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Engineering geology and mapping of the Quaternary deposits of the city of Xanthi, N. Greece

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dc.contributor.author Marinos, PG en
dc.contributor.author Xidakis, GS en
dc.date.accessioned 2014-03-01T01:08:21Z
dc.date.available 2014-03-01T01:08:21Z
dc.date.issued 1991 en
dc.identifier.issn 02679914 en
dc.identifier.uri https://dspace.lib.ntua.gr/xmlui/handle/123456789/10432
dc.subject Engineering Geology en
dc.title Engineering geology and mapping of the Quaternary deposits of the city of Xanthi, N. Greece en
heal.type journalArticle en
heal.identifier.primary 10.1144/GSL.ENG.1991.007.01.52 en
heal.identifier.secondary http://dx.doi.org/10.1144/GSL.ENG.1991.007.01.52 en
heal.publicationDate 1991 en
heal.abstract The city of Xanthi is situated on the border between the crystalline massif of Rodope and the extended coastal plain of Thrace. The broader urban area is covered mainly by Quaternary for.mat ions of screes and talus deposits from the mountain slopes, various genera- Lions of alluvial deposits in t_he form of t_orr.ential fans, r.ecenL f l u v i o - t o r. r e n t i a l deposits and eluviaI sheets on marly slopes. From data collected from natural ground cuts, boreholes, excavations for. foundations and some laboratory t e s t i n g, the area has been divided into four main geotechnical zones and a number of subzones. The soils in the main zones have similar, or analogous geotechnic:al behaviour. A folio of engineering geology and hydr.ogeology maps was produced. This study shows how a reliable geotechnical evaiuas and zoning in Quakernar.y formations can be approached by detailed engineering geological mapping, mainly for the types of terrain found in t_he Xanthi area, wher.e coarse mat_er.ials are predominant. en
heal.journalName Geological Society Engineering Geology Special Publication en
dc.identifier.doi 10.1144/GSL.ENG.1991.007.01.52 en
dc.identifier.volume 7 en
dc.identifier.spage 541 en
dc.identifier.epage 547 en


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