<?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:creator>R. Sutherland</dc:creator>
  <dc:date>2007</dc:date>
  <dc:description>Antarctica has geometric significance for global plate kinematic studies, because it links seafloor spreading systems of 
the African hemisphere (Indian and Atlantic Oceans) with 
those of the Pacific. Inferences of plate motions back to 44 
Ma, around the onset of rapid spreading south of Australia 
and formation of a new boundary through New Zealand, are 
consistent with Antarctic rifting and formation of the Adare 
Basin during 44-26 Ma (i.e., no additional plate motions 
are required in the South Pacific). The time period 52-44 
Ma represents a profound global and South Pacific tectonic 
change, and significant details remain unresolved. For 74 Ma 
a significant nonclosure of the South Pacific plate-motion circuit is identified if Antarctic motion is not included. Alternate 
inferences of motion through Antarctica during the interval 
74-44 Ma imply significantly different subduction volumes 
and directions around the Pacific, and imply different relative 
motions between hotspots</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/ofr20071047KP10</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>National Academies Press</dc:publisher>
  <dc:title>The significance of Antarctica for studies of global geodynamics</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>