Adam A. Garde, Ole Bennike, Kristine Thrane and W. Stuart Watt
This issue of Review of Survey Activities presents a selection of 24 papers reflecting the wide spectrum of current activities of the Geological Survey of Denmark and Greenland, from the microscopic to the plate-tectonic level.
The Survey’s activities in Denmark are illustrated [...]
