Probing the history of the Mathematician paleoplate using surface waves

This paper investigates the shear velocity structure under the northern East Pacific Rise at the latitude range of 9–18°N, using intermediate-period Rayleigh and Love waves. The selected ocean-bottom seismic records provide source–receiver paths that ideally constrain the lithospheric mantle structure beneath the southern Rivera plate and the Mathematician paleoplate. The Rayleigh wave data infer a relatively thin ( 30 km) lithosphere under the eastern side of the present-day East Pacific Rise. The associated shear velocities are consistent with existing models of oceanic mantle beneath this region, and the estimated plate age of 2–3 million years agrees with results from magnetic dating. The west of the rise axis is characterized by a thicker and faster lithosphere than the eastern flank, and such structural differences suggest the presence of a relatively old Mathematician paleoplate. The discontinuous change in mantle structure across the East Pacific Rise spreading center are observed in both isotropic and anisotropic velocities. The young oceanic lithosphere east of the rise axis shows strong polarization anisotropy, where the dominant orientation of crystallographic axes roughly parallels the spreading direction. However, the western flank of the rise axis is approximately isotropic, and the lack of anisotropy suggests complex deformation mechanisms associated with earlier episodes of ridge segmentation, propagation and dual-spreading on and around the Mathematician paleoplate.     

中国海岸带专用地图投影设计

地图投影是各类海岸带信息的空间定位框架要素之一。通过对目前我国海岸带常用的各种地图投影现状分析,设计并实现全国海岸带专用投影———斜轴等角圆锥投影,该投影不仅使得整个中国海岸带实现无缝的一体化表达,而且使变形达到最小。文中详细阐述该投影的设计思想和设计原理,并将结果与其他各种海岸带投影进行详细的分析比较。     

大连经济技术开发区建设与城市空间扩展研究

开发区的快速发展,推动城市空间的不断扩展和城市功能的转移扩散。通过对大连经济技术开发区建设带动城市空间扩展影响的实证研究,表明经济技术开发区建设对城市空间的规模扩张和功能扩散发挥着重要的作用,具体体现在:(1)地域空间上,再造城市空间形态、形成金州城市新区和布局十大产业功能园区;(2)经济空间上,加快传统制造业向高新技术产业转型,发展进出口贸易,引领东北地区外向型经济发展;(3)社会空间上,增加就业比重,建设人才强区,建立相对完善的现代教育体系和科研创新体系,加快原有社会空间的分异和新社会空间的形成。     

长江三角洲高新区可持续发展研究

长江三角洲是我国经济最发达、智力资源最密集的地区之一,高新区已经成为当地高新技术产业发展的主导力量。1990年以来,长江三角洲高新区凭借其良好的区位条件和政策的支持,软硬环境进一步优化,迅速集聚起各类要素资源,增长极作用明显,但也存在自主创新机制不完善,研究开发能力较弱,产品技术含量较低,国际竞争力不强等问题。本文从经济实力、经营绩效、科技创新能力、对外开放能力以及生态效率等5个方面选取29项指标,运用主成分分析法,对长江三角洲8个国家级高新区可持续发展能力进行评价。结果显示,上海张江高新区可持续发展能力最强,南京高新区和无锡高新区次之,杭州高新区和苏州高新区居中,宁波高新区和常州高新区较弱,泰州高新区最弱。并基于此提出了促进长江三角洲高新区可持续发展的对策措施。     

基于网络分析的区域铁路公司建构方法与实证

区域铁路公司是铁路运输市场组织的重要模式之一, 也是铁路改革中的焦点问题之一。 基于经济地理学功能区(结节区)的网络分析方法, 对1991～2005年我国城际铁路货流的空 间组织特征进行了系统分析, 发现我国铁路货物运输联系形成了较为稳定的功能区划, 形成 北京、广州、上海等城市枢纽节点。基于合理运输组织和减少交易成本的组织理念, 提出建 立东北、华北、西北、华中、华东、中南和西南7大区域铁路公司。该研究可以为铁路市场 化改革提供决策支持。     

