Archeomagnetic study of baked clays from a neolithic site in thessaly, Greece

Detalhes bibliográficos
Autor(a) principal: Skoulikari, Dimitra B
Data de Publicação: 2022
Tipo de documento: Dissertação
Idioma: eng
Título da fonte: Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos)
Texto Completo: http://hdl.handle.net/10174/31085
Resumo: Abstract The study conducted for this thesis was a classical archaeomagnetic study with the aim of obtaining archaeodirectional data to enrich the poorly covered Neolithic period in the Greek directional SVCs. Burnt clay samples, from the kiln complex at the Middle Neolithic site Koutroulou Magoula located in Thessaly, Greece, were studied. The grouping of the initial NRM measurements was satisfactory, thus indicating that the majority of the samples were burnt in situ. Stepwise thermal demagnetization was employed to isolate the ChRM of the samples, which in most cases revealed one characteristic component of magnetization. Rock magnetic measurements were also employed to access the mineralogical composition and stability of the sampled material. Specifically, thermomagnetic analysis and coercivity spectrum analysis (i.e., acquisition of isothermal remanent magnetization (IRM), indicated that the samples contained mainly low-coercivity magnetic minerals (such as magnetite or titanomagnetite). Some samples did contain a small portion of high-coercivity minerals as well, most likely haematite. Overall, the experimental procedures proved to be successful and the mean directions (declination – D, inclination – I, and confidence parameter - α95) for the site were calculated: D [°]= 6.9; I [°] = 55.9; and α95 [°] = 4.5. From the mean directions calculated a final date was purposed for the site by comparing the obtained directions to the Balkan and Neolithic reference curves. Date interval (Balkan curve) = 5463 – 5200 BC; date interval (Neolithic curve) = 5488 – 5187 BC, both at a 95% confidence level. Both dating intervals are similar suggesting a reliable date was obtained.
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spelling Archeomagnetic study of baked clays from a neolithic site in thessaly, GreeceArchaeomagnetismArchaeomagnetic datingArchaeodirectionsBurnt clayNeolithic PeriodGreeceAbstract The study conducted for this thesis was a classical archaeomagnetic study with the aim of obtaining archaeodirectional data to enrich the poorly covered Neolithic period in the Greek directional SVCs. Burnt clay samples, from the kiln complex at the Middle Neolithic site Koutroulou Magoula located in Thessaly, Greece, were studied. The grouping of the initial NRM measurements was satisfactory, thus indicating that the majority of the samples were burnt in situ. Stepwise thermal demagnetization was employed to isolate the ChRM of the samples, which in most cases revealed one characteristic component of magnetization. Rock magnetic measurements were also employed to access the mineralogical composition and stability of the sampled material. Specifically, thermomagnetic analysis and coercivity spectrum analysis (i.e., acquisition of isothermal remanent magnetization (IRM), indicated that the samples contained mainly low-coercivity magnetic minerals (such as magnetite or titanomagnetite). Some samples did contain a small portion of high-coercivity minerals as well, most likely haematite. Overall, the experimental procedures proved to be successful and the mean directions (declination – D, inclination – I, and confidence parameter - α95) for the site were calculated: D [°]= 6.9; I [°] = 55.9; and α95 [°] = 4.5. From the mean directions calculated a final date was purposed for the site by comparing the obtained directions to the Balkan and Neolithic reference curves. Date interval (Balkan curve) = 5463 – 5200 BC; date interval (Neolithic curve) = 5488 – 5187 BC, both at a 95% confidence level. Both dating intervals are similar suggesting a reliable date was obtained.Universidade de Évora2022-02-22T13:09:09Z2022-02-222022-01-17T00:00:00Zinfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/masterThesishttp://hdl.handle.net/10174/31085http://hdl.handle.net/10174/31085TID:202942759engDepartamento de HistóriaSchedimi@isu.edu709Skoulikari, Dimitra Binfo:eu-repo/semantics/openAccessreponame:Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos)instname:Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informaçãoinstacron:RCAAP2024-01-03T19:30:26Zoai:dspace.uevora.pt:10174/31085Portal AgregadorONGhttps://www.rcaap.pt/oai/openaireopendoar:71602024-03-20T01:20:25.500926Repositório Científico de Acesso Aberto de Portugal (Repositórios Cientìficos) - Agência para a Sociedade do Conhecimento (UMIC) - FCT - Sociedade da Informaçãofalse
