Uranium Redox and Deposition Transitions Embedded in Deep‐Time Geochemical Models and Mineral Chemistry Networks
Uranium (U) is an important global energy resource and a redox sensitive trace element that reflects changing environmental conditions and geochemical cycling. The redox evolution of U mineral chemistry can be interrogated to understand the formation and distribution of U deposits and the redox proc...
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Published in | Geochemistry, geophysics, geosystems : G3 Vol. 25; no. 2 |
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Main Authors | , , , , , , |
Format | Journal Article |
Language | English |
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Washington
John Wiley & Sons, Inc
01.02.2024
Wiley |
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Abstract | Uranium (U) is an important global energy resource and a redox sensitive trace element that reflects changing environmental conditions and geochemical cycling. The redox evolution of U mineral chemistry can be interrogated to understand the formation and distribution of U deposits and the redox processes involved in U geochemistry throughout Earth history. In this study, geochemical modeling using thermodynamic data, and mineral chemistry network analysis are used to investigate U geochemistry and deposition through time. The number of U6+ mineral localities surpasses the number of U4+ mineral localities in the Paleoproterozoic. Moreover, the number of sedimentary U6+ mineral localities increases earlier in the Phanerozoic than the number of U4+ sedimentary mineral localities, likely due to the necessity of sufficient sedimentary organic matter to reduce U6+–U4+. Indeed, modeling calculations indicate that increased oxidative weathering due to surface oxygenation limited U4+ uraninite (UO2) formation from weathered granite and basalt. Louvain network community detection shows that U6+ forms minerals with many more shared elements and redox states than U4+. The range of weighted Mineral Element Electronegativity Coefficient of Variation (wMEECV) values of U6+ minerals increases through time, particularly during the Phanerozoic. Conversely, the range of wMEECV values of U4+ minerals is consistent through time due to the relative abundance of uraninite, coffinite, and brannerite. The late oxidation and formation of U6+ minerals compared to S6+ minerals illustrates the importance of the development of land plants, organic matter deposition, and redox‐controlled U deposition from ground water in continental sediments during this time‐period.
Plain Language Summary
Uranium (U) is the most widely used fuel in nuclear fission power plants, and nuclear power results in lower greenhouse gas emissions than fossil fuel energy. The different types of U deposits and minerals have evolved throughout the Earth history with changing environmental conditions and formation processes. In this study, we use modeling calculations and network analysis to understand how the transforming Earth system impacted the global U cycle, evolving U mineral chemistry, and deposit formation through time. Modeling calculations show that the abundant U mineral uraninite (UO2) formed in much greater quantities in the anoxic conditions of the Archean eon than present day oxic conditions. We also find that U minerals are increasingly oxidized through time, in agreement with modeling calculations, resulting in new minerals with diversifying chemical element associations and expanding distribution of U in the environment. The earlier increase in the number of oxidized U minerals in sedimentary localities than unoxidized U minerals in sedimentary localities 350–250 million years ago reflects the importance of land plants and organic matter in the formation of unoxidized U minerals in sedimentary settings.
Key Points
Model calculations indicate Earth surface oxidation limited U4+ uraninite formation, in agreement with increased observed U6+ minerals
U oxidation increases the diversity of mineral chemical element associations and distribution in the environment
The later formation of U6+ minerals compared to S6+ minerals represents differential Earth surface oxidation |
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AbstractList | Uranium (U) is an important global energy resource and a redox sensitive trace element that reflects changing environmental conditions and geochemical cycling. The redox evolution of U mineral chemistry can be interrogated to understand the formation and distribution of U deposits and the redox processes involved in U geochemistry throughout Earth history. In this study, geochemical modeling using thermodynamic data, and mineral chemistry network analysis are used to investigate U geochemistry and deposition through time. The number of U6+ mineral localities surpasses the number of U4+ mineral localities in the Paleoproterozoic. Moreover, the number of sedimentary U6+ mineral localities increases earlier in the Phanerozoic than the number of U4+ sedimentary mineral localities, likely due to the necessity of sufficient sedimentary organic matter to reduce U6+–U4+. Indeed, modeling calculations indicate that increased oxidative weathering due to surface oxygenation limited U4+ uraninite (UO2) formation from weathered granite and basalt. Louvain network community detection shows that U6+ forms minerals with many more shared elements and redox states than U4+. The range of weighted Mineral Element Electronegativity Coefficient of Variation (wMEECV) values of U6+ minerals increases through time, particularly during the Phanerozoic. Conversely, the range of wMEECV values of U4+ minerals is consistent through time due to the relative abundance of uraninite, coffinite, and brannerite. The late oxidation and formation of U6+ minerals compared to S6+ minerals illustrates the importance of the development of land plants, organic matter deposition, and redox‐controlled U deposition from ground water in continental sediments during this time‐period.
Plain Language Summary
Uranium (U) is the most widely used fuel in nuclear fission power plants, and nuclear power results in lower greenhouse gas emissions than fossil fuel energy. The different types of U deposits and minerals have evolved throughout the Earth history with changing environmental conditions and formation processes. In this study, we use modeling calculations and network analysis to understand how the transforming Earth system impacted the global U cycle, evolving U mineral chemistry, and deposit formation through time. Modeling calculations show that the abundant U mineral uraninite (UO2) formed in much greater quantities in the anoxic conditions of the Archean eon than present day oxic conditions. We also find that U minerals are increasingly oxidized through time, in agreement with modeling calculations, resulting in new minerals with diversifying chemical element associations and expanding distribution of U in the environment. The earlier increase in the number of oxidized U minerals in sedimentary localities than unoxidized U minerals in sedimentary localities 350–250 million years ago reflects the importance of land plants and organic matter in the formation of unoxidized U minerals in sedimentary settings.
