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首页> 外文期刊>Tectonophysics: International Journal of Geotectonics and the Geology and Physics of the Interior of the Earth >Depth to the bottom of magnetic sources (DBMS) from aeromagnetic data of Central India using modified centroid method for fractal distribution of sources
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Depth to the bottom of magnetic sources (DBMS) from aeromagnetic data of Central India using modified centroid method for fractal distribution of sources

机译:使用改进的质心方法从印度中部的航空磁数据深入到磁源(DBMS)的底部以进行源的分形分布

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The depth to the bottom of the magnetic sources (DBMS) has been estimated from the aeromagnetic data of Central India. The conventional centroid method of DBMS estimation assumes random uniform uncorrelated distribution of sources and to overcome this limitation a modified centroid method based on scaling distribution has been proposed. Shallower values of the DBMS are found for the south western region. The DBMS values are found as low as 22. km in the south west Deccan trap covered regions and as deep as 43. km in the Chhattisgarh Basin. In most of the places DBMS are much shallower than the Moho depth, earlier found from the seismic study and may be representing the thermal/compositional/petrological boundaries. The large variation in the DBMS indicates the complex nature of the Indian crust.
机译:磁源(DBMS)底部的深度是根据印度中部的航空数据估算得出的。 DBMS估计的常规质心方法假定源的随机均匀不相关分布,并且为了克服这一限制,提出了一种基于比例分布的改进质心方法。在西南地区发现DBMS的值较浅。在西南的Deccan圈闭覆盖地区,DBMS值低至22. km,而恰蒂斯加尔邦盆地的深至43. km。在大多数地方,DBMS比Moho深度浅得多,这是从地震研究中较早发现的,并且可能代表了热/成分/岩石学的边界。 DBMS的巨大变化表明印度地壳的复杂性。

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