TERÉNNÍ A LABORATORNÍ DOKUMENTACE STAVEBNÍHO ODKRYVU NA ZÁPADNÍM OKRAJI BĚLOTÍNA, MORAVSKÁ BRÁNA
A pebble sample collected near the critical sector of the Moravian Gate was analyzed. The clasts come from the upper part of the Lower Badenian marine sand and the pebbles scattered on the surface in the W environs of Belotin village (close to the European watershed between the Baltic and Black sea)...
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ftmasarykunivojs:oai:ojs.journals.muni.cz:article/4820 2024-06-23T07:53:47+00:00 TERÉNNÍ A LABORATORNÍ DOKUMENTACE STAVEBNÍHO ODKRYVU NA ZÁPADNÍM OKRAJI BĚLOTÍNA, MORAVSKÁ BRÁNA Field and laboratory documentation of a building site exposure on western edge of Bělotín, Moravian Gate Gába, Zdeněk Vašíčková, Jarmila Matýsek, Dalibor Rozehnal, Tomáš 2016-01-21 application/pdf https://journals.muni.cz/gvms/article/view/4820 ces cze Masaryk University https://journals.muni.cz/gvms/article/view/4820/3885 https://journals.muni.cz/gvms/article/view/4820 Geologické výzkumy na Moravě a ve Slezsku; Vol 14 (2007) Geological Research in Moravia and Silesia; Vol. 14 (2007) 2336-4378 1212-6209 Moravian Gate European watershed pebble and RTG analyses opal silicite Menilitic formation info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2016 ftmasarykunivojs 2024-06-04T04:20:50Z A pebble sample collected near the critical sector of the Moravian Gate was analyzed. The clasts come from the upper part of the Lower Badenian marine sand and the pebbles scattered on the surface in the W environs of Belotin village (close to the European watershed between the Baltic and Black sea) where the overflow of the divide by the scandinavian ice sheet is still open to debate. The pebble petrology is a simple one, the clasts being composed mostly of sandstone and silicite with some quartz admixture. Most important for palaeogeographic interpretation are silicites, which might indicate nordic or local source. The microscopic study as well as RTG analyses proved a local provenance of opal silicites from the Menilitic formation (Carpathian Oligocene). A pebble sample collected near the critical sector of the Moravian Gate was analyzed. The clasts come from the upper part of the Lower Badenian marine sand and the pebbles scattered on the surface in the W environs of Belotin village (close to the European watershed between the Baltic and Black sea) where the overflow of the divide by the scandinavian ice sheet is still open to debate. The pebble petrology is a simple one, the clasts being composed mostly of sandstone and silicite with some quartz admixture. Most important for palaeogeographic interpretation are silicites, which might indicate nordic or local source. The microscopic study as well as RTG analyses proved a local provenance of opal silicites from the Menilitic formation (Carpathian Oligocene). Article in Journal/Newspaper Ice Sheet Masaryk University Journals |
institution |
Open Polar |
collection |
Masaryk University Journals |
op_collection_id |
ftmasarykunivojs |
language |
Czech |
topic |
Moravian Gate European watershed pebble and RTG analyses opal silicite Menilitic formation |
spellingShingle |
Moravian Gate European watershed pebble and RTG analyses opal silicite Menilitic formation Gába, Zdeněk Vašíčková, Jarmila Matýsek, Dalibor Rozehnal, Tomáš TERÉNNÍ A LABORATORNÍ DOKUMENTACE STAVEBNÍHO ODKRYVU NA ZÁPADNÍM OKRAJI BĚLOTÍNA, MORAVSKÁ BRÁNA |
topic_facet |
Moravian Gate European watershed pebble and RTG analyses opal silicite Menilitic formation |
description |
A pebble sample collected near the critical sector of the Moravian Gate was analyzed. The clasts come from the upper part of the Lower Badenian marine sand and the pebbles scattered on the surface in the W environs of Belotin village (close to the European watershed between the Baltic and Black sea) where the overflow of the divide by the scandinavian ice sheet is still open to debate. The pebble petrology is a simple one, the clasts being composed mostly of sandstone and silicite with some quartz admixture. Most important for palaeogeographic interpretation are silicites, which might indicate nordic or local source. The microscopic study as well as RTG analyses proved a local provenance of opal silicites from the Menilitic formation (Carpathian Oligocene). A pebble sample collected near the critical sector of the Moravian Gate was analyzed. The clasts come from the upper part of the Lower Badenian marine sand and the pebbles scattered on the surface in the W environs of Belotin village (close to the European watershed between the Baltic and Black sea) where the overflow of the divide by the scandinavian ice sheet is still open to debate. The pebble petrology is a simple one, the clasts being composed mostly of sandstone and silicite with some quartz admixture. Most important for palaeogeographic interpretation are silicites, which might indicate nordic or local source. The microscopic study as well as RTG analyses proved a local provenance of opal silicites from the Menilitic formation (Carpathian Oligocene). |
format |
Article in Journal/Newspaper |
author |
Gába, Zdeněk Vašíčková, Jarmila Matýsek, Dalibor Rozehnal, Tomáš |
author_facet |
Gába, Zdeněk Vašíčková, Jarmila Matýsek, Dalibor Rozehnal, Tomáš |
author_sort |
Gába, Zdeněk |
title |
TERÉNNÍ A LABORATORNÍ DOKUMENTACE STAVEBNÍHO ODKRYVU NA ZÁPADNÍM OKRAJI BĚLOTÍNA, MORAVSKÁ BRÁNA |
title_short |
TERÉNNÍ A LABORATORNÍ DOKUMENTACE STAVEBNÍHO ODKRYVU NA ZÁPADNÍM OKRAJI BĚLOTÍNA, MORAVSKÁ BRÁNA |
title_full |
TERÉNNÍ A LABORATORNÍ DOKUMENTACE STAVEBNÍHO ODKRYVU NA ZÁPADNÍM OKRAJI BĚLOTÍNA, MORAVSKÁ BRÁNA |
title_fullStr |
TERÉNNÍ A LABORATORNÍ DOKUMENTACE STAVEBNÍHO ODKRYVU NA ZÁPADNÍM OKRAJI BĚLOTÍNA, MORAVSKÁ BRÁNA |
title_full_unstemmed |
TERÉNNÍ A LABORATORNÍ DOKUMENTACE STAVEBNÍHO ODKRYVU NA ZÁPADNÍM OKRAJI BĚLOTÍNA, MORAVSKÁ BRÁNA |
title_sort |
terénní a laboratorní dokumentace stavebního odkryvu na západním okraji bělotína, moravská brána |
publisher |
Masaryk University |
publishDate |
2016 |
url |
https://journals.muni.cz/gvms/article/view/4820 |
genre |
Ice Sheet |
genre_facet |
Ice Sheet |
op_source |
Geologické výzkumy na Moravě a ve Slezsku; Vol 14 (2007) Geological Research in Moravia and Silesia; Vol. 14 (2007) 2336-4378 1212-6209 |
op_relation |
https://journals.muni.cz/gvms/article/view/4820/3885 https://journals.muni.cz/gvms/article/view/4820 |
_version_ |
1802645614453850112 |