<?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>J.G. Blank</dc:contributor>
  <dc:contributor>A.F. Goncharov</dc:contributor>
  <dc:contributor>Ho-kwang Mao</dc:contributor>
  <dc:contributor>R.J. Hemley</dc:contributor>
  <dc:creator>I.-M. Chou</dc:creator>
  <dc:date>1998</dc:date>
  <dc:description>A previously unknown solid phase of H2O has been identified by its peculiar growth patterns, distinct pressure-temperature melting relations, and vibrational Raman spectra. Morphologies of ice crystals and their pressure-temperature melting relations were directly observed in a hydrothermal diamond-anvil cell for H2O bulk densities between 1203 and 1257 kilograms per cubic meter at temperatures between -10??and 50??C. Under these conditions, four different ice forms were observed to melt: two stable phases, ice V and ice VI, and two metastable phases, ice IV and the new ice phase. The Raman spectra and crystal morphology are consistent with a disordered anisotropic structure with some similarities to ice VI.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1126/science.281.5378.809</dc:identifier>
  <dc:language>en</dc:language>
  <dc:title>In situ observations of a high-pressure phase of H2O ice</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>