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- W2011041143 abstract "Using a modified Piper (1976) pre-Grenville fit of Laurentia and Baltica, tectonic information from the Lewisian complex of Britain and from neighbouring Early Proterozoic belts of Laurentia and Baltica is reviewed. It is shown that a remarkable consistency in convergence directions existed across the whole region in the period 1.9-1.8 Ga suggesting that the reconstruction used may be correct, and that a common movement pattern can be inferred for the Early Proterozoic period within the North Atlantic region. A speculative plate tectonic history for the region between ∼ 2.6 and ∼ 1.6 Ga is discussed in four stages. (1) 2.6-2.4 Ga: development of conjugate shear-zone systems in the North Atlantic craton. (2) 2.4-2.0 Ga: rifting and dyke emplacement in older cratons; creation of oceanic and intracontinental basins. (3) 2.0-1.8 Ga: subduction at active margins of older cratons with creation of magmatic arcs; collision of cratons accompanied by closure of intra-cratonic basins. (4) 1.8-1.6 Ga: development of new active margin discordant to the previous ones, with significant changes in convergence direction within the amalgamated continental assembly." @default.
- W2011041143 created "2016-06-24" @default.
- W2011041143 creator A5044811433 @default.
- W2011041143 date "1994-06-01" @default.
- W2011041143 modified "2023-10-18" @default.
- W2011041143 title "Early Proterozoic tectonic overview of the northern British Isles and neighbouring terrains in Laurentia and Baltica" @default.
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- W2011041143 doi "https://doi.org/10.1016/0301-9268(94)90065-5" @default.
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