dc.title.none.fl_str_mv Archeomagnetic study of baked clays from a neolithic site in thessaly, Greece
title Archeomagnetic study of baked clays from a neolithic site in thessaly, Greece
spellingShingle Archeomagnetic study of baked clays from a neolithic site in thessaly, Greece
Skoulikari, Dimitra B
Archaeomagnetism
Archaeomagnetic dating
Archaeodirections
Burnt clay
Neolithic Period
Greece
title_short Archeomagnetic study of baked clays from a neolithic site in thessaly, Greece
title_full Archeomagnetic study of baked clays from a neolithic site in thessaly, Greece
title_fullStr Archeomagnetic study of baked clays from a neolithic site in thessaly, Greece
title_full_unstemmed Archeomagnetic study of baked clays from a neolithic site in thessaly, Greece
title_sort Archeomagnetic study of baked clays from a neolithic site in thessaly, Greece
author Skoulikari, Dimitra B
author_facet Skoulikari, Dimitra B
author_role author
dc.contributor.author.fl_str_mv Skoulikari, Dimitra B
dc.subject.por.fl_str_mv Archaeomagnetism
Archaeomagnetic dating
Archaeodirections
Burnt clay
Neolithic Period
Greece
topic Archaeomagnetism
Archaeomagnetic dating
Archaeodirections
Burnt clay
Neolithic Period
Greece
description Abstract The study conducted for this thesis was a classical archaeomagnetic study with the aim of obtaining archaeodirectional data to enrich the poorly covered Neolithic period in the Greek directional SVCs. Burnt clay samples, from the kiln complex at the Middle Neolithic site Koutroulou Magoula located in Thessaly, Greece, were studied. The grouping of the initial NRM measurements was satisfactory, thus indicating that the majority of the samples were burnt in situ. Stepwise thermal demagnetization was employed to isolate the ChRM of the samples, which in most cases revealed one characteristic component of magnetization. Rock magnetic measurements were also employed to access the mineralogical composition and stability of the sampled material. Specifically, thermomagnetic analysis and coercivity spectrum analysis (i.e., acquisition of isothermal remanent magnetization (IRM), indicated that the samples contained mainly low-coercivity magnetic minerals (such as magnetite or titanomagnetite). Some samples did contain a small portion of high-coercivity minerals as well, most likely haematite. Overall, the experimental procedures proved to be successful and the mean directions (declination – D, inclination – I, and confidence parameter - α95) for the site were calculated: D [°]= 6.9; I [°] = 55.9; and α95 [°] = 4.5. From the mean directions calculated a final date was purposed for the site by comparing the obtained directions to the Balkan and Neolithic reference curves. Date interval (Balkan curve) = 5463 – 5200 BC; date interval (Neolithic curve) = 5488 – 5187 BC, both at a 95% confidence level. Both dating intervals are similar suggesting a reliable date was obtained.
publishDate 2022
dc.date.none.fl_str_mv 2022-02-22T13:09:09Z
2022-02-22
2022-01-17T00:00:00Z
dc.type.status.fl_str_mv info:eu-repo/semantics/publishedVersion
dc.type.driver.fl_str_mv info:eu-repo/semantics/masterThesis
format masterThesis
status_str publishedVersion
dc.identifier.uri.fl_str_mv http://hdl.handle.net/10174/31085
http://hdl.handle.net/10174/31085
TID:202942759
url http://hdl.handle.net/10174/31085
identifier_str_mv TID:202942759
dc.language.iso.fl_str_mv eng
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dc.relation.none.fl_str_mv Departamento de História
Schedimi@isu.edu
709
dc.rights.driver.fl_str_mv info:eu-repo/semantics/openAccess
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dc.publisher.none.fl_str_mv Universidade de Évora
publisher.none.fl_str_mv Universidade de Évora
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