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Lithospheric thickness and mechanical strength of the Indian shield

机译:印第安盾构的岩石圈厚度和机械强度

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摘要

We determined the relative mechanical strength of the Indian subcontinent by a robust coherence method based on multitaper spectral analysis on overlapping windows of equal size. Representing the elastic properties of the lithosphere by a transitional coherence wavelength, we bypass the need to input theological variables such as Young's modulus or Poisson's ratio, which have been shown to vary on other continents. We compare our measurements in terms of age and find that regions underlain by Proterozoic basement are on average stronger than regions of Archaean age. This is in stark contrast to the common assumption that mechanical strength should increase progressively with time. This suggests they are indeed mechanically distinct, and that the transitional coherence wavelength adequately captures this distinction between regions of relative strength difference. Conversions of these values to absolute effective elastic thickness show a greater overlap, which is due to the many strong assumptions required in obtaining such absolute values and argues against their usage as a robust and well-constrained property of the elastic lithosphere. (C) 2004 Elsevier B.V. All rights reserved.
机译:我们通过基于等倍重叠窗口的多锥光谱分析的稳健相干方法,确定了印度次大陆的相对机械强度。用过渡相干波长表示岩石圈的弹性,我们无需输入神学变量,例如杨氏模量或泊松比,这些变量在其他大洲已显示出变化。我们比较了年龄的测量结果,发现元古生代基底下的区域平均强度要比古生时代的区域强。这与机械强度应随时间逐渐增加的普遍假设形成鲜明对比。这表明它们确实在机械上是不同的,并且过渡相干波长足以捕获相对强度差区域之间的区别。这些值到绝对有效弹性厚度的转换显示出更大的重叠,这是由于获得这样的绝对值需要许多强有力的假设,并反对将它们用作弹性岩石圈的稳健且受良好约束的性质。 (C)2004 Elsevier B.V.保留所有权利。

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