就业郊区化背景下郊区就业者日常活动时空间特征研究——以北京上地地区为例

个体日常活动时空间特征反映了其对城市空间利用的时空需求,是衡量社会服务、公共资源配置的新维度。基于个体行为分析郊区就业者日常生活时空间特征,有利于透视郊区就业者的空间需求以及就业郊区化带来的城市空间变革。利用2012年北京市活动出行调查数据,选取居住在北京郊区且在上地地区(郊区)工作的203个就业者样本,从非汇总角度对该群体日常活动时空间特征进行描述分析,揭示郊区就业者日常活动的时空需求。研究结果发现,郊区就业者在休息日的活动呈现较强的时间碎片化与空间分散性特征;郊区就业者对中心城区存在较强的空间依赖,很大一部分休闲购物活动需要前往中心城区发生,同时郊区大型商业设施也一定程度上吸引了郊区就业者,郊区功能趋向复合化;郊区就业空间职能较为单一,公共和商业设施供给不足,利用率较低,需进一步完善。     

综合物探方法在南京城际轨道交通S1线建设中的应用

南京地区地貌类型复杂多样,不同类型地貌单元区的地质环境条件差异较为明显,采用地质雷达和横波反射地震勘探方法,循序渐进、相互补充、相互验证,查明了南京城际轨道交通S1线(YDK2+630—YDK2+899段)土岩分界面位置以及不同岩性接触带位置,经地铁隧道施工验证,证明资料可靠准确。将综合物探方法应用于地铁施工勘察,起到了较好的效果,可供今后地铁施工勘察参考。     

A new ophiolitic mélange containing boninitic blocks in Alxa region:Implications for Permian subduction events in southern CAOB

The Alxa region, located in the southernmost part of Central Asian Orogenic Belt, is a key region for understanding the tectonic processes associated with the closure of the Paleo-Asian Ocean. Issues of late Paleozoic tectonic settings and tectonic unit divisions of the Alxa region still remain controversial. In this study, we report a new ophiolitic mélange named the Tepai ophiolitic mélange in the northern Alxa region, northwest of Alxa Youqi. The tectonic blocks in the Tepai ophiolitic mélange are mainly composed of serpentinized peridotites, serpentinites, mylonitized gabbros, gabbros, basalts, and quartzites, with a matrix comprising highly deformed clastic rocks. A gabbro exhibits a zircon LA-ICP-MS Ue Pb age of278.4 ± 3.3 Ma. Gabbros exhibit high Mg O and compatible element contents, but extremely low TiO_2,totally rare earth element and high field strength element contents. These rocks exhibit light rare earth element depleted patterns, and display enriched in large-ion lithophile elements and depleted in high field strength elements. Boninite-like geochemical data show that they were formed in a subductionrelated environment, and derived from an extremely depleted mantle source infiltrated by subduction-derived fluids and/or melts. The Tepai ophiolitic mélange exhibits similar zircon U-Pb-O isotopic compositions and whole-rock geochemical characteristics to those of the Quagan Qulu ophiolite.Therefore, we propose that the Tepai ophiolitic mélange may have been the western continuation of the Quagan Qulu ophiolite. Our new finding proves the final closure of the Paleo-Asian Ocean might have taken place later than the early Permian.     

吕梁山——华北克拉通中部中生代基底卷入褶皱系统

位于华北克拉通中部的吕梁山的形成代表了华北克拉通在晚侏罗世-早白垩世的挤压变形事件,为了更好地理解该期变形的样式、时代、机制和背景,对吕梁山地区开展了详细的野外调查,同时搜集了前人的低温热年代学工作.结果表明,吕梁山是一个中生代期间形成的发育有典型单褶（monocline）构造的陆内基底卷入型大型褶皱系统.早前寒武纪造山作用在基底中形成早期面理（片麻理、片理、劈理以及节理）,这些面理在后期近东西向挤压作用下再次活动形成了基底断裂,并导致了上覆沉积地层褶皱变形,吕梁山不同地区褶皱的古应力场方向总体为SE（122°）~NW（302°）.吕梁山单褶构造的构造样式、形成机制以及分布,与北美西部的Laramide造山带中的厚皮构造相似,形成的构造环境也类似.吕梁山褶皱及其单褶构造总体形成于晚侏罗世期间古太平洋板块向西低角度俯冲的环境中,该期俯冲也导致了华北克拉通同期陆内挤压变形.      

Influence of geosynthetic reinforcement on the progressive failure of rigid columns under an embankment load

Acta Geotechnica - Prior investigations have revealed that the stress characteristics of columns at different locations beneath an embankment vary. A failed column releases stress and causes...