首页> 外文期刊>Journal of geophysics >Airborne Magnetic Data - A Source of Subsurface Geological Information for Uranium Exploration: A Few Case Studies over some Proterozoic Sedimentary Basins of India.
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Airborne Magnetic Data - A Source of Subsurface Geological Information for Uranium Exploration: A Few Case Studies over some Proterozoic Sedimentary Basins of India.

机译:机载磁数据-铀勘探地下地质信息的来源:印度一些元古代沉积盆地的少数案例研究。

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摘要

Airborne survey was first used in India by AMD in the year 1956 for exploration of uranium. At the initial stage it was aimed to locate near surface Uranium anomalies. Acquisition of magnetic data along with radiometric data started from the year 1972. So far, AMD has acquired valuable aeromagnetic data amounting to nearly 5.2 lakh sq km area, spread over important Uranium Provinces of India. Quality of the aeromagnetic data has improved through the ages with the application of new technologies. The most recently collected aeromagnetic data collected by heliborne survey over parts of Vindhyan basin accurately sampled subtle magnetic anomalies at the basement. Aeromagnetic survey is an effective tool for studying basement features of Middle Proterozoic sedimentary basins. Nonmagnetic (low susceptibility) sediments overlying the basements of distinctly higher susceptibility makes this possible. Study of Aeromagnetic maps over Bhima, parts of Chhattisgarh, Bijawar, Gwalior and Vindhyan basins has deciphered many important geological features viz. basement morphology, movements of basement blocks along faults and continuation of fracture/fault associated with higher value of uranium below the sediment. AMD will continue to cover more and more areas by airborne surveys in future days to meet the exploration challenges imposed on it with better quality airborne multi parameter geophysical data.
机译:1956年,AMD在印度首次将机载测量用于铀的勘探。在最初阶段,其目标是定位在近地表铀异常处。从1972年开始获取磁数据以及辐射数据。到目前为止,AMD已获取了宝贵的航空磁数据,总面积近520万平方公里,分布在印度重要的铀矿省。随着新技术的应用,航磁数据的质量随着时代的发展而提高。通过对Vindhyan盆地部分地区进行的直升机俯冲调查收集的最新航磁数据,可以准确地采样地下室的细微磁异常。航磁测量是研究中元古代沉积盆地地下特征的有效工具。非磁性(低磁化率)沉积物覆盖在基底上,磁化率明显较高,这使之成为可能。对比马(Bhima),恰蒂斯加尔邦(Chhattisgarh),比贾瓦尔(Bijawar),瓜廖尔(Gwalior)和温迪扬(Vindhyan)盆地部分地区的航空磁性地图的研究已经破译了许多重要的地质特征。地下形态,地下断层沿断层的运动以及与沉积物下方铀含量较高相关的断裂/断层的延续。在未来的日子里,AMD将继续通过机载调查覆盖越来越多的领域,以通过更高质量的机载多参数地球物理数据来应对其所面临的勘探挑战。

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