Key Points
Model calculations indicate Earth surface oxidation limited U4+ uraninite formation, in agreement with increased observed U6+ minerals
U oxidation increases the diversity of mineral chemical element associations and distribution in the environment
The later formation of U6+ minerals compared to S6+ minerals represents differential Earth surface oxidation Abstract Uranium (U) is an important global energy resource and a redox sensitive trace element that reflects changing environmental conditions and geochemical cycling. The redox evolution of U mineral chemistry can be interrogated to understand the formation and distribution of U deposits and the redox processes involved in U geochemistry throughout Earth history. In this study, geochemical modeling using thermodynamic data, and mineral chemistry network analysis are used to investigate U geochemistry and deposition through time. The number of U6+ mineral localities surpasses the number of U4+ mineral localities in the Paleoproterozoic. Moreover, the number of sedimentary U6+ mineral localities increases earlier in the Phanerozoic than the number of U4+ sedimentary mineral localities, likely due to the necessity of sufficient sedimentary organic matter to reduce U6+–U4+. Indeed, modeling calculations indicate that increased oxidative weathering due to surface oxygenation limited U4+ uraninite (UO2) formation from weathered granite and basalt. Louvain network community detection shows that U6+ forms minerals with many more shared elements and redox states than U4+. The range of weighted Mineral Element Electronegativity Coefficient of Variation (wMEECV) values of U6+ minerals increases through time, particularly during the Phanerozoic. Conversely, the range of wMEECV values of U4+ minerals is consistent through time due to the relative abundance of uraninite, coffinite, and brannerite. The late oxidation and formation of U6+ minerals compared to S6+ minerals illustrates the importance of the development of land plants, organic matter deposition, and redox‐controlled U deposition from ground water in continental sediments during this time‐period. Uranium (U) is an important global energy resource and a redox sensitive trace element that reflects changing environmental conditions and geochemical cycling. The redox evolution of U mineral chemistry can be interrogated to understand the formation and distribution of U deposits and the redox processes involved in U geochemistry throughout Earth history. In this study, geochemical modeling using thermodynamic data, and mineral chemistry network analysis are used to investigate U geochemistry and deposition through time. The number of U6+ mineral localities surpasses the number of U4+ mineral localities in the Paleoproterozoic. Moreover, the number of sedimentary U6+ mineral localities increases earlier in the Phanerozoic than the number of U4+ sedimentary mineral localities, likely due to the necessity of sufficient sedimentary organic matter to reduce U6+–U4+. Indeed, modeling calculations indicate that increased oxidative weathering due to surface oxygenation limited U4+ uraninite (UO2) formation from weathered granite and basalt. Louvain network community detection shows that U6+ forms minerals with many more shared elements and redox states than U4+. The range of weighted Mineral Element Electronegativity Coefficient of Variation (wMEECV) values of U6+ minerals increases through time, particularly during the Phanerozoic. Conversely, the range of wMEECV values of U4+ minerals is consistent through time due to the relative abundance of uraninite, coffinite, and brannerite. The late oxidation and formation of U6+ minerals compared to S6+ minerals illustrates the importance of the development of land plants, organic matter deposition, and redox‐controlled U deposition from ground water in continental sediments during this time‐period. Abstract Uranium (U) is an important global energy resource and a redox sensitive trace element that reflects changing environmental conditions and geochemical cycling. The redox evolution of U mineral chemistry can be interrogated to understand the formation and distribution of U deposits and the redox processes involved in U geochemistry throughout Earth history. In this study, geochemical modeling using thermodynamic data, and mineral chemistry network analysis are used to investigate U geochemistry and deposition through time. The number of U 6+ mineral localities surpasses the number of U 4+ mineral localities in the Paleoproterozoic. Moreover, the number of sedimentary U 6+ mineral localities increases earlier in the Phanerozoic than the number of U 4+ sedimentary mineral localities, likely due to the necessity of sufficient sedimentary organic matter to reduce U 6+ –U 4+ . Indeed, modeling calculations indicate that increased oxidative weathering due to surface oxygenation limited U 4+ uraninite (UO 2 ) formation from weathered granite and basalt. Louvain network community detection shows that U 6+ forms minerals with many more shared elements and redox states than U 4+ . The range of weighted Mineral Element Electronegativity Coefficient of Variation (wMEE CV ) values of U 6+ minerals increases through time, particularly during the Phanerozoic. Conversely, the range of wMEE CV values of U 4+ minerals is consistent through time due to the relative abundance of uraninite, coffinite, and brannerite. The late oxidation and formation of U 6+ minerals compared to S 6+ minerals illustrates the importance of the development of land plants, organic matter deposition, and redox‐controlled U deposition from ground water in continental sediments during this time‐period. Plain Language Summary Uranium (U) is the most widely used fuel in nuclear fission power plants, and nuclear power results in lower greenhouse gas emissions than fossil fuel energy. The different types of U deposits and minerals have evolved throughout the Earth history with changing environmental conditions and formation processes. In this study, we use modeling calculations and network analysis to understand how the transforming Earth system impacted the global U cycle, evolving U mineral chemistry, and deposit formation through time. Modeling calculations show that the abundant U mineral uraninite (UO 2 ) formed in much greater quantities in the anoxic conditions of the Archean eon than present day oxic conditions. We also find that U minerals are increasingly oxidized through time, in agreement with modeling calculations, resulting in new minerals with diversifying chemical element associations and expanding distribution of U in the environment. The earlier increase in the number of oxidized U minerals in sedimentary localities than unoxidized U minerals in sedimentary localities 350–250 million years ago reflects the importance of land plants and organic matter in the formation of unoxidized U minerals in sedimentary settings. Key Points Model calculations indicate Earth surface oxidation limited U 4+ uraninite formation, in agreement with increased observed U 6+ minerals U oxidation increases the diversity of mineral chemical element associations and distribution in the environment The later formation of U 6+ minerals compared to S 6+ minerals represents differential Earth surface oxidation |
