城市"新经济"发展的空间效应及其启示——以西安市为例   总被引：1，自引：0，他引：1  

王慧 《地理研究》2007,26(3):577-589

以知识为基础、以计算机与信息技术为依托、技术与制度创新驱动、兼跨第二与第三产业并以服务业居重、高度外向而趋于全球化的当代"新经济"的兴起,正从诸多方面影响和改变着城市。本文以西安市为实证分析案例,依据对"新经济"内在禀赋特性的认识,从城市"产业区"格局重构、城市办公楼宇设施增长、高新技术产业区的CBD化、产业与居住功能分区的模糊化、城市经济与社会空间的极化等方面对城市"新经济"发展的空间影响效应进行了分析,并就其对于城市规划与决策的启示予以探讨。  相似文献   

Palaeomagnetism and isotopic age data from Upper Cretaceous igneous rocks of W. Portugal; geological correlation and plate tectonic aspects     

K. M. Storetvedt  H. Mogstad  M. C. Abranches  J. G. Mitchell  A. Serralheiro 《Geophysical Journal International》1987,88(1):241-263

  相似文献   

BOOK REVIEWS     

《The Professional geographer》1987,39(4):487-521

Book Reviewed in this article: Geographical Aspects of Health and Disease in India . Rais Akhtar and A.T.A. Learmonth , eds . Antarctic Treaty System: An Assessment . Proceedings of a Workshop at Beardmore South Field Camp, Antarctica. American Electoral Mosaics . J. Clark Archer and Fred M. Shelley . Kompas op Suidwes-Afrika/Namibie . W.S. Barnard , ed . Jerusalem in the 19th Century: The Old City . Yehoshua Ben -Arieh . The World as a Total System . Kenneth E. Boulding . A Social History of Housing 1815–1985, Second Ed . John Burnett . Human Migration . W.A.V. Clark . Regional Population Projection Models . Andrei Rogers . The State of Population Theory: Forward from Malthus . David Coleman and Roger Schofield , eds . Imagining Tomorrow: History, Technology and the American Future . Joseph C. Corn , ed. Swidden Agriculture in Indonesia: The Subsistence Strategies of the Kalimantan Kantú . Michael R. Dove . Glacial Geologic Processes . David Drewry . Physics of Desertification . Farouk El -Baz and M.H.A. Hassan , eds . Housing the Homeless . Jon Erickson and Charles Wilhelm , eds . Settlement Patterns in Missouri: A Study of Population Origins, with a Wall Map . Russel L. Gerlach . Desert Development: Man and Technology in Sparselands . Yehuda Gradus , ed . Nuclear Winter. The Evidence and Risks . Owen Greene , Ian Percival and Irene Ridge . The Take-off of Suburbia and the Crisis of the Central City . Günter Heinritz and Elisabeth Lichtenberger , eds . Regional Input-Output Analysis . Geoffrey J. D. Hewings . Spatial Transportation Modeling . Christian Werner . The Atlas of Georgia . Thomas W. Hodler and Howard A. Schretter , eds . Latin America. 5th ed . Preston E. James and C.W. Minkel . Applied Remote Sensing . C.P. Lo . Localities, Class, and Gender . The Lancaster Regionalism Group . Urban Social Movements: The City after Castells . Stuart Lowe . Politics and Method . Doreen Massey and Richard Meegan , eds . Land Use . A. S. Mather . The Kingdom of Coal . Donald L. Miller and Richard E. Sharpless . The Presidio and Militia on the Northern Frontier of New Spain, A Documentary History, Vol. 1: 1570–1700 . Thomas H. Naylor and Charles W. Polzer , S.J., comps . and eds . Nuclear Power: Siting and Safety . Stan Openshaw . The Central African Republic: The Continent's Hidden Heart . Thomas O'Toole . Environmental and Dynamic Geomorphology . Márton Pécsi , ed . Remote Sensing Principles and Interpretation . Floyd F. Sabins , Jr . Acid Rain and Friendly Neighbors: The Policy Dispute between Canada and the United States . Jurgen Schmandt and Hilliard Roderick , eds . Earth's Changing Surface: An Introduction to Geomorphology . M.J. Selby . International Migration: The Female Experience . Rita J. Simon and Caroline B. Brettell , eds . On Geography and Its History . D.R. Stoddart . Transportation Networks: A Quantitative Approach . D. Teodorovic . Processes in Physical Geography . R.D. Thompson , A.M. Mannion , C.W. Mitchell , M. Parry , J.R.G. Townshend . Imaging Radar for Resources Surveys . J.W. Trevett . Dominance and Affection: The Making of Pets . Yi -Fu Tuan . Capturing the Horizon. The Historical Geography of Transportation since the Transportation Revolution of the Sixteenth Century . James E. Vance , Jr . Nations at Risk: The Impact of the Computer Revolution . Edward Yourdon .  相似文献   

