Previous studies have shown structural similarities between kerogens and asphaltenes from chloroform extracts of the same rocks. Migrated oils contain a small asphaltenes fraction, which obviously must bear a relationship to the asphaltenes remaining in the source rock. In this work, investigations were extended to the joint study of kerogens, asphaltenes remaining in the source rock and asphaltenes from migrated oils. Gas chromatographic traces of total pyrolysates from kerogens, rock-extract asphaltenes and oil asphaltenes show a striking similarity, which indicates a common origin of the major components in the gas chromatographic traces. This simple examination cannot be used for compounds present in small amounts, even if they are especially informative, as with C 25-C 35 polycyclics. These compounds were therefore studied by gas chromatography-mass spectrometry. Some hydrocarbon families were distinguished, viz., tri-, tetra- and pentacyclics, which constitute remnants of biological structures, the so-called biochemical fossils. Their distributions are closely similar. The results indicate a general structural similarity between kerogens and asphaltenes from both source rocks and reservoired oils. The main difference is in the size of the macromolecular units, kerogen units being the largest and most condensed, oil asphaltenes the smallest and least condensed.
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