Author | Hummer, D. R. Zhang, A. Moore, E. K. Li, J. Hao, J. Yee, N. Morrison, S. M. |
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Cites_doi | 10.1021/es051804n 10.5382/AV75.04 10.1038/s41598‐022‐08650‐x 10.1130/0091‐7613(1999)027<0115:RSOTAA>2.3.CO;2 10.3390/min13081089 10.1021/es049963e 10.5382/AV75.02 10.2113/gselements.6.1.31 10.1016/j.oregeorev.2015.05.020 10.1016/j.precamres.2007.04.021 10.1146/annurev‐earth‐081619‐052705 10.1126/science.202.4366.430 10.1016/j.precamres.2022.106960 10.3389/feart.2020.00208 10.2138/am.2009.3208 10.1016/j.gr.2017.04.011 10.1016/j.chemgeo.2009.10.004 10.1016/j.oregeorev.2018.09.013 10.1016/j.gr.2008.09.005 10.1063/1.4869401 10.1016/0012‐821X(94)00071‐9 10.1016/S0040‐1951(03)00343‐3 10.1002/spe.4380211102 10.1016/S0016‐7037(97)00240‐8 10.1098/rsta.1979.0027 10.1073/pnas.1804655115 10.2172/138894 10.3389/feart.2020.585087 10.1016/j.epsl.2015.08.007 10.1007/BF01117679 10.2475/07.2009.03 10.1016/0016‐7037(89)90065‐3 10.1063/5.0042695 10.1107/S0365110X6300030X 10.1007/978-1-4614-7591-0 10.1038/nature11445 10.1021/cm062349c 10.1016/0012‐821X(90)90101‐3 10.1016/j.eng.2019.03.006 10.1029/2020GB006649 10.1016/S1342‐937X(05)70883‐2 10.1126/science.288.5469.1177 10.7312/mcme93416 10.1007/s00126‐008‐0223‐1 10.2113/gsecongeo.82.5.1169 10.1038/s41467‐022‐28589‐x 10.2113/gsecongeo.85.3.511 10.1007/s00126‐007‐0153‐3 10.1016/0169‐1368(95)00011‐9 10.1021/cm020258j 10.1088/1742‐5468/2008/10/P10008 10.1130/B30949.1 10.1038/s41467‐017‐02095‐x 10.1016/j.chemgeo.2019.05.022 10.1038/37918 10.1149/1.2131790 10.1029/95RG00262 10.1021/ic202161y 10.2113/gsecongeo.105.3.553 10.1029/2000JB900356 10.1016/B978-0-444-41407-6.50006-4 10.1016/0016‐7037(96)00039‐7 10.2113/gsecongeo.78.5.799 10.1016/0009‐2541(90)90080‐Q 10.1016/0301‐9268(80)90056‐X 10.1126/sciadv.aax1420 10.1016/j.chemgeo.2013.08.010 10.1016/j.precamres.2019.105583 10.2113/gsecongeo.78.1.105 10.1016/j.gca.2005.11.032 10.1016/j.earscirev.2004.10.003 10.1016/0016‐7037(91)90024‐Y 10.1016/j.chemgeo.2013.09.005 10.1111/j.1365‐3121.2011.01008.x 10.1016/j.precamres.2006.11.017 10.1007/978-94-009-6060-2_6 10.1007/978-3-662-02892-6 10.1016/0098‐3004(92)90029‐q 10.1016/j.epsl.2016.10.021 10.1016/j.oregeorev.2019.03.037 10.1016/0016‐7037(94)90117‐1 10.2475/ajs.304.5.397 10.1515/9781501509193 10.1146/annurev.micro.59.030804.121357 10.2113/0530145 10.1016/j.gca.2007.11.012 10.2113/gsecongeo.53.5.598 10.1063/1.1707867 10.3390/min10100876 10.1016/B978-0-08-095975-7.00715-4 10.1130/G30852.1 10.1016/j.oregeorev.2004.10.001 10.1016/S0009‐2541(97)00169‐1 10.2113/gsecongeo.73.8.1409 10.1016/0040‐1951(91)90416‐P 10.1016/j.gca.2011.06.041 10.1039/C1CP20996E 10.1016/j.jnucmat.2005.02.004 10.1016/j.precamres.2020.105980 10.1144/GSL.MEM.1990.012.01.01 10.1016/j.gca.2018.07.024 10.1016/j.epsl.2014.05.051 10.1007/s11837‐000‐0181‐2 10.1016/0169‐1368(95)00014‐3 10.1038/282247a0 10.1146/annurev.ns.08.120158.001353 10.1098/rsta.2017.0405 10.1016/0016‐7037(78)90001‐7 10.1016/0016‐7037(91)90157‐z 10.1086/658295 10.1016/0003‐2670(59)80094‐5 10.1016/0012‐821X(91)90029‐H 10.1038/nature06811 10.1016/0341‐8162(96)00003‐3 10.1016/0169‐1368(95)00013‐5 |
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References | 2002; 14 1959; 20 2011; 119 2010; 105 1986; 78 1978; 73 1995; 33 1958; 53 1972 2013; 362 2020; 10 2012; 489 2003; 53 1991; 187 1997; 389 1991; 102 2005; 341 1990 2004; 38 2009; 94 1996; 60 1985 2020; 338 1984 2005; 70 1981 2021; 154 1979; 282 2014; 400 2014; 126 2009; 15 2010; 6 2007; 19 2010; 38 2019; 5 1973; 34 2002; 5 2018; 102 1999; 27 2011; 75 2019; 109 2020; 34 1993 1992 2004; 304 1976; 7 2007; 15 1999 1996; 11 1983; 78 2017; 50 1989; 53 2006; 40 2018; 238 1978; 42 1997; 35 2018; 115 2007; 153 2022; 12 2022; 13 1998; 147 1978; 202 2006; 70 2009; 44 1990; 97 2017; 8 1990; 12 1991; 55 2010; 269 2023; 386 1992; 18 2019; 521 2016; 72 2011; 13 2005; 26 2008; 72 2008; 2008 2001; 106 2012; 51 2020; 8 1990; 85 2006; 60 2020; 6 1987; 82 2018; 376 2000; 52 1958; 8 2020; 48 2011; 23 2000; 288 2021; 352 2014; 9 1996; 27 2023; 13 1997; 61 2000; 28 1966; 37 2013; 43 1995; 10 2004 1999; 8 1989; 27 2003; 375 2017; 457 2014; 115 1979; 291 1990; 82 2008; 160 1994; 124 1963; 16 2009; 309 1991; 21 2020 1980; 13 2015; 430 2019 1994; 58 1958; 61 1978; 125 2013 2008; 452 e_1_2_9_98_1 Swift E. H. (e_1_2_9_118_1) 1972 e_1_2_9_52_1 e_1_2_9_79_1 e_1_2_9_94_1 e_1_2_9_10_1 e_1_2_9_56_1 e_1_2_9_33_1 e_1_2_9_90_1 McMenamin M. A. S. (e_1_2_9_71_1) 1990 e_1_2_9_103_1 e_1_2_9_126_1 e_1_2_9_107_1 e_1_2_9_122_1 e_1_2_9_14_1 e_1_2_9_37_1 Bard A. J. (e_1_2_9_7_1) 1985 e_1_2_9_18_1 Gauthier‐Lafaye F. (e_1_2_9_35_1) 1986; 78 e_1_2_9_41_1 e_1_2_9_64_1 e_1_2_9_87_1 e_1_2_9_45_1 e_1_2_9_68_1 e_1_2_9_83_1 e_1_2_9_6_1 e_1_2_9_119_1 e_1_2_9_60_1 e_1_2_9_2_1 e_1_2_9_111_1 e_1_2_9_115_1 e_1_2_9_26_1 e_1_2_9_49_1 e_1_2_9_130_1 Champion D. C. (e_1_2_9_22_1) 2007 e_1_2_9_30_1 e_1_2_9_53_1 e_1_2_9_99_1 e_1_2_9_72_1 e_1_2_9_11_1 e_1_2_9_34_1 e_1_2_9_57_1 e_1_2_9_76_1 e_1_2_9_91_1 e_1_2_9_102_1 e_1_2_9_129_1 e_1_2_9_106_1 e_1_2_9_125_1 e_1_2_9_15_1 e_1_2_9_121_1 e_1_2_9_19_1 e_1_2_9_88_1 e_1_2_9_61_1 e_1_2_9_46_1 e_1_2_9_84_1 e_1_2_9_23_1 e_1_2_9_65_1 e_1_2_9_80_1 e_1_2_9_5_1 e_1_2_9_114_1 e_1_2_9_133_1 e_1_2_9_9_1 Kyser K. (e_1_2_9_59_1) 2000; 28 e_1_2_9_27_1 e_1_2_9_69_1 Ramdohr P. (e_1_2_9_95_1) 1958; 61 e_1_2_9_110_1 e_1_2_9_31_1 e_1_2_9_50_1 e_1_2_9_73_1 e_1_2_9_77_1 e_1_2_9_96_1 e_1_2_9_12_1 e_1_2_9_54_1 e_1_2_9_109_1 e_1_2_9_101_1 e_1_2_9_128_1 e_1_2_9_105_1 e_1_2_9_124_1 e_1_2_9_120_1 e_1_2_9_16_1 e_1_2_9_20_1 e_1_2_9_62_1 e_1_2_9_89_1 e_1_2_9_24_1 e_1_2_9_43_1 e_1_2_9_66_1 e_1_2_9_85_1 e_1_2_9_8_1 Mikhailov V. A. (e_1_2_9_75_1) 1999 e_1_2_9_81_1 e_1_2_9_4_1 e_1_2_9_113_1 e_1_2_9_117_1 e_1_2_9_28_1 e_1_2_9_47_1 e_1_2_9_132_1 e_1_2_9_74_1 e_1_2_9_51_1 Harshman E. N. (e_1_2_9_42_1) 1972 e_1_2_9_78_1 e_1_2_9_13_1 e_1_2_9_55_1 e_1_2_9_97_1 e_1_2_9_93_1 e_1_2_9_108_1 e_1_2_9_70_1 Fayek M. (e_1_2_9_32_1) 1997; 35 e_1_2_9_127_1 e_1_2_9_100_1 Smits G. (e_1_2_9_112_1) 1989; 27 e_1_2_9_123_1 e_1_2_9_104_1 e_1_2_9_17_1 e_1_2_9_36_1 Grenthe I. (e_1_2_9_39_1) 2004 e_1_2_9_63_1 e_1_2_9_40_1 Grenthe I. (e_1_2_9_38_1) 1992 e_1_2_9_21_1 e_1_2_9_67_1 e_1_2_9_44_1 e_1_2_9_86_1 Phadke A. V. (e_1_2_9_92_1) 1985 e_1_2_9_82_1 e_1_2_9_3_1 e_1_2_9_116_1 e_1_2_9_25_1 e_1_2_9_131_1 e_1_2_9_48_1 Krivovichev S. (e_1_2_9_58_1) 2013; 43 e_1_2_9_29_1 |
