Geodynamic setting and deformation history of an Archaean terrane at mid-crustal level: The Tasiusarsuaq terrane of southern West Greenland

• Published in: Precambrian research 2012-08, Vol.212-213, p.34-56
• Main Authors: Kolb, J., Kokfelt, T.F., Dziggel, A.
• Format: Article
• Language: English
• Subjects: Archaean tectonics; Granulite-facies; Southern West Greenland; Tasiusarsuaq terrane
• ISSN: 0301-9268; 1872-7433
• DOI: 10.1016/j.precamres.2012.04.010

► Archaean granulites from an orogenic margin in a compressive regime. ► Thrusting of granulites on a rigid foreland. ► Insignificant exhumation in the Archaean. ► Post-collisional extension is uncommon for the exhumation of Archaean granulites. The Neoarchaean Tasiusarsuaq terrane is situated in the North Atlantic craton approximately 50km south of the capital Nuuk, and extends for 400km to the south to the Frederikshåb Isblink. It mainly consists of granulite facies and commonly migmatitic grey gneiss, narrow supracrustal belts and volumetrically minor late-tectonic granites. The supracrustal belts have a lithological association of picritic, komatiitic and basaltic rocks together with ultramafic dykes and sills, with geochemical characteristics typical of an arc-type setting. The grey gneiss is tonalitic to granodioritic in composition, and was emplaced between ca. 2.92 and 2.82Ga into crust that is probably represented by the supracrustal rocks. The gneiss, in turn, was intruded by granite dykes at ca. 2830Ma–2800Ma, and by tonalitic dykes at ca. 2770Ma. Both probably are the result of partial melting of the thickened crust. Late-tectonic tonalitic pegmatites intruded at 2673±5Ma at amphibolite-facies conditions. The structural evolution from the granulite-facies peak to amphibolite-facies levels is characterised by three deformation stages. D1 fabrics form only relics in low-strain domains of the dominant NW-vergent D2 fold-and-thrust structures. Syn-tectonic granite and tonalitic dykes date the D2 thrusting to have occurred between ca. 2800Ma and 2700Ma, contemporaneously with near-isobaric cooling. The subsequent D3 deformation, still in the amphibolite-facies, is marked by E-W to NE-SW shortening, forming upright folds and near-vertical strike slip shear zones at ca. 2670–2630Ma. The final exhumation of the terrane likely occurred first during the Proterozoic, and was probably mainly driven by erosion. The granulites of the Tasiusarsuaq terrane formed at an orogenic margin in a compressive regime. A first orogenic cycle (2.8–2.7Ga), here termed the Tasiusarsuaq orogeny, resulted in thrusting of the terrane on a rigid foreland represented by the Færingehavn terrane in the north. The Tasiusarsuaq granulites were further affected by a second Archaean orogeny (2.67–2.58Ga), the Kapisilik orogeny, which caused transcurrent deformation and only insignificant exhumation to mid-crustal levels. Significantly, there is no evidence that the exhumation of the