The Polotsk-Kurzeme and the Småland-Blekinge Deformation Zones of the East European Craton : geomorphology, architecture of the sedimentary cover and the crystalline basement
(2007) In Dissertations in Geology at Lund UniversityDepartment of Geology
- Abstract
- This is a study of the influence of the crystalline basement faults of the Polotsk-Kurzeme and the
Småland-Blekinge Deformation Zones on the development of the sedimentary cover and the formation of the present
topography. The purpose is to define the character and possible causes of this influence. The key target areas of
this study are the Polotsk part of the Polotsk-Kurzeme Deformation Zone in northern Belarus and the eastern part of
the Småland-Blekinge Deformation Zone in southeastern Sweden.
The influence of Mesoproterozoic faulting on the Paleozoic, Mesozoic, Cenozoic and recent evolutions of the Precambrian
crust has been assessed using 3D reconstructions of paleosurfaces, GIS (=Geographical Information Systems)
models of... (More) - This is a study of the influence of the crystalline basement faults of the Polotsk-Kurzeme and the
Småland-Blekinge Deformation Zones on the development of the sedimentary cover and the formation of the present
topography. The purpose is to define the character and possible causes of this influence. The key target areas of
this study are the Polotsk part of the Polotsk-Kurzeme Deformation Zone in northern Belarus and the eastern part of
the Småland-Blekinge Deformation Zone in southeastern Sweden.
The influence of Mesoproterozoic faulting on the Paleozoic, Mesozoic, Cenozoic and recent evolutions of the Precambrian
crust has been assessed using 3D reconstructions of paleosurfaces, GIS (=Geographical Information Systems)
models of basement-cover correlation and topolineaments identification. The 3D upper paleosurfaces of the
crystalline basement, the Ectasian-Stenian, Ediacaran, Ordovician, Devonian and Quaternary sedimentary deposits
and the present landform surface for the Polotsk key area as well as the 3D upper paleosurfaces of the crystalline
basement and the present landform surface for the eastern part of the SBDZ key area have been performed with
ArcGis 9.1 software. A series of maps showing correlation coefficients between the upper paleosurface of the crystalline
basement and all the various Phanerozoic deposits has been produced for the key target areas. We have also
profiled the Quaternary deposits in the Polotsk area.
The results suggest that these deformation zones, after their first formation in the Mesoproterozoic in conjunction
with orogenic processes at the southwestern margin of the East European Craton were still active during the Neoproterozoic-
Phanerozoic. The tectonic activity of the Polotsk-Kurzeme and the Småland-Blekinge Deformation
Zones has had influence both on the formation of the sedimentary cover and the present topography. (Less) - Abstract (Swedish)
- Denna undersökning rör frågan om vilket inflytande förkastningarna i de tektoniska Polotsk-
Kurzeme och Småland-Blekingezonerna utövat på det överlagrande sedimenttäckets och den nutida topografins
utbildning. Syftet var att bestämma karaktären av denna påverkan och dess tänkbara orsaker. De huvudsakliga undersökningsområdena
utgjordes av Polotskdelen av Polotsk-Kurzeme deformationszonen i norra Vitryssland och
östra delen av Småland-Blekingezonen i sydöstra Sverige.
Den mesoproterozoiska förkastningsaktivitetens inverkan på den paleozoiska, mesozoiska, kenozoiska samt recenta
utvecklingen av den prekambriska jordskorpan fastställdes med hjälp av 3-D rekonstruktioner av paleoytornas lägen
och GIS-modellering av topolineament och... (More) - Denna undersökning rör frågan om vilket inflytande förkastningarna i de tektoniska Polotsk-
Kurzeme och Småland-Blekingezonerna utövat på det överlagrande sedimenttäckets och den nutida topografins
utbildning. Syftet var att bestämma karaktären av denna påverkan och dess tänkbara orsaker. De huvudsakliga undersökningsområdena
utgjordes av Polotskdelen av Polotsk-Kurzeme deformationszonen i norra Vitryssland och
östra delen av Småland-Blekingezonen i sydöstra Sverige.
