<?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>A.V. Milkov</dc:contributor>
  <dc:contributor>V.A. Soloviev</dc:contributor>
  <dc:contributor>A.V. Egorov</dc:contributor>
  <dc:contributor>G.A. Cherkashev</dc:contributor>
  <dc:contributor>P.R. Vogt</dc:contributor>
  <dc:contributor>K. Crane</dc:contributor>
  <dc:contributor>T.D. Lorenson</dc:contributor>
  <dc:contributor>M.D. Khutorskoy</dc:contributor>
  <dc:creator>G.D. Ginsburg</dc:creator>
  <dc:date>1999</dc:date>
  <dc:description>Gas hydrate (GH) accumulation is characterized and modeled for the Hakon Mosby mud volcano, ca. 1.5 km across, located on the Norway-Barents-Svalbard margin. Pore water chemical and isotopic results based on shallow sediment cores as well as geothermal and geomorphological data suggest that the GH accumulation is of a concentric pattern controlled by and formed essentially from the ascending mud volcano fluid. The gas hydrate content of sediment peaks at 25% by volume, averaging about 1.2% throughout the accumulation. The amount of hydrate methane is estimated at ca. 108 m3 STP, which could account for about 1-10% of the gas that has escaped from the volcano since its origin.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1007/s003670050093</dc:identifier>
  <dc:language>en</dc:language>
  <dc:title>Gas hydrate accumulation at the Hakon Mosby Mud Volcano</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>