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Detrital zircon geochemistry and U-Pb geochronology as an indicator of provenance of the Namakwa Sands heavy mineral deposit, west coast of South Africa

机译:碎屑锆石地球化学和U-Pb年代学可作为南非西海岸那马夸金沙重矿物矿床出处的标志

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摘要

A representative suite of detrital zircons from the Cenozoic Namakwa Sands heavy mineral placer deposit, which is hosted by mainly unconsolidated clastic sediments of the West Coast Group, has been studied from a provenance perspective. The deposit is located along the west coast of South Africa and is underlain by a metamorphosed Meso- and Neoproterozoic basement. Mineral geochemistry of individual zircon grains indicated that the entire population is continentally derived and is dominated by zircons from a felsic magmatic source, some highly evolved, with minor contributions from a metamorphic and mafic provenance.
机译:从物源的角度研究了新生代Namakwa Sands重矿物砂矿床中一套代表性的碎屑锆石,该矿床主要由西海岸群的未固结碎屑沉积物所包裹。该矿床位于南非西海岸,并由变质的中元古代和新元古代地下。单个锆石晶粒的矿物地球化学表明,整个种群都来自大陆,并且由来自长英质岩浆岩源的锆石控制,有些是高度演化的,而变质和镁铁矿物源的贡献很小。

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