New findings of the Campanian Ignimbrite ash within slope deposits of the Treska valley (former Yugoslav Republic of Macedonia)
In this paper, we describe the first finding of the Campanian Ignimbrite tephra layer in a subaerial succession in the Former Yugoslav Republic of Macedonia. The tephra is interbedded within slope deposits mixed with colluvial loess. The identification of this fundamental stratigraphic marker is bas...
Published in: | Italian Journal of Geosciences |
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Online Access: | http://hdl.handle.net/2122/11567 https://doi.org/10.3301/IJG.2016.16 |
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ftingv:oai:www.earth-prints.org:2122/11567 2023-05-15T17:32:53+02:00 New findings of the Campanian Ignimbrite ash within slope deposits of the Treska valley (former Yugoslav Republic of Macedonia) Sulpizio, Roberto Milevski, Ivica Ribolini, Adriano Regattieri, Eleonora Isola, Ilaria Bini, Monica Zanchetta, Giovanni Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Pisa, Pisa, Italia #PLACEHOLDER_PARENT_METADATA_VALUE# 2017 http://hdl.handle.net/2122/11567 https://doi.org/10.3301/IJG.2016.16 en eng Italian Journal of Geosciences /136 (2017) http://hdl.handle.net/2122/11567 doi:10.3301/IJG.2016.16 restricted Campanian Ignimbrite slope deposit loess Republic of Macedonia (FYROM) article 2017 ftingv https://doi.org/10.3301/IJG.2016.16 2022-07-29T06:07:28Z In this paper, we describe the first finding of the Campanian Ignimbrite tephra layer in a subaerial succession in the Former Yugoslav Republic of Macedonia. The tephra is interbedded within slope deposits mixed with colluvial loess. The identification of this fundamental stratigraphic marker is based on major elements. The investigated succession is correlated to lacustrine records from Ohrid and Prespa lakes, several archives of the central and eastern Mediterranean, and mainland Ukraine and Russia. Field observations and correlation with lacustrine records (i.e. pollen) indicate that accumulation of the volcanic ash occurred in a dry environment characterized by low vegetation cover and important wind activity, which promoted loess deposition. The recognition of the Campanian Ignimbrite tephra allows the correlation of the loess sediments to the H4 event, as defined in the North Atlantic event climatic stratigraphy. Published 198-205 1V. Storia eruttiva JCR Journal Article in Journal/Newspaper North Atlantic Earth-Prints (Istituto Nazionale di Geofisica e Vulcanologia) Italian Journal of Geosciences 136 2 198 205 |
institution |
Open Polar |
collection |
Earth-Prints (Istituto Nazionale di Geofisica e Vulcanologia) |
op_collection_id |
ftingv |
language |
English |
topic |
Campanian Ignimbrite slope deposit loess Republic of Macedonia (FYROM) |
spellingShingle |
Campanian Ignimbrite slope deposit loess Republic of Macedonia (FYROM) Sulpizio, Roberto Milevski, Ivica Ribolini, Adriano Regattieri, Eleonora Isola, Ilaria Bini, Monica Zanchetta, Giovanni New findings of the Campanian Ignimbrite ash within slope deposits of the Treska valley (former Yugoslav Republic of Macedonia) |
topic_facet |
Campanian Ignimbrite slope deposit loess Republic of Macedonia (FYROM) |
description |
In this paper, we describe the first finding of the Campanian Ignimbrite tephra layer in a subaerial succession in the Former Yugoslav Republic of Macedonia. The tephra is interbedded within slope deposits mixed with colluvial loess. The identification of this fundamental stratigraphic marker is based on major elements. The investigated succession is correlated to lacustrine records from Ohrid and Prespa lakes, several archives of the central and eastern Mediterranean, and mainland Ukraine and Russia. Field observations and correlation with lacustrine records (i.e. pollen) indicate that accumulation of the volcanic ash occurred in a dry environment characterized by low vegetation cover and important wind activity, which promoted loess deposition. The recognition of the Campanian Ignimbrite tephra allows the correlation of the loess sediments to the H4 event, as defined in the North Atlantic event climatic stratigraphy. Published 198-205 1V. Storia eruttiva JCR Journal |
author2 |
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Pisa, Pisa, Italia #PLACEHOLDER_PARENT_METADATA_VALUE# |
format |
Article in Journal/Newspaper |
author |
Sulpizio, Roberto Milevski, Ivica Ribolini, Adriano Regattieri, Eleonora Isola, Ilaria Bini, Monica Zanchetta, Giovanni |
author_facet |
Sulpizio, Roberto Milevski, Ivica Ribolini, Adriano Regattieri, Eleonora Isola, Ilaria Bini, Monica Zanchetta, Giovanni |
author_sort |
Sulpizio, Roberto |
title |
New findings of the Campanian Ignimbrite ash within slope deposits of the Treska valley (former Yugoslav Republic of Macedonia) |
title_short |
New findings of the Campanian Ignimbrite ash within slope deposits of the Treska valley (former Yugoslav Republic of Macedonia) |
title_full |
New findings of the Campanian Ignimbrite ash within slope deposits of the Treska valley (former Yugoslav Republic of Macedonia) |
title_fullStr |
New findings of the Campanian Ignimbrite ash within slope deposits of the Treska valley (former Yugoslav Republic of Macedonia) |
title_full_unstemmed |
New findings of the Campanian Ignimbrite ash within slope deposits of the Treska valley (former Yugoslav Republic of Macedonia) |
title_sort |
new findings of the campanian ignimbrite ash within slope deposits of the treska valley (former yugoslav republic of macedonia) |
publishDate |
2017 |
url |
http://hdl.handle.net/2122/11567 https://doi.org/10.3301/IJG.2016.16 |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_relation |
Italian Journal of Geosciences /136 (2017) http://hdl.handle.net/2122/11567 doi:10.3301/IJG.2016.16 |
op_rights |
restricted |
op_doi |
https://doi.org/10.3301/IJG.2016.16 |
container_title |
Italian Journal of Geosciences |
container_volume |
136 |
container_issue |
2 |
container_start_page |
198 |
op_container_end_page |
205 |
_version_ |
1766131181254868992 |