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Contributions to Mineralogy and Petrology

, Volume 148, Issue 4, pp 506–509 | Cite as

Reply to comments on “Redistribution of trace elements during prograde metamorphism from lawsonite blueschist to eclogite facies: implications for deep subduction zone processes”

  • Carl SpandlerEmail author
  • Jörg Hermann
  • Richard Arculus
  • John Mavrogenes
Reply

We welcome the opportunity to reply to comments by Axel Liebscher regarding our manuscript (Spandler et al. 2003, Contrib Mineral Petrol 146:205–222). Before discussing the comments, we first wish to state that the phase identified as zoisite in the manuscript should have been labelled as epidote, due to the high ferric iron content. We wish to thank Axel Liebscher and Gerhard Franz for bringing this error to our attention. However, it should be noted that this error does not affect any of the conclusions of the paper, pertaining only to the correct application of epidote-group-mineral nomenclature.

The main focus of our paper is the distribution of trace elements among minerals during prograde subduction-zone metamorphism. We show that the breakdown of trace element-rich phases such as lawsonite and titanite does not lead to a significant change in the trace element content of rocks because the trace elements are redistributed into newly formed major and accessory phases. However, at...

Keywords

Mafic Rock Contrib Mineral Petrol Pelitic Rock Prograde Metamorphism Subducted Slab 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

References

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Copyright information

© Springer-Verlag 2004

Authors and Affiliations

  • Carl Spandler
    • 1
    Email author
  • Jörg Hermann
    • 2
  • Richard Arculus
    • 1
  • John Mavrogenes
    • 1
    • 2
  1. 1.Department of Earth and Marine SciencesAustralian National UniversityCanberraAustralia
  2. 2.Research School of Earth SciencesAustralian National UniversityCanberraAustralia

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