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   <identifier identifierType="DOI">10.1594/GFZ.SDDB.1426</identifier>
   <creators>
      <creator>
         <creatorName>KTB, WG Geochemistry</creatorName>
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   <titles>
      <title>Gas chromatography of gas samples of the KTB main hole HB1g</title>
   </titles>
   <publisher>Deutsches GeoForschungsZentrum GFZ</publisher>
   <publicationYear>2010</publicationYear>
   <subjects>
      <subject subjectScheme="project">German Continental Deep Drilling Program</subject>
      <subject subjectScheme="platform">Land based</subject>
      <subject subjectScheme="keyword">C2H6</subject>
      <subject subjectScheme="keyword">C3H8</subject>
      <subject subjectScheme="keyword">C4H10</subject>
      <subject subjectScheme="keyword">CH4</subject>
      <subject subjectScheme="keyword">Date of Sampling</subject>
      <subject subjectScheme="keyword">gas chromatography</subject>
   </subjects>
   <dates>
      <date dateType="Issued">2010-09-29</date>
   </dates>
   <language>eng</language>
   <resourceType resourceTypeGeneral="Dataset">Dataset</resourceType>
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   <descriptions>
      <description descriptionType="Abstract">The main objective of this drilling fluid analysis was the detection of inflows of formation fluids. Therefore different gases dissolved in the drilling mud were measured continuously and automatically at drill site with three different methodes (Fig.: KTB-Report 92-2 page C13). The operation principles of the mass spectrometer and the gaschromatograph have been explained by STROH et al. (1988) and FIGGEMEIER et al. (1991). The principle of radon determination is published by ERZINGER et al. (1992). 
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