转型期社区医疗服务多元供给模式——以广州市天河区为例

以广州市统计局提供的第六次人口普查数据作为人口统计数据源,以天河区卫生局提供的社区医疗机构数据作为社区医疗服务研究数据源,以广州市天河区作为研究案例,总结出社区医疗服务存在政府供给、单位制供给、集体经济供给、社会力量供给4种模式。各供给模式均具有受卫生局领导、政府部门监管和作为城市医疗体系的基础等一系列共性,同时在供给主体、服务对象、筹资与财务管理和人事管理等方面存在差异性,形成相互补充的多元模式共存体系,社区医疗服务的准公共物品属性、社会经济体制转型与城乡二元体制、居民的多元化需求和不同供给主体的利益诉求综合作用是多元模式共存的机制。只有充分利用多元模式供给主体、全方位协调机制要素、进行合理的制度设计,才能更好地促进社区医疗服务均等化,同时为其他城市公共服务供给提供参考借鉴。     

New stratigraphic,geochronological, and structural data from the southern Guanajuato Mining District,México: implications for the caldera hypothesis

Abstract

The Cenozoic stratigraphy of the southern Guanajuato Mining District (GMD) was established 40 years ago. The existence of a caldera structure that produced the Cenozoic volcanic cover was postulated and the world-class silver ore deposit of the Oligocene age has been closely related to magmatism. In this context, we present a new geological map of the southern GMD, U–Pb and Ar–Ar ages of the volcanic units, and structural data for the Cenozoic faults. Our results document that the volcanic centre was active between ca. 33.5 Ma and ca. 31.3 Ma, coeval with NW–SE normal faulting. We propose that the Bufa, Calderones, and Cedro formations are stratigraphic units directly related to the volcanic centre. Although the younger Chichíndaro Rhyolite scarcely crops out within the study area, it appears to be more extensive outside of the study area, forming part of the rhyolitic volcanism of the Mesa Central of Mexico. In the study area, the Chichíndaro Rhyolite buries major faults, demonstrating that it was emplaced after the peak of faulting. The two main structures are the El Cubo and Veta Madre grabens; also there are several faulted and brecciated zones where silver–gold mineralization was emplaced. The extension direction changed from NE to NW producing normal faulting, reactivating older structures and allowing dike intrusion. The extensional phase continued to be active throughout the Oligocene. The age of the volcanic event and a new K–Ar age of the Veta Madre vein of 29.8 ± 0.8 Ma (K–Ar in adularia) indicate that the hydrothermal event began immediately after the emplacement of the Cedro Formation. The emplacement of the Chichíndaro Rhyolite allowed hydrothermal activity to be active for two million years or more.     

基于最小二乘支持向量机的雷暴预报初探

利用2007年和2008年南京地区NCEP 1°×1°历史再分析资料和江苏省闪电定位资料,探讨最小二乘支持向量机(LS-SVM)方法在雷暴预报中的应用.将NCEP 1°×1°资料作为实况,选取了该资料与雷暴相关性较好的参数作为预报因子,而江苏省闪电定位资料则作为预报量,建立南京地区雷暴预报的最小二乘支持向量机模型,并用...     

我国大经济区的研究与实践

经济区是客观存在的,是在经济发展过程中形成的。但我国经济区一直未能正常、稳定地形成和发展,是认识和体制上的障碍。划分大经济区要着眼远景发展方向;照顾自然区域单元的完整性和自然资源的协调性;考虑经济结构相对完整和专业化特点突出,要有大的经济中心和统一的交通运输网络;适当照顾行政区和民族自治区的完整性等原则。对比众家方案,从而提出把我国划分为东北、华北、华东、华中、华南、西南、西北、新疆、西藏九大经济区的新方案。     

SPATIAL STRUCTURE EVOLUTION OF SYSTEM OF RECREATION BUSINESS DISTRICT ——A Case of Suzhou City

The growing attention on urban tourism was very widespread. There are two angles to study urban tourism: supply-side and demand-side. And the supply-side of the tourism remains very important. The RBD (Recreation Business District) is a useful framework to understand the components of urban tourism and how they fit together. The paper begins with a review on the RBD and the spatial structure of tourism in urban areas and then attempts to develop a more general understanding of the spatial structure evolution of RBDs in a tourist-historic city—Suzhou. The spatial structures and functions of the RBDs in Suzhou are examined, based on field observations, interviews with city officials and industry leaders, and a review of available documents. The urban tourism of Suzhou has developed in a range of contexts, that various types of RBDs have emerged as a result of different urban development strategies. The spatial structure has evolved from the past “Single-cored Structure“ to “Double-cored Structure“ at present, and then to “Chain Structure“ in the future. The spatial form and evolution of RBD in Suzhou are closely relative with its urban spatial expansion. Urban area dispersal is the prerequisite of the emergence of the RBD. Planning and constructing the RBD becomes a new impetus to urban growth or renewal. Finally, a number of strategies for planning and developing the RBD in Suzhou are suggested. The different RBDs should adopt different strategies.Intensification can be the possible strategy for the RBDs in the ancient city. Accreting with the urban theme park or engrafting on the Jinji Lake is suggested respectively for the RBD in the Suzhou New District and the Suzhou Indus-trial Park.     

