National territorial planning at the turn of the 21st century

In the early stages of economic development in Korea, national territorial planning was used as a policy tool to guide spatial structure and to provide physical infrastructure for urban and industrial development. Such a top-down approach was inevitable because Korea maintained the centralized political and government system until the early 1990s. Circumstances, however, have changed recently since the 1990s with progress in democratization and localization. In addition, forces of globalization are making significant impacts on the parameters of national territorial planning. Reflecting these changes in both internal and external conditions, the Fourth National Territorial Plan (2000–2020) has adopted a different approach from the past three territorial plans. This paper reviews the socio-economic background that necessitated such changes in approaches to national territorial planning. A major thrust of the Fourth Plan, a focus on emergent or anticipated planning issues in Korea, is discussed. Finally, the paper examines the rationale for long-term strategic planning in the highly fluctuating situation facing Korean society in the new century.     

Metastability of granulites and processes of eclogitisation in the UHP region of western Norway

The Flatraket Complex, a granulite facies low strain enclave within the Western Gneiss Region, provides an excellent example of metastability of plagioclase‐bearing assemblages under eclogite facies conditions. Coesite eclogites are found <200 m structurally above and <1 km below the Flatraket Complex, and are separated from it by amphibolite facies gneisses related to pervasive late‐orogenic deformation and overprinting. Granulites within the Flatraket Complex equilibrated at 9–11 kbar, 700–800°C. These predate eclogite facies metamorphism and were preserved metastably in dry undeformed zones under eclogite facies conditions. Approximately 5% of the complex was transformed to eclogite in zones of fluid infiltration and deformation, which were focused along lithological contacts in the margin of the complex. Eclogitisation proceeded by domainal re‐equilibration and disequilibrium breakdown of plagioclase by predominantly hydration reactions. Both hydration and anhydrous plagioclase breakdown reactions were kinetically linked to input of fluid. More pervasive hydration of the complex occurred during exhumation, with fluid infiltration linked to dehydration of external gneisses. Eclogite facies shear zones within the complex equilibrated at 20–23 kbar, 650–800°C, consistent with the lack of coesite and with the equilibration conditions of external HP eclogites. If the complex experienced pressures equivalent to those of nearby coesite eclogites (> 28 kbar), unprecedented metastability of plagioclase and quartz is implied. Alternatively, a tectonic break exists between the Flatraket Complex and UHP eclogites, supporting the concept of a tectonic boundary to the UHP zone of the Western Gneiss Region. The distribution of eclogite and amphibolite facies metamorphic overprints demonstrates that the reactivity of the crust during deep burial and exhumation is strongly controlled by fluid availability, and is a function of the protolith.     

华东某些山区第四纪古纬度变化

据１８８个古地磁样品和样品产地的地理坐标、余纬度、平均磁偏角和磁倾角，求得样品产地的古纬度．本区古纬度比现今纬度低：７．６°－８．２°，６．６°－６．８°，６．０°－６．５°，２．３°－３．４°，０．２°－０．６°．变化由印度板块和太平洋洋壳北推合力所致．     

浙江山区珍稀濒危植物的分布特征与保护

浙江山区的珍稀濒危植物较为丰富，有６７科、１０８属、１２５种．论述了当地珍稀濒危植物的特点、地理分布、属和种的地理成分，探讨了珍稀濒危植物的就地保护、迁地保护和离体保存．     

珠江三角洲工业地域分工研究

本文从专业化部门的数量和发展水平以及专业化部门地区分布和组合两方面揭示珠江三角洲工业地域分工的基本特点。指出新形势下虽然不少县市存在专业化部门多而不精，工业结构趋同的问题，但珠江三角洲地域分工格局已开始形成。文章还讨论了形成工业地域分工特点的原因并提出了完善地域分工的措施。     

中国热带,亚热带西部地区热量带的划分

我国热带，亚热带西部地区山多，高原广，垂直地带性的影响，给热量带的划分带来了困难，因为垂直气候都具有在该地区纬向气候带的基础上衍生而生的，因此，亚热带西部地区热量带的划分也应以纬向地带性为主，基带气候为中亚热带的云贵高原和金沙江河谷仍应归属于中亚热带，青藏高原破坏了纬向地带性规律，其东侧应有一条亚热带西界，这一界线应是北、中、南亚热带遇到青藏高原后的中断界线，而不是北、中、南亚热带与青藏高原寒气候     

秦巴地区矿产资源和成矿分布规律

对秦巴地区的成矿地质构造进行了分区和分期,定量地论述了区域矿产资源的特色和组成总貌,全面系统地总结论述了7种矿床类型及其成矿特征,阐述了区域成矿分布规律,反映了该区矿产地质的研究现状。     

核安全导则中的地震震级划分意义

本文论述了我国核安全导则中对地震进行两级划分的意义,着重讨论了大震在选址地震工作中的作用。最后,结合我国地震条件提出了大震划分的起算标度。     

新地震区划图的几个基本问题

我国新的地震区划图(1990年版)是采用地震危险性慨率分析方法编制的。该图给出的是场点地震烈度值,该值在50年内被突破的概率为0.1。人们普遍关注该图与我国曾经编制的地震区划图(1957年版,1977年版)的区别,该图超越概率概念的内含和外延以及超越概率水平为什么采用50年超越概率0.1。本文围绕这些问题进行了讨论。分析结果表明,前两张地震区划图编图的基本着眼点都是地震预测,而新的地震区划着眼于场点的地震动预测。新的地震区划图是按场点地震危险性分析方法给出的,它所表示的地震危险性只能针对具体的场点,不能完全反映区域的地震危险性特征。而弄清场点地震危险性和区域地震危险性的差异是正确进行区域防灾对策的基础。作者希望这些讨论能对正确使用新的地震区划图有所裨益。