Particle size analysis for samples from three last glacial cycle loess-palaeosol profiles along a northwestsoutheast transection
on the Chinese Loess Plateau has been carried out. The paleoclimatic significance of grain size indices has been obtained
by analyzing the fraction content variations and their comparisons with global ice volume and solar radiation variations.
The results show that (i) paleoclimatic significance of the grain size indices of loess-palaeosol deposit is different with
grain size fraction content and sampling points in Chinese Loess Plateau; (ii) the sub-coarse grain fraction is a good proxy
index of East Asia winter monsoon strength and therefore can be used to detect the global climate changes; (iii) the content
of sub-fine and fine grain fractions is influenced by both the input of sub-coarse grain fraction and pedogenesis; (iv) the
sub-coarse fraction exhibits a negative relationship with the sub-fine and fine fractlon.
Project supported by the 9.5 major project of Chinese Academy of Sciences and the open grant of the State Key Laboratory of
Loess and Quaternary Geology, Chinese Academy of Sciences. 相似文献
Well che89, located in the Chepaizi area in the northwest margin of Junggar basin, acquires high production industrial oil flow, which is an important breakthrough in the exploration of the south foreland slope area of Junggar basin. The Chepaizi area is near two hydrocarbon generation depressions of Sikeshu and Shawan, which have sets of hydrocarbon source rock of Carboniferous to Jurassic as well as Upper Tertiary. Geological and geochemical parameters are proper for the accumulation of mixed source crude oil. Carbon isotope, group composition and biomarkers of crude oil in Upper Tertiary of well Che89 show that the features of crude oil in Upper Tertiary Shawan Formation are between that of Permian and Jurassic, some of them are similar to these two, and some are of difference, they should be the mixed source of Permian and Jurassic. Geochemical analysis and geological study show that sand extract of Lower Tertiary Wulunguhe Formation has the same source as the crude oil and sand extract of Upper Tertiary Shawan Formation, but they are not charged in the same period. Oil/gas of Wulunguhe Formation is charged before Upper Tertiary sedimentation, and suffered serious biodegradation and oxidation and rinsing, which provide a proof in another aspect that the crude oil of Upper Tertiary Shawan Formation of well Che89 is not from hydrocarbon source rock of Lower Tertiary.
