A FURTHER INQUIRY ON 30-60 DAY OSCILLATION IN THE TROPICAL ATMOSPHERE

Based on the ECMWF data(1980-1983) and others, a further inquiry on the activities and the structure feature of 30-60 day oscillation in the tropical atmosphere has been completed. The following results are obtained:There is stronger perturbation kinetic energy of 30-60 day atmospheric oscillation(AO) in the equatorial eastern Pacific. This means the equatorial eastern Pacific is a stronger activity region of 30-60 day AO in the tropics. Analyses also show that the AO system with the time scale of 30-60 days might consist of various spatial scale disturbances. The zonal propagation of 30-60 day oscillation in the tropical atmosphere is not all eastward. Some differences are found for different spatial scales, and for propagations in upper and lower tropospheres. The meridional propagation of the oscillation is even more different in the various regions and might be related to the low-frequency wave train in the atmosphere. The stronger activities of 30-60 day AO in the equatorial middle-western Pacific are related to the El Nino events and the weaker ones are correspondent to the inverse El Nino phenomena.     

大气水汽的输送和收支及其对副热带干旱的影响

本文利用1979年9月至1984年8月欧洲中期天气预报中心(ECMWF)每日四次的十三层分析资料,研究不同尺度的大气运动对水汽输送和收支的贡献。指出Hadley环流对水汽从副热带向赤道输送和从冬半球向夏半球的输送中起着决定性作用。热带行星波则把水汽从热带输向副热带。在中高纬的水汽向极输送中,天气尺度的波动比行星尺度的波动更重要。在南半球,天气尺度的波动支配着水汽的输送过程。分析和数值试验表明,副热带干旱受到nadley环流和热带行星波异常的强烈影响。     

REE Geochemistry in the Weathered Crust of Granites, Longnan Area,Jiangxi Province

Warm and humid climate and gentle hilly topography have provided favourable conditions for the devel-opment of the weathering crust of the granite intrusions in the Longnan area, Jiangxi Province. REE is mostlyconcentrated in an adsorption state in clay in the wholly weathered zone. The rare-earth minerals enriched inthe parent rocks provided the source material for the REE enrichment. Exchangeable REE accounts for48-86%. Extraction experiments and stable isotopic study of clay minerals suggest that the downward infiltra-tion of meteoric water and increasing gradient of pH values have played an important role in the enrichment ofREE during the progressive weathering. Slight fractionation of individual REE can not change their distribu-tion patterns in the profiles. which are inherited from the parent rocks.     

连续测定方解石和白云石中碳、氧同位素比值的方法及其意义

本文提出了利用方解石和白云石二者的不同活性,在不同的温度条件下,在同一份碳酸盐岩样品中,连续测定碳、氧同位素比值的新方法。测定结果精度高,能用于判定白云石的成因,具有实用价值。     

陕西地区岩浆岩Nd、Sr同位素特征及其与大地构造发展的联系

岩浆岩Nd、Sr同位素特征表明,扬子地块基底有着和华北地块很不相同的早期演变历史。这意味着华北和扬子两地块在历史上曾经是相互独立的,后来才拼合在一起。Nd、Sr同位素研究还表明,华北和扬子两地块的会聚在泥盆纪以前就已经在进行中,它是通过位於两地块之间的古秦岭海洋壳俯冲消亡在华北地块之下实现;华北和扬子两陆块最终相碰撞至少发生在二叠纪以前。     

天然花岗岩块的熔融实验及其岩石学意义

本文详细论述了马兰峪中生代脉状花岗间长岩固体块样品的熔融实验结果,并据此讨论了部分熔融过程中的结构与成份平衡问题。实验表明,最初熔体产生于不同矿物的接触边界上,而且石英—碱性长石之间的熔体量较石英—斜长石间熔体多,而同种矿物之间一般不出现熔体。当熔融程度增高时,两种长石间也开始出现熔体。熔体成分的研究表明,初始部分熔融过程中,局部体系的平衡起着控制作用。     

盆地演化过程中的扇三角洲

作为构造活动和古地理演变最为敏感产物的三角洲系列(泛指河流三角洲和扇三角洲)广布于不同类型的构造盆地中,盆缘坡度常是构造活动的表现。地貌,扇三角洲的堆叠及其几何学和与之共生的层序组合就成为指示构造活动的一种物理参数。裂谷演化过程中,形成扇三角洲—浊流沉积—辫状河三角洲组合的特殊充填序列。前陆盆地则发育着由深变浅的次深海(或深海)—浅海浊积扇/扇三角洲—海陆过渡—陆上磨拉石组合。走滑拉分盆地中构成特有的歪斜扇体,普遍为向上变粗和变粗又变细的层序。故可以此作为判别古构造性质的物理参数之一。