Badania składu głazowego moren zlodowacenia południowopolskiego
STUDIES ON BOULDER COMPOSITION IN MORAINES OF THE SOUTH POLISH GLACIATIONSummaryCrystalline rocks found to occur in the moraines of the South Polish Glaciation have been investigated. The distribution of investigation points is shown in Fig. 1. For fractions from 2 to 10 cm quantitative ratios have...
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Polish Geological Institute-National Research Institute
1973
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ftjgq:oai:geojournals.pgi.gov.pl:article/12833 2023-05-15T16:11:55+02:00 Badania składu głazowego moren zlodowacenia południowopolskiego Dudziak, Józef 1973-12-01 application/pdf https://gq.pgi.gov.pl/article/view/12833 https://doi.org/10.7306/gq.v17i4.12833 eng eng Polish Geological Institute-National Research Institute https://gq.pgi.gov.pl/article/view/12833/11297 Geological Quarterly; Vol 17, No 4 (1973); 787-802 1641-7291 info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 1973 ftjgq https://doi.org/10.7306/gq.v17i4.12833 2019-08-13T19:05:53Z STUDIES ON BOULDER COMPOSITION IN MORAINES OF THE SOUTH POLISH GLACIATIONSummaryCrystalline rocks found to occur in the moraines of the South Polish Glaciation have been investigated. The distribution of investigation points is shown in Fig. 1. For fractions from 2 to 10 cm quantitative ratios have been determined between the rocks that come from both the eastern and the western areas of Fennoscandinavia. In the group of the East-Fennoscandinavian rocks there are distinguished: post-orogenic granites, rocks making transitions from granites into granite porphyries, and porphyries: granite porphyry, Aland quartz porphyry, and Baltic red porphyry. As concerns the West-Fennoscandia rocks, the following kinds have been distinguished: Sala granites, Upsala granites, Stockholm granite, Siljan granite, Bornholm granite and Smaland granite, as well as porphyries: Smaland porphyries, from the Dalarna area, and Baltic porphyries, i.e. brown porphyry and syenite porphyry. In all the investigation points the rocks coming from the eastern area of Fenno-Scandinavia distinctly prevail upon the remaining ones (Table 4). This predominance can be observed irrespective of the character of the moraine under examination (arenaceous moraine, silty moraine, clay moraine, which does not show any bedding, or schistous). Article in Journal/Newspaper Fennoscandia Geological Quarterly |
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Open Polar |
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Geological Quarterly |
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ftjgq |
language |
English |
description |
STUDIES ON BOULDER COMPOSITION IN MORAINES OF THE SOUTH POLISH GLACIATIONSummaryCrystalline rocks found to occur in the moraines of the South Polish Glaciation have been investigated. The distribution of investigation points is shown in Fig. 1. For fractions from 2 to 10 cm quantitative ratios have been determined between the rocks that come from both the eastern and the western areas of Fennoscandinavia. In the group of the East-Fennoscandinavian rocks there are distinguished: post-orogenic granites, rocks making transitions from granites into granite porphyries, and porphyries: granite porphyry, Aland quartz porphyry, and Baltic red porphyry. As concerns the West-Fennoscandia rocks, the following kinds have been distinguished: Sala granites, Upsala granites, Stockholm granite, Siljan granite, Bornholm granite and Smaland granite, as well as porphyries: Smaland porphyries, from the Dalarna area, and Baltic porphyries, i.e. brown porphyry and syenite porphyry. In all the investigation points the rocks coming from the eastern area of Fenno-Scandinavia distinctly prevail upon the remaining ones (Table 4). This predominance can be observed irrespective of the character of the moraine under examination (arenaceous moraine, silty moraine, clay moraine, which does not show any bedding, or schistous). |
format |
Article in Journal/Newspaper |
author |
Dudziak, Józef |
spellingShingle |
Dudziak, Józef Badania składu głazowego moren zlodowacenia południowopolskiego |
author_facet |
Dudziak, Józef |
author_sort |
Dudziak, Józef |
title |
Badania składu głazowego moren zlodowacenia południowopolskiego |
title_short |
Badania składu głazowego moren zlodowacenia południowopolskiego |
title_full |
Badania składu głazowego moren zlodowacenia południowopolskiego |
title_fullStr |
Badania składu głazowego moren zlodowacenia południowopolskiego |
title_full_unstemmed |
Badania składu głazowego moren zlodowacenia południowopolskiego |
title_sort |
badania składu głazowego moren zlodowacenia południowopolskiego |
publisher |
Polish Geological Institute-National Research Institute |
publishDate |
1973 |
url |
https://gq.pgi.gov.pl/article/view/12833 https://doi.org/10.7306/gq.v17i4.12833 |
genre |
Fennoscandia |
genre_facet |
Fennoscandia |
op_source |
Geological Quarterly; Vol 17, No 4 (1973); 787-802 1641-7291 |
op_relation |
https://gq.pgi.gov.pl/article/view/12833/11297 |
op_doi |
https://doi.org/10.7306/gq.v17i4.12833 |
_version_ |
1765997129256402944 |