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<https://discovery.ucl.ac.uk/id/eprint/1334086> <http://purl.org/dc/terms/title> "Tectonic evolution of the Ionian thrust belt, NW Greece"^^<http://www.w3.org/2001/XMLSchema#string> .
<https://discovery.ucl.ac.uk/id/eprint/1334086> <http://purl.org/ontology/bibo/abstract> "The Ionian Zone is a classic thin-skinned fold and thrust belt that has been believed to have\r\nundergone a multiphase clockwise vertical axis rotation of 40°-60° since the Miocene, based on\r\npalaeomagnetism and geodesy. Timings, however, are disputed and spatial variations have\r\nlargely been ignored.\r\nIn this study, data from 21 new palaeomagnetic sites are presented alongside a reappraisal of\r\nprevious results from the Ionian Zone. These results are integrated with basement geometry\r\nderived from gravity modelling and an estimate of the variation in shortening across the thrust\r\nbelt, both of which were performed as part of this study.\r\nThe palaeomagnetic analysis supports a bulk ~55° clockwise rotation of the Ionian Zone, albeit\r\nwith significant local variations. It is suggested that the Gulf of Amvrakia (GoA), which divides\r\nthe present day Ionian Zone into the geographic provinces of Epiros and Akarnania, formed an\r\nimportant boundary during thrusting; distinctly different patterns of rotational deformation are\r\nobserved in the two provinces. In Epiros, north of the GoA, relative rotations between adjacent\r\nsections of neighbouring thrust sheets suggest that rotation occurred during thrust sheet\r\nemplacement, initially slowly just prior to emplacement, followed by rapid rotation during\r\nemplacement. Conversely, in Akarnania, all thrust sheets have undergone a consistent ~70°\r\nclockwise rotation, and it is suggested that this was accommodated on the Ionian Thrust, with\r\nthe largest part of the horizontal displacement taken up by subduction.\r\nForeland basement geometry, derived from gravity modelling, is proposed to have been\r\ninfluential in the tectonic evolution of the Ionian Zone. Interaction with basement obstacles\r\nresulted in lower rotations in the northernmost Ionian Zone, duplexing in central Epiros and,\r\npossibly, out-of-sequence thrusting Akarnania.\r\nThe conclusions of this study are distinct from previous findings as they imply no rotation of the\r\nmost external Ionian Zone and the Paxos Zone occurred prior to the advance of thrusting into\r\nthis region, rather than a multiphase rotation of the whole zone."^^<http://www.w3.org/2001/XMLSchema#string> .
<https://discovery.ucl.ac.uk/id/eprint/1334086> <http://purl.org/dc/terms/date> "2011-11-28" .
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<https://discovery.ucl.ac.uk/id/eprint/1334086/> <http://purl.org/dc/elements/1.1/title> "HTML Summary of #1334086 \n\nTectonic evolution of the Ionian thrust belt, NW Greece\n\n" .
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