Provenance of Jurassic Sediments from Yuqia Sandstone-Type Uranium Deposits in the Northern Margin of Qaidam Basin, China and Its Implications for Uranium Mineralization

• Published in: Minerals (Basel) Vol. 12; no. 1; p. 82
• Main Authors: Huang, Guangwen, Wu, Dehai, Huang, Guangnan, Xue, Wanwen, Min, Zhuang, Fan, Pengfei
• Format: Journal Article
• Language: English
• Published: Basel MDPI AG 01.01.2022
• Subjects: Basins; Cenozoic; Chemical reduction; Coal; Continental margins; Drilling; Electron microprobe; Electron probe microanalysis; Electron probes; element geochemistry; Fault lines; Isotopes; Jurassic; Metallogenesis; Mineralization; Oxidation; Paleozoic; Petrography; Petrology; provenance analysis; Pyrite; Qaidam Basin; Sandstone; sandstone-type uranium deposit; Sediment; Sediment sources; Sedimentary rocks; Sediments; Tectonics; Trace elements; Uranium; Xenotime; Zircon; Qaidam Basin; China
• ISSN: 2075-163X; 2075-163X
• DOI: 10.3390/min12010082

The Yuqia uranium deposit is a newly discovered sandstone-type uranium deposit in the northern margin of the Qaidam Basin. Concerning the sources of sediment in the basin, most scholars have focused on the study of Cenozoic sediment sources in the northern part of the basin, rather than on the study of Jurassic provenance and its implications for uranium mineralization. In this paper, the Jurassic sandstones in the area were selected for petrography, petrogeochemistry and electron microprobe analysis (EPMA), and the significance of sedimentary provenance and uranium metallogeny were further discussed, based on the previous data of detrital zircon chronology. It is reported here for the first time that coffinite and pitchblende are the main contributors. Independent uranium minerals in the region mainly occur in strawberry pyrite, xenotime, and margins or of quartz. The rocks in the source area, Jurassic sandstones, were mainly formed under the tectonic setting of the active continental margin; however, the sediments are mainly derived from the Indosinian and Paleozoic granitoids exposed in the northern margin of the Qaidam Basin. The uranium-rich granites in the source area led to the preconcentration of uranium in the sandstone of the target layer, and the uranium was brought into the ore-bearing target layer through uranium-bearing oxygenated water. The reduction reaction occurred under the action of reducing matter, and finally, the U6+ was reduced to U4+ in the formation of coffinite and pitchblende.