Supracrustal rocks in the Ammassalik region, South-East Greenland

Abstract

Large belts of supracrustal rocks are abundant in the Ammassalik region of S.E. Greenland, and are referred to collectively as the Siportoq supracrustal association. They comprise overwhelmingly metasediments, mainly of quartz-rich or semipelitic composition, with variable proportions of quartz, kyanite, sillimanite, garnet and biotite. Graphitic schists are also common and marble horizons occur up to a kilometre thick. Garnet amphibolites are volumetrically minor, and ultramafic rocks are extremely rare. Lithological banding representing relict bedding and rare cross-bedding are locally well preserved. The compositions of the metasedimentary rocks suggest that their provenance was dominantly sialic and the great thickness of semi-pelitic rocks suggests that additions of immature minerals kept pace with gentle subsidence of a basin or shelf environment. The thick marble horizons indicate periods of relative stability. Unlike the surrounding quartzo-feldspathic gneisses in the north of the area, the supracrustal rocks do not appear to have undergone granulite facies metamorphism.

Evaluating the biosignature potential of nitrogen concentrations in graphite and associated K-silicates

“…The Tasiilaq region of SE Greenland exposes the suture between the North Atlantic and Rae cratons, resulting from horizontal convergence and collision that culminated in the 1.9 Ga Nagssugtoqidian orogeny (Hall et al, 1989;Kalsbeek et al, 1993;Nutman et al, 2008;Kolb, 2014). The North Atlantic Craton in the area is represented by the Isertoq terrane, which acted as the overriding plate in the convergence, whereas the Kuummiut terrane and the Schweizerland terrane to the north of it are part of the Rae craton (Fig.…”

“…(Kolb, 2014;Crotty et al, 2022) and the Fenris Unit in Schweizerland (Crotty et al, 2022). The supracrustal belts contain a diversity of metasedimentary lithologies including metapelite, marble, calc-silicate rocks and quartzite, as well as volcanic or shallow intrusive magmatic rocks, predominantly metabasalts (Hall et al, 1989;Kolb, 2014;Crotty et al, 2022;Poulsen, 2022). These lithologies are thought to have been deposited in interconnected basins in volcanic arc and back-arc basin settings at ca.…”