界在有无缥缈间——评鲁枢元的《文学的跨界研究》

鲁枢元先生三卷本的《文学的跨界研究》新近出版,这应是他三十年来文学理论研究成果的结晶,其中一个突出的关键词就是"跨学科"。他在"无界"的状态下开始进入文学的跨学科研究,涉足心理学、语言学和生态学,但所有的跨越都围绕着一个中心,那就是对文学的个体心灵与诗意空间的坚守。当他在文学心理学、文学言语学、生态文艺学三块领域都取得显著成果时,他却对"学科"由执着转向反思和质疑,在他看来,学科的跨越起源于原本的"无界"状态,经历学科壁垒森严的阶段,必然还要打破一个个"牢笼",重新回归"无界"的自然状态。     

何思源政治理念初探

作为一名从政多年且充满爱国热忱的民主人士,何思源所秉持的政治理念是当时那个时代的典型代表之一。在长期的政治与社会实践中,何思源形成了较为务实的"求生"政治理念。可以说,"求生"是其政治理念的核心内容。     

论贺铸诗词创作之间的相互影响

贺铸是北宋中后期著名词人,此外,贺铸亦擅作诗。贺铸的诗词在某些方面是大致相通的,诗词创作之间有着相互影响,贺铸通过娴熟地运用音律、以比兴寄心志、以健笔写柔情三种手法,将诗的艺术手法引入词中,对以诗为词的深化作出了自己独特的贡献。而在诗歌创作的过程中,贺铸也不自觉地将词的一些作法带入了诗中,使得其部分诗作呈现出词要眇宜修和言长的独有风致。     

《河防通议·算法门》初探

现存探讨河防技术的最早著作是由其祖为大食人的元代沙克什重编的《河防通议》。该书算法门把当时很多先进的数学方法用于工程计算，特别是使用了天元术，这在技术著作中还是首次见到。该文分三部分研究了算法门：第一部分介绍了该书的内容和沙克什的身世；第二部分研究算法门的数学问题；第三部分证明了该书各个部分都非沙克什本人所著，他只是在北宋汴本和金都水监本的基础上进行了重编，并写了部分注释。     

He-Ar isotopic system of fluid inclusions in pyrite from the molybdenum deposits in south margin of North China Block and its trace to metallogenetic and geodynamic background

The helium and argon isotopic compositions of the ore-forming fluids from the molybdenum deposits such as Jinduicheng, Donggou, Shijiawan, and Sandaozhuang, which are located in the East Qinling molybdenum belt in south margin of North China Block （SMCNB）, are reported in this paper. The origin and the evolution of the ore-forming fluids and their coupled-relationships with the intra-continental collision and orogenic process of Qinling Orogen in Mesozoic-Cenozoic have been discussed. The 3He/4He and 40Ar/36Ar values （3He/4He=1.38-3.64 Ra, and 40Ar/36Ar=295.68-346.39, respectively） of the fluid inclusions in pyrite from the molybdenum deposits in East Qinling suggest that, the ore-forming fluid system is mixed by two end members. One is the high temperature deep-derived fluid congenetic with the porphyries generated by crust-mantle mixing, and the other is the low-temperature meteoric water which is rich in crustal radiogenic He with the component of atmospheric Ar. From the Pb isotopic composition, and ore-bearing potential of the porphyry and the regional stratum, we can conclude that the ore-forming materials of the deposits in the East Qinling molybdenum belt are derived from the deep source by the mixing of lower crust and upper mantle. Therefore, the formation of the molybdenum deposits in SMNCB can be related to the crust-mantle interaction, which is accompanied by the intra-continental orogenic and extension process in the post-collision period of Qinling Orogen. The granitic porphyries which are related to Mo mineralization are not simple crust-remelting type granites or S type granites, but belong to syntexis-type or mantle-derived granites, hence their formation has a profound and regional geodynamic background.     

试论何挺颖在井冈山斗争时期的军事贡献

何挺颖参加了湘赣边界秋收起义,任工农革命军第一团一连党代表。在三湾改编中,他始终支持毛泽东同志的政治主张;面对叛徒的叛变行径,他立场坚定;在龙源口等战斗中作战勇猛,特别是在黄洋界保卫战中,他指挥英明、果断,为井冈山革命根据地的创建作出了重要贡献。     

以美学视角的“对等”比较李白诗歌中数词的英译

奈达的功能对等理论为李白诗歌英译研究提供了具体可操作的衡量标准。以数词的英译为切入口,以美学视角下的“对等”比较李白诗歌意境美、气势美和情感美等非纯形式诗歌特质在译诗中的还原和再现,对李白诗歌英译研究具有指导和突破意义。     

关于李斯研究的几个问题

李斯把法家思想作为秦统一后的统治思想是秦国传统发展的必然结果。法家思想的彩和遭到了儒家的反对,李斯为贯彻法家思想,提出了焚书之议,此后在作始皇又有坑儒之举,但焚书坑儒并没有灭绝古学,也不是造成百家争鸣局面结束的根本原因。李斯法家思想的来源,主要是荀子、韩非子、吕不韦和商鞅。桴斯工没有真正掌握法家思想的精髓。他歪曲了法家的本意,最终造成秦的速亡,使法家思想蒙受不白之冤。     

郑和下西洋与麒麟贡

明代将非洲产的长颈鹿比附为麒麟。象征圣王出世的麒麟,成为下西洋期间的重要搜求对象。整理郑和下西洋期间麒麟史料,归纳为以下数端：（1）永乐十二年（1414年）榜葛刺贡麒麟可能与郑和无关;（2）榜葛剌贡麒麟可能促使郑和第四次下西洋西进波斯湾,并促成麻林贡麒麟;（3）郑和第五、六、七次下西洋皆有麒麟史料;（4）宣德八年（1433年）之麒麟贡可能以购自天方者抵充;（5）下西洋远至东非的动机,可能是为了搜求长颈鹿等非洲特产。     

Late Cretaceous-Cenozoic exhumation history of Tiantangzhai region of Dabieshan Orogen： Constraints from （U-Th）／He and fission track analysis

Integrated fission track and (U-Th)/He analysis is carried out on 6 apatite and 6 zircon samples from a near vertical section in The Tiantangzhai region at the core of the present Dabieshan orogen. The result shows that the region experienced cooling/exhumation during the Late Cretaceousand Early Tertiary period. Age-elevation relationships for different dating systems and different minerals suggest a pulse of rapid exhumation at ～110 Ma before present, preserved in the structurally highest samples. At lower elevations, ages begin to decrease with decreasing elevation, suggesting lower exhumation rates since 90 Ma. Two periods of different exhumation rates are identified since 90 Ma. The average apparent exhumation rate for the period of 43.4—22.5 is 0.062 km/Ma, whereas that for the period of 76.4—47.4 Ma is 0.039 km/Ma.