The influence of low-density granite bodies on extensional basins |
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Authors: | Louis Howell Stuart Egan Graham Leslie Stuart Clarke Andrew Mitten Jamie Pringle |
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Institution: | 1. School of Geography, Geology and the Environment, William Smith Building, Keele University, Keele, Staffordshire, ST5 5BG UK;2. BGS Scotland, Lyell Centre, Research Avenue South, Edinburgh, EH14 4AP UK |
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Abstract: | The Carboniferous northern Pennine Basin remains the type locality for the ‘block and basin’ tectonic framework model. It has been widely believed that during periods of tectonic extension, large low-density bodies within the basement permit buoyant blocks to resist isostatic subsidence. However, lithosphere-scale structural and geodynamic modelling experiments dispute this; suggesting instead that the formation of intra-basinal highs occurs prior to lithospheric extension. In northern UK, this tectonic framework is controlled by a combination of tectonic stress, isostasy and the buoyancy forces of low-density granite, lithospheric flexure and, importantly, the inherited structural framework. It is hoped that further study can lead to a greater appreciation of the interplay of structural and geodynamic process that control the ‘block and basin’ framework. |
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