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"Journal", "mtid" : 23421, "link" : "/api/journal/23421", "label" : "INTERNATIONAL JOURNAL OF EARTH SCIENCES 1437-3254 1437-3262", "pIssn" : "1437-3254", "eIssn" : "1437-3262", "reviewType" : "REVIEWED", "noIF" : false, "sciIndexed" : true, "scopusIndexed" : true, "lang" : "FOREIGN", "hungarian" : false, "published" : true, "oldId" : 23421, "snippet" : true }, "volume" : "94", "issue" : "4", "firstPage" : "538", "lastPage" : "549", "firstPageOrInternalIdForSort" : "538", "pageLength" : 12, "publishedYear" : 2005, "abstractText" : "The Upper Rhine graben is a north-northeast trending rift \nsystem, which belongs to the European Cenozoic rift system. \nToday, the southern part of the graben is seismically still \nactive. Earthquakes of magnitude 5 have a recurrence time of \napproximately 30 years. In order to monitor and to determine the \ndisplacements in the study area, GPS measurements have been \ncarried out in two campaigns (1999 and 2000), and observations \nof the available permanent stations have been processed in 2002. \nOwing to the small size of deformations expected, high accuracy \nrequirements must be met by the GPS processing. In order to \nachieve these requirements, precise antenna modeling has been \nintroduced into the processing. As expected the short time span \nhas not enabled to detect significant displacements from the GPS \nmeasurements. The deformation analysis shows that the horizontal \ndisplacement rates do not exceed 1 mm/year, which is compatible \nwith the geological information. Owing to the fact that the \naccuracy of positioning with GPS for the vertical coordinates is \nlower than for the horizontal coordinates, the determination of \nvertical displacements has been carried out using the leveling \ntechnique. In the area of Freiburg, first-order and second-order \nleveling lines have been chosen for the detection of local \ndisplacements on the Weinstetten, on the Lehen-Scho?nberg and on \nthe Main Border Fault (MBF). Some sections of these faults are \nstill active today. Significant vertical displacements have been \nobserved at the Weinstetten fault in the area of Bad Krozingen \nand on the MBF in Freiburg. The displacement rates (1925-1984) \nare 0.17?0.01 mm/year and 0.25?0.02 mm/year respectively. The \nresults agree very well with the results of seismotectonic \ninvestigations, and show that ongoing displacements can be found \non the northern part of the Lehen-Scho?nberg fault in the \nvicinity of Eichstetten, and on the MBF in the vicinity of \nFreiburg. 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