References_xml | – volume: 187 start-page: 117 issue: 1 year: 1991 end-page: 134 article-title: Anatomy of North America: Thematic geologic portrayals of the continent publication-title: Tectonophysics – volume: 8 year: 2020 – year: 1981 – volume: 73 start-page: 1409 issue: 8 year: 1978 end-page: 1419 article-title: The time‐bound character of uranium deposits publication-title: Economic Geology – volume: 38 start-page: 2822 issue: 10 year: 2004 end-page: 2828 article-title: Spectroscopic and diffraction study of uranium speciation in contaminated vadose zone sediments from the Hanford Site, Washington State publication-title: Environmental Science & Technology – volume: 27 start-page: 105 issue: 2 year: 1996 end-page: 121 article-title: Evidence of anoxic to oxic atmospheric change during 2.45‐2.22 Ga from lower and upper sub‐Huronian paleosols, Canada publication-title: Catena – volume: 19 start-page: 567 issue: 3 year: 2007 end-page: 574 article-title: Syntheses, structure, magnetism, and optical properties of the ordered mixed‐lanthanide sulfides γ‐LnLn‘S3 (Ln = La, Ce; Ln’ = Er, Tm, Yb) publication-title: Chemistry of Materials – volume: 202 start-page: 430 issue: 4366 year: 1978 end-page: 432 article-title: Carbon‐13/Carbon‐12 isotope fractionation of organic matter associated with uranium ores induced by alpha irradiation publication-title: Science – volume: 8 start-page: 257 issue: 1 year: 1958 end-page: 298 article-title: Geochronology by radioactive decay publication-title: Annual Review of Nuclear Science – volume: 5 start-page: 397 issue: 3 year: 2019 end-page: 405 article-title: Data‐driven discovery in mineralogy: Recent advances in data resources, analysis, and visualization publication-title: Engineering – start-page: 43 year: 1984 end-page: 88 – volume: 376 issue: 2132 year: 2018 article-title: Geological archive of the onset of plate tectonics publication-title: Philosophical Transactions of the Royal Society A: Mathematical, Physical & Engineering Sciences – volume: 13 issue: 8 year: 2023 article-title: The evolution of mineral hardness reveals both changing parageneses and preservational bias in the mineralogical record publication-title: Minerals – volume: 119 start-page: 109 issue: 2 year: 2011 end-page: 126 article-title: Quantifying the timing and rate of crustal evolution: Global compilation of radiometrically dated detrital zircon grains publication-title: The Journal of Geology – volume: 48 start-page: 291 issue: 1 year: 2020 end-page: 320 article-title: Plate tectonics and the Archean Earth publication-title: Annual Review of Earth and Planetary Sciences – volume: 26 start-page: 51 issue: 1 year: 2005 end-page: 69 article-title: Mineral paragenesis and textures associated with sandstone‐hosted roll‐front uranium deposits, NW China publication-title: Ore Geology Reviews – volume: 457 start-page: 191 year: 2017 end-page: 203 article-title: A model for late Archean chemical weathering and world average river water publication-title: Earth and Planetary Science Letters – volume: 10 issue: 10 year: 2020 article-title: Photoluminescence imaging of whole zircon grains on a petrographic microscope—An underused aide for geochronologic studies publication-title: Minerals – volume: 75 start-page: 5269 issue: 18 year: 2011 end-page: 5282 article-title: Thermodynamic characterization of boltwoodite and uranophane: Enthalpy of formation and aqueous solubility publication-title: Geochimica et Cosmochimica Acta – volume: 70 start-page: 1 issue: 1 year: 2005 end-page: 46 article-title: Archaean atmospheric evolution: Evidence from the Witwatersrand gold fields, South Africa publication-title: Earth‐Science Reviews – volume: 8 year: 2020 article-title: Exploring carbon mineral systems: Recent advances in C mineral evolution, mineral ecology, and network analysis publication-title: Frontiers in Earth Science – year: 1972 – volume: 52 start-page: 12 issue: 9 year: 2000 end-page: 20 article-title: Uranium processing: A review of current methods and technology publication-title: JOM – volume: 115 start-page: 7184 issue: 28 year: 2018 end-page: 7189 article-title: US nuclear power: The vanishing low‐carbon wedge publication-title: Proceedings of the National Academy of Sciences of the United States of America – volume: 6 issue: 9 year: 2020 article-title: The Archean atmosphere publication-title: Science Advances – start-page: 121 year: 1985 end-page: 134 – year: 1993 – year: 2019 – volume: 11 start-page: 33 issue: 1 year: 1996 end-page: 51 article-title: Organic geochemistry of sedimentary uranium ore deposits publication-title: Ore Geology Reviews – volume: 160 start-page: 179 issue: 1 year: 2008 end-page: 210 article-title: Assembly, configuration, and break‐up history of Rodinia: A synthesis publication-title: Precambrian Research – volume: 338 year: 2020 article-title: The onset of oxidative weathering traced by uranium isotopes publication-title: Precambrian Research – volume: 42 start-page: 547 issue: 6, Part A year: 1978 end-page: 569 article-title: Uranium solution‐mineral equilibria at low temperatures with applications to sedimentary ore deposits publication-title: Geochimica et Cosmochimica Acta – volume: 115 issue: 12 year: 2014 article-title: Pressure effect on elastic, lattice dynamic and superconducting behaviour of yttrium sulfide: A first principle study publication-title: Journal of Applied Physics – volume: 61 start-page: 4245 issue: 20 year: 1997 end-page: 4266 article-title: Uranium in geologic fluids: Estimates of standard partial molal properties, oxidation potentials, and hydrolysis constants at high temperatures and pressures publication-title: Geochimica et Cosmochimica Acta – volume: 94 start-page: 1293 issue: 10 year: 2009 end-page: 1311 article-title: Evolution of uranium and thorium minerals publication-title: American Mineralogist – volume: 21 start-page: 1129 issue: 11 year: 1991 end-page: 1164 article-title: Graph drawing by force‐directed placement publication-title: Software: Practice and Experience – volume: 18 start-page: 899 issue: 7 year: 1992 end-page: 947 article-title: SUPCRT92—A software package for calculating the standard molal thermodynamic properties of minerals, gases, aqueous species, and reactions from 1‐Bar to 5000‐Bar and 0‐Degrees‐C to 1000‐Degrees‐C publication-title: Computers & Geosciences – volume: 43 start-page: 15 year: 2013 end-page: 119 article-title: Mineralogy and crystallography of uranium publication-title: Uranium: Cradle to Grave. Mineralogical Association of Canada Short Course – volume: 386 year: 2023 article-title: The influence of oxygen and electronegativity on iron mineral chemistry throughout Earth’s history publication-title: Precambrian Research – volume: 50 start-page: 67 year: 2017 end-page: 83 article-title: The Columbia supercontinent revisited publication-title: Gondwana Research – volume: 23 start-page: 264 issue: 4 year: 2011 end-page: 269 article-title: Origin of uranium deposits revealed by their rare Earth element signature publication-title: Terra Nova – volume: 521 start-page: 49 year: 2019 end-page: 58 article-title: Redox states of Archean surficial environments: The importance of H , g instead of O , g for weathering reactions publication-title: Chemical Geology – volume: 269 start-page: 290 issue: 3 year: 2010 end-page: 300 article-title: Retention of uranium in complexly altered zircon: An example from Bancroft, Ontario publication-title: Chemical Geology – volume: 489 start-page: 546 issue: 7417 year: 2012 end-page: 549 article-title: Ocean oxygenation in the wake of the Marinoan glaciation publication-title: Nature – year: 1992 – start-page: 1 year: 1992 – volume: 72 start-page: 345 issue: 2 year: 2008 end-page: 359 article-title: Natural fractionation of U/ U publication-title: Geochimica et Cosmochimica Acta – volume: 61 start-page: 1 year: 1958 end-page: 50 article-title: New observations of the ores of the Witwatersrand in South Africa and their genetic significance publication-title: Geological Society of South Africa Transactions – volume: 109 start-page: 426 year: 2019 end-page: 447 article-title: Occurrence of pyrites in sandstone‐type uranium deposits: Relationships with uranium mineralization in the North Ordos Basin, China publication-title: Ore Geology Reviews – volume: 58 start-page: 2829 issue: 13 year: 1994 end-page: 2843 article-title: Interaction between aqueous uranium (VI) and sulfide minerals: Spectroscopic evidence for sorption and reduction publication-title: Geochimica et Cosmochimica Acta – volume: 27 start-page: 115 issue: 2 year: 1999 end-page: 118 article-title: Redox state of the Archean atmosphere: Evidence from detrital heavy minerals in ca. 3250–2750 Ma sandstones from the Pilbara Craton, Australia publication-title: Geology – volume: 153 start-page: 179 issue: 3 year: 2007 end-page: 208 article-title: Geology and zircon geochronology of the Acasta Gneiss Complex, northwestern Canada: New constraints on its tectonothermal history publication-title: Precambrian Research – volume: 27 start-page: 643 issue: 4 year: 1989 end-page: 656 article-title: U‐Th‐bearing silicates in reefs of the Witwatersrand, South Africa publication-title: The Canadian Mineralogist – volume: 35 start-page: 627 year: 1997 end-page: 658 article-title: Characterization of multiple fluid‐flow events and rare‐Earth‐element mobility associated with formation of unconformity‐type uranium deposits in the Athabasca Basin, Saskatchewa publication-title: The Canadian Mineralogist – volume: 102 start-page: 358 issue: 3 year: 1991 end-page: 374 article-title: Geochemical and geodynamical constraints on subduction zone magmatism publication-title: Earth and Planetary Science Letters – volume: 60 start-page: 149 issue: 1 year: 2006 end-page: 166 article-title: Uranium reduction publication-title: Annual Review of Microbiology – start-page: 70 year: 1992 – volume: 28 start-page: 225 year: 2000 end-page: 262 article-title: Diagenetic fluids in paleo‐ and meso‐Proterozoic sedimentary basins and their implications for long protracted fluid histories publication-title: Mineralogical Association of Canada Short Course – volume: 60 start-page: 1515 issue: 9 year: 1996 end-page: 1529 article-title: Uranium in granitic magmas: Part 2. Experimental determination of uranium solubility and fluid‐melt partition coefficients in the uranium oxide‐haplogranite‐H O‐NaX (X = Cl, F) system at 770°C, 2 kbar publication-title: Geochimica et Cosmochimica Acta – volume: 362 start-page: 105 year: 2013 end-page: 114 article-title: Uranium isotope fractionation suggests oxidative uranium mobilization at 2.50Ga publication-title: Chemical Geology – volume: 85 start-page: 511 issue: 3 year: 1990 end-page: 536 article-title: The nature of the Witwatersrand hinterland; conjectures on the source area problem publication-title: Economic Geology – volume: 13 issue: 1 year: 2022 article-title: Evidence for the oxidation of Earth’s crust from the evolution of manganese minerals publication-title: Nature Communications – volume: 147 start-page: 11 issue: 1 year: 1998 end-page: 25 article-title: The birth of the Earth’s atmosphere: The behaviour and fate of its major elements publication-title: Chemical Geology – year: 2013 – volume: 352 year: 2021 article-title: Onset of plate tectonics by the Eoarchean publication-title: Precambrian Research – year: 1985 – volume: 97 start-page: 94 issue: 1 year: 1990 end-page: 101 article-title: Uranium removal in oceanic sediments and the oceanic U balance publication-title: Earth and Planetary Science Letters – volume: 304 start-page: 397 issue: 5 year: 2004 end-page: 437 article-title: COPSE: A new model of biogeochemical cycling over Phanerozoic time publication-title: American Journal of Science – volume: 78 issue: 1 year: 1986 article-title: Les gisements d’uranium du Gabon et les réacteurs d’Oklo. Modèle métallogénique de gîtes à fortes teneurs du Protérozoïque inférieur publication-title: Sciences Géologiques, bulletins et mémoires – volume: 82 start-page: 1169 issue: 5 year: 1987 end-page: 1176 article-title: Unusual organic matter associated with uranium from the Claude Deposit, Cluff Lake, Canada publication-title: Economic Geology – volume: 362 start-page: 82 year: 2013 end-page: 90 article-title: Uranium in iron formations and the rise of atmospheric oxygen