Cited by 577Geological and Geochemical AnalysisGeological Studies and ExplorationGeological and Geophysical Studies Worldwide

Eclogitization of lower crustal granulites by fluid migration through shear zones

Austrheim, H.·1987·Earth and Planetary Science Letters

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Crossref · 10.1016/0012-821x(87)90158-0

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  • In the Western Gneiss region of Norway, eclogitization of granulite-facies rocks is restricted to sheared and deformed zones, implying that strain and (or) hydrous fluids were essential to promote eclogite reactions despite appropriate P-T conditions.

    “This second possibility is in part based on evidence from the Western Gneiss region of Norway, in which eclogitization of granulite-facies rocks is restricted to sheared and deformed zones, implying that strain and (or) hydrous fluids were essential to promote eclogite reactions despite appropriate P-T conditions (Austrheim 1987).”

Authors
Austrheim, H.
Corresponding author
Austrheim, H.
Venue
Earth and Planetary Science Letters
Publisher
Elsevier BV
Published
1987-01
Volume
81
Issue
2-3
Pages
221-232
ISSN
0012-821X (ISSN-L)
OpenAlex
W2057408414
Cited by
577
References
0
Citations by year
2026: 9 · 2025: 13 · 2024: 26 · 2023: 24 · 2022: 31 · 2021: 31 · 2020: 29 · 2019: 21 · 2018: 38 · 2017: 22 · 2016: 28 · 2015: 23 · 2014: 18 · 2013: 15 · 2012: 19
FWCI
4.55
Type
journal article
Language
en
Open access
closed
Locations
Earth and Planetary Science Letters (publishedVersion)
Topics
  • Physical Sciences › Earth and Planetary Sciences › Geophysics › Geological and Geochemical Analysis
  • Physical Sciences › Earth and Planetary Sciences › Geology › Geological Studies and Exploration
  • Physical Sciences › Earth and Planetary Sciences › Geophysics › Geological and Geophysical Studies Worldwide
Keywords
eclogitization, lower crust, granulite, fluid migration, shear zones, Caledonian orogeny, Bergen Arcs, eclogite facies, crustal density, seismic velocity

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