<?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>E. Stolper</dc:contributor>
  <dc:contributor>D. Thomas</dc:contributor>
  <dc:contributor>F. Albarede</dc:contributor>
  <dc:contributor>O. Chadwick</dc:contributor>
  <dc:contributor>D. Clague</dc:contributor>
  <dc:contributor>M. Feigenson</dc:contributor>
  <dc:contributor>F. Frey</dc:contributor>
  <dc:contributor>M. Garcia</dc:contributor>
  <dc:contributor>A. Hofmann</dc:contributor>
  <dc:contributor>B.L. Ingram</dc:contributor>
  <dc:contributor>B. M. Kennedy</dc:contributor>
  <dc:contributor>J. Kirschvink</dc:contributor>
  <dc:contributor>M. Kurz</dc:contributor>
  <dc:contributor>Carlo Laj</dc:contributor>
  <dc:contributor>J. Lockwood</dc:contributor>
  <dc:contributor>K. Ludwig</dc:contributor>
  <dc:contributor>T. McEvilly</dc:contributor>
  <dc:contributor>R. Moberly</dc:contributor>
  <dc:contributor>G. Moore</dc:contributor>
  <dc:contributor>Jeff Moore</dc:contributor>
  <dc:contributor>R. Morin</dc:contributor>
  <dc:contributor>F. Paillet</dc:contributor>
  <dc:contributor>P. Renne</dc:contributor>
  <dc:contributor>M. Rhodes</dc:contributor>
  <dc:contributor>M. Tatsumoto</dc:contributor>
  <dc:contributor>H. Taylor</dc:contributor>
  <dc:contributor>G. Walker</dc:contributor>
  <dc:contributor>R. Wilkins</dc:contributor>
  <dc:creator>D. DePaolo</dc:creator>
  <dc:date>1996</dc:date>
  <dc:description>&lt;p&gt;Petrological, geochemical, geomagnetic, and volcanological characterization of the recovered core from a 1056-m-deep well into the flank of the Mauna Kea volcano in Hilo, Hawaii, and downhole logging and fluid sampling have provided a unique view of the evolution and internal structure of a major oceanic volcano unavailable from surface exposures. Core recovery was ~90%, yielding a time series of fresh, subaerial lavas extending back to ~400 ka. Results of this 1993 project provide a basis for a more ambitious project to core drill a well 4.5 km deep in a nearby location with the goal of recovering an extended, high-density stratigraphic sequence of lavas.&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:language>en</dc:language>
  <dc:publisher>Geological Society of America</dc:publisher>
  <dc:title>Hawaii scientific drilling protect: Summary of preliminary results</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>