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Ultra-oxidized rocks in subduction mélanges? Decoupling between oxygen fugacity and oxygen availability in a Mn-rich metasomatic environment

  • Published:2015-06 Issue: Volume:226 Page:116-130
  • ISSN:0024-4937
  • Container-title:Lithos
  • language:en
  • Short-container-title:Lithos

Author:

Tumiati Simone,Godard Gaston,Martin Silvana,Malaspina Nadia,Poli Stefano

Funder

Italian Ministry of Education, University and Research (MIUR)

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference86 articles.

1. The Mn–Al–Si–O system: an experimental study of phase relations applied to parageneses in manganese-rich ores and rocks;Abs-Wurmbach;European Journal of Mineralogy,1999

2. Phase relations in the system Mn–Si–O: an experimental petrological study;Abs-Wurmbach;Neues Jahrbuch für Mineralogie (Abhandlungen),1983

3. Synthesis and physical properties of piemontite, Ca2Al3−pMn3+p(Si2O7/SiO4/O/OH);Anastasiou;Contributions to Mineralogy and Petrology,1977

4. Slab surface temperature in subduction zones: influence of the interpolate decoupling depth and upper plate thinning processes;Arcay;Earth and Planetary Science Letters,2007

5. Oxidation status of the mantle—past and present;Arculus;Annual Review of Earth and Planetary Sciences,1985
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