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41.
普罗旺斯.你来想象一下这片永远沐浴在阳光下的人间乐土吧……山顶上的皑皑白雪;蓝宝石般的湛蓝的海洋;欧石南、各种野生植物.橄榄树,巴旦杏树:一望无际的薰衣草田:笔直的大路两旁耸立着的高大的法国梧桐;乡村住房的铜色瓦片在阳光下闪现着熠熠光彩;  相似文献   
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To contend with the racist scaling of bodies seems to tend toward the ontological and metaphysical. Counter-strategies entail engagement with the predominant framework – i.e., with its categories of being and its grounds of analysis – however, much subjected to critique and deconstruction. Shawn Copeland and Mayra Rivera both identify and accept this “risk” in their theological projects. I argue that, although each does it with differing relative emphases, their political theologies trade upon an alternation between practical and poetical modes of critical reflection – the one is more negative and formal, the other is more positive and material; and this unitary alternation is what staves off failure in ideology and foundationalism. I furthermore suggest that the practical-poetical alternation I describe represents a contemporary politicization of the aesthetical.  相似文献   
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The masjed-i jom’e of Isfahan is one of the earliest mosques of Iran. Since 1970, Italian researchers performed an extensive archaeological investigation uncovering huge amounts of finds. This study aims at investigating the technological features and provenance of the unglazed pottery finds by using a minero-petrographic approach. Twenty-three samples of storage, table and cooking wares were selected based on the recurrence of typologically identifiable fragments and fabrics. Two bricks, seven production indicators (spacers, kiln furniture, slags) and a local clay were analysed for comparison. The production indicators and most of the pottery show high-CaO concentration. Thick-walled wares contain coarse sedimentary/metamorphic inclusions. Samples with thinner walls contain similar but fine/well-sorted inclusions. The mineralogy and microstructure indicate firing temperatures mainly ranging from 850 to 1000 °C. Low-CaO samples contain coarse sedimentary inclusions; in one sample, volcanic lithics are present. Firing temperatures range from about 800 to 950 °C, and the low-CaO character can be related to their specific function for cooking foods. One sample, found in older stratigraphic levels, differs for its peculiar calcitic temper and lower firing temperature. Local production of most samples was constrained by the composition of the inclusions compatible with the sediments of the Isfahan area. High-CaO pottery shows compositional affinity with production indicators, local clay and tiles produced in Isfahan during the Safavid period. Cooking ware usually contains local temper, with the exception of a sample with volcanic inclusions, for which a non-local provenance is supposed. No appropriate information is, however, available regarding the low-CaO clays used in the area.  相似文献   
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