publication-title: Chemical Geology – volume: 78 start-page: 799 issue: 5 year: 1983 end-page: 822 article-title: The Olympic Dam copper‐uranium‐gold deposit, Roxby Downs, South Australia publication-title: Economic Geology – volume: 14 start-page: 3628 issue: 9 year: 2002 end-page: 3635 article-title: Some aspects of structure and bonding in binary and ternary uranium(VI) oxides publication-title: Chemistry of Materials – start-page: 217 year: 1990 – volume: 12 year: 1990 – volume: 288 start-page: 1177 issue: 5469 year: 2000 end-page: 1178 article-title: A nuclear solution to climate change? publication-title: Science – volume: 51 start-page: 661 issue: 1 year: 2012 end-page: 666 article-title: Ba Hg U S : A complex uranium(+4)/uranium(+5) sulfide publication-title: Inorganic Chemistry – volume: 13 start-page: 1 issue: 1 year: 1980 end-page: 26 article-title: Origin of uraniferous conglomerates at Elliot Lake, Canada and Witwatersrand, South Africa: Implications for oxygen in the Precambrian atmosphere publication-title: Precambrian Research – volume: 38 start-page: 683 issue: 8 year: 2010 end-page: 686 article-title: Potassium and uranium in the upper mantle controlled by Archean oceanic crust recycling publication-title: Geology – volume: 154 issue: 12 year: 2021 article-title: Bond dissociation energies of lanthanide sulfides and selenides publication-title: The Journal of Chemical Physics – volume: 72 start-page: 1290 year: 2016 end-page: 1306 article-title: Uraniferous paleoplacers of the Mesoarchean Mahagiri Quartzite, Singhbhum craton, India: Depositional controls, nature and source of >3.0Ga detrital uraninites publication-title: Ore Geology Reviews – volume: 452 start-page: 456 issue: 7186 year: 2008 end-page: 459 article-title: Tracing the stepwise oxygenation of the Proterozoic ocean publication-title: Nature – volume: 375 start-page: 289 issue: 1 year: 2003 end-page: 324 article-title: Palaeomagnetic configuration of continents during the Proterozoic publication-title: Tectonophysics – volume: 5 start-page: 5 issue: 1 year: 2002 end-page: 22 article-title: Configuration of Columbia, a Mesoproterozoic supercontinent publication-title: Gondwana Research – volume: 15 start-page: 369 year: 2007 end-page: 409 – volume: 34 start-page: 561 issue: 6 year: 1973 end-page: 565 article-title: Genesis of radiogenic lead halos in Precambrian uranium deposits publication-title: Soviet Atomic Energy – volume: 70 start-page: 5653 issue: 23 year: 2006 end-page: 5664 article-title: GEOCARBSULF: A combined model for Phanerozoic atmospheric O and CO publication-title: Geochimica et Cosmochimica Acta – year: 2004 – volume: 33 start-page: 241 issue: 2 year: 1995 end-page: 265 article-title: The geochemical evolution of the continental crust publication-title: Reviews of Geophysics – volume: 16 start-page: 135 issue: 2 year: 1963 end-page: 142 article-title: The synthesis and crystal structures of some alkaline Earth titanium and zirconium sulfides publication-title: Acta Crystallographica – volume: 53 start-page: 598 issue: 5 year: 1958 end-page: 616 article-title: Sulfur isotopes and the origin of sandstone‐type uranium deposits [Colorado Plateau and Wyoming] publication-title: Economic Geology – volume: 430 start-page: 43 year: 2015 end-page: 53 article-title: A redox‐stratified ocean 3.2 billion years ago publication-title: Earth and Planetary Science Letters – volume: 78 start-page: 105 issue: 1 year: 1983 end-page: 120 article-title: Iron disulfide minerals and the genesis of roll‐type uranium deposits publication-title: Economic Geology – volume: 238 start-page: 438 year: 2018 end-page: 452 article-title: A Mesoarchean shift in uranium isotope systematics publication-title: Geochimica et Cosmochimica Acta – volume: 8 start-page: 1 issue: 1 year: 2017 end-page: 7 article-title: Geochemical and mineralogical evidence that Rodinian assembly was unique publication-title: Nature Communications – volume: 15 start-page: 408 issue: 3 year: 2009 end-page: 420 article-title: Contrasting modes of supercontinent formation and the conundrum of Pangea publication-title: Gondwana Research – volume: 309 start-page: 603 issue: 7 year: 2009 end-page: 606 article-title: Phanerozoic atmospheric oxygen: New results using the GEOCARBSULF model publication-title: American Journal of Science – volume: 34 issue: 8 year: 2020 article-title: Uranium isotope fractionation in non‐sulfidic anoxic settings and the global uranium isotope mass balance publication-title: Global Biogeochemical Cycles – volume: 6 start-page: 31 issue: 1 year: 2010 end-page: 36 article-title: The great oxidation event and mineral diversification publication-title: Elements – volume: 106 start-page: 2121 issue: B2 year: 2001 end-page: 2138 article-title: On fluid flow and mineral alteration in fractured caprock of magmatic hydrothermal systems publication-title: Journal of Geophysical Research – volume: 389 start-page: 33 issue: 6646 year: 1997 end-page: 39 article-title: The origin and early evolution of plants on land publication-title: Nature – volume: 12 issue: 1 year: 2022 article-title: The expanding network of mineral chemistry throughout Earth history reveals global shifts in crustal chemistry during the Proterozoic publication-title: Scientific Reports – volume: 9 start-page: 399 year: 2014 end-page: 435 – volume: 2008 issue: 10 year: 2008 article-title: Fast unfolding of communities in large networks publication-title: Journal of Statistical Mechanics: Theory and Experiment – volume: 10 start-page: 67 issue: 2 year: 1995 end-page: 94 article-title: The Witwatersrand Basin, South Africa: Geological framework and mineralization processes publication-title: Ore Geology Reviews – volume: 82 start-page: 159 year: 1990 end-page: 186 article-title: The aqueous geochemistry of the rare‐earth elements and yttrium: 1. Review of available low‐temperature data for inorganic complexes and the inorganic REE speciation of natural waters publication-title: Chemical Geology – volume: 102 start-page: 474 year: 2018 end-page: 504 article-title: Phanerozoic uranium mineralization in Variscan Europe—More than 400 Ma of tectonic, supergene, and climate‐controlled uranium redistribution publication-title: Ore Geology Reviews – volume: 20 start-page: 430 year: 1959 end-page: 434 article-title: Determination of uranium in zircon publication-title: Analytica Chimica Acta – volume: 124 start-page: 119 issue: 1 year: 1994 end-page: 129 article-title: Uranium and thorium