中国东部中生代高Sr低Yb和低Sr高Yb型花岗岩：对比及其地质意义   总被引：21，自引：8，他引：21  

张旗李承东  王焰王元龙  金惟俊贾秀勤 韩松 《岩石学报》2005,21(6):1527-1537

中国东部在晚中生代时（晚侏罗世-旱白垩世）有广泛的中酸性岩浆活动，按照花岗岩的地球化学特征，大致可以划分为东北、华北和华南3个岩区。本文研究表明，按照Sr和Yb的含量，大致可以将花岗岩分为5类．即：高Sr低Yb型（Sr〉400μg／g，Yb〈2μg／g）、低Sr低Yb（Sr〈400μg／g，Yb〈2μ/g）、低Sr高Yb（Sr〈400μg／g，Yb〉2μg／g）、高Sr高Yb型（Sr〉400μg／g，Yb〉2μg／g）以及非常低Sr高Yb型（Sr〈100μg／g，Yb=2—18μg／g）花岗岩。东北和华南以发育低Sr高Yb花岗岩为主，有少量高Sr低Yb和非常低Sr高Yb类型的花岗岩分布；而华北则以高Sr低Yb型花岗岩（埃达克岩）最发育，低Sr高Yb、低Sr低Yb型和非常低Sr高Yb型花岗岩有少量分布。本文着重探讨了华北和华南花岗岩的特征，认为华北和华南花岗岩地球化学的区别可能主要与花岗岩源区成分和深度有关，且主要受源区深度的控制。如果花岗岩熔融的源区残留相由榴辉岩组成（石榴石＋辉石＋金红石＋／一角闪石），则花岗岩明显亏损HREE、Nb、Ta和Ti，而富集Sr和Al，无明显的负铕异常，属于高Sr低Yb（埃达克岩）类型；如果源区深度浅，由斜长角闪岩或麻粒岩组成（斜长石＋辉石＋角闪石），则花岗岩相对贫Sr富Yb。作者认为，华北和华南花岗岩地球化学特征上的上述差异，表明在晚中生代时（晚侏罗世．早白垩世）。华北和华南的地壳厚度不同：华北较厚，华南较薄；华北经历了下地壳拆沉而华南无；华北和华南的下地壳成分不同，华北较基性的下地壳拆沉后，留下的地壳平均成分与华南比偏中性。  相似文献   

The stability of primary alluaudites in granitic pegmatites: an experimental investigation of the Na2(Mn2−2x Fe1+2x )(PO4)3 system     

Frédéric Hatert  André-Mathieu Fransolet  Walter V. Maresch 《Contributions to Mineralogy and Petrology》2006,152(4):399-419

In order to assess the geothermometric potential of the Na₂(Mn_2−2x Fe_1+2x )(PO₄)₃ system (x = 0–1), which represents the compositions of natural weakly oxidized alluaudites, we performed hydrothermal experiments between 400 and 800°C, at 1 kbar, under an oxygen fugacity (f(O₂)) controlled by the Ni–NiO (NNO), Fe₂O₃–Fe₃O₄ (HM), Cu₂O–CuO (CT), and Fe–Fe₃O₄ (MI) buffers. When f(O₂) is controlled by NNO, single-phase alluaudites crystallize at 400 and 500°C, whereas the association alluaudite + marićite appears between 500 and 700°C. The limit between these two fields corresponds to the maximum temperature that can be reached by alluaudites in granitic pegmatites, because marićite has never been observed in these geological environments. Because alluaudites are very sensitive to variations of oxygen fugacity, the field of hagendorfite, Na₂MnFe²⁺Fe³⁺(PO₄)₃, has been positioned in the f(O₂)–T diagram, and provides a tool that can be used to estimate the oxygen fugacity conditions that prevailed in granitic pegmatites during the crystallization of this phosphate.  相似文献   

