<?xml version='1.0' encoding='utf-8'?>
<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:contributor>P.C. Jones</dc:contributor>
  <dc:contributor>P. Leat</dc:contributor>
  <dc:contributor>T.A. Jordan</dc:contributor>
  <dc:creator>Fausto Ferraccioli</dc:creator>
  <dc:date>2007</dc:date>
  <dc:description>The polar regions play an important role in Earth's geodynamic and climatic systems. Modern airborne
geophysical surveys combine radio-echo sounding, aeromagnetic and aerogravity methods to explore the geology of
these regions. This paper reviews some recent aerogeophysical investigations undertaken by the British Antarctic
Survey to: 1) Image subglacial rifts of Jurassic age in western Dronning Maud Land, which were associated with early
Gondwana break-up; 2) Investigate crustal growth over the Antarctic Peninsula by Cretaceous arc magmatism and
terrane accretion along the paleo-Pacific margin of Gondwana; 3) Analyse geological boundary conditions for presentday
ice dynamics over Coats Land.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/ofr20071047SRP056</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Airborne geophysics as a tool for geoscientific research in Antarctica: some recent examples</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>