The sedimentary environment in the Ljubljansko barje basin during the pile-dwelling period
Geological processes on the Ljubljansko barje basin after the Last Glacial Maximum are known merely on a general level. At few points more detailed circumstances are known, but this information is fragmented spatially and temporally. While artefacts from the archaeological sites were studied in deta...
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ZRC SAZU, Založba ZRC
2011
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ftslacadscienart:oai:ojs.zrc-sazu.si:article/7918 2023-05-15T18:12:21+02:00 The sedimentary environment in the Ljubljansko barje basin during the pile-dwelling period Sedimentacijsko okolje na Ljubljanskem barju v času kolišč Verbič, Tomaž 2011-01-01 application/pdf https://ojs.zrc-sazu.si/av/article/view/7918/7417 https://ojs.zrc-sazu.si/av/article/view/7918 slv slv ZRC SAZU, Založba ZRC https://ojs.zrc-sazu.si/av/article/view/7918 https://creativecommons.org/licenses/by-nc-sa/4.0 CC-BY-NC-SA Arheološki vestnik; Vol. 62 (2011): ARHEOLOŠKI VESTNIK Arheološki vestnik; Letn. 62 (2011): ARHEOLOŠKI VESTNIK 0570-8966 1581-1204 Ljubljansko barje geological processes Quaternary and Holocene environments Seekreide gyttja organic sediments pile-dwellings geološki procesi kvartarno in holocensko okolje jezerska kreda organski sedimenti kolišča info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2011 ftslacadscienart 2022-08-11T20:10:23Z Geological processes on the Ljubljansko barje basin after the Last Glacial Maximum are known merely on a general level. At few points more detailed circumstances are known, but this information is fragmented spatially and temporally. While artefacts from the archaeological sites were studied in detail, the sediments were mostly only imperfectly described. Better understanding of the evolution of the environment requires accurate study of these sediments and buried soils, and detection of evident stratigraphical hiatuses. Geološki procesi na Ljubljanskem barju po zadnjem glacialnem višku so le splošno poznani. Izjemoma sicer poznamo detajlne razmere, vendar so te prostorsko in časovno fragmentarne. Artefakti iz arheoloških najdišč so bili v preteklosti deležni natančnega proučevanja, sami sedimenti s kulturno vsebino, njihova talnina in krovnina pa bistveno manj. Pot do boljšega razumevanja okoljskih razmer v času kolišč verjetno vodi prav preko natančnega poznavanja sedimentov in pokopanih tal ter razumevanja evidentiranih stratigrafskih hiatusov. Article in Journal/Newspaper sami ZRC SAZU Publishing (Znanstvenoraziskovalni center - Slovenske akademije znanosti in umetnosti) |
institution |
Open Polar |
collection |
ZRC SAZU Publishing (Znanstvenoraziskovalni center - Slovenske akademije znanosti in umetnosti) |
op_collection_id |
ftslacadscienart |
language |
Slovenian |
topic |
Ljubljansko barje geological processes Quaternary and Holocene environments Seekreide gyttja organic sediments pile-dwellings geološki procesi kvartarno in holocensko okolje jezerska kreda organski sedimenti kolišča |
spellingShingle |
Ljubljansko barje geological processes Quaternary and Holocene environments Seekreide gyttja organic sediments pile-dwellings geološki procesi kvartarno in holocensko okolje jezerska kreda organski sedimenti kolišča Verbič, Tomaž The sedimentary environment in the Ljubljansko barje basin during the pile-dwelling period |
topic_facet |
Ljubljansko barje geological processes Quaternary and Holocene environments Seekreide gyttja organic sediments pile-dwellings geološki procesi kvartarno in holocensko okolje jezerska kreda organski sedimenti kolišča |
description |
Geological processes on the Ljubljansko barje basin after the Last Glacial Maximum are known merely on a general level. At few points more detailed circumstances are known, but this information is fragmented spatially and temporally. While artefacts from the archaeological sites were studied in detail, the sediments were mostly only imperfectly described. Better understanding of the evolution of the environment requires accurate study of these sediments and buried soils, and detection of evident stratigraphical hiatuses. Geološki procesi na Ljubljanskem barju po zadnjem glacialnem višku so le splošno poznani. Izjemoma sicer poznamo detajlne razmere, vendar so te prostorsko in časovno fragmentarne. Artefakti iz arheoloških najdišč so bili v preteklosti deležni natančnega proučevanja, sami sedimenti s kulturno vsebino, njihova talnina in krovnina pa bistveno manj. Pot do boljšega razumevanja okoljskih razmer v času kolišč verjetno vodi prav preko natančnega poznavanja sedimentov in pokopanih tal ter razumevanja evidentiranih stratigrafskih hiatusov. |
format |
Article in Journal/Newspaper |
author |
Verbič, Tomaž |
author_facet |
Verbič, Tomaž |
author_sort |
Verbič, Tomaž |
title |
The sedimentary environment in the Ljubljansko barje basin during the pile-dwelling period |
title_short |
The sedimentary environment in the Ljubljansko barje basin during the pile-dwelling period |
title_full |
The sedimentary environment in the Ljubljansko barje basin during the pile-dwelling period |
title_fullStr |
The sedimentary environment in the Ljubljansko barje basin during the pile-dwelling period |
title_full_unstemmed |
The sedimentary environment in the Ljubljansko barje basin during the pile-dwelling period |
title_sort |
sedimentary environment in the ljubljansko barje basin during the pile-dwelling period |
publisher |
ZRC SAZU, Založba ZRC |
publishDate |
2011 |
url |
https://ojs.zrc-sazu.si/av/article/view/7918/7417 https://ojs.zrc-sazu.si/av/article/view/7918 |
genre |
sami |
genre_facet |
sami |
op_source |
Arheološki vestnik; Vol. 62 (2011): ARHEOLOŠKI VESTNIK Arheološki vestnik; Letn. 62 (2011): ARHEOLOŠKI VESTNIK 0570-8966 1581-1204 |
op_relation |
https://ojs.zrc-sazu.si/av/article/view/7918 |
op_rights |
https://creativecommons.org/licenses/by-nc-sa/4.0 |
op_rightsnorm |
CC-BY-NC-SA |
_version_ |
1766184896646086656 |