Modulation of Western North Pacific Tropical Cyclone Genesis by Intraseasonal Oscillation of the ITCZ: A Statistical Analysis

The present study investigates modulation of western North Pacific(WNP) tropical cyclone(TC) genesis in relation to different phases of the intraseasonal oscillation(ISO) of ITCZ convection during May to October in the period 1979-2008.The phases of the ITCZ ISO were determined based on 30-80-day filtered OLR anomalies averaged over the region(5-20 N,120-150 E).The number of TCs during the active phases was nearly three times more than during the inactive phases.The active(inactive) phases of ISO were characterized by low-level cyclonic(anticyclonic) circulation anomalies,higher(lower) midlevel relative humidity anomalies,and larger(smaller) vertical gradient anomalies of relative vorticity associated with enhanced(weakened) ITCZ convection anomalies.During the active phases,TCs tended to form in the center of the ITCZ region.Barotropic conversion from the low-level mean flow is suggested to be the major energy source for TC formation.The energy conversion mainly depended on the zonal and meridional gradients of the zonal flow during the active phases.However,barotropic conversion weakened greatly during the inactive phases.The relationship between the meridional gradient of absolute vorticity and low-level zonal flow indicates that the sign of the absolute vorticity gradient tends to be reversed during the two phases,whereas the same sign between zonal flow and the absolute vorticity gradient is more easily satisfied in the active phases.Thus,the barotropic instability of low-level zonal flow might be an important mechanism for TC formation over the WNP during the active phases of ISO.     

洞错混杂带内部结构及构造岩片组合特征

为了对洞错混杂带进行深入研究,通过遥感图像解译将其分为玄武岩岩片带、蛇绿混杂岩带和蛇绿岩带3个次级构造带,这3个次级构造带在平面上近平行延伸,向东、西方向收敛,在剖面上呈叠瓦式向南逆冲.实地检查证明,遥感解译结果符合实际情况,各带内岩块的物质组成、几何结构大不相同,中部的蛇绿混杂岩带是洞错混杂带的主带.     

甘孜—理塘断裂带北段玄武岩地球化学特征及构造意义

沿甘孜-理塘断裂带广泛发育有三叠纪玄武岩,该断裂带北段的玄武岩多为SiO_2大部分不饱和蚀变较强的基性岩,根据TiO_2K_2O、P_2O_5、Al_2O_3和CaO含量判定为亚碱性拉斑玄武岩系列。痕量元素特征表明,玄武岩为轻稀土弱富集型,∑REE、∑LREE/∑HREE、δEu、Eu/Sm、Sm/Nd都显示与大洋拉斑玄武岩一致。笔者认为,理塘断裂带南段在晚二叠世打开并逐步向北推进,北段于早三叠世打开,中三叠世为甘孜-理塘海发育的鼎盛时期,晚三叠世逐渐闭合。     

秦岭勉略缝合带组成与古洋盆演化

秦岭勉略构造带是典型的蛇绿构造混杂岩带,带内组成复杂、变形强烈,其主导构造样式表现为以系列北倾逆冲断层为格架,不同岩片推覆叠置的叠瓦状构造。详细的组成及构造研究表明,缝合带由洋盆形成演化不同阶段、不同性质的陆缘沉积岩系、不同类型蛇绿岩以及洋盆俯冲－碰撞造山过程中以不同方式出露的构造岩块组成,同时区域地层对比表明勉略古洋盆形成过程具有自西而东“剪刀式”打开扩展的性质与特点。     

宝塔滑坡稳定性计算与评价

宝塔滑坡群是由多个滑体组成，本文着重阐述滑坡群中的主体─—宝塔滑坡的稳定性计算与评价。通过采用不平衡推力传递系数法，对宝塔滑坡各个可能滑动的滑动面进行多种方案的计算，以及长江库区水位对宝塔滑坡稳定性的影响。进而对宝塔滑坡作出了稳定性分析和评价，同时也阐明了宝塔滑坡所采用的计算模型的计算结果是切合实际的。