Tephrochronology : Methodology and correlations, Antarctic Peninsula Area

Abstract Methods for tephrochronology are evaluated, in the following way: Lake sediments <500 years old from three small Antarctic lakes were analysed for identification of tephras. Subsamples were analysed for a) grain size, and identification and concentration of volcanogenic grains, b) identi...

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Main Author: Molén, Mats
Format: Bachelor Thesis
Language:English
Published: Institutionen för ekologi, miljö och geovetenskap 2012
Subjects:
Online Access:http://urn.kb.se/resolve?urn=urn:nbn:se:umu:diva-61327
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spelling ftumeauniv:oai:DiVA.org:umu-61327 2023-10-09T21:45:49+02:00 Tephrochronology : Methodology and correlations, Antarctic Peninsula Area Molén, Mats 2012 application/pdf http://urn.kb.se/resolve?urn=urn:nbn:se:umu:diva-61327 eng eng Institutionen för ekologi, miljö och geovetenskap http://urn.kb.se/resolve?urn=urn:nbn:se:umu:diva-61327 info:eu-repo/semantics/openAccess Tephrochronology Antarctica Molén Zale Deception Island LA-ICP-MS EDS WDS SEM Earth and Related Environmental Sciences Geovetenskap och miljövetenskap Student thesis info:eu-repo/semantics/bachelorThesis text 2012 ftumeauniv 2023-09-22T13:46:00Z Abstract Methods for tephrochronology are evaluated, in the following way: Lake sediments <500 years old from three small Antarctic lakes were analysed for identification of tephras. Subsamples were analysed for a) grain size, and identification and concentration of volcanogenic grains, b) identification of tephra horizons, c) element abundance by EPMA WDS/EDS and LA-ICP-MS, and d) possible correlations between lakes and volcanoes. Volcanogenic minerals and shards were found all through the sediment cores in all three lakes, in different abundances. A high background population of volcanogenic mineral grains, in all samples, made the identification of tephra horizons difficult, and shards could only be distinguished by certainty after chemical analysis of elements. The tephra layers commonly could not be seen by the naked eye, and, hence they are regarded as cryptotephras. Because of the small size of recent eruptions in the research area, and the travel distance of ash, most shards are small and difficult to analyse. Nine possible tephra horizons have been recorded in the three lakes, and preliminary correlations have been made. But because of analytical problems, the proposed correlations between the lakes and possible volcanic sources are preliminary. Bachelor Thesis Antarc* Antarctic Antarctic Peninsula Antarctica Deception Island Umeå University: Publications (DiVA) Antarctic Antarctic Peninsula Deception Island ENVELOPE(-60.633,-60.633,-62.950,-62.950)
institution Open Polar
collection Umeå University: Publications (DiVA)
op_collection_id ftumeauniv
language English
topic Tephrochronology Antarctica Molén Zale Deception Island LA-ICP-MS EDS WDS SEM
Earth and Related Environmental Sciences
Geovetenskap och miljövetenskap
spellingShingle Tephrochronology Antarctica Molén Zale Deception Island LA-ICP-MS EDS WDS SEM
Earth and Related Environmental Sciences
Geovetenskap och miljövetenskap
Molén, Mats
Tephrochronology : Methodology and correlations, Antarctic Peninsula Area
topic_facet Tephrochronology Antarctica Molén Zale Deception Island LA-ICP-MS EDS WDS SEM
Earth and Related Environmental Sciences
Geovetenskap och miljövetenskap
description Abstract Methods for tephrochronology are evaluated, in the following way: Lake sediments <500 years old from three small Antarctic lakes were analysed for identification of tephras. Subsamples were analysed for a) grain size, and identification and concentration of volcanogenic grains, b) identification of tephra horizons, c) element abundance by EPMA WDS/EDS and LA-ICP-MS, and d) possible correlations between lakes and volcanoes. Volcanogenic minerals and shards were found all through the sediment cores in all three lakes, in different abundances. A high background population of volcanogenic mineral grains, in all samples, made the identification of tephra horizons difficult, and shards could only be distinguished by certainty after chemical analysis of elements. The tephra layers commonly could not be seen by the naked eye, and, hence they are regarded as cryptotephras. Because of the small size of recent eruptions in the research area, and the travel distance of ash, most shards are small and difficult to analyse. Nine possible tephra horizons have been recorded in the three lakes, and preliminary correlations have been made. But because of analytical problems, the proposed correlations between the lakes and possible volcanic sources are preliminary.
format Bachelor Thesis
author Molén, Mats
author_facet Molén, Mats
author_sort Molén, Mats
title Tephrochronology : Methodology and correlations, Antarctic Peninsula Area
title_short Tephrochronology : Methodology and correlations, Antarctic Peninsula Area
title_full Tephrochronology : Methodology and correlations, Antarctic Peninsula Area
title_fullStr Tephrochronology : Methodology and correlations, Antarctic Peninsula Area
title_full_unstemmed Tephrochronology : Methodology and correlations, Antarctic Peninsula Area
title_sort tephrochronology : methodology and correlations, antarctic peninsula area
publisher Institutionen för ekologi, miljö och geovetenskap
publishDate 2012
url http://urn.kb.se/resolve?urn=urn:nbn:se:umu:diva-61327
long_lat ENVELOPE(-60.633,-60.633,-62.950,-62.950)
geographic Antarctic
Antarctic Peninsula
Deception Island
geographic_facet Antarctic
Antarctic Peninsula
Deception Island
genre Antarc*
Antarctic
Antarctic Peninsula
Antarctica
Deception Island
genre_facet Antarc*
Antarctic
Antarctic Peninsula
Antarctica
Deception Island
op_relation http://urn.kb.se/resolve?urn=urn:nbn:se:umu:diva-61327
op_rights info:eu-repo/semantics/openAccess
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