东海陆架盆地中生代残留地层特征及其构造启示          下载免费PDF全文

王磊  李春峰  李珂迪  姚泽伟  陶天生 《海洋学研究》2022,40(4):11-24

东海陆架盆地是位于中国东部华南大陆边缘的一个中、新生代叠合盆地,具有较大油气潜力。目前东海陆架盆地油气的发现均来自于新生界,对中生代残留地层的各方面特征认识不足:在空间上通常集中于特定构造单元,且基本位于盆地西部;在时间上主要涉及白垩纪和侏罗纪,且多是定性或半定量的研究。本文在前人研究的基础上,收集、整理了研究区目前最新、最全的反射地震资料和钻井数据,从钻遇中生界井的标定出发,以地震资料的层序划分和解释为基础,进行残留地层的研究,空间上统一盆地东、西两大坳陷带,时间上统揽白垩纪、侏罗纪以及前侏罗纪三个时期。结果表明,东海陆架盆地中生代残留地层遭受了后期严重的剥蚀改造,总体呈现东厚西薄、南厚北薄的特征,残留地层范围随时间不断东扩。对比各时期残留地层平面展布特征,揭示了东海陆架盆地的演变过程:三叠纪时期盆地原型为被动大陆边缘坳陷型盆地,早、中侏罗世时期为活动大陆边缘弧前盆地,晚侏罗世—晚白垩世时期为大陆边缘弧后伸展盆地;与此相对应,古太平洋板块俯冲肇始于晚三叠世—早、中侏罗世时期,板块后撤始于晚侏罗世。东海陆架盆地在中生代的东侧边界位于钓鱼岛隆褶带的东侧。  相似文献   

腾冲地块高地热异常区晚白垩世-始新世钾玄质强过铝花岗岩岩石地球化学、年代学特征及构造意义   总被引：3，自引：2，他引：1  

林木森  彭松柏  乔卫涛  李辉 《岩石学报》2014,30(2):527-546

腾冲地块高地热异常区清水左所营初糜棱岩化黑云母二长花岗岩岩体、新华黑石河热田强糜棱岩化黑云母二长花岗岩岩体、热海热田硫磺塘硅化碎裂正长花岗岩岩体变形变质、岩石地球化学及锆石年代学的研究表明,晚白垩世(73Ma)初糜棱岩化黑云母二长花岗岩岩体为高温钾玄质强过铝花岗岩,形成于活动大陆边缘火山弧-后碰撞转换或过渡构造环境,并经历强烈伸展变形作用,普遍发育早期近水平-低角度(30°)韧性伸展剪切糜棱面理,局部发育晚期高角度右旋走滑挤压韧性糜棱面理;始新世(48~46Ma)强糜棱岩化黑云母二长花岗岩岩体、硅化碎裂正长花岗岩岩体为中-高温钾玄质强过铝花岗岩,并具铝质A型花岗岩特征,形成于后碰撞-板内构造环境,以发育晚期高角度(70°~87°)右旋走滑挤压韧性糜棱面理为特征,其右旋走滑韧性剪切变形时代晚于始新世(48~46Ma)。晚白垩世-始新世钾玄质强过铝花岗岩的形成与俯冲-碰撞造山隆升后的伸展垮塌、拆沉地幔物质上涌玄武质岩浆底侵和地壳部分熔融作用密切相关。始新世-第四纪岩浆活动与高地热异常区(带)空间上密切伴生,新近纪晚期-第四纪构造活动主要表现为脆性走滑-拉张正断层和构造拉分断陷盆地的形成,构造断陷边界断裂与深部岩浆活动是导致腾冲地区高地热异常区(带)中-高温地热温泉沿走滑-拉张断裂带集中分布的主要原因。  相似文献   

