Detection and visualization of micron-scale U-Ca phosphates as a key to redox and acid-base conditions in ores: Sandstone-hosted uranium deposit
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P. Mikysek | M. Slobodník | T. Trojek | J. Adamovič | N. Mészárosová | D. Trojková | Eliska Mikyskova
[1] E. Nigmatulina,et al. Origin of the Pd-Rich Pentlandite in the Massive Sulfide Ores of the Talnakh Deposit, Norilsk Region, Russia , 2021, Minerals.
[2] M. Kartal,et al. Rapid Marcasite to Pyrite Transformation in Acidic Low-Temperature Hydrothermal Fluids and Saturation Index Control on FeS2 Precipitation Dynamics and Phase Selection , 2021, ACS Earth and Space Chemistry.
[3] T. Zikmund,et al. Multi-scale visualization of uranium-rich domains dispersed in U-Zr mineralization of sandstone-type (Břevniště, Czech Republic) , 2021 .
[4] L. Krmíček,et al. The story of post-Variscan lamprophyres of the Bohemian Massif: from ultramafic (Upper Cretaceous–Paleocene) to alkaline (Eocene–Oligocene) types , 2021, Special Publications.
[5] A. Ghahreman,et al. Effect of Ultrasound on the Oxidative Copper Leaching from Chalcopyrite in Acidic Ferric Sulfate Media , 2020, Minerals.
[6] J. Bargar,et al. Experimental redox transformations of uranium phosphate minerals and mononuclear species in a contaminated wetland. , 2020, Journal of hazardous materials.
[7] P. Mikysek,et al. X-ray fluorescence mapping as a first-hand tool in disseminated ore assessment: sandstone-hosted U–Zr mineralization , 2019, Minerals Engineering.
[8] P. Tremaine,et al. An Investigation of Uranyl Sulfate Complexation under Hydrothermal Conditions by Quantitative Raman Spectroscopy and Density Functional Theory. , 2019, The journal of physical chemistry. B.
[9] C. Ryan,et al. Micron-scale distribution of metals in Cambrian metalliferous shales, South China: Insights into local biologically driven redox disequilibrium , 2019 .
[10] R. Pascal,et al. How Prebiotic Chemistry and Early Life Chose Phosphate , 2019, Life.
[11] V. Šrein,et al. Uraninite, Coffinite and Ningyoite from Vein-Type Uranium Deposits of the Bohemian Massif (Central European Variscan Belt) , 2019, Minerals.
[12] Pavel Pořízka,et al. Application of self-organizing maps to the study of U-Zr-Ti-Nb distribution in sandstone-hosted uranium ores , 2017 .
[13] P. Burns,et al. Uranyl phosphates and associated minerals in the Koprubasi (Manisa) uranium deposit, Turkey , 2017 .
[14] Pavel Pořízka,et al. Multivariate approach to the chemical mapping of uranium in sandstone-hosted uranium ores analyzed using double pulse Laser-Induced Breakdown Spectroscopy , 2016 .
[15] Nick Wilson,et al. The application of automated electron beam mapping techniques to the characterisation of low grade, fine-grained mineralisation; potential problems and recommendations , 2015 .
[16] D. Layton-Matthews,et al. Chemical Compositions of Natural Uraninite , 2015 .
[17] Shaun T. Brown,et al. Characterization of cores from an in-situ recovery mined uranium deposit in Wyoming: Implications for post-mining restoration , 2014 .
[18] J. Málek,et al. Architecture of thrust faults with alongstrike variations in fault-plane dip: anatomy of the Lusatian Fault, Bohemian Massif , 2014 .
[19] J. Brugger,et al. The Sandstone-Hosted Beverley Uranium Deposit, Lake Frome Basin, South Australia: Mineralogy, Geochemistry, and a Time-Constrained Model for Its Genesis , 2011 .
[20] R. Ewing,et al. Crystal chemistry and radiation-induced amorphization of P-coffinite from the natural fission reactor at Bangombé, Gabon , 2009 .
[21] M. Pownceby,et al. Mineral characterisation by EPMA mapping , 2007 .
[22] O. A. Doinikova. Uranium deposits with a new phosphate type of blacks , 2007 .
[23] T. Iwatsuki,et al. A system model for the origin and evolution of the Tono Uranium Deposit, Japan , 2006, Geochemistry: Exploration, Environment, Analysis.
[24] Kunio Ota,et al. Geochemical constraints on the origin and stability of the Tono Uranium Deposit, Japan , 2006, Geochemistry: Exploration, Environment, Analysis.
[25] E. Wakai,et al. Mechanisms of uranium mineralization by the yeast Saccharomyces cerevisiae , 2005 .
[26] C. MacRae,et al. Hyperspectral mapping—combining cathodoluminescence and X‐ray collection in an electron microprobe , 2005, Microscopy research and technique.
[27] T. K. Kyser,et al. EFFECTS OF CATIONIC SUBSTITUTIONS AND ALTERATION IN URANINITE, AND IMPLICATIONS FOR THE DATING OF URANIUM DEPOSITS , 2005 .
[28] M. Fayek,et al. Mineral paragenesis and textures associated with sandstone-hosted roll-front uranium deposits, NW China , 2005 .
[29] W. Zech,et al. The forms of phosphorus in humic and fulvic acids of a toposequence of alpine soils in the northern Caucasus , 1997 .
[30] R. Ewing,et al. Phosphatian coffinite with rare earth elements and Ce-rich françoisite-(Nd) from sandstone beneath a natural fission reactor at Bangombé, Gabon , 1996, Mineralogical Magazine.
[31] P. Landais. Organic geochemistry of sedimentary uranium ore deposits , 1996 .
[32] R. Ewing,et al. Structural formula of uraninite , 1992 .
[33] R. Ewing,et al. Dissolution and alteration of uraninite under reducing conditions , 1992 .
[34] Koji Watanabe. Geochemical behaviour of iron and manganese ions in the Ningyo-Toge uranium deposit district, Southwest Japan , 1987 .
[35] K. Scott. Sulphide geochemistry and wall rock alteration as a guide to mineralization, mammoth area, NW Queensland, Australia , 1986 .
[36] K. Kajitani. A geochemical study on the genesis of ningyoite the special calcium uranous phosphate mineral , 1970 .
[37] R. Meyrowitz,et al. Ningyoite, a new uranous phosphate mineral from Japan , 1959 .
[38] M. Sarfraz,et al. Determination of uranium content in phosphate ores using different measurement techniques , 2016 .
[39] K. Jensen,et al. Review of spatial relations between uraninite and coffinite - implications for alteration mechanisms , 2012 .
[40] A. Horbe,et al. Chemical composition of black-watered rivers in the western Amazon Region (Brazil) , 2009 .
[41] B. Scharm,et al. Rhabdophane group minerals in the uranium ore district of northern Bohemia (Czech Republic) , 1994 .
[42] A. Oberlin,et al. Characterization of organic matter associated with uranium deposits in the Francevillian formation of Gabon (lower proterozoic) , 1990 .
[43] M. Goldhaber,et al. Origin of coffinite in sedimentary rocks by a sequential adsorption-reduction mechanism. , 1987 .
[44] 片山 信夫,et al. Favourable conditions for the formation of basal type uranium deposits. , 1977 .
[45] T. Muto. THERMOCHEMICAL STABILITY OF NINGYOITE , 1965 .
[46] T. Muto. THE PRECITITATION ENVIRONMENT OF NINGYOITE , 1962 .
[47] T. Muto. PARAGENESES OF THE MINERALS OF THE NINGYÔ-TÔGÉ MINE , 1961 .