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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Institutionen för ekologi, miljö och geovetenskap
2012
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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 |
_version_ |
1779321462879944704 |