<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>Kjær, Kurt H.</dc:creator>
  <dc:creator>Larsen, Nicolaj K.</dc:creator>
  <dc:creator>Binder, Tobias</dc:creator>
  <dc:creator>Bjørk, Anders A.</dc:creator>
  <dc:creator>Eisen, Olaf</dc:creator>
  <dc:creator>Fahnestock, Mark A.</dc:creator>
  <dc:creator>Funder, Svend</dc:creator>
  <dc:creator>Garde, Adam A.</dc:creator>
  <dc:creator>Haack, Henning</dc:creator>
  <dc:creator>Helm, Veit</dc:creator>
  <dc:creator>Houmark-Nielsen, Michael</dc:creator>
  <dc:creator>Kjeldsen, Kristian K.</dc:creator>
  <dc:creator>Khan, Shfaqat A.</dc:creator>
  <dc:creator>Machguth, Horst</dc:creator>
  <dc:creator>McDonald, Iain</dc:creator>
  <dc:creator>Morlighem, Mathieu</dc:creator>
  <dc:creator>Mouginot, Jérémie</dc:creator>
  <dc:creator>Paden, John D.</dc:creator>
  <dc:creator>Waight, Tod E.</dc:creator>
  <dc:creator>Weikusat, Christian</dc:creator>
  <dc:creator>Willerslev, Eske</dc:creator>
  <dc:creator>MacGregor, Joseph A.</dc:creator>
  <dc:date>2018-11-01</dc:date>
  <dc:description xmlns:ns0="xml" ns0:lang="en">We report the discovery of a large impact crater beneath Hiawatha Glacier in  northwest Greenland. From airborne radar surveys, we identify a 31-kilometer-wide,  circular bedrock depression beneath up to a kilometer of ice. This depression has an  elevated rim that cross-cuts tributary subglacial channels and a subdued central uplift  that appears to be actively eroding. From ground investigations of the deglaciated  foreland, we identify overprinted structures within Precambrian bedrock along the ice  margin that strike tangent to the subglacial rim. Glaciofluvial sediment from the largest  river draining the crater contains shocked quartz and other impact-related grains.  Geochemical analysis of this sediment indicates that the impactor was a fractionated  iron asteroid, which must have been more than a kilometer wide to produce the  identified crater. Radiostratigraphy of the ice in the crater shows that the Holocene ice  is continuous and conformable, but all deeper and older ice appears to be debris rich  or heavily disturbed. The age of this impact crater is presently unknown, but from our  geological and geophysical evidence, we conclude that it is unlikely to predate the  Pleistocene inception of the Greenland Ice Sheet.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>https://folia.unifr.ch/global/documents/307201</dc:identifier>
  <dc:identifier>https://folia.unifr.ch/documents/307201/files/mac_lic.pdf</dc:identifier>
  <dc:language>eng</dc:language>
  <dc:relation>info:eu-repo/semantics/altIdentifier/doi/10.1126/sciadv.aar8173</dc:relation>
  <dc:rights>info:eu-repo/semantics/openAccess</dc:rights>
  <dc:rights>License undefined</dc:rights>
  <dc:source>Science Advances. - 2018, vol. 4, no. 11, p. eaar8173</dc:source>
  <dc:subject>info:eu-repo/classification/udc/55</dc:subject>
  <dc:title xmlns:ns1="xml" ns1:lang="en">A large impact crater beneath Hiawatha Glacier in northwest Greenland</dc:title>
  <dc:type>http://purl.org/coar/resource_type/c_6501</dc:type>
</oai_dc:dc>