A STUDY ON LANDSCAPE MOSAIC STRUCTUREIN URBANRURAL AREA IN NORTHWESTOF CHINA WITH RS AND GIS- A Case Study of Xigu District in Lanzhou City

IREGIONAL BACKGROUND AND RESEARCH W6St to 68St，dlVld6S th6 Whol6 distriCt lflto tWO pdrts．METHODS The Huangshul River，the Zhuanglang River and theXlanshul River respectively low Into the Huanghe Riverl．IReglonalBackground Inthe west and northdthe region．The whole geo－morphology of＊thelogy region Is that nofth Is much lowerInknzhou City，Xlgu District，、hlch covers an than south，but both a…     

The geomorphological impact of Loch Lomond (Younger Dryas) Stadial plateau icefields in the central Lake District,northwest England

Detailed geomorphological mapping has revealed evidence for the development of plateau icefields in the central fells of the English Lake District during the Loch Lomond (Younger Dryas) Stadial (ca. 12.9–11.5 ka). The largest plateau icefield system, which covered an area of approximately 55 km² (including outlet glaciers), was centred on High Raise. To the west, smaller plateau icefields developed on Grey Knotts/Brandreth and Dale Head, covering areas of 7 km² and 3 km² respectively. The geomorphological impact of these plateau icefields appears to have been minimal on the summits, where the survival of blockfields and other frost‐weathered debris (mostly peat‐covered) implies the existence of at least patches of protective, cold‐based ice. Ice‐moulded bedrock at some plateau edges, however, documents a transition to wet‐based, erosive conditions. Prominent moraine systems were produced by outlet glaciers, which descended into the surrounding valleys where their margins became sediment traps for supraglacial debris and inwash. In some valleys, ice‐marginal moraines record successive positions of outlet glaciers, which actively backwasted towards their plateau source. This interpretation differs from that of previous workers, who assumed an alpine style of glaciation, with reconstructed glaciers emanating from corries and valley heads. It is likely that plateau icefields were more common at this time in upland Britain than hitherto has been appreciated. Copyright © 2001 John Wiley & Sons, Ltd.     

Mineral Paragenesis of the Lepanto Copper and Gold and the Victoria Gold Deposits, Mankayan Mineral District, Philippines

Abstract: Mineral paragenesis of the alteration, ore and gangue minerals of the Lepanto epithermal copper‐gold deposit and the Victoria gold deposit, Mankayan Mineral District, Northern Luzon, Philippines, is discussed. The principal ore minerals of the Lepanto copper‐gold deposit are enargite and luzonite, with significant presence of tennantite‐tetrahedrite, chalcopyrite, sphalerite, galena, native gold/electrum and gold‐silver tellurides. Pervasive alteration zonations are commonly observed from silicification outward to advanced argillic then to propylitic zone. The ore mineralogy of the Lepanto copper‐gold deposit suggests high f_S2 in the early stages of mineralization corresponding to the deposition of the enargite‐luzonite‐pyrite assemblage. Subsequent decrease in the f_S2 formed the chalcopyrite‐tennantite‐pyrite assemblage. An increase in the f_S2 of the fluids with the formation of the covellite‐digenite‐telluride assemblage caused the deposition of native gold/electrum and gold‐silver tellurides. The principal ore minerals of the Victoria gold deposit are sphalerite, galena, chalcopyrite, tetrahedrite and native gold/electrum. The alteration halos are relatively narrow and in an outward sequence from the ore, silica alteration grades to illitic‐argillic alteration, which in turn grades to propylitic alteration. The Victoria gold mineralization has undergone early stages of silica supersaturation leading to quartz deposition. Vigorous boiling increased the pH of the fluids that led to the deposition of sulfides and carbonates. The consequent decrease in H₂S precipitated the gold. Gypsum and anhydrite mainly occur as overprints that cut the carbonate‐silica stages. The crosscutting and overprinting relationships of the Victoria quartz‐gold‐base metal veins on the Lepanto copper‐gold veins manifest the late introduction of near neutral pH hydrothermal fluids.     

四川南坪马脑壳金矿区的构造与成矿

论述了马脑壳金矿区成矿地质构造背景和构造变形特征，探讨了构造演化及应力场特征。重点总结了构造控矿规律：即不同级序断裂对金矿的控制、NWW向韧脆性扭压性断裂及NIVE－NE向张扭性断裂对金矿的控制、断裂性质转化及复合叠加对金矿的控制、控制金矿化局部富集的构造因素、控矿断裂构造地球化学特征及与成矿的关系。指出本区金矿的形成经历了成矿物质多期活化—迁移—富集的复杂演化过程。     

乡村景观多功能权衡–协同关系时空格局研究——以上海市青浦区为例

景观多功能定量化及其权衡–协同关系研究是景观生态学研究的热点。研究针对景观功能相互表征的科学性和景观多功能间关系定量化问题,以上海市青浦区为例,采用"生产–生活–生态"功能框架构建6种乡村景观功能,利用1980–2018年的基础数据,采用Spearman秩相关系数分析和双变量空间自相关相结合的方法,对该区域184个行政村的乡村景观多功能间权衡–协同关系变化特征进行研究,得到以下结果:(1)都市郊区的农业生产功能不能取代经济发展功能,青浦区经济发展功能已成为主导的功能形态。(2)青浦区乡村景观多功能间权衡–协同关系时空差异显著,表现为:农业生产功能与经济发展功能、经济发展功能与生态调节功能、经济发展功能与环境维衡功能始终呈现为权衡关系,为该区不可回避的矛盾,该结果表明该区经济发展是以牺牲生态环境为代价实现的;经济发展功能与景观美学功能间权衡关系显著,且二者关系格局呈东部权衡、西部协同,权衡区的数量递增;经济发展功能与空间承载功能间关系格局呈现东部权衡和西部协同格局,且协同关系区呈增长趋势;景观美学功能与生态调节功能/环境维衡功能间权衡区集中在青东区域,协同区分布于青西区域,且权衡区数量先增后减,协同区先减后增。(3)时空结合的分析方法能准确全面地反映乡村景观多功能间权衡–协同关系演变特征。