Cited by 1,308Geological and Geochemical AnalysisGeochemistry and Elemental AnalysisPaleontology and Stratigraphy of Fossils

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

Bau, Michael·1991·Chemical Geology

Integrity signals

Registry

Crossref · 10.1016/0009-2541(91)90115-8

Cites

41 of 41 references verified0 citation errors · 0 not checkable

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Claims the paper makes

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Claims other papers make about this one

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  • Eu remains in the soluble Eu2+ state in hydrothermal fluids because Eu2+ is more stable at higher temperatures.

    “Furthermore, Eu remains in the soluble Eu 2+ state in hydrothermal fluids because Eu 2+ is more stable at higher temperatures (Sverjensky, 1984; Bau, 1991).”
  • Typically, HREE are enriched in the oxide facies of iron formations, as the result of interaction between hydrothermal fluids and mid-ocean ridge basalt (MORB) at spreading centres, which are typically tholeiitic and depleted in LREE.

    “Typically, HREE are enriched in the oxide facies of IF, as the result of interaction between hydrothermal fluids and mid-ocean ridge basalt (MORB) at spreading centres, which are typically tholeiitic and depleted in LREE (Derry and Jacobsen, 1990; Bau, 1991).”

Cites

Flagged first, then by citations

Research works printed but not linked: 5

  1. Bau, 1990, Stabilität zweiwertiger Lanthaniden (Eu, Yb, Sm) in heißthermalen geologischen Systemen?, Hahn-Meitner-Inst. Berlin, Berlin, Intern. Rep.
  2. Bilal, 1992, Chem. Geol.
  3. Lausch, 1974, Die Verteilung der Seltenen Erden in den Karbonaten und penninischen Gneisen der Zillertaler Alpen (Tirol, Österreich), Neues Jahrb. Mineral., Monatsh., 11, 490
  4. 1986, Vol. 5, 218
  5. Wood, 1991, The genesis of pegmatites containing high technology metals (Be, Li, Nb, Ta, REE, Zr, Ga and Ge): Theoretical thermodynamic calculations of the content of high technology metals in aqueous vapor from 600 to 1200 K at 1 Kb, Contrib. Mineral. Petrol.

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Authors
Bau, M.
Corresponding author
Bau, Michael
Venue
Chemical Geology
Publisher
Elsevier BV
Published
1991-12
Volume
93
Issue
3-4
Pages
219-230
ISSN
0009-2541 (ISSN-L)
OpenAlex
W1982560803
Cited by
1,308
References
41
Citations by year
2026: 99 · 2025: 106 · 2024: 102 · 2023: 105 · 2022: 101 · 2021: 92 · 2020: 85 · 2019: 78 · 2018: 66 · 2017: 62 · 2016: 37 · 2015: 38 · 2014: 42 · 2013: 26 · 2012: 31
FWCI
5.05
Type
journal article
Language
en
Open access
closed
Locations
  • Chemical Geology (publishedVersion)
  • HZB Repository (Helmholtz-Zentrum Berlin für Materialien und Energie GmbH (HZB)) (submittedVersion)
Topics
  • Physical Sciences › Earth and Planetary Sciences › Geophysics › Geological and Geochemical Analysis
  • Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geochemistry and Elemental Analysis
  • Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
Keywords
rare earth elements, hydrothermal alteration, oxygen fugacity, Eu anomaly, infiltration metasomatism, water/rock ratio, REE fractionation

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