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41.
Alexandros I. ValsamisGeorge D. Bouckovalas Yannis K. Chaloulos 《Soil Dynamics and Earthquake Engineering》2012,34(1):99-110
Extensive damage to pile-supported structures has been witnessed in several recent earthquakes (Chi-Chi, 1999; Kobe, 1995, etc.), as a result of liquefaction-induced lateral spreading of slightly sloping ground or free-face topographic irregularities. This paper presents a parametric analysis of the basic pile and soil parameters, as well as the pile-soil interaction mechanisms affecting the response of single piles subjected to such lateral spreading, based on numerical simulation with the nonlinear P-y method. In parallel, a set of design charts and analytical relations is established, for approximate computation of maximum pile deflections and bending moments, using a “theory guided” multi-variable statistical analysis of the numerical predictions. Three different combinations (design cases) of pile head constraints and soil conditions were considered, which are commonly encountered in practice. The overall accuracy of the proposed analytical relations is evaluated against experimental results from seven centrifuge and five large shaking table experiments. 相似文献
42.
Pull-apart Basins and the Total Lateral Displacement Along the Haiyuan Fault Zone in Cenozoic 总被引:2,自引:0,他引:2
INTRODUCTIONItisdebatedaboutthetotallateraldisplacementalongthemainboundaryfaultsofintraplateblocksineasternAsiacontinentinCenozoicera .Inthe 1 970sof2 0thcentury ,somescientistshades timatedlateraldisplacementbasedongeomorphicdata .Theyproposedthatthetotald… 相似文献
43.
利用新疆地震台网及其毗邻地区的国外地震台站提供的地震P波到时数据,重建了新疆及其毗邻地区地壳上地幔的三维速度图像.主要结果是:1.研究区地壳上地幔的地震波速度存在明显的横向不均匀性.这种不均匀性出现在不同构造单元之间,也出现在各构造单元之内.2.一般来说,研究区域内盆地是上地幔的隆起区,褶皱系是上地幔的坳陷区.3.岩石层厚度和软流层的深度与全球的平均结果有较大不同.4.海洋岩石层或大陆岩石层板块在兴都库什和克什米尔与中国交界地区的消减明显存在.5.地壳上地幔物质运动比较剧烈,有部分熔融物质上涌到地壳中部或更浅的深度. 相似文献
44.
MARIANA I. OLARIU CORNEL OLARIU RONALD J. STEEL ROBERT W. DALRYMPLE ALLARD W. MARTINIUS 《Sedimentology》2012,59(2):356-378
The first sandstone unit of the Esdolomada Member of the Roda Formation (hereafter referred to as ‘Esdolomada 1’) was formed by a laterally‐migrating, shelf tidal bar. This interpretation is based on detailed mapping of the bedding surfaces on the digital terrain model of the outcrop built from light detection and ranging data and outcrop photomosaics combined with vertical measured sections. The Esdolomada 1 sandbody migrated laterally (i.e. transverse to the tidal currents) towards the south‐west along slightly inclined (1.6° to 4.6°) master bedding surfaces. The locally dominant tidal current flowed to the north‐west. This current direction is indicated by the presence of stacked sets of high‐angle (average 21°) cross‐stratification formed by dunes that migrated in this direction, apparently in an approximately coast‐parallel direction. The tidal bar contains sets and cosets of medium‐grained cross‐stratified sandstone that stack to reach a thickness of about 5·5 m. Individual cross‐bed sets average about 50 cm thick (with a range of 10 to 70 cm) and have lengths of ca 130 to 250 m in a direction perpendicular to the palaeocurrent. Set thickness decreases in the direction of migration, towards the south‐west, and the degree of bioturbation increases, so that the cross‐bedded sandstones gradually change into highly bioturbated finer‐grained and thinner‐bedded sandstones lacking any cross‐stratification. The rate of thinning of individual dune sets as they are traced down any obliquely‐accreting master surface is some 40 cm per 100 m (0·004) for the older, thicker sandstones, whereas the younger, thinner beds thin at a rate of 15 cm over 100 m (0·0015). The tidal bar has a sharp base and top and is encased in finer‐grained bioturbated, marine sandstones. The Esdolomada bar crest was oriented north‐west to south‐east, parallel to the tidal palaeocurrents and to the nearby palaeoshoreline, but built by lateral accretion towards the south‐west. Lateral outbuilding generated a flat‐topped bar with a measured width of about 1700 m, and a preserved height of 5·5 m. The bar, disconnected from a genetically related south‐westward prograding delta some 2 km to the north‐east, developed during the transgressive phase of a sedimentary cycle. The tidal bar was most probably initiated as a delta‐attached bar at the toesets of the delta front and during transgression evolved into a detached tidal bar. 相似文献
45.
