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991.
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西藏驱龙矿区早侏罗世斑岩的Sr-Nd-Pb及锆石Hf同位素研究 总被引:8,自引:3,他引:5
近年的研究基本揭示,在冈底斯南缘存在一条晚三叠世-侏罗纪的花岗岩带,其成因认识有助于恢复青藏高原中生代演化历史,但却存在争议。为此,本文选择拉萨东部驱龙早侏罗世花岗斑岩开展Sr-Nd-Pb及锆石Hf同位素研究,调查岩浆源区特征,以期查明岩浆成因。分析结果显示,驱龙早侏罗世斑岩具有相对较低的87Sr/86Sr初始比值(0.7029~0.7050)、正的εNd(t)(平均0.7)和锆石εHf(t)值(2.6~8.2),表明岩浆来自新生地壳物质的部分熔融。综合对比发现,冈底斯南部晚三叠世-早侏罗世花岗岩的锆石Hf同位素在500km宽的范围内显示出由西向东亏损程度逐渐减弱、甚至变得富集的规律,表明在此类花岗岩的形成过程中,成熟地壳组分的贡献自西向东逐渐增多。这既可因南部拉萨地体基底Hf同位素组成的东西向不均一所引起,也可能因东段驱龙、米林等地花岗岩更靠近古老的拉萨微陆块所致。 相似文献
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Garth A. Barber 《Astrophysics and Space Science》2006,305(2):169-176
The new theory of Self Creation Cosmology has been shown to yield a concordant cosmological solution that does not require inflation, exotic non-baryonic Dark matter or unknown Dark Energy to fit observational constraints. In vacuo there is a conformal equivalence between this theory and canonical General Relativity and as a consequence an experimental degeneracy exists as the two theories predict identical results in the standard tests. However, there are three definitive experiments that are able to resolve this degeneracy and distinguish between the two theories. Here these standard tests and definitive experiments are described. One of the definitive predictions, that of the geodetic precession of a gyroscope, has just been measured on the Gravity Probe B satellite, which is at the present time of writing in the data processing stage. This is the first opportunity to falsify Self Creation Cosmology. The theory predicts a ‘frame-dragging’ result equal to GR but a geodetic precession of only 2/3 the GR value. When applied to the Gravity Probe B satellite, Self Creation Cosmology predicts an E–W gravitomagnetic/frame-dragging precession, equal to that of GR, of 40.9 milliarcsec/yr but a N–S gyroscope (geodetic + Thomas) precession of just 4.4096 arcsec/yr. 相似文献
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空间权重矩阵的生成方法分析与实验 总被引:23,自引:0,他引:23
区域空间动力学过程 (例如疾病传播、区域社会经济可持续发展等 )所涉及的数据样本和状态变量都是以区域多边形形式存在的。区域群发展在空间上的此起彼伏和相互影响则是通过区域之间相互联系得以实现的 ,空间权重矩阵用以传载这一作用过程。因此 ,构建区域空间连接权重矩阵是建立区域空间动力学方程的核心问题之一。本文分析了空间权重矩阵的不同生成方法 ,并对空间权重矩阵的一种形式. 相似文献
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In this study, measurements of gravity were made to map and model the thickness of Quaternary deposits (sand and clay) overlying Ordovician limestones in a suburb of Ottawa (Orléans, Ontario). Because ground motion amplification is partly related to the thickness of unconsolidated deposits, this work helps refine the assessment of the earthquake damage potential of the area. It also helps the mapping of clay basins, which can locally exceed 100 m in thickness, where ground motion amplification can occur. Previous work, including well log data and seismic methods, have yielded a wealth of information on near-surface geology in Orléans, thereby providing the necessary constraints to test the applicability of gravity modeling in other locations where other methods cannot always be used. Some 104 gravity stations were occupied in an 8 × 12 km test area in the Orléans. Stations were accurately located with differential GPS that provided centimetric accuracy in elevation. Densities of the unconsolidated Quaternary deposits (Champlain Sea clay) determined on core samples and densities determined on limestone samples from outcrops were used to constrain models of the clay layer overlying the higher density bedrock formations (limestone). The gravity anomaly map delineates areas where clay basins attain > 100 m depth. Assuming a realistic density for the Champlain Sea clays (1.9-2.1 g/cm3), the thickness over the higher density bedrock formations (Ordovician carbonate rocks) was modeled and compared with well logs and two seismic reflection profiles. The models match quite well with the information determined from well logs and seismic methods. It was found that gravity and the thickness of unconsolidated deposits are correlated but the uncertainties in both data sets preclude the definition of a direct correlation between the two. We propose that gravity measurements at a local scale be used as an inexpensive means of mapping the thickness of unconsolidated deposits in low-density urban areas. To obtain meaningful results, three conditions must exist. Firstly, elevations of gravity stations must be measured accurately using differential GPS; secondly, that the regional gravity field must be well defined, and thirdly, that the local geology be simple enough to be realistically represented with a two-layer model. 相似文献
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