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931.
Juan Getino José M. Farto José M. Ferrándiz 《Celestial Mechanics and Dynamical Astronomy》1998,71(2):95-108
In this paper, the mathematical algorithm elaborated by González, Getino and Farto (1998) is applied to four different nonrigid Earth models, in order to obtain the analytical expressions of the corresponding free frequencies. The solutions are studied, and the contributions of the different considered effects are evaluated. A numerical integration is also carried out, showing the validity of the obtained analytical solutions. 相似文献
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934.
本文报告6例经CT诊断的主动脉夹层。CT能显示两个不同增强密度的主动脉腔,被内瓣分离,称”双腔征“。本文还讨论了其发病机制及CT对本病早期,准确,迅速诊断的重要意义。 相似文献
935.
利用正交试验法研究了高功率CO2激光工艺参数对钻杆接头表面硬化效果的影响,利用显微硬度计测定了硬化层硬度的分布规律及组织特征,采用计算机回归处理分析得出了P、D、V、E对硬化层面积大小因子h·b影响的表达式。研究结果为高功率CO2激光强化钻杆接头提供了一定的依据 相似文献
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938.
泥炭样品不同有机组分的~(14)C测年的初步研究 总被引:3,自引:0,他引:3
分别用NaClO、NaOH溶液、Na4P2O7和NaOH混合溶液和有机溶剂对采自延庆盆地大王庄两个泥炭样品进行前处理,每个样品获得10个不同有机组分,对这些有机组分的14C年龄测定值进行对比。以探讨泥炭等样品不同有机组分14C测年的可靠性 相似文献
939.
The available petrochemical data indicate that volcanic rocks in the Sanshui basin of Guangdong Prov-ince are characteristic of the island-arc tholeiite-calc-alkaline series.Their K-Ar ages range from 43 to 64 Ma,corresponding to Early Tertiary.The Nd-Sr-Pb isotopic correlations give two binary mixing trends,indicating a mixed source of Leiqiong depleted mantle,seawater and altered sediments pertaining to subduction.Our studies have confirmed the existence of an ancient subduction zone beneath the South Chi-na continent,which is considered to have resulted from the suturing of various terrains in southern China. 相似文献
940.
Recent and new faunal data from the Cambrian to Silurian rocks of the Precordillera, Famatina and Northwest Argentina basins are used to discriminate between different paleogeographic models, and especially to establish to what extent they are compatible with a previous conclusion that the Precordillera is a Laurentian-derived microcontinent. There is no paleontological evidence to support a para-autochthonous Gondwanan origin of the Precordillera. The strong differences in the Cambrian trilobite faunas and lithologic successions preclude a common origin of the Precordillera terrane, eastern Antarctica and South Africa. Recent discoveries of brachiopods and organisms of the Phylum Agmata strengthened Laurentian affinities during the Cambrian. The latest Cambrian-early Ordovician faunas that inhabited the autochthonous Northwest Argentina basin, including the western Puna volcaniclastic successions, are mostly peri-Gondwanan. The early Ordovician brachiopods, ostracods and trilobites display mixed Laurentian, Baltic and Avalonian biogeographical links supporting a drifting of the Precordillera across the Iapetus Ocean. Increasing Gondwanan elements during the Llanvirn, along with varied geological evidence, indicate that the first stages of collision may have begun at that time, involving a major change in the plate kinematics. The distribution of facies and faunas, basin development, and timing of deformation are interpreted as resulting from a north to south diachronous closing of the remnant basin during the last phases of convergence and oblique collision of the Precordillera terrane with the Gondwana margin. The high level of endemism of Caradoc faunas may be a consequence of the rearrangement and partial isolation of sedimentary areas during the strike-slip movement of the colliding Precordillera plate with respect to the Gondwana margin. Suggested relationships between facies distribution, geographic barriers and faunal migrations before and during the collision are depicted in a series of schematic reconstructions at five time slices from late Cambrian to Silurian. 相似文献