<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:creator>Kapper, Lisa</dc:creator>
  <dc:creator>Donadini, Fabio</dc:creator>
  <dc:creator>Serneels, Vincent</dc:creator>
  <dc:creator>Tema, Evdokia</dc:creator>
  <dc:creator>Goguitchaichvili, Avto</dc:creator>
  <dc:creator>Morales, Juan Julio</dc:creator>
  <dc:date>2017-03-28</dc:date>
  <dc:description xmlns:ns0="xml" ns0:lang="en">We present absolute geomagnetic intensities from iron smelting furnaces discovered at  the metallurgical site of Korsimoro, Burkina Faso. Up to now, archaeologists  recognized four different types of furnaces based on different construction methods,  which were related to four subsequent time periods. Additionally, radiocarbon ages  obtained from charcoal confine the studied furnaces to ages ranging from 700–1700  AD, in good agreement with the archaeologically determined time periods for each type  of furnace. Archaeointensity results reveal three main groups of Arai diagrams. The  first two groups contain specimens with either linear Arai diagrams, or slightly curved  diagrams or two phases of magnetization. The third group encompasses specimens  with strong zigzag or curvature in their Arai diagrams. Specimens of the first two  groups were accepted after applying selection criteria to guarantee the high quality of  the results. Our data compared to palaeosecular variation curves show a similar  decreasing trend between 900–1500 AD. However, they reveal larger amplitudes at  around 800 AD and 1650 AD than the reference curves and geomagnetic field models.  Furthermore, they agree well with archaeomagnetic data from Mali and Senegal around  800 AD and with volcanic data around 1700 AD.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>https://folia.unifr.ch/global/documents/305369</dc:identifier>
  <dc:identifier>https://folia.unifr.ch/documents/305369/files/see_rgf.pdf</dc:identifier>
  <dc:language>eng</dc:language>
  <dc:relation>info:eu-repo/semantics/altIdentifier/doi/10.1038/srep45225</dc:relation>
  <dc:rights>info:eu-repo/semantics/openAccess</dc:rights>
  <dc:rights>License undefined</dc:rights>
  <dc:source>Scientific Reports. - 2017, vol. 7, p. 45225</dc:source>
  <dc:subject>info:eu-repo/classification/udc/55</dc:subject>
  <dc:title xmlns:ns1="xml" ns1:lang="en">Reconstructing the geomagnetic field in west africa: first absolute intensity results from Burkina Faso</dc:title>
  <dc:type>http://purl.org/coar/resource_type/c_6501</dc:type>
</oai_dc:dc>
