<?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>R. A. Robie</dc:contributor>
  <dc:contributor>J.A. Kittrick</dc:contributor>
  <dc:contributor>E.S. Grew</dc:contributor>
  <dc:contributor>J.A. Nelen</dc:contributor>
  <dc:contributor>D. London</dc:contributor>
  <dc:creator>B. S. Hemingway</dc:creator>
  <dc:date>1984</dc:date>
  <dc:description>Modifications to an automated low-T, adiabatic calorimeter are described. Thermodynamic data obtained with this instrument are reported for minerals from metamorphic terrains. (U.S. Bureau of Mines Report of Investigations 8451)-J.A.Z.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:language>en</dc:language>
  <dc:title>The heat capacities of osumilite from 298.15 to 1000 K, the thermodynamic properties of two natural chlorites to 500 K, and the thermodynamic properties of petalite to 1800 K.</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>