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Monitoring of tunnel behaviour through catacclastic rocks

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dc.contributor.author Georgiannou, VN en
dc.contributor.author Lefas, ID en
dc.contributor.author Boronkay, KA en
dc.date.accessioned 2014-03-01T01:24:40Z
dc.date.available 2014-03-01T01:24:40Z
dc.date.issued 2006 en
dc.identifier.issn 1353-2618 en
dc.identifier.uri https://dspace.lib.ntua.gr/xmlui/handle/123456789/17380
dc.subject Roads & highways en
dc.subject Rock mechanic en
dc.subject Tunnels & tunneling en
dc.subject.classification Engineering, Geological en
dc.subject.classification Geosciences, Multidisciplinary en
dc.subject.other Gypsum en
dc.subject.other Highway systems en
dc.subject.other Limestone en
dc.subject.other Roads and streets en
dc.subject.other Rock mechanics en
dc.subject.other Rocks en
dc.subject.other Surveying en
dc.subject.other Roads & highways en
dc.subject.other Sedimentary clay formation en
dc.subject.other Tunnel diameters en
dc.subject.other Tunnels & tunneling en
dc.subject.other Vehicular tunnels en
dc.subject.other cataclasite en
dc.subject.other geological structure en
dc.subject.other gypsum en
dc.subject.other limestone en
dc.subject.other sandy soil en
dc.subject.other silt en
dc.subject.other tunneling en
dc.subject.other Eurasia en
dc.subject.other Europe en
dc.subject.other Greece en
dc.subject.other Southern Europe en
dc.title Monitoring of tunnel behaviour through catacclastic rocks en
heal.type journalArticle en
heal.identifier.primary 10.1680/geng.2006.159.2.113 en
heal.identifier.secondary http://dx.doi.org/10.1680/geng.2006.159.2.113 en
heal.language English en
heal.publicationDate 2006 en
heal.abstract Field instrumentation was used in the construction of two twin tunnels for the new Egnatia Motorway in Greece. This paper describes the displacement monitoring results taken during tunnelling through heavily fragmented limestone varying from a block size > 10 cm down to sandy gravel and sandy silt or gouge. The primary lining displacements monitored by surveying methods appear to be directly related to the detailed geological subdivisions of the limestone observed at the tunnel face. Maximum values of settlement were recorded during tunnelling through the gouge and reached 80 mm, while horizontal movements up to 40 mm were recorded associated with outward deflection of the support frames. The development of settlement with time shows that settlement of the tunnel crown and sides increased sharply while the face of the tunnel was within a tunnel diameter of the station point under consideration and reached equilibrium when the excavation face was at least 3 to 4 tunnel diameters beyond it. Surface settlements above the axis of the tunnel were first observed when the face of the tunnel was directly beneath the station. At the entrance portals of the tunnels the limestone overlies a thin sedimentary clay formation and gypsum. Horizontal movements along the interface between the limestone and the underlying clay sequence as well as within a clay/gypsum layer at the portals were observed using a standard inclinometer. en
heal.publisher THOMAS TELFORD PUBLISHING en
heal.journalName Proceedings of the Institution of Civil Engineers: Geotechnical Engineering en
dc.identifier.doi 10.1680/geng.2006.159.2.113 en
dc.identifier.isi ISI:000236625300005 en
dc.identifier.volume 159 en
dc.identifier.issue 2 en
dc.identifier.spage 113 en
dc.identifier.epage 123 en


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