<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>Andjić, Goran</dc:creator>
  <dc:creator>Escuder‐Viruete, Javier</dc:creator>
  <dc:creator>Baumgartner‐Mora, Claudia</dc:creator>
  <dc:creator>Baumgartner, Peter O.</dc:creator>
  <dc:creator>Mitchell, Simon F.</dc:creator>
  <dc:creator>Caron, Michèle</dc:creator>
  <dc:creator>Caus, Esmeralda</dc:creator>
  <dc:date>2019</dc:date>
  <dc:description xmlns:ns0="xml" ns0:lang="en">The western margin of the Caribbean Plate is a typical example where oceanic and  continental terranes have amalgamated by subduction, collision, and strike‐slip  processes. The boundaries between these blocks, as well as their tectonostratigraphic  records, are generally covered by younger deposits and dense tropical vegetation,  which may hamper reconstructing the accretionary evolution of the convergent  margin. In that context, the study of overlap sedimentary assemblages represents an  important tool to constrain the accretion timing of terranes. In northern Central  America, the geology of the suture zone between the Chortis Block and the exotic  Siuna Intraoceanic Arc indicates that the two terranes were assembled together  during a Hauterivian arc‐continent collision (approximately 134–131 Ma). The exotic  origin of the intraoceanic arc is based on the nature of metamorphic blocks within and  the kinematics of the Siuna Serpentinite Mélange. The short duration of the collision  event is suggested by coeval exhumation of the Siuna Serpentinite Mélange and  Chortis‐derived coarse sedimentation (El Amparo Formation) along the suture zone,  rapidly followed by onset of pelagic sedimentation (Rio Matis Formation). Although the  collision appears to have been short lived and preserved only in the suture zone,  postcollisional extension affected intra‐arc to back‐arc settings of the Chortis Block  and led to the formation of kilometer‐thick extensional basins. We envisage that the  convergent margin inboard of SW Mexico—represented by the fringing Guerrero  Intraoceanic Arc and the Mixteca continental terrane—underwent similar  postcollisional extension, whereas the western margin of the proto‐Caribbean oceanic  realm experienced onset of WSW dipping subduction beneath the accreted Siuna  Intraoceanic Arc.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>https://folia.unifr.ch/global/documents/308290</dc:identifier>
  <dc:identifier>https://folia.unifr.ch/documents/308290/files/car_sra.pdf</dc:identifier>
  <dc:language>eng</dc:language>
  <dc:relation>info:eu-repo/semantics/altIdentifier/doi/10.1029/2019TC005741</dc:relation>
  <dc:rights>info:eu-repo/semantics/openAccess</dc:rights>
  <dc:rights>License undefined</dc:rights>
  <dc:source>Tectonics. - 2019, vol. 38, no. 12, p. 4399–4425</dc:source>
  <dc:subject>info:eu-repo/classification/udc/55</dc:subject>
  <dc:title xmlns:ns1="xml" ns1:lang="en">Sedimentary record of arc-continent collision along mesozoic SW north america (Siuna belt, Nicaragua)</dc:title>
  <dc:type>http://purl.org/coar/resource_type/c_6501</dc:type>
</oai_dc:dc>