solubilities in subduction zone fluids publication-title: Earth and Planetary Science Letters – volume: 53 start-page: 145 issue: 1 year: 2003 end-page: 181 article-title: Historical development of zircon geochronology publication-title: Reviews in Mineralogy and Geochemistry – volume: 13 start-page: 12940 issue: 28 year: 2011 end-page: 12958 article-title: Actinide sulfides in the gas phase: Experimental and theoretical studies of the thermochemistry of AnS (An = Ac, Th, Pa, U, Np, Pu, Am and Cm) publication-title: Physical Chemistry Chemical Physics – volume: 44 start-page: 41 issue: 1 year: 2009 end-page: 59 article-title: Geochronology of unconformity‐related uranium deposits in the Athabasca Basin, Saskatchewan, Canada and their integration in the evolution of the basin publication-title: Mineralium Deposita – volume: 37 issue: 1 year: 1966 article-title: Preparation of uranium sulfide single crystals publication-title: Journal of Applied Physics – volume: 126 start-page: 813 issue: 5–6 year: 2014 end-page: 830 article-title: O constraints from Paleoproterozoic detrital pyrite and uraninite publication-title: GSA Bulletin – volume: 55 start-page: 989 issue: 4 year: 1991 end-page: 1004 article-title: Thermodynamic assessment of hydrothermal alkali feldspar‐mica‐aluminosilicate equilibria publication-title: Geochimica et Cosmochimica Acta – volume: 291 start-page: 289 issue: 1381 year: 1979 end-page: 300 article-title: The mode of occurrence and distribution of uranium deposits publication-title: Philosophical Transactions of the Royal Society of London—Series A: Mathematical and Physical Sciences – volume: 55 start-page: 1799 issue: 7 year: 1991 end-page: 1806 article-title: Uranium in the oceans: Where it goes and why publication-title: Geochimica et Cosmochimica Acta – volume: 53 start-page: 1307 issue: 6 year: 1989 end-page: 1322 article-title: Irradiation of organic matter by uranium decay in the Alum Shale, Sweden publication-title: Geochimica et Cosmochimica Acta – volume: 125 issue: 6 year: 1978 article-title: Tables of standard electrode potentials publication-title: Journal of the Electrochemical Society – volume: 40 start-page: 4666 issue: 15 year: 2006 end-page: 4671 article-title: Kinetics of uranium(VI) reduction by hydrogen sulfide in anoxic aqueous systems publication-title: Environmental Science & Technology – volume: 105 start-page: 553 issue: 3 year: 2010 end-page: 569 article-title: Evolution of uranium fractionation processes through time: Driving the secular variation of uranium deposit types publication-title: Economic Geology – year: 2020 – volume: 11 start-page: 1 issue: 1 year: 1996 end-page: 31 article-title: The role of humic substances in the transport and fixation of metals of economic interest (Au, Pt, Pd, U, V) publication-title: Ore Geology Reviews – volume: 400 start-page: 184 year: 2014 end-page: 194 article-title: A modern framework for the interpretation of U/ U in studies of ancient ocean redox publication-title: Earth and Planetary Science Letters – volume: 282 start-page: 247 issue: 5736 year: 1979 end-page: 250 article-title: Rare earth element mobility associated with uranium mineralisation publication-title: Nature – volume: 341 start-page: 209 issue: 2 year: 2005 end-page: 223 article-title: Uranium secondary phase formation during anoxic hydrothermal leaching processes of UO nuclear fuel publication-title: Journal of Nuclear Materials – volume: 7 start-page: 89 year: 1976 end-page: 156 – volume: 8 start-page: 65 year: 1999 end-page: 82 – volume: 44 start-page: 3 issue: 1 year: 2009 end-page: 9 article-title: The extreme diversity of uranium deposits publication-title: Mineralium Deposita – year: 1999 – ident: e_1_2_9_45_1 doi: 10.1021/es051804n – ident: e_1_2_9_86_1 doi: 10.5382/AV75.04 – ident: e_1_2_9_48_1 – ident: e_1_2_9_78_1 doi: 10.1038/s41598‐022‐08650‐x – volume-title: Chemical thermodynamics of uranium year: 2004 ident: e_1_2_9_39_1 contributor: fullname: Grenthe I. – ident: e_1_2_9_96_1 doi: 10.1130/0091‐7613(1999)027<0115:RSOTAA>2.3.CO;2 – ident: e_1_2_9_10_1 doi: 10.3390/min13081089 – ident: e_1_2_9_19_1 doi: 10.1021/es049963e – ident: e_1_2_9_74_1 doi: 10.5382/AV75.02 – ident: e_1_2_9_115_1 doi: 10.2113/gselements.6.1.31 – ident: e_1_2_9_83_1 doi: 10.1016/j.oregeorev.2015.05.020 – volume-title: Quantitative measurements and chemical equilibria year: 1972 ident: e_1_2_9_118_1 contributor: fullname: Swift E. H. – start-page: 65 volume-title: Regional geology and metallogeny year: 1999 ident: e_1_2_9_75_1 contributor: fullname: Mikhailov V. A. – ident: e_1_2_9_65_1 doi: 10.1016/j.precamres.2007.04.021 – ident: e_1_2_9_15_1 doi: 10.1146/annurev‐earth‐081619‐052705 – ident: e_1_2_9_63_1 doi: 10.1126/science.202.4366.430 – ident: e_1_2_9_79_1 doi: 10.1016/j.precamres.2022.106960 – ident: e_1_2_9_82_1 doi: 10.3389/feart.2020.00208 – ident: e_1_2_9_44_1 doi: 10.2138/am.2009.3208 – ident: e_1_2_9_72_1 doi: 10.1016/j.gr.2017.04.011 – ident: e_1_2_9_85_1 doi: 10.1016/j.chemgeo.2009.10.004 – ident: e_1_2_9_103_1 doi: 10.1016/j.oregeorev.2018.09.013 – start-page: 369 volume-title: Developments in Precambrian geology year: 2007 ident: e_1_2_9_22_1 contributor: fullname: Champion D. C. – ident: e_1_2_9_84_1 doi: 10.1016/j.gr.2008.09.005 – ident: e_1_2_9_104_1 doi: 10.1063/1.4869401 – ident: e_1_2_9_6_1 doi: 10.1016/0012‐821X(94)00071‐9 – ident: e_1_2_9_91_1 doi: 10.1016/S0040‐1951(03)00343‐3 – volume: 78 issue: 1 year: 1986 ident: e_1_2_9_35_1 article-title: Les gisements d’uranium du Gabon et les réacteurs d’Oklo. Modèle métallogénique de gîtes à fortes teneurs du Protérozoïque inférieur publication-title: Sciences Géologiques, bulletins et mémoires contributor: fullname: Gauthier‐Lafaye F. – ident: e_1_2_9_34_1 doi: 10.1002/spe.4380211102 – ident: e_1_2_9_109_1 doi: 10.1016/S0016‐7037(97)00240‐8 – ident: e_1_2_9_14_1 doi: 10.1098/rsta.1979.0027 – ident: e_1_2_9_80_1 doi: 10.1073/pnas.1804655115 – ident: e_1_2_9_130_1 doi: 10.2172/138894 – ident: e_1_2_9_114_1 doi: 10.3389/feart.2020.585087 – ident: e_1_2_9_107_1 doi: 10.1016/j.epsl.2015.08.007 – ident: e_1_2_9_119_1 doi: 10.1007/BF01117679 – ident: e_1_2_9_12_1 doi: 10.2475/07.2009.03 – ident: e_1_2_9_64_1 doi: 10.1016/0016‐7037(89)90065‐3 – ident: e_1_2_9_113_1 doi: 10.1063/5.0042695 – ident: e_1_2_9_24_1 doi: 10.1107/S0365110X6300030X – ident: e_1_2_9_81_1 doi: 10.1007/978-1-4614-7591-0 – ident: e_1_2_9_105_1 doi: 10.1038/nature11445 – ident: e_1_2_9_51_1 doi: 10.1021/cm062349c – volume: 61 start-page: 