Volume change in contractional kink bands; examples from the NNE-SSW Late Variscan kink bands of Portugal
Kink bands are usually associated to the late deformation stages in polydeformed areas, being developed in rocks that present a strong planar mechanical anisotropy (e.g. layering or cleavage). In Portugal, the Late Variscan deformation episode generates in Almograve and Abrantes regions (SW Iberian...
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Format: | lecture |
Language: | eng |
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2018
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Online Access: | http://hdl.handle.net/10174/22801 |
Country: | Portugal |
Oai: | oai:dspace.uevora.pt:10174/22801 |