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351.
本文在分析新疆对中亚五国的外贸结构基础上,阐述了目前在与中亚五国的贸易中存在的一些问题,提出相应的对策建议,以推动新疆与中亚五国外贸发展的良性循环。 相似文献
352.
Study on the Gravity Field and Deep-Seated Crustal Structure at the North Margin of the Qinghai-Tibet Plateau 总被引:1,自引:0,他引:1
MENG Lingshun 《Continental Dynamics》1997,(1)
1.I~ductionThenorthernmarginoftheQinghai-TibetplateauincludestheAltllnMis.,theQilianMis.,KunlunMis.,theQaidambasinandthesouthernTarimbasin.ThisareaistCctonicallycharacterizedbyintensiveCenozoicdeformationwithcomplicateddeformationalmechedsm(Molnaretal.,1987;Zheng,1991;Culetal.,1994;Ding,1995andXuetal.,1996).Thedeformationalmechanismsincludethrust-napping,strike-slipping,extensionandblockrotation,aswellassimultaneousupliftingandtypicalbasin-rangetectonics(CulandXu,1996).IntermsofCenozoi… 相似文献
353.
1.IntroductionUntilnowTibetisstillthearchetypalregionwithcontinentalcollisiongoingoninit,henceitisanidealnaturallaboratoryforstudyingthegeologicevolutionofintracontinentalorogenicbeltandthecrust-mantledeepprocesses,aswellastheinteractionbetweenthemandthesupracrustalmovements.Forthisreason,forseveraldecadesgeologistsandgeophysicistsfromvariouscountrieshavemadeunremittingeffortsinthisregiontoprobeintotheoriginandprocessoftheplateauformation,withavarietyofcognitionsproposed.TheCMPresultsoftheSi… 相似文献
354.
355.
356.
Are assemblages of black bream (Acanthopagrus butcheri) in different estuaries genetically distinct?
J.A. Chaplin G.A. Baudains H.S. Gill R. Mcculloch I.C. Potter 《International Journal of Salt Lake Research》1997,6(4):303-321
Samples of the estuarine-spawning teleostAcanthopagrus butcheri were collected from nine estuaries and a coastal lake, located in the Pilbara and South-western drainage divisions of Western
Australia and distributed along a coastline covering a distance of nearly 2,000 km. The patterns of allozyme variation in
these samples were used to explore the extent to which there was variation in the genetic compositions of black bream assemblages
in geographically-isolated estuarine systems, and whether or not any such variation could be related to the geographical location
or type of estuary. Although only three of 36 scorable loci (Gpi-1, Ldh andMdh-2) exhibited variation that could be used for analysis, there was considerable variation in allele frequencies at these loci
among the different samples (mean FST=0.166). Much of the detected variation was attributable to differences between the samples collected from the two drainage
divisions, which are located in very different climatic regions. Furthermore, the genetic compositions of samples from neighbouring
estuaries were typically more similar to each other than to those of samples collected from more distantly-located systems.
However, the assemblages in one west coast and two south coast estuaries, that are closed to the ocean for extensive periods
of time during the year, all showed very similar genetic compositions. Nevertheless, it is crucial to recognise that, pairwise
comparisons of samples collected from the different estuaries, both within and between the two drainage divisions, almost
invariably showed statistically significant differences in allele frequencies at one or more loci. Thus, our results indicate
that the local populations of black bream in individual estuaries are genetically distinct, which is probably a consequence
of both a limited movement by individuals between estuaries and the effects of differences in regional and local environmental
conditions. 相似文献
357.
The phase velocity and the attenuation coefficient of compressional seismic waves, propagating in poroelastic, fluid-saturated, laminated sediments, are computed analytically from first principles. The wavefield is found to be strongly affected by the medium heterogeneity. Impedance fluctuations lead to poroelastic scattering; variations of the layer compressibilities cause inter-layer flow (a 1-D macroscopic local flow). These effects result in significant attenuation and dispersion of the seismic wavefield, even in the surface seismic frequency range, 10–100 Hz. The various attenuation mechanisms are found to be approximately additive, dominated by inter-layer flow at very low frequencies. Elastic scattering is important over a broad frequency range from seismic to sonic frequencies. Biot's global flow (the relative displacement of solid frame and fluid) contributes mainly in the range of ultrasonic frequencies. From the seismic frequency range up to ultrasonic frequencies, attenuation due to heterogeneity is strongly enhanced compared to homogeneous Biot models. Simple analytical expressions for the P -wave phase velocity and attenuation coefficient are presented as functions of frequency and of statistical medium parameters (correlation lengths, variances). These results automatically include different asymptotic approximations, such as poroelastic Backus averaging in the quasi-static and the no-flow limits, geometrical optics, and intermediate frequency ranges. 相似文献
358.
从地貌学角度,分析了三峡工程永久船闸边坡岩体的自然及人为卸荷特性,指出了地表侵蚀、河流下切、开挖船闸等自然及人为地貌过程诱发了岩体的基本卸荷过程,构筑了一个三峡工程永久船闸边坡岩体卸荷特性的宏观模式。实地调砥及数值计算成果均表明,地貌分析法在分析实际岩体工程中,岩体卸荷特性方面具有较强的应用价值。 相似文献
359.
90年代世界贸易发展及空间格局变化的新特点 总被引:3,自引:0,他引:3
在世界贸易组织、日趋强烈的开放的区域主义倾向、跨国公司强劲的直接投资影响下,世界贸易正在经历着巨大变化,处在一个新的转换时期。本文从影响当今世界贸易发展的多重因素分析,揭示90年代世界贸易增长、内容结构以及空间格局发展变化的新特征,并展望世界贸易的未来发展。 相似文献
360.
P-SH conversion is commonly observed in teleseismic P waves, and is often attributed to dipping interfaces beneath the receiver. Our modelling suggests an alternative explanation in terms of flat-layered anisotropy. We use reflectivity techniques to compute three-component synthetic seismograms in a 1-D anisotropic layered medium. For each layer of the medium, we prescribe values of seismic velocities and hexagonally symmetric anisotropy about a common symmetry axis of arbitrary orientation. A compressional wave in an anisotropic velocity structure suffers conversion to both SV -and SH -polarized shear waves, unless the axis of symmetry is everywhere vertical or the wave travels parallel to all symmetry axes. The P-SV conversion forms the basis of the widely used 'receiver function' technique. The P-SH conversion occurs at interfaces where one or both layers are anisotropic. A tilted axis of symmetry and a dipping interface in isotropic media produce similar amplitudes of both direct ( P ) and converted ( Ps ) phases, leaving the backazimuth variation of the P-Ps delay as the main discriminant. Seismic anisotropy with a tilted symmetry axis leads to complex synthetic seismograms in velocity models composed of just a few flat homogeneous layers. It is possible therefore to model observations of P coda with prominent transverse components with relatively simple 1-D velocity structures. Successful retrieval of salient model characteristics appears possible using multiple realizations of a genetic-algorithm (GA) inversion of P coda from several backazimuths. Using GA inversion, we determine that six P coda recorded at station ARU in central Russia are consistent with models that possess strong (> 10 per cent) anisotropy in the top 5 km and between 30 and 43 km depth. The symmetry axes are tilted, and appear aligned with the seismic anisotropy orientation in the mantle under ARU suggested by SKS splitting. 相似文献