Recent activity of the regional geologic structures in western Slovenia

Several important geological structures in the western Slovenia were identifiedas active and their activity was quantified. Geologic interpretation is based on the analysis of repeated leveling line campaigns data along the Sečovlje–Bled polygon. Taking intoaccount the limitations of the method – on...

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Main Authors: Miloš Bavec, Božo Koler, Igor Rižnar
Format: Article
Language:English
Published: Geological Survey of Slovenia 2007-06-01
Series:Geologija
Subjects:
Online Access:http://www.geologija-revija.si/dokument.aspx?id=350
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author Miloš Bavec
Božo Koler
Igor Rižnar
author_facet Miloš Bavec
Božo Koler
Igor Rižnar
author_sort Miloš Bavec
collection DOAJ
description Several important geological structures in the western Slovenia were identifiedas active and their activity was quantified. Geologic interpretation is based on the analysis of repeated leveling line campaigns data along the Sečovlje–Bled polygon. Taking intoaccount the limitations of the method – only the vertical component of displacement is measured – the following structures were identified as active:a juvenile syncline between Strunjan and Koper, the Kras Imbricate Structure, the Diva~a fault, the Ra{a fault, the Southalpine Front and the Julian Alps thrust. Vertical movement rate is relative, calculated with respect to the benchmark in Sečovlje. The largest uplift rate difference between Sečovlje and Bled is 7 mm/a.Vertical Geodynamic Activity (VGA) is introduced as a link between geologic interpretation of geodetic measurements on one side and possible applications on the other as well as a mean of comparison between tectonically active regions.
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spelling doaj.art-86806243eb8d43989a1320053cb085dc2023-01-23T08:10:15ZengGeological Survey of SloveniaGeologija0016-77891854-620X2007-06-01501111120Recent activity of the regional geologic structures in western SloveniaMiloš BavecBožo KolerIgor RižnarSeveral important geological structures in the western Slovenia were identifiedas active and their activity was quantified. Geologic interpretation is based on the analysis of repeated leveling line campaigns data along the Sečovlje–Bled polygon. Taking intoaccount the limitations of the method – only the vertical component of displacement is measured – the following structures were identified as active:a juvenile syncline between Strunjan and Koper, the Kras Imbricate Structure, the Diva~a fault, the Ra{a fault, the Southalpine Front and the Julian Alps thrust. Vertical movement rate is relative, calculated with respect to the benchmark in Sečovlje. The largest uplift rate difference between Sečovlje and Bled is 7 mm/a.Vertical Geodynamic Activity (VGA) is introduced as a link between geologic interpretation of geodetic measurements on one side and possible applications on the other as well as a mean of comparison between tectonically active regions.http://www.geologija-revija.si/dokument.aspx?id=350recent tectonic activitygeodynamicslevelling lineKraški RobSouthalpine FrontJulian Alps thrustRaša faultDivača faultvertical geodynamic activitySlovenia
spellingShingle Miloš Bavec
Božo Koler
Igor Rižnar
Recent activity of the regional geologic structures in western Slovenia
Geologija
recent tectonic activity
geodynamics
levelling line
Kraški Rob
Southalpine Front
Julian Alps thrust
Raša fault
Divača fault
vertical geodynamic activity
Slovenia
title Recent activity of the regional geologic structures in western Slovenia
title_full Recent activity of the regional geologic structures in western Slovenia
title_fullStr Recent activity of the regional geologic structures in western Slovenia
title_full_unstemmed Recent activity of the regional geologic structures in western Slovenia
title_short Recent activity of the regional geologic structures in western Slovenia
title_sort recent activity of the regional geologic structures in western slovenia
topic recent tectonic activity
geodynamics
levelling line
Kraški Rob
Southalpine Front
Julian Alps thrust
Raša fault
Divača fault
vertical geodynamic activity
Slovenia
url http://www.geologija-revija.si/dokument.aspx?id=350
work_keys_str_mv AT milosbavec recentactivityoftheregionalgeologicstructuresinwesternslovenia
AT bozokoler recentactivityoftheregionalgeologicstructuresinwesternslovenia
AT igorriznar recentactivityoftheregionalgeologicstructuresinwesternslovenia