Redistribution of trace elements during prograde metamorphism from lawsonite blueschist to eclogite facies; implications for deep subduction-zone processes
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Lawsonite is stable up to ~10 GPa and may carry H2O and trace elements into the mantle more effectively than other hydrous phases.
“Lawsonite is stable up to ~10 GPa and may so carry H 2 O and other trace elements (REE, Sr, Th, and U) into the mantle more effectively than other hydrous phases, such as amphibole, epidote, and chlorite (Pawley, 1994;Schmidt and Poli, 1998;Spandler et al., 2003;Usui et al., 2007;Martin et al., 2014).”
From Secular change and the onset of plate tectonics on Earth (2020) · cites this paper as Spandler et al., 2003
The Introduction (page unavailable) identifies lawsonite as a potential host of water and Sr, Th, U, and REE in subducting crust, and says such phases may be stable above 5 GPa. The Liberation of trace elements section (page unavailable) reports appreciable trace elements in lawsonite, but the paper does not establish stability to ~10 GPa or that lawsonite carries water and trace elements into the mantle more effectively than the named hydrous phases. (LLM, conf=0.86)
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“Lawsonite is stable up to ~10 GPa and may so carry H2O and other trace elements (REE, Sr, Th, and U) into the mantle more effectively than other hydrous phases, such as amphibole, epidote, and chlorite (Pawley, 1994; Schmidt and Poli, 1998; Spandler et al., 2003; Usui et al., 2007; Martin et al., 2014).”
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- Authors
- Spandler, C., Hermann, J., Arculus, R., & Mavrogenes, J.
- Affiliations
- Australian National University (AU)
- Corresponding author
- Spandler, Carl
- Venue
- Contributions to Mineralogy and Petrology
- Published
- 2003-11-01
- Volume
- 146
- Issue
- 2
- Pages
- 205-222
- ISSN
- 0010-7999 (ISSN-L)
- 1432-0967
- OpenAlex
- W2092367277
- Cited by
- 367
- References
- 79
- Citations by year
- 2026: 8 · 2025: 11 · 2024: 17 · 2023: 17 · 2022: 13 · 2021: 25 · 2020: 18 · 2019: 20 · 2018: 19 · 2017: 19 · 2016: 20 · 2015: 19 · 2014: 21 · 2013: 11 · 2012: 22
- FWCI
- 11.13
- Type
- journal article
- Language
- en
- Open access
- bronze
- doi.org
- Licence
- www.springer.com/tdm (tdm)
- Locations
- Contributions to Mineralogy and Petrology (publishedVersion)
- ResearchOnline - JCU (James Cook University) (submittedVersion)
- BORIS (University Library Bern) (submittedVersion, other-oa)
- ANU Open Research (Australian National University) (submittedVersion)
- Open Access CRIS of the University of Bern
- 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 › Geophysics › High-pressure geophysics and materials
- Keywords
- trace element redistribution, prograde metamorphism, lawsonite blueschist, eclogite facies, subduction zone fluids, fluid release, dehydration reactions, trace element partitioning, fluid-rock interaction, partial melting, mantle wedge, New Caledonia
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