历史观与意识形态:世界历史叙事中的现代化理论

作为世界历史叙事的一种范式,现代化理论不仅体现了一种历史观,也展示了其意识形态的特质。现代化理论的意识形态功能包括：解释功能、压制宣传功能、整合和激发功能以及合法化功能,这些功能使世界历史叙事充斥着偏见与“公允”、“真理”与权力、压制与整合等悖论。这种悖论在历史观层面,则凸显为现代化的“历史观”和历史观的“现代化”二者之间的张力。只有克服二者之间的张力,才能超越现代化的“历史观”的局限,才能使历史观的“现代化”成为一种世界历史叙事的实践理念。     

‘Las Vegas is not where we are’: Queer readings of the Civil Partnership Act

This article interrogates the United Kingdom's new Civil Partnership Act, which is intended to create a new legal status of ‘civil partner’. The Act confers benefits and imposes legal responsibilities on those same-sex couples who register their relationships. Analysing the Governmental material produced in support of the legislation, as well as Parliamentary debates, the article provides a critical analysis of the ideological underpinnings of civil partnership. A series of dichotomies—marriage/not marriage; sex/no sex; status/contract; conjugality/care; love/money; responsibilities/rights—informs the Government's construction of the category of ‘same-sex partner’. Those dichotomies lend themselves to a deconstructive analysis, applying the insights of queer theory. The result is a skepticism regarding the Act's replication of a marriage model for same-sex couples. Instead, the article concludes by advocating the search for more pluralistic and flexible legal models that better represent the diversity of relationship forms found today.     

改革以前的中国共产党与自然科学基础理论研究

毛泽东是中国共产党科技思想发展的奠基者和探索者。他认为,科学技术是认识自然、改造自然、争取自由的思想武装;是推动生产力发展的革命力量;是经济和社会发展的重要动力;是社会主义本质的内在要求;是实行社会主义现代化的关键因素;是发挥社会主义制度优越性、赶超世界先进水平的重要保证。发展科学技术,要坚持跨越式发展和重视基础理论研究的统一;坚持自力更生和争取外援的统一;坚持社会革命和技术革命的统一;坚持培养人文精神和科学精神的统一;坚持党的领导和百花齐放、百家争鸣的统一;坚持发挥科学技术专家和普通工人群众的作用。毛泽东科技思想为邓小平科技思想的形成和发展奠定了理论基础。     

日本的海权观及其海洋领土争端——一种建构主义的尝试分析

东北亚国家对于海洋权益的认知渐进深入,以及地缘政治实况和国家实力消长等,构成了社会意识与物质力量变迁的合力,加剧了日本与周边国家之间普遍存在海洋领土争端这一社会情势。当代西方国际关系理论中的建构主义为上述实况提供了一种新的思维尝试、分析框架与消解困境的方案补充。东北亚海洋领土争端困境的解决关键在于如何利用预留的政治空间。     

The Materiality of Social Power: The Artifact-Acquisition Perspective

This paper explores the materiality of social power relationally through study of social interactions with artifacts. Specifically, it is argued that acquisition of an artifact instantiates social power by imposing interactions on groups taking part in that artifact's life-history activities. We introduce the “performance-preference matrix,” an analytic tool for systematically studying the effects of such acquisition events on activity groups. The use of the performance-preference matrix is illustrated through an example: the acquisition of electric-arc lights for lighthouses in the 19th century. Suggestions are offered for analyzing culture-contact situations and for handling singularized artifacts such as heirlooms and monuments.

Fluid flow in shear zones: insights from the geometry and evolution of ore bodies at Renco gold mine,Zimbabwe

The geometry of mineral deposits can give insights into fluid flow in shear zones. Lode gold ore bodies at Renco Mine, in the Limpopo Belt, Zimbabwe, occur as siliceous breccias and mylonites within amphibolite facies shear zones that dip either gently or steeply. The two sets of ore bodies formed synchronously from hydrothermal fluids. The ore bodies are oblate, but have well‐defined long axes. Larger ore bodies are more oblate. High‐grade gold ore shoots have long axes that plunge down dip; this direction is perpendicular to the long axes of the low‐grade ore bodies. The centres of the high‐grade ore bodies align within the low‐grade ore bodies along strike in both gently and steeply dipping groups. The range of sizes and shapes of the ore bodies are interpreted as a growth sequence. Geometrical models are proposed for the gently and steeply dipping ore bodies, in which individual ore bodies grow with long axes plunging down dip, and merge to form larger, more oblate ore bodies. The models show that when three or more ore bodies coalesce, the long axis of the merged ore body is perpendicular to the component ore bodies, and that ore bodies in the deposit may have a range of shapes due to both growth of individual ore bodies, and their coalescence. The long axes of the high‐grade ore bodies are parallel to the shear directions of both the gently and steeply dipping dip slip shear zones, which were the directions of greatest permeability and fluid flow. The larger, lower grade bodies, which may have formed by coalescence, are elongate perpendicular to these directions.     

