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131.
132.
西藏层序地层研究进展 总被引:2,自引:0,他引:2
迄今为止,西藏区内所开展的层序地层分析主要涉及到中生代的二级或三级层序。基于露头剖面的沉积相、古生物、磁性地层以及地质事件的综合研究,探讨了三叠纪、侏罗纪和白垩纪的层序地层模式及其形成机制。现今所取得的进展主要表现在3个方面:①初步建立了区内中生代层序地层年代格架;②不同时代、不同类型盆地中的层序数量、结构与层序类型具有较大的差异;③层序地层与磁性地层的结合研究,取得了重要的成果。未来区内的层序地层研究应在3个方面展开;①高分辨率层序地层研究,树立株罗纪-第三纪海平面变化曲线;②探索层序地层填图新方法;③多岛弧造山模式和多机制的隆升模式等大陆动力学问题也是层序地层所遇到的新挑战。 相似文献
133.
Dissolved and particulate trace metals and their partitioning in a hypoxic estuary: The Tanshui Estuary in Northern Taiwan 总被引:1,自引:0,他引:1
The distribution and partitioning of trace metals (Co, Cu, Fe, Mn, Ni, and Zn) between dissolved and particulate phases were studied in the Tanshui Estuary. The upper reach of the estuary is hypoxic and heavily polluted due to domestic and industrial discharges. The concentration ranges of dissolved and leachable particulate trace metals in the Tanshui Estuary were: Co: 0.3–6.1 nM, 1.8–18.6 mg kg−1; Cu: 5–53 nM, 22–500 mg kg−1; Fe: 388–3,364 nM, 1.08–6.67%; Mn: 57–2,914 nM, 209–1,169 mg kg−1; Ni: 7–310 nM, 6–108 mg kg−1; and Zn: 12–176 nM, 62–1,316 mg kg−1; respectively. The dissolved concentrations of the metals were 2–35 times higher than the average values of the world river water. The distributions of dissolved and particulate studied metals, except Mn, in the estuary showed scattering, which could be attributed to the discharges from many industrial wastewater disposal works located in the upper tributaries. The daily input of dissolved metals from the disposal works to the Tanshui Estuary ranged from 0.1–0.4 tons. Dissolved Mn was nearly conservative in the region with salinity higher than 10 psu, while particulate Mn decreased in the region with salinity of 10–15 psu. The concentration increased significantly seawards, corresponding with the distribution of dissolved oxygen. The distribution coefficient (KD) for Mn in the lower estuary was nearly three orders of magnitude higher than in the upper estuary. This phenomenon may be attributed to the diffusion of Mn from the anoxic sediment in the upper estuary and gradual oxidation into particulate Mn in the middle and lower estuary as the estuarine water became more oxygenated. The distribution coefficient for Cu decreased with increasing salinity. The percentages of trace metals bound by suspended particulate matter decreased in the following order: Fe>Zn, Cu>Co>Mn>Ni. 相似文献
134.
135.
地质图空间数据库建设中的拓扑关系处理 总被引:2,自引:0,他引:2
拓扑关系是空间数据库的核心。主要阐述拓扑关系的基本概念,详细介绍MAPGIS和ARC/INFO两大模块中,拓扑关系具体表现形式、处理方法及处理过程中的注意事项,形成了一套较为完善的工作流程,提高了工作效率,为今后的信息化提供了行之有效的工作方法。 相似文献
136.
根据摩擦型单元的力一位移一滑移量关系,建立了包含摩擦型单元的结构整体分析方法.算例分析表明,在结构中安装摩擦阻尼器可以大大地减小结构的地震反应. 相似文献
137.
昆仑山口西8.1级地震在四川地区的前兆异常效应 总被引:2,自引:0,他引:2
对昆仑口西8.1级地震发生前后四川地区地震前兆监测台网的测值曲线进行了系统的清理,发现存在有明显的孕震效应和震时效应,异常效应的幅度很大,容易鉴别,这对人类认识特大地震的影响场很有意义。 相似文献
138.
螺旋CT三维重建在骨盆骨折中的应用 总被引:2,自引:0,他引:2
目的:探讨用螺旋CT三维重建评价骨盆骨折的临床应用价值。方法:收集骨盆骨折17例,采用螺旋CT三维重建检查。结果:17例检查均取得清晰立体图像,且可消除某一骨性结构,单独观察骨盆某一组成骨的骨折情况。结论:螺旋CT三维重建在骨盆骨折的诊断、手术方案的设计及教学等有较高价值。 相似文献
139.
140.
Velocity profile of a sand cloud blowing over a gravel surface 总被引:2,自引:0,他引:2
Particle dynamic analyzer (PDA) measurement technology was used to study the turbulent characteristics and the variation with height of the mean horizontal (in the downwind direction) and vertical (in the upward direction) particle velocity of a sand cloud blowing over a gravel surface. The results show that the mean horizontal particle velocity of the cloud increases with height, while the mean vertical velocity decreases with height. The variation of the mean horizontal velocity with height is, to some extent, similar to the wind profile that increases logarithmically with height in the turbulent boundary layer. The variation of the mean vertical velocity with height is much more complex than that of the mean horizontal velocity. The increase of the resultant mean velocity with height can be expressed by a modified power function. Particle turbulence in the downwind direction decreases with height, while that in the vertical direction is complex. For fine sands (0.2–0.3 mm and 0.3–0.4 mm), there is a tendency for the particle turbulence to increase with height. In the very near-surface layer (<4 mm), the movement of blown sand particles is very complex due to the rebound of particles on the bed and the interparticle collisions in the air. Wind starts to accelerate particle movement about 4 mm from the surface. The initial rebound on the bed and the interparticle collisions in the air have a profound effect on particle movement below that height, where particle concentration is very high and wind velocity is very low. 相似文献