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.
A multiple time scale perturbation method is used to discuss the Lagrangian residual current and residual transport on the
basis of a weakly nonlinear dynamic model of shallow seas. The governing equations for the long-term variation of zero order
“apparent concentration” (which is a linear combination of salinity, temperature of seawater and the concentration of any
tracer which is conservative and passive) and its mean value over tidal cycles are obtained for the system with single tidal
constituent, and for the one with multi-constituents, winds and thermohaline. The equations for the two cases are in the same
form and show this long-term variation resulted from the cumulative effect of residual convection and turbulent diffusion.
The multiple time scale variation of current is caused by tides, winds, and the thermohaline and the nonlinear effects of
the system. The derived set of governing field equations of the Lagrangian current for this multiple time scale system is
also in the same form as that for a single time scale system. 相似文献
We investigate the relationship between the rise width and the full width of gamma-ray burst pulses.Theoretical analysis shows that either width is proportional to Γ~(-2)Δ_(Тθ),FWHM(RRc)/c(Γ the Lorentz factor of the bulk motion,Δ_(Тθ),FWHM a local pulse's width,R_c the radius of fireballs and c the velocity of light).We study the relationship for four samples of observed pulses.We find:(1)merely the curvature effect could reproduce the relationship between the rise and full widths with the same slope as derived from the model of Qin et al.;(2)gamma-ray burst pulses,selected from both the short and long GRBs,follow the same sequence in the rise width vs. full width diagram,with the shorter pulses at one end;(3)all GRBs may intrinsically result from local Gaussian pulses.These features place constraints on the physical mechanism(s)for producing long and short GRBs. 相似文献