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Regional aeromagnetic and stratigraphic correlations of the Kalahari Copperbelt in Namibia and Botswana

机译:纳米比亚和博茨瓦纳的卡拉哈里铜矿带的区域航磁和地层相关性

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摘要

The late Mesoproterozoic to Neoproterozoic Kalahari Copperbelt (KCB) in Namibia and Botswana is widely covered by Kalahari sand, which precludes direct correlations between known stratabound sediment-hosted Cu-Ag districts. We use a combination of review of literature data, and newly processed and interpreted high-resolution aeromagnetic maps in both countries to provide a new correlative cross-border interpretation. Lithostratigraphic control on the aeromagnetic response allows detailed indirect mapping of the Kalahari Copperbelt lithotectonic domains below the sand cover. This enabled us to redefine the width and lateral extent of the KCB as two continuous magnetic domains (the Rehoboth and Ghanzi-Chobe domains) extending from central Namibia to northern Botswana, and helped in resolving problems of stratigraphic correlations across the international border.
机译:纳米比亚和博茨瓦纳的中元古代到新元古代的卡拉哈里铜矿带(KCB)被卡拉哈里砂广泛地覆盖,这排除了已知的以地层为界的沉积物所主导的铜银地区之间的直接联系。我们结合了文献数据的审查,两国新近处理和解释的高分辨率航空电磁图的组合,以提供新的相关跨境解释。对航空磁响应的岩石地层学控制可以对砂覆层下方的卡拉哈里铜带岩性构造域进行详细的间接映射。这使我们能够将KCB的宽度和横向范围重新定义为从纳米比亚中部延伸到博茨瓦纳北部的两个连续的磁畴(瑞霍博斯磁畴和甘兹-乔贝磁畴),并有助于解决跨国际边界的地层相关性问题。

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