New data about the Upper Cretaceous from eastern part of the Southern Baltic Sea
During preparing the sheets of the Geological Map of the Baltic Sea Bottom, scale 1 :200 000, the current boundary of occurrence of the Upper Cretaceous deposits in eastern part of the Southern Baltic was located about 75 km northward from its previous position. The Upper Cretaceous was documented w...
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Polish Geological Institute-National Research Institute
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ftjgq:oai:geojournals.pgi.gov.pl:article/8387 2024-09-15T18:12:24+00:00 New data about the Upper Cretaceous from eastern part of the Southern Baltic Sea Pikies, Radosław 2013-03-05 application/pdf https://gq.pgi.gov.pl/article/view/8387 eng eng Polish Geological Institute-National Research Institute https://gq.pgi.gov.pl/article/view/8387/pdf_475 10.7306/gq.v36i2.8387.g6939 https://gq.pgi.gov.pl/article/view/8387 Geological Quarterly; Vol. 36 No. 2 (1992); 245-258 Geological Quarterly; Tom 36 Nr 2 (1992); 245-258 1641-7291 10.7306/gq.v36i2 info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2013 ftjgq https://doi.org/10.7306/gq.v36i2 2024-07-30T03:29:08Z During preparing the sheets of the Geological Map of the Baltic Sea Bottom, scale 1 :200 000, the current boundary of occurrence of the Upper Cretaceous deposits in eastern part of the Southern Baltic was located about 75 km northward from its previous position. The Upper Cretaceous was documented with micropalaeontological, mineralogical and seismic-acoustic data on area of sheet Gotland Basin and it lies with unconformity on the Upper Devonian and - probably - on Upper Silurian deposits. The meridional faults of older network, renewed in the Laramide Phase, had significant influence on such far northward extension of the described Cretaceous deposits, for example: Żarnowiec, Karwia and Kuźnica faults. Final position of limit of the Upper Cretaceous extent was determined by denudation processes, prevailed on this area during Tertiary (Paleocene - Lower Eocene, Neogene) as well as several times repeated ice-sheet exaration. Article in Journal/Newspaper Ice Sheet Geological Quarterly |
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Open Polar |
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Geological Quarterly |
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ftjgq |
language |
English |
description |
During preparing the sheets of the Geological Map of the Baltic Sea Bottom, scale 1 :200 000, the current boundary of occurrence of the Upper Cretaceous deposits in eastern part of the Southern Baltic was located about 75 km northward from its previous position. The Upper Cretaceous was documented with micropalaeontological, mineralogical and seismic-acoustic data on area of sheet Gotland Basin and it lies with unconformity on the Upper Devonian and - probably - on Upper Silurian deposits. The meridional faults of older network, renewed in the Laramide Phase, had significant influence on such far northward extension of the described Cretaceous deposits, for example: Żarnowiec, Karwia and Kuźnica faults. Final position of limit of the Upper Cretaceous extent was determined by denudation processes, prevailed on this area during Tertiary (Paleocene - Lower Eocene, Neogene) as well as several times repeated ice-sheet exaration. |
format |
Article in Journal/Newspaper |
author |
Pikies, Radosław |
spellingShingle |
Pikies, Radosław New data about the Upper Cretaceous from eastern part of the Southern Baltic Sea |
author_facet |
Pikies, Radosław |
author_sort |
Pikies, Radosław |
title |
New data about the Upper Cretaceous from eastern part of the Southern Baltic Sea |
title_short |
New data about the Upper Cretaceous from eastern part of the Southern Baltic Sea |
title_full |
New data about the Upper Cretaceous from eastern part of the Southern Baltic Sea |
title_fullStr |
New data about the Upper Cretaceous from eastern part of the Southern Baltic Sea |
title_full_unstemmed |
New data about the Upper Cretaceous from eastern part of the Southern Baltic Sea |
title_sort |
new data about the upper cretaceous from eastern part of the southern baltic sea |
publisher |
Polish Geological Institute-National Research Institute |
publishDate |
2013 |
url |
https://gq.pgi.gov.pl/article/view/8387 |
genre |
Ice Sheet |
genre_facet |
Ice Sheet |
op_source |
Geological Quarterly; Vol. 36 No. 2 (1992); 245-258 Geological Quarterly; Tom 36 Nr 2 (1992); 245-258 1641-7291 10.7306/gq.v36i2 |
op_relation |
https://gq.pgi.gov.pl/article/view/8387/pdf_475 10.7306/gq.v36i2.8387.g6939 https://gq.pgi.gov.pl/article/view/8387 |
op_doi |
https://doi.org/10.7306/gq.v36i2 |
_version_ |
1810449978877804544 |