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首页> 外文期刊>Journal of the Geological Society of India >The Role of Telluric (TE) and Magnetotelluric (MT) Methods in the Exploration of deep Sedimentary Basins
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The Role of Telluric (TE) and Magnetotelluric (MT) Methods in the Exploration of deep Sedimentary Basins

机译:碲(TE)和磁通(MT)方法在深沉积盆地探索中的作用

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After a methodical overview of the magnctotelluric and telluric methods, the paper with the help of test example from the Pannonian basin (Hungary) illustrates the effectiveness of a combined telluric and magnctotcHuric methods in the study of basement structures of deep basins. It is strongly emphasized that in the case of such adeep basin the relation between the gravity map and basin structure may be totally distorted by the crustal-mantle anomalies, first of all by the intrusion of mantle material of high density. Recognising the merits of combined telluric-magnetotelluric method in the exploration of sedimentary basins for hydrocarbon traps, the significance of the application of these methods to Indian sedimentary basins is highlighted. Usefulness of electrical conductance map, derived from these investigations, in demarcating thermally favourable zones of hydrocarbon maturation is envisaged.
机译:在铸造丸和碲化方法的方法概述之后,该论文借助于Pannonian盆地(匈牙利)的测试示例,说明了在深盆地下盆地研究中的组合碲和手球菌方法的有效性。 强烈强调,在这种ADEEP盆地的情况下,重力图和盆地结构之间的关系可以完全由地壳 - 地幔异常扭曲,首先是通过高密度的地幔材料的侵入。 认识到结合碲 - 磁仪方法的优点,在碳氢化合物陷阱沉积盆地探索中,突出了这些方法对印度沉积盆地的应用意义。 设想源自这些研究的电导图的用途,以划分碳氢化合物成熟的热良好良好的区域。

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