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Estimation of crustal thickness by combination of two geophysical methods: A case study

机译:结合两种地球物理方法估算地壳厚度:一个案例研究

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In this study an extended geophysical survey using gravity and high angle refracted seismic methods with recorded earthquake has been carried out in Kerman province in southeast of Iran. The purpose of the applied geophysical surveys was to provide information on crustal structure and lithospheric thickness. The purpose of this research is focused on determination of Moho depthand for this reason several profiles for both methods were performed and by use of topography and gravity data with a reasonable combination with high angle refracted seismic data and earthquake record, the crustal and lithospheric thickness of Kerman province in the southeast of Iran was calculated.Oldenburg- Parker algorithm was the base of gravity survey of the present work but by use of Matlab programming environment and generated C Sharp computer codes was optimized, improve and then executed. For seismic data, a least-squares analysis of the travel-time data was made and the uncertainties were taking in to account. Finally, depth calculations for the velocity discontinuities and gravity anomaly contour maps were made. The comprehensive comparison between the obtained results and other studies on the selected area showed good agreement, which verified the ability of produced code.
机译:在这项研究中,已在伊朗东南部的克尔曼省开展了利用重力和大角度折射地震方法进行扩展的地球物理调查,并记录了地震。应用地球物理调查的目的是提供有关地壳结构和岩石圈厚度的信息。这项研究的目的是确定莫霍面深度,因此对这两种方法都进行了几种剖面分析,并利用地形和重力数据,并结合了大角度折射地震数据和地震记录,地壳厚度和岩石圈厚度计算了伊朗东南部的克尔曼省。奥尔登堡-帕克算法是当前工作的引力调查基础,但是通过使用Matlab编程环境和生成的C Sharp计算机代码进行了优化,改进然后执行。对于地震数据,对旅行时间数据进行了最小二乘法分析,并考虑了不确定性。最后,对速度不连续性和重力异常轮廓图进行了深度计算。所得结果与选定区域其他研究的综合比较显示出很好的一致性,这证明了所产生代码的能力。

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