Abstract
Pyrolysates of the organic carbon-rich and oil-prone rocks of the Kimmeridge Clay Formation (KCF) are dominated by a sulfur-rich unresolved complex mixture (UCM). Structural characterization of this UCM by preparative capillary gas chromatography, gas chromatography (GC), gas chromatography/mass spectrometry (GC/MS), isotope-ratio-monitoring GC/MS, elemental analysis, nuclear magnetic resonance spectroscopy, and Fourier
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