在融汇中走向疏离——闽文学史建构中的域性特质论

闽文学史是有着自己鲜明地域文化特色的区域文学史。其形成是在静态的福建地域文化和动态的外来文化的双向影响、润渍下完成的。两种文化融汇的契机是闽人外迁和外籍士人内迁入闽的双向人员流动。闽文学史的艺术特质体现在文学创作主体的殊异性、文学创作客体的参差性、文学发展演变轨迹的乖违性、文学思潮与运动的源发性等四个方面。闽文学史的发展是一个在融汇中不断走向疏离的过程。在融汇中,闽文学史走向了成熟;而在不断地疏离中,闽文学史最终获得了新生,从而确立了其作为学科存在的意义。

区域文化与闽文学史的建构

作为区域文学史，闽文学的发展轨迹深深烙上了鲜明的地域文化印记。其形成是在静态的福建地域文化和动态的外来文化的双向影响、润渍下完成的。闽文学史的发展是一个在融汇中不断走向疏离的过程。在融汇中，闽文学史走向了成熟；而在不断地疏离中，闽文学史最终获得了新生，从而确立了其作为学科存在的意义。

Exterior Quality and Physical Properties of Hongda Tobacco in Yunnan Province

[Objective] The aim was to analyze the exterior quality and physical prop- erties of Hongda Tobacco in Yunnan Province, thus providing references for planting planning, technology and selection of raw materials. [Method] Hongda C3F progenies were chosen from 24 villages and towns in Qujing, Kunming, Baoshan and Dali, and the concerning exterior quality and physical properties were analyzed through cluster analysis. [Result] The openness and width of C3F differed significantly among Qujing, Kunming, Baoshan and Dali. The thickness, stem content, equilibrium moisture con- tent extremely differed, and density and filling power varied significantly. Most physi- cal properties, such as equilibrium moisture content and density, of Dali Hongda were quite different from those in Qujing, Kunming and Baoshan, indicating that Dali Hongda enjoys special characteristics in physical properties. In addition, stem content in east, center and west areas of Yunnan Province differed significantly and Hongda in Yunnan could be classified into four species according to physical property. [Conclusion] The research has laid basis for planting planning, technology and raw mate- rials selection of Hongda tobacco.

Regional differences in crustal structure of the North China Craton from receiver functions

Moho depth and crustal average Poisson＇s ratio for 823 stations are obtained by H-n： stacking of receiver functions. These, to- gether with topography and receiver function amplitude information, were used to study the crustal structure beneath the North China Craton （NCC）. The results suggest that modified and preserved crust coexist beneath the craton with generally Airy-type isostatic equilibrium. The equilibrium is relatively low in the eastern NCC and some local areas in the central and western NCC, which correlates well with regional geology and tectonic features. Major differences in the crust were observed beneath the eastern, central, and western NCC, with average Moho depths of 33, 37, and 42 km and average Poisson＇s ratios of 0.268, 0.267 and 0.264, respectively. Abnormal Moho depths and Poisson＇s ratios are mainly present in the rift zones, the northern and southern edges of the central NCC, and tectonic boundaries. The crust beneath Ordos retains the characteristics of typical craton. Poisson＇s ratio increases roughly linearly as Moho depth decreases in all three parts of the NCC with different slopes. Receiver function amplitudes are relatively large in the northern edge of the eastern and central NCC, and small in and near the rifts. The Yanshan Mountains and southern part of the Shanxi rift show small-scale variations in the receiver-function ampli- tudes. These observations suggest that overall modification and thinning in the crust occurred in the eastern NCC, and local crustal modification occurred in the central and westem NCC. Different crustal structures in the eastern, central, and western NCC suggest different modification processes and mechanisms. The overall destruction of the crustal structure in the eastern NCC is probably due to the westward subduction of the Pacific Plate during the Meso-Cenozoic time; the local modifications of the crust in the central and western NCC may be due to repeated reactivations at zones with a heterogeneous structure by successive thermal-tectonic events during the long-term evolution of the NCC.