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Thermal alteration of young kerogen in relation to petroleum genesisKerogen, humic acid, and lipid material were separated from a young marine sediment and heated in sealed tubes in a nitrogen atmosphere at 150 and 410 C. Gaseous and liquid products generated during heating, and also the residual organic material, were characterized by gas-liquid chromatography, elemental analysis, infrared and electron spin resonance spectroscopy, and X-ray diffraction.
Document ID
19770032192
Acquisition Source
Legacy CDMS
Document Type
Reprint (Version printed in journal)
External Source(s)
doi:10.1038/264347a0
Authors
Ishiwatari, R. (California Univ. Los Angeles, CA, United States)
Ishiwatari, M. (California Univ. Los Angeles, CA, United States)
Kaplan, I. R. (California Univ. Los Angeles, CA, United States)
Rohrback, B. G. (California, University Los Angeles, Calif., United States)
Date Acquired
August 9, 2013
Publication Date
November 25, 1976
Publication Information
Publication: Nature
Volume: 264
Subject Category
Energy Production And Conversion
Accession Number
77A15044
Distribution Limits
Public
Copyright
Other

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