Potash-rich volcanic rocks and lamprophyres in western Shandong Province: 40Ar39Ar dating and source tracing

Highly precise 40Ar39Ar dating results demonstrate that the ages of potash-rich volcanic rocks in western Shandong Province are 114.7-124.3 Ma, and that of the lamprophyres is 119.6 Ma. The potash-rich volcanic rocks have relatively high (87Sr/86Sr)i ratios ( 0.708715-0.711418)and distinctly negative εNd values ( -11.47 - -17.54), and are enriched in radiogenic lead (206Pb/204pb=17.341-17.622,207pb/204Pb=15.525-15.538, 208Pb/204pb = 37.563-37.684).Similarly, the lamprophyres also have quite low εNd values ( -11.57 - -19.64). Based on the fact that the Sr, Nd and Pb isotopic compositions of potash-rich volcanic rocks are very consistent with that of the clinopyroxene separates, and by integrating comprehensive analyses of their tectonic settings,and extensive comparisons of the Sr, Nd isotopic compositions with that of the related simultaneous rocks, it is concluded that the potash-rich volcanic rocks and lamprophyres in western Shandong Province were most possibly derived from the partial melting of enriched mantle which was caused by source contamination and metasomatism of subducted continental crustal materials.``     

Further support for a Cretaceous age for the feathered-dinosaur beds of Liaoning,China:New 40Ar/39Ar dating of the Yixian and Tuchengzi Formations

We report new 40Ar/39Ar dating results obtained from total fusion and incremental-heating analyses of sanidine and biotite from three tuffs found interbedded within the fossil-bearing deposits of Liaoning, northeast China. The first is a new sample of the Bed 6 Sihetun tuff from the Yixian Formation, previously dated by our team as middle Early Cretaceous, and recently considered by Lo et al., partially reset due to metamorphism from a nearby basaltic sill. The second is the Yixian Bed 9 tuff from Hengdaozi considered by Lo et al. to be unaffected by metamorphism and whose age, based on total fusion 40Ar/39Ar dating of biotite, argues for a Jurassic age for the Yixian Formation.The third tuff is a previously undated tuff from the upper part of the underlying Tuchengzi Formation. Single crystal total fusion 40Ar/39Ar analyses of the Sihetun sanidine showed homogeneous radiogenic Ar, Ca/K ratios, excellent reproducibility and gave a mean age of 125.0 ± 0.18 (1SD) ±0.04 (SE) Ma. Single sanidine crystal total fusion 40Ar/39Aranalyses of the Hengdaozi tuff gave a mean age of 125.0 +0.19 (1SD) ± 0.04 (SE) Ma, which is indistinguishable from the Sihetun tuff. The Tuchengzi Formation tuff gave a mean age of 139.4 ± 0.19 (1SD) ± 0.05 (SE) Ma. Detailed laser incremental-heating analyses of biotite from Sihetun, Hengdaozi, and Tuchengzi tuffs show disturbed Ar release patterns and evidence of trapped argon components. We conclude from these analyses that the total fusion dates on biotite by Lo et al. are erroneously old and isotopic dating of both biotite and sanidine from tuffs of the Yixian Formation point to a middle Early Cretaceous age. The upper part of the Tuchengzi Formation can be referred to the Early Cretaceous.``     

Modeling studies on the changes of the Subtropical High over the Western Pacific during the last 100 years

Intensity index series of Subtropical High over the Western Pacific was constructed according to modeling results by using of CCM3.6 atmospheric model with climatologically SST forcing for 30 years, and with observed SST forcing from 1900 to 2000. The index series constructed by modeling closely correlated to the observations for 1951-1999 (c.c. 0.72) and to the statistically reconstructed one for 1900-1950 (c.c. 0.51). The index series for 1900-1999 showed significant 80 a and 40 a periodicity. A minimum of persistence in seasonal variations of the index occurred in Autumn, which was called "Autumn Barrier". It may relate to the "Spring Barrier", found in the seasonal variations of SST over the Eastern Equatorial Pacific. The increasing trend shown in the index series for the 20th century may associate with the global warming caused by enhancement of greenhouse effect.     

