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ABSTRACT

To be labeled an “eco-millenarian” has invariably pejorative connotations, insinuating the use of catastrophic rhetoric of an ecological end-times to bypass rational decision-making and democratic processes. In this article I critically assess this association, and also consider whether new political concerns – the suggestion that we are in a “climate emergency” – lend a new credibility to the structure of millenarian belief for an era of climate change. Clearly, caution is required here: the legacy of Christian millenarianism to secular politics has at times inspired peaceful, egalitarian revolution, but it is probably better known for motivating violent conflict and new forms of authoritarianism. Thus, we need to specify carefully which theological legacies are being evoked when discussing the relevance of millenarian belief today. Political theology can offer guidance to a new generation of environmental activists seeking resources with which to renew politics in times of emergency.  相似文献   
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There is growing interest in the German‐Polish border area's future status in the changing regional structure of Europe—contrasting scenarios contain, on the one hand, a vision of the region as a new ‘tiger’ region, and are seen at the other extreme as a ‘drainage area’ on the outskirts of the EU. In this article, border areas are treated from a point of view that pays more attention to the regions’ system of production and regulation. The first part deals with some general characteristics of border areas; the second part outlines in more detail the specific developmental conditions of the German‐Polish border area, especially the region between Berlin and Poznan along the middle part of the River Oder (comprising the Euro Region Pro Europa Viadrina). Three aspects of the border region's developmental conditions are emphasized: the region's quality of location within Europe and the respective national territories; the permeability of the border; and the economic structure in the border area, whereby forms of trans‐border economic linkage and cooperation are of particular interest. The last section discusses new challenges for European border areas as posed by economic change and the restructuring of the European spatial fabric.  相似文献   
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In order to constrain the age of the Upper Cretaceous continental Densuş-Ciula Formation from the Haţeg basin, South Carpathians, and correlate it with the other continental unit that occurs in the region, the Sanpetru Formation, we separated and dated by the K-Ar method biotites and amphiboles from volcanoclastic deposits. The mineral phases analysed are from two tuff layers and volcanic bombs cropping out near Rachitova village. Two tuff layers from the Densuş-Ciula Formation give early Maastrichtian ages of 69.8±1.3 and 71.3±1.6 Ma, respectively. The ages determined for the tuff layers constrain the age of deposition for the Densuş-Ciula Formation and enable further correlations with the available palaeomagnetic data from the deposits occurring along the Sibişel Valley that belong to the Sanpetru Formation. The volcanic bombs collected near to Răchitova village are andesites and dacites. The age determined by K-Ar method on hornblende separated from a volcanic bomb is 82.7±1.5 Ma, which is older than the underlying Campanian marine deposits in turbidite facies. This suggests that the volcanic bombs were re-deposited during the early Maastrichtian. Thus, the volcanics found at Răchitova have at least two origins: one type is related to an explosive synsedimentary volcanic activity, and the other type is represented by older andesitic/dacitic bombs, which most probably originate from a volcanic centre situated in the Haţeg region.  相似文献   
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