The modemization paradigm based on monistic multi-linear theory: a response to some comments

Long before 1979, Chinese historical research had been dominated by the theory of “the Five Modes of Production”, according to which the whole Chinese history as well as the other parts of the world had been developed from the first MOD to the last one by one. The modernization theories prevailed during the 1950s and the 1960s, bringing about another uni-linear model of historical changes. For example, W. W. Rostow designed a five-stage process as a universal frame work of economic development, based on which each society could find its position in this uni-line. The task of the less developed societies is just to introduce modemity from the modernized societies so that they can make some developments. Thus modernization is a uni-direction movement as well as a uni-linear process. After 1979, modernization as a new paradigm has been accepted by an increasing number of Chinese historians. The increasing depth and breadth of the academic researches have encouraged such an acceptance, but, admittedly, as a new conceptual system that corresponded to the historic breakthrough and the new direction towards modernization in China. This acceptance also showed the “crisis of paradigm”, that is, the contradiction between the new themes and the old ones that had dominated Chinese humanities and social sciences. The modernization paradigm based on monistic multi-linear theory considers modernization as a unique breakthrough in history, a great transformation around the whole world, and a historical process that does not have a given ultimate aim and value but different models and routes. The monistic multi-linear theory on historical development is open and all-embracing in historical studies. A variety of historical paradigms is favorable to prosperity of Chinese history. __________ Translated from: Shixue Yuekan 史学月刊 (Journal of Historical Science), No.5, 2004, by Wang Fan; Revised by Chong Hua     

Foreign Banking in China: A Study of 279 Branch Units in 32 Cities

Two China-based geographers examine the gradual relaxation of restrictions on the activity of foreign banks in China as a prelude to a more focused investigation of the concentrated locational pattern of foreign banking in that country. The study, which embraces 32 Chinese cities, emphasizes the factors that have attracted foreign banks to particular cities and regions of China, including the existence of special banking opportunities, the so-called "follow-the customer" strategy, externalities associated with major financial centers such as Beijing and Shanghai, relaxed banking regimes in particular urban centers and special economic zones, and exposure to international trade and to a variety of foreign business enterprises. The locational preferences of foreign banks in relation to their countries of origin are addressed in some detail.     

The Archaeology of California

Stimulated by several important, recent empirical advances, California archaeologists are engaged in a series of lively debates. These advances include new discoveries about the early peopling of western North America and sustained occupation of the California coasts as early as 12–13,000 BP. There also have been significant new developments in the role of paleoenvironmental change in cultural evolution, the emergence of long-distance interaction spheres, the presence of intensive craft specializations, and the appearance of sociopolitically complex hunter–gatherers. This article addresses these issues—and several others—with a view to the general interests of scholars worldwide. The exceptional heterogeneity of California ecosystems (from deserts to dense redwood forests to bountiful offshore islands) and the remarkable cultural diversity exhibited by the dozens of major groups who made these lands their home combine to produce a complex indigenous sociopolitical picture. Current understandings reveal myriad trajectories of cultural change across nine major subregions of the state.     

Thermal convection in faulted extensional sedimentary basins: theoretical results from finite-element modeling

Thermal convection has the potential to be a significant and widespread mechanism of fluid flow, mass transport, and heat transport in rift and other extensional basins. Based on numerical simulation results, large‐scale convection can occur on the scale of the basin thickness, depending on the Rayleigh number for the basin. Our analysis indicates that for syn‐rift and early post‐rift settings with a basin thickness of 5 km, thermal convection can occur for basal heat flows ranging from 80 to 150 mW m^?2, when the vertical hydraulic conductivity is on the order of 1.5 m year^?1 and lower. The convection cells have characteristic wavelengths and flow patterns depending on the thermal and hydraulic boundary conditions. Steeply dipping extensional faults can provide pathways for vertical fluid flow across large thicknesses of basin sediments and can modify the dynamics of thermal convection. The presence of faults perturbs the thermal convective flow pattern and can constrain the size and locations of convection cells. Depending on the spacing of the faults and the hydraulic properties of the faults and basin sediments, the convection cells can be spatially organized to align with adjacent faults. A fault‐bounded cell occurs when one convection cell is constrained to occupy a fault block so that the up‐flow zone converges into one fault zone and the down‐flow zone is centred on the adjacent fault. A fault‐bounded cell pair occurs when two convection cells occupy a fault block with the up‐flow zone located between the faults and the down‐flow zones centred on the adjacent faults or with the reverse pattern of flow. Fault‐bounded cells and cell pairs can be referred to collectively as fault‐bounded convective flow. The flow paths in fault‐bounded convective flow can be lengthened significantly with respect to those of convection cells unperturbed by the presence of faults. The cell pattern and sense of circulation depend on the fault spacing, sediment and fault permeabilities, lithologic heterogeneity, and the basal heat flow. The presence of fault zones also extends the range of conditions for which thermal convection can occur to basin settings with Rayleigh numbers below the critical value for large‐scale convection to occur in a basin without faults. The widespread potential for the occurrence of thermal convection suggests that it may play a role in controlling geological processes in rift basins including the acquisition and deposition of metals by basin fluids, the distribution of diagenetic processes, the temperature field and heat flow, petroleum generation and migration, and the geochemical evolution of basin fluids. Fault‐bounded cells and cell pairs can focus mass and heat transport from longer flow paths into fault zones, and their discharge zones are a particularly favourable setting for the formation of sediment‐hosted ore deposits near the sea floor.