鄂西-渝东区石炭系油气成藏影响因素及富集规律

针对鄂西－渝东区近年钻探效果不理想的问题，分析了该区油气成藏的影响因素和富集规律。结果表明，该区大型古隆起的继承性发育、区域性油气运移和圈闭形成时间早晚的匹配、石炭系储层的发育程度和上覆地层异常高压的存在、有效供气面积的大小，以及断裂的封堵性和渗入水的强度等，是影响油气聚集和保存的主要因素。认为该区石炭系的油气勘探，应以开江－梁平古隆起南缘和石柱古隆起为重点。     

北祁连山西段石炭二叠系界线初析兼论对大黄沟群的再研究

在大量野外工作和充分讨论国内外石炭——二叠系界线划分意见的基础上,本文初步分析了北祁连山西段石炭——二叠系界线,讨论了该区大黄沟群、大黄沟组和山西组的关系及时代,指明早二叠世早期地层在北祁连山西段确实存在,没有缺失。     

用蛋白质印迹技术检测马槟榔甜蛋白

从马槟榔（ＣａｐｐａｒｉｓｍａｓａｉｋａｉＬ．）种子中分离纯化了马槟榔甜蛋白，并对其氨基酸组成和紫外吸收光谱等理化性质进行了分析测定。用纯化的马槟榔甜蛋白免疫家兔，获得其抗血清，并利用此抗血清通过蛋白质印迹技术检测马槟榔甜蛋白，为马槟榔甜蛋白的基因工程研究提供了专一和灵敏的检测方法。     

中西药结合治疗感染性少、弱精子症临床分析

为探讨中西药结合治疗感染性少、弱精子症疗效,对73例存在不同部位生殖系统感染的少精子症或弱精子症引起的不育症患者应用相应抗生素治疗的同时均给予中药治疗,3个月为一个疗程,间隔3个月后复查精液常规,随访生育情况一年.结果:少精子症组随访中有9例妻子妊娠,妊娠率为33.3%.其中1例因剧烈活动妊娠2个月流产.弱精子症组随访中有17例妻子妊娠,妊娠率为37.0%,其中1例无明显原因妊娠2个月后流产.治疗前、后两组精液各项参数明显改善(P＜0.05).说明中、西药结合治疗感染性少、弱精子症起到标本兼治的疗效,少精子症、弱精子症妻子妊娠率均高于自然妊娠率,精液参数明显提高.     

近代知识分子与中国近代化

近代的知识分子是当代社会中一个独特的群体。面对历史性的民族危机,他们表现出：（1）同一个“救亡图存,富国强兵”的心愿;（2）共一条学习西方的道路;（3）开放与守旧并蓄的“中体西用”原则;（4）幻想化的教育救亡途径;（5）痛苦的“鱼”与“熊掌”的选择。显现出当代知识分子在特定的历史背景下所作的强国之举,及其在客观上推进中国社会近代化进程的有限却富历史意义的作用。     

浅论西方国家会计信息失真

通过考察西方治理会计信息失真的过程和经验,提出了一些治理我国会计信息失真的制度建设和制度安排的建议。     

^226Ra evidence for the ecosystem shift over the past 40 years in the North Pacific Subtropical Gyre

Surface seawater was collected for ~(226)Ra measurement in the North Pacific Subtropical Gyre from July to October, 1999 and October to December, 2003. Combined with the historical data reported for this sea area, a declined trend of surface ~(226)Ra concentrations was observed since 1960s, indicating the ecosystem shift in response to global warming. On one side, the enhanced stratification of the upper water column resulting from global warming reduced the ~(226)Ra input from the depth, on the other, the temporal increase of biological production resulting from the climate-related ecosystem structure change strengthened the ~(226)Ra removal from the surface ocean. Both the physical and biological processes resulted in the decrease of surface ~(226)Ra concentrations in the North Pacific Subtropical Gyre. The temporal trend of surface ~(226)Ra concentrations was consistent with the trends of chlorophyll a, silicate, phosphate and primary production previously reported. This study provided ~(226)Ra evidence for the ecosystem shift under global change.