1 year: 1958 ident: e_1_2_9_95_1 article-title: New observations of the ores of the Witwatersrand in South Africa and their genetic significance publication-title: Geological Society of South Africa Transactions contributor: fullname: Ramdohr P. – ident: e_1_2_9_8_1 doi: 10.1016/0012‐821X(90)90101‐3 – ident: e_1_2_9_43_1 doi: 10.1016/j.eng.2019.03.006 – ident: e_1_2_9_25_1 doi: 10.1029/2020GB006649 – ident: e_1_2_9_102_1 doi: 10.1016/S1342‐937X(05)70883‐2 – ident: e_1_2_9_106_1 doi: 10.1126/science.288.5469.1177 – start-page: 217 volume-title: The emergence of animals: The Cambrian breakthrough year: 1990 ident: e_1_2_9_71_1 doi: 10.7312/mcme93416 contributor: fullname: McMenamin M. A. S. – ident: e_1_2_9_26_1 doi: 10.1007/s00126‐008‐0223‐1 – ident: e_1_2_9_62_1 doi: 10.2113/gsecongeo.82.5.1169 – ident: e_1_2_9_46_1 doi: 10.1038/s41467‐022‐28589‐x – ident: e_1_2_9_98_1 doi: 10.2113/gsecongeo.85.3.511 – ident: e_1_2_9_3_1 doi: 10.1007/s00126‐007‐0153‐3 – ident: e_1_2_9_99_1 doi: 10.1016/0169‐1368(95)00011‐9 – volume: 43 start-page: 15 year: 2013 ident: e_1_2_9_58_1 article-title: Mineralogy and crystallography of uranium publication-title: Uranium: Cradle to Grave. Mineralogical Association of Canada Short Course contributor: fullname: Krivovichev S. – ident: e_1_2_9_56_1 doi: 10.1021/cm020258j – ident: e_1_2_9_13_1 doi: 10.1088/1742‐5468/2008/10/P10008 – ident: e_1_2_9_52_1 doi: 10.1130/B30949.1 – ident: e_1_2_9_66_1 doi: 10.1038/s41467‐017‐02095‐x – ident: e_1_2_9_41_1 doi: 10.1016/j.chemgeo.2019.05.022 – ident: e_1_2_9_55_1 doi: 10.1038/37918 – ident: e_1_2_9_76_1 doi: 10.1149/1.2131790 – ident: e_1_2_9_120_1 doi: 10.1029/95RG00262 – ident: e_1_2_9_17_1 doi: 10.1021/ic202161y – ident: e_1_2_9_27_1 doi: 10.2113/gsecongeo.105.3.553 – ident: e_1_2_9_133_1 doi: 10.1029/2000JB900356 – ident: e_1_2_9_94_1 doi: 10.1016/B978-0-444-41407-6.50006-4 – ident: e_1_2_9_89_1 doi: 10.1016/0016‐7037(96)00039‐7 – volume: 28 start-page: 225 year: 2000 ident: e_1_2_9_59_1 article-title: Diagenetic fluids in paleo‐ and meso‐Proterozoic sedimentary basins and their implications for long protracted fluid histories publication-title: Mineralogical Association of Canada Short Course contributor: fullname: Kyser K. – ident: e_1_2_9_100_1 doi: 10.2113/gsecongeo.78.5.799 – ident: e_1_2_9_131_1 doi: 10.1016/0009‐2541(90)90080‐Q – ident: e_1_2_9_37_1 doi: 10.1016/0301‐9268(80)90056‐X – ident: e_1_2_9_20_1 doi: 10.1126/sciadv.aax1420 – ident: e_1_2_9_54_1 doi: 10.1016/j.chemgeo.2013.08.010 – ident: e_1_2_9_116_1 – ident: e_1_2_9_16_1 doi: 10.1016/j.precamres.2019.105583 – ident: e_1_2_9_97_1 doi: 10.2113/gsecongeo.78.1.105 – ident: e_1_2_9_11_1 doi: 10.1016/j.gca.2005.11.032 – ident: e_1_2_9_33_1 doi: 10.1016/j.earscirev.2004.10.003 – volume-title: Geology and uranium deposits, Shirley Basin area, Wyoming (No. 745) year: 1972 ident: e_1_2_9_42_1 contributor: fullname: Harshman E. N. – ident: e_1_2_9_57_1 doi: 10.1016/0016‐7037(91)90024‐Y – ident: e_1_2_9_88_1 doi: 10.1016/j.chemgeo.2013.09.005 – start-page: 1 volume-title: Chemical thermodynamics of uranium year: 1992 ident: e_1_2_9_38_1 contributor: fullname: Grenthe I. – ident: e_1_2_9_73_1 doi: 10.1111/j.1365‐3121.2011.01008.x – volume: 35 start-page: 627 year: 1997 ident: e_1_2_9_32_1 article-title: Characterization of multiple fluid‐flow events and rare‐Earth‐element mobility associated with formation of unconformity‐type uranium deposits in the Athabasca Basin, Saskatchewa publication-title: The Canadian Mineralogist contributor: fullname: Fayek M. – ident: e_1_2_9_47_1 doi: 10.1016/j.precamres.2006.11.017 – ident: e_1_2_9_111_1 doi: 10.1007/978-94-009-6060-2_6 – ident: e_1_2_9_29_1 doi: 10.1007/978-3-662-02892-6 – ident: e_1_2_9_53_1 doi: 10.1016/0098‐3004(92)90029‐q – ident: e_1_2_9_40_1 doi: 10.1016/j.epsl.2016.10.021 – ident: e_1_2_9_23_1 doi: 10.1016/j.oregeorev.2019.03.037 – ident: e_1_2_9_126_1 doi: 10.1016/0016‐7037(94)90117‐1 – ident: e_1_2_9_9_1 doi: 10.2475/ajs.304.5.397 – ident: e_1_2_9_18_1 doi: 10.1515/9781501509193 – volume-title: Standard potentials in aqueous solution year: 1985 ident: e_1_2_9_7_1 contributor: fullname: Bard A. J. – ident: e_1_2_9_124_1 doi: 10.1146/annurev.micro.59.030804.121357 – ident: e_1_2_9_30_1 doi: 10.2113/0530145 – ident: e_1_2_9_127_1 doi: 10.1016/j.gca.2007.11.012 – ident: e_1_2_9_50_1 doi: 10.2113/gsecongeo.53.5.598 – ident: e_1_2_9_121_1 doi: 10.1063/1.1707867 – volume: 27 start-page: 643 issue: 4 year: 1989 ident: e_1_2_9_112_1 article-title: U‐Th‐bearing silicates in reefs of the Witwatersrand, South Africa publication-title: The Canadian Mineralogist contributor: fullname: Smits G. – ident: e_1_2_9_67_1 doi: 10.3390/min10100876 – ident: e_1_2_9_122_1 doi: 10.1016/B978-0-08-095975-7.00715-4 – ident: e_1_2_9_87_1 doi: 10.1130/G30852.1 – ident: e_1_2_9_77_1 doi: 10.1016/j.oregeorev.2004.10.001 – ident: e_1_2_9_49_1 doi: 10.1016/S0009‐2541(97)00169‐1 – ident: e_1_2_9_101_1 doi: 10.2113/gsecongeo.73.8.1409 – ident: e_1_2_9_128_1 doi: 10.1016/0040‐1951(91)90416‐P – ident: e_1_2_9_36_1 – ident: e_1_2_9_110_1 doi: 10.1016/j.gca.2011.06.041 – ident: e_1_2_9_90_1 doi: 10.1039/C1CP20996E – start-page: 121 volume-title: Uranium mineralisation in some Phanerozoic sandstones in India year: 1985 ident: e_1_2_9_92_1 contributor: fullname: Phadke A. V. – ident: e_1_2_9_4_1 doi: 10.1016/j.jnucmat.2005.02.004 – ident: e_1_2_9_129_1 doi: 10.1016/j.precamres.2020.105980 – ident: e_1_2_9_69_1 doi: 10.1144/GSL.MEM.1990.012.01.01 – ident: e_1_2_9_125_1 doi: 10.1016/j.gca.2018.07.024 – ident: e_1_2_9_5_1 doi: 10.1016/j.epsl.2014.05.051 – ident: e_1_2_9_31_1 doi: 10.1007/s11837‐000‐0181‐2 – ident: e_1_2_9_60_1 doi: 10.1016/0169‐1368(95)00014‐3 – ident: e_1_2_9_70_1 doi: 10.1038/282247a0 – ident: e_1_2_9_2_1 doi: 10.1146/annurev.ns.08.120158.001353 – ident: e_1_2_9_21_1 doi: 10.1098/rsta.2017.0405 – ident: e_1_2_9_61_1 doi: 10.1016/0016‐7037(78)90001‐7 – ident: e_1_2_9_117_1 doi: 10.1016/0016‐7037(91)90157‐z – ident: e_1_2_9_123_1 doi: 10.1086/658295 – ident: e_1_2_9_28_1 doi: 10.1016/0003‐2670(59)80094‐5 – ident: e_1_2_9_68_1 doi: 10.1016/0012‐821X(91)90029‐H – ident: e_1_2_9_108_1 doi: 10.1038/nature06811 – ident: e_1_2_9_93_1 doi: 10.1016/0341‐8162(96)00003‐3 – ident: e_1_2_9_132_1 doi: 10.1016/0169‐1368(95)00013‐5 |
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Title | Uranium Redox and Deposition Transitions Embedded in Deep‐Time Geochemical Models and Mineral Chemistry Networks |
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