斑岩钼-热液脉状铅锌银矿成矿系统特征、控制因素及勘查指示   总被引：1，自引：0，他引：1  

金露英  秦克章  李光明  赵俊兴  李真真 《岩石学报》2020,36(12):3813-3839

斑岩钼矿与热液脉状铅锌银矿为两类重要的矿床类型,两者往往分别独立产出,但越来越来的勘查实例揭示二者也可共生产出,构成统一的成矿系统。斑岩钼-热液脉状铅锌银成矿系统,主要分布在北美西部、加拿大西南部、中国秦岭-大别地区、华北北缘及西拉沐伦带、大兴安岭北段-额尔古纳等地区。根据斑岩钼矿与热液脉状铅锌银矿的平面关系,成矿系统可分为近源和远源两类：近源时,两者直接叠置或者平面距离小于2km;而远源时,两类矿化平面距离一般不超过6km。成矿系统空间上表现可为上铅-锌-银、下钼的垂向叠置或者内钼、外铅-锌-银侧向共存的形式。时间上两类矿化一般近同期形成,或者相差通常不超过8Myr。成矿系统岩浆性质多为高演化的钙碱性花岗质岩浆,起源于下地壳且加入了不同比例的地幔物质。成矿系统的蚀变特征一般为斑岩钼矿化蚀变向热液脉状铅锌银矿蚀变的渐变,其中粘土化带与绢英岩化带是两类矿床的叠加区。钼矿化常与钾硅酸盐化或者绢英岩化带内侧密切相关,铅锌银矿化则常与浅部的低温硅化-绢云母-伊利石-水白云母化、碳酸盐化密切相关。基于S、Pb、Sr、Nd等同位素研究成果,钼铅锌银系统中成矿物质主要为岩浆来源,但可能有地层物质的加入。成矿流体主要以岩浆水来源为主,初始流体通常为单相中低密度流体,辉钼矿沉淀往往伴随着减压沸腾、大气水混合、冷却及/或水岩反应的进行,发生大规模钼矿化的温度区间通常在300~450℃。浅部脉状铅锌银矿化则由持续降温的流体在混入较多大气水或流体pH值中和而形成,温度区间在175~320℃。成矿系统空间上钼-铅-锌-银的分带,可能受控于流体演化过程中上述多个过程的综合叠加作用。通过总结对比钼铅锌银成矿系统、单一斑岩钼矿、单一热液脉状铅锌银矿床在勘查历史、构造因素、成矿岩体属性、流体特征、特征矿物、地球物理-地球化学勘查指标等方面的异同,本文提出了指示浅部热液脉状铅锌银矿之下同一成矿系统深部斑岩钼矿的找矿标志,且对该成矿系统形成的岩浆性质、岩浆-热液系统、成矿元素、构造条件、保存条件等多个方面进行了探讨。在前人基础上,本文提出本类成矿系统理论研究展望：1）利用微区原位技术分辨矿物的不同期次及元素的分布状态,进而获得该类型铅锌银矿相对准确的成矿年龄;2）确定斑岩钼-热液脉状铅锌银成矿系统的初始流体成矿元素和相关配位剂元素的含量;3）建立钼铅锌银成矿系统的矿物学指示标志;4）查明成矿系统岩浆过程、元素行为等精细成矿过程,研究其与其他成矿系统的差异。上述问题的深入研究和找矿标志的提出或将提高对斑岩钼-脉状铅锌银成矿系统成矿过程的认识,为该类系统勘查找矿工作提供理论支撑。  相似文献   

SHRIMP U–Pb ages of zircons from the Lengshuikeng ore field,North Wuyi Mountains,South China: Implications for dating volcaniclastic rocks     

Jian‐Hua Wu  Heng‐Fei Guo  Dong‐Guang Yang  Kai‐Xing Wang  Chang‐Xi Wei  Jia‐Lei Guo 《Island Arc》2020,29(1)

The Lengshuikeng Ag‐Pb‐Zn ore field is located in the North Wuyi Mesozoic volcanic belt south of the Qinzhou–Hangzhou suture zone between the Yangtze and Cathaysia paleo‐plates. Previous zircon U–Pb geochronological studies on ignimbrites and tuffs from this area have yielded conflicting ages of 157–161 Ma (Early Upper Jurassic) and 137–144 Ma (Early Lower Cretaceous). Volcanic rocks in the ore field have even been proposed to include both ages. Our SHRIMP zircon U–Pb dating of the ignimbrite and tuff samples from the ore field, along with field observations and results from geochronological work on other volcanic and sub‐volcanic rocks in the region, shows that two populations of magmatic zircons, one autocrystic and the other xenocrystic, are present in the pyroclastic rocks. The autocrystic zircons have ages suggesting formation/eruption at approximately 140 Ma, whereas the xenocrystic zircons give ages of 155–159 Ma, indicating intrusion of granitic porphyries in the Early Upper Jurassic. Therefore, the pyroclastic rocks in the Lengshuikeng Ag–Pb–Zn ore field formed in the Early Lower Cretaceous. The youngest zircon U–Pb ages from pyroclastic rocks may not represent the formation/eruption ages of the host rock, depending most likely on the existence and/or abundance of juvenile or vitric pyroclasts in the rocks.  相似文献   

2017年西藏米林6.9级地震震源参数及其构造意义   总被引：1，自引：0，他引：1       下载免费PDF全文

白玲  李国辉  宋博文 《地球物理学报》2017,60(12):4956-4963

北京时间2017年11月18日06时34分,西藏自治区林芝市米林县发生了M6.9级地震.地震位于印度板块向欧亚板块插入的东北犄角,是喜马拉雅造山带地壳缩短和构造旋转变形最为强烈的部位.本研究利用多种近震和远震台网记录的波形和到时数据,对该地震的震源位置和发震时刻进行重新确定.结果表明,地震震源深度为海平面以下7 km±2 km （或地表以下10 km±2 km）,经纬度为（29.87°N±0.01°N,95.02°E±0.01°E）.结合其他地球物理和地质学资料,我们推测该地震发生在NNW向西兴拉断裂带,南迦巴瓦构造结北东向的逆冲推覆和青藏高原东南向逃逸的侧向挤出是该地震发生的主要构造背景.  相似文献