<?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>C. Gaina</dc:contributor>
  <dc:contributor>T.F. Redfield</dc:contributor>
  <dc:creator>T.H. Torsvik</dc:creator>
  <dc:date>2007</dc:date>
  <dc:description>Neoproterozoic Rodinia reconstructions associate East Antarctica (EANT) with cratonic Western Australia. By further 
linking EANT to both Gondwana and Pangea with relative 
plate circuits, a Synthetic Apparent Polar Wander (SAPW) 
path for EANT is calculated. This path predicts that EANT 
was located at tropical to subtropical southerly latitudes from 
ca. 1 Ga to 420 Ma. Around 400 Ma and again at 320 Ma, 
EANT underwent southward drift. Ca. 250 Ma Antarctica 
voyaged briefly north but headed south again ca. 200 Ma. 
Since 75 Ma EANT became surrounded by spreading centers 
and has remained extremely stable. Although paleomagnetic 
data of the blocks that embrace West Antarctica are sparse, 
we attempt to model their complex kinematics since the 
Mesozoic. Together with the SAPW path and a revised 
circum-Antarctic seafloor spreading history we construct a 
series of new paleogeographic maps.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/ofr20071047KP11</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>National Academies Press</dc:publisher>
  <dc:title>Antarctica and global paleogeography: from Rodinia, rhrough Gondwanaland and Pangea, to the birth of the Southern Ocean and the opening of gateways</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>