摘要
The 22S/(22S + 22R) ratios for C31–C35 homohopanes and the 20S/(20S + 20R) ratio for C29 steranes were measured by gas chromatography–mass spectrometry (GC–MS) on six Oligocene saline lacustrine rock samples from a borehole located in the western Qaidam Basin, northwest China. These ratios vary significantly and irregularly with burial depth from 2831 m to 3054 m around the threshold of the oil generation window. In addition, 22S/(22S + 22R) ratios also vary substantially among different homologs within the same sample, generally decreasing from C31 to C35 homohopanes. The distribution patterns of homohopanes for the six samples are unusual, such as, C31 < C32 > C33 > C34 < C35, or C31 > C32 > C33 < C34 < C35, or C31 < C32 > C33 < C34 < C35. All of these observations can be mainly ascribed to the release of bound hopanes and steranes from kerogen and other macromolecules.