Den mesoproterozoiska förkastningsaktivitetens inverkan på den paleozoiska, mesozoiska, kenozoiska samt recenta
utvecklingen av den prekambriska jordskorpan fastställdes med hjälp av 3-D rekonstruktioner av paleoytornas lägen
och GIS-modellering av topolineament och relationerna mellan underlag och sedimenttäcke. ArcGis 9.1 mjukvaran
användes för att fastställa 3-D övre paleoytor for det kristallina underlaget, de ektasisk-steniska, ediakariska,
ordoviciska, devonska och kvartära avlagringarna och den nutida jordytan i Polotskområdet samt den 3-D övre paleoytan
för det kristallina underlaget och dagens landyta i östra delen av Småland-Blekingezonen. Dessutom sammanställdes
en serie kartor som visar korrelationskoefficienterna mellan det kristallina underlagets paleoyta och alla
de andra övre gränsytorna för de fanerozoiskasedimenten i de två huvudsakliga undersökningsområdena. Profilering
av de kvartära avlagringarna utfördes i Polotskområdet.
Resultaten visar att deformationszonerna efter sin bildning i samband med mesoproterozoiska orogena processer
vid den östeuropeiska kratonens sydvästkant fortsatte att vara aktiva även under neoproterozoikum och fanerozoikum.
Den tektoniska verksamheten inom Polotsk-Kurzeme och Småland-Blekinge deformationszonerna påverkade
såväl sedimenttäckets bildning som den nutida topografin. (Less)
Please use this url to cite or link to this publication:
http://lup.lub.lu.se/student-papers/record/2335521
- author
- Kurlovich, Dzmitry
- supervisor
-
- Svetlana Bogdanova LU
- Per Möller LU
- organization
- alternative title
- Polotsk-Kurzeme och Småland-Blekinge deformationszonerna i den Östeuropeiska kratonen : geomorfologin samt arkitekturen av sedimenttäcket och det kristallina underlaget
- year
- 2007
- type
- H1 - Master's Degree (One Year)
- subject
- keywords
- the Polotsk-Kurzeme Deformation Zone, the Småland-Blekinge Deformation Zone, GIS, fault, tectonic activity, geomorphology, sedimentary cover, Polotsk-Kurzeme deformationszonen, Småland-Blekinge deformationszonen, förkastning, tektonisk verksamhet, geomorfologi, sedimenttäcket
- publication/series
- Dissertations in Geology at Lund University
- report number
- 214
- language
- English
- id
- 2335521
- date added to LUP
- 2012-01-31 16:07:27
- date last changed
- 2012-01-31 16:07:27
@misc{2335521, abstract = {{This is a study of the influence of the crystalline basement faults of the Polotsk-Kurzeme and the Småland-Blekinge Deformation Zones on the development of the sedimentary cover and the formation of the present topography. The purpose is to define the character and possible causes of this influence. The key target areas of this study are the Polotsk part of the Polotsk-Kurzeme Deformation Zone in northern Belarus and the eastern part of the Småland-Blekinge Deformation Zone in southeastern Sweden. The influence of Mesoproterozoic faulting on the Paleozoic, Mesozoic, Cenozoic and recent evolutions of the Precambrian crust has been assessed using 3D reconstructions of paleosurfaces, GIS (=Geographical Information Systems) models of basement-cover correlation and topolineaments identification. The 3D upper paleosurfaces of the crystalline basement, the Ectasian-Stenian, Ediacaran, Ordovician, Devonian and Quaternary sedimentary deposits and the present landform surface for the Polotsk key area as well as the 3D upper paleosurfaces of the crystalline basement and the present landform surface for the eastern part of the SBDZ key area have been performed with ArcGis 9.1 software. A series of maps showing correlation coefficients between the upper paleosurface of the crystalline basement and all the various Phanerozoic deposits has been produced for the key target areas. We have also profiled the Quaternary deposits in the Polotsk area. The results suggest that these deformation zones, after their first formation in the Mesoproterozoic in conjunction with orogenic processes at the southwestern margin of the East European Craton were still active during the Neoproterozoic- Phanerozoic. The tectonic activity of the Polotsk-Kurzeme and the Småland-Blekinge Deformation Zones has had influence both on the formation of the sedimentary cover and the present topography.}}, author = {{Kurlovich, Dzmitry}}, language = {{eng}}, note = {{Student Paper}}, series = {{Dissertations in Geology at Lund University}}, title = {{The Polotsk-Kurzeme and the Småland-Blekinge Deformation Zones of the East European Craton : geomorphology, architecture of the sedimentary cover and the crystalline basement}}, year = {{2007}}, }