Sequence of Early Precambrian metamorphic events in the southern Prince Charles Mts., Eastern Antarctica

Autor: E. N. Kamenev, V. S. Semenov, S. V. Semenov, V. M. Mikhailov, I. A. Kamenev
Rok vydání: 2009
Předmět:
Zdroj: Geology of Ore Deposits. 51:723-740
ISSN: 1555-6476
1075-7015
DOI: 10.1134/s1075701509080054
Popis: The results of geological study of the mountain framework of the southern part of the Lambert Glacier, Mawson Escarpment, Eastern Antarctica, are discussed. The studied territory is of key importance for understanding the regional geological history. The Ruker and the Lambert rock complexes have been distinguished at the Mawson Escarpment. The former is subdivided into the Mawson and Menzies groups. The polymetamorphic rocks of the Mawson Group comprise granite gneiss, orthopyroxene gneiss, and crystalline schists dated at >3000 Ma combined with tectonic wedges and blocks of the variegated sequence with ultramafic (komatiitic) rocks. The find of those rocks allows us to suggest that an ancient granite-greenstone domain existed in the territory of the Prince Charles Mts.; this domain is retained only as tectonic wedges amongst granite gneisses of the Mawson and Menzies groups composed of polymetamorphic terrigenous rocks with basic sills. The following sequence of metamorphic mineral assemblages in the Menzies Group has been established: (1) And-Crd ± St, (2) Ky-St-Grt-Bt-Ms, (3) Sil-Grt-Crd. The andalusite-type metamorphism of rocks pertaining to the Menzies Group probably has the same age as greenschist metamorphism of rocks belonging to the Collaboration Group (2917 ± 82–2878 ± 65 Ma at Mt. Ruker). The formation of kyanite-staurolite mineral assemblage (mounts Stinear, Maguire, Rymill; South Mawson Escarpment) might be related to a metamorphic event dated at 2400–2350 Ma. The formation of sillimanite-garnet and sillimanite-cordierite assemblages with staurolite relics correlates in time with emplacement of the MacColly granite 600–500 Ma ago. Polymetamorphic rocks of the Lambert Complex are migmatites and gneisses, often with orthopyroxene relics. Blocks of ultramafic rocks are localized amongst granite gneisses. The superimposed metamorphism of amphibolite and granulite facies took place 1800 Ma ago. The model Nd age of ultramafic rocks (2500 Ma) is treated as the time of emplacement of magma into the rocks of the Lambert Complex. Isotopic and geochemical evidence for Early Paleozoic granulite-facies metamorphism is known.
Databáze: OpenAIRE
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