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Outcrop modeling of flow units and reductant within a sandstone uranium reservoir in the Zhiluo Formation, eastern Ordos Basin: implications for the uranium mineralization mechanism

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Abstract

The spatial distribution of flow units and reductant within a sandstone uranium reservoir is very beneficial for exploring the uranium mineralization mechanism; however, such studies have been almost neglected. As such, this paper aims to provide the sedimentological interpretation and heterogeneity models of the sandstone of the Middle Jurassic Zhiluo Formation at Shiwan outcrop area, in the eastern Ordos Basin. The outcrops are sandstone-dominated subaqueous distributary channel successions, in which five distinct architectural elements are identified and interpreted: channel units (CU), downstream accretion elements (DA), lateral accretion elements (LA), sandy bedforms (SB) and no-channelized fine-grained sediments (NFS). Within the sandstone succession, six flow units are present in the middle and lower parts of CU, or the lower parts of DA and SB elements, with their geometry to be controlled by the fourth- or third-order bounding surfaces. Moreover, the carbonaceous debris-rich zones (CDZ) are places with the highest abundance of reductant and preserve exclusively upon the basal erosional surfaces of CU and DA elements. Based on those results, a prediction model is established and shows that the formation of interlayer oxidation zone is strongly selective and confined within the CU and DA elements. The favorable site of uranium mineralization is preferentially distributed in the transition zone between the front of flow unit and the CDZ.

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Acknowledgments

This study was financially supported by the Doctoral Fund of Huanggang Normal University (No. 2042021013), the National Key Research and Development Program of China (No. 2018YFC0604202) from the Ministry and Technology of China, and the International Geosciences Program (IGCP675): Supergene Fluid Ore-forming Process of sandstone-type Uranium Deposits. The authors express their gratitude to Xiaoquan, Jiao and Liang, Yue for assistance in fieldworks. We thank Geosciences Journal editors and reviewers for their thorough and critical reviews of an early version of this manuscript and suggestions to improve the manuscript.

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Tao, Z., Wu, L., Jiao, Y. et al. Outcrop modeling of flow units and reductant within a sandstone uranium reservoir in the Zhiluo Formation, eastern Ordos Basin: implications for the uranium mineralization mechanism. Geosci J 26, 569–586 (2022). https://doi.org/10.1007/s12303-022-0008-z

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