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ID18F: a new X-ray microprobe end station”. Somogyi A, Drakopoulos M, Vincze L, Vekemans B, Camerani C, Janssens K, Snigirev A, Adams F, ESRF highlights 2001 , 96 (2002)
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A Monte Carlo model for studying the microheterogeneity of trace elements in reference materials by means of synchrotron microscopic X-ray fluorescence”. Kempenaers L, Janssens K, Vincze L, Vekemans B, Somogyi A, Drakopoulos M, Simionovici AS, Adams F, Analytical chemistry 74, 5017 (2002). http://doi.org/10.1021/AC025662G
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Quantitative trace element analysis of individual fly ash particles by means of X-ray microfluorescence”. Vincze L, Somogyi A, Osán J, Vekemans B, Török S, Janssens K, Adams F, Analytical chemistry 74, 1128 (2002). http://doi.org/10.1021/AC010789B
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Molecular speciation of inorganic mixtures by Fourier transform laser microprobe mass sepctrometry”. Ignatova VA, van Vaeck L, Gijbels R, Adams F, International journal of mass spectrometry 225, 213 (2003). http://doi.org/10.1016/S1387-3806(02)01116-8
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Micro-heterogeneity study of trace elements in USGS, MPI-DING and glass reference materials by means of synchrotron micro-XRF”. Kempenaers L, Janssens K, Jochum KP, Vincze L, Vekemans B, Somogyi A, Drakopoulos M, Adams F, Journal of analytical atomic spectrometry 18, 350 (2003). http://doi.org/10.1039/B212196D
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Effects of beamline components (undulators, monochromator, focusing devices) on the beam intensity at ID18F (ESRF)”. Somogyi A, Drakopoulos M, Vekemans B, Vincze L, Simionovici AS, Adams F, Nuclear instruments and methods: B 199, 559 (2003). http://doi.org/10.1016/S0168-583X(02)01535-5
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Quantitative X-ray fluorescence analysis at the ESRF ID18F microprobe”. Vekemans B, Vincze L, Somogyi A, Drakopoulos M, Kempenaers L, Simionovici AS, Adams F, Nuclear instruments and methods: B 199, 396 (2003). http://doi.org/10.1016/S0168-583X(02)01396-4
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Study of microgeometry of porous materials using synchrotron computed microtomography”. Jones KW, Feng H, Lindquist WB, Adler PM, Thover JF, Vekemans B, Vincze L, Szalóki I, Van Grieken R, Adams F, Riekel C page 39 (2003).
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Synchrotron computed X-ray fluorescence microtomography in environmental and earth sciences”. Vincze L, Vekemans B, Adams F, (2003)
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Kempenaers L, Vincze L, Vekemans B, Janssens K, Adams F, Somogyi A, Drakopoulos M, Simionovici AS (2004) Micro-heterogeneity study of trace elements in reference materials. 132 p
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Monte Carlo simulation for X-ray fluorescence spectroscopy”. Vincze L, Janssens K, Vekemans B, Adams F page 435 (2004).
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Application of combined micro-proton-induced X-ray emission and micro-synchrotron radiation X-ray fluorescence techniques for the characterization of impact materials around Barringer Meteor Crater”. Uzonyi I, Szöör G, Vekemans B, Vincze L, Rozsa P, Szabo G, Somogyi A, Adams F, Kiss ÁZ, Spectrochimica acta: part B : atomic spectroscopy 59, 1717 (2004). http://doi.org/10.1016/J.SAB.2004.05.030
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Characterization of impact materials around Barringer meteor crater by micro-PIXE nd micro-SRXRF techniques”. Uzonyi I, Szöör G, Rozsa P, Vekemans B, Vincze L, Adams F, Drakopoulos M, Somogyi A, Kiss ÁZ, Nuclear instruments and methods in physics research: B: beam interactions with materials and atoms 219/220, 555 (2004). http://doi.org/10.1016/J.NIMB.2004.01.119
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Processing of three-dimensional microscopic X-ray fluorescence data”. Vekemans B, Vincze L, Brenker FE, Adams F, Journal of analytical atomic spectrometry 19, 1302 (2004). http://doi.org/10.1039/B404300F
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Synchrotron computed X-ray fluorescence tomography in environmental and earth sciences: radiation”. Vincze L, Vekemans B, Adams F, (2004)
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Synchrotron radiation for microscopic X-ray fluorescence analysis”. Adams F, Vincze L, Vekemans B page 343 (2004).
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Three-dimensional trace element analysis by confocal X-ray microfluorescence imaging”. Vincze L, Vekemans B, Brenker FE, Falkenberg G, Rickers K, Somogyi A, Kersten M, Adams F, Analytical chemistry 76, 6786 (2004). http://doi.org/10.1021/AC049274L
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X-ray fluorescence microtomography and polycapillary based confocal imaging using synchrotron radiation”. Vincze L, Vekemans B, Szaloki I, Brenker FE, Falkenberg G, Rickers K, Aerts K, Van Grieken R, Adams F, , 220 (2004). http://doi.org/10.1117/12.560416
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Detection of a Ca-rich lithology in the Earth's deep (>, 300 km) convecting mantle”. Brenker FE, Vincze L, Vekemans B, Nasdala L, Stachel T, Vollmer C, Kersten M, Somogyi A, Adams F, Joswig W, Harris JW, Earth and planetary science letters 236, 579 (2005). http://doi.org/10.1016/J.EPSL.2005.05.021
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