<?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>V.A. Soloviev</dc:contributor>
  <dc:contributor>R.E. Cranston</dc:contributor>
  <dc:contributor>T.D. Lorenson</dc:contributor>
  <dc:contributor>K.A. Kvenvolden</dc:contributor>
  <dc:creator>G.D. Ginsburg</dc:creator>
  <dc:date>1993</dc:date>
  <dc:description>Ten gas-vent fields were discovered in the Okhotsk Sea on the northeast continental slope offshore from Sakhalin Island in water depths of 620-1040 m. At one vent field, estimated to be more than 250 m across, gas hydrates, containing mainly microbial methane (??13C = -64.3???), were recovered from subbottom depths of 0.3-1.2 m. The sediment, having lenses and bedded layers of gas hydrate, contained 30-40% hydrate per volume of wet sediment. Although gas hydrates were not recovered at other fields, geochemical and thermal measurements suggest that gas hydrates are present. ?? 1993 Springer-Verlag.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1007/BF01204391</dc:identifier>
  <dc:language>en</dc:language>
  <dc:title>Gas hydrates from the continental slope, offshore Sakhalin Island, Okhotsk Sea</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>