<?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>James H. Dieterich</dc:contributor>
  <dc:contributor>A.T. Okamura</dc:contributor>
  <dc:contributor>Asta Mikijus</dc:contributor>
  <dc:creator>V. Cayol</dc:creator>
  <dc:date>2000</dc:date>
  <dc:description>After a magnitude 7.2 earthquake in 1975 and before the start of the ongoing eruption in 1983, deformation of Kilauea volcano was the most rapid ever recorded. Three-dimensional numerical modeling shows that this deformation is consistent with the dilation of a dike within Kilauea's rift zones coupled with creep over a narrow area of a low-angle fault beneath the south flank. Magma supply is estimated to be 0.18 cubic kilometers per year, twice that of previous estimates. The 1983 eruption may be a direct consequence of the high rates of magma storage within the rift zone that followed the 1975 earthquake.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1126/science.288.5475.2343</dc:identifier>
  <dc:language>en</dc:language>
  <dc:title>High magma storage rates before the 1983 eruption of Kilauea, Hawaii</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>