Rare-earth element mobility during hydrothermal and metamorphic fluid-rock interaction and the significance of the oxidation state of europium

1991/12/01 by Michael Bau · 28 citations
Chemistry · Earth and Planetary Sciences · #Radioactive element chemistry and processing #Geochemistry and Elemental Analysis #Geological and Geochemical Analysis

paper · doi:10.1016/0009-2541(91)90115-8

Cited by

• Trace element distribution in Neoproterozoic carbonates as palaeoenvironmental indicator
• The Rare Earth Elements and Uranium in Garnets from the Beinn an Dubhaich Aureole, Skye, Scotland, UK: Constraints on Processes in a Dynamic Hydrothermal System
• REE in skarn systems: A LA-ICP-MS study of garnets from the Crown Jewel gold deposit
• The influence of sediment recycling and basement composition on evolution of mudrock chemistry in the southwestern United States
• Origin of oscillatory zoned garnets from the Xieertala Fe–Zn skarn deposit, northern China: In situ LA–ICP-MS evidence
• The formation and trace elements of garnet in the skarn zone from the Xinqiao Cu-S-Fe-Au deposit, Tongling ore district, Anhui Province, Eastern China
• Major and rare earth element mineral chemistry of low-grade assemblages inform dynamics of hydrothermal ocean-floor metamorphism in the Dinaridic Neotethys
• Contrasting rare earth element responses to climate and pedogenesis in two sand chronosequences along a climosequence in southwestern Australia
• Unusual magnetic order in Eu₁₀Hg₅₅
• Distribution of yttrium and rare-earth elements in the Penge and Kuruman iron-formations, Transvaal Supergroup, South Africa
• Geochemistry of the Krivoy Rog Banded Iron Formation, Ukraine, and the impact of peak episodes of increased global magmatic activity on the trace element composition of Precambrian seawater
• Trace element and Nd isotope composition of shallow seawater prior to the Great Oxidation Event: Evidence from stromatolitic bioherms in the Paleoproterozoic Rooinekke and Nelani Formations, South Africa
• Earth's youngest banded iron formation implies ferruginous conditions in the Early Cambrian ocean. [europepmc]
• The Origin of Carbonate Veins Within the Sedimentary Cover and Igneous Rocks of the Cocos Ridge: Results From IODP Hole U1414A. [europepmc]
• Anaerobic reduction of europium by a Clostridium strain as a strategy for rare earth biorecovery. [europepmc]
• Geochemistry of Vein Calcites Hosted in the Troodos Pillow Lavas and Their Implications for the Timing and Physicochemical Environment of Fracturing, Fluid Circulation, and Vein Mineral Growth. [europepmc]
• Geochemistry and Microtextures of Vein Calcites Pervading the Izu-Bonin Forearc and Rear Arc Crust: New Insights From IODP Expeditions 352 and 351. [europepmc]
• Sedimentary and geochemical characteristics of Triassic new type of polyhalite potassium resources in Northeast Sichuan and its genetic study. [europepmc]
• Enrichment and Occurrence of Mn in 5 -2 Coal from Qinglongsi Coal Mine, Northern Ordos Basin, China. [europepmc]
• Potential of garnet sand as an unconventional resource of the critical high-technology metals scandium and rare earth elements. [europepmc]
• Quantification of individual Rare Earth Elements from industrial sources in sewage sludge. [europepmc]
• Earth's geodynamic evolution constrained by 182 W in Archean seawater. [europepmc]
• Rare earth element geochemistry of Middle Devonian reefal limestones of the Dianqiangui Basin, South China: implications for nutrient sources and expansion of the reef ecosystem. [europepmc]
• Blooming of a microbial community in an Ediacaran extreme volcanic lake system. [europepmc]
• Unravelling the Flotation Performance of 1-Hydroxy-2-naphthyl hydroxamic Acid and Styrene Phosphonic Acid Collectors on Monazite Using Experiments and DFT Calculations. [europepmc]
• Localized and Transient Oxygenation of Shallow Oceans of Southwestern Laurentia at the Ediacaran-Cambrian Boundary. [europepmc]
• Unusual Magnetic Order in Eu 11- x Hg 54+ x . [europepmc]
• Sedimentary environment evolution and organic matter enrichment mechanisms of the cambrian Qiongzhusi Formation in the southwestern Yangtze Block. [europepmc]