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Elastic properties of granulite facies rocks of Mahabalipuram, Tamil Nadu, India

机译:印度泰米尔纳德邦Mahabalipuram粒岩相岩的弹性特性

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Compressional and shear wave velocities and attenuation measurements have been carried out in some of the borehole samples of acidic, basic and intermediate granulites of Mahabalipuram, Tamil Nadu, India. The results have been obtained at ambient conditions using a€?time-of-???ighta€? pulse transmission technique at 1.0MHz frequency. The results show linear relationships between velocity and density, and velocity and attenuation properties of the rocks. The acidic granulites show lower velocities and higher attenuation than the intermediate and basic granulites. The average values of the Poissona€?s ratio of acidic, intermediate and basic granulites have been found to be 0.210, 0.241 and 0.279 respectively. The variations in velocities and attenuation in these low porosity crystalline rocks are found to be strongly in???uenced by their mineral composition. The laboratory velocity data (extrapolated to high pressure) of the present study and the published ???eld velocity data from deep seismic sounding studies indicate that these granulite facies rocks may belong to mid-crustal depths only.
机译:在印度泰米尔纳德邦Mahabalipuram的酸性,碱性和中间花岗石的一些井眼样品中进行了压缩波和剪切波速度以及衰减测量。该结果是在环境条件下使用“时间校正”获得的。 1.0MHz频率的脉冲传输技术。结果表明速度与密度之间的线性关系,以及岩石的速度与衰减特性。与中性和碱性颗粒相比,酸性颗粒显示出较低的速度和较高的衰减。酸性,中间和碱性颗粒的泊松纳比的平均值分别为0.210、0.241和0.279。人们发现,这些低孔隙度的晶体岩石的速度和衰减变化强烈地受到其矿物成分的影响。本研究的实验室速度数据(推断为高压)和已发表的来自深部地震测深的速度数据表明,这些花岗石相岩可能仅属于中地壳深度。

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