TY - JOUR
T1 - Partial melting of the Archaean Thrym Complex of southeastern Greenland
AU - Bagas, Leon
AU - Næraa, Tomas
AU - Kolb, Jochen
AU - Reno, Barry L.
AU - Fiorentini, Marco L.
N1 - Funding Information:
Greenland Bureau of Minerals and Petroleum (BMP) and the Geological Survey of Denmark and Greenland (GEUS) are gratefully acknowledged for financial support of the field and analytical work. This contribution is a product of collaboration between GEUS, the Centre for Exploration Targeting (CET) at the University of Western Australia and the Australian Research Council (ARC) Centre of Excellence for Core to Crust Fluid Systems (CCFS) . This is contribution 228 from CCFS ( www.ccfs.mq.edu.au ). The manuscript benefited from comments by Y. Lu, C.R.L. Friend and H. Rollinson, and the helpful reviews by Robert Kerrich and Marco Scambelluri.
PY - 2013/2
Y1 - 2013/2
N2 - High-grade Archaean rocks of the remote Thrym Complex of southeastern Greenland expose a lower crustal section that formed at a depth of > 30. km at temperatures reaching 1000. °C and pressures approaching 1.5. GPa. The complex is part of the North Atlantic Craton, which is bound to the north by the Trans Hudson-Nagssugtoqidian-Ammassalik Orogen and to the south by the Makkovik-Ketilidian Orogen. The rocks in the complex include orthogneiss, migmatitic orthogneiss with banded or nebulitic fabrics, migmatite with a breccia-like structure (agmatite), and narrow bands of lensoidal mafic and ultramafic rocks (granulites) with associated widespread garnet-bearing mafic granulite, and a minor proportion of garnet-cordierite-sillimanite-biotite gneiss. The latter high-grade rocks form part of the substrate for the emplacement of the protoliths for orthogneiss that was synchronous with the ca. 2790-2700. Ma Skjoldungen Orogeny.At least two suites have been recognised in the Thrym Complex based on geochemistry. The oldest is a tholeiitic suite of mafic to ultramafic granulites, and the other is a calc-alkaline suite that includes felsic to intermediate orthogneiss. Most of the orthogneiss has a granodioritic (oldest) to quartz monzodioritic (younger) composition with rare monzogranitic, tonalitic, monzonitic and quartz dioritic protoliths. Historically, the orthogneiss units have been called TTGs, although monzogranite and tonalite are rare, and no trondhjemite is observed. In addition, they could also be called adakitic on geochemical grounds. Instead of using this terminology, which has genetic connotations, the orthogneiss is referred to as predominantly granodioritic to quartz-monzodioritic.Assuming that modern tectonics operated during the Neoarchaean, at least some of the mafic and ultramafic granulites and orthogneiss exposed in the Thrym Complex represent the root zone of a magmatic-arc that might have been relaminated around 2760. Ma during the collisional Skjoldungen Orogeny.
AB - High-grade Archaean rocks of the remote Thrym Complex of southeastern Greenland expose a lower crustal section that formed at a depth of > 30. km at temperatures reaching 1000. °C and pressures approaching 1.5. GPa. The complex is part of the North Atlantic Craton, which is bound to the north by the Trans Hudson-Nagssugtoqidian-Ammassalik Orogen and to the south by the Makkovik-Ketilidian Orogen. The rocks in the complex include orthogneiss, migmatitic orthogneiss with banded or nebulitic fabrics, migmatite with a breccia-like structure (agmatite), and narrow bands of lensoidal mafic and ultramafic rocks (granulites) with associated widespread garnet-bearing mafic granulite, and a minor proportion of garnet-cordierite-sillimanite-biotite gneiss. The latter high-grade rocks form part of the substrate for the emplacement of the protoliths for orthogneiss that was synchronous with the ca. 2790-2700. Ma Skjoldungen Orogeny.At least two suites have been recognised in the Thrym Complex based on geochemistry. The oldest is a tholeiitic suite of mafic to ultramafic granulites, and the other is a calc-alkaline suite that includes felsic to intermediate orthogneiss. Most of the orthogneiss has a granodioritic (oldest) to quartz monzodioritic (younger) composition with rare monzogranitic, tonalitic, monzonitic and quartz dioritic protoliths. Historically, the orthogneiss units have been called TTGs, although monzogranite and tonalite are rare, and no trondhjemite is observed. In addition, they could also be called adakitic on geochemical grounds. Instead of using this terminology, which has genetic connotations, the orthogneiss is referred to as predominantly granodioritic to quartz-monzodioritic.Assuming that modern tectonics operated during the Neoarchaean, at least some of the mafic and ultramafic granulites and orthogneiss exposed in the Thrym Complex represent the root zone of a magmatic-arc that might have been relaminated around 2760. Ma during the collisional Skjoldungen Orogeny.
KW - Archaean
KW - Geochemistry
KW - Geochronology
KW - Granulite-facies
KW - Greenland
KW - Thrym Complex
UR - http://www.scopus.com/inward/record.url?scp=84872446686&partnerID=8YFLogxK
U2 - 10.1016/j.lithos.2012.11.026
DO - 10.1016/j.lithos.2012.11.026
M3 - Article
VL - 160-161
SP - 164
EP - 182
JO - Lithos
JF - Lithos
SN - 0024-4937
ER -