<rdf:RDF xmlns:rdf="http://www.openarchives.org/OAI/2.0/rdf/" xmlns:ow="http://www.ontoweb.org/ontology/1#" xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ds="http://dspace.org/ds/elements/1.1/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns:doc="http://www.lyncode.com/xoai" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/rdf/ http://www.openarchives.org/OAI/2.0/rdf.xsd">
   <ow:Publication rdf:about="oai:digibug.ugr.es:10481/61805">
      <dc:title>Deciphering the metamorphic evolution of the Pulo do Lobo metasedimentary domain (SW Iberian Variscides)</dc:title>
      <dc:creator>Pérez Cáceres, Irene</dc:creator>
      <dc:creator>Martínez Poyatos, David Jesús</dc:creator>
      <dc:creator>Vidal, Olivier</dc:creator>
      <dc:creator>Beyssac, Olivier</dc:creator>
      <dc:creator>Nieto García, Fernando</dc:creator>
      <dc:creator>Simancas Cabrera, José Fernando</dc:creator>
      <dc:creator>Azor Pérez, Antonio</dc:creator>
      <dc:creator>Bourdelle, Franck</dc:creator>
      <dc:description>The Pulo do Lobo domain is one of the units exposed&#xd;
within the orogenic suture zone between the Ossa-&#xd;
Morena and the South Portuguese zones in the SW Iberian&#xd;
Variscides. This metasedimentary unit has been classically&#xd;
interpreted as a Rheic subduction-related accretionary prism&#xd;
formed during pre-Carboniferous convergence and eventual&#xd;
collision between the South Portuguese Zone (part of Avalonia)&#xd;
and the Ossa-Morena Zone (peri-Gondwanan terrane).&#xd;
Discrete mafic intrusions also occur within the dominant&#xd;
Pulo do Lobo metapelites, related to an intra-orogenic Mississippian&#xd;
transtensional and magmatic event that had a significant&#xd;
thermal input. Three different approaches have been&#xd;
applied to the Devonian–Carboniferous phyllites and slates&#xd;
of the Pulo do Lobo domain in order to study their poorly&#xd;
known low-grade metamorphic evolution. X-ray diffraction&#xd;
(XRD) was used to identify the mineralogy and measure&#xd;
crystallographic parameters (illite “crystallinity” and Kwhite&#xd;
mica b-cell dimension). Compositional maps of selected&#xd;
samples were obtained from electron probe microanalysis,&#xd;
which allowed for processing with XMapTools&#xd;
software, and chlorite semiempirical and thermodynamic&#xd;
geothermometry was performed. Thermometry based on Raman&#xd;
spectroscopy of carbonaceous material (RSCM) was&#xd;
used to obtain peak temperatures.</dc:description>
      <dc:date>2020-05-05T11:49:32Z</dc:date>
      <dc:date>2020-05-05T11:49:32Z</dc:date>
      <dc:date>2020-04-03</dc:date>
      <dc:type>journal article</dc:type>
      <dc:identifier>Pérez-Cáceres, I., Martínez Poyatos, D., Vidal, O., Beyssac, O., Nieto, F., Simancas, J. F., ... &amp; Bourdelle, F. (2020). Deciphering the metamorphic evolution of the Pulo do Lobo metasedimentary domain (SW Iberian Variscides).</dc:identifier>
      <dc:identifier>http://hdl.handle.net/10481/61805</dc:identifier>
      <dc:identifier>10.5194/se-11-469-2020</dc:identifier>
      <dc:language>eng</dc:language>
      <dc:rights>http://creativecommons.org/licenses/by/3.0/es/</dc:rights>
      <dc:rights>open access</dc:rights>
      <dc:rights>Atribución 3.0 España</dc:rights>
      <dc:publisher>European Geosciences Union</dc:publisher>
   </ow:Publication>
</rdf:RDF>