The reasons that pillars with small width-to-height ratios fail remain unclear. This study established a mechanical model for the buckling failure of a thin pillar subjected to compressive forces to investigate the stability of reserved thin pillars (RTPs) on both sides of mining units during barrier pillar recovery. The critical buckling stress of the thin pillar was obtained using the energy variational method, and its relationship to the aspect ratio (length-to-width ratio) was investigated. The buckling instability of RTPs can be determined by comparing the RTP stress obtained from numerical simulations with the buckling stress derived from the mechanical model. 相似文献
46.
47.
Shantanu Joshi Amit Prashant Arghya Deb Sudhir K. Jain 《Soil Dynamics and Earthquake Engineering》2011
Presently available simplified analytical methods and semi-empirical methods for the analysis of buried pipelines subjected to fault motion are suitable only for the strike-slip and the normal-slip type fault motions, and cannot be used for the reverse fault crossing case. A simple finite element model, which uses beam elements for the pipeline and discrete nonlinear springs for the soil, has been proposed to analyse buried pipeline subjected to reverse fault motion. The material nonlinearities associated with pipe-material and soil, and geometric nonlinearity associated with large deformations were incorporated in the analysis. Complex reverse fault motion was simulated using suitable constraints between pipe-nodes and ground ends of the soil spring. Results of the parametric study suggest that the pipeline's capacity to accommodate reverse fault offset can be increased significantly by choosing a near-parallel orientation in plan with respect to the fault line. Further improvement in the response of the pipeline is possible by adopting loose backfill, smooth and hard surface coating, and shallow burial depth in the fault crossing region. For normal or near normal orientations, pipeline is expected to fail due to beam buckling at very small fault offsets. 相似文献
48.
采用非线性有限元软件Msc.Marc对高层钢管混凝土组合框架-钢板剪力墙结构底部四层两跨未加劲薄钢板墙模型进行了推覆分析与滞回分析。计算结果表明,组合钢板剪力墙结构具有良好的延性及稳定的滞回性能,结构进入弹塑性阶段后钢板墙的拉力带方向与CAN/CSA S16—01(2001)推荐公式吻合良好。根据分析结果,比较了不同分析类型及不同钢板墙厚度的影响。研究发现,考虑钢材强化及包辛格效应后,结构滞回分析的极限承载力将小于推覆分析的极限承载力;随着钢板墙厚度的增大,结构的弹塑性屈曲模态由局部屈曲向整体屈曲过渡;在罕遇地震作用下,钢板墙结构的底层边缘约束柱将产生较大的轴拉力,甚至被拉断而导致结构整体破坏。 相似文献
49.
The leading edge of the ENE-trending Himalayan thrust front in Pakistan exhibits along-strike changes in deformational style, ranging from fault-bend to fault-propagation folds. Although the structural geometry is very gently deformed throughout the Salt Range, it becomes progressively more complex to the east as the leading edge of the emergent Salt Range Thrust becomes blind. Surface geology, seismic reflection, petroleum well, and chronostratigraphic data are synthesized to produce a 3-D kinematic model that reconciles the contrasting structural geometries along this part of the Himalayan thrust front. We propose a model whereby displacement was transferred, across a newly-identified lateral ramp, from a fault-bend fold in the west to fault-propagation folds in the east and comparable shortening was synchronously accommodated by two fundamentally different mechanisms: translation vs. telescoping. However, substantially different shortening distribution patterns within these structurally contrasting segments require a tear fault, which later is reactivated as a thrust fault. The present geometry of this S-shaped displacement transfer zone is a combined result of the NW–SE compression of the lateral culmination wall and associated tear fault, and their subsequent modification due to mobilization of underlying ductile salt. 相似文献
50.
介绍了杭州某地铁站基坑开挖过程中的监测的侧向位移变化情况,总结了其变化规律,对施工过程提供了参考。用FLAC软件对基坑的侧向位移进行了数值模拟,然后与实际监测结果进行了对比,阐述了影响模拟结果准确性的影响因素。 相似文献