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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

DOI 10.1016/0009-2541(91)90115-8

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Authors: Bau, M.
Corresponding author: Bau, Michael
ORCID: Bau, Michael
Venue: Chemical Geology
Publisher: Elsevier BV
Published: 1991-12
Volume: 93
Issue: 3-4
Pages: 219-230
ISSN: 0009-2541 (ISSN-L)
DOI: 10.1016/0009-2541(91)90115-8
OpenAlex: W1982560803
Semantic Scholar: b262391a8fc3eba81f63bd12a12067f78f83b5ad
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
Licence: www.elsevier.com/tdm/userlicense/1.0/ (tdm)
Locations: Chemical Geology (publishedVersion)
HZB Repository (Helmholtz-Zentrum Berlin für Materialien und Energie GmbH (HZB)) (submittedVersion)
Topics: Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › 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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Rare-earth element mobility during hydrothermal and metamorphic fluid-rock interaction and the significance of the oxidation state of europium

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