articleScienceApr 20, 2007Closed access

The Amount of Recycled Crust in Sources of Mantle-Derived Melts

Australian National University · Russian Academy of Sciences · +12 more institutions

Indexed incrossref

Abstract

Plate tectonic processes introduce basaltic crust (as eclogite) into the peridotitic mantle. The proportions of these two sources in mantle melts are poorly understood. Silica-rich melts formed from eclogite react with peridotite, converting it to olivine-free pyroxenite. Partial melts of this hybrid pyroxenite are higher in nickel and silicon but poorer in manganese, calcium, and magnesium than melts of peridotite. Olivine phenocrysts' compositions record these differences and were used to quantify the contributions of pyroxenite-derived melts in mid-ocean ridge basalts (10 to 30%), ocean island and continental basalts (many >60%), and komatiites (20 to 30%). These results imply involvement of 2 to 20% (up…

Citation impact

1,467
total citations
FWCI
48.69
Percentile
100%
References
38
Citations per year

Authors

20

Topics & keywords

Keywords
  • Eclogite
  • Peridotite
  • Geology
  • Geochemistry
  • Mantle (geology)
  • Basalt
  • Oceanic crust
  • Crust
UN Sustainable Development Goals
  • Life below water
No related works found for this paper.