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All abstracts by Xiangli Wang in conference series: Goldschmidt

(2018) ╬┤238U in Organic-Rich Marine and Lake Sediment Suggest Surface Oxygenation at 3.0 Ga
Wang X, Ossa Ossa F & Planavsky N

(2018) The Tl and Cr Isotope Composition of the Upper Continental Crust from the Archean to Present
Gaschnig R, Owens J, Newby S, Reinhard C, Wang X, Asael D, Planavsky N & Rudnick R

(2018) Uranium Isotope Fractionation Factors in Ferruginous Settings
Cole D, Longley M, Wilkes D, Wang X, Swanner E, Witkop C, Sperling E & Planavsky N

(2017) Coupled U and Fe Isotope Records Suggest Onset of Oxygenic Photosynthesis Three Billion Years Ago
Wang X & Planavsky N

(2017) Behavior of Mo, U, and Tl Isotopes during Differentiation in the Kilauea Iki System
Gaschnig R, Reinhard C, Owens J, Planavsky N, Wang X, Asael D, Greaney A & Helz R

(2016) Integrated Geochemical-Sedimentological Tests for the Preservation of Seawater Paleo-Redox Signals in Carbonates
Hood A, Planavsky N, Wallace M, Wang X, Gueguen B, Cole D & Bellefroid E

(2016) Mo and U Isotope Behavior in the Lesser Antilles Subduction System
Gaschnig R, Reinhard C, Planavsky N, Wang X, Asael D & Chauvel C

(2015) Chromium Isotope Effects Induced by Metamorphic, Weathering, and Hydrothermal Alterations
Wang X, Planavsky N, Reinhard C, Zou H, Ague J, Wu Y & Peucker Ehrenbrink B

(2014) Cenozoic Seawater Uranium Isotopic Composition Recorded in Mn-Fe Crusts
Wang X, Planavsky N, Reinhard C, Hein J, Lyons T & Johnson T

(2014) Cr, Se, and U Isotopic Fractionation Induced by Oxidation: A Synthesis
Johnson T, Wang X, Ellis A & Lundstrom C

(2013) Earth Surface Redox Constraints from the Ancient Cr Cycle
Planavsky N, Reinhard C, Wang X, Fischer W, Johnson T & Lyons T

(2013) The Isotopic Composition of Selenium in Chinese Coals
Zhu J-M, Johnson TM, Liang L, Wang X-L, Qin H-B & Yin Z-Y

(2012) Isotopic Fractionation of Selenium in Higher Plants
Zhu J, Johnson TM, Qin H, Wang X & Yuan Y

(2012) Isotope Exchange Rates and Equilibrium Fractionation between Cr(III) and Cr(VI)
Wang X & Johnson TM

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